{"id":514,"date":"2019-03-10T12:16:12","date_gmt":"2019-03-10T12:16:12","guid":{"rendered":"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/?post_type=chapter&#038;p=514"},"modified":"2019-04-25T07:36:41","modified_gmt":"2019-04-25T07:36:41","slug":"aquatic-redox-chemistry","status":"publish","type":"chapter","link":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/chapter\/aquatic-redox-chemistry\/","title":{"rendered":"Aquatic Redox Chemistry"},"content":{"raw":"<div><span style=\"float: right\"><a href=\"https:\/\/youtu.be\/n4U3wpbQEl0\" target=\"_blank\" rel=\"noopener\"><img src=\"http:\/\/epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/2018\/11\/download.png\" alt=\"epgp books\" width=\"75px\" height=\"75px;\" \/><\/a>\r\n<\/span><\/div>\r\n<strong>Contents<\/strong>\r\n<ol>\r\n \t<li>Introduction<\/li>\r\n \t<li>Half Reactions<\/li>\r\n \t<li>Reduction Potential<\/li>\r\n \t<li>Standard Reduction Potential<\/li>\r\n \t<li>Interpretation and Significance<\/li>\r\n \t<li>Cell Reaction and Cell Potential<\/li>\r\n \t<li>Hydrogen Electrode and determination of Electrode Potential<\/li>\r\n \t<li>pE-Scale<\/li>\r\n \t<li>Significance of pE Values<\/li>\r\n \t<li>Measurement of pE-Values<\/li>\r\n \t<li>Solved Problem<\/li>\r\n \t<li>pE and pH Relationship<\/li>\r\n \t<li>Pourbaix diagram<\/li>\r\n \t<li>Interpretation and Significance<\/li>\r\n \t<li>Solved Problem<\/li>\r\n \t<li>The Limits of pE and pH in Natural Waters<\/li>\r\n \t<li>Redox Potentials in Natural Systems<\/li>\r\n \t<li>Redox Ladder<\/li>\r\n \t<li>Effect of redox on Metal Pollution<\/li>\r\n \t<li>Suggesting Reading<\/li>\r\n<\/ol>\r\n<strong>Introduction<\/strong>\r\n<p style=\"text-align: justify\">In aquatic environmental systems, including soils, sediments, aquifers, rivers, lakes, and water treatment systems, the most important and interesting chemical reactions occurring are the <strong>oxidation-reduction (redox)<\/strong> <strong>reactions<\/strong>. These reactions are central to major element cycling, to many sorption processes, to trace element mobility and toxicity, to most remediation schemes, and to life itself.<\/p>\r\n&nbsp;\r\n\r\n<em>Why study Redox Reactions?<\/em>\r\n\r\nThey fuel and constrain more or less all life processes.\r\n\r\nThey are a major determinant of chemical species present in natural environments.\r\n\r\n&nbsp;\r\n<p style=\"text-align: justify\"><strong>Redox reactions <\/strong>are core to many emerging domains of the aquatic sciences research, which includes all aspects of the aquatic sciences: involving the hydrosphere, aquatic (i.e., aqueous) aspects of environmental processes in the atmosphere, lithosphere, biosphere, etc. The <strong><em>Aquatic Redox Chemistry<\/em><\/strong> has multidisciplinary roots (straddling mineralogy to microbiology) and interdisciplinary applications (e.g., in removal of contaminants from sediment, soil or water).<\/p>\r\n<p style=\"text-align: justify\">To characterize the oxidation-reduction status of surface environments, the geochemists, soil scientists and limnologists have used redox potential (Ered) measurements. The redox potential of aquatic, marine and soil systems is a measure of electrochemical potential or electron availability within these systems. The redox potential (Ered) is determined from the concentration of oxidants and reductants in the environment. Oxygen, nitrate, nitrite, manganese, iron, sulphate, and CO2 are some of the prominent inorganic oxidants; while organic substrates and reduced inorganic compounds are the well-known reductants.<\/p>\r\n<p style=\"text-align: justify\">The redox-potential is the evaluation of the equilibrium potential, i.e. reduction\/oxidation potential, built at the interface between an electrode (a noble metal) and the solution consisting of electroactive redox species and is measured under standard state conditions (at 25 0C, 1 atmospheric pressure and one unit activity for all species) with respect to the standard hydrogen electrode. The term <strong>\u2018redox\u2019<\/strong> is the occurrence of both the chemical changes: oxidation and reduction, in a chemical reaction. The redox reactions i.e. oxidation-reduction reactions<\/p>\r\n<p style=\"text-align: justify\">entail the changes of oxidation states of reactants in a reaction and it is the sum up of two half reactions. The two processes: oxidation (loss of electrons) and reduction (gain of electrons) takes place together during the same reaction, i.e. oxidation\/reduction never takes place in isolation; hence, these reactions are called <strong>oxidation-reduction reactions <\/strong>or<strong> redox reactions. <\/strong>The potential of the overall reaction at the standard state<\/p>\r\n<p style=\"text-align: justify\">\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0+ E0red can be depicted as E0\u00a0 = E0 ox\u00a0 \u00a0 (where E0 ox \u00a0and E0red\u00a0 are the potentials of oxidation half-reaction and reduction half-reaction respectively)<\/p>\r\n<img class=\"aligncenter size-full wp-image-515\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-6.png\" alt=\"\" width=\"347\" height=\"299\" \/>\r\n<p style=\"text-align: justify\">In both these reactions, the hydrogen and carbon removes oxygen from copper(II) oxide and zinc oxide respectively, hence hydrogen and carbon are <strong>reducing agents<\/strong> or <strong>reductants<\/strong>. Similarly, those which are oxygen providers are called <strong>oxidizing agents<\/strong> or <strong>oxidants.<\/strong><\/p>\r\nThe modern electronic concept of <strong>oxidant<\/strong> and <strong>reductant<\/strong> is: one which accepts electrons is <strong>oxidant<\/strong> and one which donates electron is <strong>reductant.<\/strong>\r\n\r\nFor example:\u00a0 \u00a0 \u00a0 \u00a0Cl2\u00a0 + 2 I\u00a0 \u00a0------&gt;\u00a0 \u00a02 Cl\u00a0\u00a0\u00a0 + I2\r\n\r\nHere, Cl2 is an oxidant and I\u00a0 is a reductant; as I\u00a0 is oxidized to I2 by Cl2 and Cl2 is reduced to Cl\u00a0 \u00a0by I ).\r\n\r\n<img class=\"aligncenter size-full wp-image-516\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-7.png\" alt=\"\" width=\"529\" height=\"263\" \/>\r\n<p style=\"text-align: justify\">Thus, in a <strong>redox reaction<\/strong> which is brought about by loss and gain of electrons simultaneously, the oxidant is reduced and the reductant oxidized with an exchange of <em>n<\/em> electron (e ) which may be depicted as:<\/p>\r\n\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0Oxidant\u00a0 + <em>n<\/em> e\u00a0 -------&gt;\u00a0 reductant\r\n\r\nSome examples of Reductant in wetland soil are:\r\n<ol>\r\n \t<li>Organic matter &amp; other organic compounds;<\/li>\r\n \t<li>Reduced inorganic compounds, viz, Mn2+, S2 , CH4, H2, Fe2+, NH4 etc. Oxidants are inorganic compounds, viz, O2, NO3 , FeOOH, SO42 , HCO3 etc.<\/li>\r\n<\/ol>\r\n<p style=\"text-align: justify\">It may be noted that in the overall redox reaction no free electrons are generated. The movement of electrons is from reductant to oxidant, thereby an electrical potential is developed between the two which is measured in volts and denoted by E\u00b0. Since the redox potential depends on the members of the pair in a reaction, hence it\u2019s a relative rather than an absolute value. The standard redox potential values for elements, compounds and ions can be ascertained under standard conditions (unit molar concentration at 1 atm pressure and 25 0C), relative to a standard hydrogen electrode (SHE) potential (which is arbitrarily given a potential, E\u00b0 = zero volts). The greater the positive potential, the more anticipated it will be reduced.\u00a0The redox-potentials (also known as electrochemical version of Gibbs free energy G) are used to ascertain the direction and the free energy (the change in the system\u2019s free energy G) of redox-reaction at standard states as:\u00a0 G0 (eV) =\u00a0\u00a0\u00a0 nF\u00a0\u00a0 E\u00b0<\/p>\r\n<p style=\"text-align: justify\">where F is the Faraday constant number (96,485 C\/mol or 96,485 J\/mol\/V or \u2248100 kJ\/mol\/V) and n is the number of electrons involved in the redox-reaction). (The 0 symbol is for the substances involved in the reaction in their standard states).<\/p>\r\n<p style=\"text-align: justify\">For non-standard redox-reactions, the difference in redox-potential (precisely reduction potential E) is correlated to G as: \u0394G (eV) = -nF E<\/p>\r\n<strong>Half-Reactions<\/strong>\r\n<p style=\"text-align: justify\"><strong>A half reaction <\/strong>is either the reduction or the oxidation reaction component of a redox-reaction. The reactions occurring in an electrochemical cell is frequently described on the basis of the half-reaction concept. A redox reaction is expressed as the difference of two reduction <strong>half-reactions.\u00a0<\/strong><\/p>\r\n<img class=\"aligncenter size-full wp-image-517\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-8.png\" alt=\"\" width=\"685\" height=\"467\" \/>\r\n\r\n&nbsp;\r\n\r\nSimilarly, adding the simultaneously occurring two half reactions of metallic zinc atoms reaction with aqueous nickel ions give the net redox-reaction\r\n\r\n<img class=\"aligncenter size-full wp-image-518\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-9.png\" alt=\"\" width=\"283\" height=\"119\" \/>\r\n\r\nThe half-reactions depict the exact oxidation state changes happening in two half-reactions.\r\n\r\n<strong>Reduction Potential<\/strong>\r\n\r\n<strong>Definition<\/strong>\r\n<p style=\"text-align: justify\">By definition, redox-potential (reduction potential\/electrode potential) is the tendency of a substance to accept electrons. The positive (high) values of electrode potential means that the elements or ions would readily accept electrons; on the other hand, negative (low) values indicate their easy capability of electron donation.<\/p>\r\nFew examples are cited below:\r\n\r\n<img class=\"aligncenter size-full wp-image-519\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-10.png\" alt=\"\" width=\"451\" height=\"129\" \/>\r\n<p style=\"text-align: justify\">The <strong>standard reduction potential<\/strong> Eored is measured <em>relative<\/em> to: 2H+(aq) + 2e H2(g) (which has an assigned value Eored= 0.00 V and hence treated as reference)<\/p>\r\n<p style=\"text-align: justify\">Measurement of redox potential, E, allows quantitative appraisal of the force and tendency of the system. It can be measured by the difference between the potential of the hydrogen electrode (or more easily, the calomel electrode) and the potential of a platinum electrode immersed in the medium.<\/p>\r\n<strong>Interpretation and Significance<\/strong>\r\n<p style=\"text-align: justify\">Redox (electron-transfer) reactions provide the energetic basis for the life process, and through this, play a decisive role in the geochemical cycle of the elements. Redox reactions are very significant in water-saturated environments, such as sediments, soils, and sludges. Actually, all aquatic organisms obtain their energy for metabolic processes from oxidation-reduction reactions. Photosynthetic organisms catalytically reduce CO2 to reduced organic matter by locking light energy, while non-photosynthetic organisms catalytically decompose the organic products of photosynthesis through energy-yielding redox reactions. One of the major elements in the terrestrial and aquatic environments \u2013 nitrogen \u2013 circulates by many microbially catalyzed redox reactions. In truth, the only non-redox process in the entire nitrogen cycle is NH3 integration with and liberation from N-containing organic matter. The movements of many other elements also involve redox reactions, such as C, Fe, and S. The oxidizing power of anaerobic environments in the biosphere is mainly controlled by five molecules. In decreasing order of energy produced, they are nitrate (NO3\u2013), manganese dioxide (MnO2), ferric hydroxide (Fe(OH)3), sulfate (SO42\u2013) and, under extreme conditions, carbohydrate (CH2O) itself.