PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Potential use of alluvial groundwater for irrigation in arid zones - Mhamid Oasis (S Morocco)

Identyfikatory
Warianty tytułu
PL
Przydatność wód aluwialnych do nawadniania w obszarach suchych - Oaza Mhamid (Płd Maroko)
Języki publikacji
EN
Abstrakty
EN
In arid zones, the availability of fresh water is usually very limited because of high salinity, which greatly limits their use for irrigation purposes. High mineralization of water used for irrigation leads to increased soil salinity. The aim of the study was to examine the potential use of alluvial groundwater for irrigation in arid zones. The works were conducted in the Middle Draa Valley in southern Morocco (the Mhamid Oasis) in October 2015. Water samples of alluvial groundwater were collected for laboratory analysis from 42 wells located in the oasis. In order to determine the possibility to use the water for irrigation purposes, the Sodium Adsorption Ratio (SAR), sodium percentage (%Na), permeability index (PI), Kelly’s ratio (KR), magnesium hazards (MH) and electrical conductivity (EC) were assessed. EC values, exceeding 3000 μS·cm-1 in all the samples, classify the water as unsuitable for irrigation. MH and the KR indexes show that 30% of water samples represent levels making them unsuitable for irrigation. SAR confirms the very high degree of susceptibility of the analyzed waters to salinity hazard. The PI index of these waters is moderate, however in terms of sodium content they can be deemed suitable for irrigation purposes. It has been found that even within a small area of the oasis, a very large differentiation in the alluvial groundwater suitability for irrigation purposes occurs.
Rocznik
Strony
129--140
Opis fizyczny
Bibliogr. 31 poz., wykr., tab., rys.
Twórcy
  • Department of Geomorphology, Faculty of Geography and Regional Studies, University of Warsaw, ul. Krakowskie Przedmieście 30, 00-927 Warszawa, Poland
  • Department of Environmental Protection and Modelling, Faculty of Mathematics and Natural Sciences, The Jan Kochanowski University in Kielce, ul. Świętokrzyska 15, 25-406 Kielce, Poland
  • Department of Hydrometry, Faculty of Geography and Geological Sciences, Adam Mickiewicz University in Poznań, ul. B. Krygowskiego 10, 61-680 Poznań, Poland
Bibliografia
  • [1] El Mandour A, El Yaouti CF, Fakir CY, Zarhloule CY, Benavente CJ. Evolution of groundwater salinity in the unconfined aquifer of Bou-Areg, Northeastern Mediterranean coast, Morocco. Environ Geol. 2008;54:491-503. DOI: 10.1007/s00254-007-0842-3.
  • [2] Kudoda AM, Abdalla OAE. Hydrochemical characterization of the main aquifers in Khartoum, the capital city of Sudan. Environ Earth Sci. 2015;74:4771-4786. DOI: 10.1007/s12665-015-4464-x.
  • [3] Ammar BS, Taupin JD, Zouari K, Khouatmia M. Identifying recharge and salinization sources of groundwater in the Oussja Ghar el Melah plain (northeast Tunisia) using geochemical tools and environmental isotopes. Environ Earth Sci. 2016;75:606. DOI: 10.1007/s12665-016-5431-x.
  • [4] Fakharian K, Narany TS. Multidisciplinary approach to evaluate groundwater salinity in Saveh Plain, Iran. Environ Earth Sci. 2016;75:624. DOI: 10.1007/s12665-015-5104-1.
  • [5] Wilcox LV. Classification and Use of Irrigation Water. USDA; 1955. https://www.ars.usda.gov/arsuserfiles/20360500/pdf_pubs/P0192.pdf.
  • [6] Deshpande SM, Ather KR. Evaluation of groundwater quality.and its suitability for drinking and agriculture use in parts of Vaijapur, District Aurangabad, MS, India. Res J Chem Sci. 2012;2(1):25-31. http://www.isca.in/rjcs/Archives/v2/i1/04.ISCA-RJCS-2011-216_Done.php.
  • [7] Alaya BM, Saidi S, Zemni T, Zargouni F. Suitability assessment of deep groundwater for drinking and irrigation use in the Djeffara aquifers (Northern Gabes, south-eastern Tunisia). Environ Earth Sci. 2014;71(8):3387-3421. DOI: 10.1007/s12665-013-2729-9.
  • [8] Ghazaryan K, Chen Y. Hydrochemical assessment of surface water for irrigation purposes and its influence on soil salinity in Tikanlik oasis, China. Environ Earth Sci. 2016;75:383. DOI: 10.1007/s12665-016-5287-0.
  • [9] Houatmia F, Azouzi R, Charef A, Bedir M. Assessment of groundwater quality for irrigation and drinking purposes and identification of hydrogeochemical mechanisms evolution in Northeastern, Tunisia. Environ Earth Sci. 2016;75:746. DOI: 10.1007/s12665-016-5441-8.
  • [10] Wang YG, Li Y, Xiao DN. Catchment scale spatial variability of soil salt content in agricultural oasis, Northwest China. Environ Geol. 2008;56:439-446. DOI: 10.1007/s00254-007-1181-0.b.
  • [11] Ghassemi F, Jakeman AJ, Nix HA. Salinisation of Land and Water Resources: Human Causes, Extent, Management and Case Studies. Wallingford: CAB International; 1995; 526 p.
