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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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Journal ArticleDOI

Processes affecting the behavior of dissolved aluminum in estuarine waters

TL;DR: In this article, sediment-water interactions have been shown to have a significant influence on dissolved aluminum distributions in estuaries, and the extent of net Al removal in these waters will be determined by both the amount and nature of the dissolved organic matter present.
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Oscillatory flow through submerged canopies: 2. Canopy mass transfer

TL;DR: In this paper, a model was developed to predict canopy mass transfer rates on the basis of the in-canopy flow speed and was generalized to incorporate either unidirectional or oscillatory flow.
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Isotopic approaches for quantifying the rates of marine burial diagenesis

TL;DR: In this paper, the authors describe advances in the use of Ca, Sr, and U series isotopes in constraining carbonate recrystallization and silicate dissolution rates in marine systems.
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Oxygen Consumption in Pelagic Marine Sediments

TL;DR: Measurements in the interstitial waters of pelagic red clay and carbonate ooze sediments in the central equatorial Pacific show that the dissolved oxygen content decreases with depth and levels off at nonzero values.
Journal ArticleDOI

Nitrification and denitrification in the rhizosphere of rice: the detection of processes by a new multi-channel electrode.

TL;DR: In this article, the root-associated nitrification and denitrification in rice soil was measured using a multi-channel microelectrode, which measured NH4+, NO2− and NO3− at the same point.
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