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Titlebook: Interactions of C, N, P and S Biogeochemical Cycles and Global Change; Roland Wollast,Fred T. Mackenzie,Lei Chou Conference proceedings 19

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41#
發(fā)表于 2025-3-28 17:20:08 | 只看該作者
42#
發(fā)表于 2025-3-28 19:50:09 | 只看該作者
C, N, P and S in Rivers: From Sources to Global Inputsaviours in aquatic systems, the occurrence of their specific forms, and the rates of transport by rivers are first considered in this paper. The anthropogenic influences on riverine C, N, P, and S are briefly presented. Finally the global fluvial budgets of the specific forms, including the anthropogenic loads are estimated.
43#
發(fā)表于 2025-3-29 01:05:43 | 只看該作者
Interactions of Carbon and Nitrogen Cycles in the Coastal Zonetal zone. Besides the high productivity generally observed on the continental shelves, the carbon cycle in this area exhibits peculiar properties which are of primary interest in terms of global sources and sinks of carbon.
44#
發(fā)表于 2025-3-29 03:35:09 | 只看該作者
45#
發(fā)表于 2025-3-29 09:10:28 | 只看該作者
46#
發(fā)表于 2025-3-29 13:15:17 | 只看該作者
47#
發(fā)表于 2025-3-29 15:48:06 | 只看該作者
48#
發(fā)表于 2025-3-29 23:05:33 | 只看該作者
The Coupling of Carbon and Ion Cycles Including N, P and S in Soils of Terrestrial Ecosystems. In the context of the 1991 NATO conference, ecosystem processes describing storage changes in the ecosystem were of main concern. The aspects of biochemical and chemical reactions in soil which are involved in the cycles are not discussed; these are covered in many textbooks.
49#
發(fā)表于 2025-3-30 03:52:16 | 只看該作者
50#
發(fā)表于 2025-3-30 06:59:57 | 只看該作者
Multi-Phase Processes in the Atmospheric Sulfur Cycle is approximately 150–40 pptv (Maroulis and Bandy, 1980; Jones .., 1983). The “background” troposphere, the main focus of this paper, is defined as the part of the troposphere that is not directly affected by anthropogenic emissions of trace compounds, a predominantly marine environment.
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