  • [12] Ahmed MA, Abdel Samie SG, Badawy HA. Factors controlling mechanisms of groundwater salinization and hydrogeochemical processes in the Quaternary aquifer of the Eastern Nile Delta, Egypt. Environ Earth Sci. 2013;68:369-394. DOI: 10.1007/s12665-012-1744-6.
  • [13] El Maghraby MMS. Geochemical and isotopic evidence of seawater intrusion into the shallow pleistocene coastal aquifer, West Alexandria Egypt. Life Sci J. 2014;11(7):749-762. http://www.lifesciencesite.com/lsj/life1107/110_25356life110714_749_762.pdf. [14] Kijne JW. Water and salinity balances for irrigated agriculture in Pakistan. Research Report 6. Colombo, Sri Lanka: International Irrigation Management Institute (IIMI); 1996. http://www.iwmi.cgiar.org/Publications/IWMI_Research_Reports/PDF/pub006/REPORT06.PDF.
  • [15] Ma JZ, Wang XS, Edmunds WM. The characteristics of ground-water resources and their changes under the impacts of human activity in the arid Northwest China - a case study of the Shiyang River Basin. J Arid Environ. 2005;61:277-295. DOI: 10.1016/j.jaridenv.2004.07.014.
  • [16] Bouchaou L, Michelot JL, Vengosh A, Hsissou Y, Qurtobi M, Gaye CB, et al. Application of multiple isotopic and geochemical tracers for investigation of recharge, salinization, and residence time of water in the Souss-Massa aquifer, Southwest of Morocco. J Hydrol. 2008;352:267-287. DOI: 10.1016/j.jhydrol.2008.01.022.
  • [17] Warner N, Lgourna Z, Bouchaou L, Boutaleb S, Tagma T, Hsaissoune M, et al. Integration of geochemical and isotopic tracers for elucidating water sources and salinization of shallow aquifers in the sub-Saharan Drâa Basin, Morocco. Appl Geochem. 2013;34:140-151. DOI: 10.1016/j.apgeochem.2013.03.005.
  • [18] Dłużewski M, Krzemień K. Physical and geographical characteristics of Coude du Dra region. In: Dłużewski M, editor. Modern Evolution of the Natural Environment of the Coude du Dra Region (Morocco) and its Impact on the Human Living Conditions. Warszawa: Academic Publisher Dialog; 2003:11-44.
  • [19] Sobczak K. Changes in the environment and migration in the south Morocco - the example of Mhamid oasis. Miscellanea Geographica Warszawa: Uniwersytet Warszawski; 2008;13:239-250.
  • [20] Richards LA. Diagnosis and Improvement of Saline and Alkali Soils. Handbook 60. Washington DC: US Dept. of Agriculture; 1954;160 pp.
  • [21] Ragunath HM. Groundwater, 2nd Ed. New Delhi: Wiley Eastern Ltd; 1987. https://www.ars.usda.gov/ARSUserFiles/20360500/hb60_pdf/hb60complete.pdf.
  • [22] Kelly WP. Use of saline irrigation water. Soil Sci. 1963; 95(4):355-391. http://journals.lww.com/soilsci/Citation/1963/06000/USE_OF_SALINE_IRRIGATION_WATER_.3.aspx.
  • [23] Flowers TJ. Improving crop salt tolerance. J Exp Bot. 2004;55(396):307-319. DOI: 10.1093/jxb/erh003.
  • [24] Mer RK, Prajith PK, Pandya DH, Pandey A. Effect of salts on germination of seeds and growth of young plants of Hordeum vulgare, Tricticum aestivum, Cicer arietinum and Brassica juncea. J Agron Crop Sci. 2000;185:209-217. DOI: 10.1046/j.1439-037x.2000.00423.x.
  • [25] Martinez V, Creda A. Nitrate reductase activity in tomato and cucumber leaves as influence by NaCl and N source. J Plant Nutr. 1989;12:1335-1350. DOI: 10.1080/01904168909364040.
  • [26] Zhu JK. Plant salt tolerance. Trends Plant Sci. 2001;6(2):66-71. DOI: 10.1016/S1360-1385(00)01838-0.
  • [27] Jungklang J, Usui K, Masumoto H. Differences in physiological responses to NaCl between salt-tolerant Sesbania rostrata Brem. & Oberm. and non-tolerant Phaseolus vulgaris L. Weed Biology Manage. 2003;(3):21-27. DOI: 10.1046/j.1445-6664.2003.00077.x.
  • [28] Ashraf M. Some important physiological selection criteria for salt tolerance in plants. Flora - Morphol Distribut Functional Ecology Plants. 2004;199(5):361-376. DOI: 10.1078/0367-2530-00165.
  • [29] Parida AK, Das AB. Salt tolerance and salinity effects on plants: a review. Ecotoxicol Environ Saf. 2005;60(3):324-49. DOI: 10.1016/j.ecoenv.2004.06.010.
  • [30] Wu J, Qian H, Fang Y. Assessment of soil salinization based on a low-cost method and its influencing factors in a semiarid agricultural area, northwest China. Environ Earth Sci. 2014;71:3465-3475. DOI: 10.1007/s12665-013-2736-x.
  • [31] Omar SA, Abdel Sater MH, Khallil AM, Abd Alla MH. Growth and enzyme activity of fungi and bacteria in soil salinized with sodium chloride. Folia Microbiol. 1994;39:23-28. DOI: 10.1007/BF02814524.
Uwagi
PL
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-29fef3e2-9bcc-41fb-8317-bece15299bf3
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.