hypolimnion वाक्य
उदाहरण वाक्य
मोबाइल
- The hypolimnion may be much warmer in lakes at warmer latitudes.
- The lowest zone in the lake is the coldest and is called the hypolimnion.
- This relieves the downward pressure on the hypolimnion, so cold, dense water flows northward.
- As the epilimnion gets thicker, it exerts more and more pressure on the denser hypolimnion below.
- Typically the hypolimnion is the coldest layer of a lake in summer, and the warmest layer during winter.
- The lake is thus anoxic and has reduced hypolimnion, winter circulation, large phytoplankton and relatively lower animal population.
- Many soda lakes are strongly anoxic lower layer ( hypolimnion ), without oxygen and often high concentrations of sulfide.
- The two layers of water, the epilimnion and the hypolimnion, on the other hand, differ in density only slightly.
- Therefore, the warm top layer, called the epilinmion, tends not to mix with the denser lower layer, the hypolimnion.
- In deep, temperate lakes, the bottom-most waters of the hypolimnion are typically close to 4 �C throughout the year.
- Deep reservoirs with multiple level draw off towers can discharge deep cold water into the downstream river greatly reducing the size of any hypolimnion.
- Cold water is denser than warm water and the epilimnion generally consists of water that is not as dense as the water in the hypolimnion.
- As the hypolimnion of lakes gradually filled with sediments, oxygen depletion would promote the release of iron-bound phosphorus to the overlying water.
- As they grow and reproduce they absorb nutrients from the water, when they die they sink into the hypolimnion resulting in the epilimnion becoming depleted of nutrients.
- The extreme depths over most of its area causes the greater part of Loch Lomond to become stratified each summer and has characteristically low temperatures in the hypolimnion.
- At the bottom of lakes ( in the sediment or hypolimnion, methanogens use these compounds to derive energy, by producing methane, a procedure known as " methanogenesis ".
- As the temperature increases in the spring, the lake water divides into an upper half which is warm ( epilimnion ), while the lower half ( hypolimnion ) stays cold and lacking in oxygen.
- The northwest to southeast orientation of Uvas Reservoir is in line with prevailing winds which drive the warm surface layer ( epilimnion ) down into the cool bottom layer ( hypolimnion ), so that by late summer the bottom water is warm and anoxic.
- "' Lake stratification "'is the separation of lakes into three layers : 1 ) Epilimnion-top of the lake; 2 ) Metalimnion ( or thermocline )-middle layer that may change depth throughout the day; 3 ) and the Hypolimnion-the bottom layer.
- In all but the shallowest lakes, there are major changes in the chemical composition of lake water at different depths, especially during the summer months when many lakes stratify into a warm, well oxygenated upper layer ( " epilimnion " ) and a cool de-oxygenated lower layer " ( hypolimnion " ).
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