Differential Responses of Soil Thermal Conductivity, Microbial Carbon Use Efficiency, and Soil Organic Carbon to Feedstock-Specific Biochar Under Alternate Drying–Wetting Cycles

Biochar can alter soil physical conditions, microbial carbon processing, and soil organic carbon (SOC) responses under fluctuating moisture, yet how these changes are coordinated remains insufficiently understood. We conducted a two-season greenhouse pot experiment to examine the initial (first-year) and residual (second-year) effects of wheat-straw biochar (WSB) and softwood biochar (SWB) under conventional deficit irrigation (CDI) and alternate drying–wetting cycles (DWC). Compared with unamended soil, biochar amendment improved water-dispersible microaggregate-size distribution, mean microaggregate size, and water-holding capacity, which contributed to reduced soil thermal conductivity (STC) by 6.0–14.2%. Biochar application also improved microbial carbon use efficiency (CUE) by 41.1–52.3%, with WSB generally showing stronger and more persistent effects than SWB. Relative to CDI, DWC increased soil respiration rate by 14.9–48.8% but decreased CUE by 7.4–10.2% and SOC by 3.0–10.3%, indicating a shift toward greater respiratory carbon loss under repeated moisture fluctuations. Biochar amendment increased SOC across both seasons, particularly under WSB, and partially alleviated the DWC-associated reductions in CUE and SOC. Correlation analyses showed that lower STC was associated with higher CUE and SOC, but these relationships should be interpreted as coordinated associations rather than direct evidence of a causal thermal-regulation mechanism. Principal component and random forest analyses further highlighted STC as a prominent variable associated with variation in CUE and SOC among the measured soil attributes. These findings indicate that biochar-mediated changes in soil physical conditions are closely associated with microbial CUE and SOC responses under drying–wetting cycles, wherein soil thermal properties may represent an important physical dimension of these carbon responses.

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Publication Details

Journal
Agronomy
Published
2026-06-30
DOI
https://doi.org/10.3390/agronomy16131262
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
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article

Differential Responses of Soil Thermal Conductivity, Microbial Carbon Use Efficiency, and Soil Organic Carbon to Feedstock-Specific Biochar Under Alternate Drying–Wetting Cycles

Jingxiang Hou, Heng Wan, Gang Cao, Ninghui Xie et al.
Agronomy
Soil Carbon and Nitrogen Dynamics
article

Differential Responses of Soil Thermal Conductivity, Microbial Carbon Use Efficiency, and Soil Organic Carbon to Feedstock-Specific Biochar Under Alternate Drying–Wetting Cycles

Jingxiang Hou, Heng Wan, Gang Cao, Ninghui Xie, Fulai Liu, Zhenhua Wei, Xi Zhang, Hailin Zhang, Jinhui Ma, Yunfei Di, He Ye, Fei Li, Mei Hong
article en

Abstract

Biochar can alter soil physical conditions, microbial carbon processing, and soil organic carbon (SOC) responses under fluctuating moisture, yet how these changes are coordinated remains insufficiently understood. We conducted a two-season greenhouse pot experiment to examine the initial (first-year) and residual (second-year) effects of wheat-straw biochar (WSB) and softwood biochar (SWB) under conventional deficit irrigation (CDI) and alternate drying–wetting cycles (DWC). Compared with unamended soil, biochar amendment improved water-dispersible microaggregate-size distribution, mean microaggregate size, and water-holding capacity, which contributed to reduced soil thermal conductivity (STC) by 6.0–14.2%. Biochar application also improved microbial carbon use efficiency (CUE) by 41.1–52.3%, with WSB generally showing stronger and more persistent effects than SWB. Relative to CDI, DWC increased soil respiration rate by 14.9–48.8% but decreased CUE by 7.4–10.2% and SOC by 3.0–10.3%, indicating a shift toward greater respiratory carbon loss under repeated moisture fluctuations. Biochar amendment increased SOC across both seasons, particularly under WSB, and partially alleviated the DWC-associated reductions in CUE and SOC. Correlation analyses showed that lower STC was associated with higher CUE and SOC, but these relationships should be interpreted as coordinated associations rather than direct evidence of a causal thermal-regulation mechanism. Principal component and random forest analyses further highlighted STC as a prominent variable associated with variation in CUE and SOC among the measured soil attributes. These findings indicate that biochar-mediated changes in soil physical conditions are closely associated with microbial CUE and SOC responses under drying–wetting cycles, wherein soil thermal properties may represent an important physical dimension of these carbon responses.

AgronomyVol. 16(13)
Inner Mongolia University for Nationalities (CN), Oklahoma State University (US), Inner Mongolia Agricultural University (CN), University of Copenhagen (DK), Inner Mongolia University (CN), Institute of Soil and Water Conservation (CN), Tongliao Academy of Agricultural Sciences (CN), Xinjiang Academy of Agricultural Sciences (CN), China Agricultural University (CN)
Inner Mongolia Agricultural University
Clean water and sanitation
Openalex Percentile: Top 11%
Soil Carbon and Nitrogen Dynamics
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