J4 ›› 2010, Vol. 40 ›› Issue (5): 1098-1103.

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Inverse Geochemical Modeling of Arsenic Groundwater at Arseniasis Area in the Western of Jilin Province

BIAN Jian-min1, ZHA En-shuang1, TANG Jie1, MA Li1,2,CHEN Gang1,3   

  1. 1.College of Environment and Resources, Jilin University, Changchun 130026, China;
    2.Geo-Environmental Monitoring Central Station of Jilin Province, Changchun 130021, China;
    3.Jilin Water Industry Investment Co.Ltd, Changchun 130033, China
  • Received:2010-01-15 Online:2010-09-26 Published:2010-09-26

Abstract:

In order to reveal the water-rock interaction process of high arsenic groundwater formation and transportation in the western of Jilin Province, field investigation, samples collection and data analysis had been finished. We used the experimental data to analyze the groundwater chemical features and high arsenic groundwater distribution in horizontal and vertical direction. By application to the PHREEQC, inverse modeling of the high arsenic groundwater was carried out. Based on the simulation, the minerals dissolution or resolution of arsenic, iron and manganese were calculated under different flow paths. The result shows that the deliquescent quantities into groundwater of both paths between different samples of scorodite mineral rich in arsenic are 2.44×10-6, 8.03×10-7, 7.98×10-6 and 4.14×10-7 mmol/L. The minerals rich in iron or manganese such as goethite, hematite, pyrolusite and bixbyite had been dissolved into groundwater, while the sulfate and carbon dioxide dissolved out, which revealed that arsenic is related to them and enriched in the alkaline and reduction environment.

Key words: groundwater, high arsenic distribution, inverse geochemical modeling, western of Jilin Province

CLC Number: 

  • P641.3
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