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贵州表层土壤有机质空间变异特征及其影响因素分析
引用本文:文鑫,王艺惠,钟聪,胡宝清,张新英. 贵州表层土壤有机质空间变异特征及其影响因素分析[J]. 水土保持学报, 2023, 37(3): 218-224
作者姓名:文鑫  王艺惠  钟聪  胡宝清  张新英
作者单位:1. 南宁师范大学北部湾环境演变与资源利用教育部重点实验室, 广西地表过程与智能模拟重点实验室, 南宁 530001;2. 南宁师范大学地理与海洋研究院, 南宁 530001
基金项目:国家自然科学基金项目(41867049);广西自然科学基金项目(2018GXNSFAA281263,2016GXNSFBA380106);国家重点研发计划项目(2016YFC0502401)
摘    要:为探究贵州表层土壤有机质的空间变异特征及其主要影响因素,使用贵州省第二次土壤普查资料中193个土壤剖面数据,结合贵州省气象资料、土地利用类型图及土壤类型图等资料,运用地统计学和多元回归分析各因素对表层土壤有机质空间变异的解释能力。结果表明:(1)贵州省表层土壤有机质含量范围为0.05%~36.68%,平均含量为5.23%±4.96%,变异系数为94.90%;(2)表层土壤有机质在空间分布上表现出东北部高,西南部较低的格局;(3)半变异函数分析表明,贵州省土壤有机质主要受自然因素影响,海拔、CEC、耕作方式和土壤质地对表层土壤有机质含量变异的综合解释能力为35.9%,海拔作为最重要的影响因素能独立解释其变异的25.6%,CEC和耕作方式分别能解释11.3%,7.4%。贵州表层土壤有机质与年均气温呈负相关关系,与海拔呈正相关关系。研究区表层土壤有机质的分布与碳酸盐岩分布面积比例存在相关关系,整体上,随着喀斯特分布面积比例增大而受自然因素影响增大。喀斯特分布面积比例为0~10%区域主要受农业耕作施肥等人类活动的影响,11%~30%区域主要受海拔影响,31%~50%区域受年均温和CEC影响,5...

关 键 词:地统计学  回归分析  土壤有机质  空间异质性  喀斯特
收稿时间:2022-10-28

Spatial Variation of Surface Soil Organic Matter and Its Influencing Factors in Guizhou Province
WEN Xin,WANG Yihui,ZHONG Cong,HU Baoqing,ZHANG Xinying. Spatial Variation of Surface Soil Organic Matter and Its Influencing Factors in Guizhou Province[J]. Journal of Soil and Water Conservation, 2023, 37(3): 218-224
Authors:WEN Xin  WANG Yihui  ZHONG Cong  HU Baoqing  ZHANG Xinying
Affiliation:1. Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education, Guangxi Key Laboratory of Earth Surface Processes and Intelligent Simulation, Nanning Normal University, Nanning 530001;2. Institute of Geography and Oceanography, Nanning Normal University, Nanning 530001
Abstract:In order to study the spatial variability of soil organic matter and its main influencing factors, 193 soil profiles from the second soil survey in Guizhou province were used, based on the meteorological data, land use type map and soil type map of Guizhou province, geostatistics and multiple regression were used to analyze the explanatory ability of each factor to the spatial variability of topsoil organic matter. The results showed that: (1) The organic matter content of surface soil in Guizhou Province ranged from 0.05% to 36.68%, with an average of 5.23%±4.96% and a coefficient of variation of 94.90%. (2) The spatial distribution of topsoil organic matter was higher in the northeast and lower in the southwest. (3) According to the results of semi-variational function analysis, soil organic matter in Guizhou province was mainly affected by natural factors. The comprehensive explanatory ability of altitude, CEC, tillage and soil texture for the variation of organic matter content was 35.9%, and altitude, as the most important influencing factor, could independently explain 25.6% of the variation. CEC and farming methods could explain 11.3% and 7.4%, respectively. There was a negative correlation between surface soil organic matter and average annual temperature and a positive correlation between surface soil organic matter and altitude. There was a correlation between the distribution of surface soil organic matter and the distribution area proportion of carbonate rocks in the study area. On the whole, the distribution area proportion of karst increased with the influence of natural factors. The areas with 0~10% karst distribution area were mainly affected by human activities such as agricultural cultivation and fertilization, 11%~30% were mainly affected by altitude, 31%~50% were mainly affected by average annual temperature and CEC, and 51%~100% of the areas were more affected by elevation, average annual temperature, precipitation, CEC and pH. The results are helpful to understand quantitatively the spatial distribution of organic matter in Guizhou, and provide scientific basis and reference for soil fertility regulation and ecological management.
Keywords:geostatistics  regression analysis  soil organic matter  spatial heterogeneity  karst
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