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Carbon-13 and Carbon-14 isotopes were utilized in this study to determine the age, flow direction, flow velocity and recharge area of groundwater in the two main aquifers of Kuwait. For this purpose 20 groundwater samples were collected from the Kuwait group aquifer and lower Dammam formation aquifer. The collected groundwater samples were analyzed for 14 C activity and 13 C activity. 14 C activity was measured using accelerator mass spectrometry (AMS) and expressed as percentage modern carbon (pmc) while 13 C was measured using an isotope ratio mass spectrometer (IRMS) and expressed as permil (‰) in the form of CO 2 gas. The interpretation of the analysis results of carbon isotopes data indicated that the general groundwater flow direction is towards north east and the estimated groundwater velocities are 11 to 30 m/a for Kuwait group aquifer and 12 to 21 m/a for Dammam formation aquifer. Based on the estimated groundwater velocities, the approximate location of the recharge areas of these aquifers was identified. The groundwater ages calculated for Kuwait group aquifer varied from 800 a B.P for modern ground water in the northern part to 22500 a B.P for very old groundwater in the northeastern part, while the age of Dammam formation groundwater is 26000 to 36000 a B.P. [ABSTRACT FROM AUTHOR]

Residential areas of Kuwait have been affected by rising groundwater levels for many years. The main reason for this problem is the increased recharge derived from the excessive irrigation of gardens and parks, and leaks from sewage networks, where the hydraulic characteristics of the lithology play an important role in intensifying the impacts of this phenomenon at local scale. The objective of this paper is to assess the hydrological conditions of Al-Qurain residential area to identify the extent and the causes of the water rise problem. A total of 25 wells of various depths were drilled, constructed and sampled at the study area. Water level loggers installed in the drilled wells indicated that water levels are fluctuating on daily bases and increasing up to 50 cm during winter months due to the reduction of evapotranspiration and recharge from rainfall. Combining the water level records and the results of the isotopic, chemical and biological analysis, it was concluded that the top 20 m of the aquifer water is made up of mostly irrigation, waste and rain water in addition to the aquifer groundwater. It was also observed that the intruding water from lower Dammam aquifer is dominating the aquifer beneath 40 m depth. This conclusion along with the steep topography of the area explained why this area is naturally prone to water rise. The study recommended the utilization of integrated system of dewatering wells along with desalination units to lower the water level and re-utilize the groundwater. On the prevention side, it is recommended to conduct an awareness campaign that educate the residents of the impacts of over use of water on their own properties. [ABSTRACT FROM AUTHOR]

Numerical modeling of the recovery of moisture by injecting warm air in the unsaturated zone in a 100 m × 100 m plot of agricultural land in Kuwait, a country located in an arid environment, was conducted to provide "proof of concept" of the technique. If technically and economically feasible, it will be a potential additional source of water that could be exploited for farming activities and other uses. The COMSOL software was used to develop the model and, based on the results of the scenario runs, the effects of different hydraulic and operational parameters, including that of well spacing, on moisture recovery were assessed. In general, the results suggested that the recovery should increase with the increase in the hydraulic conductivity of the unsaturated zone, the amount of heat input, and the pressure differential between the unsaturated zone and the well head. Within the period examined (0 to 11 days), the recovery decreases with the increase in the soil moisture content, possibly due to the fall in relative permeability to moisture-rich air with the increased water contents in the pore spaces, although the effects may change over a longer period as water contents decrease with moisture recovery. The moisture recovery from the unsaturated zone through the injection of warm air appears to be a feasible proposition from this study that should be demonstrated through a pilot scale experiment in the field., (© 2024 National Ground Water Association.)

