科尔沁沙地双辽地区地表基质化学元素垂向分布特征及含量等级

    Vertical distribution and content levels of chemical elements in the ground substrate in Shuangliao area of Horqin sandy land

    • 摘要: 对吉林省双辽地区SLZK04钻孔50 m以浅的主量元素、矿质元素、有益元素和有害元素的垂向分布特征进行了系统研究.结果表明,主量元素中Al2O3、CaO、MgO、TiO2、P2O5、Fe2O3含量与SiO2含量变化呈负相关,这与土壤质地密切相关.矿质元素分布特征总体表现为氧化风化搬运环境下矿质元素含量较高,在还原的湖相沉积环境下矿质元素含量较少.有益元素分布同样受沉积环境制约,有害元素在钻孔中整体呈现较低水平.对全心土质部分化学元素质量评价结果显示:全心CaO含量为二等较丰富级,MgO含量为四等较缺乏级,Fe2O3、Mn和P含量为五等缺乏级,K含量属于三等中等级,Se、I和F含量属于五等缺乏级,土壤环境质量为一等清洁级.

       

      Abstract: This study systematically investigates the vertical distribution characteristics of major, mineral, beneficial, and harmful elements in the top 50 m of borehole SLZK04 in Shuangliao area, Jilin Province. The results reveal that the contents of Al2O3, CaO, MgO, TiO2, P2O5, and Fe2 O3 exhibit a negative correlation with SiO2 content, which is closely associated with soil texture. The distribution patterns of mineral elements generally show higher concentrations in oxidizing weathering and transport environments, whereas lower concentrations are found in reducing lacustrine sedimentary conditions. The distribution of beneficial elements is also constrained by sedimentary environments, while harmful elements maintain consistently low levels throughout the borehole. Quality assessment of chemical elements in the whole soil profile indicates that the average CaO content falls into Grade Ⅱ(relatively abundant), MgO into Grade Ⅳ(relatively deficient), Fe2O3, Mn, and P into Grade V(deficient), K into Grade Ⅲ(moderate), and Se, I, and F into Grade Ⅴ(deficient). The soil environmental quality is classified as Class Ⅰ(clean).

       

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