Mingtao Xiang , Xiaojia Chen , Songchao Chen , Chunyan Wu , Meiling Sheng , Zhouqiao Ren , Wanzhu Ma , Ming Ming , Xunfei Deng , Yu Zhan
{"title":"Spatiotemporal changes of soil organic carbon in intensive croplands over three decades: Emerging role of farmland utilization shifts","authors":"Mingtao Xiang , Xiaojia Chen , Songchao Chen , Chunyan Wu , Meiling Sheng , Zhouqiao Ren , Wanzhu Ma , Ming Ming , Xunfei Deng , Yu Zhan","doi":"10.1016/j.still.2025.106734","DOIUrl":null,"url":null,"abstract":"<div><div>Understanding spatiotemporal variation characteristics and key driving factors of soil organic carbon (SOC) is crucial for refined managements of farmland quality and carbon emissions. Nevertheless, the impact of human-induced farmland utilization activities on regional SOC dynamics remains unclear. In this study, based on 1577 farmland topsoil (0–20 cm) samples, we developed a two-tiered stratification-contextualized framework within digital soil mapping paradigm for determining the drivers for spatiotemporal SOC dynamics by partitioning farmland and constructing individual machine learning method within farmland units (FUs) in East China during the 1980s-2010s, and then estimated spatiotemporal patterns of SOC as well as evaluated drivers on SOC changes within FUs using random forest models. Our results showed that the temporal changes in topsoil SOC stocks exhibited high spatial heterogeneity across three decades. The average SOC densities for the 1980s, 2000s, and 2010s were 41.4 ± 9.3 C ha<sup>−1</sup>, 47.4 ± 8.6 C ha<sup>−1</sup> and 39.7 ± 14.4 C ha<sup>−1</sup>, respectively, with SOC densities initially increasing and then decreasing in our intensively cultivated region. Climatic changes accounted for > 75 % of the relative importance (RI) to SOC dynamics over the past 30 years. Farmland utilization shifts accelerated temporal SOC changes, with the effects coefficient increasing from 2.6 % (95 % CI: 1.7∼3.1 %) to 6.4 % (95 % CI: 3.9∼7.4 %). Induced by farmland utilization shifts, the overall changes of SOC stock increased by 0.10 Mt C during the 1980s-2000s with minimal SOC changes in FU3 and parts of FU1 (only 1 %), while decreased by 0.33 Mt C during the 2000s-2010s with approximately 12.9 % of regions in FU3, FU5, FU1 and FU6 exhibiting changes over 3 %. This work enhanced the understanding of spatiotemporal SOC variability induced by farmland utilization using machine learning method based on determined FUs, which also provided valuable guidance for soil monitoring and carbon accounting management for intensively cultivated farmland.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"254 ","pages":"Article 106734"},"PeriodicalIF":6.1000,"publicationDate":"2025-06-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Soil & Tillage Research","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0167198725002880","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0
Abstract
Understanding spatiotemporal variation characteristics and key driving factors of soil organic carbon (SOC) is crucial for refined managements of farmland quality and carbon emissions. Nevertheless, the impact of human-induced farmland utilization activities on regional SOC dynamics remains unclear. In this study, based on 1577 farmland topsoil (0–20 cm) samples, we developed a two-tiered stratification-contextualized framework within digital soil mapping paradigm for determining the drivers for spatiotemporal SOC dynamics by partitioning farmland and constructing individual machine learning method within farmland units (FUs) in East China during the 1980s-2010s, and then estimated spatiotemporal patterns of SOC as well as evaluated drivers on SOC changes within FUs using random forest models. Our results showed that the temporal changes in topsoil SOC stocks exhibited high spatial heterogeneity across three decades. The average SOC densities for the 1980s, 2000s, and 2010s were 41.4 ± 9.3 C ha−1, 47.4 ± 8.6 C ha−1 and 39.7 ± 14.4 C ha−1, respectively, with SOC densities initially increasing and then decreasing in our intensively cultivated region. Climatic changes accounted for > 75 % of the relative importance (RI) to SOC dynamics over the past 30 years. Farmland utilization shifts accelerated temporal SOC changes, with the effects coefficient increasing from 2.6 % (95 % CI: 1.7∼3.1 %) to 6.4 % (95 % CI: 3.9∼7.4 %). Induced by farmland utilization shifts, the overall changes of SOC stock increased by 0.10 Mt C during the 1980s-2000s with minimal SOC changes in FU3 and parts of FU1 (only 1 %), while decreased by 0.33 Mt C during the 2000s-2010s with approximately 12.9 % of regions in FU3, FU5, FU1 and FU6 exhibiting changes over 3 %. This work enhanced the understanding of spatiotemporal SOC variability induced by farmland utilization using machine learning method based on determined FUs, which also provided valuable guidance for soil monitoring and carbon accounting management for intensively cultivated farmland.
期刊介绍:
Soil & Tillage Research examines the physical, chemical and biological changes in the soil caused by tillage and field traffic. Manuscripts will be considered on aspects of soil science, physics, technology, mechanization and applied engineering for a sustainable balance among productivity, environmental quality and profitability. The following are examples of suitable topics within the scope of the journal of Soil and Tillage Research:
The agricultural and biosystems engineering associated with tillage (including no-tillage, reduced-tillage and direct drilling), irrigation and drainage, crops and crop rotations, fertilization, rehabilitation of mine spoils and processes used to modify soils. Soil change effects on establishment and yield of crops, growth of plants and roots, structure and erosion of soil, cycling of carbon and nutrients, greenhouse gas emissions, leaching, runoff and other processes that affect environmental quality. Characterization or modeling of tillage and field traffic responses, soil, climate, or topographic effects, soil deformation processes, tillage tools, traction devices, energy requirements, economics, surface and subsurface water quality effects, tillage effects on weed, pest and disease control, and their interactions.