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从沙尘暴看黄土的沉积及黄土高原的形成
引用本文:胡良军,邵明安.从沙尘暴看黄土的沉积及黄土高原的形成[J].安徽师范大学学报(自然科学版),2001,24(2):148-152.
作者姓名:胡良军  邵明安
作者单位:中国科学院、水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室.
基金项目:中国科学院知识创新工程项目;KZCX2-411;
摘    要:以近年来我国西北地区多发的沙尘暴现象为缘起,对沙尘暴的特征、发生机制等进行了讨论;论述了沙尘暴引起的降尘与黄土的堆积与沉积的过程;黄土堆积沉积的年龄、颗粒成分等;以及沙尘暴与高土高原的形成之间的关系,同时论述了黄土高原的环境变迁,认为高空均质粉尘的降落是不均匀的;高空降尘是突发的,而风及流水对堆积粉尘的改造是长期和连续的。

关 键 词:沙尘暴  黄土沉积  黄土高原
文章编号:1001-2443(2001)02-0148-05
修稿时间:2000年11月6日

RELATIONSHIP BETWEEN DUST-STORM AND LOESS ACCUMULATION & FORMATION OF THE LOESS PLATEAU
HU Liang jun,SHAO Ming an.RELATIONSHIP BETWEEN DUST-STORM AND LOESS ACCUMULATION & FORMATION OF THE LOESS PLATEAU[J].Journal of Anhui Normal University(Natural Science Edition),2001,24(2):148-152.
Authors:HU Liang jun  SHAO Ming an
Abstract:Taking the dust storm phenomenon occurred in recent years as an excuse, the characteristic and regulation of dust storm are discussed. Then the loess deposit, vegetation vicissitude the relationship between dust storm and formation of the Loess Plateau are also discussed. Some results are: the falling of the even dust in the sky from the remote west is not even; the occurrence of dust storm is abrupt, and the effect of runoff and wind to loess deposit is continuous and lasting.
Keywords:dust  storm  loess accumulation  the Loess Plateau
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