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樓主
發(fā)表于 2025-3-21 17:49:29 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Greenhouse Gas Emissions - Fluxes and Processes
編輯Alain Tremblay,Louis Varfalvy,Michelle Garneau
視頻videohttp://file.papertrans.cn/389/388567/388567.mp4
叢書名稱Environmental Science and Engineering
圖書封面Titlebook: ;
出版日期Book 20051st edition
版次1
doihttps://doi.org/10.1007/978-3-540-26643-3
isbn_softcover978-3-642-06249-0
isbn_ebook978-3-540-26643-3Series ISSN 1863-5520 Series E-ISSN 1863-5539
issn_series 1863-5520
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 20:23:36 | 只看該作者
Terence Gourlay PhD,Tipo Qureshi MDe values are similar to those observed in boreal regions. Although several limnological parameters can influence the fluxes of CO., only the pH was significantly related with the CO. gross fluxes, which decrease with increasing pH.
板凳
發(fā)表于 2025-3-22 01:48:53 | 只看該作者
地板
發(fā)表于 2025-3-22 08:23:17 | 只看該作者
ost of Canada. These values are comparable to those observed in Finland or in the sub-tropical semi-arid western USA. Although several limnological parameters can influence these fluxes, none showed a statistical relationship. However, levels of CO. or CH. fluxes are influenced by pH, wind speed, depth at sampling stations and latitude.
5#
發(fā)表于 2025-3-22 10:46:02 | 只看該作者
6#
發(fā)表于 2025-3-22 15:20:40 | 只看該作者
7#
發(fā)表于 2025-3-22 18:19:42 | 只看該作者
GHG Emissions from Boreal Reservoirs and Natural Aquatic Ecosystems,ost of Canada. These values are comparable to those observed in Finland or in the sub-tropical semi-arid western USA. Although several limnological parameters can influence these fluxes, none showed a statistical relationship. However, levels of CO. or CH. fluxes are influenced by pH, wind speed, depth at sampling stations and latitude.
8#
發(fā)表于 2025-3-23 00:01:14 | 只看該作者
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發(fā)表于 2025-3-23 04:27:13 | 只看該作者
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發(fā)表于 2025-3-23 09:21:19 | 只看該作者
On Classical Liberalism and Libertarianismoelectric reservoir in boreal Québec, this model estimated an average CO. diffusive flux across the air-water interface of 225±51 mg CO.·m.·d. in the summer of 2000 and of 446±93 mg CO.·m.·d. in the summer of 2001. These average fluxes are representative of the whole icefree period.
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