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...
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 ...
supported by the National Basic Research Program of China(973 Program) (2009CB421006);the State Key Laboratory of Geological Processes and Mineral Resources (GPMR200843)
REE fractionation during the weathering of dolomite has been recognized for decades.A regolith profile on dolomite in southwest Yunnan of China was selected to investigate the behaviors of REE during weathering.The we...
supported by the Science Foundation of Nanjing University of Information Science and Technology,China(No.20080328);the National Key Technology R&D Program (No.2006BAK21B02);the National Key Basic Research Program (973 Program) of China (No.2003CB415201);the National Natural Science Foundation of China (No.40671016)
Trace element(TE) and rare earth element(REE) contents in red soils from the Dongting Lake area of China were determined to understanding the provenance and weathering characteristics of the red soils.The results show...