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Balancing Redox Equations02:58

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Electrochemistry is the science involved in the interconversion of electrical and chemical reactions. Such reactions are called reduction-oxidation, or redox reactions. These important reactions are defined by changes in oxidation states for one or more reactant elements and include a subset of reactions involving the transfer of electrons between reactant species. Electrochemistry as a field has evolved to yield sufficient insights on the fundamental principles of redox chemistry and multiple...
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Oxidation-reduction or redox reactions involve the transfer of electrons from one molecule or atom to another. When an atom gains an electron, another atom must lose an electron, meaning oxidation and reduction must occur together. Since the redox occurs in pairs, the atom that gets oxidized is also called the reducing agent or reductant, and the atom that is reduced is also called the oxidizing agent or oxidant. A straightforward way to remember the definitions of oxidation and reduction is...
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Redox reactions are vital biochemical processes that underpin energy metabolism in cells. These reactions involve the transfer of electrons between molecules, occurring in tandem as oxidation and reduction. Oxidation refers to the loss of electrons, while reduction denotes their gain. This coupling ensures the seamless flow of electrons through metabolic pathways. For example, in bacterial metabolism, glucose undergoes oxidation to carbon dioxide, while oxygen is simultaneously reduced to...
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On comparing the reactivity of silver and lead, it is observed that the two ionic species, Ag+ (aq) and Pb2+ (aq), show a difference in their redox reactivity towards copper: the silver ion undergoes spontaneous reduction, while the lead ion does not. This relative redox activity can be easily quantified in electrochemical cells by a property called cell potential. This property is commonly known as cell voltage in electrochemistry, and it is a measure of the energy which accompanies the charge...
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Stream Function01:20

Stream Function

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In two-dimensional incompressible fluid flow, the continuity equation is essential for ensuring mass conservation, meaning that any change in fluid entering or exiting a region is balanced by a corresponding change elsewhere. For incompressible flow, where density remains constant, this requirement simplifies to the condition that the divergence of the velocity field must be zero. Mathematically, this is expressed as,
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Cell Potential and Free Energy

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Thermodynamics of a Redox Reaction
Thermodynamics is the branch of physics dealing with the relationship between heat and other forms of energy. In an electrochemical cell, chemical energy is converted into electrical energy.
Thus, a link can be predicted between cell potential, free energy change, and the equilibrium constant for the reaction. Cell potential can also be measured as the oxidant or the reducing strength, and similar acid-base strength measures are reflected in equilibrium...
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Related Experiment Video

Updated: Feb 1, 2026

Modifying the Bank Erosion Hazard Index BEHI Protocol for Rapid Assessment of Streambank Erosion in Northeastern Ohio
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Varying redox potential affects P release from stream bank sediments.

Suroso Rahutomo1, John L Kovar2, Michael L Thompson3

  • 1Indonesian Oil Palm Research Institute, Medan, North Sumatra, Indonesia.

Plos One
|December 15, 2018
PubMed
Summary

Agricultural stream sediments can either adsorb or release phosphorus (P). Redox potential significantly influences this, with younger sediments acting as P sources in low-oxygen conditions, while older till acts as a P sink.

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Area of Science:

  • Environmental Science
  • Geochemistry
  • Hydrology

Background:

  • Stream sediments in agricultural watersheds can act as phosphorus (P) sinks or sources.
  • Sediment characteristics and redox potential dictate P adsorption or release.
  • Walnut Creek in Iowa represents small streams in the glaciated upper Midwest.

Purpose of the Study:

  • Investigate P adsorption and release by four distinct sediments.
  • Evaluate the effects of redox potential on phosphorus buffering capacity (PBC) and equilibrium phosphorus concentration (EPC).

Main Methods:

  • Batch adsorption experiments to determine PBC and EPC.
  • Simulated aerobic and anaerobic conditions over 24 days.
  • Measured solution-phase P concentrations using dialysis tubing in stirred systems.

Main Results:

  • Holocene-age sediments had similar EPCs that increased with decreasing redox potential.
  • Camp Creek and Roberts Creek sediments released more dissolved P under anaerobic conditions.
  • Pre-Illinoian-age Till exhibited the greatest P buffering capacity.

Conclusions:

  • Younger, Holocene-age sediments (Camp Creek, Roberts Creek) are likely P sources in suboxic stream conditions.
  • Older Pre-Illinoian-age Till likely acts as a P adsorbing sink in contact with stream water.