TY - JOUR
T1 - Factors affecting groundwater chemistry in regional arid basins of variable lithology
T2 - Example of Wadi Umairy, Oman
AU - Abdalla, Osman
AU - Al-Abri, Rashid bin Yahya
N1 - Funding Information:
Acknowledgments The study was financed by project SR/SCI/ ETHS/11/01 provided by His Majesty Trust Fund (HMTF). Thanks are also due to MRMWR for providing required data.
PY - 2014/7
Y1 - 2014/7
N2 - Understanding factors influencing groundwater chemistry in regional groundwater basins is important to prevent groundwater pollution especially in arid areas where rainfall is low and water resources are limited. The present study assesses such factors in the regional, geologically diverse, groundwater basin of Wadi Umairy in Oman. The basin is composed of five different lithostratigraphic units with different hydraulic properties. Water samples (41) have been collected from the different units and analyzed for the major ions. Factor analysis and conventional hydrochemical methods were used to define the factors that have significant impact on the aquifer's hydrochemistry. It was found that evaporation and mineral weathering/dissolution are the main factors defining the groundwater chemistry along the flow path from recharge to discharge zones, whereas anthropogenic activities and alkalinity are found to be of lesser effect, and the latter prevails when the rocks are predominantly monomineralic. It was concluded that in regional groundwater basins, recharge/discharge relations together with the flow scale control the hydrochemistry irrespective of lithological variation in the basin.
AB - Understanding factors influencing groundwater chemistry in regional groundwater basins is important to prevent groundwater pollution especially in arid areas where rainfall is low and water resources are limited. The present study assesses such factors in the regional, geologically diverse, groundwater basin of Wadi Umairy in Oman. The basin is composed of five different lithostratigraphic units with different hydraulic properties. Water samples (41) have been collected from the different units and analyzed for the major ions. Factor analysis and conventional hydrochemical methods were used to define the factors that have significant impact on the aquifer's hydrochemistry. It was found that evaporation and mineral weathering/dissolution are the main factors defining the groundwater chemistry along the flow path from recharge to discharge zones, whereas anthropogenic activities and alkalinity are found to be of lesser effect, and the latter prevails when the rocks are predominantly monomineralic. It was concluded that in regional groundwater basins, recharge/discharge relations together with the flow scale control the hydrochemistry irrespective of lithological variation in the basin.
KW - Arid areas
KW - Evaporation
KW - Factor analysis
KW - Hydrochemistry
KW - Oman
KW - Weathering
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U2 - 10.1007/s12517-013-0981-7
DO - 10.1007/s12517-013-0981-7
M3 - Article
AN - SCOPUS:84902830064
SN - 1866-7511
VL - 7
SP - 2861
EP - 2870
JO - Arabian Journal of Geosciences
JF - Arabian Journal of Geosciences
IS - 7
ER -