陕西省韩城市土壤硒含量分布特征与影响因素分析

Distribution Characteristics and Influencing Factors of Soil Selenium Content in Hancheng, Shaanxi Province

  • 摘要:
    目的 探究陕西省韩城市土壤硒含量空间分布特征及其影响因素,为合理开发利用土壤硒资源、保障区域生态环境安全和居民健康提供科学依据。
    方法 通过检测陕西省韩城市不同深度土壤硒元素含量,利用统计学方法分析不同土壤类型、不同土地利用类型、不同地形坡度及不同地貌类型土壤硒含量水平及空间分布与影响因素。
    结果 韩城市表层土壤硒含量相对中层、深层土壤更加丰富,硒元素分布具有明显的表聚现象;土壤硒含量平均水平属于适量状态,是全国平均水平的0.87倍,陕西省的2.17倍,韩城市局部地区属于高硒地区。不同土壤类型中,冲积土与中性粗骨土各土层的硒含量均处于最高水平,其中,褐土的硒含量在表层土壤中最低,而钙质石质土的硒含量在中层、深层土壤中最低。不同土地利用类型中,硒含量呈现出明显的分布特征。在表层土壤,草地的硒含量最高,水浇地最低;中、深层土壤中草地硒含量降至最低,其他土地利用类型间硒含量差异并不显著。值得注意的是,草地土壤的硒含量随土层深度增加急剧下降,表层土壤硒含量是中层的3.5倍,是深层的5.8倍。不同地形坡度中,土壤硒含量没有显著变化。不同地貌类型中,表层土壤河谷阶地及黄土台塬土壤硒含量最高,中、深层土壤,硒含量差异越来越小。
    结论 韩城市土壤硒含量分布特征在不同土壤类型、不同土地利用类型、不同地貌类型中差异明显,具有一定的规律性;在不同地形坡度中,差异很小。可见土壤硒含量分布是土壤类型、土地利用类型、地形地貌等多种因素共同作用的结果。

     

    Abstract:
    Objective The aims were to explore the spatial distribution characteristics and influencing factors of soil selenium (Se) content in Hancheng, Shaanxi Province, in order to provide theoretical basis and practical guidance for rational development and utilization of soil Se resources, protection of regional ecological environment safety and residents' health.
    Methods The Se contents in soils at different depths in Hancheng, Shaanxi Province, was detected, and the spatial distribution and influencing factors of Se contents in different soil types, land use types, terrain gradients and landforms were analyzed by statistical methods.
    Results The Se contents in the surface soils of Hancheng were more enriched than that in the middle soil and deep soil, with obvious surface accumulation. The average level of Se content in soil was a moderate state, which was 0.87 times of the national average level and 2.17 times of Shaanxi Province. Some areas of Hancheng belonged to high Se area. Among different soil types, alluvial soil and neutral coarse bone soil had the highest Se content in each soil layer, and the Se content in drab soil was the lowest in the surface soil, while the Se content of calcareous stony soil was the lowest in the middle and deep soil. In different land use types, Se content showed obvious distribution characteristics. In the surface soil, the Se content of grassland was the highest, and that of irrigated land was the lowest. The Se content of grassland in middle and deep soil was the lowest, and the difference of Se content among other land use types was not significant. It was worth noting that the Se content of grassland soil decreased sharply with the increase of soil depth. The Se content of surface layer was 3.5 times that of middle layer and 5.8 times that of deep layer. There was no significant change in soil Se content in different terrain slope. Among the different landform types, the Se contents in the surface soil valley terrace and loess tableland were the highest, and the difference between the middle soil and the deep soil was less and less.
    Conclusion The distribution characteristics of soil Se content in Hancheng were different in soil types, land use types and different geomorphic types. In the different terrain slopes, the difference was very small. Soil Se content was the result of the combined effect of soil type, land use type, topography and other factors.

     

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