土壤全碳全氮空间异质性及影响因素分析——以祁连山南坡黑河上游为例
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S152.4;S156.6

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青海省祁连山自然保护区管理局及祁连山国家公园长期科研基地祁连山国家公园(青海片区)湿地保护恢复及其生态服务功能评估监测项目(QHTX-2020-043-02)资助。


Analysis of Spatial Heterogeneity and Influencing Factors of Soil Total Carbon and Nitrogen——Take the Upper Reaches of Heihe River on Southern Slope of Qilian Mountain as an Example
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    摘要:

    为深入了解影响土壤养分的主控因素及影响因素之间的耦合作用,以黑河为研究区,采用野外采样、实验分析、地统计分析对研究区表层(0~20 cm)土壤全碳全氮空间异质性进行研究,并利用地理探测器模型对在单因素、双因素作用下对土壤全碳全氮的影响及适用条件进行探究。结果表明:①研究区土壤全碳、全氮含量均属于正态分布,且根据第二次土壤普查分级标准,均为第一级,属于中等变异;②土壤全碳、全氮含量插值模型均为指数模型,由结构性因素与随机性因素共同作用,总体呈现出东南向西北递减的趋势,且全氮的插值精度(0.71)>全碳的插值精度(0.55);③自变量对全氮的解释力大小前3位为:有机质>容重>归一化植被指数,自变量对全碳的解释力大小前3位为:有机质>容重>电导率,有机质与其他因素的交互作用大都在0.6以上;土壤全氮及全碳含量最大值出现的区域土壤容重<0.6 g/cm3、电导率0.3~0.35 μS/cm、pH 7~8、有机质含量100~150 g/kg、粒度10~100 μm、年均气温–1~1℃、年降水量360~390 mm、地形湿度6~9、坡度15°~25°、植被指数0.95~1、坡向为北方、DEM 2 500~3 500 m (高中山)。因此,为提高土壤质量,应根据其地形、气候、植被等因素进行分类治理。

    Abstract:

    In order to further understand the main factors affecting soil nutrients and the coupling between the influencing factors, this paper takes the Heihe River Basin as the study area and uses field sampling, experimental analysis, and geostatistical analysis to analyze the total carbon (TC) and nitrogen (TN) of the topsoils (0-20 cm). The spatial heterogeneity is studied, and the single factor and dual factor effects and applicable conditions of TC and TN are explored using the geo-detector model. The results show that both TC and TN are belonged to the normal distribution with medium variation, belonged to the first level according to the grading standard of the 2nd national soil survey, in exponential interpolation models, and the interpolation are influenced by both the structural factors and random factors. The contents of TC and TN both show the decreasing trend from southeast to northwest, and the interpolation accuracy of TN is 0.71, higher than that of TC (0.55). The top three independent variables are soil organic matter(SOM) > bulk density(BD) >NDVI(normalized differential vegetation index) for TN explanatory and SOM > BD >EC(electrical conductivity) for TC explanatory, the interaction between SOM and other factors is mostly above 0.6. The areas where the maximum values of TN and TC contents of the soil appear are on the conditions of BD <0.6 g/cm3, EC in 0.3-0.35 µS/cm, pH in 7-8, SOM in 100-150 g/kg, particle size in 10-100 µm, TEM(average temperature) in -1-1℃, PER(annual precipitation) in 360-390 mm, TWI(terrain humidity index) in 6-9, slope in 15°-25°, NDVI in 0.95-1, aspect in north, and DEM in 2 500-3 500 m. It should be classified and managed according to the terrain, climate, vegetation and other factors for the improvement of soil quality.

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童珊,曹广超,张卓,刁二龙,闫欣.土壤全碳全氮空间异质性及影响因素分析——以祁连山南坡黑河上游为例[J].土壤,2022,54(5):1064-1072. TONG Shan, CAO Guangchao, ZHANG Zhuo, DIAO Erlong, YAN Xin. Analysis of Spatial Heterogeneity and Influencing Factors of Soil Total Carbon and Nitrogen——Take the Upper Reaches of Heihe River on Southern Slope of Qilian Mountain as an Example[J]. Soils,2022,54(5):1064-1072

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  • 收稿日期:2021-12-04
  • 最后修改日期:2021-12-18
  • 录用日期:2021-12-21
  • 在线发布日期: 2022-10-31
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