Wild - a lake located in the valley of the Byura River, 15 km north of the city of Sorsk in the territory of the Khogassia Bogradsky district .
| Lake | |
| Wild | |
|---|---|
| Morphometry | |
| Area | 0.3 km² |
| Deepest | 7 m |
| Location | |
| A country |
|
| The subject of the Russian Federation | Khakassia |
| Area | Bogradsky district |
Length - 900 m, width - 440 m, area - 0.3 km², depth - up to 7 m. It has an oval shape, is suspended. Mineralization of water 0.3 g / dm3, waste. Basin of tectonic origin. At the bottom there are outlets of radon waters confined to the deep crushing zones of sedimentary-metamorphic deposits, pressureless, fresh water, t ° +4 ° C, hydrocarbonate - sulphate , calcium, mineralization does not exceed 0.7 g / liter, occur at a depth of more than 80 m
The vicinity of the lake is a zone of unorganized recreation for the population of the Republic of Khakassia and the Krasnoyarsk Territory. Along the shores - mixed forest (pine, larch, birch).
Dikoozerskoye field of radon waters
It is located 10 km north-east of the city of Sorsk, in the immediate vicinity of the Tumanny railway station of the Abakan - Achinsk branch. Exploration work was carried out in 1978 - 1980 , 1983 - 1985 . The field is confined to the crushing zone. The host rocks are represented by graphite-clay and siliceous schists. Non-pressure water. The depth of the aquifer is 100 m, the thickness is 30 m, and the filtration coefficient is 0.7 m / day. According to the chemical composition of the water, hydrocarbonate-sulphate, calcium-magnesium, with a salinity of 0.6-0.7 g / l. The radon content is 66 nCi / l. Radon waters are localized within the zones of fracture and are characterized by a limited focal distribution. Sources of formation of operational reserves are mainly natural resources. The main component of the field, determining its balneological value, is radon. Microcomponents, standardized by GOST 13273-73, are contained in small quantities. Non-normalized microcomponents are represented by copper , zinc , manganese, strontium, silver , titanium , nickel, bismuth , barium. Their content varies over a wide range and does not exceed 100 μg / L. Of the specific elements that enhance the balneological effect of water, there is total iron in quantities from units of μg / l to 20.3 μg / l. The operational reserves of radon water of medium concentration are approved by the State Reserves Committee of the USSR in the amount of 265 m³ / day. The balneological value of radon waters is confirmed by the Tomsk Scientific Research Institute of Balneology. Radon waters are recommended for external use only. According to the results of bacteriological analyzes, the water meets the requirements of GOST 2874-82 and refers to the Khusartaevsky type. The closest analogues are the Lipovskoye and Kolyvansko deposits. Since 1989, the Tumanny sanatorium has been operating on the basis of proven reserves. Waters are used heated in the form of bathtubs for the treatment of diseases of joints, bones, muscles, the nervous system, gynecological, skin and cardiovascular diseases.
Literature
- Encyclopedia of the Republic of Khakassia: [in 2 volumes] / Government Rep. Khakassia [scientific ed. Advice: V. A. Kuzmin (previous) and others.]. - Abakan: Polikor, 2007. T. 1: [A - H]. - 2007. - 430, [2] p. : ill., portr. - Bibliogr. at the end of words. Art. - S. 179.