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清华大学校园内不同绿地类型空气PM10浓度变化规律     被引量:16

Variations of Air PM10 Concentration in Different Greenlands in Tsinghua University

文献类型:期刊文献

中文题名:清华大学校园内不同绿地类型空气PM10浓度变化规律

英文题名:Variations of Air PM10 Concentration in Different Greenlands in Tsinghua University

作者:校建民[1] 王成[2,3] 吴志萍[3] 杨伟伟[3] 侯晓静[3]

第一作者:校建民

机构:[1]中国林业科学研究院林业科技信息研究所;[2]中国林业科学研究院林业研究所国家林业局森林培育重点实验室;[3]国家林业局城市林业研究中心

年份:2009

卷号:45

期号:5

起止页码:153-156

中文期刊名:林业科学

外文期刊名:Scientia Silvae Sinicae

收录:CSTPCD;;Scopus;北大核心:【北大核心2008】;CSCD:【CSCD2011_2012】;

基金:国家科技部科研院所社会公益研究专项(2004DIB1J031);国家十一五科技支撑计划重大项目课题(2006BAD03A06)

语种:中文

中文关键词:绿地类型;空气PM10质量浓度;时间变化;清华大学

外文关键词:greenland type; air PM10 concentration; temporal variation; Tsinghua University

分类号:S173

摘要:The concentration of air PM10 in six types of green lands in campus of Tsinghua university was measured. The results showed that PM10 concentration exhibited obvious daily and monthly variation,and also had remarkable difference among different seasons. However there was no remarkable difference in concentration of PM10 within the same season over all types of green lands. As for average concentration,the value was lower in arbor land of spring,autumn and winter,and in lawn of summer. The concentration of PM10 was 43% higher in cloudy days than that of sunny ones. Moreover,the difference increased to 137% between cloudy day after raining and sunny day after raining because of the clarification of rain.
The concentration of air PM10 in six types of green lands in campus of Tsinghua university was measured. The results showed that PM10 concentration exhibited obvious daily and monthly variation, and also had remarkable difference among different seasons. However there was no remarkable difference in concentration of PM10 within the same season over all types of green lands. As for average concentration, the value was lower in arbor land of spring, autumn and winter, and in lawn of summer. The concentration of PM10 was 43 % higher in cloudy days than that of sunny ones. Moreover, the difference increased to 137% between cloudy day after raining and sunny day after raining because of the clarification of rain.

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