Root Carbon Interaction with Soil Minerals Is Dynamic, Leaving a Legacy of Microbially Derived Residues-Reference-Cited by-同舟云学术

Root Carbon Interaction with Soil Minerals Is Dynamic, Leaving a Legacy of Microbially Derived Residues

Published:2021-09-24 Issue: Volume: Page:
ISSN:0013-936X
Container-title:Environmental Science & Technology
language:en
Short-container-title:Environ. Sci. Technol.

Author:

Neurath Rachel A.¹²^ORCID,Pett-Ridge Jennifer³⁴^ORCID,Chu-Jacoby Ilexis¹,Herman Donald¹,Whitman Thea⁵^ORCID,Nico Peter S.⁶,Lipton Andrew S.⁷^ORCID,Kyle Jennifer⁷,Tfaily Malak M.⁷⁸,Thompson Alison⁷^ORCID,Firestone Mary K.¹

Affiliation:

1. Department of Environmental Science, Policy, and Management, University of California, Berkeley, California 94720, United States

2. Biosciences Division, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States

3. Physical and Life Sciences Directorate, Lawrence Livermore National Laboratory, Livermore, California 94551, United States

4. Life & Environmental Sciences Department, University of California Merced, Merced, California 95343, United States

5. Department of Soil Science, University of Wisconsin, Madison, Madison, Wisconsin 53706, United States

6. Earth and Environmental Sciences Area, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States

7. Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99354, United States

8. Department of Environmental Science, University of Arizona, Tucson, Arizona 85721, United States

Publisher

American Chemical Society (ACS)

Subject

Environmental Chemistry,General Chemistry

Link

https://pubs.acs.org/doi/pdf/10.1021/acs.est.1c00300

Reference90 articles.

1. The nature and dynamics of soil organic matter: Plant inputs, microbial transformations, and organic matter stabilization

2. Evidence for the primacy of living root inputs, not root or shoot litter, in forming soil organic carbon

3. Rhizosphere processes are quantitatively important components of terrestrial carbon and nutrient cycles

4. Carbon input by plants into the soil. Review

5. Is soil carbon mostly root carbon? Mechanisms for a specific stabilisation

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