<\/p>\r\n<p style=\"text-align: justify\">Like Gibb\u2019s free energy (G), the redox potentials (E) are not absolute. The redox potentials are measured with reference to the reduction of hydrogen ions to hydrogen gas at standard state conditions (SHE), i.e., 25 degrees Celsius (\u00b0C), 1 atmospheric pressure, and one unit activity for all species. The potential of this reaction, by convention, is taken as zero. Furthermore, as the redox potentials are comprised of two parts: the oxidation potential, and the reduction potential, the potential of the overall reaction of a cell at the standard state can be\u00a0<span style=\"text-align: initial;font-size: 1em\">expressed as:\u00a0 \u00a0E0<sub>cel<\/sub>l = E<sup>0<\/sup><sub>ox<\/sub> + E<sup>0<\/sup><\/span><\/p>\r\n<p style=\"text-align: justify\">A positive Eored indicate that a half-reaction will proceed in the direction indicated (reduction) when paired with the hydrogen half-reaction where as a negative Eored means that a half-reaction will move in the opposite direction indicated (oxidation).<\/p>\r\n<p style=\"text-align: justify\">The numerical values of E\u00b0ox and E\u00b0red of a substance in a half-reaction are the same with opposite in sign (until the conditions are changed). Thus, numerically, the potential for oxidation half-reaction is the negative of the potential of the reduction half-reaction, i.e. E\u00b0ox = E\u00b0red (with opposite sign). The voltage produces by an electrochemical cell is determined by summing up all the potentials in circuit, as:<\/p>\r\n<img class=\"aligncenter size-full wp-image-520\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-11.png\" alt=\"\" width=\"201\" height=\"49\" \/>\r\n\r\n<img class=\"aligncenter size-full wp-image-521\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-12.png\" alt=\"\" width=\"471\" height=\"545\" \/>\r\n<p style=\"text-align: justify\">The value of redox potential (E) (for non-standard states) under concentration conditions can be related to standard potential (E0) by the <strong>Nernst equation<\/strong>:<\/p>\r\nE = E0 + RT\/nF * ln {(Ox)\/(Red)} = E0 RT\/nF * ln {(Red)\/(Ox)} = E0 RT\/nF * ln Q\r\n\r\nOr at 298 K, this is expressed as: E = E0 0.0592\/n * log {(Red)\/(Ox)}\r\n<p style=\"text-align: justify\">where, E0 = standard electrode potential, R = ideal gas constant (8.314 J\/mol-K); T = absolute temperature (Kelvin); n = number of electrons involved in the reaction; F = the Faraday constant number and (Red)\/(Ox) is the concentration ration of reduced and oxidized forms of a given reaction pair, i.e. the reaction quotient.<\/p>\r\n<p style=\"text-align: justify\">The important factors upon which the redox potential of a substance depends are: nature of the substance, its affinity for electron, concentration of reductants and oxidants (referred as redox pair) and temperature.<\/p>\r\n&nbsp;\r\n\r\n<strong>Solved Problem <\/strong>(based on Nernst equation)<strong>:<\/strong>\r\n\r\nFor the half reaction 2H+ + 2e\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 = H2. What is E1\/2 at pH 5 and PH2 = 1 atm?\r\n\r\n<strong>Solution: <\/strong>pH =\u00a0\u00a0\u00a0 log [H+] = 5, therefore [H+] = 10-5 M.\r\n\r\nIn the above half-reaction, n = 2.\r\n\r\nPutting these values in the Nernst equation: E = E0 0.0592\/2 * log PH2\/(H+)2 E = E0 0.0592\/2 * log (105)2\r\n\r\nSince, for the given half-reaction, the E01\/2 = 0 V, hence, E = 0.000\u00a0 0.0592\/2 * (10)\r\n\r\nTherefore, E =\u00a0\u00a0 0.296 V.\r\n<p style=\"text-align: justify\">Many electrode combinations are possible in electrochemical cells, and it is convenient to specify a standard potential, Eo, for each electrode by referencing it to the SHE (whose standard potential is defined as zero). There are many half-reactions whose electrode potential cannot be measured, because the electron transfer reaction at an electrode is too slow.<\/p>\r\nThese potentials can nevertheless be calculated from the free energy of appropriate redox reactions\r\n\r\nFor example, the formation of NO from N2 and O2 is a redox reaction:\r\n\r\n<img class=\"aligncenter size-full wp-image-522\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-13.png\" alt=\"\" width=\"463\" height=\"97\" \/>\r\n<p style=\"text-align: justify\">From the free energy of the overall reaction 173.4 kJ, we obtain a cell potential of -0.45 V (using equation <em>G <\/em>= \u2013<em>n<\/em>F E). Then knowing that the standard potential of the oxygen electrode is 1.24 V, we can readily evaluate the standard potential for half reaction as 1.69 V, (1.24 V \u2013[\u20100.45 V]), even though it is impossible to measure this potential directly because the electron transfer between the electrode and NO and N2 molecules is too slow to establish a reversible potential.<\/p>\r\n<strong>Significance of Redox Electrodes, Redox Potentials &amp; Redox Reactions in the determination of:<\/strong>\r\n\r\n&nbsp;\r\n<ul>\r\n \t<li>mobility and toxicity of chemical species in the environment (natural aquatic systems vary widely in redox conditions; therefore, fate may constantly change);<\/li>\r\n \t<li>equilibrium constant: single electrode potentials may be used to determine equilibrium constants of ionic reactions;<\/li>\r\n \t<li>solubility product of a sparingly soluble salt;<\/li>\r\n \t<li>pH, using hydrogen electrode<\/li>\r\n<\/ul>\r\n<strong>Cell Reaction and Cell Potential<\/strong>\r\n<p style=\"text-align: justify\">Let us see how the redox-reactions are a source of electric current in the electrochemical cells (a device for producing current from a chemical (redox) reaction).<\/p>\r\n<p style=\"text-align: justify\">For example, in the redox-reaction: Cu2+(aq) + Zn(s) &lt;-----&gt; Cu(s) + Zn2+(aq); the electrons released from a half-reaction, i.e. oxidation of Zn(s) are consumed by the other half-reaction, i.e. reduction of Cu2+(aq). Since both the reactions occur on the zinc electrode itself (dipped in CuSO4 solution), there is no net charge.<\/p>\r\n<p style=\"text-align: justify\">Now, if the two half-reactions occur in two separate compartments (one with Zn rod dipped in ZnSO4 solution and other with Cu rod dipped in CuSO4 solution) and both well connected by a wire, there will be a net flow of electrons from the reductant in one compartment to the oxidant in another through wire. However, the flow of current will be instant and later it will stop due to charge built up in the two compartments. The current flow can be restarted just by connecting the two compartments by a <strong>Salt bridge<\/strong> (a U-tube filled with an electrolyte such as NaCl, KCl, K2SO4 etc.) thus providing a passage to ions from one compartment to other without extensive mixing of the two solutions. This will complete the circuit and the electrons pass freely through the wire to maintain the net charge zero in the two compartments. This kind of circuitry cell is a simple <strong>Voltaic (Galvanic)<\/strong> <strong>cell <\/strong>where electrical current is generated by a spontaneous redox reaction.<\/p>\r\n<img class=\"aligncenter size-full wp-image-523\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-14.png\" alt=\"\" width=\"375\" height=\"329\" \/>\r\n<p style=\"text-align: justify\">In an electrochemical cell, the flow of electrons from one electrode to the other is due to the half-reactions occurring in the anodic and cathodic compartments and the addition of these two half-reactions gives the net chemical change called as <strong>cell reaction<\/strong>. Thus, the E\u00b0 (electrode potential) for a given substance can be determines by constructing an electrochemical cell consisting of two half-cells. If the flow of electrons is from oxidant (hydrogen half-cell) to the other half-cell, the substance has a positive redox potential; whereas the E\u00b0 negative indicate the substance is reductant. Knowing the redox potentials values of two substances will help to predict whether a redox reaction between them is theoretically possible.<\/p>\r\n<p style=\"text-align: justify\">In electrochemical cells, or in redox reactions that happen in solution, the thermodynamic driving force can be measured as the <strong>cell potential<\/strong>. Chemical reactions are spontaneous in the direction of -\u0394G, which is also the direction in which the cell potential (defined as Eanode - Ecathode) is positive. A cell operating in the <strong>spontaneous<\/strong> direction (for example, a battery that is discharging) is called a <strong>galvanic cell<\/strong>. A cell that is being driven in the <strong>non-spontaneous<\/strong> direction is called an <strong>electrolytic cell<\/strong>.<\/p>\r\n<strong>Hydrogen Electrode and Determination of Electrode Potential<\/strong>\r\n\r\nHydrogen electrode is based on the redox half cell:\r\n\r\n2 H+ (aq) + 2e\u00a0 &lt;----&gt; H2 (g)\r\n<p style=\"text-align: justify\">The <strong>Standard hydrogen electrode (SHE)<\/strong> is a redox electrode which forms the basis of the thermodynamic scale of oxidation-reduction potentials. The absolute electrode potential of SHE is estimated to be 4.44 \u00b1 0.02 V at 25 \u00b0C, but for constructing a base for comparison with all other electrode reactions, hydrogen\u2019s standard electrode potential, E<sup>0<\/sup>, is declared to be zero at all temperature. The absolute electrode potential, according to IUPAC, is the electrode potential of a metal measured with respect to a universal reference system (without any additional metal-solution interface).<\/p>\r\n<p style=\"text-align: justify\">The standard electrode potential, E<sup>0<\/sup>, is measured under standard conditions: 25 <sup>0<\/sup>C, 1 M concentration for each ion participating in the reaction, a partial pressure of 1 atm for each part of the reaction, and metals in their pure state. The standard reduction potential is defined relative to a SHE reference electrode (arbitrary with a potential 0.00 V). Since, E<sup>0<\/sup> (SHE) = 0, E<sup>0<\/sup> for other half reaction can be &gt;0 [oxidizes H2 (g) or &lt;0 [is oxidized by H2 (g)].<\/p>\r\n<img class=\"aligncenter size-full wp-image-525\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-16.png\" alt=\"\" width=\"225\" height=\"243\" \/>\r\n\r\nThe conventions for E\u00ba:\r\n<ul>\r\n \t<li>E\u00ba values (units of volts) are compared on the basis of half reactions, which by convention are written as reductions;<\/li>\r\n \t<li>all substances are assumed to be at unit activity;<\/li>\r\n \t<li>all E\u00ba values are determined relative to the reduction potential of the standard hydrogen electrode (SHE).<\/li>\r\n<\/ul>\r\n<ol>\r\n \t<li>If the E\u00ba for a given half-reaction is &gt;0, that couple has the potential (under standard conditions) to oxidize the SHE;<\/li>\r\n \t<li>A negative E\u00ba indicates a couple that can reduce the SHE (at standard conditions).