Global Journal of Science Frontier Research, H: Environment & Earth Science, Volume 23 Issue 1

in:Blue Issyk-Kul (wells 773.1/81), Cholpon-Ata (well 846), Issyk-Kul (wells 775, 1268), Kazakhstan (well 999), Ala-Too (well 887). Kosh-Kol, wells 1112, 1112, -A, 1375 are located 30-39 km from Rybachie. Thermal (39-42˚ C) waters are brought out on the northern shore of the lake.The flow rate of the wells is 2592, 2281, and 1296 m 3 /day, respectively, water salinity is 0.6-1.7 g/l and sodium chloride-sulfate and sulfate-chloride composition. The pH value is about 7.80 to 9.50. Silicic acid concentration is up to 40 mg/l and fluorine-12 mg/l. Tamchi. Well 1579 was drilled in 1984 in the territory of Tamchyvillage. The water flow rate is 1347, 8 m 3 /day. Water temperature is 42˚ С , pH 8.9, salinity 0.5 g/l, the composition is characterized by sodium chloride-sulfate, concentration of silicic acid 40 mg/l, fluoride 2.2 mg/l. Thermal water is used for household and domestic needs. Chock-Tal, well 1517. Drilledin 1983 with a supply of 1036 m 3 /day and used for balneological and therapeutic-drinking purposes according to indications. Water temperature is 45˚C, the reaction is alkaline (pH 9.50). In terms of composition, it belongs to the hydro- carbonate-sulfate sodium with mineralization of 0.5 g/l. The content of silicic acid is about 50-53 g/l. and fluorine 3-4 mg/l. Chon-Sary-Oy well 1543, discovered in 1981 and located on the territory of the Altyn-Kum resort. Preliminary reserve of this spring is 503.7 m 3 /day, temperature 36˚C, pH -8.90. Water is characterized by mineralization up to 0.8 g/l chloride-hydrocarbonate- sulfate composition. Silicic acid content is up to 35 mg/l and fluorine content is up to 5.0 mg/l. Well 1215 with a flow rate of 1209.6 m 3 /day and temperature of 29˚ С has a similar composition and properties of water of well 1543. Kurskoye wells 833, 1516. Well 833 was discovered as one of the first on the shore of Lake Issyk- Kul. It was drilled in the end of 1985 in the territory of the boarding house "Geologist".Wells 1516 and 833 are put into exploitation to provide household needs. Mineral water of these wells is characterized as slightly mineralized (0.9-1.9 g/l) of sodium chloride-sulfate composition and alkaline (pH 8.50-9.12).Concentration of silicic acid is in the range of 31-45mg/l, fluorine-4,2- 6,6mg/l. Preliminary water reserves for well 833-388-388 m³, and for well 1516-604.8 m³/d. Dolinkawells 888 and 1183 were opened in 1979 and 1981, of which well 888 is mothballed, and well 1183 is used for self-monitoring and for domestic needs. Approximate water reserves of the wells make respectively 259.2 m 3 /day and 224.6 m 3 /day.Water composition of these wells is the same type of sulfate- chloride sodium water with significant fluoride content (up to 9.0 mg/l) and silicic acid (up to 50 mg/l). Water temperature is within 48-49˚C with salinity of 2.2-2.9 g/l and water reaction is alkaline (pH 8.20-8, 8.55). Karabulunskoe thermal water deposit (39-50˚ С ) is located on the peninsula of the same name in the southeastern part of the Issyk-Kul depression, 15 km northwest of the Kara-Suu village. Exploration of the field was carried out in 1975-1981. Reserves amount to 3154 m 3 /day. Waters of this deposit have an alkaline reaction (pH 9.50-10.50), low mineralization in the range of 0.3- 1.2 g/l, different anionic composition. These waters are characterized by a high content of silicic acid (up to 52 mg/l) and fluorine (7.6-9.3 mg/l). Ak-Terek, well 851 was drilled in 1979 with an estimated supply of 1296 m 3 /day. The water temperature of the well is 26-27˚ С , the pH value is 8.90.The composition of this source belongs to the sulfate-chloride-hydrocarbonate sodium with a total salt content of 0.3 g/l. The Chon-Kyzyl-Suu springs, represented by three springs, are located on the northern slope of the Terskey Ala-Too ridge, in the gorge of the river of the same name, 19 km to the south of the Kyzyl-Suu village. The Chon-Kyzyl-Suu springs, represented by three springs, are located on the northern slope of the Terskey Ala-Too ridge, in the gorge of the river of the same name, 19 km to the south of the Kyzyl-Suu village. Of the three springs, two of them are captive pools with overhead wooden logs. The water of the springs is clear, clean, fresh to the taste of hydrogen sulfide. Water temperature is 32.4-43.0˚C, water reaction is alkaline (pH 9.0-9.08). The total water flow rate of the springs is about 1.5 l/sec. Their chemical composition is low- mineralized (0.4-0.5 g/l) sodium chloride-sulfate with a significant content of silicic acid (over 50 mg/l) and fluoride up to 9.5 mg/l. The Juukuchak spring is located in the river gorge of the same name, 15 km away from these springs is the village of Kyzyl-Suu. Kyzyl-Suu. The springs are used by the local population. The water of the springs is transparent, clean, fresh to the taste with a smell of hydrogen sulfide. Water temperature 32.0- 35.0˚C, alkaline water with pH 7.9-8.70, flow rate 1 l/sec. Water refers to nitric, slightly mineralized (0.3-0.4 g/l), chloride-sulfate sodium, with silicic acid 50mg/l and fluoride -7-9 mg/l. The Altyn-Arashan springs are located on the northern side of the Teskei Ala-Too ridge and are divided into three groups of springs: northern, middle and southern. These springs are characterized by the same composition. The Altyn-Arashan northern springs are located on the northern slope of the Ak-Suu river, 20-23 km southwest of Karakol. The water temperature varies from 35.5 to 43.0˚ С with a flow rate of about 1 l/sec. All the springs are captive, used for therapeutic purposes and are difficult to access. Altyn-Arashan middle springs are located upstream the Ak-Suu River southeast of Karakol and are hard to reach. Along 1000 m along the river valley 15 outlets of the springs were fixed with the total flow rate Overview of the Geothermal Sources in Kyrgyzstan 1 Year 2023 59 © 2023 Global Journals Global Journal of Science Frontier Research Volume XXIII Issue ersion I VI ( H )