Foundation item:The National Science and Technology Major Project of the Ministry of Science and Technology of China under contract No.2016ZX05026007-03;the National Natural Science Foundation of China under contract Nos 41876046 and 41930536。
Rapid changes on nutrient supply and CO2 concentration that occurred in the northern South China Sea(SCS)during the Early Oligocene,provides an ideal natural laboratory,allowing us to peer into the coccolithophores’p...
supported by the National Natural Science Foundation of China(Grant Nos.41210004;41661144042; 41603018);National Basic Research Program(973project)of China(2013CB956401)
Exploring the relationship between weathering and erosion is essential for understanding the evolution of landscapes and formation of soil under the influence of climate, tectonics, and topography. We measured the bul...
supported by the National Basic Research Program of China (973 Program) (No.2006CB403200);the Chinese National Natural Science Foundation (No.41403107 and No.41325010);the Basic Science Research Fund from the Institute of Hydrogeology and Environmental Geology (Grant No.SK200906 and SK201208);the China Geological Survey Projects (No.12120113005900)
Fertilization and aglime(agricultural lime) application, as important agricultural activities in acid soil, exert an influence on the fluxes of carbon both between and within ecosystems. Animal manure added to soil ca...
supported by the National Natural Science Foundation of China (Grant Nos. 41373078; 41173091);the National Key Basic Research Programme of China (Grant No. 2013CB956702)
1 Introduction Global climate change is one of the greatest challenges facing humankind in the 21st century.Studying,and utilising,the carbon sink caused by the weathering of silicate minerals has been a key research ...
supported by the National Natural Science Foundation of China(Grant No.41210004;41661144042);National Basic Research Program(973 project)of China(2013CB956401)
The distribution and anomalies of rare earth elements(REEs) of granitic regolith were studied in Inner Mongolia and Hainan Island, China. One profile showed slight REE enrichment of an upper layer and no obvious light...
funded by the National Basic Research Programs of China(Grant Nos.2011CB013504 and 2014CB046901);the National Funds for Distinguished Young Scientists of China(Grant No.51025932);the National Nature Science Foundation of China(Grant No.41372272)
The distinct element method(DEM) incorporated with a novel bond contact model was applied in this paper to shed light on the microscopic physical origin of macroscopic behaviors of weathered rock, and to achieve the...
the National Key Technology Research and Development Program of the Ministry of Science and Technology of China (Grant No. 2012BAD05B06)
Fertile topsoil was added onto the surface of barren slope land in Three Gorges Reservoir region of China in an anthropogenic process known as the foreign soil reconstruction project. The main goal of this paper was t...
supported by the National Natural Science Foundation of China (Grant Nos. 40972230, 41290250);Institute of Earth Environment, Chinese Academy of Sciences (Grant No. ZZBS1301);the National Basic Research Program of China (Grant No. 2010CB833406)
Located at the northeastern margin of the Qinghai-Tibet Plateau(QTP) in the Asian interior, the Lake Qinghai is sensitive to environmental change and thus an outstanding site for studying paleoenvironmental changes. T...
supported by the National Key Basic Research Program of China (No. 2013CB956702);the National Natural Science Foundation of China (No. 41373078)
The weathering of carbonate rocks by biological soil crusts (BSC) in karst areas is very common. It is helpful to understand the weathering mechanisms and processes for avoiding karst rock-desertification. The weath...
granted by the fund of State Key Laboratory of Ore Deposit Geochemistry (SKLODG-ZY125-01);the Major Project of Chinese National Programs for Fundamental Research and Development (973 Program)(No. 2014CB440906 and 2012CB416602)
The bauxites in central Guizhou are hosted by the Lower Carboniferous Jiujialu Formation.Geochemistrial characteristics of the Lindai bauxite deposit indicate that the underlying Shilengshui Formation dolomite is the ...