STUDY ON THE EOLIAN DUST FLUX OVER THE LOESS PLATEAU:AN EXAMPLE  

作　　者：安芷生 肖举乐 

机构地区：[1]Xi'an Laboratory of Loess and Quaternary Geology, Academia Sinica, Xi'an 710061, PRC

出　　处：《Chinese Science Bulletin》1990年第19期1627-1631,共5页

摘　　要：The wind is a basic factor in the atmosphere subsystem in the Earth system, and an agent in transferring the mass and energy within the system. The grain size and mass flux of the eolian dust in the Neocene deep-sea sediments recorded the intensity of the atmospheric circulation and the aridity in the dust source area. The loess on the Loess Plateau, the dust accumulation after its origin, transportation, deposition, and reworked process, is

关 键 词：median(Md) apparent DRY BULK DENSITY true DRY BULK DENSITY EOLIAN dust flux. 

分 类 号：N[自然科学总论]