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中国沙漠 ›› 2004, Vol. 24 ›› Issue (5): 623-627.

• 研究简报 • 上一篇    下一篇

科尔沁沙地奈曼旗近5年来风况及合成输沙势

张华1,2, 李锋瑞2, 李玉霖2, 伏乾科3   

  1. 1. 辽宁师范大学 城市与环境学院, 辽宁 大连 116029;
    2. 中国科学院 寒区旱区环境与工程研究所, 甘肃 兰州 730000;
    3. 辽宁师范大学 生命科学学院, 辽宁 大连 116029
  • 收稿日期:2003-06-05 修回日期:2003-07-09 出版日期:2004-10-20 发布日期:2004-10-20
  • 作者简介:张华(1965-),女(汉族),山东东明人,理学博士,主要从事旱区恢复生态学和植物生态学研究。E-mail:zhanghua0323@sina.com
  • 基金资助:
    中国科学院寒区旱区环境与工程研究所知识创新工程项目(210097); 中国科学院"百人计划"项目共同资助

Wind Regime and Resultant Sand-transporting Potential of Naiman Banner in Horqin Sandy Land during Past Five Years

ZHANG Hua1,2, LI Feng-rui2, LI Yu-lin2, FU Qian-ke3   

  1. 1. College of City and Environment, Liaoning Normal University, Dalian 116029, Liaoning Province, China;
    2. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    3. College of Life Sciences, Liaoning Normal University, Dalian 116029, Liaoning Province, China
  • Received:2003-06-05 Revised:2003-07-09 Online:2004-10-20 Published:2004-10-20

摘要: 应用奈曼沙漠化研究站1998-2002年的气象资料, 统计分析了奈曼旗近5a来的风况特征和输沙势。结果表明: ①研究区3~5月起沙风发生频数最高, 占全年起沙风的38%~58%; 平均风速和最大风速值最大, 分别为6.0~7.5m·s-1和9.5~16.9m·s-1。该风况特征与地表冻融、裸露、干旱疏松相耦合, 形成了区内的风沙活动期。②在风沙活动期内, 风环境基本为锐双峰风况, 西北风居主导地位, 频数占54%; 南风和西南风次之, 频数占38%。③在风沙活动期内, 研究区属于高风能环境, 合成输沙势RDP为66.3VU(风速以m·s-1为单位), 合成输沙方向RDD为ESE113°。

关键词: 风况, 起沙风, 输沙量, 合成输沙势, 风沙活动期

Abstract: In this study a statistical analysis on the wind regime of Naiman banner in Horqin sandy land in past five years was made, meantime the resultant sand-transporting potential in the study area was explored. The results showed that:(1)The threshold wind of transporting sand in the study area between March to May were most frequent, with an accumulated frequency of 38%~58%. Mean and maximum wind velocities were 6.0~7.5 m·s-1 and 9.5~16.9 m·s-1 respectively. Such wind regime features, coupling with surface thawing, barren, drought and loose structure in the same period, initiated a phase of wind-sand activity.(2)During the phase of wind-sand activity the wind environment in the area roughly exhibited a bimodal wind regime, the northwest wind held a leading place, with a frequency of 54%; followed by south wind and southwest wind, with a frequency of 38%.(3)While throughout the phase of wind-sand activity resultant sand-transporting potential(RDP) was 66.7 VU(m·s-1 is the unit of wind speed), resultant sand-transporting direction(RDD) was 113°ESE, this shows that the study area belongs to a high wind energy environment, sand activity is dominated by wind erosion and sand is transported southeastward.

Key words: wind regime, threshold wind of transporting sand, sand transportion rate, resultant sand-trans-porting potential, phase of wind-sand activity

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