Soybean inclusion reduces soil organic matter mineralization despite increasing its temperature sensitivity

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • Zhengjun Yan
  • Rong Jia
  • Jie Zhou
  • Kazem Zamanian
  • Yadong Yang
  • Kevin Z Mganga
  • Zhaohai Zeng
  • Huadong Zang

Organisationseinheiten

Externe Organisationen

  • China Agricultural University
  • Nanjing Agricultural University
  • Utrecht University
  • Ministry of Agriculture and Rural Affairs
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Details

OriginalspracheEnglisch
Aufsatznummer171334
Seiten (von - bis)171334
FachzeitschriftScience of the Total Environment
Jahrgang922
Frühes Online-Datum27 Feb. 2024
PublikationsstatusVeröffentlicht - 20 Apr. 2024

Abstract

Legume-based cropping increased the diversity of residues and rhizodeposition input into the soil, thus affecting soil organic matter (SOM) stabilization. Despite this, a comprehensive understanding of the mechanisms governing SOM mineralization and its temperature sensitivity across bulk soil and aggregate scales concerning legume inclusion remains incomplete. Here, a 6-year field experiment was conducted to investigate the effects of three cropping systems (i.e., winter wheat/summer maize, winter wheat/summer maize-soybean, and nature fallow) on SOM mineralization, its temperature sensitivity, and the main drivers in both topsoil (0–20 cm) and subsoil (20–40 cm). Soybean inclusion decreased the SOM mineralization by 17%–24%, while concurrently increasing the majority of soil biochemical properties, such as carbon (C) acquisition enzyme activities (5%–22%) and microbial biomass C (5%–9%), within the topsoil regardless of temperature. This is attributed to the increased substrate availability (e.g., dissolved organic C) facilitating microbial utilization, thus devoting less energy to mining nutrients under diversified cropping. In addition, SOM mineralization was lower within macroaggregates (∼12%), largely driven by substrate availability irrespective of aggregate sizes. In contrast, diversified cropping amplified the Q 10 of SOM mineralization in mesoaggregates (+6%) and microaggregates (+5%) rather than in macroaggregates. This underscores the pivotal role of mesoaggregates and microaggregates in dominating the Q 10 of SOM mineralization under soybean-based cropping. In conclusion, legume-based cropping diminishes soil organic matter mineralization despite increasing its temperature sensitivity, which proposes a potential strategy for C-neutral agriculture and climate warming mitigation.

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Soybean inclusion reduces soil organic matter mineralization despite increasing its temperature sensitivity. / Yan, Zhengjun; Jia, Rong; Zhou, Jie et al.
in: Science of the Total Environment, Jahrgang 922, 171334, 20.04.2024, S. 171334.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Yan, Z., Jia, R., Zhou, J., Zamanian, K., Yang, Y., Mganga, K. Z., Zeng, Z., & Zang, H. (2024). Soybean inclusion reduces soil organic matter mineralization despite increasing its temperature sensitivity. Science of the Total Environment, 922, 171334. Artikel 171334. Vorabveröffentlichung online. https://doi.org/10.1016/j.scitotenv.2024.171334
Yan Z, Jia R, Zhou J, Zamanian K, Yang Y, Mganga KZ et al. Soybean inclusion reduces soil organic matter mineralization despite increasing its temperature sensitivity. Science of the Total Environment. 2024 Apr 20;922:171334. 171334. Epub 2024 Feb 27. doi: 10.1016/j.scitotenv.2024.171334
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title = "Soybean inclusion reduces soil organic matter mineralization despite increasing its temperature sensitivity",
abstract = "Legume-based cropping increased the diversity of residues and rhizodeposition input into the soil, thus affecting soil organic matter (SOM) stabilization. Despite this, a comprehensive understanding of the mechanisms governing SOM mineralization and its temperature sensitivity across bulk soil and aggregate scales concerning legume inclusion remains incomplete. Here, a 6-year field experiment was conducted to investigate the effects of three cropping systems (i.e., winter wheat/summer maize, winter wheat/summer maize-soybean, and nature fallow) on SOM mineralization, its temperature sensitivity, and the main drivers in both topsoil (0–20 cm) and subsoil (20–40 cm). Soybean inclusion decreased the SOM mineralization by 17%–24%, while concurrently increasing the majority of soil biochemical properties, such as carbon (C) acquisition enzyme activities (5%–22%) and microbial biomass C (5%–9%), within the topsoil regardless of temperature. This is attributed to the increased substrate availability (e.g., dissolved organic C) facilitating microbial utilization, thus devoting less energy to mining nutrients under diversified cropping. In addition, SOM mineralization was lower within macroaggregates (∼12%), largely driven by substrate availability irrespective of aggregate sizes. In contrast, diversified cropping amplified the Q 10 of SOM mineralization in mesoaggregates (+6%) and microaggregates (+5%) rather than in macroaggregates. This underscores the pivotal role of mesoaggregates and microaggregates in dominating the Q 10 of SOM mineralization under soybean-based cropping. In conclusion, legume-based cropping diminishes soil organic matter mineralization despite increasing its temperature sensitivity, which proposes a potential strategy for C-neutral agriculture and climate warming mitigation.",
keywords = "Aggregates, Diversified cropping, Legumes, Microbial biomass, Rotation, Temperature sensitivity",
author = "Zhengjun Yan and Rong Jia and Jie Zhou and Kazem Zamanian and Yadong Yang and Mganga, {Kevin Z} and Zhaohai Zeng and Huadong Zang",
note = "Funding Information: This study was financially supported by the National Natural Science Foundation of China ( 32101850 ).",
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Download

