Biochar improves soil organic carbon stability by shaping the microbial community structures at different soil depths four years after an incorporation in a farmland soil DOI Creative Commons
Ruiling Ma,

Xiulan Wu,

Zhiwei Liu

et al.

Current Research in Environmental Sustainability, Journal Year: 2023, Volume and Issue: 5, P. 100214 - 100214

Published: Jan. 1, 2023

Soil organic carbon (SOC), mineralization and microbial community structures were investigated at different depths of farmland soils 4 years after a single biochar amendment. Biochar increased SOC 0-20cm (10.7%) 20-40cm (24.9%). Mineralization decreased with depth further 12.3% (0-20cm), 8.5% (20-40cm) 30.5% (40-60cm) Subsoils selected for oligotrophs (e.g., Chloroflexi, Acidobacteria) associated lower rates limited copiotrophs Proteobacteria, Ascomycota) which exhibit higher respiration rates. enhanced in topsoil restricted all depths. This demonstrates how increases stability by changing

Language: Английский

Deep-injected straw incorporation enhances subsoil quality and wheat productivity DOI
Jun Ling, Jie Zhou,

Gong Wu

et al.

Plant and Soil, Journal Year: 2022, Volume and Issue: 499(1-2), P. 207 - 220

Published: Aug. 20, 2022

Language: Английский

Citations

32

Assessing the effect of arable management practices on carbon storage and fractions after 24 years in boreal conditions of Finland DOI Creative Commons
Anna‐Reetta Salonen, Helena Soinne, Rachel Creamer

et al.

Geoderma Regional, Journal Year: 2023, Volume and Issue: 34, P. e00678 - e00678

Published: July 1, 2023

Soil organic matter (SOM) plays an important role in soil functions that are crucial for sustainable agriculture. Understanding how agricultural management and properties affect SOM different depths would aid maintaining increasing throughout the profile. We sampled a 24 year-old cultivation field experiment with conventional cropping systems, adjacent unmanaged meadow to 70 cm depth assess total carbon (OC) stocks distribution of OC into mineral-associated (MAOM), particulate (POM) dissolved (DOM) matter. found >83% was MAOM fraction, across MAOM, POM DOM within not strongly affected by management. Largest (169 t ha−1) together largest plant root biomass meadow, which highlights potential deep-rooting plants sequestering soil. The saturation state assessed based on clay ratio Hassink's Equation (Hassink 1997). seemed underestimate accrual capacity these soils thus overestimated state, whereas indicated all depths, except topsoil. These varying results suggest applied metric should be type -depth specific. also determined contribution content aluminum iron oxides explaining amount OC, MAOM-C POM-C. In contrast oxides, well correlated any fractions below 20 depth, suggesting estimating deeper texture alone. Our indicate can play transporting stabilizing

Language: Английский

Citations

17

A quantitative review of the effects of residue removing on soil organic carbon in croplands DOI
Roberto Álvarez

Soil and Tillage Research, Journal Year: 2024, Volume and Issue: 240, P. 106098 - 106098

Published: March 27, 2024

Language: Английский

Citations

8

Deciphering microbial drivers of soil organic matter mineralization in surface and subsurface soil during long-term vegetation succession DOI
Jingwei Shi, Lei Deng, Lin Yang

et al.

Agriculture Ecosystems & Environment, Journal Year: 2024, Volume and Issue: 374, P. 109186 - 109186

Published: July 21, 2024

Language: Английский

Citations

8

Biochar improves soil organic carbon stability by shaping the microbial community structures at different soil depths four years after an incorporation in a farmland soil DOI Creative Commons
Ruiling Ma,

Xiulan Wu,

Zhiwei Liu

et al.

Current Research in Environmental Sustainability, Journal Year: 2023, Volume and Issue: 5, P. 100214 - 100214

Published: Jan. 1, 2023

Soil organic carbon (SOC), mineralization and microbial community structures were investigated at different depths of farmland soils 4 years after a single biochar amendment. Biochar increased SOC 0-20cm (10.7%) 20-40cm (24.9%). Mineralization decreased with depth further 12.3% (0-20cm), 8.5% (20-40cm) 30.5% (40-60cm) Subsoils selected for oligotrophs (e.g., Chloroflexi, Acidobacteria) associated lower rates limited copiotrophs Proteobacteria, Ascomycota) which exhibit higher respiration rates. enhanced in topsoil restricted all depths. This demonstrates how increases stability by changing

Language: Английский

Citations

16