Statistical analysis of the hydro-geochemical evolution of groundwater in the aquifers of the Yarmouk basin, North Jordan
Autor: | Iyad Ahmed Abboud |
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Rok vydání: | 2018 |
Předmět: |
Pollution
Hydrology geography Topsoil geography.geographical_feature_category Brackish water media_common.quotation_subject 0208 environmental biotechnology Aquifer 02 engineering and technology 010501 environmental sciences Structural basin 01 natural sciences 020801 environmental engineering Salinity General Earth and Planetary Sciences Environmental science Leaching (agriculture) Groundwater 0105 earth and related environmental sciences General Environmental Science media_common |
Zdroj: | Arabian Journal of Geosciences. 11 |
ISSN: | 1866-7538 1866-7511 |
DOI: | 10.1007/s12517-018-3448-z |
Popis: | The aim of this study is to determine the main factors affecting the quality of groundwater and its changes through hydro-geochemical analysis and statistical studies. Therefore, hydro-geochemical properties of groundwater are analyzed as Ca2+, Mg2+, Na+, K+, HCO3−, Cl−, NO3−, SO42−, and F− as well as their statistical data. Correlation, cluster, and factor analyses were applied on 1322 groundwater samples collected from 148 wells distributed through Yarmouk basin region, North Jordan. Clusters analysis shows two groups of ionic concentrations. Cluster 1 includes 37% of the total samples and classified as brackish and unsuitable water, while 63% follows cluster 2 and is classified as moderately soft and suitable water. Factor analysis tends to increase concentration and spread of Ca2+, Mg2+, Na+, K+, Cl−, and SO42− in the groundwater through factor 1 which reflects the high salinity as a result of over-pumping, weathering processes, and salts leaching from the top soil. Cluster 2 shows high concentrations of NO3− in groundwater as a result of the pollution due to agricultural and industrial human activities. Factor scores suggest the main hydro-geochemical zones in the study area, which are distributed in the northern, eastern, and south-eastern parts, which recorded an increase of Cl− (high salinity areas). The western region appears to increase in nitrate and chlorine concentrations (high level of salinity), while hardness factor spreads across the northern and southern parts of the study area. |
Databáze: | OpenAIRE |
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