Carbondioxidi Emen Kaya Keşfed

07.11.2008 NTVMSNBC

carbon dioxide from important source that lead to change of hope, discovered a rock type that can absorb in circulation that will slow global warming.

According to the article "Proceedings of the Natural Academy of Sciences", the scientific journal "Proceedings of the Natural Academy of Sciences" will be published on November 11, this type of rock is more encountered in Umman. [[[T]] [[

carbonene gas turning by solid reacting when the “peridotite” type is in contact with rock, creating calcium carbonate. [

According to the explanations of Lamont-Doherty Observation House, Jeolog Peter Kelemen and Jeokimyacı Juerg Matter, each year 30 billion tons of carbon dioxide is produced and left to the atmosphere. This carbon dioxide is absorbed by 2 billion tons of underground per year. If this rock type is used extensively, this suction process is already made of underground alive can be increased to 1 million times.

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The rock type calledPeridotite is one of the most common rocks in the manto layer, which is located close to the floor shell. This rock is also on the earth. The most important thing in the earth is in Umman.

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This rock is removed from the ground, it has the possibility to be transported to carbon dioxide or other facilities and to be used in these places to be absorbed by the gas. However, it is necessary that this will be a very expensive transaction.

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The two scientists can be injected into the rocky area in Oman, with the help of hot water, so they can remove 4-5 billion tons of carbon dioxide from the earth in the year.

Sentetic trees

Makalede, again through the “ trees trees” developed by Klaus Lackner from Columbia University, where the carbon dioxide can be brewed into the atmosphere, with this special rocky area in Umman, the artificial trees were used together, which leads to global warming, the amount of carbon dioxide in the atmosphere was determined.

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Although this rock type is less in harmony, Adriyatic coasts and California coasts were recorded in Papua New Guinea and Kalidonya from Pacific reserve. [

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