Development of a Multi-Aspects Groundwater Vulnerability Index in the Transboundary Aquifer between Syria, Iraq, and Turkey in light of the water conflict and climate change

نوع مقاله : مقاله پژوهشی

نویسندگان

1 Water Engineering Department, Faculty of Agriculture and Natural Resources, Imam Khomeini International University, Qazvin, Iran and Environmental Engineering Technologies Department, Faculty of Technical Engineering, Aleppo University, Aleppo, Syria.

2 Water Engineering Department, Faculty of Agriculture and Natural Resources, Imam Khomeini International University, Qazvin, Iran

3 Civil, Environmental and Natural Resources Engineering Department, Lulea University of Technology, Lulea, Sweden.

4 Water Engineering Department, Faculty of Agriculture and Natural Resources, Imam Khomeini International University, Qazvin, Iran.

چکیده

Groundwater vulnerability assessment is an effective tool in the joint management of transboundary groundwater, especially in developing countries where data is scarce, monitoring networks are insufficient, and water is both a cause and a target of conflicts. The Jezira Tertiary Limestone Aquifer Transboundary System (JTLATS) region, which Syria, Iraq, and Turkey share, gives a clear description of the shared water problem in developing countries with arid and semiarid environments. In this study, a comprehensive multidisciplinary Groundwater Vulnerability Index (GVI) was developed as a distributed composite index to assess the groundwater vulnerability in JTLATS by combining different environmental and political socioeconomic datasets and models for three periods between 2003 and 2017. The JTLATS was categorized into five zones: very low, low, moderate, high, and very high vulnerability. The results showed a low vulnerability in the southern regions of the aquifer. In comparison, the areas with high vulnerability are primarily spread in the northern and western parts of the JTLATS and along the Euphrates river. The results showed an increase in the percentage of areas with high vulnerability from 10.45% in (2003-2007) to 13.42% and 20.57% of the aquifer area in (2007-2011) and (2011-2017), respectively. The groundwater vulnerability in the aquifer increased with the spread of political instability in both Syria and Iraq and the increase in cultivated areas in Turkey

کلیدواژه‌ها

موضوعات

عنوان مقاله [English]

Development of a Multi-Aspects Groundwater Vulnerability Index in the Transboundary Aquifer between Syria, Iraq, and Turkey in light of the water conflict and climate change

نویسندگان [English]

  • Mmohamed Al-Mohamed 1
  • Abbas Sotoodehnia 2
  • Peyman Daneshkar Arasteh 2
  • Nadhir Al-Ansari 3
  • Asghar Azizian 4
  • Hadi Ramezani Etedali 4
1 Water Engineering Department, Faculty of Agriculture and Natural Resources, Imam Khomeini International University, Qazvin, Iran and Environmental Engineering Technologies Department, Faculty of Technical Engineering, Aleppo University, Aleppo, Syria.
2 Water Engineering Department, Faculty of Agriculture and Natural Resources, Imam Khomeini International University, Qazvin, Iran
3 Civil, Environmental and Natural Resources Engineering Department, Lulea University of Technology, Lulea, Sweden.
4 Water Engineering Department, Faculty of Agriculture and Natural Resources, Imam Khomeini International University, Qazvin, Iran
چکیده [English]

Groundwater vulnerability assessment is an effective tool in the joint management of transboundary groundwater, especially in developing countries where data is scarce, monitoring networks are insufficient, and water is both a cause and a target of conflicts. The Jezira Tertiary Limestone Aquifer Transboundary System (JTLATS) region, which Syria, Iraq, and Turkey share, gives a clear description of the shared water problem in developing countries with arid and semiarid environments. In this study, a comprehensive multidisciplinary Groundwater Vulnerability Index (GVI) was developed as a distributed composite index to assess the groundwater vulnerability in JTLATS by combining different environmental and political socioeconomic datasets and models for three periods between 2003 and 2017. The JTLATS was categorized into five zones: very low, low, moderate, high, and very high vulnerability. The results showed a low vulnerability in the southern regions of the aquifer. In comparison, the areas with high vulnerability are primarily spread in the northern and western parts of the JTLATS and along the Euphrates river. The results showed an increase in the percentage of areas with high vulnerability from 10.45% in (2003-2007) to 13.42% and 20.57% of the aquifer area in (2007-2011) and (2011-2017), respectively. The groundwater vulnerability in the aquifer increased with the spread of political instability in both Syria and Iraq and the increase in cultivated areas in Turkey

کلیدواژه‌ها [English]

  • Groundwater
  • Transboundary
  • Vulnerability
  • Syria
  • Composite Index

مراجع

  • ACSAD, GDTKB and GCHS (Arab Center for the Studies of Arid Zones and Dry Lands, 2003. General Directorate for Tigris and Khabour Basins; General Corporation for Hydrological Studies. Project of Preparation of a Database and a Mathematical Model for the Northern Part of the Khabour Basin. In The Mathematical Model (General Report). Damascus.

