关中平原土壤剖面微量元素空间分布特征及其影响因素
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S153.6

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自然资源要素耦合过程与效应重点实验室开放基金项目(2022KFKTC019)和陕西林业科技创新青年人才培育专项(SXLK2023-06-7)资助。


Spatial Distribution Characteristics and Its Influencing Factors of Trace Elements in Soil Profiles of Guanzhong Plain
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Open Fund of Key Laboratory of Coupling Process and Effect of Natural Resource Elements

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    摘要:

    以关中平原为研究对象,通过野外采集0~10、10~20、20~40、40~60和60~100 cm 5个土层深度的土壤样本并进行室内分析,研究了该区域6种土壤微量元素(Fe、Mn、Zn、Cu、Ba和Co)的空间分布特征及其影响因素。研究发现:①研究区0~100 cm土层中不同元素的含量均值由大到小均为Fe>Mn>Ba>Zn>Cu>Co;与陕西省土壤背景值相比,不同土层Fe、Mn和Co含量均值均高于背景值,Zn和Cu含量均值在背景值附近波动,Ba含量均值则均低于背景值;随着土层深度的增加,Fe、Ba和Co含量呈现增加的趋势,Zn和Cu含量呈现减少的趋势,而Mn含量则是先升高后降低。②整体上,不同土层中大部分微量元素的最优插值模型均为指数模型,且不同土层中6种微量元素表现出不同程度的空间相关性和变程差异,具有深度依赖性。③关中平原土壤微量元素含量分布呈现西高东低的趋势。④0~10、10~20和60~100 cm土层土壤微量元素空间分布的主要影响因素为土壤含水量和砂粒含量,20~40 cm土层为含水量、pH和砂粒含量,40~60 cm土层为砂粒含量。

    Abstract:

    In this paper, the Guanzhong Plain was taken as the research object, soil samples were collected from five depths of 0-10, 10-20, 20-40, 40-60, and 60-100 cm in the fields, and the contents of six trace elements (Fe, Mn, Zn, Cu, Ba, and Co) were determined, and their spatial distribution characteristics and influencing factors were explored. The results showed that: 1) The mean values of trace elements in the 0-100 cm depth in the Guanzhong Plain, from highest to lowest, was as follows: Fe>Mn>Ba>Zn>Cu>Co. Compared with soil background values in Shaanxi Province, the mean values of Fe, Mn and Co were higher in different soil layers, the mean value of Ba was lower, while the mean values of Zn and Cu were varied and irregular. As the depth increased, the contents of Fe, Ba, and Co increased, the contents of Zn and Cu decreased, while the content of Mn first increased and then decreased. 2) The optimal interpolation model was an exponential model for most elements in different soil layers, and the six elements in different soil layers exhibited varying degrees of spatial correlation and range differences, with depth dependence. 3) The contents of soil trace elements were higher in the west and lower in the east in the study area. 4) The main influencing factors were moisture and sand particles in the 0-10, 10-20, and 60-100 cm soil layers, moisture, pH and sand particles in the 20-40 cm soil layer, and sand particles in the 40-60 cm soil layer.

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袁遥遥,马雅莉,张锡唐,张晨晨,朱绪超,刘喜东,乔江波.关中平原土壤剖面微量元素空间分布特征及其影响因素[J].土壤,2025,57(5):1185-1195. YUAN Yaoyao, MA Yali, ZHANG Xitang, ZHANG Chenchen, ZHU Xuchao, LIU Xidong, QIAO Jiangbo. Spatial Distribution Characteristics and Its Influencing Factors of Trace Elements in Soil Profiles of Guanzhong Plain[J]. Soils,2025,57(5):1185-1195

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  • 收稿日期:2024-09-06
  • 最后修改日期:2024-12-19
  • 录用日期:2024-12-22
  • 在线发布日期: 2025-11-24
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