NDLI: Hydrochemical Simulation and Using the Hydrochemical Kinetics to Calculate the Parameters in Longkeng

Content Provider	IEEE Xplore Digital Library
Author	Liu Jin-feng Xiao Changlai Feng Bo Lin Yaju Li Yuqiu
Copyright Year	2010
Abstract	This paper goes up each node representative sample using PHREEQC software , on the flow line, to carry out the calculation of degree of saturation and the inverse hydrochemical simulation , the chemical type whose result shows of the study district underground water belongs to typical dissolve water. In the entire runoff process, dolomite, gypsum and halite are in not saturation state, calcite is part to reach saturation , gypsum and halite dissolve continuously. Applying the method of groundwater chemical kinetics to calculate the hydrogeology parameter is the synthesize utilizing of the theories of chemical thermodynamics, hydrochemical dynamics and ground-water dynamics. This method can not only remedy the difficulty that is hard to determine hydrogeology parameter because of lacking the information of pumping test and can reduce the work of pumping test , save cost. The infiltration coefficient and velocity that uses chemical dynamics method to calculate show that the permeability of the aquifer in the middle of the study area is higher, in the recharge area is little high, the drainage area is most weak. The cycle time of underground water will take about 90 years.
Starting Page	1
Ending Page	3
File Size	291193
Page Count	3
File Format	PDF
ISBN	9781424447121
ISSN	21517622
DOI	10.1109/ICBBE.2010.5515515
Language	English
Publisher	Institute of Electrical and Electronics Engineers, Inc. (IEEE)
Publisher Date	2010-06-18
Publisher Place	China
Access Restriction	Subscribed
Rights Holder	Institute of Electrical and Electronics Engineers, Inc. (IEEE)
Subject Keyword	Thermodynamics Inverse problems Atmospheric modeling Cities and towns Kinetic theory Minerals Permeability Chemicals Water resources Testing
Content Type	Text
Resource Type	Article

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