文石
方解石
碳酸盐
水合物
矿物学
碳酸钙
化学
镁
无机化学
有机化学
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:1969-09-12
卷期号:165 (3898): 1119-1121
被引量:42
标识
DOI:10.1126/science.165.3898.1119
摘要
Hydrocalcite (CaCO(3) * H(2)O) with exactly one molecule of hydrate water is the main component of carbonate scales deposited from cold water in contact with air. When the magnesium content of the water is high, the hydrocalcite occurs together with MgCO(3) * 3H(2)O (nesquehonite). From the conditions under which hydrocalcite is transformed into calcite and aragonite, it appears that in some cases aragonite in nature may be formed by way of an intermediary of CaCO(3) * H(2)O.
科研通智能强力驱动
Strongly Powered by AbleSci AI