Arid
DOI10.1016/j.jhydrol.2018.03.003
Groundwater flowpaths and residence times inferred by C-14, Cl-36 and He-4 isotopes in the Continental Intercalaire aquifer (North-Western Africa)
Petersen, J. O.1,2; Deschamps, P.1; Hamelin, B.1; Fourre, E.3; Goncalves, J.1; Zouari, K.4; Guendouz, A.5; Michelot, J. -L.6; Massault, M.6; Dapoigny, A.3
通讯作者Petersen, J. O.
来源期刊JOURNAL OF HYDROLOGY
ISSN0022-1694
EISSN1879-2707
出版年2018
卷号560页码:11-23
英文摘要

In a semi-arid to arid climate context, dependency on groundwater resources may lead to overexploitation and deterioration of water quality. The Continental Intercalaire (CI) aquifer is one such continentalscale aquifer (more than a million of km(2)), which is mainly confined, poorly recharged but intensely abstracted. To date, the management of this resource relies on hydrogeological modelling and key parameters such as recharge/discharge rate and groundwater dynamics. We use a combination of residence time indicators (C-14, Cl-36, He-4) and stable isotopes of water (H-2 and O-18) to give greater constraint on the groundwater residence time in the CI. In previous studies, C-14 measurements and steady state modelling indicate a residence time of less than 100 ka whereas in others, Cl-36 measurements and transient scenarios modelling suggest a longer residence time (>500 ka).


In this study, most of the C-14 measurements are below the limit of detection, establishing residence times greater than 40 ka and confirming the necessity of strict sampling protocols to exclude all air and AMS measurements when low C-14 concentrations are expected.


In the Tunisian recharge area, detectable C-14 indicate sporadic recharge episodes (3-7 ka and 29-43 ka), whereas He-4 and Cl-36 concentrations in central areas suggest very old (<2 Ma) groundwaters. In these central areas, chlorine concentration can reach more than 2 g/l. Since Cl-36 concentrations are up to 4 time less than the initial input, we are confident there is no excessive deep Cl-36 production.


We characterise five distinct flowpaths reaching the Tunisian discharge area using their isotopic signatures. According to our mixing model, the average contribution from the main recharge area, the Algerian Atlas Mountains, is around 88%. This value is close to hydrogeological models. Conversely, the contribution from the Dahar Mountains is lower than in the hydrogeological modelling (2% against 10%) whereas the Tinhert shows a greater contribution (10% against 1%).


Increase of abstraction from the CI can potentially activate the circulation of old brackish groundwaters and dramatically decrease the water quality in the whole system. (C) 2018 Elsevier B.V. All rights reserved.


英文关键词Recharge Groundwater budget Radioactive isotopes Stables isotopes Continental-scale aquifer Tunisia and Algeria
类型Article
语种英语
国家France ; England ; Tunisia ; Algeria
收录类别SCI-E
WOS记录号WOS:000430882300002
WOS关键词GREAT ARTESIAN BASIN ; HELIUM ACCUMULATION ; OLD GROUNDWATER ; STABLE-ISOTOPE ; DEEP AQUIFERS ; CRUSTAL HE-4 ; NOBLE-GASES ; TUNISIA ; TRANSPORT ; RECHARGE
WOS类目Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
WOS研究方向Engineering ; Geology ; Water Resources
来源机构French National Research Institute for Sustainable Development ; E17
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/211058
作者单位1.Aix Marseille Univ, CNRS, IRD, CEREGE UM34, F-13545 Aix En Provence, France;
2.British Geol Survey, Maclean Bldg, Wallingford OX10 8BB, Oxon, England;
3.UVSQ, CNRS, CEA, LSCE,ISPL,UMR8212, F-91191 Gif Sur Yvette, France;
4.ENIS, LRAE, BP 1173, Sfax 3038, Tunisia;
5.Univ Blida, Blida, Algeria;
6.Univ Paris Saclay, Univ Paris Sud, CNRS, GEOPS, Rue Belvedere,Bat 504, F-91405 Orsay, France
推荐引用方式
GB/T 7714
Petersen, J. O.,Deschamps, P.,Hamelin, B.,et al. Groundwater flowpaths and residence times inferred by C-14, Cl-36 and He-4 isotopes in the Continental Intercalaire aquifer (North-Western Africa)[J]. French National Research Institute for Sustainable Development, E17,2018,560:11-23.
APA Petersen, J. O..,Deschamps, P..,Hamelin, B..,Fourre, E..,Goncalves, J..,...&Dapoigny, A..(2018).Groundwater flowpaths and residence times inferred by C-14, Cl-36 and He-4 isotopes in the Continental Intercalaire aquifer (North-Western Africa).JOURNAL OF HYDROLOGY,560,11-23.
MLA Petersen, J. O.,et al."Groundwater flowpaths and residence times inferred by C-14, Cl-36 and He-4 isotopes in the Continental Intercalaire aquifer (North-Western Africa)".JOURNAL OF HYDROLOGY 560(2018):11-23.
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