A STUDY OF SPRING WATER QUALITY AND ITS SUITABILITY FOR DIFFERENT USES IN THE AREA OF BARTELLA – EASTERN MOSUL
| Autor: | Mohammed A. M. Sulaiman, Asaad A. M. AL-Hussein, Alaa S. Saleh |
|---|---|
| Rok vydání: | 2020 |
| Předmět: |
Gypsum
Tarjla village lcsh:Mechanical engineering and machinery General Physics and Astronomy chemistry.chemical_element 02 engineering and technology engineering.material water use 01 natural sciences physical and chemical properties Human use Spring (hydrology) lcsh:TJ1-1570 springs water Animal use Hydrology geography geography.geographical_feature_category tarjla village 010401 analytical chemistry General Engineering 021001 nanoscience & nanotechnology Sulfur lcsh:QC1-999 0104 chemical sciences Time factor chemistry Soil water engineering Environmental science Water quality 0210 nano-technology lcsh:Physics |
| Zdroj: | EUREKA: Physics and Engineering, Iss 3, Pp 87-96 (2020) |
| ISSN: | 2461-4262 2461-4254 |
| DOI: | 10.21303/2461-4262.2020.001257 |
| Popis: | The water of the three springs in the village of Tarjla (located in the area of Bartala, eastern Mosul) is characterized by different physical and chemical properties depending on the results of the laboratory tests of (NTU, EC, TDS, TH, PH) and major ions (Na+, Ca+2, Mg+2, Cl-, ) for six selected water samples for the study area. This difference did not remain constant, but changed with the flow of water to the neighboring villages (Sheikh Amir, Shaquli, Karemlesh), where the percentages of physical and chemical concentrations have changed in terms of the increase and decrease of some water samples. This is due to the time factor and the water contact of some of the soils and rocks that encountered their flow as well as exposure to the sun. The purpose of the research is to study the quality of springs water to determine its suitability for different uses. Using the Piper and Stiff classifications, the water quality is calcium-bicarbonate, the calcium ion predominates over the rest of the positive ions and the bicarbonate ion prevails over the rest of the negative ions, this indicates that spring number (1) and spring number (3) are derived from the Fat'ha formation deposits, which contain limestone and gypsum rocks that contain high concentrations of sulphates. The spring number (2) is derived from the Injana formation and modern sediments that is hydraulically connected with each other and can be considered one reservoir. By comparing the results of laboratory tests with the international standards, it was found that the water of spring number (2) is suitable for human use, and that the water of spring’s number (1) and (3) are not suitable for human use because they contain a high proportion of sulfur ions. All water samples are suitable for agricultural and animal use and very good to excellent |
| Databáze: | OpenAIRE |
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