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Sulfide Mineralogy and Geochemistry

机译:硫化物矿物学与地球化学

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Volume 61 of the MSA's influential Reviews in Mineralogy and Geochemistry series seems, at first glance, to be a reprise of Volume 1, published in 1974 under the title Sulfide Mineralogy. However, a closer look quickly reveals just how far sulfide mineral studies have come in the succeeding 32 years. A few chapters have similar titles; for example, chapters on crystal structures, chemical bonding, and phase equilibria, but the chapter contents of Volume 61 are both up-to-date and major advances on their predecessors. The biggest difference between Volumes 1 and 61 is not the updating of older topics, but the new areas of research that have emerged and that are treated in depth in Volume 61. Surface chemistry of sulfides, for example, which is discussed in two chapters by Rosso and Vaughan, has emerged as a vibrant area of research for practical reasons such as sulfide mineral oxidation and acid mine drainage, and for scientific reasons because new, high-resolution tools have been developed that are ideal for studying surfaces on an atomic scale. Sulfur isotope geochemistry was in its infancy when Volume 1 was written. Today, sulfur isotopes have become key research tools for studies ranging from the chemistry of ore deposits to the evolution of Earths atmosphere. In Volume 61, sulfur isotopes are reviewed in a concisely elegant chapter by Seal. Another new topic in Volume 61 concerns sulfide minerals in biosystems. The knowledge that some sulfide minerals form as a consequence of biological activities is certainly not new, but discoveries of deep-sea sulfide chimneys, and the realization that life might have first arisen on a sulfide mineral surface in such an environment, has heightened studies of biologically mediated sulfide reactions.
机译:乍一看,MSA具有影响力的《矿物学和地球化学评论》系列的第61卷似乎是对第1卷的再版,该卷于1974年出版,标题为“硫化物矿物学”。但是,仔细观察很快就会发现,在随后的32年中,硫化物矿物研究已经走了多远。有几章标题相似。例如,有关晶体结构,化学键合和相平衡的章节,但是第61卷的章节内容既是其前身的最新内容,也是其主要进展。第1卷和第61卷之间的最大区别不是更新较旧的主题,而是在第61卷中出现并深入研究的新研究领域。例如,硫化物的表面化学在以下两章中进行了讨论:由于诸如硫化物矿物氧化和酸性矿山排水之类的实际原因,以及出于科学原因,Rosso和Vaughan成为活跃的研究领域,因为已经开发出了新的高分辨率工具,这些工具非常适合研究原子尺度的表面。撰写第一卷时,硫同位素地球化学才刚刚起步。如今,硫同位素已成为从矿床化学到地球大气演变的主要研究工具。 Seal在简洁简洁的一章中回顾了第61卷中的硫同位素。第61卷中的另一个新主题涉及生物系统中的硫化物矿物。某些硫化物矿物是由于生物活性而形成的知识当然不是什么新鲜事,但是深海硫化物烟囱的发现以及人们认识到在这种环境下可能首先在硫化物矿物表面上出现了生命,这一认识已经得到了进一步的研究。生物介导的硫化物反应。

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