Separating emitted dust from the total suspension in airflow based on the characteristics of PM10 vertical concentration profiles on a Gobi surface in northwestern China  

作　　者：ZHANG Chunlai WANG Xuesong CEN Songbo ZHENG Zhongquan Charlie WANG Zhenting 

机构地区：[1]State Key Laboratory of Earth Surface Processes and Resource Ecology,MOE Engineering Research Center of Desertification and Blown-sand Control,Faculty of Geographical Science,Beijing Normal University,Beijing 100875,China [2]School of Environment,Beijing Normal University,Beijing 100875,China [3]Aerospace Engineering Department,University of Kansas,Lawrence,KS 66045-7621,USA [4]Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China

出　　处：《Journal of Arid Land》2022年第6期589-603,共15页干旱区科学（英文版）

基　　金：This work was supported by the National Natural Science Foundation of China(41630747).

摘　　要：During aeolian processes,the two most critical factors related to dust emissions are soil particle and aggregate saltation,which greatly affect the vertical profiles of near-surface dust concentrations.In this study,we measured PM10 concentrations at four different heights(0.10,0.50,1.00 and 2.00 m)with and without continuous and simultaneous aeolian saltation processes on a Gobi surface in northwestern China from 31 March to 10 April,2017.We found that the vertical concentration profiles of suspended PM10 matched the log-law model well when there was no aeolian saltation.For the erosion process with saltation,we divided the vertical concentration profiles of PM10 into the saltation-affected layer and the airflow-transport layer according to two different dust sources(i.e.,locally emitted PM10 and upwind transported PM10).The transition height between the saltation-affected layer and the airflow-transport layer was not fixed and varied with saltation intensity.From this new perspective,we calculated the airflow-transport layer and the dust emission rate at different times during a wind erosion event occurred on 5 April 2017.We found that dust emissions during wind erosion are primarily controlled by saltation intensity,contributing little to PM10 concentrations above the ground surface compared to PM10 concentrations transported from upwind directions.As erosion progresses,the surface supply of erodible grains is the most crucial factor for saltation intensity.When there was a sufficient amount of erodible grains,there was a significant correlation among the friction velocity,saltation intensity and dust emission rate.However,when supply is limited by factors such as surface renewal or an increase in soil moisture,the friction velocity will not necessarily correlate with the other two factors.Therefore,for the Gobi surface,compared to limiting dust emissions from upwind directions,restricting the transport of suspended dust in its path is by far a more efficient and realistic option for small areas that are often

关 键 词：PM10 vertical concentration profiles dust emission rate saltation intensity suspensions Gobi surface 

分 类 号：X513[环境科学与工程—环境工程]