TY - JOUR

T1 - Soybean inclusion reduces soil organic matter mineralization despite increasing its temperature sensitivity

AU - Yan, Zhengjun

AU - Jia, Rong

AU - Zhou, Jie

AU - Zamanian, Kazem

AU - Yang, Yadong

AU - Mganga, Kevin Z

AU - Zeng, Zhaohai

AU - Zang, Huadong

N1 - Funding Information: This study was financially supported by the National Natural Science Foundation of China ( 32101850 ).

PY - 2024/4/20

Y1 - 2024/4/20

N2 - Legume-based cropping increased the diversity of residues and rhizodeposition input into the soil, thus affecting soil organic matter (SOM) stabilization. Despite this, a comprehensive understanding of the mechanisms governing SOM mineralization and its temperature sensitivity across bulk soil and aggregate scales concerning legume inclusion remains incomplete. Here, a 6-year field experiment was conducted to investigate the effects of three cropping systems (i.e., winter wheat/summer maize, winter wheat/summer maize-soybean, and nature fallow) on SOM mineralization, its temperature sensitivity, and the main drivers in both topsoil (0–20 cm) and subsoil (20–40 cm). Soybean inclusion decreased the SOM mineralization by 17%–24%, while concurrently increasing the majority of soil biochemical properties, such as carbon (C) acquisition enzyme activities (5%–22%) and microbial biomass C (5%–9%), within the topsoil regardless of temperature. This is attributed to the increased substrate availability (e.g., dissolved organic C) facilitating microbial utilization, thus devoting less energy to mining nutrients under diversified cropping. In addition, SOM mineralization was lower within macroaggregates (∼12%), largely driven by substrate availability irrespective of aggregate sizes. In contrast, diversified cropping amplified the Q 10 of SOM mineralization in mesoaggregates (+6%) and microaggregates (+5%) rather than in macroaggregates. This underscores the pivotal role of mesoaggregates and microaggregates in dominating the Q 10 of SOM mineralization under soybean-based cropping. In conclusion, legume-based cropping diminishes soil organic matter mineralization despite increasing its temperature sensitivity, which proposes a potential strategy for C-neutral agriculture and climate warming mitigation.

AB - Legume-based cropping increased the diversity of residues and rhizodeposition input into the soil, thus affecting soil organic matter (SOM) stabilization. Despite this, a comprehensive understanding of the mechanisms governing SOM mineralization and its temperature sensitivity across bulk soil and aggregate scales concerning legume inclusion remains incomplete. Here, a 6-year field experiment was conducted to investigate the effects of three cropping systems (i.e., winter wheat/summer maize, winter wheat/summer maize-soybean, and nature fallow) on SOM mineralization, its temperature sensitivity, and the main drivers in both topsoil (0–20 cm) and subsoil (20–40 cm). Soybean inclusion decreased the SOM mineralization by 17%–24%, while concurrently increasing the majority of soil biochemical properties, such as carbon (C) acquisition enzyme activities (5%–22%) and microbial biomass C (5%–9%), within the topsoil regardless of temperature. This is attributed to the increased substrate availability (e.g., dissolved organic C) facilitating microbial utilization, thus devoting less energy to mining nutrients under diversified cropping. In addition, SOM mineralization was lower within macroaggregates (∼12%), largely driven by substrate availability irrespective of aggregate sizes. In contrast, diversified cropping amplified the Q 10 of SOM mineralization in mesoaggregates (+6%) and microaggregates (+5%) rather than in macroaggregates. This underscores the pivotal role of mesoaggregates and microaggregates in dominating the Q 10 of SOM mineralization under soybean-based cropping. In conclusion, legume-based cropping diminishes soil organic matter mineralization despite increasing its temperature sensitivity, which proposes a potential strategy for C-neutral agriculture and climate warming mitigation.

KW - Aggregates

KW - Diversified cropping

KW - Legumes

KW - Microbial biomass

KW - Rotation

KW - Temperature sensitivity

UR - http://www.scopus.com/inward/record.url?scp=85186381464&partnerID=8YFLogxK

U2 - 10.1016/j.scitotenv.2024.171334

DO - 10.1016/j.scitotenv.2024.171334

M3 - Article

C2 - 38423335

VL - 922

SP - 171334

JO - Science of the Total Environment

JF - Science of the Total Environment

SN - 0048-9697

M1 - 171334

ER -

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