Titlebook: Non-CO2 Greenhouse Gases: Why and How to Control?; Proceedings of an In J. Ham,L. J. H. M. Janssen,R. J. Swart Conference proceedings 1994

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呼吸

果仁

破裂

異常

ORBIT

Methane in Ocean Waters: Concentration and Carbon Isotope Variability at East Pacific Rise and in the been determined. EPR surface water is in equilibrium (ca. 50 nl/L and ?50%o < δ.CH. < ?46%o) with atmospheric methane. Deep “background” water has the signature of the remaining fraction of atmospheric methane partially oxidized in the water column by bacteria. Bottom near, hydrothermally influenc

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Affection

Emissions of NO and N2O from Soilsemissions of NO and N.O were measured from the agricultural soils shortly after fertiliser application (7 ng NO-N m. s. and 91 ng N.O-N m. s.). For the non-agricultural soils the NO flux ranged from ?0.3 to 0.5 ng NO-N m. s. and the N.O flux ranged from 1 to 2.7 ng N.O-N m. s.. Emissions, however, w

labile

Nitrous Oxide Emissions from Waste Watertance with all significant nitrous oxide sources. A potentially important source for which emission data are lacking is the sewage system transporting waste water from human activities. For this study an experimental measurement campaign has been carried out on waste water sampled at different sewag

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