1·New carbonates will no longer be laid down.
新的碳酸盐将不再沉淀。
2·Carbonic Acid, Carbonates and Carbides.
碳酸，碳酸盐，碳化物。
3·Reservoir space in carbonates is mainly controlled by diagenesis.
碳酸盐岩储集空间主要受成岩作用制约。
4·Carbonates and organic matter are main carrying zinc matter in soils.
土壤中的碳酸盐和有机质是主要吸锌载体。
5·Carbon isotope in soil carbonates is an important paleoclimate data carrier.
土壤碳酸盐中碳稳定同位素是记录古气候变化信息的重要载体。
6·The most common biogenetic minerals are carbonates, sulfides and iron oxides.
最普遍的生物成因矿物有碳酸盐、硫化物和铁的氧化物。
7·As important inorganic industrial chemicals, calcium carbonates have wide USES.
碳酸钙是重要的无机化工原料，有极广泛的用途。
8·The impact of land use and soil parent on the soil carbonates content is significant.
成土母质和土地利用方式对土壤碳酸盐含量有明显的影响。
9·However, other rocks are also radioactive, notably some carbonates and feldspar-rich rocks.
然而其它一些岩石也有放射性，常见于碳酸盐岩和富含长石的岩石。
10·We can get calcium carbonates of different shapes and grain sizes through different techniques.
在不同工艺条件下可制得不同形态和粒径的碳酸钙产品。
1·New carbonates will no longer be laid down.
新的碳酸盐将不再沉淀。
2·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.
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。
3·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.
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。
4·Since these carbonates dissolve in acid, the persistence of these mounds indicates that water perhaps less acidic and more favorable for life might have once flowed across Mars.
因为这些碳酸盐可以溶解在酸中，这些岩石能长久保存下来就说明在火星上可能曾经流动着酸性并不太大，更适宜生命存在的水。
5·Most grades contain up to 25% non-attapulgite material in the form of carbonates and other inclusions.
最等级含有高达25 %非凹凸棒材料的形式，碳酸盐和其他夹杂物。