Influence of Mining Subsidence on Physical and Chemical Properties of Soil in Windy Desert Area
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Influence of Mining Subsidence on Physical and Chemical Properties of Soil in Windy Desert Area
Vol. 20, Issue 5, Pages: 52-55(2006)
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CLC:X752S153
Published:2006
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WANG Jian, GAO Yong, WEI Jiang-sheng, et al. Influence of Mining Subsidence on Physical and Chemical Properties of Soil in Windy Desert Area[J]. 2006, 20(5): 52-55.
DOI:
WANG Jian, GAO Yong, WEI Jiang-sheng, et al. Influence of Mining Subsidence on Physical and Chemical Properties of Soil in Windy Desert Area[J]. 2006, 20(5): 52-55.DOI:
Influence of Mining Subsidence on Physical and Chemical Properties of Soil in Windy Desert Area
In order to reveal the influence of mining subsidence on physical and chemical properties of soil
provide scientific theories for land reclamation of windy desert area in Arid and Semi-arid Regions
here measures and figures out the soil mechanical composition
bulk density
soil porosity
field water-holding capacity
saturated conductivity and nutrient of subsidence area and no-subsidence area in Bulanta mining area that lies in southeast Mu Us Sandland using basic principles and methods of Soil Science.The result of anova shows: the physical clay content of sinking dune
especially in the 10 cm of surface
significantly decreases;bulk density and soil porosity of top and middle in sinking dune is not significantly different
however
bulk density of bottom and depression in sinking dune significantly decreases
soil porosity of bottom and depression in sinking dune significantly increases;bulk density and soil porosity from 0 to 40 cm is not significantly different
but bulk density from 40 to 100 cm significantly decreases
soil porosity from 40 to 100 cm significantly increases;field water-holding capacity from 0 to 60 cm significantly decreases;saturated conductivity from 0 to 60 cm is not significantly different;total nitrogen
total potassium and total phosphorus from 0 to 100 cm is not significantly different.