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
纸质出版:2012
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潘磊, 唐万鹏, 肖文发, 等. 三峡库区不同退耕还林模式林地水文效应[J]. 水土保持通报, 2012,31(5):103-106.
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.
在三峡库区兰陵溪小流域内选定3种典型退耕还林模式
基于2007-2009年连续3a的观测
对退耕还林林地水文效应进行了定量研究。 结果表明:(1)与坡耕地比较
退耕还林地土壤总孔隙度增加4.2%~11.5%
非毛管孔隙度增加了69.1%~162.6%
平均可增加饱和蓄水量42.5%
非毛管蓄水量221.4%; (2)各退耕还林模式A层土壤的初渗速率和稳渗速率分别在2.73~4.74mm/min和1.30~2.96mm/min
与对照相比A层土壤渗透性能差异不大
B层土壤初渗及稳渗速率分别较对照提高0.85~5.21倍和3.33~6.83倍
在0.14~0.87mm/min和0.06~0.47mm/min间变动; (3)各退耕还林模式年均径流深为13.21~22.38mm
较农耕地减少74.7%~57.3%
各退耕模式土壤侵蚀模数在137.1~331.1t/(km
2
.a)
较对照减少92.4%~81.6%。
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.
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