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On Earth, the oceans are known for their large water reserves. So it brings us not only abundant resources, beautiful landscapes, and a variety of creatures. At the same time, there are a lot of things that we can't explain, we know that when the company reaches a large state, the state of the water will change, we thought that the water in the ocean is liquid, but at a very deep level, so deep that we humans can't reach the state of the sea, because of the pressure, it will change accordingly.
Especially at the bottom of the glacier, because of the huge ice, we can't explore, what kind of secrets exist in it, it may be related to our human **. However, this time, researchers from the Chinese Academy of Sciences found gaseous water resources in a very deep seabed, and its temperature is particularly high. Through their own research probes, our scientists discovered the presence of high-temperature bubbles on the ocean floor, that is, gaseous water.
This discovery takes our exploration of the ocean one step further. <>
So what kind of special substance is the formation of this bubble discovered by scientists this time? In fact, the main reason is that the location of this bubble is relatively special. In this place, the density of the seabed is relatively low, and the salinity of the water is also relatively low, so there is a phenomenon of separation between waters.
However, as the sea surface rises, the temperature becomes lower, so steam cannot appear on the surface of the sea. So this is the case in this place, where the steam does not come up on the bottom of the sea. <>
This is the first time that this phenomenon has been discovered in our country, and it has also brought us a lot of information about this value. It is also an important breakthrough in our research on the ocean. It is also an important breakthrough in our research on the ocean.
At the same time, we also have different solutions and views on the marine environment and the temperature changes on the earth. Scientists will continue to study the latest research later, and it is still unknown whether this large bubble can be reused, so we must look forward to further scientific discoveries.
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It is a substance that can heat up in the sea and has its own temperature, and it is something that can be used to study this substance.
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Gaseous water is mixed with gas components such as carbon dioxide, methane, and hydrogen sulfide. It is not possible to take advantage of the current technology.
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The ultra-high bubbles on the icy seabed are gaseous water that can be utilized. The in-situ detection of such gas-phase hydrothermal eruption systems is helpful to reveal the hydrothermal sulfide mineralization process of such low-density gas-phase hydrothermal eruption systems and their impact on the deep-sea environment, and this major discovery is made thanks to the application of the world's first deep-sea in-situ Raman spectroscopy probe independently developed by China that can be directly inserted into a deep-sea hydrothermal vent at 450 degrees Celsius, which has successfully broken through the technical bottlenecks such as the low temperature resistance of ordinary optical lenses and the poor anti-particle adhesion performance. It provides the first multi-parameter in-situ optical detection sensor for the study of geochemical properties of deep-sea hydrothermal high-temperature fluids, and provides a new method for studying the impact of hydrothermal fluids on the marine environment and global change.
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Bubbles are not special substances, they are very simple substances that can be used and maybe new things can be made.
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