Topographical changes of ground surface affected by the shelterbelt along the Tarim Desert Highway

查看全文 作　　者：LI [1]ShengYu;LEI [1]JiaQiang;XU [1]XinWen;WANG [1,2]HaiFeng;FAN [1,2]JingLong;GU [3]Feng;QIU [3]YongZhi;XU [3]Bo;GONG [4]Qing;ZHENG [4]Wei

机构地区：[1]Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,Urumqi 830011,China;[2]Graduate University of the Chinese Academy of Sciences,Beijing 100049,China;[3]Tarim Branch,PetroChina Company Limited,Korla 841000,China;[4]Weather Station of Tazhong,Qiemo 841000,China

出　　处：《Chinese Science Bulletin》索引2008年第53卷第S2期,共14页

基　　金：Supported by Major Orientation Foundation of the CAS Innovation Program (Grant No. KZCX3-SW-342);CAS Action-Plan for West Development (Grant No. KZCX2-XB2-13);Major Scientific and Technological Special of Xinjiang Uygur Autonomous Region (Grant No. 200733144-3);National Natural Science Foundation of China (Grant No. 40701019);the research projects of the Tarim Branch of Petro-China Company Limited (Grant Nos. 971008090016 and 971008090017);the Western Light of the Chinese Academy of Sciences (Grant No. 20052118) 摘　　要：To study the effects of sand protection project on modern aeolian landform, the types, distribution, and intensity of topographical changes of the ground surface affected by the shelterbelt along the Tarim Desert Highway were determined by measuring the deflation and deposition of sand surface in the Tazhong area located in the hinterland of the Taklimakan Desert. The results showed that (1) the newly-formed landform in sand protection systems is dominated by aeolian deposition including the small-scale Nabkha Dunes, the medium-scale sheet-like sand deposition and the large-scale ridge-like sand deposition. To some degree, aeolian deflation landform can also be formed in the open space in the shelterbelt. Furthermore, it is difficult for aeolian deflation landform to develop in a large scale in the interdunes. However, aeolian deflation landform can be developed in a large-scale on the windward slope of secondary dunes in longitudinal complex sand ridges; (2) on the windward side of the sand protection systems, both the morphology and strike of dwarf mobile dunes in the interdunes are changed by the sand-obstructing forest belts and the ridge-like sand deposition around it. The wind- ward slope of the ridge-like deposition around the sand-obstructing forest belt forms a stable ground surface. After being damaged by forward-moving dunes in a short period, the ground surface is re- covered gradually; (3) on the leeward side of the sand protection systems, aeolian deflations are formed widely. Particularly, the deflation depression is formed in the interdunes. In addition, the dunes in the region with highly topographic relief are cut flat by aeolian deflations; thereafter its relief of to- pography is reduced. The above analysis indicates that shelterbelts have obvious effects on the windward wind-sand flux in terms of dissipating energy and intercepting sand. With the recovery of wind velocity on the leeward side of the sand protection systems, the wind-sand flux gradually tends to be unsaturated; therefore the sand surface deflation is formed. 关键词：aeolian LANDFORM DEFLATION and deposition of sand SURFACE SHELTERBELT TARIM DESERT Highway

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Topographical changes of ground surface affected by the shelterbelt along the Tarim Desert Highway

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