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Hydrogeochemical and isotopic characteristics of water resources in Cubuk-Meliksah (Ankara/Turkey)

机译:古克 - 梅丽西亚(Ankara / Turkey)水资源资源的水力代科学和同位素特征

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摘要

In this study, the chemical characteristics, isotopic compositions (delta O-18, delta H-2), geothermal properties, and suitability for irrigation of groundwater resources were explored in Cubuk-Melikah (Ankara/Turkey). Water types present in the study area were mainly CaMgHCO3 and NaHCO3, with isotope compositions ranging from -10.6 to -9.06 for delta O-18 and from -75.62 to -61.93 for delta H-2. The mineral saturation index showed that samples were saturated with respect to aragonite, calcite, and dolomite, while anhydrite and gypsum were undersaturated. Reservoir temperatures, computed from silica geothermometers were 60-75 degrees C for Melikah thermal water. Based on the sodium adsorption ratio, residual sodium carbonate, soluble sodium percentage, permeability index, sodium percentage, boron and electrical conductivity values, waters examined in the study area were generally considered to be suitable for irrigation purposes.
机译:在该研究中,在古克 - 梅利科(安卡拉/土耳其)探讨了化学特性,同位素组合物(Delta O-18,Delta H-2),地热性能和对地下水资源灌溉的适合性。 研究区域中存在的水类型主要是CAMGHCO3和NaHCO 3,同位素组合物为ΔO-18的-10.6至-9.06,ΔH-2的-75.62至-61.93。 矿物饱和度指数显示,样品相对于树脂,方解石和白云石饱和,而无水晶和石膏是不饱和的。 从二氧化硅地热水计算的水库温度为60-75摄氏度。 基于钠吸附率,残留碳酸钠,可溶性钠百分比,渗透率指数,钠百分比,研究区域中检测的水域通常被认为适用于灌溉目的。

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