生物结皮影响下土壤水分效应的研究进展  

A Review on Effects of Biological Soil Crusts on Soil Water Cycle

作　　者：郭建芳[1] 徐杰[1] 闫彩霞 

机构地区：[1]内蒙古师范大学生命科学与技术学院,内蒙古呼和浩特010022 [2]呼和浩特市赛罕区民族小学,内蒙古呼和浩特010070

出　　处：《内蒙古师范大学学报（自然科学汉文版）》2012年第1期99-104,共6页Journal of Inner Mongolia Normal University(Natural Science Edition)

基　　金：国家自然科学基金资助项目(30860063;30660027);内蒙古自然科学基金资助项目(200607010512)

摘　　要：干旱地区生物结皮的生态功能具有重要意义,生物结皮对土壤水分循环的影响已成为干旱地区生态学研究的热点之一.就生物结皮对不同来源水分的影响和利用过程的研究进展进行综述,并对今后该领域的发展状况做出展望.The ecological role of biological soil crust is obviously important in arid areas.Effects of biological soil crust on soil water cycle become one of the research hotspot in recent years.Meanwhile,the research results are sometime different in similar studies.In this paper,the effects of biological soil crust on different water source and the process of the water utilization were summarized by reviewing lots of research literatures and some research prospects in this field were proposed.

关 键 词：生物结皮 土壤水分循环 干旱区 

分 类 号：Q948.112[生物学—植物学]