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显示全部楼层 · 发表于 2025-3-21 17:49:29

书目名称Greenhouse Gas Emissions - Fluxes and Processes影响因子(影响力)

书目名称Greenhouse Gas Emissions - Fluxes and Processes影响因子(影响力)学科排名

书目名称Greenhouse Gas Emissions - Fluxes and Processes网络公开度

书目名称Greenhouse Gas Emissions - Fluxes and Processes网络公开度学科排名

书目名称Greenhouse Gas Emissions - Fluxes and Processes被引频次

书目名称Greenhouse Gas Emissions - Fluxes and Processes被引频次学科排名

书目名称Greenhouse Gas Emissions - Fluxes and Processes年度引用

书目名称Greenhouse Gas Emissions - Fluxes and Processes年度引用学科排名

书目名称Greenhouse Gas Emissions - Fluxes and Processes读者反馈

书目名称Greenhouse Gas Emissions - Fluxes and Processes读者反馈学科排名

显示全部楼层 · 发表于 2025-3-21 20:23:36

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.

显示全部楼层 · 发表于 2025-3-22 01:48:53

显示全部楼层 · 发表于 2025-3-22 08:23:17

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.

显示全部楼层 · 发表于 2025-3-22 10:46:02

显示全部楼层 · 发表于 2025-3-22 15:20:40

显示全部楼层 · 发表于 2025-3-22 18:19:42

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.

显示全部楼层 · 发表于 2025-3-23 00:01:14

显示全部楼层 · 发表于 2025-3-23 04:27:13

显示全部楼层 · 发表于 2025-3-23 09:21:19

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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