{"title":"通过施用农作有机肥增加土壤有机碳作为土壤深度的函数:全球综合","authors":"Roberto Alvarez","doi":"10.1016/j.scitotenv.2025.179933","DOIUrl":null,"url":null,"abstract":"<div><div>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<sup>−1</sup>. 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.</div></div>","PeriodicalId":422,"journal":{"name":"Science of the Total Environment","volume":"991 ","pages":"Article 179933"},"PeriodicalIF":8.0000,"publicationDate":"2025-06-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Increasing soil organic carbon by applying farm-made organic fertilizers as a function of soil depth: A global synthesis\",\"authors\":\"Roberto Alvarez\",\"doi\":\"10.1016/j.scitotenv.2025.179933\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>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<sup>−1</sup>. 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.</div></div>\",\"PeriodicalId\":422,\"journal\":{\"name\":\"Science of the Total Environment\",\"volume\":\"991 \",\"pages\":\"Article 179933\"},\"PeriodicalIF\":8.0000,\"publicationDate\":\"2025-06-24\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Science of the Total Environment\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0048969725015736\",\"RegionNum\":1,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Science of the Total Environment","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0048969725015736","RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
摘要
增加土壤有机碳(SOC)的管理实践具有生产和环境效益。施用有机肥可增加表层土壤(≤30 cm)的有机碳,但其在剖面水平上的影响尚不清楚。目的是通过使用农作有机肥来量化表层和深层土壤(30-150 cm)的有机碳变化。数据收集自434个现场实验,并采用元分析技术。在施用有机肥的处理中,在60厘米深的土壤有机碳储量显著增加,增幅在28%至30%之间。在初始有机碳含量低、质地粗糙、水分有效度低的土壤中,表层有机碳的增加幅度较大,谷物和蔬菜作物的有机碳增加幅度大于饲料作物。表层土壤有机碳储量变化与肥料累积碳输入呈线性相关。碳保持效率(CRE)在低碳投入下最高,随着碳投入的增加呈指数下降,在施用200 Mg C ha - 1时稳定在8%左右。利用42个试验的数据,计算出考虑表层土和底土(30-60 cm)的有机碳储量比单独考虑表层土增加41%,这将使CRE增加11%以上,这一值与文献中报道的作物残茬的CRE相似。这些结果表明,有机肥对有机碳储量的影响也应在底土中进行测量,并且有机碳的增加大于以往仅考虑表土的综合研究报告。
Increasing soil organic carbon by applying farm-made organic fertilizers as a function of soil depth: A global synthesis
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−1. 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.
期刊介绍:
The Science of the Total Environment is an international journal dedicated to scientific research on the environment and its interaction with humanity. It covers a wide range of disciplines and seeks to publish innovative, hypothesis-driven, and impactful research that explores the entire environment, including the atmosphere, lithosphere, hydrosphere, biosphere, and anthroposphere.
The journal's updated Aims & Scope emphasizes the importance of interdisciplinary environmental research with broad impact. Priority is given to studies that advance fundamental understanding and explore the interconnectedness of multiple environmental spheres. Field studies are preferred, while laboratory experiments must demonstrate significant methodological advancements or mechanistic insights with direct relevance to the environment.