 

  • Al-Ansari N, Adamo N, Knutsson S, Laue J, 2018. Geopolitics of the Tigris and Euphrates basins. Journal of Earth Sciences and Geotechnical Engineering, 8(3), 187-222.‏

 

  • Allan T, 2012. The Middle East water question: Hydropolitics and the global economy. Bloomsbury Publishing.‏

 

  • Aller L, Bennett T, Lehr J, Petty R J, Hackett G, 1987. DRASTIC: A standardized system for evaluating ground water pollution potential using hydrogeologic settings. US Environmental Protection Agency. Washington, DC, 455.‏

 

  • Avci H, Dokuz U E, Avci A S, 2018. Hydrochemistry and groundwater quality in a semiarid calcareous area: an evaluation of major ion chemistry using a stoichiometric approach. Environmental monitoring and assessment, 190(11), 1-16.‏

 

  • Barbulescu A, 2020. Assessing groundwater vulnerability: DRASTIC and DRASTIC-like methods: a review. Water, 12(5), 1356.‏

 

  • Burdon, D.J. and Safadi, C., 1963. Ras-el-ain: The great karst spring of mesopotamia: An hydrogeological study. Journal of Hydrology, 1(1), pp.58-95.

 

  • Chao N, Luo Z, Wang Z, Jin T, 2018. Retrieving groundwater depletion and drought in the Tigris‐Euphrates Basin between 2003 and 2015. Groundwater, 56(5), 770-782.‏

 

  • Choo E U, Wedley W C, 2008. Comparing fundamentals of additive and multiplicative aggregation in ratio scale multi-criteria decision making. The Open Operational Research Journal, 2(1).‏

 

  • Fan, Y., Li, H., & Miguez-Macho, G. (2013). Global patterns of groundwater table depth. Science, 339(6122), 940-943.‏

 

  • Fraser C M, Kalin R M, Kanjaye M, Uka Z, 2020. A methodology to identify vulnerable transboundary aquifer hotspots for multi-scale groundwater management. Water International, 45(7-8), 865-883.‏ https://doi.org/10.1080/02508060.2020.1832747.

 

  • Friedl, M., & MCD12Q1, S. M. D. v006. MODIS. Terra+ Aqua land cover type yearly L3 global, 500.‏.‏ https://doi.org/10.5067/MODIS/MCD12Q1.006.

 

  • Ghadimi M, Zangenehtabar S, Malekian A, Kiani M, 2022. Groundwater vulnerability assessment in a karst aquifer: a case study of western Iran. International Journal of Environmental Science and Technology, 1-14.‏

 

  • Gogu, R. C., & Dassargues, A. (2000). Current trends and future challenges in groundwater vulnerability assessment using overlay and index methods. Environmental geology, 39(6), 549-559.‏

 

  • Gleeson T, Smith L, Moosdorf N, Hartmann J, Dürr H H, Manning A H, Jellinek A M, 2011. Mapping permeability over the surface of the Earth. Geophysical Research Letters, 38(2).‏ http://dx.doi.org/10.1029/2010GL045565.

 

  • Gleeson T, Moosdorf N, Hartmann J, Van Beek L P H, 2014. A glimpse beneath Earth's surface: GLobal HYdrogeology MaPS (GLHYMPS) of permeability and porosity. Geophysical Research Letters, 41(11), 3891-3898.‏

 

  • Hartmann J, Moosdorf N, 2012. The new global lithological map database GLiM: A representation of rock properties at the Earth surface. Geochemistry, Geophysics, Geosystems, 13(12).‏ http://dx.doi.org/10.29/2012GC004370.

 

  • Heijden P V D, Falguerolles A, Leeuw J, 1989. A combined approach to contingency table analysis using correspondence analysis and log-linear analysis. Applied Statistics, 38(2), 249-292.‏ https://doi.org/10.2307/2348058.

 

  • Heiser W J, Meulman J, 1983. Analyzing rectangular tables by joint and constrained multidimensional scaling. Journal of Econometrics, 22(1-2), 139-167.‏ https://doi.org/1016/0304-4076(83)90097-0

 

 

 

  • Huan H, Zhang B T, Kong H, Li M, Wang W, Xi B, Wang G, 2018. Comprehensive assessment of groundwater pollution risk based on HVF model: a case study in Jilin City of northeast China. Science of the total Environment, 628, 1518-1530.‏ https://doi.org/10.1016/j.scitotenv.2018.02.130.

 

  • IGRAC U. I, 2015. Transboundary aquifers of the world [map]. 15 Scale 1: 50 000 000.‏

 

  • Joint Research Centre-European Commission, 2008. Handbook on constructing composite indicators: methodology and user guide. OECD publishing.‏

 

  • Kattan, Z., 2018. Using hydrochemistry and environmental isotopes in the assessment of groundwater quality in the Euphrates alluvial aquifer, Syria. Environmental earth sciences, 77(2), pp.1-18.

