A5050032602- Clay minerals and soil interactions
- Geological and Geochemical Analysis
- Geochemistry and Elemental Analysis
- Geology and Paleoclimatology Research
- Geochemistry and Geologic Mapping
- Iron oxide chemistry and applications
- Soil and Unsaturated Flow
- Paleontology and Stratigraphy of Fossils
- Therapeutic Uses of Natural Elements
- Pharmaceutical and Antibiotic Environmental Impacts
- Adsorption and biosorption for pollutant removal
- X-ray Diffraction in Crystallography
- Soil Geostatistics and Mapping
- Crystallization and Solubility Studies
- Geological formations and processes
- Pleistocene-Era Hominins and Archaeology
- Crystal Structures and Properties
- Mineralogy and Gemology Studies
- Geological and Geophysical Studies
- Analytical chemistry methods development
- Heavy metals in environment
- Arsenic contamination and mitigation
- Coal and Its By-products
- Hydrocarbon exploration and reservoir analysis
- Mine drainage and remediation techniques
China University of Geosciences
2016-2025
University of Cincinnati
2021
Wuhan University of Technology
2005
Abstract Decomposition of soil organic matter (SOM) can be stimulated by fresh input, a phenomenon known as the ‘priming effect’. Despite its global importance, relationship priming effect to mineral weathering and nutrient release remains unclear. Here we show close linkages between in critical zone primed decomposition SOM. Intensified rock-derived are generally coupled with SOM resulting from “triggered” microbial activity. Fluxes products decomposed via linearly correlated congruency....
Sorption of dissolved organic matter (DOM) is one major pathway in the formation mineral-associated (MOM), but there little information on how previous sorption events feedback to later ones by leaving their imprint mineral surfaces and solutions ("legacy effect"). In order conceptualize role legacy effects MOM formation, we conducted sequential experiments with kaolinite gibbsite as minerals DOM derived from forest floor materials. The efficiency leveled off upon repeated addition identical...
Abstract Clay minerals are common in martian geological units and globally widespread on Earth. Understanding the origin, formation, alteration of clay is crucial for unraveling past environmental conditions Earth Mars, which composition crystallinity serve as important surrogate indicators addressing these issues. Here, 621 soil sediment samples from five chronosequences representing different climatic zones China were investigated using visible to near-infrared reflectance (VNIR)...
Abstract A red soil profile in Xuancheng, Anhui province, southern China, the middle to lower reaches of Yangtze River, was investigated using X‐ray diffraction, fluorescence spectrometer, and scanning electron microscopy. The mobile components K 2 O Na trace elements Ba Sr Xuancheng section exhibit a general trend decrease downward along profile, together with an increase chemical index alteration (CIA) values, suggesting more intense depletion portion than upper portion. major SiO , Al 3...