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通过施用农家有机肥增加土壤有机碳随土壤深度的变化:一项全球综合研究。

Increasing soil organic carbon by applying farm-made organic fertilizers as a function of soil depth: A global synthesis.

作者信息

Alvarez Roberto

机构信息

Facultad de Agronomía, Universidad de Buenos Aires-CONICET, Av. San Martín 4453 (1417), Buenos Aires, Argentina.

出版信息

Sci Total Environ. 2025 Aug 20;991:179933. doi: 10.1016/j.scitotenv.2025.179933. Epub 2025 Jun 24.

DOI:10.1016/j.scitotenv.2025.179933
PMID:40555046
Abstract

Management practices that increase soil organic carbon (SOC) have productive and environmental benefits. Application of organic fertilizers increases SOC in the topsoil (≤30 cm) but its impact at the profile level is poorly known. The objective was to quantify SOC changes in surface and deep soil (30-150 cm) through the use farm-made organic fertilizers. Data were collected from 434 field experiments and meta-analysis techniques were used. Significant increases in SOC stock were detected up to 60 cm depth in treatments that received organic fertilizers, ranging between 28 and 30 %. SOC increases were greater in the topsoil layer in soils with low initial SOC, coarse texture, low water availability, and in grain and vegetable crops compared to forage crops. Changes in topsoil SOC stocks were linearly related to the cumulative carbon input from fertilizers. Carbon retention efficiency (CRE) was highest for low carbon inputs and decreased exponentially as carbon input increased, stabilizing at approximately 8 % with applications >200 Mg C ha. Using data from 42 experiments, it was calculated that the increase in SOC stocks was 41 % higher considering both the topsoil and subsoil (30-60 cm) compared to the topsoil alone, which would increase the CRE over 11 %, a value similar to the CRE of crop residues reported in the literature. These results show that the effect of organic fertilizers on SOC stocks should also be measured in the subsoil and that the increases in SOC are greater than those reported in previous synthesis studies that considered only the topsoil.

摘要

增加土壤有机碳(SOC)的管理措施具有生产效益和环境效益。施用有机肥料可增加表层土壤(≤30厘米)中的有机碳含量,但其在剖面层面的影响却鲜为人知。目的是通过使用农家自制有机肥料来量化表层和深层土壤(30 - 150厘米)中有机碳的变化。数据来自434个田间试验,并采用了荟萃分析技术。在施用有机肥料的处理中,在60厘米深度以内检测到有机碳储量显著增加,增幅在28%至30%之间。与饲料作物相比,初始有机碳含量低、质地粗糙、水分供应少的土壤以及谷物和蔬菜作物的表层土壤中有机碳增加幅度更大。表层土壤有机碳储量的变化与肥料累积碳输入呈线性相关。低碳输入时碳保留效率(CRE)最高,随着碳输入增加呈指数下降,当施用量>200 Mg C ha时稳定在约8%。利用42个试验的数据计算得出,考虑表层土壤和底土(30 - 60厘米)时有机碳储量的增加比仅考虑表层土壤时高41%,这将使碳保留效率提高超过11%,该值与文献中报道的作物残茬的碳保留效率相似。这些结果表明,有机肥料对有机碳储量的影响也应在底土中进行测量,并且有机碳的增加幅度大于以往仅考虑表层土壤的综合研究报告中的增幅。

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