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中国沙漠 ›› 1997, Vol. 17 ›› Issue (2): 127-132.

• 研究论文 • 上一篇    下一篇

腾格里沙漠东南缘降尘粒度特征和沉积速率

肖洪浪, 张继贤, 李金贵   

  1. 中国科学院兰州沙漠研究所, 兰州 730000
  • 收稿日期:1995-12-11 修回日期:1996-09-03 出版日期:1997-06-20 发布日期:1997-06-20
  • 作者简介:肖洪浪,男,1956年生,理学硕士,研究员。主要从事水土资源与环境的研究工作。
  • 基金资助:
    中国科学院沙坡头试验研究站基金项目

DUSTFALL PARTICLE-SIZE AND SEDIMENT RATE AT THE SOUTHERN EDGE OF TENGGER DESERT

Xiao Honglang, Zhang Jixian, Li Jingui   

  1. Institute of Desert Research, Chinese Academy of Sciences, Lanzhou 730000
  • Received:1995-12-11 Revised:1996-09-03 Online:1997-06-20 Published:1997-06-20

摘要: 从多年降尘实测资料入手,分析了粉尘粒度特征、沉积速率和时变过程。提出了气象要素相关估测模型.确定0.25 mm为本区粉尘沉积粒径上限。周围沙漠是粉尘沉积细砂部分的尘源,粉砂和粘土部分沉积来自一个较大的时空范围,二者几乎各占降尘量的1/2。研究区年平均粉尘沉积速率4358kg/km2,每年5月的季风转期具有年内最大沉积速率。

关键词: 粉尘粒度特征, 尘源分析, 沉积速率, 估测模型

Abstract: Dustfall is a important process of weather in the arid zone.However,studies of dustfall can not meet development of environment sciences because of absence of long-term observation in the world.This paper analysed time-space changes of dustfall and brought forward two prediction models.Annual mean dustfall is 4 358 kg/km2,of which dustfall makes up 79.32% in Spring and Summer.In a year the highest dustfall comes forth in May and June which is the transitional period of the season wind in eastern Asia.Particles between 0.07~0.5 mm make up 49.43% of total dustfall and come from near deserts;particles below 0.07 mm count for 50.57% and from a intercontinental scale.

Key words: Dustfall particle-size, Sediment rate, Dust sources, Prediction models

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