<\/li>\r\n<\/ol>\r\n<strong>\u00a0<img class=\"aligncenter size-full wp-image-526\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-17.png\" alt=\"\" width=\"309\" height=\"257\" \/><\/strong>\r\n\r\n<strong>pE-Scale<\/strong>\r\n<p style=\"text-align: justify\">The most important factor affecting redox reactions of some species is pH, and the effects are very well illustrated by Eh-pH (or p<em>e<\/em>-pH, or pE-pH, or Pourbaix) diagrams. Since it is frequently difficult to determine which half-reactions are actually coupled in nature, the concept of pE is preferred.<\/p>\r\n<p style=\"text-align: justify\">pE may be defined as the <em>activity<\/em> of the free electron in water, thus only half reactions can be focused upon. Forever, the reactions are expressed as the reduction half reaction. From the equation: G<sup>0<\/sup> = \u2013<em>n<\/em>F E, a negative G<sup>0<\/sup> corresponds to a positive E<sup>0<\/sup>, and thus to a potentially spontaneous reduction half-reaction (at standard conditions) versus the SHE.<\/p>\r\nFor graphical expressions, <strong>pE<\/strong> is negative log of electron activity, i.e., pE = -log(e ) = F E<sup>0<\/sup> \/ 2.3 RT = 1\/n log K = -1\/n G<sup>0<\/sup> \/ 2.3 RT.\r\n<p style=\"text-align: justify\">Or, the pE equation can be expressed as: pE = pE<sup>0<\/sup> - log (Red) \/ (Ox); where pE<sup>0<\/sup> can be calculated from log K. If the equilibrium distribution of (Red)\/(Ox) is known, this equation can be used to solve for the pE of the environment.<\/p>\r\nFor example, for the half-reaction Cu<sup>2+<\/sup> + 2e -----&gt; Cu (s);\r\n\r\nSince n = two electrons involved and K= 1\/({Cu2+} {e }2), therefore, pE will be expressed as:\r\n\r\npE = 1\/2 log K + 1\/2 Log {Cu<sup>2+<\/sup>}\r\n\r\n[as\u00a0 pE<sup>0<\/sup> = 1\/n log K and pE = pE<sup>0<\/sup> + (1\/n) log {ox}\/{red}]\r\n\r\npE<sup>0<\/sup> is readily obtainable from thermodynamic data, now multiplying both the sides of above equation by 2.303\r\n\r\nRT\/F, equation becomes:\r\n\r\npE = F\/(2.303RT) EH\r\n\r\npE<sup>0<\/sup> = 16.90 E0H\r\n\r\npE<sup>0<\/sup> = -1\/n (1.753x10-4) ( G0)\r\n\r\nG<sup>0<\/sup> =\u00a0\u00a0\u00a0\u00a0 G0f (products) -\u00a0 G0f (reactants)\r\n\r\n<strong>Significance of pE Values<\/strong>\r\n<p style=\"text-align: justify\">At equilibrium, solution has one pE value; if this is assumed, the ratio of oxidized to reduced species activities can be calculates; moreover, determination of prominent species is possible. Usually, electrons move from high to low activity (Ae); small pE corresponds to reducing environments, reduced species predominates; and large pE correspond to oxidizing environments, oxidized species predominates. The pE diagrams can be an asset to know how species predominate as a function of pE.<\/p>\r\n<strong>Measurement of pE Values<\/strong>\r\n<p style=\"text-align: justify\">The pE0 of a half reaction expresses the electron activity required to maintain reactants and products at unit activities. There are two main types of redox calculations. The first is the calculation of what controls the pE of the environment. This is analogous to calculating the pH of the environment.<\/p>\r\n<p style=\"text-align: justify\">The second type of calculation is to determine how trace species respond or distribute themselves with respect to that pE. Again by analogy, when we know the pH, we can calculate the pH dependent speciation of trace species.<\/p>\r\n<strong>Solved Problem:<\/strong>\r\n\r\nFor the reduction:\u00a0 Fe3+ + 2e -----&gt; Fe2+\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 K = 10<sup>13<\/sup>\r\n<p style=\"text-align: justify\">The electron activity of the solution must be held to the very low value of 10<sup><em>-<\/em>13<\/sup> (pE = 13) to maintain equal activities of the two ions; this corresponds to usually referred as an oxidizing environment.<\/p>\r\nThe value of K = 1013 actually refers, of course, to the reaction; Fe<sup>3<\/sup><span style=\"text-align: initial;font-size: 1em\"><sup>+<\/sup> + H<\/span><sup style=\"text-align: initial\">2<\/sup><span style=\"text-align: initial;font-size: 1em\"> -----&gt;\u00a0Fe<\/span><sup style=\"text-align: initial\">2+<\/sup><span style=\"text-align: initial;font-size: 1em\">\u00a0 + 2H<\/span><sup style=\"text-align: initial\">+<\/sup>\r\n\r\nK = {Fe2+} {H+} \/{Fe3+} {<em>P<\/em>H52}\r\n<p style=\"text-align: justify\">So that the equilibrium condition {Fe3+} = {Fe2+} would require a pH of 13 at this unit pressure of H2 or a hydrogen partial pressure of 1026 atm at zero pH.<\/p>\r\n<strong>pE and pH Relationship:<\/strong>\r\n\r\n<strong><em>Pourbaix Diagram<\/em><\/strong>\r\n<p style=\"text-align: justify\">A <strong>Pourbaix diagram<\/strong> (also known as <strong>Potential\/pH diagram, E<\/strong><strong>H<\/strong><strong>-pH diagram<\/strong> or a <strong>pE\/pH diagram<\/strong>) is essentially an <strong>electrochemical phase diagram,<\/strong> the best representation of the possible thermodynamically stable phases of an aqueous electrochemical system (i.e. redox-active substances). The diagrams are invented by the Russian born, Belgium Chemist <strong>Marcel Pourbaix<\/strong> (1904-1998) and are named after him.<\/p>\r\n<img class=\"aligncenter size-full wp-image-527\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-18.png\" alt=\"\" width=\"467\" height=\"399\" \/>\r\n<p style=\"text-align: justify\">The diagrams have two axes, the vertical axis labeled as pE or EH represent the voltage potential with respect to SHE (as EH (SHE)\/V; where H stands for hydrogen); and the horizontal axis measures pH. The lines depict the conditions under which two phases coexist in equilibrium and also the redox and acid-base reactions. The<\/p>\r\n<p style=\"text-align: justify\">shaded area represents the conditions of potential and pH for the stable phase of the substance, whereas outside the shaded region represents the thermodynamically unstable phase which either gets reduced or oxidized.<\/p>\r\n<p style=\"text-align: justify\">Eh-pH diagram showing the predominance fields for oxidized (upper right) and reduced (lower left) forms of selected redox-active species. Dashed diagonal lines are for the H2\/H2O (lower) and H2O\/O2 (upper) couples and together they enclose the conditions over which water is stable.<\/p>\r\n<strong>Interpretation and Significance<\/strong>\r\n<p style=\"text-align: justify\">A Pourbaix diagram designates mainly three regions: \u2018immunity\u2019, \u2018corrosion\u2019 and \u2018passivity\u2019 instead of stable species. These regions describe the stability of a particular substance in a specific environment. \u2018Immunity\u201d indicate the safe and non-attacked region which is opposite to the \u2018corrosion\u2019 region; \u2018passivity\u2019 other hand depict the relative stability (i.e. when a metal forms a stable oxide or other salt coating on its surface).<\/p>\r\nFor example, in the Pourbaix diagram for Fe (above):\r\n\r\n<strong>Areas <\/strong>in the Pourbaix diagram mark regions where a single species (Fe2+(aq), Fe3O4(s), etc.) is stable. More stable species tend to occupy larger areas.\r\n\r\n<strong>Lines <\/strong>mark places where two species exist in equilibrium.\r\n<p style=\"text-align: justify\"><strong>Pure redox <\/strong>reactions are<strong> horizontal <\/strong>lines - these reactions are not pH-dependent<strong> Pure acid-base <\/strong>reactions are<strong> vertical <\/strong>lines - these do not depend on potential Reactions that are <strong>both<\/strong> acid-base and redox have a slope of -0.0592 V\/pH x4H+\u20444e-)<\/p>\r\nIllustration of equilibria in the iron Pourbaix diagram (numbered on the plot):\r\n<ol>\r\n \t<li>Fe2+ + 2e- \u2192 Fe (s) (pure redox reaction - no pH dependence)<\/li>\r\n \t<li>Fe3+ + e- \u2192 Fe2+ (pure redox reaction - no pH dependence)<\/li>\r\n \t<li>2 Fe3+ + 3 H2O \u2192 Fe2O3(s)+ 6H+ (pure acid-base, no redox)<\/li>\r\n \t<li>2 Fe2+ + 3 H2O \u2192 Fe2O3(s)+ 6H+ + 2e- (slope = -59.2 x 6\/2 = -178 mV\/pH)<\/li>\r\n \t<li>2 Fe3O4(s) + H2O \u2192 3 Fe2O3(s) + 2H+ + 2e- (slope = -59.2 x 2\/2 = -59.2 mV\/pH)<\/li>\r\n<\/ol>\r\n<p style=\"text-align: justify\">For an element, such as iron, the water redox lines have special significance on a Pourbaix diagram. In other case, such as liquid water, it is stable <em>only<\/em> in the region between the dotted lines. Below the H2 line, water is unstable relative to hydrogen gas, and above the O2 line, water is unstable with respect to oxygen; while, for active metals such as Fe, the region where the pure element is stable is typically below the H2 line. This means that iron metal is unstable in contact with water, undergoing reactions:<\/p>\r\nFe(s) + 2H+ \u2192 Fe2+(aq) + H2 (in acid)\r\n\r\nFe(s) + 2 H2O \u2192 Fe(OH)2(s) + H2 (in base)\r\n<p style=\"text-align: justify\">Iron (and most other metals) are also thermodynamically unstable in air-saturated water, where the potential of the solution is close to the O2 line in the Pourbaix diagram. Here the spontaneous reactions are:<\/p>\r\n4 Fe(s) + 3 O2 + 12H+ \u2192 4 Fe3+ + 6 H2O (in acid)\r\n\r\n4 Fe(s) + 3 O2 \u2192 2 Fe2O3(s) (in base)\r\n\r\n<img class=\"aligncenter size-full wp-image-528\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-19.png\" alt=\"\" width=\"579\" height=\"511\" \/>\r\n\r\n<img class=\"aligncenter size-full wp-image-529\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-20.png\" alt=\"\" width=\"545\" height=\"543\" \/>\r\n<p style=\"text-align: justify\">Line-a \u2013 depicting Reducing limit and Line-b \u2013 depicting Oxidizing limit. Below line-a (zone-I) is too reducing for water; whereas above line-b (zone-III) is too oxidizing for water. Zone falling in between Reducing &amp; Oxidizing limits, i.e. between the two parallel lines a &amp; b (zone-II) is just right for water.<\/p>\r\nSimilarly, Pourbaix diagram for other ions in the water stability field can be drawn.\r\n<p style=\"text-align: justify\">The creation of phase diagram for any solute ion, or combination of solute ions will illustrate the <em>speciation<\/em> (form) of that\/those ion(s) in EH vs pH or pE vs pH space for a given solute concentration in solution. Though creating phase diagram for mixed ions are quite complex in comparison to single ion diagrams.<\/p>\r\n<strong>Applications:<\/strong>\r\n\r\nMonitoring of industrial waste water\r\n\r\nSwimming pool water monitoring\r\n\r\nSoil investigation\r\n\r\nFreshwater habitat quality\r\n\r\n<strong>Redox potentials in natural systems:<\/strong>\r\n<p style=\"text-align: justify\">At almost neutral pH (7-8), the redox potentials in natural waters range from about \u2013400 mV to +800 mV. They are bounded in the negative range by the reduction of H2O to hydrogen gas (H2(g)) and in the positive range by the oxidation of H2O to O2(g).<\/p>\r\nIn water and sediment, four representative ranges of redox potentials exist:\r\n<ol>\r\n \t<li style=\"text-align: justify\">Range I: <em>For oxygen-bearing waters<\/em>: water saturated with oxygen may have a redox potential within the first range (710 to 800 mV at pH 7 to 8).<\/li>\r\n \t<li style=\"text-align: justify\">Range II: in systems where some oxygen has been consumed, the redox potentials may range between \u2013 100 to 710 mV (at pH 7 to 8). It is representative of many ground and soil waters where O2 has been 2consumed (by degradation of organic matter), but SO4 is not yet reduced. In this range soluble Fe (II) and Mn (II) are present; their concentration is redox-buffered because of the presence of solid Fe (III) and Mn (III, IV) oxides.