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Titlebook: Organic geochemistry of natural waters; E. M. Thurman Book 1985 Springer Science+Business Media Dordrecht 1985 Oxidation.amino acid.carbon

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樓主: 雜技演員
41#
發(fā)表于 2025-3-28 16:18:45 | 只看該作者
Amount of Organic Carbon in Natural Watersreview of the literature, and instructive diagrams that give basic information on dissolved organic carbon. This chapter will be especially useful to those needing information on the amount and distribution of organic carbon in natural waters.
42#
發(fā)表于 2025-3-28 20:29:59 | 只看該作者
Classification of Dissolved Organic Carbonter 1 discussed the amount of dissolved organic carbon in different waters, and how it varies with climate and season. This chapter asks the question, “Now that the amount of DOC is known, how can we classify and identify it?”
43#
發(fā)表于 2025-3-29 00:56:39 | 只看該作者
44#
發(fā)表于 2025-3-29 04:00:33 | 只看該作者
Geochemical Processeslow. Because an entire book could be written on the subject of geochemical processes, this chapter is only an overview of major geochemical processes with references to “in-depth” studies in each area.
45#
發(fā)表于 2025-3-29 08:02:14 | 只看該作者
46#
發(fā)表于 2025-3-29 14:00:21 | 只看該作者
47#
發(fā)表于 2025-3-29 17:01:31 | 只看該作者
Carboxylic Acids and Phenols into various classes, which are based on their acidity and geochemistry. They include: carboxylic acids, phenols, and tannins. Because of weak acidity of the phenolic group, phenols and tannins are addressed in the same chapter as carboxylic acids.
48#
發(fā)表于 2025-3-29 19:45:22 | 只看該作者
49#
發(fā)表于 2025-3-30 01:01:25 | 只看該作者
Aquatic Humic Substances in water, elemental composition of aquatic humus, functional group analysis, molecular weight, characterization by spectroscopy, trace components of humic substances, characterization by chromatography, chemical degradation of humic substances, structure of aquatic humic substances, and theories of formation of soil and aquatic humic substances.
50#
發(fā)表于 2025-3-30 05:29:25 | 只看該作者
Introductionstream, formed in an eddy, is from natural surfactants (soaps) from plant and soil organic matter. In the spring the foam may be several inches deep as melting snow and ice leach plant pigments from last year’s fallen leaves.
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