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Titlebook: Marine Geochemistry; Roy Chester Book 1990 Roy Chester 1990 geochemistry

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发表于 2025-3-21 17:54:57 | 显示全部楼层 |阅读模式
书目名称Marine Geochemistry
编辑Roy Chester
视频video
图书封面Titlebook: Marine Geochemistry;  Roy Chester Book 1990 Roy Chester 1990 geochemistry
描述The past two or three decades have seen many important advances in our knowledge of the chemistry, physics, geology and biology of the oceans. It has also become apparent that in order to understand the manner in which the oceans work as a ‘chemical system‘, it is necessary to use a framework which takes account of these interdisciplinary advances. Marine geochemistry has been written in response to the need for a single state-of-the-art text that addresses the subject of treating the sea water, sediment and rock reservoirs as a unified system. In taking this approach, a process-orientated framework has been adopted in which the emphasis is placed on identifying key processes operating within the ‘unified ocean‘. In doing this, particular attention has been paid to making the text accessible to students from all disciplines in such a way that future advances can readily be understood. I would like to express my thanks to those people who have helped with the writing of this volume. In particular, I wish to put on record my sincere appreciation of extremely helpful suggestions made by Professor John Edmond, FRS. In addition, I thank Dr S. Rowlatt for his comments on the sections cov
出版日期Book 1990
关键词geochemistry
版次1
doihttps://doi.org/10.1007/978-94-010-9488-7
isbn_softcover978-94-010-9490-0
isbn_ebook978-94-010-9488-7
copyrightRoy Chester 1990
The information of publication is updating

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Dissolved gases in sea waterces of a number of these are given in Table 8.1. The ocean can act as either a source or a sink for atmospheric gases. The gases enter or leave the ocean via exchange across the air/sea interface, and are transported within the ocean reservoir by physical processes.
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Nutrients, organic carbon and the carbon cycle in sea waterate organic carbon, i.e. the ., drives the processes that control the removal of material from the water column and its incorporation into the sediment sink. The nutrient and carbon cycles are intimately interrelated, but for convenience they are considered separately in the following sections.
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The input of material to the ocean reservoirThe World Ocean may be regarded as a planetary dumping ground for material that originates in other geospheres, and to understand marine geochemistry it is necessary to evaluate the composition, flux rate and subsequent fate of the material that is delivered to the ocean reservoir.
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The transport of material to the oceans: relative flux magnitudesIn the preceding chapters we have considered the three principal primary pathways by which material is transported to the World Ocean at the present day, i.e. river run-off, atmospheric deposition and hydrothermal exhalations. The magnitudes of the fluxes associated with each of these transport pathways are discussed below.
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Marine sedimentsMarine sediments represent the major sink for material that leaves the sea water reservoir. However, before attempting to understand how this sink operates, it is necessary briefly to describe the sediments within a global ocean context.
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re benign in character with a ratio of benign to malig­ nant of about 60 to 40. The relative incidence of malignant mediastinal tumors in children is about 50%. Even though mediastinal tumors are not common, they represent a unique problem with regards to treatment whether by surgery, radiation ther
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