<\/li>\r\n \t<li style=\"text-align: justify\">Range III: though the potential is not sensitive to oxygen concentrations and has been observed to remain nearly constant down to values of 0.1% O2 saturation. It is characterized by SO4 \/ HS or SO4 \/ FeS2 redox equilibria.<\/li>\r\n \t<li style=\"text-align: justify\">Range IV: <em style=\"text-align: initial;font-size: 1em\">for anaerobic sediments and sludges<\/em><span style=\"text-align: initial;font-size: 1em\"><span style=\"text-align: initial;font-size: 1em\">: Within the second range, solid Fe (III), and Mn (III, IV) are reduced to soluble Fe (II) and Mn (II) when organic matter is mineralized. Phosphorus, which is\u00a0<\/span><\/span>Many researchers have studied the relationships between oxidation-reduction potential and the physical, chemical, and biological processes in soil-water systems. One of the pioneers in this field was Mortimer (1941, 1942). Mortimer studied the factors which control the rate of nutrient supply to phytoplankton in systems of lake water and sediment deposits.<\/li>\r\n<\/ol>\r\n<img class=\"aligncenter size-full wp-image-530\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-21.png\" alt=\"\" width=\"351\" height=\"291\" \/>\r\n\r\n&nbsp;\r\n\r\n<strong>Figure 3: <\/strong>Redox intensity representative ranges in soil and water. (pE = 16.9 E ).\r\n\r\n<strong>Redox Ladder:<\/strong>\r\n<p style=\"text-align: justify\">The change in the pE of a fresh natural water in contact with sediment as a function of amount of organic matter decomposed or in other words, the <strong>Redox Ladder<\/strong> may be defined as: the step by step sequencing of common redox. The redox reactions occurring in an aquatic environment, a step wise pE sketch is formed in which at a particular place or time, pE is fixed until a particular oxidant is consumed.<\/p>\r\n<p style=\"text-align: justify\">As illustrated in fig., at almost 7 pH, the change in the pE of fresh natural water in contact with sediment as a function of amount of organic matter decomposed. The amount of the organic matter reacted is depicted horizontally (thus its length depends on the availability of specific solid phases for reaction).<\/p>\r\n<img class=\"aligncenter size-full wp-image-533\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-22.png\" alt=\"\" width=\"231\" height=\"195\" \/>\r\n\r\n<strong>Effect of redox on metal pollution:<\/strong>\r\n<p style=\"text-align: justify\">Changes in the redox potential can have important consequences for environmental pollution, especially with respect to metal ions such as cadmium, lead, and nickel. In general, the solubility of heavy metals is highest in oxidizing and acidic environments (Figure: Eh\/pH as a function of different aquatic environments). At neutral to alkaline pHs in oxidizing environments, these metals often adsorb onto the surface of insoluble Fe(OH)3 and MnO2 particles, especially when phosphate is present to act as a bridging ion. When the redox potential shifts to only slightly oxidizing or slightly reducing conditions as a result of microbial action, and the pH shifts toward the acidic range, Fe(OH)3 and MnO2 in soils and sediments are reduced and solubilized. The adsorbed metal ions likewise become solubilized and move into groundwater (or into the water column of lakes when there is Fe(OH)3 or MnO2 in the sediment). Conversely, if sulfate is reduced microbially to HS\u2013 metal ions are immobilized as insoluble sulfides. But if sulfide rich sediments are exposed to air through drainage or dredging operations, then HS\u2013 is oxidized back to sulfate, and the heavy metal ions are released.<\/p>\r\n<img class=\"aligncenter size-full wp-image-534\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-23.png\" alt=\"\" width=\"419\" height=\"353\" \/>\r\n<p style=\"text-align: justify\"><strong>Figure 4: <\/strong>EH\/pH as a function of different aquatic environments. Oval enclosed by dashed line indicates region of highest solubility of heavy metals. [<em>Source:<\/em> Adapted from W. Salomons (1995). Long\u2010term strategies for handling contaminated sites and large\u2010scale areas. In <em>Biogeodynamics of Pollutants in Soils and Sediments<\/em>, W Salomons and W.M. Stigliani, eds. (Berlin: Springer\u2010Verlag)].<\/p>\r\n<p style=\"text-align: justify\">A particularly important instance of biological redox mediation of heavy-metal pollution occurs in the case of mercury. Inorganic mercury, in any of its common valence states, Hg0, Hg22+, and Hg2+, is not toxic when ingested; it tends to pass through the digestive system, although Hg0 is highly toxic when inhaled. But the methylmercury ion (CH3)Hg+ is very toxic, regardless of the route of exposure. The environmental route to toxicity involves sulfate reducing bacteria that live in anaerobic sediments. As part of their metabolism these bacteria use methyl groups to produce acetate. When exposed to Hg2+ the bacteria transfer the methyl groups to the mercury, producing (CH3)Hg+; because methylmercury is soluble, it enters the aquatic food chain, where it is bioaccumulated in the protein-laden tissue of fish.<\/p>\r\n<table>\r\n<tbody>\r\n<tr>\r\n<td><strong>you can view video on Aquatic Redox Chemistry<\/strong><\/td>\r\n<td><a href=\"https:\/\/youtu.be\/n4U3wpbQEl0\" target=\"_blank\" rel=\"noopener\"><img class=\"alignnone wp-image-120\" src=\"http:\/\/epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/2018\/11\/download.png\" alt=\"\" width=\"36\" height=\"36\" \/><\/a><\/td>\r\n<\/tr>\r\n<\/tbody>\r\n<\/table>\r\n\r\n<strong>Suggested Reading<\/strong>\r\n<ol>\r\n \t<li>Stanley E. Manahan, Environmental Chemistry, 9th Edition, CRC Press, New York, 2009.<\/li>\r\n \t<li style=\"text-align: justify\">Colin Baird and Michael Cann, Environmental Chemistry, 4th Edition, WH Freeman, New York, 2008.<\/li>\r\n \t<li style=\"text-align: justify\">Peter Atkins and Julio de Paula, Elements of Physical Chemistry, 5th Edition, Oxford University Press Inc., New York, 2009.<\/li>\r\n \t<li>Richard Harwood, Chemistry: New Edition, Cambridge University Press, UK, 2002.<\/li>\r\n \t<li>Brian J Knapp, Oxidation and Reduction, CT Danbury, Grolier Educational, 1998.<\/li>\r\n \t<li style=\"text-align: justify\">J C Morris; W Stumm, Redox equilibria and measurements of potentials in the aquatic environment. In Equilibrium Concepts in Natural Water Systems; ACS Symposium Series No. 67; American Chemical Society: Washington, DC, 1967; pp 270\u2212285.<\/li>\r\n \t<li style=\"text-align: justify\">M. Taillefert, T. F. Rozan, Eds.; Environmental Electrochemistry: Analyses of Trace Element Bigeochemistry<span style=\"text-align: initial;font-size: 1em\">; ACS Symposium Series No. 811; American Chemical Society: Washington, DC, 2002.<\/span><\/li>\r\n \t<li style=\"text-align: justify\">K R Reddy and R Delaune, Biogeochemistry of wetlands, 2004, CRC.<\/li>\r\n \t<li style=\"text-align: justify\">T. Borch, R. Kretzschmar, A. Kappler, P. V. Cappellen, M. Ginder-Vogel, A. Voegelin, K. Campbell, Biogeochemical redox processes and their impact on contaminant dynamics. Environ. Sci. Technol. 44, 2010, 15\u201323.<\/li>\r\n \t<li style=\"text-align: justify\">Werner Stumm,\u00a0 James\u00a0 J.\u00a0 Morgan,\u00a0 Aquatic\u00a0 Chemistry:\u00a0 Chemical\u00a0 Equilibria and\u00a0 Rates\u00a0 in\u00a0 Natural Waters, 3rd Edition, John Wiley &amp; Sons, Inc., <span style=\"text-align: initial;font-size: 1em\">(1995) Pp. 1040. ISBN: 978-0-471-51185-4.<\/span><\/li>\r\n \t<li style=\"text-align: justify\">Aquatic Redox Chemistry, Editor(s): Paul G. Tratnyek, Timothy J. Grundl, Stefan B. Haderlein, Vol 1071, American Chemical Society, 2011. ISBN13: 9780841226524.<\/li>\r\n \t<li style=\"text-align: justify\">Andri Stef\u00e1nsson, Stef\u00e1n Arn\u00f3rsson, \u00c1rn\u00fd E. Sveinbj\u00f6rnsd\u00f3ttir, Redox reactions and potentials in natural waters at disequilibrium, Chemical Goelogy, 221, (3\u20134) 2005, Pp. 289\u2013311.<\/li>\r\n<\/ol>\r\n&nbsp;\r\n\r\n&nbsp;","rendered":"<div><span style=\"float: right\"><a href=\"https:\/\/youtu.be\/n4U3wpbQEl0\" target=\"_blank\" rel=\"noopener\"><img decoding=\"async\" src=\"http:\/\/epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/2018\/11\/download.png\" alt=\"epgp books\" width=\"75px\" height=\"75px;\" \/><\/a><br \/>\n<\/span><\/div>\n<p><strong>Contents<\/strong><\/p>\n<ol>\n<li>Introduction<\/li>\n<li>Half Reactions<\/li>\n<li>Reduction Potential<\/li>\n<li>Standard Reduction Potential<\/li>\n<li>Interpretation and Significance<\/li>\n<li>Cell Reaction and Cell Potential<\/li>\n<li>Hydrogen Electrode and determination of Electrode Potential<\/li>\n<li>pE-Scale<\/li>\n<li>Significance of pE Values<\/li>\n<li>Measurement of pE-Values<\/li>\n<li>Solved Problem<\/li>\n<li>pE and pH Relationship<\/li>\n<li>Pourbaix diagram<\/li>\n<li>Interpretation and Significance<\/li>\n<li>Solved Problem<\/li>\n<li>The Limits of pE and pH in Natural Waters<\/li>\n<li>Redox Potentials in Natural Systems<\/li>\n<li>Redox Ladder<\/li>\n<li>Effect of redox on Metal Pollution<\/li>\n<li>Suggesting Reading<\/li>\n<\/ol>\n<p><strong>Introduction<\/strong><\/p>\n<p style=\"text-align: justify\">In aquatic environmental systems, including soils, sediments, aquifers, rivers, lakes, and water treatment systems, the most important and interesting chemical reactions occurring are the <strong>oxidation-reduction (redox)<\/strong> <strong>reactions<\/strong>. These reactions are central to major element cycling, to many sorption processes, to trace element mobility and toxicity, to most remediation schemes, and to life itself.<\/p>\n<p>&nbsp;<\/p>\n<p><em>Why study Redox Reactions?<\/em><\/p>\n<p>They fuel and constrain more or less all life processes.<\/p>\n<p>They are a major determinant of chemical species present in natural environments.<\/p>\n<p>&nbsp;<\/p>\n<p style=\"text-align: justify\"><strong>Redox reactions <\/strong>are core to many emerging domains of the aquatic sciences research, which includes all aspects of the aquatic sciences: involving the hydrosphere, aquatic (i.e., aqueous) aspects of environmental processes in the atmosphere, lithosphere, biosphere, etc. The <strong><em>Aquatic Redox Chemistry<\/em><\/strong> has multidisciplinary roots (straddling mineralogy to microbiology) and interdisciplinary applications (e.g., in removal of contaminants from sediment, soil or water).<\/p>\n<p style=\"text-align: justify\">To characterize the oxidation-reduction status of surface environments, the geochemists, soil scientists and limnologists have used redox potential (Ered) measurements. The redox potential of aquatic, marine and soil systems is a measure of electrochemical potential or electron availability within these systems. The redox potential (Ered) is determined from the concentration of oxidants and reductants in the environment. Oxygen, nitrate, nitrite, manganese, iron, sulphate, and CO2 are some of the prominent inorganic oxidants; while organic substrates and reduced inorganic compounds are the well-known reductants.