A5101503054- Aeolian processes and effects
- Soil erosion and sediment transport
- Geology and Paleoclimatology Research
- Atmospheric aerosols and clouds
- Atmospheric chemistry and aerosols
- Hydrology and Sediment Transport Processes
- Tree Root and Stability Studies
- Rangeland Management and Livestock Ecology
- Vehicle emissions and performance
- Wind and Air Flow Studies
- Particle Dynamics in Fluid Flows
- Hydrology and Watershed Management Studies
- Marine and environmental studies
- Hemophilia Treatment and Research
- Lichen and fungal ecology
- Big Data and Business Intelligence
- Business Strategy and Innovation
- Soil and Unsaturated Flow
- Biocrusts and Microbial Ecology
- Tree-ring climate responses
- Plant responses to elevated CO2
- Fire effects on ecosystems
- African Botany and Ecology Studies
- Soil Geostatistics and Mapping
- Geological formations and processes
Xinjiang Institute of Ecology and Geography
2014-2025
Chinese Academy of Sciences
2014-2025
Hebei University of Economics and Business
2006-2024
University of Chinese Academy of Sciences
2014-2021
National Soil Erosion Research Laboratory
2020
Beijing Normal University
2010-2020
Abstract The Tibetan Plateau experienced severe aeolian desertification during the mid‐ and late 20th century, but mitigation of this has occurred since 2000 despite a warming climate. causes desertiffication its have been debated by scientists because their potentially huge significance for PR China Asia, as well global climate systems. Based on review previous studies our own investigations, it appears that from 1970s to was caused primarily unsustainable irrational human activities,...
Abstract The question of whether the emitted dust size distribution (EDSD) depends on wind velocity or soil (SSD) remains to be resolved. This study used tunnel tests investigate influence and SSD EDSD. results showed that EDSD was influenced by both texture, supporting saltation bombardment theory. ratios PM 2.5 10 ( R PM2.5/10 ) 1.0 PM1.0/10 ), which reflect in range 0–10 μm, trends increase with increasing friction u * for all six tested soils. trend more significant than , indicates...
Desert steppe is widely distributed in wind erosion regions, and also an important potential dust emission source the regions. Recognition of characteristics desert foundation for accurate simulation regions; however, few related studies have been conducted areas. In this study, we selected four sites a region to conducting observations, analyzing horizontal saltation flux vertical flux, identifying suitable models steppe, examining relationship between bombardment efficiency friction speed...
Abstract Dust emission depends directly and indirectly on soil particle distribution, but little information is available that examines dust potential its relationship with wind erosion for different soils. This study aimed to elucidate the difference in characteristics between loamy farmland (LF) sandy (SF) discuss influence of this potential. Field observations were conducted during 2012–2016 Bashang district, North China. With increasing friction speed, horizontal mass flux increased...
Abstract Recent studies have shown that the dust emission efficiency ( E d ) of some soil surfaces undergoes changes with wind speed and such are related to properties. Through tunnel experiments, we investigate comprehensive effect particle size composition (PSC) (both minimally fully dispersed) friction u * on . Results show initially increases then decreases as texture from fine coarse, intermediate‐textured soils having highest strongest ability. The ratio silt sand in is an index...