Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China

Wei, Y., Fan, J., Xu, X., & Lei, J. (March-April, 2017). Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China. Water Technology and Sciences (in Spanish), 8(2), 151-158. In this article, hydrogeological parameters were determined by a single well pum...

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Main Authors: Wei Yaping, Fan Jinglong, Xu Xinwen, Lei Jiaqiang
Format: Article
Language:Spanish
Published: Instituto Mexicano de Tecnología del Agua 2017-08-01
Series:Tecnología y ciencias del agua
Subjects:
Online Access:http://www.revistatyca.org.mx/ojs/index.php/tyca/article/view/1315
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spelling doaj-eda5d064709245659622e99772d8df282020-11-24T20:48:17ZspaInstituto Mexicano de Tecnología del AguaTecnología y ciencias del agua0187-83362007-24222017-08-018215115810.24850/j-tyca-2017-02-141202Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, ChinaWei Yaping0Fan Jinglong1Xu Xinwen2Lei Jiaqiang3Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences/ University of Chinese Academy of SciencesXinjiang Institute of Ecology and Geography Chinese Academy of SciencesXinjiang Institute of Ecology and Geography Chinese Academy of SciencesXinjiang Institute of Ecology and Geography Chinese Academy of SciencesWei, Y., Fan, J., Xu, X., & Lei, J. (March-April, 2017). Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China. Water Technology and Sciences (in Spanish), 8(2), 151-158. In this article, hydrogeological parameters were determined by a single well pumping test. Over the course of the study, BETCO was used to eliminate the effects of atmospheric pressure changes on water level based on the regression deconvolution method. The aquifer test was used to analyze data and to calculate hydrogeological parameters. Finally, from the three unconfined aquifer models, though the Boulton model cannot successfully gain well-fitting results, the Theis model with Jacob correction and the Neuman model results obtained hydrogeological parameters by curve-fitting. Additionally, permeability coefficient of the two models is in good agreement with previous research, which can provide a reference for further study in the hinterland of the desert, especially for the construction of hydrological modeling research.http://www.revistatyca.org.mx/ojs/index.php/tyca/article/view/1315Pumping test, aquifer test, pressure correction, hydrogeological parameters
collection DOAJ
language Spanish
format Article
sources DOAJ
author Wei Yaping
Fan Jinglong
Xu Xinwen
Lei Jiaqiang
spellingShingle Wei Yaping
Fan Jinglong
Xu Xinwen
Lei Jiaqiang
Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China
Tecnología y ciencias del agua
Pumping test, aquifer test, pressure correction, hydrogeological parameters
author_facet Wei Yaping
Fan Jinglong
Xu Xinwen
Lei Jiaqiang
author_sort Wei Yaping
title Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China
title_short Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China
title_full Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China
title_fullStr Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China
title_full_unstemmed Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China
title_sort water table response to a pumping test in the hinterland core area of the taklimakan desert, china
publisher Instituto Mexicano de Tecnología del Agua
series Tecnología y ciencias del agua
issn 0187-8336
2007-2422
publishDate 2017-08-01
description Wei, Y., Fan, J., Xu, X., & Lei, J. (March-April, 2017). Water table response to a pumping test in the hinterland core area of the Taklimakan Desert, China. Water Technology and Sciences (in Spanish), 8(2), 151-158. In this article, hydrogeological parameters were determined by a single well pumping test. Over the course of the study, BETCO was used to eliminate the effects of atmospheric pressure changes on water level based on the regression deconvolution method. The aquifer test was used to analyze data and to calculate hydrogeological parameters. Finally, from the three unconfined aquifer models, though the Boulton model cannot successfully gain well-fitting results, the Theis model with Jacob correction and the Neuman model results obtained hydrogeological parameters by curve-fitting. Additionally, permeability coefficient of the two models is in good agreement with previous research, which can provide a reference for further study in the hinterland of the desert, especially for the construction of hydrological modeling research.
topic Pumping test, aquifer test, pressure correction, hydrogeological parameters
url http://www.revistatyca.org.mx/ojs/index.php/tyca/article/view/1315
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AT fanjinglong watertableresponsetoapumpingtestinthehinterlandcoreareaofthetaklimakandesertchina
AT xuxinwen watertableresponsetoapumpingtestinthehinterlandcoreareaofthetaklimakandesertchina
AT leijiaqiang watertableresponsetoapumpingtestinthehinterlandcoreareaofthetaklimakandesertchina
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