<\/p>\n<p style=\"text-align: justify\">The redox-potential is the evaluation of the equilibrium potential, i.e. reduction\/oxidation potential, built at the interface between an electrode (a noble metal) and the solution consisting of electroactive redox species and is measured under standard state conditions (at 25 0C, 1 atmospheric pressure and one unit activity for all species) with respect to the standard hydrogen electrode. The term <strong>\u2018redox\u2019<\/strong> is the occurrence of both the chemical changes: oxidation and reduction, in a chemical reaction. The redox reactions i.e. oxidation-reduction reactions<\/p>\n<p style=\"text-align: justify\">entail the changes of oxidation states of reactants in a reaction and it is the sum up of two half reactions. The two processes: oxidation (loss of electrons) and reduction (gain of electrons) takes place together during the same reaction, i.e. oxidation\/reduction never takes place in isolation; hence, these reactions are called <strong>oxidation-reduction reactions <\/strong>or<strong> redox reactions. <\/strong>The potential of the overall reaction at the standard state<\/p>\n<p style=\"text-align: justify\">\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0+ E0red can be depicted as E0\u00a0 = E0 ox\u00a0 \u00a0 (where E0 ox \u00a0and E0red\u00a0 are the potentials of oxidation half-reaction and reduction half-reaction respectively)<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-515\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-6.png\" alt=\"\" width=\"347\" height=\"299\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-6.png 347w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-6-300x259.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-6-65x56.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-6-225x194.png 225w\" sizes=\"auto, (max-width: 347px) 100vw, 347px\" \/><\/p>\n<p style=\"text-align: justify\">In both these reactions, the hydrogen and carbon removes oxygen from copper(II) oxide and zinc oxide respectively, hence hydrogen and carbon are <strong>reducing agents<\/strong> or <strong>reductants<\/strong>. Similarly, those which are oxygen providers are called <strong>oxidizing agents<\/strong> or <strong>oxidants.<\/strong><\/p>\n<p>The modern electronic concept of <strong>oxidant<\/strong> and <strong>reductant<\/strong> is: one which accepts electrons is <strong>oxidant<\/strong> and one which donates electron is <strong>reductant.<\/strong><\/p>\n<p>For example:\u00a0 \u00a0 \u00a0 \u00a0Cl2\u00a0 + 2 I\u00a0 \u00a0&#8212;&#8212;&gt;\u00a0 \u00a02 Cl\u00a0\u00a0\u00a0 + I2<\/p>\n<p>Here, Cl2 is an oxidant and I\u00a0 is a reductant; as I\u00a0 is oxidized to I2 by Cl2 and Cl2 is reduced to Cl\u00a0 \u00a0by I ).<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-516\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-7.png\" alt=\"\" width=\"529\" height=\"263\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-7.png 529w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-7-300x149.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-7-65x32.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-7-225x112.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-7-350x174.png 350w\" sizes=\"auto, (max-width: 529px) 100vw, 529px\" \/><\/p>\n<p style=\"text-align: justify\">Thus, in a <strong>redox reaction<\/strong> which is brought about by loss and gain of electrons simultaneously, the oxidant is reduced and the reductant oxidized with an exchange of <em>n<\/em> electron (e ) which may be depicted as:<\/p>\n<p>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0Oxidant\u00a0 + <em>n<\/em> e\u00a0 &#8212;&#8212;-&gt;\u00a0 reductant<\/p>\n<p>Some examples of Reductant in wetland soil are:<\/p>\n<ol>\n<li>Organic matter &amp; other organic compounds;<\/li>\n<li>Reduced inorganic compounds, viz, Mn2+, S2 , CH4, H2, Fe2+, NH4 etc. Oxidants are inorganic compounds, viz, O2, NO3 , FeOOH, SO42 , HCO3 etc.<\/li>\n<\/ol>\n<p style=\"text-align: justify\">It may be noted that in the overall redox reaction no free electrons are generated. The movement of electrons is from reductant to oxidant, thereby an electrical potential is developed between the two which is measured in volts and denoted by E\u00b0. Since the redox potential depends on the members of the pair in a reaction, hence it\u2019s a relative rather than an absolute value. The standard redox potential values for elements, compounds and ions can be ascertained under standard conditions (unit molar concentration at 1 atm pressure and 25 0C), relative to a standard hydrogen electrode (SHE) potential (which is arbitrarily given a potential, E\u00b0 = zero volts). The greater the positive potential, the more anticipated it will be reduced.\u00a0The redox-potentials (also known as electrochemical version of Gibbs free energy G) are used to ascertain the direction and the free energy (the change in the system\u2019s free energy G) of redox-reaction at standard states as:\u00a0 G0 (eV) =\u00a0\u00a0\u00a0 nF\u00a0\u00a0 E\u00b0<\/p>\n<p style=\"text-align: justify\">where F is the Faraday constant number (96,485 C\/mol or 96,485 J\/mol\/V or \u2248100 kJ\/mol\/V) and n is the number of electrons involved in the redox-reaction). (The 0 symbol is for the substances involved in the reaction in their standard states).<\/p>\n<p style=\"text-align: justify\">For non-standard redox-reactions, the difference in redox-potential (precisely reduction potential E) is correlated to G as: \u0394G (eV) = -nF E<\/p>\n<p><strong>Half-Reactions<\/strong><\/p>\n<p style=\"text-align: justify\"><strong>A half reaction <\/strong>is either the reduction or the oxidation reaction component of a redox-reaction. The reactions occurring in an electrochemical cell is frequently described on the basis of the half-reaction concept. A redox reaction is expressed as the difference of two reduction <strong>half-reactions.\u00a0<\/strong><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-517\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-8.png\" alt=\"\" width=\"685\" height=\"467\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-8.png 685w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-8-300x205.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-8-65x44.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-8-225x153.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-8-350x239.png 350w\" sizes=\"auto, (max-width: 685px) 100vw, 685px\" \/><\/p>\n<p>&nbsp;<\/p>\n<p>Similarly, adding the simultaneously occurring two half reactions of metallic zinc atoms reaction with aqueous nickel ions give the net redox-reaction<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-518\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-9.png\" alt=\"\" width=\"283\" height=\"119\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-9.png 283w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-9-65x27.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-9-225x95.png 225w\" sizes=\"auto, (max-width: 283px) 100vw, 283px\" \/><\/p>\n<p>The half-reactions depict the exact oxidation state changes happening in two half-reactions.<\/p>\n<p><strong>Reduction Potential<\/strong><\/p>\n<p><strong>Definition<\/strong><\/p>\n<p style=\"text-align: justify\">By definition, redox-potential (reduction potential\/electrode potential) is the tendency of a substance to accept electrons. The positive (high) values of electrode potential means that the elements or ions would readily accept electrons; on the other hand, negative (low) values indicate their easy capability of electron donation.<\/p>\n<p>Few examples are cited below:<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-519\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-10.png\" alt=\"\" width=\"451\" height=\"129\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-10.png 451w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-10-300x86.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-10-65x19.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-10-225x64.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-10-350x100.png 350w\" sizes=\"auto, (max-width: 451px) 100vw, 451px\" \/><\/p>\n<p style=\"text-align: justify\">The <strong>standard reduction potential<\/strong> Eored is measured <em>relative<\/em> to: 2H+(aq) + 2e H2(g) (which has an assigned value Eored= 0.00 V and hence treated as reference)<\/p>\n<p style=\"text-align: justify\">Measurement of redox potential, E, allows quantitative appraisal of the force and tendency of the system. It can be measured by the difference between the potential of the hydrogen electrode (or more easily, the calomel electrode) and the potential of a platinum electrode immersed in the medium.<\/p>\n<p><strong>Interpretation and Significance<\/strong><\/p>\n<p style=\"text-align: justify\">Redox (electron-transfer) reactions provide the energetic basis for the life process, and through this, play a decisive role in the geochemical cycle of the elements. Redox reactions are very significant in water-saturated environments, such as sediments, soils, and sludges. Actually, all aquatic organisms obtain their energy for metabolic processes from oxidation-reduction reactions. Photosynthetic organisms catalytically reduce CO2 to reduced organic matter by locking light energy, while non-photosynthetic organisms catalytically decompose the organic products of photosynthesis through energy-yielding redox reactions. One of the major elements in the terrestrial and aquatic environments \u2013 nitrogen \u2013 circulates by many microbially catalyzed redox reactions. In truth, the only non-redox process in the entire nitrogen cycle is NH3 integration with and liberation from N-containing organic matter. The movements of many other elements also involve redox reactions, such as C, Fe, and S. The oxidizing power of anaerobic environments in the biosphere is mainly controlled by five molecules. In decreasing order of energy produced, they are nitrate (NO3\u2013), manganese dioxide (MnO2), ferric hydroxide (Fe(OH)3), sulfate (SO42\u2013) and, under extreme conditions, carbohydrate (CH2O) itself.<\/p>\n<p style=\"text-align: justify\">Like Gibb\u2019s free energy (G), the redox potentials (E) are not absolute. The redox potentials are measured with reference to the reduction of hydrogen ions to hydrogen gas at standard state conditions (SHE), i.e., 25 degrees Celsius (\u00b0C), 1 atmospheric pressure, and one unit activity for all species. The potential of this reaction, by convention, is taken as zero. Furthermore, as the redox potentials are comprised of two parts: the oxidation potential, and the reduction potential, the potential of the overall reaction of a cell at the standard state can be\u00a0<span style=\"text-align: initial;font-size: 1em\">expressed as:\u00a0 \u00a0E0<sub>cel<\/sub>l = E<sup>0<\/sup><sub>ox<\/sub> + E<sup>0<\/sup><\/span><\/p>\n<p style=\"text-align: justify\">A positive Eored indicate that a half-reaction will proceed in the direction indicated (reduction) when paired with the hydrogen half-reaction where as a negative Eored means that a half-reaction will move in the opposite direction indicated (oxidation).<\/p>\n<p style=\"text-align: justify\">The numerical values of E\u00b0ox and E\u00b0red of a substance in a half-reaction are the same with opposite in sign (until the conditions are changed). Thus, numerically, the potential for oxidation half-reaction is the negative of the potential of the reduction half-reaction, i.e. E\u00b0ox = E\u00b0red (with opposite sign). The voltage produces by an electrochemical cell is determined by summing up all the potentials in circuit, as:<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-520\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-11.png\" alt=\"\" width=\"201\" height=\"49\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-11.png 201w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-11-65x16.png 65w\" sizes=\"auto, (max-width: 201px) 100vw, 201px\" \/><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-521\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-12.png\" alt=\"\" width=\"471\" height=\"545\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-12.png 471w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-12-259x300.png 259w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-12-65x75.