Woodland Hydrological Effects of Converting Cropland to Forest in the Three Gorges Reservoir Region
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Woodland Hydrological Effects of Converting Cropland to Forest in the Three Gorges Reservoir Region
Bulletin of Soiland Water ConservationVol. 31, Issue 5, Pages: 103-106(2012)
作者机构:
1. 湖北省林业科学研究院,湖北,武汉,430079
2. 中国林业科学研究院,北京,100091
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Published:2012
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PAN Lei, TANG Wan-peng, XIAO Wen-fa, et al. Woodland Hydrological Effects of Converting Cropland to Forest in the Three Gorges Reservoir Region[J]. Bulletin of Soiland Water Conservation, 2012, 31(5): 103-106.
DOI:
PAN Lei, TANG Wan-peng, XIAO Wen-fa, et al. Woodland Hydrological Effects of Converting Cropland to Forest in the Three Gorges Reservoir Region[J]. Bulletin of Soiland Water Conservation, 2012, 31(5): 103-106.DOI:
Woodland Hydrological Effects of Converting Cropland to Forest in the Three Gorges Reservoir Region
Based on 3 year(2007-2009) continuous observations
characteristics of woodland hydrological effects from the three typical models of converting cropland to forest were studied in Lanningxi small water- shed of the Three Gorges Reservoir region.Results are as follows:(1) Compared with sloping farmland
t he total soil porosity and non-capillary porosity increased from 4.2% to 11.5% and 69.1% to 162.6%
respec- tively. The maximum soil water capacity and non-capillary water capacity increased by 42.5% and 221.4%
respectively
after converting cropland to forest. (2)Initial infiltration rate and stable infiltration rate in A layer for each of the three models were between 2.73and 4.74mm / min and 1.30and 2.96mm /m in
respec-tively
which had no great differences from those on sloping farmland; and in B layer
between 0.14~0.87 mm/ min and 0.06~0.47mm/min
respectively
which were 0.85~5.21and 3.33~6.83times of those on sloping farmland. (3)The surface runoff depths for the three models were between 13.21 and 22.38mm
which were reduced by 74.7%~57.3% as compared with those on cropland.The average annual soil erosion modulus for the three models were between 137.1and 331.1t/km2
which were reduced by 92.4%~81.6% in contrast to CK.
Hydrological Effects of Soil and Water Conservation Forest in Red-soil Erosion Region
Assessment of Sediment Delivery Ratio in Daning River Watershed Based on AnnAGNPS Model
Soil Water Storage and Infiltration Characteristics of Different Forest Soils in Laotudingzi Natural Reserve
Sylvicultural Cost of Super Absorbent Polymers in the Converting Cropland to Forest Program
Community Characteristics and Litter Hydrological Effects of Quercus Liaotungensis,Pinus Tabulaeformis,and Pinus Tabulaeformis f.Shekannesis Forests in Ziwuling Region