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Sea Water: Dolomitization

2024-01-10 02:32:34

Dolomitization - Problem C One of the difficulties in the sequestering action of carbonate is that sea water is supersaturated with dolomite, but dolomite seldom directly precipitate directly. Explain the advantages and disadvantages of the various mechanisms used to explain dolomitization and why it is important to understand it from a hydrocarbon perspective. Introduction Dolomite (CaMg - (CO_3) _ 2) exists in various ages of carbonate rocks formed under various conditions, but today it is formed only in super salt water lagoons, lakes and tidal flats.

Magnesium is found together with carbonate as carbonate and forms an important part of mineral magnetite and rock dolomite. The bitterness of sea water and some mineral water is due to the presence of magnesium oxide salt. Combined with silica, it forms an important part of rocks such as serpentinite, saponite, talc and so on. In this form it is found in animal bones, plant seeds and constitutes an essential part of mineral apatite and phosphate. Although the proportion of phosphorus is small, phosphorus is a very important ingredient of fertile soil. Its main cause is mineral apatite in old crystalline rock.

Water is an important resource for every life. You can find water in many places on the earth: sea, river and lake, pond etc ... water occupies three quarters of the earth's surface. Saltwater is called seawater and the water of the river and lake is sweet, but because the gap meets salt water and fresh river, the resulting mixture of water is called brackish water. Animals living in the water are called aquatic animals such as aquatic animals. Fish, algae or whales. Are these seas and freshwater in inland water (freshwater)? There are still plenty of water in the body, more than half of all are presumed to be water. Fruits, vegetables, and many foods contain plenty of water.

From the point of view of physicists, the difference in density between freshwater and saltwater makes the estuary interesting. When the river encounters sea water, light fresh water rises and passes through a dark salt water. Sea water enters the estuary under the river that flows and goes upstream along the valley. The renowned Roman naturalist, Senator and commander of the Imperial Fleet, Prini observed the unique behavior of the Bosphorus Strait Fisherman's net near Istanbul. Pliny concluded that the ground and sea floor flows in the opposite direction and provided the first document he called the estuary circulation for the first time.