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21#
發(fā)表于 2025-3-25 06:20:45 | 只看該作者
The Use of Carbon Mass Budgets and Stable Carbon Isotopes to Examine Processes Affecting CO2 and CH during each of the three flooding seasons, but neither CO. nor CH. production was related to overall mass of flooded OC. Net reservoir CO. production in the second and third flooding seasons (408 to 479 kg C ha.) was lower than in the first flooding season (703 to 797 kg C ha.), while reservoir CH.
22#
發(fā)表于 2025-3-25 07:58:28 | 只看該作者
23#
發(fā)表于 2025-3-25 11:43:58 | 只看該作者
24#
發(fā)表于 2025-3-25 15:51:34 | 只看該作者
Production and Consumption of Methane in Soil, Peat, and Sediments from a Hydro-Electric Reservoir nmental factors, including the amounts and quality of organic carbon, and the abundance of oxidizing ions (Fe., SO.). Periodically flooded or flooded peats contributed more to methane production than unflooded peats, soils and natural lake sediments. Similarly, methane oxidation rates were higher in
25#
發(fā)表于 2025-3-25 23:48:52 | 只看該作者
Gunnhildur Una Jonsdottir PhD Studentnt les flux de GES sont avant tout le résultat de variations spatiales et temporelles naturelles des flux, et non pas des techniques de mesure disponibles. La présente synthèse se base sur les résultats de plus de dix ans de suivis obtenus par différentes équipes de recherche de plusieurs université
26#
發(fā)表于 2025-3-26 01:52:35 | 只看該作者
From Republics to a National Empire,for duplicate measurements of fluxes is similar for all methods with floating chambers. In general, the thin boundary layer method tends to measure lower fluxes than the floating chamber method with laboratory analysis and there is no good correlation between the two methods. Fluxes measured with au
27#
發(fā)表于 2025-3-26 08:19:53 | 只看該作者
https://doi.org/10.1007/978-94-007-0062-8tted by lakes and hydro reservoirs in different regions. Recent optimizations of the developed prototype allow quick on site set-up and operation of the laser device, even in remote areas without local facilities, as well as the continuous measurement of low GHG concentration gradients during long t
28#
發(fā)表于 2025-3-26 08:43:00 | 只看該作者
The Role of Emotions in Coachingorests can be offset by nearly 30% by N.O emissions from the soils. In northern forests, some sites have been found to be net sources of CO., particularly during warm and dry years..In wetlands, water-saturated soils are conducive to anaerobic decomposition of organic matter and methane production.
29#
發(fā)表于 2025-3-26 15:28:04 | 只看該作者
The Role of Emotions in Coaching (1.8-3, n=3)]. The CO. concentrations in acidotrophic lakes were, however, high [0.9 ± 0.7 (0.1–2, n=14)]. Diffuse flux of the two greenhouse gases - CH. and CO. — from the surficial sediments across the sediment-water interface (SWI) were calculated from Fick‘s first law of diffusion. These result
30#
發(fā)表于 2025-3-26 18:17:24 | 只看該作者
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