Farm-scale desalination units are gaining popularity for agricultural irrigation in arid countries, such as Kuwait to meet freshwater demands. However, less attention has been given to the management of environmentally hazardous brine reject water they produce. In this study we investigated the fate of brine water produced by the inland desalination units on the underlying aquifers using numerical modelling and field investigations. The methodology involved developing groundwater flow and solute transport models using Flex VMF-SEAWAT to simulate the movement of reject brine. The field investigations included collecting 150 water samples and conducting pumping tests on newly drilled wells. This numerical simulation considered advection, dispersion, and adsorption processes with variable groundwater density following rigorous validation and calibration of the developed numerical models. The results show that the RO reject brine will significantly increase groundwater salinity, exceeding 10,000 mg/L when accounting for advection, dispersion, and adsorption processes. The sustainable yield of the aquifer, with a salinity of <10,000 mg/L, averages 500 Mm 3 but is expected to be depleted within 16 years with the current extraction rate. The resulting hydraulic properties are favourable with K about 100 m/d, T > 1000 m 2 /day, and Sy just >0.1. The adopted values for dispersivity and adsorption coefficients for chloride and sulphate salts in the aquifer were 10 m and 1 × 10 -7 [mg/L] -1 respectively. Chemical and numerical analyses indicate a mixing ratio between the reject brine and groundwater in the study area of approximately 10 %. Uncontrolled groundwater extraction, combined with the surface disposal of RO reject brine, has led to a significant decline in groundwater levels and an increase in the salinity. The adsorption ratio of simulated brine plume was 13 %. The authors recommend to dispose the RO reject water in a safe location or transfer it to the nearest wastewater treatment plant for proper treatment and reuse., Competing Interests: Declaration of competing interest The authors declare the following financial interests/personal relationships which may be considered as potential competing interests: Harish Bhandary reports financial support was provided by Kuwait Foundation for the Advancement of Sciences. Harish Bhandary reports a relationship with Kuwait Foundation for the Advancement of Sciences that includes: funding grants. If there are other authors, they declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2024 Elsevier B.V. All rights reserved.)

Kuwait Group aquifers and Dammam Formation are the two prominent aquifers, the wells tapping Dammam Formation and Dual completion wells are used for groundwater production. The current study investigates the spatiotemporal evolution of hydrochemical characteristics of the Shagaya water field utilizing long-term (1975-2019) hydrochemical data from 116 water wells. The Shagaya water well field has been differentiated into A to F sub-Fields. Mann-Kendall and Sen's Slope method along with spatial interpolation of change in TDS with time identified a significant decrease in TDS with time in the major portions of the Shagaya B, C, D, and E Fields. The study infers that 82% of wells extracting water from the Dammam Formation and 42% of Dual completion wells show a decrease in TDS concentration. The most plausible explanation for this phenomenon was the inflow of better-quality water from the up gradient parts of the Kuwait Group and the Dammam Formation aquifers due to the fall in the potentiometric head with high volume production in the well field. The results of ionic ratios (Na/Cl, Ca/Mg, Ca/SO 4 , Ca + Mg/SO 4 +HCO 3 ), isotopes ( 34 S, 87 Sr/ 86 Sr), relationships between 2 H and 18 O, and Ne/He and 3 He/ 4 He ratios identified that salinization was due to the result of rock-water interaction, ion exchange, mixing between groundwater of Kuwait Group and Dammam Formation and with groundwater from deeper parts of the aquifer. The long-term analysis of the data shows a notable variation of chemistry in a few locations and thus the study helps to manage, sustain groundwater resources, and protection of host aquifers., Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2022. Published by Elsevier Ltd.)

The sea water serves as a source for desalination and shelter for dependent biota. To understand the sources of metal in Kuwait Bay and the open sea, samples were collected and analyzed for metals like B, Li, Sr, Hg, Pb, Ba, Fe, Zn, Mn, Be, Cd, Co, Cr, Ni, Se, V, Al, Mo, and As. The comparison of Bay and Seawater shows that most of the metals were higher in sea water. Samples were collected in two different transects in the territorial sea water (TSW), the northern, and the southern transects. The heavy metal evaluation index and degree of contamination calculated for Bay and TSW show that they are contaminated, and the degree was higher in TSW. The variation of metal concentration along the transects in TSW reflects three different behaviors; (1) few metals decrease from the shore, (2) few increases from the shore, and (3) others show no significant trend. The statistical analysis of the data shows a representation of five factors for bay water and six for TSW indicating the complexity in sources of metal in TSW. The analysis infers the metal contamination due to petroleum products, and oxidation-reduction cycles are predominant in TSW. But, tidal influence along with dustfall plays a key role in the metal contamination of bay waters. Apart from these, desalination rejects and domestic sewage effluents are common sources contributing metals to both the environment. It is also observed that the suspended sediments play a significant role in the leaching, adsorption, and distribution of metals. The extraneous process has a predominant control over the distribution of the metals in TSW than the Bay.