Li Cheng, Wang Rang-Hui, Li Zhao-Zhe, Xu Yang
College of Horticulture and Plant Protection, Yangzhou University, Yangzhou 225009, China.
Jiangsu Provincial Key Laboratory of Agricultural Meteorology, Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, China.
Huan Jing Ke Xue. 2021 May 8;42(5):2432-2439. doi: 10.13227/j.hjkx.202010029.
Cropland soil organic carbon density (SOCD) is an important indicator for measuring soil fertility and soil quality. To understand the spatial differentiation characteristics of cropland SOCD and its influencing factors across China, a dataset on the cropland SOCD of 19 typical stations during 2005-2015 was collected from the China Ecosystem Research Network. The geodetector method was used to analyze the influencing factors affecting the spatial patterns of cropland SOCD. The results indicated that the mean cropland SOCD ranged from 0.83 kg·m to 4.97 kg·m in different stations across China, and was higher in humid monsoon regions than in arid and semi-arid regions. Under different land use patterns, the SOCD of paddy fields was higher than that of other croplands and showed a tendency of significant increase from 2005 to 2015, reaching 0.13 kg·(m·a). The soil physical and chemical properties and precipitation were important influencing factors that affected the spatial patterns of cropland SOCD. In particular, the soil alkaline nitrogen content had the greatest impact on the cropland SOCD patterns. Furthermore, the interaction forces between the soil alkaline nitrogen content and latitude, soil type, precipitation, and soil pH were clearly strengthened. The findings can provide an important scientific basis for reducing cropland greenhouse gas emissions and increasing soil carbon sequestration across China.
农田土壤有机碳密度(SOCD)是衡量土壤肥力和土壤质量的重要指标。为了解中国农田SOCD的空间分异特征及其影响因素,从中国生态系统研究网络收集了2005 - 2015年期间19个典型站点的农田SOCD数据集。采用地理探测器方法分析影响农田SOCD空间格局的影响因素。结果表明,中国不同站点的农田SOCD平均值在0.83 kg·m至4.97 kg·m之间,湿润季风区高于干旱和半干旱地区。在不同土地利用模式下,水田的SOCD高于其他农田,且2005年至2015年呈显著增加趋势,达到0.13 kg·(m·a)。土壤理化性质和降水量是影响农田SOCD空间格局的重要因素。特别是,土壤碱氮含量对农田SOCD格局影响最大。此外,土壤碱氮含量与纬度、土壤类型、降水量和土壤pH值之间的相互作用力明显增强。这些研究结果可为中国减少农田温室气体排放和增加土壤碳固存提供重要的科学依据。