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    洪湖市中北部地区土壤硒元素分布特征

    Distribution characteristics of selenium in the soils of the north central region of Honghu, Hubei Province

    • 摘要: 选取洪湖市中北部地区汊河、黄家口和小港3个区域为研究区,采集1540件表层土壤样,100件深层土壤样,通过系统研究土壤样的硒含量,总结该区土壤硒元素分布特征。在无外界作用影响下,硒在偏酸性土壤中的富集程度优于在碱性土壤中的富集程度,表层土壤硒含量高于深层土壤硒含量。该区富硒土壤主要赋存在中性、中酸性土壤区中,当土壤酸碱度由酸性向碱性转化时,土壤中的硒含量表现为弱酸性≈酸性>中性>碱性>强碱性。土壤三级划分图表明农业、水产养殖用地中一级富硒土地占41.43%,二级富硒土地占32.21%,三级土地占26.36%。

       

      Abstract: This study selected three areas(Chahe, Huangjiakou and Xiaogang)in the north central region of Honghu as a target area, from which 1540 surface soil samples and 100 deep soil samples were collected. Through a systematic study of selenium contents for the soil samples, authors summarized the distribution characteristics of the selenium element in soil. The results show that under the condition that there is no external impact, the concentration of Se in the acidic soil is higher than that in the alkaline soil, i.e. the selenium content in surface soil is higher than that in the deep soil. Selenium-rich soil occurs mainly in neutral and acidic soil. With the soil pH value converting from acidic to alkaline, the selenium content in soil gradually decreases from weak acidity(equal to slightly acidic), neutral, alkaline, and to strong alkaline. The three-level classification diagram of soil shows 41.43% of first-level Se-rich soil used as agricultural and aquaculture land, 32.21% of the secondary selenium-rich land area, and 26.36% of three level Se-rich land.

       

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