Miaoying An, Haoxin Zhang, Yang Xu, Yanmei Dong, Siqi Yang, Shengyue Yu, Qiuliang Lei, Xinzhong Du, Hongbin Liu, Huiping Ou
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SOC stocks increased by 227.73 Tg over four decades, with an average sequestration rate of 220.30 kg C ha<jats:sup>−1</jats:sup> year<jats:sup>−1</jats:sup>, indicating the region's significant carbon sink potential. Spatially, SOC stocks were higher in the south and lower in the north, with south–north SOC density differences of 0.70, 0.57, and 1.04 kg m<jats:sup>−2</jats:sup> in the 1980s, 2010s, and 2020s, respectively. The soil pH, nitrogen input, mean annual temperature, and precipitation were the dominant explanatory variables, contributing 18.46%, 10.67%, 10.37%, and 8.05% to the explained variance in SOC density. Among these, soil pH and annual nitrogen fertilizer input showed highly significant negative correlations (<jats:italic>p</jats:italic> < 0.01), as pH regulates SOC stability through mineral interactions, microbial community composition, and enzyme activity. Nitrogen input of 0.072–0.177 Mg ha<jats:sup>−1</jats:sup> accelerates SOC decomposition and contributes to carbon input via increased root exudates. Furthermore, both the mean annual precipitation and temperature were positively correlated with changes in SOC density, with the strongest association observed with precipitation (<jats:italic>p</jats:italic> < 0.05). Therefore, managing soil pH, optimizing nitrogen use, and adapting to climate change are vital for enhancing the region's soil carbon sink and supporting sustainable agricultural development.","PeriodicalId":203,"journal":{"name":"Land Degradation & Development","volume":"62 1","pages":""},"PeriodicalIF":3.7000,"publicationDate":"2025-09-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Spatiotemporal Variation Characteristics of the Soil Organic Carbon Stock in the Huaihe River Eco‐Economic Belt From the 1980s to 2020s\",\"authors\":\"Miaoying An, Haoxin Zhang, Yang Xu, Yanmei Dong, Siqi Yang, Shengyue Yu, Qiuliang Lei, Xinzhong Du, Hongbin Liu, Huiping Ou\",\"doi\":\"10.1002/ldr.70132\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The Huaihe River Eco‐Economic Belt (HREEB), a vital grain‐producing region in China, contributes 11% of the nation's arable land and one‐sixth of its grain output. As an essential indicator of soil health, soil organic carbon (SOC) underpins long‐term productivity and ecological stability. However, the spatiotemporal dynamics of SOC stocks and the relative roles of climate and land management remain poorly quantified. This study investigated spatiotemporal changes in SOC stock in the HREEB (1980s–2020s), identified main SOC sequestration drivers, and proposed strategies for enhancing carbon stocks in sustainable agriculture. SOC stocks increased by 227.73 Tg over four decades, with an average sequestration rate of 220.30 kg C ha<jats:sup>−1</jats:sup> year<jats:sup>−1</jats:sup>, indicating the region's significant carbon sink potential. Spatially, SOC stocks were higher in the south and lower in the north, with south–north SOC density differences of 0.70, 0.57, and 1.04 kg m<jats:sup>−2</jats:sup> in the 1980s, 2010s, and 2020s, respectively. The soil pH, nitrogen input, mean annual temperature, and precipitation were the dominant explanatory variables, contributing 18.46%, 10.67%, 10.37%, and 8.05% to the explained variance in SOC density. Among these, soil pH and annual nitrogen fertilizer input showed highly significant negative correlations (<jats:italic>p</jats:italic> < 0.01), as pH regulates SOC stability through mineral interactions, microbial community composition, and enzyme activity. Nitrogen input of 0.072–0.177 Mg ha<jats:sup>−1</jats:sup> accelerates SOC decomposition and contributes to carbon input via increased root exudates. Furthermore, both the mean annual precipitation and temperature were positively correlated with changes in SOC density, with the strongest association observed with precipitation (<jats:italic>p</jats:italic> < 0.05). 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引用次数: 0
