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川西北壤塘县沙化土地土壤化学性质变化研究

A Study of Changes of Soil Chemical Properties of Sandy Land in Rangtang County in Northwest Sichuan

  • 摘要: 采用空间序列代替时间序列的方法,研究了壤塘县对照地、露沙地、沙化耕地、固定沙地的土壤化学性质变化。结果发现:1)0~20 cm和20 cm~40 cm土层中,pH值均随沙化程度的加重逐步升高,而有机质、全N、水解N、全P含量则逐步降低;2)不同土层之间同种类型沙化土壤pH值差异不明显;除对照土壤水解N外,有机质、全N、水解N、全P含量均表现为0~20 cm土层等于(近似等于)或大于20 cm~40 cm土层的特点。3)各种沙化类型中,土壤上层和下层全K含量变化不大,速效K和有效P含量均表现出对照 > 沙化耕地 > 露沙地、固定沙地的特点。

     

    Abstract: The chemical properties changes of soil were studied listed as follows:control land, exposed sandy soil, sandy farmland and fixed sandy land in Rangtang County, by the way of spatial sequence instead of the time series. The results showed that:1) Under 0 cm~20 cm and 20 cm~40 cm soil layer, the pH value increased with the increasing of desertification degree; organic matter, total N, the hydrolysis of N,and total P content gradually reduced; 2) Among the same sandy land type of different soil layer, the pH values were not significantly different.Except hydrolysis N of the control soil, organic matter, total N and hydrolysis N, total P content in 0 cm~20 cm soil layer were equal to (approximately equal to) or greater than that in 20 cm~40 cm soil. 3) In different types of sandy soil, no significant change of total K content in the upper and lower soli were found, available K and P content showed as:control land > sandy farmland > expose sandy soil and fixed sandy land.

     

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