Structural equation modeling reveals iron (hydr)oxides as a strong mediator of N mineralization in California agricultural soils-Reference-Cited by-同舟云学术

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Structural equation modeling reveals iron (hydr)oxides as a strong mediator of N mineralization in California agricultural soils

Published:2018-04 Issue: Volume:315 Page:120-129
ISSN:0016-7061
Container-title:Geoderma
language:en
Short-container-title:Geoderma

Author:

Wade Jordon,Waterhouse Hannah^ORCID,Roche Leslie M.,Horwath William R.

Publisher

Elsevier BV

Subject

Soil Science

Reference117 articles.

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2. Soil minerals and humic acids alter enzyme stability: implications for ecosystem processes;Allison;Biogeochemistry,2006

3. Responses of extracellular enzymes to simple and complex nutrient inputs;Allison;Soil Biol. Biochem.,2005

4. Protein-mineral interactions: molecular dynamics simulations capture importance of variations in mineral surface composition and structure;Andersen;Langmuir,2016

5. Visions of a more precise soil biology;Andrén;Eur. J. Soil Sci.,2008

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2. Comparison of reactive transport and non-equilibrium modeling approaches for the estimation of nitrate leaching under large water application events;Journal of Hydrology;2024-01

3. Reviews and syntheses: Iron – a driver of nitrogen bioavailability in soils?;Biogeosciences;2023-09-26

4. Rhizosphere Fungal Dynamics in Sugarcane during Different Growth Stages;International Journal of Molecular Sciences;2023-03-16

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