西德里特和铁氧氧化物意味着火星上相互关联的碳,铁和素循环
Kaushik Mitra1, Lauren A Malesky1, Michael T Thorpe2
1Department of Earth & Planetary Sciences, The University of Texas at San Antonio, San Antonio, TX 78249.
概括
氧盐水,而不是酸性液体,可能在火星上经过气候变化的 siderite,释放二氧化碳并形成铁矿物质. 这表明火星的素,铁和碳循环之间存在联系.
科学领域:
- 行星科学 行星科学
- 地质化学 地质化学
- 天体生物学 天体生物学
背景情况:
- 在火星上发现的 siderite (FeIICO3) 表明大气中二氧化碳的释放和铁矿物质的形成通过diagenesis.
- 之前的假设提出了用于 siderite 改变的酸代谢.
研究的目的:
- 为了研究在火星相关条件下 siderite 的化学气候变化.
- 确定负责 siderite 变化和由此产生的矿物学的具体代理.
主要方法:
- 实验室实验模拟火星条件.
- 在不同的液体组合下 (酸性与氧素) 分析 siderite 变化产物.
主要成果:
- 封闭系统酸代谢对于改变火星 siderite 是无效的.
- 氧化化合物 (酸盐,酸盐) 在酸性和近中性溶液中有效地化 siderite.
- 变化产物 (铁氧化) 取决于液体成分;磁铁的缺失表明氧化气候对光氧化产生影响.
结论:
- 氧化盐水,而不是酸性液体,是盖尔火山口 siderite 变化的可能原因.
- 这种气候变化过程解释了火星沉积物中观察到的氧化还原不平衡.
- 火星上的素循环可能与铁和碳循环相互联系.
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