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April 22, 2026Land0 citationsOpen Access

Spatiotemporal Dynamics of Deep Soil Organic Carbon and Its Response to Agricultural Management: Evidence from Long-Term Monitoring Data in Typical Farmlands in China

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SZS Y ZhangCWChengjun Wang

Key Points

  • The study aims to analyze the dynamics of deep soil organic carbon in response to various agricultural management practices.
  • Analyzed long-term fixed-site monitoring data from 120 farmland plots across China.
  • Characterized SOC dynamics below 20 cm using spatial analysis and panel fixed-effects model.
  • Compared effects of different fertilization, tillage modes, and farmland types on SOC levels at various depths.
  • SOC content significantly increased by 4.07% in the 60–100 cm layer during the study period.
  • Co-application of organic and inorganic materials was more effective for SOC enhancement than single organic inputs.
  • Conventional tillage favored SOC enhancement at deeper layers but was less effective in shallower layers than reduced or no-tillage methods.

Abstract

Understanding the dynamics of soil organic carbon (SOC) in farmland is crucial for assessing soil health, quantifying ecosystem potential for SOC enrichment, and guiding sustainable agricultural management. Existing research on SOC sequestration and mineralization has focused mainly on the topsoil layer (0–20 cm), whereas systematic evidence on how deep SOC (>20 cm) responds to agricultural management, and on strategies to enhance deep carbon sequestration, remains limited. This study uses long-term fixed-site monitoring data from 120 farmland plots across 21 typical farmland ecosystem stations and farmland–complex ecosystem stations within the Chinese Ecosystem Research Network (CERN) over 17 years (2004–2020). Using spatial analysis, we characterize the spatiotemporal dynamics of SOC below 20 cm along soil profiles across seven major geographical zones in China. We then estimate the heterogeneous effects of fertilization and straw-management practices (S, straw returning; SCF, straw returning with chemical fertilizer; OF, organic fertilizer; OCF, organic fertilizer with chemical fertilizer), tillage modes, and farmland types on SOC in the 20–40 cm, 40–60 cm, and 60–100 cm layers using a panel fixed-effects model. The results indicate pronounced vertical heterogeneity in SOC below 20 cm and a clear spatial gradient. The 60–100 cm layer shows a significant increase in SOC content during the study period, with a cumulative increase of 4.07%. Relative to single organic inputs, the co-application of organic and inorganic materials improves deep soil SOC enhancement efficiency. Compared with reduced tillage and no-tillage, conventional tillage is less conducive to SOC enhancement in layers shallower than 60 cm, yet it has a significant positive impact on SOC in the 60–100 cm layer. Compared with dryland and irrigated land, paddy fields are less favorable for SOC enhancement below 20 cm. Consequently, regarding agricultural practice, a composite tillage regime combining “surface conservation tillage with periodic deep tillage” should be promoted to foster deep SOC enhancement.

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Cite This Study

Zhang et al. (2026) studied this question.

synapsesocial.com/papers/69e866c96e0dea528ddeb1c2https://doi.org/10.3390/land15040676
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