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Study on Soil Capacities of Water-retention on Typical Vegetations in the North Side of Liupan Mountains in Ningxia

  • Received Date: 2005-11-22
  • The capacity of water-retention and-supply for plants of the soils on five typical vegetations were analyzed by measuring the soil water characteristic curves and physical properties in the north side of Liupan Mountains,Ningxia.The results showed that the relationship between soil moisture and soil suction could be successfully expressed by the power function proposed by Gardner et al.(1970).The soil density in different layers on five vegetations were ranged from high to low values as follow: abandoned land,Prunus davidiana plantation,Stipa bungcana community,Larix principi-rupprechtii plantation and Hippophae rhamnoides community.However,the order of total soil capillary porosity of the five vegetations was just contrary.From 0.1 to 1.5 MPa in soil suction,soil water content of Larix principi-rupprechtii plantation,Stipa bungcana community,Hippophae rhamnoides community, Prunus davidiana plantation and abandoned land were ranged in 169.7~239.3 g·kg-1,160.3~236.1 g·kg-1,140.9~224.5 g·kg-1,119.9~198.1 g·kg-1and 113.5~176.4 g·kg-1 respectively,it meant that the soil capacity of water-retention of the five vegetations decreased in order.The order of soil capacity of water-supply for the five vegetation types was the same as soil capacity of water-retention,and it decreased with increasing of soil suction.The results could be explained by the positive effect of soil physical properties(i.e.soil density and total capillary porosity et al.) caused by planting trees and grass on the soil capacities of water-retention and-supply.
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    [2] 张小泉, 张清华, 毕树峰, 等. 太行山北部中山幼林地土壤水分的研究[J] -林业科学, 1994, 30 (3) : 193 ~ 200

    [3] 周择福, 李昌哲. 北京九龙山不同植被土壤水分特征的研究[J] . 林业科学研究, 1994, 7(1): 48~ 53

    [4] 吴文强, 李吉跃, 张志明, 等. 北京西山地区人工林土壤水分特性的研究[J] . 北京林业大学学报, 2002, 24(4) : 51~ 55

    [5] 赵世伟, 周印东, 吴金水. 子午岭北部不同植被类型土壤水分特征研究[J] . 水土保持学报, 2002, 16(4) : 119~ 122

    [6] 孙中峰, 张学培, 刘卉芳, 等. 晋西黄土区坡面林地土壤持水性能研究[J] . 干旱区研究, 2004, 21(4) : 343~ 347

    [7] 史竹叶, 赵世伟. 黄土高原土壤持水曲线的计算方法[J] . 西北农业学报, 1999, 8 (6) : 44~ 47

    [8] 姚其华, 邓银霞. 土壤水分特征曲线模型及其预测方法的研究进展[J] -土壤通报, 1992, 23(3) : 142~ 144

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    GardnerW R, H illel D, Benyam in iY. Post irrigat ion m ovem en t ofw ater: ? . R ed istribu tion[J] . W ater R esour R es, 1970, 6: 851~ 861
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Study on Soil Capacities of Water-retention on Typical Vegetations in the North Side of Liupan Mountains in Ningxia

  • 1. The Forestry Administrstion of Yuanzhou District, Guyuan 756000, Ningxia, China
  • 2. Liupanshan Forestry Bureau of Guyuan City in Ningxia Autonomous Region, Jingyuan 756401, Ningxia, China
  • 3. Research Institute of Forest Ecology, Environment and Protection, CAF, Beijing 100091, China

Abstract: The capacity of water-retention and-supply for plants of the soils on five typical vegetations were analyzed by measuring the soil water characteristic curves and physical properties in the north side of Liupan Mountains,Ningxia.The results showed that the relationship between soil moisture and soil suction could be successfully expressed by the power function proposed by Gardner et al.(1970).The soil density in different layers on five vegetations were ranged from high to low values as follow: abandoned land,Prunus davidiana plantation,Stipa bungcana community,Larix principi-rupprechtii plantation and Hippophae rhamnoides community.However,the order of total soil capillary porosity of the five vegetations was just contrary.From 0.1 to 1.5 MPa in soil suction,soil water content of Larix principi-rupprechtii plantation,Stipa bungcana community,Hippophae rhamnoides community, Prunus davidiana plantation and abandoned land were ranged in 169.7~239.3 g·kg-1,160.3~236.1 g·kg-1,140.9~224.5 g·kg-1,119.9~198.1 g·kg-1and 113.5~176.4 g·kg-1 respectively,it meant that the soil capacity of water-retention of the five vegetations decreased in order.The order of soil capacity of water-supply for the five vegetation types was the same as soil capacity of water-retention,and it decreased with increasing of soil suction.The results could be explained by the positive effect of soil physical properties(i.e.soil density and total capillary porosity et al.) caused by planting trees and grass on the soil capacities of water-retention and-supply.

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