The Origin of Clay Minerals in Soils and Weathered Rocks
The Origin of Clay Minerals in Soils and Weathered Rocks
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DOI：
10.1007/978-3-540-75634-7
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发表时间：
2008-08
期刊：
影响因子：
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通讯作者：
B. Velde;A. Meunier
中科院分区：
文献类型：
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作者：
B. Velde;A. Meunier
当然，我们在这里提出的这样一本书并不是两个人合作的产物，尽管这段经历对我们来说是一种巨大的乐趣。我们要感谢我们的许多合作者和学生，他们经常尖锐地批评我们，鼓励我们的努力。我们希望我们已经利用了他们的评论取得了良好的效果。我们特别要感谢皮埃尔·巴雷的帮助、热情和同意，因为他在制定本书的最后一章时使用了他的大部分论文材料。Dominique Righi在为我们的大量想法和在制定我们的结论期间给我们提供了想法、有用的评论和激烈的辩论方面发挥了重要作用。我们的方法来自矿物化学，因此从与了解土壤和植物的人的讨论中受益匪浅。这本书的项目是在沃尔夫冈·恩格尔的帮助下实现和鼓励的，不幸的是，恩格尔没有和我们一起看到它的定稿。我们对他的逝世深表遗憾。这本书没有对影响粘土在地表环境中发生的现象的一般模式进行公认的知识和分析。我们强调植物在生物界面的作用，以及微系统在水/岩石界面的重要性。我们相信，我们和任何人掌握的文献表明，粘土的形成和反应系统是高度动态的，特别是在地表。
Of course such a book as we propose here is not the product of just two people working together, although the experience has been a great pleasure for us. We would like to thank our many collaborators and students who have encouraged our effort by their, often, sharp criticism. We hope that we have used their comments to good effect. Es-cially we would like to thank Pierre Barré for his help, enthusiasm and consent for the use of much of his thesis material in formulating the last chapter of the book. Dominique Righi was instrumental in giving us ideas, useful comments and vigorous debate for a great number of our ideas and during the periods of formulation of our conclusions. Our approach is from mineral chemistry and hence has greatly benefited from disc-sions with people who know soils and plants. The project of this book was realized and encouraged with the help of Wolfgang Engel who, unfortunately is not with us to see its finalization. We greatly regret his passing. This book is not in the general pattern of accepted knowledge and analysis of the phenomena which affect the occurrence of clays in the surface environment. We stress the role of plants at the bio-interface and the importance of microsystems at the water/rock interface. We believe that the literature at our and anyone’s disposal shows that the system of clay formation and reaction is highly dynamic, especially at the surface.