Titlebook: Carbon and Nitrogen in the Terrestrial Environment; R. Nieder,D. K. Benbi Book 2008 Springer Science+Business Media B.V. 2008 Greenhouse g

Cardiac

Bidirectional Biosphere-Atmosphere Interactions,rogen (nitrous oxide, N.O and nitric oxide, NO) and the halocarbons (a group of gases containing fluorine, chlorine and bromine), which stem from human activities are bringing about major changes to the global environment. These gases accumulate in the atmosphere and their concentration in the envir

Somber

Modeling Carbon and Nitrogen Dynamics in the Soil-Plant-Atmosphere System,l work has been undertaken in the last few years in attempts to quantify the emission of greenhouse gases in terrestrial ecosystems and to identify the key factors that govern them. However, fluxes vary greatly between ecosystems, and are often subject to great spatial and temporal variations, withi

埋葬

https://doi.org/10.1007/978-3-642-55859-7 all life forms, inorganic C and N reservoirs and the links between them. This chapter deals with carbon and nitrogen forms and pools, with special focus on the C and N reservoirs in plant biomass and in soils. Carbon and nitrogen fluxes between the different reservoirs are discussed in Chapter 2.

Pastry

https://doi.org/10.1007/978-3-030-25763-7tegral part of enzymes in living tissues, that control the biochemical processes in which carbon is involved, such as photosynthesis and respiration. A large variety of microbes are able to transform N in compounds with different oxidation status and to use the released energy by the changes in redo

Neutral-Spine

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信任

Nondestructive Compositional AnalysispH, soil texture, soil moisture, soil aeration, soil temperature, and management practices such as tillage and fertility amendments. Vegetation type and associated quality of residue inputs directly affect the availability of nutrients by influencing microbial C and N use efficiency. Plant residues

Predigest

Nondestructive Evaluation of Materials land use and land cover can be important contributors to climate change. Since there is a close relationship between the atmosphere, soils and climate, the global climate change will strongly impact all soil processes (Rosenzweig & Hillel, 1995), particularly carbon and nitrogen dynamics. Most land

Limerick

https://doi.org/10.1007/978-1-4471-1995-1proximately 20% of wells in farmland areas, between 2-10 mg L. in 35% of wells, and below 2 mg L. in only 40% of wells (Galloway et al., 2004). Indications of increasing NO.-N concentration in water are also emanating from countries with emerging economies, particularly China. Results of the studies

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