The molecular composition of soil dissolved organic matter regulated by reactive mineral-associated organic matter under a broad range of climates
Organic matter retained by reactive minerals constitutes an essential mechanism for long-term storage of carbon in soil, a process that is governed by climate factors. However, how the reactive mineral-associated organic matter affects the composition of soil dissolved organic matter (DOM) across a...
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| Published in: | Applied geochemistry Vol. 179; p. 106261 |
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| Main Authors: | , |
| Format: | Journal Article |
| Language: | English |
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01.01.2025
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| ISSN: | 0883-2927 |
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| Abstract | Organic matter retained by reactive minerals constitutes an essential mechanism for long-term storage of carbon in soil, a process that is governed by climate factors. However, how the reactive mineral-associated organic matter affects the composition of soil dissolved organic matter (DOM) across a broad range of climates remains unclear. In this study, the contents of reactive minerals and their associated organic matter were determined by the chemical extraction method. Moreover, the effects of organic matter retained by reactive minerals on soil DOM composition were investigated at molecular level across a wide environmental gradient, by employing Fourier transform ion cyclotron resonance mass spectrometry, solid-state 13C nuclear magnetic resonance and statistical analyses. The results of FT-ICR-MS and correlation analyses indicated that the relative abundances of carbohydrates and proteins/amino sugars decreased, while the relative abundance of condensed aromatics increased with the increase of the content of organic matter retained by reactive minerals per unit mass (i.e., (OC)RN) in soils. We highlighted that the adsorption and dissolution processes of DOM molecules, especially aromatic molecules, on reactive minerals played crucial roles in regulating the molecular composition of DOM in soil solution. Furthermore, (OC)RN was controlled by climate-driven chemical weathering (e.g., precipitation). Our results imply that (OC)RN is a key variable for regulating soil DOM composition under the impacts of climates, and can be used in developing prediction models for carbon cycling.
•Soil DOM composition was regulated by reactive mineral-retained organic matter.•(OC)RN was driven by precipitation.•The abundances of carbohydrates and proteins decreased with the increase of (OC)RN.•The abundance of condensed aromatics increased with the increase of (OC)RN. |
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| AbstractList | Organic matter retained by reactive minerals constitutes an essential mechanism for long-term storage of carbon in soil, a process that is governed by climate factors. However, how the reactive mineral-associated organic matter affects the composition of soil dissolved organic matter (DOM) across a broad range of climates remains unclear. In this study, the contents of reactive minerals and their associated organic matter were determined by the chemical extraction method. Moreover, the effects of organic matter retained by reactive minerals on soil DOM composition were investigated at molecular level across a wide environmental gradient, by employing Fourier transform ion cyclotron resonance mass spectrometry, solid-state 13C nuclear magnetic resonance and statistical analyses. The results of FT-ICR-MS and correlation analyses indicated that the relative abundances of carbohydrates and proteins/amino sugars decreased, while the relative abundance of condensed aromatics increased with the increase of the content of organic matter retained by reactive minerals per unit mass (i.e., (OC)RN) in soils. We highlighted that the adsorption and dissolution processes of DOM molecules, especially aromatic molecules, on reactive minerals played crucial roles in regulating the molecular composition of DOM in soil solution. Furthermore, (OC)RN was controlled by climate-driven chemical weathering (e.g., precipitation). Our results imply that (OC)RN is a key variable for regulating soil DOM composition under the impacts of climates, and can be used in developing prediction models for carbon cycling.
•Soil DOM composition was regulated by reactive mineral-retained organic matter.•(OC)RN was driven by precipitation.•The abundances of carbohydrates and proteins decreased with the increase of (OC)RN.•The abundance of condensed aromatics increased with the increase of (OC)RN. |
| ArticleNumber | 106261 |
| Author | Ding, Yang Shi, Zhenqing |
| Author_xml | – sequence: 1 givenname: Yang surname: Ding fullname: Ding, Yang email: yding@usc.edu.cn organization: Key Discipline Laboratory for National Defense for Biotechnology in Uranium Mining and Hydrometallurgy, University of South China, Hengyang, 421001, PR China – sequence: 2 givenname: Zhenqing surname: Shi fullname: Shi, Zhenqing organization: The Key Lab of Pollution Control and Ecosystem Restoration in Industry Clusters, Ministry of Education, School of Environment and Energy, South China University of Technology, Guangzhou, Guangdong, 510006, PR China |
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| Keywords | Precipitation Reactive minerals Dissolved organic matter Molecular composition Carbon cycling |
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