Abstract
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.
| Original language | English |
|---|---|
| Pages (from-to) | 2861-2870 |
| Number of pages | 10 |
| Journal | Arabian Journal of Geosciences |
| Volume | 7 |
| Issue number | 7 |
| DOIs | |
| Publication status | Published - 2014 |
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Keywords
- Arid areas
- Evaporation
- Factor analysis
- Hydrochemistry
- Oman
- Weathering
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Cite this
Factors affecting groundwater chemistry in regional arid basins of variable lithology : Example of Wadi Umairy, Oman. / Abdalla, Osman; Al-Abri, Rashid bin Yahya.
In: Arabian Journal of Geosciences, Vol. 7, No. 7, 2014, p. 2861-2870.Research output: Contribution to journal › Article
}
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
PY - 2014
Y1 - 2014
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
UR - http://www.scopus.com/inward/record.url?scp=84902830064&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84902830064&partnerID=8YFLogxK
U2 - 10.1007/s12517-013-0981-7
DO - 10.1007/s12517-013-0981-7
M3 - Article
AN - SCOPUS:84902830064
VL - 7
SP - 2861
EP - 2870
JO - Arabian Journal of Geosciences
JF - Arabian Journal of Geosciences
SN - 1866-7511
IS - 7
ER -