A5102840299- Plant Water Relations and Carbon Dynamics
- Hydrology and Watershed Management Studies
- Climate variability and models
- Soil Carbon and Nitrogen Dynamics
- Soil and Unsaturated Flow
- Soil and Water Nutrient Dynamics
- Irrigation Practices and Water Management
- Soil erosion and sediment transport
- Environmental and Agricultural Sciences
- Meteorological Phenomena and Simulations
- Microbial Metabolic Engineering and Bioproduction
- Plant responses to elevated CO2
- Greenhouse Technology and Climate Control
- Soil Moisture and Remote Sensing
- Groundwater and Isotope Geochemistry
- Microbial Community Ecology and Physiology
- Advanced Computational Techniques and Applications
- Plant Ecology and Soil Science
- Hydrology and Drought Analysis
- Liver Disease Diagnosis and Treatment
- Integrated Water Resources Management
- Fermentation and Sensory Analysis
- Peatlands and Wetlands Ecology
- Forest, Soil, and Plant Ecology in China
- Scientific Research and Discoveries
Chinese Academy of Sciences
2007-2025
Institute of Soil and Water Conservation
2010-2025
Northwest A&F University
2016-2025
University of Chinese Academy of Sciences
2016-2025
China Tobacco
2023-2025
Ministry of Water Resources of the People's Republic of China
2018-2025
Abstract. Within the Budyko framework, controlling parameter (ω in Fu equation) is widely considered to represent landscape conditions terms of vegetation coverage (M); however, some qualitative studies have concluded that climate seasonality (S) should be incorporated ω. Here, we discuss relationship between ω, M, and S, further develop an empirical equation so contributions from M actual annual evapotranspiration (ET) can determined more accurately. Taking 13 catchments Loess Plateau as...
Abstract The advection‐aridity approach to estimate actual evaporation from natural land surfaces is one of the better known implementations Bouchet's complementary principle. Detailed measurements at 2, 12, and 32 m above ground surface during growing seasons 2004–2007 allowed validation a generalized nonlinear form this highly variable terrain in Changwu County southern Loess Plateau Yellow River basin China. obtained values parameters were found lie well within ranges be expected on...
Flavors and fragrances are essential for product quality, yet they highly susceptible to contamination due high moisture content rich nutrients. This study investigates microbial growth, pH changes, volatile compound dynamics, community changes during the storage of flavors fragrances. Results indicate that total viable counts (TVC) remained stable first three days but increased rapidly afterward, exceeding acceptable limit 5 log CFU/mL by day 7. The levels initially rose slightly, followed...
The generalized proportionality hypothesis (GPH) highlights the competitive relationships among hydrological components as precipitation (P) transforms into runoff (Q) and evapotranspiration (E), providing a novel perspective on E partitioning that differs from traditional physical source-based approach. To achieve sequential of initial (Ei) continuing (Ec) under GPH, P-Q relationship-based Ei estimation method was proposed for Model Parameter Estimation Experiment (MOPEX) catchments. On...
Abstract The legacy nitrate–nitrogen (NO 3 − −N) in the soils is a long‐term threat to groundwater regions with thick unsaturated zones, and it thus important investigate amounts sources of NO −N for effective environmental management. Given substantial conversions arable farmlands non‐fertilizer land uses restoration degraded land, effects loessial zones China remain uncertain. We collected soil samples from loess profiles >13‐m deep under farmland grassland, apricot, pine, peashrub,...
Abstract. Within the Budyko framework, controlling parameter (ω in Fu equation) is widely considered to represent landscape conditions terms of vegetation coverage (M); however, some qualitative studies have concluded that climate seasonality (S) should be incorporated ω. Here, we discuss relationship between ω, M, and S, further develop an empirical equation so contributions from M actual evapotranspiration (ET) can determined more accurately. Taking 13 catchments Loess Plateau as examples,...