Cited by 142Soil Carbon and Nitrogen DynamicsMicrobial bioremediation and biosurfactantsMicrobial Community Ecology and Physiology

Interactions Between Soil Particles and Microorganisms: Impact on the Terrestrial Ecosystem

Huang, P. M., Bollag, J. M., Senesi, N.·2002·Chemistry International -- Newsmagazine for IUPAC

Abstract

List of Contributors. Series Preface. Preface. PART I: FUNDAMENTALS OF SOIL PARTICLE-MICROORGANISM INTERACTIONS. Interactions between Microorganisms and Soil Particles: An Overview (C. Chenu and G. Stotzky). A Fractal Approach for Interactions between Soil Particles and Microorganisms (N. Senesi and L. Boddy). Interactions of Organic Materials and Microorganisms with Minerals in the Stabilization of Structure (J. A. Baldock). Impact of Organic Substances on the Formation and Transformation of the Metal Oxides in Soil Environments (A. Violante, G. S. R. Krishnamurti and P. M. Huang). Microbial Mobilization of Metals from Soil Minerals under Aerobic Conditions (E. Kurek). Interactions of Bacteria and Environmental Metals, Fine-grained Mineral Development and Bioremediation Strategies (J. S. McLean, J.-U. Lee and T. J. Beveridge). PART II: IMPACT OF SOIL PARTICLE-MICROORGANISM INTERACTIONS ON THE TERRESTRIAL ENVIRONMENT. (A) ION CYCLING AND ORGANIC POLLUTANT TRANSFORMATION. Effect of Mineral Colloids on Biogeochemical Cycling of C, N, P and S in Soil (G. Guggenberger and K. M. Haider). Impact of Interactions between Microorganisms and Soil Colloids on the Transformation of Organic Pollutants (J. Dec, J.-M. Bollag, P. M. Huang, and N. Senesi). (B) RHIZOSPHERE CHEMISTRY AND BIOLOGY. Chemical and Biological Processes in the Rhizosphere: Metal Pollutants (P. M. Huang and J. J. Germida). Biotic and Abiotic Interactions in the Rhizosphere: Organic Pollutants (T. A. Anderson, D. P. Shupack and H. Awata). (C) ANAEROBIC AND TRANSPORT PROCESSES, AND THE SUBSURFACE TERRESTRIAL ENVIRONMENT. Interactions between Microorganisms and Minerals under Anaerobic Conditions (H. L. Ehrlich). The Role of Mineral Colloids in the Facilitated Transport of Contaminants in Saturated Porous media (M. Elimelech and J. N. Ryan). Index.

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Crossref · 10.1515/ci.2002.24.4.26a

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  • Organic matter and variable charge minerals are much more effective scavengers of polyvalent cations because complexation processes are the dominant binding mechanisms.

    “Organic matter and variable charge minerals (metal oxides, allophanes, imogolite) are much more effective scavengers of polyvalent cations because complexation processes are the dominant binding mechanisms [5, 6, 9, 10].”
  • The geochemical cycling of Se parallels that of sulfur so Se is predominantly cycled through biological pathways.

    “The geochemical cycling of Se parallels that of sulfur so Se is predominantly cycled through biological pathways [9, 28].”

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Cited by 142

Authors
Huang, P. M., Bollag, J. M., & Senesi, N.
Venue
Chemistry International -- Newsmagazine for IUPAC
Published
2002-01
Volume
24
Issue
4
ISSN
  • 0193-6484 (ISSN-L)
  • 1365-2192
OpenAlex
W1980689999
Cited by
142
References
0
Citations by year
2025: 3 · 2024: 7 · 2023: 4 · 2022: 6 · 2021: 8 · 2020: 10 · 2019: 7 · 2018: 6 · 2017: 9 · 2016: 4 · 2015: 3 · 2014: 12 · 2013: 3 · 2012: 7
FWCI
9.83
Type
journal article
Language
en
Open access
closed
Locations
Chemistry International (publishedVersion)
Topics
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
  • Physical Sciences › Environmental Science › Pollution › Microbial bioremediation and biosurfactants
  • Physical Sciences › Environmental Science › Ecology › Microbial Community Ecology and Physiology
Keywords
soil microbes, soil minerals, soil colloids, metal oxide formation, metal mobilization, bioremediation, rhizosphere, biogeochemical cycles, mineral colloids, anaerobic conditions, contaminant transport in porous media, soil structure stabilization

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