Physicochemistry and Mineralogy of S

时间:2023-04-29 12:24:11 天文地理论文 我要投稿
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Physicochemistry and Mineralogy of Storm Dust and Dust Sediment in Northern China

Dust sediments collected from 1995 to 1998 in Beijing, Dunhuang, Inner Mongolia, Kashi, the Kunlun Mountains, Lanzhou, Ningxia, the Taklimakan Desert, and Xi'an, China, were characterized in terms of their physical, chemical, and mineralogical properties. Most aerosols and dust analysed ranged in texture from silty clay to clay loam. Their median particle diameters (Mds) generally ranged between 5 to 63μm,coinciding with those of loess from central China and the finest sand from northwestern China. The dust sediments were characterized by a predominance of SiO2 and Al2O3, followed by K2O. Their SiO2/Al2O3and K2O/SiO2 molar ratios ranged from 5.17 to 8.43 and from 0.009 to 0.0368, respectively. The mass concentration spectrum during a dust storm showed a single peak, rather than the triple peak generally observed under clear sky conditions. The dominant minerals were chlorite, illite, calcite, and dolomite.These physical, chemical, and mineralogical properties were consistent with those of aeolian soils and loess in western and central China. The results suggest that aerosols and fine-gained fractions of dust sediments collected in northern China are mainly composed of soil material transported from the arid and semiarid regions of China and Mongolia by prevailing winds. The rate of deposition and properties of dust falling on eastern China were strongly influenced by meteorological conditions, season, latitude, longitude, and altitude of the sampling sites.

作 者: 刘蔚 冯起 王涛 张艳武 施建华   作者单位: Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, No. 260 West Dong Gang Road, Lanzhou 730000  刊 名: 大气科学进展(英文版)  ISTIC SCI 英文刊名: ADVANCES IN ATMOSPHERIC SCIENCES  年,卷(期): 2004 21(5)  分类号: P4  关键词: physical chemistry and mineralogy   dust storm   dust sediment   northern China  

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