Reverse Osmosis
The major ions in sea water are chloride, sodium, sulphate, magnesium, calcium, potassium, bicarbonate, bromide, strontium,boron and flouride.
The most predominant ions in seawater are Na+,Mg+,I-,cl-.
Distilled water does not contain any ions because the distillation process removes all impurities, including ions, from the water.
Distilled water typically contains very low levels of ions, as the distillation process removes most impurities, including ions.
The more H2CO3 there is in seawater, the greater the number of hydrogen ions present. This decreases the pH of seawater, making it more acidic. Higher concentrations of H2CO3 also lessen the number of available carbonate ions (CO32).
Chlorine can be produced from seawater through a process called electrolysis. In this process, an electric current is passed through the seawater, causing the chloride ions to undergo oxidation at the anode, producing chlorine gas.
These ions are Na+ and Cl-.
It should say, "Magnesium and CHLORINE make up most of the ions in seawater." Not chloride.
Magnesium ions make up approximately 7.7 percent of the ions in seawater. These ions play a key role in various biological processes and are important for the health of marine organisms.
The most negatively charged ion dissolved in seawater is chloride. In fact, Cl- makes up 55 percent of the seawater's salinity.
The major source of oceanic salinity is the dissolution of ions from rocks on land that are carried into the ocean by rivers. This process adds various salts to seawater, contributing to its overall salinity. Additionally, hydrothermal vents on the ocean floor can also introduce elements and minerals that affect salinity.
The process that contributes the most to the salts found in seawater is weathering and erosion of rocks on land. As rainwater, which is slightly acidic, flows over rocks, it dissolves minerals and releases ions such as sodium, chloride, magnesium, and calcium into rivers. These ions eventually reach the oceans, where they accumulate over time, contributing to the salinity of seawater. Additionally, hydrothermal vents and volcanic activity also contribute some salts, but the majority comes from terrestrial sources.