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祁连山主要植被下土壤对降雨分配的研究 被引量:3

Study on main vegetation tykes to distribute rainfall in soil on QiLian Mountain
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摘要 以祁连山主要植被类型下的土壤为研究对象,对其物理性质、渗透率、渗流速度及其地表径流进行研究,结果表明:土壤的物理性质决定着土壤对降雨的分配情况,有林地将降雨全部分配成入渗水,而牧坡草地根据降雨强度和持续时间不同将降雨按不同的比例分配成入渗水和地表径流水2部分,不同植被的土壤蓄水量也各不相同。林地土壤100cm土层蓄水量为320.2~509.7mm,比牧坡草地高5.4%~60.47%,灌丛云杉和高山灌丛土壤蓄水量最高;轻度放牧的草地土壤蓄水量比强度放牧的高33.48%。 based on the research on main vegetation type to drstr:lutl rarn in soil on QiLian mountains, its physical property, osmosis rate, infiltrating fluid speed and surface runoff were conducted. The results showed that the physical property of soil decided the distribution of rainfall. The forest land completely distributes the rainfall into infiltrating water, whereas the grassland distributes the rainfall into both infiltrating water and surface water based on the intensity of rainfall and its duration, and the retaining water capacity of different vegetations soil is not same. The retaining water of forest land with the depth of 100cm is 320.2~509.7 mm, over 5.4~60.47 percent than that of grassland; the highest retaining water of soil ware shrub spruces and alpine shrubs; the retaining water of soil of slight graving grassland was higher than that of intensive graving grassland.;
出处 《甘肃林业科技》 2003年第4期1-4,29,共5页 Journal of Gansu Forestry Science and Technology
关键词 祁连山 植被 土壤 降雨 径流 土壤渗透 土壤蓄水量 强度 持续时间 rain soil osmosis runoff soil of main vegetation
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  • 1王金叶,常学向,葛双兰,苗毓新,常宗强,张虎.祁连山(北坡)水热状况与植被垂直分布[J].西北林学院学报,2001,16(z1):1-3. 被引量:71
  • 2林业部科技司.森林生态系统定位研究方法(第1版)[M].北京:中国科学技术出版社,1994.84-166.
  • 3中国科学技术情报研究所重庆分所.土壤物理性测定[M].重庆:中国科学技术出版社重庆分社,1979.150-177.
  • 4车克钧,傅辉恩,贺红元.祁连山水源涵养林综合效能的计量研究[J].林业科学,1992,28(4):290-296. 被引量:25
  • 5贺红元 车克钧 傅辉恩 等.祁连山森林植被对河川径流的影响.北京林业大学学报,1993,15(3):4-9.

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