Phosphorus sorption by terrestrial basalt and granite and implications for the martian crust

被引：5

作者：

Dreibus, G ^{[1
]}

Haubold, R ^{[1
]}

机构：

[1] Max Planck Inst Chem, D-55128 Mainz, Germany

来源：

ICARUS | 2004年 / 167卷 / 01期

关键词：

mars; surface; geochemistry;

D O I：

10.1016/j.icarus.2003.09.014

中图分类号：

P1 [天文学];

学科分类号：

0704 ;

摘要：

High phosphorus concentrations in the range of 0.5 wt% in rocks and soil have been measured on the martian surface, terrestrial P concentrations are far less uniform and generally lower. Reactions of terrestrial basalt and granite powders with phosphate solution result in an enrichment of phosphorus in both, with basalt having a far better reactivity than granite. The implications of these results for P on Mars are discussed. (C) 2003 Elsevier Inc. All rights reserved.

引用

页码：166 / 169

页数：4

共 24 条

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