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首页> 外文期刊>Advance journal of food science and technology >Contents, Species of Soil Selenium in Kashin-beck Disease-endemic Area, Ruoergai Wetland, Sichuan, China
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Contents, Species of Soil Selenium in Kashin-beck Disease-endemic Area, Ruoergai Wetland, Sichuan, China

机译:四川省若尔盖湿地Kashin-beck病流行区土壤硒的含量,种类

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This study studied that the amounts, species of Se in four kinds of soil (sandy soil, meadow soil, bog soil and peat soil) by a method of successive extraction in order to accumulate scientific data for preventing and curing the selenium response symptom of people and livestock in Ruoergai wetland. The results showed that the content range of Total Se (T-Se) in surface soil layer was 65-260 μg/kg in ten sampling sites and the low Se circumstance existed because of soil Se deficiency. Among several kinds of Se forms, Water soluble Se (W-Se), Exchangeable Se (E-Se) and Organic Se (O-Se) accounted for 1.12-3.08%, 2.91-6.03% and 10.28-45.6% of total Se respectively, unavailable Se including Acid soluble Se (A-Se), Sulfidic Se (S-Se) and Residual Se (R-Se) accounted for more than 60% of total Se. Of the soil O-Se, 57.84% (on average) was associated with the Humic Acid fraction (HA-Se) and 42.16% with the Fulvic Acid fraction (FA-Se), the range of C/Se in soil organic matter was 0.65×106-7.28×106 (on average 2.96×106) in surface soil layer. The soil organic matter was the most important factor affecting the content of soil T-Se and O-Se, the rich soil organic matter was helpful to the accumulation of soil T-Se and O-Se. It was clear that the lower utilization ratio of Se due to the low content of soil T-Se, the higher portion of O-Se and HA-Se were the possible reason for a deficiency of selenium in Kashin-Beck Disease-endemic area, Ruoergai wetland, Sichuan, China.
机译:本研究通过连续提取的方法研究了四种土壤(沙质土壤,草甸土壤,沼泽土壤和泥炭土壤)中硒的含量,种类,以积累预防和治疗人的硒反应症状的科学数据。和若尔盖湿地的牲畜。结果表明,十个采样点表层土壤总硒(T-Se)的含量范围为65-260μg/ kg,由于土壤硒缺乏而存在低硒环境。在几种硒形式中,水溶性硒(W-Se),可交换硒(E-Se)和有机硒(O-Se)分别占总硒的1.12-3.08%,2.91-6.03%和10.28-45.6%。包括酸溶性硒(A-Se),硫化硒(S-Se)和残留硒(R-Se)在内的不可用硒占硒总量的60%以上。在土壤O-Se中,腐殖酸组分(HA-Se)的平均含量为57.84%,而在黄腐酸组分(FA-Se)中的含量为42.16%,土壤有机质中C / Se的范围为表层土层0.65×106-7.28×106(平均2.96×106)土壤有机质是影响土壤T-Se和O-Se含量的最重要因素,丰富的土壤有机质有助于土壤T-Se和O-Se的积累。显然,由于土壤中T-Se含量低,Se利用率低,O-Se和HA-Se含量较高,可能是造成Kashin-Beck病流行地区硒缺乏的原因,若尔盖湿地,四川,中国。

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