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Reduction of discharge of radioactive gases from the VVR-M reactor into the atmosphere

✍ Scribed by E. A. Konovalov; K. A. Konoplev; R. G. Pikulik; L. M. Ploshchanskii; B. S. Razov; Yu. P. Saikov

Publisher
Springer US
Year
1981
Tongue
English
Weight
162 KB
Volume
50
Category
Article
ISSN
1573-8205

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Volcanism has been a major process during most of the geologic history of Mars. Based on data collected from terrestrial basaltic eruptions, we assume that the volatile content of martian lavas was typically $0.5 wt.% water, $0.7 wt.% carbon dioxide, $0.14 wt.% sulfur dioxide, and contained several