Hydrogeochemical processes constrained by multivariate statistical methods and isotopic evidence of groundwater recharge in the aquifer of Figuig, Eastern High Atlas of Morocco
详细信息 查看全文
- 作者：Abdelhakim Jilali ; Nathalie Fagel ; Mounir Amar…
- 关键词：Hydrogeochemistry ; Statistical analysis ; Isotopes ; Figuig aquifer ; Morocco
- 刊名：Arabian Journal of Geosciences
- 出版年：2016
- 出版时间：January 2016
- 年：2016
- 卷：9
- 期：1
- 全文大小：6,058 KB
- 参考文献：Abderamane H, Razack M, Vassolo S (2013) Hydrogeochemical and isotopic characterization of the groundwater in the Chari-Baguirmi depression, Republic of Chad. Environ Earth Sci 69(7):2337鈥?350CrossRef
Assou M (1996) Salinit茅 des sols et qualit茅 des eaux d鈥檌rrigation de l鈥檕asis de Figuig. Minist猫re de l鈥檃griculture et de la mise en valeur agricole, Administration du g茅nie rural, Direction du d茅veloppement et de la gestion de l鈥檌rrigation. Rabat, 99 p.
Craig H (1961) Isotopic variations in meteoric water. Sci 133:1702鈥?703CrossRef
Eichinger L (1983) A contibution to the interpretation of 14C groundwater ages considering the exemple of a partially confined sandstone aquifer. Radiocarbon 25(2):347鈥?56
Fontes J-C, Garnier J-M (1979) Determination of the initial 14C activity of the total dissolved carbon: a review of the existing models and a new approach. Water Resour Res 15(2):399鈥?13CrossRef
Ingerson E, Pearson F-J (1964) Estimation of age and rate of motion of groudwater by the 14C method. In: Recent Researches in the Fields of Hydrosphere, Atmosphere and Nuclear Geochemistry (ed. by Maruzen). Maruzen, Tokyo, Japan, pp 263鈥?83
Jilali A (2014a) Contribution 脿 la compr茅hension du fonctionnement hydrodynamique de la nappe souterraine de l鈥檕asis de Figuig (Haut Atlas Oriental). Universit茅 Mohammed Premier, Oujda, 161 pp
Jilali A (2014b) Impact of climate change on the Figuig aquifer using a numerical model: oasis of Eastern Morocco. J Biol Earth Sci 4(1):E16鈥揈24
Jilali A, Zarhloule Y (2015) Structural control of the hydrogeology in Figuig Oasis in the eastern High Atlas of Morocco. P Geologists Assoc 126(2):232鈥?43CrossRef
Jilali A, Abbas M, Amar M, Zarhloule Y (2015a) Groundwater contamination by wastewater in Figuig Oasis (eastern High Atlas, Morocco). Nature Environ Pollu Techno 14(2):275鈥?82
Jilali A, Amar M, Zarhloule Y, Amar N, Kerchaoui S, Baba E (2015b) Apport de la g茅ophysique 脿 la compr茅hension des structures g茅ologiques de l鈥檕asis de Figuig (Haut Atlas Oriental, Maroc). J Materials Environ Sci 6(1):236鈥?45
Jilali A, Zarhloule Y, Georgiadis M (2015c) Vulnerability mapping and risk of groundwater of the oasis of Figuig, Morocco: application of DRASTIC and AVI methods. Arab J Geosci 8(3):1611鈥?621CrossRef
Kortatsi B (2006) Hydrochemical characterization of groundwater in the Accra plains of Ghana. Environ Geol 50(3):299鈥?11CrossRef
Kumar M, Herbert J-R, Ramanathan A-L, Someshwar Rao M, Kim K, Deka J-P, Kumar B (2013) Hydrogeochemical zonation for groundwater management in the area with diversified geological and land-use setup. Chem Erde-Geochem 73(3):267鈥?74CrossRef
Parkhurst D-L, Appelo C-A-J (1999) User鈥檚 guide to PHREEQC (Version 2): a computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations. Water-Resources Investigations Report. USGS, Denver, Colorado, 99鈥?259, p 312
