云南省林业科学院,云南,昆明,650204
纸质出版:2001
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孟广涛, 郎南军, 方向京, 等. 滇中高原山地防护林体系水土保持效益研究[J]. 水土保持通报, 2001,20(1):66-69.
MENG Guang tao, LANG Nan jun, FANG Xiang jing, et al. Soil and Water Conservative Effect of Protection Forest System in Plateau and Mountainous Region of Central Guizhou Province[J]. Bulletin of Soiland Water Conservation, 2001, 20(1): 66-69.
孟广涛, 郎南军, 方向京, 等. 滇中高原山地防护林体系水土保持效益研究[J]. 水土保持通报, 2001,20(1):66-69. DOI:
MENG Guang tao, LANG Nan jun, FANG Xiang jing, et al. Soil and Water Conservative Effect of Protection Forest System in Plateau and Mountainous Region of Central Guizhou Province[J]. Bulletin of Soiland Water Conservation, 2001, 20(1): 66-69. DOI:
以小流域为单元
根据山地防护林体系配置的特点
采取定位和半定位研究方法
分层次对山地防护林体系蓄水保土功能进行监测分析。研究结果表明 :不同地类及用地方式
不同森林类型保持水土效益差异较大
在滇中高原
裸地和坡耕地是流域产沙的主要来源
农耕地侵蚀量是林地的 18.7~ 36 .0倍
裸地侵蚀量远大于坡耕地
高达林地的 10 0倍左右;营建防护林体系后
防护效益显著
土壤侵蚀模数随森林覆盖率的增加而减少
流域森林覆盖率由 18.6 %上升到 42 .4%时
土壤侵蚀模数减少 36 %;坡地造林后
地表径流减少 79.44 %~ 96 .9%
泥沙削减 87.8%~ 99.9%;要使山地小流域水土流失得以控制
森林覆盖率必须达到 30 %以上.
Taking small watershed as a unit
acxeording to the allocating feature of mountainous protection forest system
and adopting locating and semi-locating research technique
the function of water accumulation and soil conservation of mountainous protection forest system was monitor
d and analyzed in hierarchical way. The research results are as follows. The difference of soil and water conserative effectis relatively large in different land types
different land use methods and different forest types. The main source of sand producing is the bare area of central Guizhou plateau and cultivated slopeland in drainage area
The erosion quantity of cropland is 18.7-36.0 times than that of forest land; The erosion quantity of bare land is far larger than that of cultivated slopeland
and is as high as about 100 times than that of forest land. After the protection forest system was established
the protection effect was obvious
the mlulus of soil erosion reduced following the increase of forest cover rate The modulus of soil erosion decreased 36% when the forest cover rate of drainage area increased from 18.6% to 42.4%.After the construction of plantation in sloping field
the surfac
mnoff decreased from 79.4% to 96.9%,and the silt amount d
creas
d from 87.8% to 99.9%;In order to control soil and w ester loss of small westershed in mountainous region
forest cover rate must be more than 30%.
孟广涛,等.金沙江山地系统典型小流域水文效应监测方法[J].云南林业科技,1994(3):31-35.
郭立群,等.滇中高原区卞要森林类型及其演变趋势[J].云南林业科技,1999(1):1-4.
张增哲.流域水文学[M].北京:中国林业出版社,1992.123-157.
雷孝章,等.长江上游防护林体系保土效益研究[J].林业科学1995, 31(1):35-43.
林业部科技司编.森林生态系统定位研究方法[M].北京:中国科学技术出版社1994.143-173.
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