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-12-225x260.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-12-350x405.png 350w\" sizes=\"auto, (max-width: 471px) 100vw, 471px\" \/><\/p>\n<p style=\"text-align: justify\">The value of redox potential (E) (for non-standard states) under concentration conditions can be related to standard potential (E0) by the <strong>Nernst equation<\/strong>:<\/p>\n<p>E = E0 + RT\/nF * ln {(Ox)\/(Red)} = E0 RT\/nF * ln {(Red)\/(Ox)} = E0 RT\/nF * ln Q<\/p>\n<p>Or at 298 K, this is expressed as: E = E0 0.0592\/n * log {(Red)\/(Ox)}<\/p>\n<p style=\"text-align: justify\">where, E0 = standard electrode potential, R = ideal gas constant (8.314 J\/mol-K); T = absolute temperature (Kelvin); n = number of electrons involved in the reaction; F = the Faraday constant number and (Red)\/(Ox) is the concentration ration of reduced and oxidized forms of a given reaction pair, i.e. the reaction quotient.<\/p>\n<p style=\"text-align: justify\">The important factors upon which the redox potential of a substance depends are: nature of the substance, its affinity for electron, concentration of reductants and oxidants (referred as redox pair) and temperature.<\/p>\n<p>&nbsp;<\/p>\n<p><strong>Solved Problem <\/strong>(based on Nernst equation)<strong>:<\/strong><\/p>\n<p>For the half reaction 2H+ + 2e\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 = H2. What is E1\/2 at pH 5 and PH2 = 1 atm?<\/p>\n<p><strong>Solution: <\/strong>pH =\u00a0\u00a0\u00a0 log [H+] = 5, therefore [H+] = 10-5 M.<\/p>\n<p>In the above half-reaction, n = 2.<\/p>\n<p>Putting these values in the Nernst equation: E = E0 0.0592\/2 * log PH2\/(H+)2 E = E0 0.0592\/2 * log (105)2<\/p>\n<p>Since, for the given half-reaction, the E01\/2 = 0 V, hence, E = 0.000\u00a0 0.0592\/2 * (10)<\/p>\n<p>Therefore, E =\u00a0\u00a0 0.296 V.<\/p>\n<p style=\"text-align: justify\">Many electrode combinations are possible in electrochemical cells, and it is convenient to specify a standard potential, Eo, for each electrode by referencing it to the SHE (whose standard potential is defined as zero). There are many half-reactions whose electrode potential cannot be measured, because the electron transfer reaction at an electrode is too slow.<\/p>\n<p>These potentials can nevertheless be calculated from the free energy of appropriate redox reactions<\/p>\n<p>For example, the formation of NO from N2 and O2 is a redox reaction:<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-522\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-13.png\" alt=\"\" width=\"463\" height=\"97\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-13.png 463w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-13-300x63.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-13-65x14.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-13-225x47.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-13-350x73.png 350w\" sizes=\"auto, (max-width: 463px) 100vw, 463px\" \/><\/p>\n<p style=\"text-align: justify\">From the free energy of the overall reaction 173.4 kJ, we obtain a cell potential of -0.45 V (using equation <em>G <\/em>= \u2013<em>n<\/em>F E). Then knowing that the standard potential of the oxygen electrode is 1.24 V, we can readily evaluate the standard potential for half reaction as 1.69 V, (1.24 V \u2013[\u20100.45 V]), even though it is impossible to measure this potential directly because the electron transfer between the electrode and NO and N2 molecules is too slow to establish a reversible potential.<\/p>\n<p><strong>Significance of Redox Electrodes, Redox Potentials &amp; Redox Reactions in the determination of:<\/strong><\/p>\n<p>&nbsp;<\/p>\n<ul>\n<li>mobility and toxicity of chemical species in the environment (natural aquatic systems vary widely in redox conditions; therefore, fate may constantly change);<\/li>\n<li>equilibrium constant: single electrode potentials may be used to determine equilibrium constants of ionic reactions;<\/li>\n<li>solubility product of a sparingly soluble salt;<\/li>\n<li>pH, using hydrogen electrode<\/li>\n<\/ul>\n<p><strong>Cell Reaction and Cell Potential<\/strong><\/p>\n<p style=\"text-align: justify\">Let us see how the redox-reactions are a source of electric current in the electrochemical cells (a device for producing current from a chemical (redox) reaction).<\/p>\n<p style=\"text-align: justify\">For example, in the redox-reaction: Cu2+(aq) + Zn(s) &lt;&#8212;&#8211;&gt; Cu(s) + Zn2+(aq); the electrons released from a half-reaction, i.e. oxidation of Zn(s) are consumed by the other half-reaction, i.e. reduction of Cu2+(aq). Since both the reactions occur on the zinc electrode itself (dipped in CuSO4 solution), there is no net charge.<\/p>\n<p style=\"text-align: justify\">Now, if the two half-reactions occur in two separate compartments (one with Zn rod dipped in ZnSO4 solution and other with Cu rod dipped in CuSO4 solution) and both well connected by a wire, there will be a net flow of electrons from the reductant in one compartment to the oxidant in another through wire. However, the flow of current will be instant and later it will stop due to charge built up in the two compartments. The current flow can be restarted just by connecting the two compartments by a <strong>Salt bridge<\/strong> (a U-tube filled with an electrolyte such as NaCl, KCl, K2SO4 etc.) thus providing a passage to ions from one compartment to other without extensive mixing of the two solutions. This will complete the circuit and the electrons pass freely through the wire to maintain the net charge zero in the two compartments. This kind of circuitry cell is a simple <strong>Voltaic (Galvanic)<\/strong> <strong>cell <\/strong>where electrical current is generated by a spontaneous redox reaction.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-523\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-14.png\" alt=\"\" width=\"375\" height=\"329\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-14.png 375w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-14-300x263.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-14-65x57.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-14-225x197.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-14-350x307.png 350w\" sizes=\"auto, (max-width: 375px) 100vw, 375px\" \/><\/p>\n<p style=\"text-align: justify\">In an electrochemical cell, the flow of electrons from one electrode to the other is due to the half-reactions occurring in the anodic and cathodic compartments and the addition of these two half-reactions gives the net chemical change called as <strong>cell reaction<\/strong>. Thus, the E\u00b0 (electrode potential) for a given substance can be determines by constructing an electrochemical cell consisting of two half-cells. If the flow of electrons is from oxidant (hydrogen half-cell) to the other half-cell, the substance has a positive redox potential; whereas the E\u00b0 negative indicate the substance is reductant. Knowing the redox potentials values of two substances will help to predict whether a redox reaction between them is theoretically possible.<\/p>\n<p style=\"text-align: justify\">In electrochemical cells, or in redox reactions that happen in solution, the thermodynamic driving force can be measured as the <strong>cell potential<\/strong>. Chemical reactions are spontaneous in the direction of -\u0394G, which is also the direction in which the cell potential (defined as Eanode &#8211; Ecathode) is positive. A cell operating in the <strong>spontaneous<\/strong> direction (for example, a battery that is discharging) is called a <strong>galvanic cell<\/strong>. A cell that is being driven in the <strong>non-spontaneous<\/strong> direction is called an <strong>electrolytic cell<\/strong>.<\/p>\n<p><strong>Hydrogen Electrode and Determination of Electrode Potential<\/strong><\/p>\n<p>Hydrogen electrode is based on the redox half cell:<\/p>\n<p>2 H+ (aq) + 2e\u00a0 &lt;&#8212;-&gt; H2 (g)<\/p>\n<p style=\"text-align: justify\">The <strong>Standard hydrogen electrode (SHE)<\/strong> is a redox electrode which forms the basis of the thermodynamic scale of oxidation-reduction potentials. The absolute electrode potential of SHE is estimated to be 4.44 \u00b1 0.02 V at 25 \u00b0C, but for constructing a base for comparison with all other electrode reactions, hydrogen\u2019s standard electrode potential, E<sup>0<\/sup>, is declared to be zero at all temperature. The absolute electrode potential, according to IUPAC, is the electrode potential of a metal measured with respect to a universal reference system (without any additional metal-solution interface).<\/p>\n<p style=\"text-align: justify\">The standard electrode potential, E<sup>0<\/sup>, is measured under standard conditions: 25 <sup>0<\/sup>C, 1 M concentration for each ion participating in the reaction, a partial pressure of 1 atm for each part of the reaction, and metals in their pure state. The standard reduction potential is defined relative to a SHE reference electrode (arbitrary with a potential 0.00 V). Since, E<sup>0<\/sup> (SHE) = 0, E<sup>0<\/sup> for other half reaction can be &gt;0 [oxidizes H2 (g) or &lt;0 [is oxidized by H2 (g)].<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-525\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-16.png\" alt=\"\" width=\"225\" height=\"243\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-16.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-16-65x70.png 65w\" sizes=\"auto, (max-width: 225px) 100vw, 225px\" \/><\/p>\n<p>The conventions for E\u00ba:<\/p>\n<ul>\n<li>E\u00ba values (units of volts) are compared on the basis of half reactions, which by convention are written as reductions;<\/li>\n<li>all substances are assumed to be at unit activity;<\/li>\n<li>all E\u00ba values are determined relative to the reduction potential of the standard hydrogen electrode (SHE).<\/li>\n<\/ul>\n<ol>\n<li>If the E\u00ba for a given half-reaction is &gt;0, that couple has the potential (under standard conditions) to oxidize the SHE;<\/li>\n<li>A negative E\u00ba indicates a couple that can reduce the SHE (at standard conditions).<\/li>\n<\/ol>\n<p><strong>\u00a0<img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-526\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-17.png\" alt=\"\" width=\"309\" height=\"257\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-17.png 309w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-17-300x250.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-17-65x54.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-17-225x187.png 225w\" sizes=\"auto, (max-width: 309px) 100vw, 309px\" \/><\/strong><\/p>\n<p><strong>pE-Scale<\/strong><\/p>\n<p style=\"text-align: justify\">The most important factor affecting redox reactions of some species is pH, and the effects are very well illustrated by Eh-pH (or p<em>e<\/em>-pH, or pE-pH, or Pourbaix) diagrams. Since it is frequently difficult to determine which half-reactions are actually coupled in nature, the concept of pE is preferred.