Masters in ground water science and engineering in Beijing normal university

Groundwater is the water present beneath Earth's surface in soil pore spaces and in the fractures of rock formations. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from and eventually flows to the surface naturally; natural discharge often occurs at springs and seeps, and can form oases or wetlands.

Official transcripts from all the previously attended institutions, Submission of undergraduate academic transcripts and one original authenticated copy of Bachelor s degree certificate and graduation certificate, 2 Recommendation letters, Personal Statement, Proof of Chinese language proficiency (HSK certificate and transcript)

Researcher, Counselor, Administrator, Professor

30th May