摘要
淮河生态经济带是中国重要的粮食产区,占全国耕地面积的11%,粮食产量占全国的六分之一。土壤有机碳(SOC)是土壤健康的重要指标,是土壤长期生产力和生态稳定的基础。然而,土壤有机碳储量的时空动态以及气候和土地管理的相关作用仍然缺乏量化。本研究探讨了1980 - 2020年森林碳储量的时空变化,确定了森林碳储量的主要驱动因素,并提出了可持续农业碳储量增加的策略。40年来,碳储量增加了227.73 Tg,平均固存率为220.30 kg C ha−1年−1,表明该地区具有巨大的碳汇潜力。土壤有机碳储量在空间上呈南高北低的趋势,1980年代、2010年代和2020年代南北碳密度差异分别为0.70、0.57和1.04 kg m−2。土壤pH、氮输入、年平均温度和降水是主要的解释变量,对土壤有机碳密度的贡献率分别为18.46%、10.67%、10.37%和8.05%。其中,土壤pH与年氮肥投入量呈极显著负相关(p < 0.01), pH通过矿物相互作用、微生物群落组成和酶活性调节有机碳稳定性。0.072 ~ 0.177 Mg ha−1的氮输入加速了土壤有机碳的分解,并通过增加根系分泌物促进了碳输入。此外,年平均降水量和气温与土壤有机碳密度变化均呈正相关,其中与降水量的相关性最强(p < 0.05)。因此,管理土壤pH值、优化氮素利用和适应气候变化对于增强该地区土壤碳汇和支持农业可持续发展至关重要。
Spatiotemporal Variation Characteristics of the Soil Organic Carbon Stock in the Huaihe River Eco‐Economic Belt From the 1980s to 2020s
The Huaihe River Eco‐Economic Belt (HREEB), a vital grain‐producing region in China, contributes 11% of the nation's arable land and one‐sixth of its grain output. As an essential indicator of soil health, soil organic carbon (SOC) underpins long‐term productivity and ecological stability. However, the spatiotemporal dynamics of SOC stocks and the relative roles of climate and land management remain poorly quantified. This study investigated spatiotemporal changes in SOC stock in the HREEB (1980s–2020s), identified main SOC sequestration drivers, and proposed strategies for enhancing carbon stocks in sustainable agriculture. SOC stocks increased by 227.73 Tg over four decades, with an average sequestration rate of 220.30 kg C ha−1 year−1, indicating the region's significant carbon sink potential. Spatially, SOC stocks were higher in the south and lower in the north, with south–north SOC density differences of 0.70, 0.57, and 1.04 kg m−2 in the 1980s, 2010s, and 2020s, respectively. The soil pH, nitrogen input, mean annual temperature, and precipitation were the dominant explanatory variables, contributing 18.46%, 10.67%, 10.37%, and 8.05% to the explained variance in SOC density. Among these, soil pH and annual nitrogen fertilizer input showed highly significant negative correlations (p < 0.01), as pH regulates SOC stability through mineral interactions, microbial community composition, and enzyme activity. Nitrogen input of 0.072–0.177 Mg ha−1 accelerates SOC decomposition and contributes to carbon input via increased root exudates. Furthermore, both the mean annual precipitation and temperature were positively correlated with changes in SOC density, with the strongest association observed with precipitation (p < 0.05). Therefore, managing soil pH, optimizing nitrogen use, and adapting to climate change are vital for enhancing the region's soil carbon sink and supporting sustainable agricultural development.
期刊介绍:
Land Degradation & Development is an international journal which seeks to promote rational study of the recognition, monitoring, control and rehabilitation of degradation in terrestrial environments. The journal focuses on:
- what land degradation is;
- what causes land degradation;
- the impacts of land degradation
- the scale of land degradation;
- the history, current status or future trends of land degradation;
- avoidance, mitigation and control of land degradation;
- remedial actions to rehabilitate or restore degraded land;
- sustainable land management.