Rodier J (1984) L鈥檃nalyse de l鈥檈au: eaux naturelles, eaux r茅siduaires, eau de mer. Dunod, 7th ed, Paris
Thivya C, Chidambaram S, Thilagavathi R, Prasanna M-V, Singaraja C, Nepolian M, Sundararajan M (2013) Identification of the geochemical processes in groundwater by factor analysis in hard rock aquifers of Madurai District. South India Arab J Geosci 1鈥?1
Tlili-Zrelli B, Hamzaoui-Azaza F, Gueddari M, Bouhlila R (2013) Geochemistry and quality assessment of groundwater using graphical and multivariate statistical methods. A case study: Grombalia phreatic aquifer (Northeastern Tunisia). Arab J Geosci 6(9):3545鈥?561CrossRef
Vasanthavigar M, Srinivasamoorthy K, Prasanna M-V (2013) Identification of groundwater contamination zones and its sources by using multivariate statistical approach in Thirumanimuthar sub-basin, Tamil Nadu, India. Environ Earth Sci 68(6):1783鈥?795CrossRef
Wang P, Yu J, Zhang Y, Liu C (2013) Groundwater recharge and hydrogeochemical evolution in the Ejina Basin, northwest China. J Hydrol 476:72鈥?6CrossRef
Wildemeersch S, Orban P, Ruthy I, Gri猫re O, Olive P, El Youbi A, Dassargues A (2010) Towards a better understanding of the Oulmes hydrogeological system (Mid-Atlas, Morocco). Environ Earth Sci 60(8):1753鈥?769CrossRef
Wu J, Li P, Qian H, Duan Z, Zhang X (2013) Using correlation and multivariate statistical analysis to identify hydrogeochemical processes affecting the major ion chemistry of waters: a case study in Laoheba phosphorite mine in Sichuan. China Arab J Geosci 1鈥?0
Zhai Y, Wang J, Teng Y, Zuo R (2013) Hydrogeochemical and isotopic evidence of groundwater evolution and recharge in aquifers in Beijing Plain, China. Environ Earth Sci 69(7):2167鈥?177CrossRef - 作者单位：Abdelhakim Jilali (1)
Nathalie Fagel (2)
Mounir Amar (3)
Mahmoud Abbas (4)
Yassine Zarhloule (1)
1. Laboratory of Mineral Deposits, Hydrogeology & Environment, Faculty of Sciences, University Mohammed I, Boulevard Mohammed VI, BP: 524, 60000, Oujda, Morocco
2. Department of Geology, Faculty of Science, University of Liege, Liege, Belgium
3. Department of Geology, Faculty of Science, University of Moulay Ismail Meknes, Meknes, Morocco
4. Laboratory of Water Analysis of Figuig (L.A.E.F), Municipality of Figuig, BP 121, Administrative Centre, 61000, Figuig, Morocco - 刊物类别：Earth and Environmental Science
- 出版者：Springer Berlin Heidelberg
- ISSN：1866-7538
文摘
In this paper, we present and discuss 72 samples of groundwater (borehole, well, and spring), collected over a period of time of 20 years (i.e., between 1983 and 2004) in the Figuig aquifer. The chemical and isotopic analyses were carried out to improve our understanding of the hydrogeochemical processes. Most of the waters sampled consist of Ca-Mg-HCO3 and Na-K-Cl types. The samples are grouped according to two factors. Factor 1 shows strong negative loadings of EC, Cl-, Na+, Ca2+, Mg2+, and NO3鈭?/sup>, K+ with 73.91 % of the total variance (TV); factor 2 shows strong positive loadings of SO4 2鈭?/sup>, HCO3鈭?/sup> with TV of 11.02 %. The 18O and 2H values of well and spring waters are linearly correlated, in a similar manner to the World Meteoric Water Line (WMWL). The 14C datings indicate that the age of groundwater obtained using different models ranges between 2495 and 10,696 years. Keywords Hydrogeochemistry Statistical analysis Isotopes Figuig aquifer Morocco