川西北草原土壤及冷暖季牧草微量元素含量比较
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Q948,Q581

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Research on caparison of the content of trace element in soil and forage in
Northwest Sichuan Grassland
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    摘要:

    改善土壤的理化环境及提高牧草的营养水平必须了解草地土壤及牧草微量元素的分布与含量。试验从川西北草地的亚高山丘原草甸、亚高山平坝草甸和沼泽平坝草甸采集土样和冷暖季草样。 土样采集深度范围是0~10cm, 10~20cm, 20~30cm。应用火焰原子吸收光谱法测定了草样中铜、铁、锰、锌和钴的含量和土样中这些元素的有效态含量,应用氟离子选择电极法测定了土样中的氟离子浓度和草样中的氟含量。土壤pH高低顺序为草甸土>冲积土>泥炭草甸土,pH随土壤深度变深而下降;土壤和牧草的钴含量都处于缺乏状态, 分别为0.64 mg/kg和0.26 mg/kg。牧草铁和锰含量都高于正常水平, 铁为414.51~565.06 mg/kg,锰为138.68~247.09 mg/kg.

    Abstract:

    Fully understanding of the distribution and contents of trace elements in soil and forage is important in order to improve the physical and chemic environment of soil and enhance the nutritional value of forage. Forage in warm and cold season and soil samples were collected from subalpine hill meadow, subalpine flat meadow and subalpine swampy meadow in northwest Sichuan grassland, with the depth of soil in the ranges of 0-10cm, 10-20cm and 20-30cm.Contents of Cu, Fe, Mn, Zn and Co in forages and valid contents of these trace elements in soils were determined with flame atomic absorption spectrometry. Concentrations of F- in soils and F in forages were tested with fluoride-ion selective electrode method. The pH of soils displayed an order as hill meadow Soil > alluvium > turfy meadow Soil. Moreover, soil pH decreased with the increasing depth of soil. Deficiency of Co in soil and forage was observed, 0.64 mg/kg in soil and 0.26 mg/kg in forage respectively. The forage contained higher normal level of Fe and Mn, namely, 414.51-565.06 mg/kg of Fe, and 138.68-247.09 mg/kg of Mn.

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文勇立,李辉,李学伟,杨雪,王洪志,朱刚.川西北草原土壤及冷暖季牧草微量元素含量比较.生态学报,2007,27(7):2837~2846

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