DocumentCode
3333900
Title
Notice of Retraction
Hydrochemical Features of the Thermal Waters in Chongqing Metropolitan, Southwest China
Author
Xiao Qiong ; Chen Zhantu ; Yang Lei ; Shen Licheng ; Wu Kunyu
Author_Institution
Sch. of Geogr. Sci., Southwest Univ., Chongqing, China
fYear
2011
fDate
10-12 May 2011
Firstpage
1
Lastpage
4
Abstract
Notice of Retraction
After careful and considered review of the content of this paper by a duly constituted expert committee, this paper has been found to be in violation of IEEE´s Publication Principles.
We hereby retract the content of this paper. Reasonable effort should be made to remove all past references to this paper.
The presenting author of this paper has the option to appeal this decision by contacting TPII@ieee.org.
There are about 100 million m3 underground thermal water resource storage in Chongqing, and 13 thermal water samples were collected from the Chongqing metropolitan area and analyzed. The results shows that HCO3-, SO42-, Ca2+, Mg2+ are the main ions in all the thermal waters and the hydrochemical types of these thermal springs are all SO42--Ca and SO42--Ca-Mg, which suppose that all the thermal waters have the same recharge. What´s more, a good positive correlation between SO42- and Ca2+, Mg24--reveals that SO42-, Ca2+, Mg2+ in these thermal waters have the same origin. But a little difference of hydrochemical characters between nature springs and drilling wells shows that thermal water in nature springs is a mixture of water in sandstone and water in thermal aquifer.
After careful and considered review of the content of this paper by a duly constituted expert committee, this paper has been found to be in violation of IEEE´s Publication Principles.
We hereby retract the content of this paper. Reasonable effort should be made to remove all past references to this paper.
The presenting author of this paper has the option to appeal this decision by contacting TPII@ieee.org.
There are about 100 million m3 underground thermal water resource storage in Chongqing, and 13 thermal water samples were collected from the Chongqing metropolitan area and analyzed. The results shows that HCO3-, SO42-, Ca2+, Mg2+ are the main ions in all the thermal waters and the hydrochemical types of these thermal springs are all SO42--Ca and SO42--Ca-Mg, which suppose that all the thermal waters have the same recharge. What´s more, a good positive correlation between SO42- and Ca2+, Mg24--reveals that SO42-, Ca2+, Mg2+ in these thermal waters have the same origin. But a little difference of hydrochemical characters between nature springs and drilling wells shows that thermal water in nature springs is a mixture of water in sandstone and water in thermal aquifer.
Keywords
calcium; groundwater; hydrogen compounds; magnesium; negative ions; positive ions; sulphur compounds; water quality; water resources; Ca2+; Chongqing metropolitan area; HCO3-; Mg2+; SO42-; bicarbonate ions; calcium ions; hydrochemical characters; hydrochemical features; magnesium ions; sandstone; southwest China; sulfate ions; thermal aquifer; thermal springs; underground thermal water resource; Correlation; Iron; Springs; Temperature measurement; Thermal analysis; Water; Water resources;
fLanguage
English
Publisher
ieee
Conference_Titel
Bioinformatics and Biomedical Engineering, (iCBBE) 2011 5th International Conference on
Conference_Location
Wuhan
ISSN
2151-7614
Print_ISBN
978-1-4244-5088-6
Type
conf
DOI
10.1109/icbbe.2011.5780873
Filename
5780873
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