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In electronics of water can we seperate hydrogen from oxygen?
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In electronics of water can we seperate hydrogen from oxygen?
Separation of Hydrogen from Oxygen in Water
Hydrogen and oxygen can be separated from water through a process called electrolysis. This involves passing an electric current through water, which causes the water molecules to break apart into their constituent elements - hydrogen and oxygen.

Electrolysis Process
- In the electrolysis of water, two electrodes are placed in a container of water.
- The electrodes are connected to a power source, such as a battery or a power supply.
- When the electric current is passed through the water, it causes the water molecules to split into hydrogen gas at the cathode (negative electrode) and oxygen gas at the anode (positive electrode).

Chemical Reaction
- The chemical reaction that takes place during electrolysis of water is:
2H2O(l) → 2H2(g) + O2(g)

Collection of Gases
- The hydrogen gas is collected at the cathode, while the oxygen gas is collected at the anode.
- These gases can then be collected separately and used for various applications.

Uses of Hydrogen and Oxygen
- Hydrogen is used in various industries, such as in the production of ammonia and in fuel cells.
- Oxygen is used in medical applications, such as in respiratory therapy and in the production of steel.
In conclusion, the process of electrolysis allows for the separation of hydrogen and oxygen from water, providing a method for obtaining these important gases for various industrial and scientific purposes.
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Milankovitch proposed in the early twentieth century that the ice ages were caused by variations in the Earth’s orbit around the Sun. For some time, this theory was considered untestable, largely because there was no sufficiently precise chronology of the ice ages with which the orbital variations could be matched. To establish such a chronology, it is necessary to determine the relative amounts of land ice that existed at various times in the Earth’s past. A recent discovery makes such a determination possible: relative land-ice volume for a given period can be deduced from the ratio of two oxygen isotopes, 16 and 18, found in ocean sediments. Almost all the oxygen in water is oxygen 16, but a few molecules out of every thousand incorporate the heavier isotope 18.When an ice age begins, the continental ice sheets grow, steadily reducing the amount of water evaporated from the ocean that will eventually return to it. Because heavier isotopes tend to be left behind when water evaporates from the ocean surfaces, the remaining ocean water becomes progressively enriched in oxygen 18. The degree of enrichment can be determined by analyzing ocean sediments of the period, because these sediments are composed of calcium carbonate shells of marine organisms, shells that were constructed with oxygen atoms drawn from the surrounding ocean. The higher the ratio of oxygen 18 to oxygen 16 in a sedimentary specimen, the more land ice there was when the sediment was laid down.It can be inferred from the passage that precipitation formed from evaporated ocean water has

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In electronics of water can we seperate hydrogen from oxygen?
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