<\/p>\n<p style=\"text-align: justify\">pE may be defined as the <em>activity<\/em> of the free electron in water, thus only half reactions can be focused upon. Forever, the reactions are expressed as the reduction half reaction. From the equation: G<sup>0<\/sup> = \u2013<em>n<\/em>F E, a negative G<sup>0<\/sup> corresponds to a positive E<sup>0<\/sup>, and thus to a potentially spontaneous reduction half-reaction (at standard conditions) versus the SHE.<\/p>\n<p>For graphical expressions, <strong>pE<\/strong> is negative log of electron activity, i.e., pE = -log(e ) = F E<sup>0<\/sup> \/ 2.3 RT = 1\/n log K = -1\/n G<sup>0<\/sup> \/ 2.3 RT.<\/p>\n<p style=\"text-align: justify\">Or, the pE equation can be expressed as: pE = pE<sup>0<\/sup> &#8211; log (Red) \/ (Ox); where pE<sup>0<\/sup> can be calculated from log K. If the equilibrium distribution of (Red)\/(Ox) is known, this equation can be used to solve for the pE of the environment.<\/p>\n<p>For example, for the half-reaction Cu<sup>2+<\/sup> + 2e &#8212;&#8211;&gt; Cu (s);<\/p>\n<p>Since n = two electrons involved and K= 1\/({Cu2+} {e }2), therefore, pE will be expressed as:<\/p>\n<p>pE = 1\/2 log K + 1\/2 Log {Cu<sup>2+<\/sup>}<\/p>\n<p>[as\u00a0 pE<sup>0<\/sup> = 1\/n log K and pE = pE<sup>0<\/sup> + (1\/n) log {ox}\/{red}]<\/p>\n<p>pE<sup>0<\/sup> is readily obtainable from thermodynamic data, now multiplying both the sides of above equation by 2.303<\/p>\n<p>RT\/F, equation becomes:<\/p>\n<p>pE = F\/(2.303RT) EH<\/p>\n<p>pE<sup>0<\/sup> = 16.90 E0H<\/p>\n<p>pE<sup>0<\/sup> = -1\/n (1.753&#215;10-4) ( G0)<\/p>\n<p>G<sup>0<\/sup> =\u00a0\u00a0\u00a0\u00a0 G0f (products) &#8211;\u00a0 G0f (reactants)<\/p>\n<p><strong>Significance of pE Values<\/strong><\/p>\n<p style=\"text-align: justify\">At equilibrium, solution has one pE value; if this is assumed, the ratio of oxidized to reduced species activities can be calculates; moreover, determination of prominent species is possible. Usually, electrons move from high to low activity (Ae); small pE corresponds to reducing environments, reduced species predominates; and large pE correspond to oxidizing environments, oxidized species predominates. The pE diagrams can be an asset to know how species predominate as a function of pE.<\/p>\n<p><strong>Measurement of pE Values<\/strong><\/p>\n<p style=\"text-align: justify\">The pE0 of a half reaction expresses the electron activity required to maintain reactants and products at unit activities. There are two main types of redox calculations. The first is the calculation of what controls the pE of the environment. This is analogous to calculating the pH of the environment.<\/p>\n<p style=\"text-align: justify\">The second type of calculation is to determine how trace species respond or distribute themselves with respect to that pE. Again by analogy, when we know the pH, we can calculate the pH dependent speciation of trace species.<\/p>\n<p><strong>Solved Problem:<\/strong><\/p>\n<p>For the reduction:\u00a0 Fe3+ + 2e &#8212;&#8211;&gt; Fe2+\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 K = 10<sup>13<\/sup><\/p>\n<p style=\"text-align: justify\">The electron activity of the solution must be held to the very low value of 10<sup><em>&#8211;<\/em>13<\/sup> (pE = 13) to maintain equal activities of the two ions; this corresponds to usually referred as an oxidizing environment.<\/p>\n<p>The value of K = 1013 actually refers, of course, to the reaction; Fe<sup>3<\/sup><span style=\"text-align: initial;font-size: 1em\"><sup>+<\/sup> + H<\/span><sup style=\"text-align: initial\">2<\/sup><span style=\"text-align: initial;font-size: 1em\"> &#8212;&#8211;&gt;\u00a0Fe<\/span><sup style=\"text-align: initial\">2+<\/sup><span style=\"text-align: initial;font-size: 1em\">\u00a0 + 2H<\/span><sup style=\"text-align: initial\">+<\/sup><\/p>\n<p>K = {Fe2+} {H+} \/{Fe3+} {<em>P<\/em>H52}<\/p>\n<p style=\"text-align: justify\">So that the equilibrium condition {Fe3+} = {Fe2+} would require a pH of 13 at this unit pressure of H2 or a hydrogen partial pressure of 1026 atm at zero pH.<\/p>\n<p><strong>pE and pH Relationship:<\/strong><\/p>\n<p><strong><em>Pourbaix Diagram<\/em><\/strong><\/p>\n<p style=\"text-align: justify\">A <strong>Pourbaix diagram<\/strong> (also known as <strong>Potential\/pH diagram, E<\/strong><strong>H<\/strong><strong>-pH diagram<\/strong> or a <strong>pE\/pH diagram<\/strong>) is essentially an <strong>electrochemical phase diagram,<\/strong> the best representation of the possible thermodynamically stable phases of an aqueous electrochemical system (i.e. redox-active substances). The diagrams are invented by the Russian born, Belgium Chemist <strong>Marcel Pourbaix<\/strong> (1904-1998) and are named after him.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-527\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-18.png\" alt=\"\" width=\"467\" height=\"399\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-18.png 467w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-18-300x256.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-18-65x56.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-18-225x192.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-18-350x299.png 350w\" sizes=\"auto, (max-width: 467px) 100vw, 467px\" \/><\/p>\n<p style=\"text-align: justify\">The diagrams have two axes, the vertical axis labeled as pE or EH represent the voltage potential with respect to SHE (as EH (SHE)\/V; where H stands for hydrogen); and the horizontal axis measures pH. The lines depict the conditions under which two phases coexist in equilibrium and also the redox and acid-base reactions. The<\/p>\n<p style=\"text-align: justify\">shaded area represents the conditions of potential and pH for the stable phase of the substance, whereas outside the shaded region represents the thermodynamically unstable phase which either gets reduced or oxidized.<\/p>\n<p style=\"text-align: justify\">Eh-pH diagram showing the predominance fields for oxidized (upper right) and reduced (lower left) forms of selected redox-active species. Dashed diagonal lines are for the H2\/H2O (lower) and H2O\/O2 (upper) couples and together they enclose the conditions over which water is stable.<\/p>\n<p><strong>Interpretation and Significance<\/strong><\/p>\n<p style=\"text-align: justify\">A Pourbaix diagram designates mainly three regions: \u2018immunity\u2019, \u2018corrosion\u2019 and \u2018passivity\u2019 instead of stable species. These regions describe the stability of a particular substance in a specific environment. \u2018Immunity\u201d indicate the safe and non-attacked region which is opposite to the \u2018corrosion\u2019 region; \u2018passivity\u2019 other hand depict the relative stability (i.e. when a metal forms a stable oxide or other salt coating on its surface).<\/p>\n<p>For example, in the Pourbaix diagram for Fe (above):<\/p>\n<p><strong>Areas <\/strong>in the Pourbaix diagram mark regions where a single species (Fe2+(aq), Fe3O4(s), etc.) is stable. More stable species tend to occupy larger areas.<\/p>\n<p><strong>Lines <\/strong>mark places where two species exist in equilibrium.<\/p>\n<p style=\"text-align: justify\"><strong>Pure redox <\/strong>reactions are<strong> horizontal <\/strong>lines &#8211; these reactions are not pH-dependent<strong> Pure acid-base <\/strong>reactions are<strong> vertical <\/strong>lines &#8211; these do not depend on potential Reactions that are <strong>both<\/strong> acid-base and redox have a slope of -0.0592 V\/pH x4H+\u20444e-)<\/p>\n<p>Illustration of equilibria in the iron Pourbaix diagram (numbered on the plot):<\/p>\n<ol>\n<li>Fe2+ + 2e- \u2192 Fe (s) (pure redox reaction &#8211; no pH dependence)<\/li>\n<li>Fe3+ + e- \u2192 Fe2+ (pure redox reaction &#8211; no pH dependence)<\/li>\n<li>2 Fe3+ + 3 H2O \u2192 Fe2O3(s)+ 6H+ (pure acid-base, no redox)<\/li>\n<li>2 Fe2+ + 3 H2O \u2192 Fe2O3(s)+ 6H+ + 2e- (slope = -59.2 x 6\/2 = -178 mV\/pH)<\/li>\n<li>2 Fe3O4(s) + H2O \u2192 3 Fe2O3(s) + 2H+ + 2e- (slope = -59.2 x 2\/2 = -59.2 mV\/pH)<\/li>\n<\/ol>\n<p style=\"text-align: justify\">For an element, such as iron, the water redox lines have special significance on a Pourbaix diagram. In other case, such as liquid water, it is stable <em>only<\/em> in the region between the dotted lines. Below the H2 line, water is unstable relative to hydrogen gas, and above the O2 line, water is unstable with respect to oxygen; while, for active metals such as Fe, the region where the pure element is stable is typically below the H2 line. This means that iron metal is unstable in contact with water, undergoing reactions:<\/p>\n<p>Fe(s) + 2H+ \u2192 Fe2+(aq) + H2 (in acid)<\/p>\n<p>Fe(s) + 2 H2O \u2192 Fe(OH)2(s) + H2 (in base)<\/p>\n<p style=\"text-align: justify\">Iron (and most other metals) are also thermodynamically unstable in air-saturated water, where the potential of the solution is close to the O2 line in the Pourbaix diagram. Here the spontaneous reactions are:<\/p>\n<p>4 Fe(s) + 3 O2 + 12H+ \u2192 4 Fe3+ + 6 H2O (in acid)<\/p>\n<p>4 Fe(s) + 3 O2 \u2192 2 Fe2O3(s) (in base)<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-528\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-19.png\" alt=\"\" width=\"579\" height=\"511\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-19.png 579w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-19-300x265.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-19-65x57.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-19-225x199.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-19-350x309.png 350w\" sizes=\"auto, (max-width: 579px) 100vw, 579px\" \/><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-529\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-20.png\" alt=\"\" width=\"545\" height=\"543\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-20.png 545w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-20-150x150.png 150w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-20-300x300.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-20-65x65.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-20-225x224.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-20-350x349.png 350w\" sizes=\"auto, (max-width: 545px) 100vw, 545px\" \/><\/p>\n<p style=\"text-align: justify\">Line-a \u2013 depicting Reducing limit and Line-b \u2013 depicting Oxidizing limit. Below line-a (zone-I) is too reducing for water; whereas above line-b (zone-III) is too oxidizing for water. Zone falling in between Reducing &amp; Oxidizing limits, i.e. between the two parallel lines a &amp; b (zone-II) is just right for water.<\/p>\n<p>Similarly, Pourbaix diagram for other ions in the water stability field can be drawn.<\/p>\n<p style=\"text-align: justify\">The creation of phase diagram for any solute ion, or combination of solute ions will illustrate the <em>speciation<\/em> (form) of that\/those ion(s) in EH vs pH or pE vs pH space for a given solute concentration in solution. Though creating phase diagram for mixed ions are quite complex in comparison to single ion diagrams.<\/p>\n<p><strong>Applications:<\/strong><\/p>\n<p>Monitoring of industrial waste water<\/p>\n<p>Swimming pool water monitoring<\/p>\n<p>Soil investigation<\/p>\n<p>Freshwater habitat quality<\/p>\n<p><strong>Redox potentials in natural systems:<\/strong><\/p>\n<p style=\"text-align: justify\">At almost neutral pH (7-8), the redox potentials in natural waters range from about \u2013400 mV to +800 mV. They are bounded in the negative range by the reduction of H2O to hydrogen gas (H2(g)) and in the positive range by the oxidation of H2O to O2(g).