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Geochemical Processes: Water and Sediment Environments

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TLDR
The approach of this book to geochemistry can be summarized in the question: What happens, and how fast does it happen, when waters, solids, and gases interact in the earth's surface environment? The environment of the earths surface is made of solids and fluids, and the interactions among them are responsible for much of what is taking place in the physical world around us as mentioned in this paper.
Abstract
The approach of this book to geochemistry can be summarized in the question: What happens, and how fast does it happen, when waters, solids, and gases interact in the earths surface environment? The environment of the earths surface is made of solids and fluids, and theinteractions among them are responsible for much of what is taking place in the physical world around us. The dissolved load of natural waters and the materials of which sediments are made are the products of reactions taking place practically everywhere on land, in the atmosphere, and in the hydrosphere. Thus the term water and sediment environments applies effectivelly to much of the surface environment of the earth, including the zone of up to a few kilometers above and below the land and ocean surface. Evolution present itself to us as a more or less complex variety of processes-geological, physical, chemical, and biological. To this end, the inclusive title Geochemical Processes was chosen for the book, to introduce a text that emphasizes processes and time-dependent phenomena.

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Is Vostok lake in steady state

TL;DR: In this article, stable isotope (d Da ndd 18 O) data from the Vostok (East Antarctica) ice core are used to explore whether or not subglacial Vostoks lake is in isotopic steady state.
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The atmospheric carbon dioxide response to oceanic primary productivity fluctuations

TL;DR: In this article, a model of the ocean in which the downward transport of carbon by the sinking and oxidation of organic particulate matter is balanced by upward hydrodynamic mixing of dissolved inorganic carbon was used to estimate the effect of periodic and impulsive changes in the rate of primary production on the atmospheric CO2 concentration.
Journal ArticleDOI

Facies types of sedimentary iron ore deposits and their geochemical features: Communication 2. Problems of the geochemistry of phanerozoic iron ores

TL;DR: In this paper, mineralogical-geochemical features of different facies types of sedimentary iron ore deposits are described and the multistage formation of their geochemical properties is proved available geochemical models are considered.
Journal ArticleDOI

Unusual diagenetic alteration of volcanoclastic sediments in the Tonga fore-are: Evidence from chemical and strontium isotopic compositions of interstitial waters

TL;DR: The depth variations in the major chemical components dissolved in interstitial waters from the Tonga margin (ODP Site 841) are much more pronounced than those usually observed in deep-sea sediments as discussed by the authors.
ReportDOI

Effluent migration from septic tank systems in two different lithologies, Broward County, Florida

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