 

  • Kattan Z, 2002. Effects of sulphate reduction and geogenic CO₂ incorporation on the determination of ¹⁴C groundwater ages–a case study of the Palaeogene groundwater system in north-eastern Syria. Hydrogeology journal.‏ https://doi.org/1007/s10040-002-0199-3.
  • Lapworth D J, Nkhuwa D C W, Okotto-Okotto J, Pedley S, Stuart M E, Tijani M N, Wright J J H J, 2017. Urban groundwater quality in sub-Saharan Africa: current status and implications for water security and public health. Hydrogeology Journal, 25(4), 1093-1116.‏ https://doi.org/10.1007/s10040-016-1516-6.

 

  • Lezzaik K, Milewski A, Mullen, J, 2018. The groundwater risk index: Development and application in the Middle East and North Africa region. Science of the Total Environment, 628, 1149-1164.‏ https://doi.org/10.1016/j.scitotenv.2018.02.066.

 

  • Lutz A, Thomas J M, Keita M, 2011. Effects of population growth and climate variability on sustainable groundwater in Mali, West Africa. Sustainability, 3(1), 21-34.‏ https://doi.org/10.3390/su3010021.

 

  • McCracken M, 2017. Measuring transboundary water cooperation: options for Sustainable Development Goal Target 6.5(pp. 1-88). Stockholm, Sweden: Global Water Partnership (GWP).‏

 

  • Mohtadi S, 2013. Climate change and the Syrian uprising. Bulletin of the Atomic Scientists, 16.‏

 

  • Ouedraogo I, Defourny P, Vanclooster M, 2016. Mapping the groundwater vulnerability for pollution at the pan African scale. Science of the Total Environment, 544, 939-953.‏ https://doi.org/10.1016/j.

 

  • Ouedraogo I, Girard A, Vanclooster, M, Jonard F, 2020. Modelling the temporal dynamics of groundwater pollution risks at the african scale. Water, 12(5), 1406.‏ https://doi.org/3390/w12051406.

 

  • Ostrom E, 1990. Governing the commons: The evolution of institutions for collective action. Cambridge university press.‏

 

  • Pacheco F A, Fernandes L F S, 2013. The multivariate statistical structure of DRASTIC model. Journal of Hydrology, 476, 442-459.‏ https://doi.org/10.1016/j.jhydrol.2012.11.020.

 

  • Pacheco F A L, Landim P M B, 2005. Two-way regionalized classification of multivariate datasets and its application to the assessment of hydrodynamic dispersion. Mathematical geology, 37(4), 393-417.‏ https://doi.org/1007/s11004-005-5955-1.

 

  • Stadler S, Geyh M A, Ploethner D, Koeniger P, 2012. The deep Cretaceous aquifer in the Aleppo and Steppe basins of Syria: assessment of the meteoric origin and geographic source of the groundwater. Hydrogeology Journal, 20(6), 1007-1026.‏

 

  • Team R. C, 2019. R: A language and environment for statistical computing. Vienna, Austria.‏

 

 

  • Rivera A, Candela L, 2018. Fifteen-year experiences of the internationally shared aquifer resources management initiative (ISARM) of UNESCO at the global scale. Journal of Hydrology: Regional Studies, 20, 5-14.‏ https://doi.org/10.1016/j.ejrh.2017.12.003.

 

  • Raupach M R, Haverd V, Briggs P R, 2013. Sensitivities of the Australian terrestrial water and carbon balances to climate change and variability. Agricultural and Forest Meteorology, 182, 277-291.‏ https://doi.org/10.1016/j.agrformet.2013.06.017.

 

  • Taghavi N, Niven R K, Paull D J, Kramer M, 2022. Groundwater vulnerability assessment: A review including new statistical and hybrid methods. Science of The Total Environment, 153486.‏

 

  • UN-ESCWA, B.G.R., 2013. Inventory of shared water resources in Western Asia: Chapter 6 Jordan River Basin. United Nations Economic and Social Commission for Western Asia. Federal Institute for Geosciences and Natural Resources, Beirut.
  • World Bank. World Development Indicators database, edited, Washington DC, USA.

 

  • Worth R F, 2010. Earth is parched where Syrian farms thrived. New York Times, 13.‏

 

  • Yahia A, Bouabid El M, 2011. Assessment of aquifer vulnerability based on GIS and ARCGIS methods: a case study of the Sana'a Basin (Yemen). Journal of Water Resource and Protection, 2011.‏

 

  • Yesilnacar M I, Gulluoglu M S, 2008. Hydrochemical characteristics and the effects of irrigation on groundwater quality in Harran Plain, GAP Project, Turkey. Environmental Geology, 54(1), 183-196.‏ https://doi.org/ 10.1007/s00254-007-0804-9.
علوم و مهندسی آبیاری
دوره 45، شماره 2
تیر 1401
صفحه 1-18

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سابقه مقاله

  • تاریخ دریافت: 29 اردیبهشت 1401
  • تاریخ بازنگری: 21 خرداد 1401
  • تاریخ پذیرش: 23 خرداد 1401
  • تاریخ انتشار: 01 تیر 1401

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