Sea water doesn't contain organic salts.
About 86% of the dissolved salts in seawater are major salts, which include sodium chloride (table salt), magnesium chloride, and sulfate ions. These major salts make up the majority of the total dissolved solids present in seawater.
Seawater is a mixture. It consists of water (H₂O) along with various dissolved salts, minerals, and organic matter. Unlike a compound, which has a fixed composition and properties, the composition of seawater can vary based on location and environmental factors.
Seawater is hypertonic to drinking water. This means that seawater has a higher concentration of solutes (such as salts) compared to drinking water. Drinking seawater can lead to dehydration as the body would need to excrete more water to get rid of the excess salts.
The dissolved materials in seawater are thought to originate from the weathering of rocks on land, as well as from volcanic activity and chemical reactions at hydrothermal vents on the ocean floor. These processes contribute minerals, salts, and organic matter to the water, creating the diverse composition of seawater.
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It is dissolved salts, gases, and nutrients that are presented in seawater.
About 86% of the dissolved salts in seawater are major salts, which include sodium chloride (table salt), magnesium chloride, and sulfate ions. These major salts make up the majority of the total dissolved solids present in seawater.
Sea water is water with a few thousand different dissolved salts and a variety of dissolved or suspended organic compounds.
Seawater is a mixture. It is composed of water, various dissolved salts and minerals, gases, and organic matter. These components can be physically separated through processes such as evaporation or filtration.
Dissolved salts are transported by the rivers.
Precipitation, land water runoff and the melting of icebergs do not add salts to seawater.
One thousand grams of seawater typically consists of around 35 grams of dissolved substances, such as salts, minerals, and organic matter. The remaining weight is mostly water.
Seawater is hypertonic to drinking water. This means that seawater has a higher concentration of solutes (such as salts) compared to drinking water. Drinking seawater can lead to dehydration as the body would need to excrete more water to get rid of the excess salts.
The dissolved materials in seawater are thought to originate from the weathering of rocks on land, as well as from volcanic activity and chemical reactions at hydrothermal vents on the ocean floor. These processes contribute minerals, salts, and organic matter to the water, creating the diverse composition of seawater.
Desalination. Desalination is the process of removing salts and minerals from seawater to make it suitable for consumption or agricultural use.
Seawater is a mixture. It is a combination of salt and water that is a homogeneous mixture. An example of a pure substance is either pure salt or pure sugar.
The average salinity of seawater is about 35 grams of dissolved salts per kilogram of seawater, or 3.5% by weight.