Kukkarahalli lake
| Kukkarahalli Lake | |
|---|---|
 |
|
| Location | Mysore |
| Coordinates | 12°18′N 76°38′E / 12.3°N 76.63°ECoordinates: 12°18′N 76°38′E / 12.3°N 76.63°E |
| Type | Freshwater Kukkarahally- Recreational and Fisheries |
| Catchment area | 414 km2 (160 sq mi) |
| Basin countries | India |
| Surface area | 62 ha (150 acres) |
| Max. depth | 5 m (16 ft) |
| Water volume | 2.53×106 m3 (89×106 cu ft) |
| Shore length1 | 5 km (3.1 mi) |
| Surface elevation | 755.73 m (2,479.4 ft) |
| Settlements | Mysore |
| 1 Shore length is not a well-defined measure. | |
Kukkarahalli Lake also called Kukkarhalli Kere (Lake is ‘’kere’’ in local Kannada language), located in the heart of the Mysore city, adjoins the Manasgangotri (University of Mysore), the Kalamandir (Rangyana) and the Central Food Technological Research Institute (CFTRI) campus (separated by the Hunsur Road). It provides lung-space to the city. Mummadi Krishnaraja Wodeyar, (1794–1868) of the Mysore Dynasty (Kingdom of Mysore) was responsible for getting the lake created, in the year 1864, to provide water for irrigation to about 4000 ha (10,000 acres) of land outside the city. The Lake also used to be a source of water supply to the city of Mysore but over the years, sewage and excessive land encroachments (mostly illegal) and blockage of water flow sources almost led to the eutrophication of the lake. The University of Mysore and the citizen forums of Mysore continue to make efforts to preserve the lake by implementing several remedial measures. There is a 4.5 km walkway on the periphery of the lake with shaded stone benches for visitors to sit, relax and enjoy the scenic serenity of the lake.
The lake is located within the Mysore city limits. The Mysore City railway station is about 3 km (1.9 mi) from the Lake. The nearest airport is at Mysore, at a road distance of 15 km (9.3 mi).
The lake drains a catchment area of more than 414 square kilometres (160 sq mi) and the water body spreads over 62 hectares (150 acres). Dewan Poornaiah feeder canal, 27 km (17 mi) long, which passes through Hinkal, Bogadi, Kudremala and Manasagangotri outfalls into the Lake. The Lake is ‘J’ shaped. The maximum depth of lake is reported to be 5 m (16 ft). The east-west bund holds water on one side. Sandy loam to clay loam form the dominant geological condition of the Lake. On the northern side another temporary bund hold back the direct flow of waste water into the lake.
The highest flood level in the lake is 755.73 m (2,479.4 ft).
A detailed study of the physico-chemical and bio-chemical parameters of the lake waters carried out in the period 1981-2001 confirmed the deteriorating status of the lake necessitating action for restoration. There was a high percentage of chemicals but low percentage of total plankton (43%). The activity of chemicals lead to the liberation of extra quantity of cellular products which increased to 53.19%. Lake indicated high productivity of bio-chemical products; with death and decay of algal blooms adding to the biochemical concentration. The lake waters showed high electrolytes, low dissolved oxygen, high phosphate and nitrogen content with abundance of plankton blooms, all of which have contributed to a high degree of eutrophication. The non potability of the water body is indicated by the high degree of faecal contamination with organisms that produce H2S that may include forms of Salmonella, Proteus, Citrobacter and some strains of Klebsiella. The distribution pattern of plank tonic forms, for the decade ending 2001, as per laboratory tests of lake’s water samples provides the values of parameters such as the Chlorococcales, Desmids, Diatoms, Blue-greens and Euglenoids, as the biological indicators of water body, as given in table below which testify to the lake’s eutrophication status. The numbers indicate the microorganisms present in the sample per litre.
...
Wikipedia