Pathways of soil organic carbon stabilization driven by long-term straw returning practices in a rainfed agroecosystem

IF 7.9 1区 农林科学 Q1 SOIL SCIENCE
Geoderma Pub Date : 2026-10-01 Epub Date: 2026-10-05 DOI:10.1016/j.geoderma.2026.118077
Gu Fengxue, Wang Hetan, Yang Zhenxing, Zhou Huaiping, Zhang Wenju, Sun Dongbao, Mei Xurong, Li Suhang
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Abstract

Enhancing soil organic carbon (SOC) stability is a central strategy for achieving carbon sequestration, emission reduction, and sustainable soil fertility improvement in rainfed agroecosystems. Straw returning is a widely adopted practice to increase SOC stocks, yet the microbially mediated mechanisms by which different straw return modes regulate SOC stabilization remain poorly constrained, particularly across the Loess Plateau of China. Here, we leveraged a 30-year field experiment in a rainfed maize system to compare three straw return strategies under equivalent carbon input: straw mulching (S1), shredded straw incorporation (S2), and livestock digestion return (S3). We integrated physical aggregate fractionation with multi-biomarker analyses (lignin phenols, amino sugars, and phospholipid fatty acids) and extracellular enzyme assays to elucidate the divergent pathways of SOC stabilization. Our results demonstrated distinct carbon stabilization pathways among the three treatments. S1 followed a physical protection pathway, characterized by the highest fungal-to-bacterial ratio and the preservation of plant-derived lignin within macroaggregates, but resulted in a limited SOC increase (+15.56 %) and low carbon conversion efficiency (+17.45 %). S2 represented an intermediate fungal decomposition pathway; although lignin phenol content increased significantly across all aggregate fractions, high ligninolytic enzyme activities consumed substantial carbon, yielding a moderate SOC gain of + 19.44 %. In contrast, S3 achieved synergistic stabilization via microbial transformation. The low C/N ratio of manure alleviated nutrient limitation, fostering a bacterial- and actinobacterial-dominated community (reaching 84.96 nmol·g−1 PLFA in microaggregates) and upregulating hydrolytic enzyme activities by 73.93 %–193.65 %. This shift promoted the formation of microaggregates (+21.18 %) and silt–clay particles (+40.55 %), with microbial necromass contributing > 40 % to stable SOC pools. Consequently, S3 maximized SOC storage with a 40.00 % increase and achieved the highest carbon conversion efficiency (+29.15 %). These findings highlight that livestock-mediated straw return optimizes the continuum of bacterial proliferation, microaggregate assembly, and microbial necromass accrual, representing an effective strategy for enhancing both the magnitude and long-term stability of SOC in dryland agroecosystems on the Loess Plateau.
长期秸秆还田对旱作农业生态系统土壤有机碳稳定的影响
提高土壤有机碳(SOC)稳定性是实现旱作农业生态系统固碳、减排和土壤肥力可持续改善的核心战略。秸秆还田是增加土壤有机碳储量的一种普遍做法,但不同秸秆还田方式对土壤有机碳稳定的微生物调控机制尚不清楚,特别是在黄土高原地区。在此,我们利用一项为期30年的旱作玉米系统田间试验,比较了在同等碳输入条件下秸秆还田的三种策略:秸秆覆盖(S1)、秸秆碎化(S2)和牲畜消化还田(S3)。我们将物理聚集体分离与多生物标志物分析(木质素酚类、氨基糖和磷脂脂肪酸)和细胞外酶分析结合起来,阐明了SOC稳定的不同途径。我们的研究结果表明,三种处理之间的碳稳定途径不同。S1遵循物理保护途径,其特点是真菌与细菌的比例最高,并且在大团聚体中保存了植物来源的木质素,但导致有限的SOC增加(+ 15.56%)和低碳转化效率(+ 17.45%)。S2为中间真菌分解途径;虽然木质素酚含量在所有团聚体组分中显著增加,但高木质素分解酶活性消耗了大量碳,产生了+ 19.44%的适度SOC增益。相比之下,S3通过微生物转化实现了协同稳定。低碳氮比缓解了养分限制,形成了以细菌和放线菌为主的群落(微团聚体达到84.96 nmol·g−1 PLFA),水解酶活性提高了73.93% ~ 193.65%。这种转变促进了微团聚体(+ 21.18%)和粉质粘土颗粒(+ 40.55%)的形成,微生物坏死团块对稳定的有机碳库贡献了40%。结果表明,S3最大限度地增加了40.00%的碳储量,并实现了最高的碳转化效率(+ 29.15%)。这些研究结果表明,家畜介导的秸秆还田优化了细菌增殖、微团聚体聚集和微生物坏死块积累的连续性,是提高黄土高原旱地农业生态系统有机碳含量和长期稳定性的有效策略。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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