<\/p>\n<p>In water and sediment, four representative ranges of redox potentials exist:<\/p>\n<ol>\n<li style=\"text-align: justify\">Range I: <em>For oxygen-bearing waters<\/em>: water saturated with oxygen may have a redox potential within the first range (710 to 800 mV at pH 7 to 8).<\/li>\n<li style=\"text-align: justify\">Range II: in systems where some oxygen has been consumed, the redox potentials may range between \u2013 100 to 710 mV (at pH 7 to 8). It is representative of many ground and soil waters where O2 has been 2consumed (by degradation of organic matter), but SO4 is not yet reduced. In this range soluble Fe (II) and Mn (II) are present; their concentration is redox-buffered because of the presence of solid Fe (III) and Mn (III, IV) oxides.<\/li>\n<li style=\"text-align: justify\">Range III: though the potential is not sensitive to oxygen concentrations and has been observed to remain nearly constant down to values of 0.1% O2 saturation. It is characterized by SO4 \/ HS or SO4 \/ FeS2 redox equilibria.<\/li>\n<li style=\"text-align: justify\">Range IV: <em style=\"text-align: initial;font-size: 1em\">for anaerobic sediments and sludges<\/em><span style=\"text-align: initial;font-size: 1em\"><span style=\"text-align: initial;font-size: 1em\">: Within the second range, solid Fe (III), and Mn (III, IV) are reduced to soluble Fe (II) and Mn (II) when organic matter is mineralized. Phosphorus, which is\u00a0<\/span><\/span>Many researchers have studied the relationships between oxidation-reduction potential and the physical, chemical, and biological processes in soil-water systems. One of the pioneers in this field was Mortimer (1941, 1942). Mortimer studied the factors which control the rate of nutrient supply to phytoplankton in systems of lake water and sediment deposits.<\/li>\n<\/ol>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-530\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-21.png\" alt=\"\" width=\"351\" height=\"291\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-21.png 351w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-21-300x249.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-21-65x54.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-21-225x187.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-21-350x290.png 350w\" sizes=\"auto, (max-width: 351px) 100vw, 351px\" \/><\/p>\n<p>&nbsp;<\/p>\n<p><strong>Figure 3: <\/strong>Redox intensity representative ranges in soil and water. (pE = 16.9 E ).<\/p>\n<p><strong>Redox Ladder:<\/strong><\/p>\n<p style=\"text-align: justify\">The change in the pE of a fresh natural water in contact with sediment as a function of amount of organic matter decomposed or in other words, the <strong>Redox Ladder<\/strong> may be defined as: the step by step sequencing of common redox. The redox reactions occurring in an aquatic environment, a step wise pE sketch is formed in which at a particular place or time, pE is fixed until a particular oxidant is consumed.<\/p>\n<p style=\"text-align: justify\">As illustrated in fig., at almost 7 pH, the change in the pE of fresh natural water in contact with sediment as a function of amount of organic matter decomposed. The amount of the organic matter reacted is depicted horizontally (thus its length depends on the availability of specific solid phases for reaction).<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-533\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-22.png\" alt=\"\" width=\"231\" height=\"195\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-22.png 231w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-22-65x55.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-22-225x190.png 225w\" sizes=\"auto, (max-width: 231px) 100vw, 231px\" \/><\/p>\n<p><strong>Effect of redox on metal pollution:<\/strong><\/p>\n<p style=\"text-align: justify\">Changes in the redox potential can have important consequences for environmental pollution, especially with respect to metal ions such as cadmium, lead, and nickel. In general, the solubility of heavy metals is highest in oxidizing and acidic environments (Figure: Eh\/pH as a function of different aquatic environments). At neutral to alkaline pHs in oxidizing environments, these metals often adsorb onto the surface of insoluble Fe(OH)3 and MnO2 particles, especially when phosphate is present to act as a bridging ion. When the redox potential shifts to only slightly oxidizing or slightly reducing conditions as a result of microbial action, and the pH shifts toward the acidic range, Fe(OH)3 and MnO2 in soils and sediments are reduced and solubilized. The adsorbed metal ions likewise become solubilized and move into groundwater (or into the water column of lakes when there is Fe(OH)3 or MnO2 in the sediment). Conversely, if sulfate is reduced microbially to HS\u2013 metal ions are immobilized as insoluble sulfides. But if sulfide rich sediments are exposed to air through drainage or dredging operations, then HS\u2013 is oxidized back to sulfate, and the heavy metal ions are released.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-534\" src=\"http:\/\/esp16.epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-23.png\" alt=\"\" width=\"419\" height=\"353\" srcset=\"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-23.png 419w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-23-300x253.png 300w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-23-65x55.png 65w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-23-225x190.png 225w, https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-content\/uploads\/sites\/161\/2019\/03\/Untitled-23-350x295.png 350w\" sizes=\"auto, (max-width: 419px) 100vw, 419px\" \/><\/p>\n<p style=\"text-align: justify\"><strong>Figure 4: <\/strong>EH\/pH as a function of different aquatic environments. Oval enclosed by dashed line indicates region of highest solubility of heavy metals. [<em>Source:<\/em> Adapted from W. Salomons (1995). Long\u2010term strategies for handling contaminated sites and large\u2010scale areas. In <em>Biogeodynamics of Pollutants in Soils and Sediments<\/em>, W Salomons and W.M. Stigliani, eds. (Berlin: Springer\u2010Verlag)].<\/p>\n<p style=\"text-align: justify\">A particularly important instance of biological redox mediation of heavy-metal pollution occurs in the case of mercury. Inorganic mercury, in any of its common valence states, Hg0, Hg22+, and Hg2+, is not toxic when ingested; it tends to pass through the digestive system, although Hg0 is highly toxic when inhaled. But the methylmercury ion (CH3)Hg+ is very toxic, regardless of the route of exposure. The environmental route to toxicity involves sulfate reducing bacteria that live in anaerobic sediments. As part of their metabolism these bacteria use methyl groups to produce acetate. When exposed to Hg2+ the bacteria transfer the methyl groups to the mercury, producing (CH3)Hg+; because methylmercury is soluble, it enters the aquatic food chain, where it is bioaccumulated in the protein-laden tissue of fish.<\/p>\n<table>\n<tbody>\n<tr>\n<td><strong>you can view video on Aquatic Redox Chemistry<\/strong><\/td>\n<td><a href=\"https:\/\/youtu.be\/n4U3wpbQEl0\" target=\"_blank\" rel=\"noopener\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-120\" src=\"http:\/\/epgpbooks.inflibnet.ac.in\/wp-content\/uploads\/2018\/11\/download.png\" alt=\"\" width=\"36\" height=\"36\" \/><\/a><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p><strong>Suggested Reading<\/strong><\/p>\n<ol>\n<li>Stanley E. Manahan, Environmental Chemistry, 9th Edition, CRC Press, New York, 2009.<\/li>\n<li style=\"text-align: justify\">Colin Baird and Michael Cann, Environmental Chemistry, 4th Edition, WH Freeman, New York, 2008.<\/li>\n<li style=\"text-align: justify\">Peter Atkins and Julio de Paula, Elements of Physical Chemistry, 5th Edition, Oxford University Press Inc., New York, 2009.<\/li>\n<li>Richard Harwood, Chemistry: New Edition, Cambridge University Press, UK, 2002.<\/li>\n<li>Brian J Knapp, Oxidation and Reduction, CT Danbury, Grolier Educational, 1998.<\/li>\n<li style=\"text-align: justify\">J C Morris; W Stumm, Redox equilibria and measurements of potentials in the aquatic environment. In Equilibrium Concepts in Natural Water Systems; ACS Symposium Series No. 67; American Chemical Society: Washington, DC, 1967; pp 270\u2212285.<\/li>\n<li style=\"text-align: justify\">M. Taillefert, T. F. Rozan, Eds.; Environmental Electrochemistry: Analyses of Trace Element Bigeochemistry<span style=\"text-align: initial;font-size: 1em\">; ACS Symposium Series No. 811; American Chemical Society: Washington, DC, 2002.<\/span><\/li>\n<li style=\"text-align: justify\">K R Reddy and R Delaune, Biogeochemistry of wetlands, 2004, CRC.<\/li>\n<li style=\"text-align: justify\">T. Borch, R. Kretzschmar, A. Kappler, P. V. Cappellen, M. Ginder-Vogel, A. Voegelin, K. Campbell, Biogeochemical redox processes and their impact on contaminant dynamics. Environ. Sci. Technol. 44, 2010, 15\u201323.<\/li>\n<li style=\"text-align: justify\">Werner Stumm,\u00a0 James\u00a0 J.\u00a0 Morgan,\u00a0 Aquatic\u00a0 Chemistry:\u00a0 Chemical\u00a0 Equilibria and\u00a0 Rates\u00a0 in\u00a0 Natural Waters, 3rd Edition, John Wiley &amp; Sons, Inc., <span style=\"text-align: initial;font-size: 1em\">(1995) Pp. 1040. ISBN: 978-0-471-51185-4.<\/span><\/li>\n<li style=\"text-align: justify\">Aquatic Redox Chemistry, Editor(s): Paul G. Tratnyek, Timothy J. Grundl, Stefan B. Haderlein, Vol 1071, American Chemical Society, 2011. ISBN13: 9780841226524.<\/li>\n<li style=\"text-align: justify\">Andri Stef\u00e1nsson, Stef\u00e1n Arn\u00f3rsson, \u00c1rn\u00fd E. Sveinbj\u00f6rnsd\u00f3ttir, Redox reactions and potentials in natural waters at disequilibrium, Chemical Goelogy, 221, (3\u20134) 2005, Pp. 289\u2013311.<\/li>\n<\/ol>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n","protected":false},"author":3,"menu_order":23,"template":"","meta":{"_acf_changed":false,"pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":["dr-alka-sharma"],"pb_section_license":""},"chapter-type":[],"contributor":[63],"license":[],"class_list":["post-514","chapter","type-chapter","status-publish","hentry","contributor-dr-alka-sharma"],"part":3,"_links":{"self":[{"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/pressbooks\/v2\/chapters\/514","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/wp\/v2\/users\/3"}],"version-history":[{"count":5,"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/pressbooks\/v2\/chapters\/514\/revisions"}],"predecessor-version":[{"id":933,"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/pressbooks\/v2\/chapters\/514\/revisions\/933"}],"part":[{"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/pressbooks\/v2\/parts\/3"}],"metadata":[{"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/pressbooks\/v2\/chapters\/514\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/wp\/v2\/media?parent=514"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/pressbooks\/v2\/chapter-type?post=514"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/wp\/v2\/contributor?post=514"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/ebooks.inflibnet.ac.in\/esp16\/wp-json\/wp\/v2\/license?post=514"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}