Cross-formational rising groundwater at an artesian karstic basin: the Ayalon Saline Anomaly, Israel
- Permanent Link:
- Cross-formational rising groundwater at an artesian karstic basin: the Ayalon Saline Anomaly, Israel
- Series Title:
- Journal of Hydrology
- Frumkin, Amos
- Publication Date:
- Subjects / Keywords:
- Groundwater ( local )
Rising Water ( local )
H2s ( local )
Confined Karst ( local )
Maze Caves ( local )
Yarkonâ€“Taninim Aquifer ( local )
- serial ( sobekcm )
- It is proposed that a geothermal artesian karstic system at the central part of the Yarkonâ€“Taninim aquifer creates the â€˜Ayalon Saline Anomalyâ€™ (ASA), whose mechanism has been under debate for several decades. A 4-year-long detailed groundwater monitoring was carried out at 68 new shallow boreholes in the Ayalon region, accompanied by a comprehensive survey of karstic voids. Results indicate the rising of warm-brackish groundwater through highly permeable swarms of karstic shafts, serving as an outflow of the artesian geothermal system. The ASA area contains â€˜hot spotsâ€™, where groundwater contrasts with â€˜normalâ€™ water hundreds of meters away. The ASA temperature reaches 30 °C (âˆ¼5 °C warmer than its surroundings), chloride concentration reaches 528 mg/l (50â€“100 mg/l in the surrounding), H2S concentration reaches 5.6 mg/l (zero all around) and pH value is 7.0 (compared with 7.8 around). Subsequently, the hydrothermal water flows laterally of at the watertable horizon through horizontal conduits, mixing with â€˜normalâ€™ fresh water which had circulated at shallow depth. Following rainy seasons, maximal watertable rise is observed in the ASA compared to its surroundings. Regional hydrogeology considerations suggest that the replenishment area for the ASA water is at the Samaria Mountains, east of the ASA. The water circulates to a great depth while flowing westward, and a cross-formational upward flow is then favored close the upper sub-aquifer's confinement border.
- Original Version:
- Journal of Hydrology, Vol. 318, no. 1-4 (2006-03-01).
- Source Institution:
- University of South Florida Library
- Holding Location:
- University of South Florida
- Rights Management:
- This object is protected by copyright, and is made available here for research and educational purposes. Permission to reuse, publish, or reproduce the object beyond the bounds of Fair Use or other exemptions to copyright law must be obtained from the copyright holder.
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