详细信息
乌兰布和沙漠东北部大气降尘特征及影响因素分析 被引量:18
Analysis of the characteristics and affecting factors of atmospheric dustfall in northeastern Ulan Buh Desert
文献类型:期刊文献
中文题名:乌兰布和沙漠东北部大气降尘特征及影响因素分析
英文题名:Analysis of the characteristics and affecting factors of atmospheric dustfall in northeastern Ulan Buh Desert
作者:高君亮[1,2,3] 辛智鸣[1,3] 刘芳[1,3] 原伟杰[4] 冯伟[2] 徐军[1,3] 赵英铭[1,3] 郝玉光[1,3]
第一作者:高君亮
机构:[1]中国林业科学研究院沙漠林业实验中心;[2]中国林业科学研究院荒漠化研究所;[3]国家林业局内蒙古磴口荒漠生态系统定位观测研究站;[4]国际竹藤中心
年份:2014
期号:8
起止页码:145-150
中文期刊名:干旱区资源与环境
外文期刊名:Journal of Arid Land Resources and Environment
收录:北大核心:【北大核心2011】;CSSCI:【CSSCI2014_2016】;CSCD:【CSCD2013_2014】;
基金:"十二五"农村领域国家科技计划课题(2012BAD16B0103);国家林业局林业科学技术推广项目(2012)31号共同资助
语种:中文
中文关键词:大气降尘;下垫面;防风固沙;乌兰布和沙漠
外文关键词:atmospheric dustfall; underlying surface; wind- breaking and sand -fixing; Ulan Buh Desert
分类号:P425.55
摘要:采用野外定位实测法,对乌兰布和沙漠东北部5种不同下垫面(绿洲防护林带、农田、固定沙丘、半固定沙丘、流动沙丘)的大气降尘进行了研究。结果表明:(1)研究区大气降尘具有明显的时空分异规律,不同月份的降尘量之间有着极显著差异(P<0.0001),4月份的降尘量达年内最大值,3-6月的降尘量之和占全年总量的46.3%;不同下垫面的年降尘量之间存在极显著差异(P<0.0001),从大到小为:流动沙丘>半固定沙丘>固定沙丘>林带>农田;不同高度的降尘量也存在极显著差异(P<0.0001),0.5m的降尘量大于1.5m的。(2)扬沙和沙尘暴发生的总天数与降尘量之间存在极显著线性相关关系(P<0.01),因此认为大风(≥6m/s)持续时间与扬沙和沙尘暴发生总天数是影响降尘的一个主要因子;降雨对降尘具有一定的抑制作用;下垫面状况是决定起尘强度的一个关键因子,其对降尘的影响主要是通过地表植被的防风固沙作用实现的。
Using field observation method, the atmosphere dustfall of different underlying surfaces ( oasis protec- tion forest belt, farmland, fixed dune, semi- fixed dune and mobile dune ) in northeastern Ulan Buh Desert were studied. The results showed that: (1) there were obvious temporal and spatial distribution laws in atmos- pheric dusffall. An highly significant difference about dusffall capacity existed among different months (P 〈 0. 0001 ) , dusffall capacity reached the peak in April; from March to June, the summation of dustfall capacity to- taled 46.3% of annual total quantity. There was an extremely significant difference about dusffall capacity among different underlying surfaces (P 〈 0.0001 ) ; the order from high to low was mobile dune, semi fixed sand dune, fixed sand dune, forest land and farmland; Besides, there was also a very significant difference between different sampling height ( P 〈 0. 0001 ) ; dustfall capacity in 0.5m height was larger than that in 1.5m height. (2) The total days of blowing sand and sandstorms had highly significant linear correlation ( P 〈 O. O1 ) with dustfall capac- ity, which suggested that the time of wind duration and the total days of blowing sand and sandstorms are impor- tant factors to the change of dustfall capacity; rainfall has some certain inhibition effect to dustfall; the condition of underlying surface is a key factor to decide dustfall intensity, and its influence is mainly accomplished by the wind prevention and sand fixation effect of land vegetation.
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