Using Statistical Analysis Approach to Evaluate the Groundwater Quality in Jisser Diyala Area

Ramadhan, Ahmad A.; Hussian, Tariq A.; Nada, Kamal B.

doi:10.22401/jnus.20.1.02

Cited by 2 publications

(4 citation statements)

References 6 publications

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“…The maximum yield (well discharge) of (37) wells was demonstrated in figure (9) where maximum values were located in west and southwest part of the basin. Maximum yields depends on transmissivity and sedimentary facies of groundwater bearing as well as groundwater flow direction [14], taking in consideration thickness of aquifer.…”

Section: Figure (8): Water Table Contour Map Of Unconfined Aquifermentioning

confidence: 95%

“…(Nada, et.al , 2010) [8] Studied under ground water assessment in Diyala bridge area. (Ramadhan, et. al, 2017) [9] used Statistical Analysis Approach to Evaluate the Groundwater Quality in Jisser Diyala Area.…”

Section: Figure (1): Location and Topographic Map Of Khanaqin Basinmentioning

confidence: 99%

“…(Ramadhan, et. al, 2017) [9] used Statistical Analysis Approach to Evaluate the Groundwater Quality in Jisser Diyala Area. The work plan in the studied area included the following items: 1-Office work including preparing data and preliminary information of the area (wells stratigraphic columns, maps, literature reviews, scientific references, hydrogeological data bank ...).…”

Section: Figure (1): Location and Topographic Map Of Khanaqin Basinmentioning

confidence: 99%

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Groundwater System of Khanaqin Basin in Diyala Governorate – East of Iraq

Al-Sudani¹,

Ramadhan²,

Saeed³

2023

Tikrit J. Pure Sci.

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Land and water resources are generally depleting due to rapid increase in population, urbanization and industrialization. The demand has increased tremendously for these resources; hence optimal utilization of them is essential for sustainable development. The study area is located in Diyala Governorate in the east of Iraq covering 1920 km2. The hydrogeological investigation of the basin divided groundwater aquifers into two main units, the unconfined and confined aquifers, where geographical position, elevations, static water levels, depths, thicknesses, maximum yields as well as water sampling and pumping tests have been carried out during these investigations. Quaternary deposits, Bai Hassan and Mukdadiyah formations reflect the unconfined aquifer while confined aquifer consists of Mukdadiyah and Injana formations. The promising zone of unconfined aquifer is located around Khanaqin city within the southern part of the basin, while two promising zones of confined aquifer are located to western part of the basin and near the border within north part of the basin.

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Section: Figure (8): Water Table Contour Map Of Unconfined Aquifermentioning

confidence: 95%

Section: Figure (1): Location and Topographic Map Of Khanaqin Basinmentioning

confidence: 99%

Section: Figure (1): Location and Topographic Map Of Khanaqin Basinmentioning

confidence: 99%

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Groundwater System of Khanaqin Basin in Diyala Governorate – East of Iraq

Al-Sudani¹,

Ramadhan²,

Saeed³

2023

Tikrit J. Pure Sci.

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“…Using a multivariate statistical method, groundwater categorization and hydrogeochemical evaluation have recently been researched in various regions, Bangladesh [8], Latvia [9], India [10], Morocco [11], Mexico [12], USA [13], South Africa [14], China [15], Egypt [16], India [17]. The researches in Iraq used multivariate statistical analysis to evaluate the quality of groundwater, such as in Makhmor plain [18], Baghdad City [19], Jisser Diyala [20], Erbil City [21], Al -Waffa and Kubayasa regions [22], in Zuber area [23], and in Rutba Area [24].…”

Section: Introductionmentioning

confidence: 99%

Identification the Hydrogeochemical Facies of Groundwater in Rutba-Dhabaa, Western Iraq Using Multivariate Statistics Methods

Al-Heety

Al-Kubaisi

et al. 2023

IOP Conf. Ser.: Earth Environ. Sci.

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The groundwater in the Rutba-Dhabaa region in Western Iraq has been studied using multiple statistical methods. These methods proved successful in giving a hydrochemical description of water as an alternative to the Piper scheme, and therefore they can be relied upon in future studies, whether for groundwater or surface water. The groundwater in the Rutba-Dhabaa region is hard and the percentage of calcium is high, due to the type of rocks incubating that groundwater, represented by the carbonate rocks that make up the Mulussa aquifer in the study area. According to the Piper diagram, correlation matrix analysis, cluster analysis, and principle component analysis, the hydrogeochemical facies are: Class 1 (Ca2+ - Mg2+ - Cl− - SO4 2-) where the wells (W1, W4, W13, W15, W16, W17, W20) fall within the category I (SO4 2- - Cl− and Ca2+ - Mg2+) and rest of the samples falls within the category V (Mixing zone); Class 1 (Ca2+ - Mg2+ - Na+ - SO4 2-- Cl− - HCO3 −), Class 2 (Na+ - Ca2+ - SO4 2-), and Class 3 (Na+ - HCO3 −); Class 1 (Mg2+, Na+, and K+), Class 2 (HCO3 −and SO4 2-), and Class 3 (Cl− and Ca2+); and Class 1 (Mg2+, HCO3 −, and Cl−), and Class 2 (Na+, K+, and SO4 2-) respectively.

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Using Statistical Analysis Approach to Evaluate the Groundwater Quality in Jisser Diyala Area

Cited by 2 publications

References 6 publications

Groundwater System of Khanaqin Basin in Diyala Governorate – East of Iraq

Groundwater System of Khanaqin Basin in Diyala Governorate – East of Iraq

Identification the Hydrogeochemical Facies of Groundwater in Rutba-Dhabaa, Western Iraq Using Multivariate Statistics Methods

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