二氧化碳溶解于水的时候形成一种酸，这种酸可以跟矿物起反应生成碳酸盐，这样就能够以相对稳定的状态将碳密闭起来。
Carbon dioxide forms an acid when it dissolves in water. This acid can react with minerals to form carbonates, locking away the carbon in a relatively inert state.
地理学家们以前就发现橄榄岩暴露于空气中会很快与二氧化碳反应生成碳酸盐，和石灰岩或大理石的反应一样。
Geologists have long known that when peridotite is exposed to the air it can react quickly with carbon dioxide to form carbonates like limestone or marble.
在实验室的测量表明他们能将捕获的每磅二氧化碳转化为约两磅的碳酸盐。
Their process, which has been tested in the lab, can produce about two pounds of carbonate for every pound of carbon dioxide captured.
在实验室的测量表明他们能将捕获的每磅二氧化碳转化为约两磅的碳酸盐。
Their process which has been tested in the lab can produce about two pounds of carbonate for every pound of carbon dioxide captured.
一些二氧化碳会被海水吸收，改变海水中氢和碳酸盐离子的比例，使得海水酸化。
Some of this carbon dioxide is absorbed by ocean water, altering the proportion of hydrogen and carbonate ions, and making the water more acidic.
那种基因决定了一种特殊的酶，这种酶能将二氧化碳和水（不要忘了水）分解成重碳酸盐和质子团。
That gene encodes an enzyme that breaks down CO2—and water…don’t forget the water—into bicarbonate and protons.
液化二氧化碳将会在岩石中贮存很长的时间，与铁、钙以及海水产生化学反应产生白垩(即术语所说的碳酸盐)。
It would become trapped inside for a long period of time, reacting with iron, calcium, and sea water in the rocks to make chalk (known more technically as carbonates).
经高温燃烧管的水样受高温催化氧化，使在有机化合物和无机碳酸盐均转化为二氧化碳。
The high temperature combustion of the water by high-temperature catalytic oxidation, so that the organic compounds and inorganic carbonate were converted into carbon dioxide.
相比之下，二氧化碳可以随岩石风化通过与硅酸盐矿物反应形成碳酸盐，直接从大气中自然收集。
In contrast, CO2 is naturally captured directly from the atmosphere by its reaction with silicate minerals to form carbonates as rocks are weathered.
烃源岩的热降解和储层中的烃类热催化裂解，生成有机酸和二氧化碳，引起深层碳酸盐岩发生溶解作用。
Organic acid and CO2, generated from thermal degradation of source rocks and thermo-catalytic cracking of hydrocarbons in reservoirs, destabilized and dissolved the carbonates at depth.
烃源岩的热降解和储层中的烃类热催化裂解，生成有机酸和二氧化碳，引起深层碳酸盐岩发生溶解作用。
Organic acid and CO2, generated from thermal degradation of source rocks and thermo-catalytic cracking of hydrocarbons in reservoirs, destabilized and dissolved the carbonates at depth.
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