Abed Salih Fayyadh

University of Anbar

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Bayan Muhie Hussien

University of Anbar

Husam N. Mukhlef

Varoujan K. Sissakian

Komar University of Science and Technology

Mahmood Al-Kubaisi

University of Anbar

Saifuldeen A. Salim

University of Anbar

Jasim M. Al-Halboosi

University of Baghdad

Mohammed Affan Al Hamdani

Ministry of Higher Education and Scientific Research

Maher Ahmed Abed

University of Anbar

Jassim Mohmmed Hammed

University of Baghdad

Mohamed A. Al-Hamdani

Cooperative Institutions

University of Anbar

University of Baghdad

Komar University of Science and Technology

University of Kurdistan Hewler

National Institute of Oceanography and Fisheries

Park University

Cukurova University

Luleå University of Technology

ORCID

University of Kurdistan

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Impact of intense exploitation on the groundwater balance and flow within Mullusi aquifer (arid zone, west Iraq)

Arabian Journal of Geosciences (2011)

Bayan Muhie Hussien Abed Salih Fayyadh

Depression-focused recharge

Water balance

Groundwater discharge

Groundwater model

Infiltration (HVAC)

Cone of depression

Environmental isotopes

Overexploitation

10.1007/s12517-011-0513-2

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Citations (7)

Geological Hazards in Al-Anbar Governorate, West Iraq

IOP Conference Series Earth and Environmental Science (2022)

Varoujan K. Sissakian Abed Salih Fayyadh

Abstract Al-Anbar Governorate has the largest coverage area among the 18 Iraqi gover-norates. The coverage area is about 138 579 km2 forming about 32% of the whole coverage area of the Iraqi territory. The governorate forms the western part of Iraq representing the Iraqi Western Desert and a small part north of the Eu-phrates River within the Jazira Plain. This large coverage area with diversity of rock types with large time span (Permi-an – Pleistocene) and different topographic forms have contributed to develop-ment of different types of geological hazards, which act at different parts of the governorate with different intensities and different damages caused to the infra-structure and community, even life losses. Three main types of geological hazards are active in the governorate; these are: 1) Floods, 2) Karstification, and 3) Swell-ing (Expensive) clays; however, other types like mass movements, depressions, active tectonic areas are also present but with less significance as their risks and caused damages to the community and infrastructure is concerned.

Rockfall

Geologic hazards

10.1088/1755-1315/1080/1/012015

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Citations (1)

Hydrochemical model and probable pollution in the water of Euphrates River (Qaem–Falluja)

Arabian Journal of Geosciences (2011)

Bayan Muhie Hussien Abed Salih Fayyadh Jassim Mohmmed Hammed Mohammed Affan Al Hamdani

River pollution

10.1007/s12517-011-0390-8

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Citations (4)

Integrated Hydrogeological Approach for an Aquifer System and Groundwater Flow, Nukhaib-Km160 Area, Western Iraq

IOP Conference Series Earth and Environmental Science (2022)

Bayan Muhie Hussien Jasim M. Al-Halboosi Mahmood Al-Kubaisi Abed Salih Fayyadh

Abstract The hydraulic characteristics and the hydrogeological conditions of the hydrogeological system at Nukhaib-Km160 were studied within the water-bearing horizons, highlighting the flow system and its effects on the groundwater velocities and its balance (hydraulic gradients and permeability) taking into account the regional situations of structural. Several hydrogeological areas have been selected for future exploitation and development. 3D models and maps of spatial distribution are utilized for interpretation, it is supported by points of hydrogeological controls such as transmissivity and storage coefficients, depth of groundwater, lateral extensions, aquifers thickness, specific capacity, and well productivity. Prediction applications on specific capacities and transmissivity of aquifer and Kimball’s statistical method were used to calculate the ratio of groundwater mixing and recharge from aquifers of Umm Er Dhuma and/or Tayarat Fn. to production wells. The hydrogeological system of the Nukhaib- Km160 region has been categorized into eight major aquifers which include the Mulussa, Mulussa-Ubaid, Muhaywir-Ubaid, Hartha, Muhaywir-Najma, Umm Er Dhuma, Tayarat, and Tayarat- Umm Er Dhuma aquifers. Changes in hydraulic parameters for all aquifers have been examined in order to determine the spatial-hydrologic facts of aquifers, where the traditional TDS distribution, in addition to the hydraulic interpretation, shows the same phenomenon of interconnection and the source of groundwater. According to facts of the hydrogeological, the aquifers of Umm Er Dhuma and Tayrat are important and preferred for the plan of the future of water supply in the Western Desert of Iraq, especially for the increased demand for water resources and the sustainability of the assessment.

10.1088/1755-1315/1080/1/012003

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Citations (3)

HYDROLOGIC SYSTEM OF EUPHRATES RIVER (SPATIAL ANALYSIS) BETWEEN AL-QAEM AND FALLUJA

Iraqi Bulletin of Geology and Mining (2016)

Abed Salih Fayyadh Bayan Muhie Hussien Mohamed A. Al-Hamdani Saifuldeen A. Salim Husam N. Mukhlef

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Preferable Districts for Groundwater Exploitation Based on Hydrogeologic Data of Aquifers-West Iraq

Journal of Water Resource and Protection (2014)

Bayan Muhie Hussien Abed Salih Fayyadh

The study examines the hydrogeological conditions and the hydraulic characteristics of the water bearing horizons within the hydrogeologic regime of the study area located west of Iraq to the west of longitude 40°40'. Also the study shed light on the flow behavior regime and its impacts on the groundwater movement, ground water flow velocities (permeability and hydraulic gradients) considering the regional structural phenomena. The Hydrogeological data presented as spatial distribution maps and three dimensional models. The results which were achieved from the field measurements are correlated with the main hydrogeologic control points such as storage and transmissivity coefficients, groundwater depths, aquifers thickness, lateral extensions and groundwater recharge to classify the hydrogeologic districts for development and exploitation. The hydrogeologic regime of the study area is classified and screened into various aquifers, including Ga'ra, Mullusi, Mullusi-Ubaid, Hartha, Tayarat-Digma (Jeed), Muhaywir-Ubaid and Rattga aquifers. The statistical results of the hydraulic and hydrochemical parameters were examined for explaining the spatial distribution of each parameter within the uppermost aquifers and determining the preference hydrogeologic districts for future groundwater exploitation as hereinafter order, Ubaid Mullusi aquifer within district-6, Rattga and Digma-Tayarat aquifer within district-7, Mullusi aquifer within district-2, Hartha aquifer within district-3, Digma-Tayarat aquifer within district-4, Ga'ra aquifer within district-1, Muhaywir-Ubaid aquifer within district-5 and Digma-Tayarat within district-8, respectively.

Aquifer properties

Aquifer test

Specific storage

10.4236/jwarp.2014.612108

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Citations (7)