青海湖西吉尔孟附近土壤水分研究  

Soil Moisture at Jiermeng Village in West Qinghai Lake

作　　者：赵景波[1,2] 侯雨乐[1,3] 曹军骥[2] 张冲[1] 

机构地区：[1]陕西师范大学旅游与环境学院,陕西西安710062 [2]中国科学院地球环境研究所黄土与第四纪地质国家重点实验室,陕西西安710075 [3]阿坝师范高等专科学校,四川成都611741

出　　处：《地理科学》2011年第4期394-400,共7页Scientia Geographica Sinica

基　　金：国家科技支撑计划(2007BAC30B01)项目资助

摘　　要：根据对青海湖北刚察县吉尔孟乡草地土壤含水量测定和粒度分析,研究了土壤水分变化等问题。研究区土层上部粒度成分以粗粉砂为主,下部以细砂为主。2009年该区草地土壤重力水分布深度达到了60 cm左右。土壤上部含水量丰富,下部水分严重不足。在土层约80 cm深度之下出现了中等干层和部分严重干层。该区土壤干层的发育阻隔了大气降水向地下深处的入渗,属于异常水分循环类型。该区土壤水分处于负平衡状态,指示当地的降水量并不能充分满足草原植被生长的需要。吉尔孟乡土壤蓄水量较少,易于发生生态环境的退化。According to the analysis on soil moisture and particle size of the grass land at Jiermeng in Gangcha,the soil moisture content and its impacts on vegetation development were studied.The grain size composition of the middle and upper part of soil in the study area is mainly coarse silt,and at the lower part of soil is mainly fine sand.Soil moisture content in grassland appeared more gravity water in 2009 in this region,and the depth of gravity water in the grass land was up to about 60 cm.Soil moisture is rich in the upper layers and seriously short in the lower.Moderate dried layers with the soil moisture lower than 9% and some serious dried layers with the soil moisture lower than 6% occurred under the soil profiles with the depth of about 80 cm.The development of dried soil layer at this region is due to less precipitation,which held up precipitation infiltrating into the deeper area under ground,so precipitation is generally not the supply source of groundwater.Surface water circulation is mainly through evaporation and transpiration,and belongs to the type of abnormal water cycle.Soil water balance is the negative one in this region,which shows that the local rainfall does not fully meet the needs of growth and development of grass vegetation and is not suitable to forest planting.Soil thickness at Jiermeng Village is thicker than other areas around Qinghai Lake.Because soil water storage is less and soil reservoir can not provide enough water for the growth of herbaceous plants in dry year,the area is prone to environmental degradation.In order to maintain the water level stable and ecological balance of Qinghai Lake,we should develop natural grass vegetation which is suitable to the local climate and consumes less water,and limit the development of artificial vegetation such as the rape consuming more water and simultaneously restrict grazing.

关 键 词：土壤含水量 土壤干层 水分循环 水分平衡 青海湖西部 

分 类 号：P941.75[天文地球—自然地理学]