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Related Concept Videos

Microbes and Other Elemental Cycles01:24

Microbes and Other Elemental Cycles

Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
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Mining activities that disturb sulfide-rich rocks, particularly those containing pyrite (FeS₂), initiate a cascade of geochemical and microbiological processes with serious environmental implications. When exposed to air and water, pyrite undergoes oxidation, releasing sulfate, ultimately forming sulfuric acid and mobilizing heavy metals into surrounding water systems. This phenomenon, known as acid mine drainage (AMD), results in low pH waters laden with toxic elements that threaten aquatic...
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Factors Affecting Solubility

Compared with pure water, the solubility of an ionic compound is less in aqueous solutions containing a common ion (one also produced by dissolution of the ionic compound). This is an example of a phenomenon known as the common ion effect, which is a consequence of the law of mass action that may be explained using Le Chȃtelier’s principle. Consider the dissolution of silver iodide:
Microbial Leaching01:27

Microbial Leaching

Microbial leaching, also known as bioleaching, is an environmentally favorable method for extracting metals from low-grade ores using specific microorganisms. This biotechnological approach is particularly valuable for mining operations targeting copper, gold, and uranium, where traditional extraction methods may be economically or environmentally impractical.Copper Leaching and Microbial CatalysisIn copper bioleaching, crushed ore is arranged into heaps and irrigated with a dilute sulfuric...
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Coagulation01:06

Coagulation

Colloidal solids are solid particles suspended in solution. They are usually negatively charged, attracting a compact primary layer of positively charged ions, which attract more counterions to form an electrical double layer. Electrostatic repulsion between the charged double layers prevents the particles from colliding, stabilizing the colloids. These solids are often undesirable because they can contain toxins that are difficult to remove. Coagulation is a technique that helps aggregate and...

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Related Experiment Video

Updated: Jul 7, 2026

Preparation of Free-Surface Hyperbolic Water Vortices
04:35

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Published on: July 28, 2023

[Effect on iron release in drinking water distribution systems].

Zhang-bin Niu1, Yang Wang, Xiao-jian Zhang

  • 1Department of Environment Science and Technology, Tsinghua University, Beijing 100084, China. nzb03@mails.tsinghua.edu.cn

Huan Jing Ke Xue= Huanjing Kexue
|February 14, 2008
PubMed
Summary

Controlling iron release in drinking water requires specific inorganic chemical conditions. Maintaining a pH above 7.6 and sufficient alkalinity, dissolved oxygen, and low chloride levels minimizes iron release.

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Area of Science:

  • Environmental Chemistry
  • Water Quality Science
  • Corrosion Science

Context:

  • Drinking water distribution systems are susceptible to iron release from infrastructure.
  • Inorganic chemical parameters significantly influence water quality and system integrity.
  • Understanding these factors is crucial for maintaining safe and reliable water supply.

Purpose:

  • To quantitatively investigate the impact of key inorganic chemical parameters on iron release.
  • To elucidate a theoretical critical formula governing iron release rates.
  • To establish optimal conditions for controlling iron release in water distribution systems.

Summary:

  • Batch-scale experiments revealed that increasing pH, alkalinity, and dissolved oxygen concentration decreases iron release rates.
  • Conversely, elevated chloride concentrations were found to increase iron release.
  • A critical formula was developed, identifying necessary conditions: pH > 7.6, alkalinity > 150 mg/L, dissolved oxygen > 2 mg/L, and chloride < 150 mg/L.

Impact:

  • Provides a scientific basis for water utilities to manage water chemistry and mitigate iron release.
  • Contributes to improved drinking water quality and reduced operational issues related to iron.
  • Offers a predictive tool for assessing and controlling iron release based on water chemistry parameters.