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YOU Qiu-ming, JIAO Si-ming, GAO Jun, LIU Kai, WANG Bo, CAI Fan-long. A Study of Changes of Soil Chemical Properties of Sandy Land in Rangtang County in Northwest Sichuan[J]. Journal of Sichuan Forestry Science and Technology, 2017, 34(6): 59-63,106. doi: 10.16779/j.cnki.1003-5508.2017.06.015
Citation: YOU Qiu-ming, JIAO Si-ming, GAO Jun, LIU Kai, WANG Bo, CAI Fan-long. A Study of Changes of Soil Chemical Properties of Sandy Land in Rangtang County in Northwest Sichuan[J]. Journal of Sichuan Forestry Science and Technology, 2017, 34(6): 59-63,106. doi: 10.16779/j.cnki.1003-5508.2017.06.015

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


doi: 10.16779/j.cnki.1003-5508.2017.06.015
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  • Received Date: 2017-07-13
  • 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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A Study of Changes of Soil Chemical Properties of Sandy Land in Rangtang County in Northwest Sichuan

doi: 10.16779/j.cnki.1003-5508.2017.06.015
  • Sichuan Forestry Survey and Planning Institute, Chengdu 624000, China

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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