2017
DOI: 10.1016/j.jafrearsci.2017.07.005
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Recharge sources and hydro geochemical evaluations of Na2SO4 deposits in the Acıgöl Lake (Denizli, Turkey)

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Cited by 3 publications
(2 citation statements)
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“…The lake receives spring water primarily characterized by high Na 2 SO 4 and NaCl values, with a total flow of 1140 L/s [69] that enters the lake from a fault line on the southern side (Figure 11). Lake Acıgöl is the source of more than 85% of the anhydrous Na 2 SO 4 production of Turkey (400,000 tons in the late 1990s) [70]. The lake had a surface area of 160 km 2 and a maximum depth of 8 m until the mid-1970s before the soda production operations started in the region [71].…”
Section: Lake Acıgölmentioning
confidence: 99%
“…The lake receives spring water primarily characterized by high Na 2 SO 4 and NaCl values, with a total flow of 1140 L/s [69] that enters the lake from a fault line on the southern side (Figure 11). Lake Acıgöl is the source of more than 85% of the anhydrous Na 2 SO 4 production of Turkey (400,000 tons in the late 1990s) [70]. The lake had a surface area of 160 km 2 and a maximum depth of 8 m until the mid-1970s before the soda production operations started in the region [71].…”
Section: Lake Acıgölmentioning
confidence: 99%
“…In fact, the major ions in salt water are the same as those in freshwater, Na + , K + , Ca + , Mg + , Cl -, SO4 2and CO3 2-, but the ionic proportions are different. In salt lakes, Na + and Clare the dominant ions, while HCO3is the dominant ion in freshwater lakes (Kuşcu et al, 2017).…”
Section: Introductionmentioning
confidence: 99%