DIVALENT ION CHEMISTRY AS AN INDICATOR OF GROUNDWATER FLOW TYPE THROUGH THE CARBONATE AQUIFER IN ELARISH – RAFAH AREA | ||||
| Egyptian Journal of Desert Research | ||||
| Volume 50, Issue 1, June 2000, Page 175-207 PDF (11.51 MB) | ||||
| Document Type: Original Article | ||||
| DOI: 10.21608/ejdr.2000.450170 | ||||
 View on SCiNiTO | ||||
| Author | ||||
| M. H. El Sayed* | ||||
| Desert Research Center, Matareya, Cairo, Egypt | ||||
| Keywords | ||||
| Hydrogeochemistry; Carbonate aquifers; Arish–Rafah; Divalent ion chemistry; flow type; Variation coefficient; Total hardness; Temporary hardness; Permanent hardness; Leaching and dissolution process; Cation exchange | ||||
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