Surface water salinity ranges from 32 to 37 parts per 1000
I think that as the salinity increases, density increses. The minerals that contribute to the salinity of sater, such as sodium and chloride, are denser that water. Thus, when the dense particles are added, the density of the water increases I think that as the salinity increases, density increses. The minerals that contribute to the salinity of sater, such as sodium and chloride, are denser that water. Thus, when the dense particles are added, the density of the water increases
Nohkalikai Falls is the tallest WATER FALL in INDIA, its height of 335 metres (1100 ft).The waterfall is located near Cherapunji, one of the wettest places on Earth.
India has many lakes. These differ from each other in the size, and other characteristics. Most lakes are permanent; some contain water only during the rainy season, like the lakes in the basins of inland drainage of semi-arid regions. There are some of the lakes which are the result of the action of glaciers and ice sheets, while the others have been formed by wind, river action, and human activities. A meandering river across a flood plain forms cut-offs that later develop into ox-bow lakes. Spits and bars form lagoons in the coastal areas, eg the Chilika lake, the Pulicat lake, the Kolleru lake. Lakes in the region of inland drainage are sometimes seasonal; for example, the Sambhar lake in Rajasthan, which is a salt water lake. Its water is used for producing salt. Most of the fresh water lakes are in the Himalayan region. They are of glacial origin. In other words, they formed when glaciers dug out a basin, which was later filled with snowmelt. The Wular lake in Jammu and Kashmir, in contrast, is the result of the tectonic activity. It is the largest freshwater lake in India. The Dal lake, Bhimtal, Nainital, Loktak and Barapani are some other important fresh water lakes. Apart from natural lakes, the damming of the rivers for the generation of hydel power has also led to the formation of Lakes such as Guru Gobind Sagar (Bhakra Nangal Project)
In India, wherever surface water from rivers is drawn for drinking water purpose, there is a full-scale water treatment plants of varying capacities. Besides, where sea water is used as raw water, desalination water treatment plants are also put up. In areas affected specifically by ground water pollutants like fluoride, arsenic, iron, salinity, there also corresponding water treatment plants are available in the country to bring down the pollutants' level within permissible limits. If the question is still more specific about the interest in water treatment plants in India, it would be easy to answer to the point with relevant details. OK?
The highest levels of salinity are found in hypersaline ecosystems such as salt flats, salt lakes, and salt ponds. These environments often have extremely high concentrations of salt due to evaporation of water, leading to conditions that are too harsh for many organisms to survive.
In regards to body of water, the highest amount on salinity can be found in Lake Don Juan in Antarctica.
Salinity can be categorized into several types, including: Seawater Salinity: The average salinity of ocean water, typically around 35 parts per thousand (ppt). Brackish Water Salinity: A mix of freshwater and seawater, with salinity levels between 1 and 30 ppt, commonly found in estuaries. Hypersaline Salinity: Extremely high salinity levels exceeding 40 ppt, often found in evaporation ponds or certain salt lakes. Freshwater Salinity: Water with very low salinity, usually less than 0.5 ppt, typical of rivers and lakes.
Surface water has the highest salinity, however it is also the warmest, and because temperature has more effect on the density than the salinity, it rises to the top.
Temperature and salinity affect the density of water, which in turn affects its stability. Cold water is denser than warm water, so temperature differences can lead to stratification and stability issues. Salinity also affects density, with higher salinity water being denser. This can drive vertical mixing or stratification patterns in oceans and lakes.
Two natural processes that increase salinity are evaporation and the inflow of saline water. Evaporation removes water from oceans and lakes, leaving behind dissolved salts and increasing salinity. Additionally, the inflow of saline water from sources like rivers, groundwater, or seawater intrusion can contribute to higher salinity levels in freshwater bodies.
The body of water with the lowest salinity is typically freshwater, such as rivers and lakes. Among larger bodies of water, the Baltic Sea is known for having low salinity levels due to its significant freshwater inflow from rivers and limited exchange with oceanic waters. In general, salinity levels decrease in areas where freshwater mixes with saltwater.
The salinity in isolated seas and salt-water lakes (for example, the Dead Sea) can be considerably greater. SO there's a high salinity in the Dead Sea. :D
Any kind from fresh to Salt. The Caspian Sea is the larget Lake in the world...it is Salt water...Great Salt Lake another example. Lakes are not defined by salinity!
chilka lake
luni or lake sambar
Freshwater biomes, such as rivers, streams, lakes, and ponds, typically have a salinity of 0.005 or less. These bodies of water contain very low levels of dissolved salts compared to marine or estuarine environments.