风水复合侵蚀研究述评

• Published in: 地理学报（英文版） 2006, Vol.16 (2), p.231-241
• Main Authors: 宋阳, 严平, 刘连友
• Format: Article
• Language: Chinese
• ISSN: 1009-637X
• DOI: 10.3969/j.issn.1009-637X.2006.02.012

P4; Complex erosion by wind and water, which is also called aeolian-fluvial interactions, is an important erosion process and landscape in arid and semiarid regions. The effectiveness of links between wind and water process, spatial environmental transitions and temporal environmental change are the three main driving forces determining the geomorphologic significance of aeolian-fluvial interactions. As a complex interrelating and intercoupling system, complex erosion by wind and water has spatialtemporal variation features. The process of complex erosion by wind and water can be divided into palaeoenvironmental process and contemporary process. Early work in drylands has often been attributed 1930s that the research on complex erosion by wind and water had been conducted. There are two obstacles restricting the research of complex erosion by wind and water. Firstly, how to transform in different temporal and spatial scales is still unsettled; and secondly, the research methodology is still immature. In the f