Mitigation of saltwater intrusion by ‘integrated fresh-keeper’ wells combined with high recovery reverse osmosis

Abstract

Most countermeasures to mitigate saltwater intrusion in coastal, karstic or fractured aquifers are hindered by anisotropy, high transmissivities and complex dynamics. A coupled strategy is introduced here as a localized remedy to protect shallow freshwater reserves while utilizing the deeper intercepted brackish water. It is a double sourcing application where fresh-keeper wells are installed at the bottom of a deepened borehole of selected salinized wells, and then supported by high recovery RO desalination. The RO design has <1kWh/m energy consumption, and up to 96% recovery in addition to low scaling propensity without use of any anti-scalant. A feasibility study is presented as an example for a salinizing, brackish well (TDS ~1600mg/L) in the Damour coastal aquifer in Lebanon. The concept is expected to produce ca. 1000m/d of freshwater from this well by pumping 250m/d of fresh groundwater from the top well screen and 800m/d of brackish groundwater (to be later desalinized) from the fresh-keeper well screen below. Cost analysis shows that the capital cost could be returned back in 1 to 4years depending on the choice of produced water (bottled or tap) and available market. As an alternative, water from the RO plant could be blended with lower quality water, for instance untreated brackish groundwater (if unpolluted), to supply 3 more volumes for domestic use. The usage of brackish groundwater from integrated fresh-keeper wells thus serves 3 purposes: production of high quality drinking water, financial gain and mitigation of water stress by overpumping.

Distributed Temperature Sensing to Measure Infiltration Rates Across a Groundwater Recharge Basin

“…For comparison, Lake Elsinore, southern California's largest natural lake, can store 51.4 × 10 6 m 3 (41,700 acre‐feet) and Lake Shasta, California's largest reservoir, can store 5.6 × 10 9 m 3 (4.5 million acre‐feet). Furthermore, storing water in groundwater aquifers reduces evaporation losses (Kazner et al 2012), prevents saltwater intrusion in coastal regions (Sherif and Hamza 2001; Khadra et al 2017), and improves water quality through soil aquifer treatment (Drewes 2009; Dillon et al 2010; Fox and Makam 2011).…”

Problems and promise of managed recharge in karstified aquifers: the example of Lebanon

“…Figure 3The common types of managed aquifer recharge (modified after W.M Khadra, Stuyfzand, & Khadra, 2017a)…”