Evaluation the Water Quality for Water Bottles in Some Provinces in Iraq

Hammood, Zahraa Ali; Al-Khafaji, Zainab S.; Al-Naely, Halah K.

doi:10.5373/jardcs/v11sp12/20193338

Cited by 8 publications

(1 citation statement)

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“…The results indicate to lack of interaction between the groundwater and river, with no interaction between Sawa lake and groundwater. Al-Hadithi (2018) studied the interaction between groundwater-surface waters in Baghdad using the stable isotopes as a comparison with the isotope of groundwater, rainwater, and the Tigris river proved that the groundwater is a mixture of the Tigris river water and rainwater (Hammood et al, 2019). In Fallujah-Anbar area, the study on isotope technology was conducted to determine flow direction, recharge areas, and the relative age of groundwater.…”

Section: Introductionmentioning

confidence: 99%

Surface Water-Groundwater Interaction in Diwaniya, Southern Iraq Using Isotopic and Chemical Techniques

Hadi¹

2020

IGJ

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The stable isotopes of 2 H, 18 O, and 3 H reinforced by hydrochemical data, were used to identify the interaction between groundwater and Shatt Al-Diwaniya water and estimate the age of groundwater in the research area. For achieving these two goals, twenty-two samples of water were collected at the suggested area through a sampling campaign for twelve shallow wells, three from Shatt Al-Diwaniya, six rainfall samples, and one sample of sewer water. Three additional samples were collected for comparison from outside of the study area. The results of stable isotopes and hydrochemical composition indicated that there is a similarity between shallow groundwater samples and Shatt Al-Diwaniya water. The surface water interacts with groundwater for all boreholes, except for the borehole in the Al-Jameih District (WR2), which showed similar results spring water as comparing with SW1 and SW2 spring water samples. The isotopic composition of Shatt Al-Diwaniya (2 H and 18 O) is close to the local, and meteoric global water line, this indicates that the rainfall makes a significant contribution to the water of Shatt-Aldiwaniya. There is a convergence with the values of isotopes of wastewater and groundwater, which indicates that the formation of shallow groundwater is a mixture of Shatt Al-Diwaniya water and the recharge (wastewater and rainfall). The results of 3 H concentration remaining in shallow groundwater showed that the age of the groundwater ranges from1.8 to 6.3 years, this indicates that recharge of shallow groundwater is modern.

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Section: Introductionmentioning

confidence: 99%