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改造火星:蓝细菌对碳酸盐岩的溶解作用

Terraforming Mars: dissolution of carbonate rocks by cyanobacteria.

作者信息

Friedmann E I, Hua M, Ocampo-Friedmann R

机构信息

Department of Biological Science, Florida State University, Tallahassee 32306-2043, USA.

出版信息

J Br Interplanet Soc. 1993;46:291-2.

Abstract

One of the most difficult tasks in terraforming Mars is the release into the atmosphere of CO2 bound by the surface of Mars. Even if a sufficiently dense CO2 atmosphere can be created by appropriate technology, the maintenance of CO2 concentration remains a problem. As Mars lacks plate tectonics as well as active volcanism, an Earth-like carbon cycle cannot be reproduced there. We suggest that Matteia sp., a lime-boring cyanobacterium isolated from Negev desert rocks, be used to dissolve carbonate rocks both for initial release of CO2 and in design of a Martian carbon cycle.

摘要

在火星地球化改造过程中,最困难的任务之一是将火星表面结合的二氧化碳释放到大气中。即使能够通过适当技术创造出足够浓密的二氧化碳大气层,二氧化碳浓度的维持仍然是个问题。由于火星缺乏板块构造和活火山活动,无法在那里重现类似地球的碳循环。我们建议使用从内盖夫沙漠岩石中分离出的一种钻孔石灰蓝藻菌——马特亚属(Matteia sp.),来溶解碳酸盐岩,既用于二氧化碳的初始释放,也用于火星碳循环的设计。

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