Soil Physical Properties and Water Conservation Function of Natural Quercus Mongolica Forest in Mountainous Area of Northern Hebei Province
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Soil Physical Properties and Water Conservation Function of Natural Quercus Mongolica Forest in Mountainous Area of Northern Hebei Province
Bulletin of Soiland Water ConservationVol. 32, Issue 2, Pages: 83-86(2013)
作者机构:
1. 河北农业大学林学院河北省林木种质资源与森林保护重点实验室,河北,保定,071000
2. 河北省木兰围场国有林场管理局, 河北围场,068450
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Published:2013
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Soil Physical Properties and Water Conservation Function of Natural Quercus Mongolica Forest in Mountainous Area of Northern Hebei Province[J]. Bulletin of Soiland Water Conservation, 2013, 32(2): 83-86.
DOI:
Soil Physical Properties and Water Conservation Function of Natural Quercus Mongolica Forest in Mountainous Area of Northern Hebei Province[J]. Bulletin of Soiland Water Conservation, 2013, 32(2): 83-86.DOI:
Soil Physical Properties and Water Conservation Function of Natural Quercus Mongolica Forest in Mountainous Area of Northern Hebei Province
Soil physical properties and water conservation of Natural Quercus mongolicaforest were studied atdifferent slope positions in the mountainous area of Northern Hebei Province.The results showed that soilbulk density
soil non-capillary porosity
and effective water storage at the upper 40cm soil layer varied atdifferent slope positions
in a descending order as middle slope>lower slope>upslope.Soil bulk density varied between 1.0g/cm3 and 1.1g/cm3.The means of soil non-capillary porosity and effective water storageamount were 8.9%and 347.6t/hm2
respectively.Soil capillary porosity
total porosity
soil capillary waterstorage and maximum water storage at different slopes had average values of 38.5%
47.5 %
1 521.5t/hm2
and 1 869.1t/hm2
respectively
with the highest values at lower slope and the lowest at upslope.The litter thickness
total litter and maximum water storage had averages of 48.7cm
23.6t/hm2
and 49.3t/hm2
respectively
and can be ranked in terms of slope positions as:lower slope>upslope>middle slope.Maximum water holding capacity varied from 219.34%to 231.8%
exhibited highest values at upslope
followed by middle slope
and then lower slope.Water storage of the forest at different positions can be arranged in a descending order as:lower slope(1 996.0t/hm2)>middle slope(1 930.0t/hm2)>upslope(1 829.3t/hm2).The average value of water storage was 1 918.4t/hm2.The results indicated that waterstorage capacity of natural Quercus mongolicaforest was significantly affected by slope position.