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黄河乌兰布和沙漠段沿岸不同高度典型沙丘风沙特征

尹瑞平 郭建英 董智 何京丽 李锦荣 田世民 代豫杰

水土保持研究2017,Vol.24Issue(5):157-161,5.
水土保持研究2017,Vol.24Issue(5):157-161,5.

黄河乌兰布和沙漠段沿岸不同高度典型沙丘风沙特征

Wind Velocity and Sand Flow Transport Characteristics of Different Height Typical Dunes in Ulan Buh Desert Along the Yellow River

尹瑞平 1郭建英 1董智 2何京丽 1李锦荣 1田世民 3代豫杰2

作者信息

  • 1. 水利部牧区水利科学研究所,呼和浩特010020
  • 2. 山东农业大学林学院,山东泰安271018
  • 3. 黄河水利科学研究院,郑州450003
  • 折叠

摘要

Abstract

Flow fields of wind speed and aeolian transport are concerned by scientists because of its basic position in desert research.We took 3 typical dunes with different heights as samples and measured flow fields of wind,wind profiles,velocity accelerations,sediment discharges of 5 heights of different parts.Results show that:(1) wind velocity is greater over the top of dune but lowest at central leeward and appeares to increase firstly and decrease later and increase eventually from dune windward slope foot to leeward slope foot,showing the tendency of ‘S' shape;(2) vertical changes of wind at different parts of dune and height changes of logarithmic follows the linear regression equation [V=aln(z)+b],slope of wind profile increases gradually from top of dune to slope foot of windward and leeward,friction velocity and roughness changes appear inconsistently;(3) wind velocity acceleration of low-rise (20 cm) is higher than high-rice;dune development scale impacts wind velocity acceleration of windward obviously,and feedback is significant with its growth;(4) sediment discharges of different dune parts within 0~ 100 cm show a uneven law of diminishing power function and concentrate in 0~10 cm,and distribute in 0~4 cm mostly.Relative sediment discharges are stable and do not transform with height changes.

关键词

风速流场/风速廓线/风沙流/乌兰布和沙漠

Key words

wind velocity flow field/sand flow/wind profile/Ulan Buh Desert

分类

天文与地球科学

引用本文复制引用

尹瑞平,郭建英,董智,何京丽,李锦荣,田世民,代豫杰..黄河乌兰布和沙漠段沿岸不同高度典型沙丘风沙特征[J].水土保持研究,2017,24(5):157-161,5.

基金项目

水利部公益性行业科研专项经费(201401084) (201401084)

国家自然科学基金(41301303,51409114) (41301303,51409114)

中国水利水电科学研究院科研专项(MK2016J03) (MK2016J03)

水土保持研究

OA北大核心CSCDCSTPCD

1005-3409

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