苏北脑湖盆地典型植物根系水分吸收特征

Li Ying, H. Guangcai, Yin Li-he, Wang Cunliang, Yang Feng, Zhang Jing, Huang Jin-ting, Dong Jiaqiu, L. Hua
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摘要

苏北瑙湖盆地地处干旱半干旱区,生态环境脆弱,植被高度依赖地下水。通过对植物覆盖区和空旷区渗透带含水量的测量,分析了典型植被根系吸水量的时空分布。得到以下结论:(1)在地下水深度较浅的地区,根系可以抬升地下水;(2)渗透带含水率在10cm ~ 110cm之间保持最大值,约为13.4%;植物根系从渗透带或地下水中获得足够的水分,以保证其生长过程中所需的水分。(3)对比有盖区与无盖区水势,地表总水势排序为:有盖区>;柳>;沙柳。综上所述,植被覆盖度不仅影响地表总含水量,而且影响渗透带水分的再分布。
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Root water uptake of typical plants in the Subeinao Lake Basin
The Subeinao Lake Basin, where the ecological environment is fragile and the vegetation depends tightly on groundwater, is located in the arid and semi-arid area. Based on the water content of the vadose zone measured in the plant-covered and clear area, we analyzed the distribution of root water uptake of typical vegetation in space and time. The following conclusions are obtained: (1) roots can ascend groundwater in the area where the depth to groundwater is shallow; (2) water contents in the vadose zone keeps a maximum around 13.4% between 10cm-110cm; The plant roots obtain enough moisture from the vadose zone or groundwater in order to guarantee required moisture during its growing. (3) Compared the water potential in covered and clear area, it can be concluded that the surface total head potential ranks as follows: the covered area>;Salix>;Salix psammophila. In conclusion, the vegetation coverage has effect on not only the total water content of surface, but also influence redistribution of water content in the vadose zone.
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