青海湖湖东克土沙区固定沙丘土壤水分动态变化的初步研究  

A preliminary study on dynamics of soil water content of the fixed dune in Ketu sand land on the east of Qinghai Lake

作　　者：鲁瑞洁[1] 唐清亮[1] 张登山[1] 石昊[1] 赵爱斌[2] 

机构地区：[1]北京师范大学环境演变与自然灾害教育部重点实验室,北京100875 [2]北京师范大学生命科学院,北京100875

出　　处：《地球环境学报》2010年第3期183-188,共6页Journal of Earth Environment

基　　金：国家科技支撑计划(2007BAC30B03);国家自然科学基金项目(40801004)

摘　　要：本文通过土壤水分观测，结合降水记录及地表沉积物粒度分析，对青海湖湖东克土沙区固定沙丘不同地貌部位土壤水分的时空变化规律进行了初步研究。结果表明：0-100cm深度内，丘间地的土壤含水量最高，丘顶与背风坡次之，迎风坡最低。迎风坡丘间地与迎风坡脚受地下水的影响，分别以40cm和100cm为界，土壤含水量在界限以上变化不大，界限以下随着深度增加而迅速增大。其他地貌部位土壤水分来源主要是大气降水，0～20cm土壤含水量都随土壤深度增加而增加，20cm以下则表现出不同的变化规律。By observing soil water content, integrating rainfall monitoring and surface sediments particle size analysis, we preliminarily studied the dynamics of soil water content at different geomorphological locations of the fixed dune in Ketu sand land on the east of Qinghai Lake. The results showed that from 0-100 cm the soil water content of the interdunal areas was the highest, dune top and leeward slop was the second, and windward slop was the lowest. On the vertical profile, under the influence of groundwater, both the dune slack next to the windward slope and the feet of windward slope had critical depth, separately, 40 cm and 100 cm. Above the critical depth, the soil water content changed little, whereas below it the soil water content increased rapidly with depth. While the soil water content of other geomorphological locations, whose major source was precipitation, increased with depth during 0-20 cm. while the changes were comolicated below 20 cm.

关 键 词：土壤水分 固定沙丘 降雨量 时空变化 

分 类 号：S152.7[农业科学—土壤学]