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分析了潜艇舱室固态胺CO2吸附及水蒸气再生的反应机理,指出了CO2水合反应和水合CO2分解反应分别为吸附与再生过程的慢反应.在实际工况下,固态胺吸附CO2的速率受传质控制,水蒸气再生过程很快,其速率不是主要关注的问题.基于双膜理论及双电层理论,分析讨论了固态胺吸附传质过程,推导出了CO2总的传质速率方程,给出了影响速率的2个可调因素--温度及固态胺的含水量. 相似文献
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分析了潜艇舱室固态胺CO_2吸附及水蒸汽再生的反应机理,指出了CO_2水合反应和水合CO_2分解反应分别为吸附与再生过程的慢反应。在实际工况下,固态胺吸附CO_2的速率受传质控制,水蒸汽再生过程很快,其速率不是主要关注的问题。基于双膜理论及双电层理论,分析讨论了固态胺吸附传质过程,推导出了CO_2总的传质速率方程,给出了影响速率的两个可调因素--温度及固态胺的含水量。 相似文献
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三乙烯四胺在较优的反应条件,在温度150℃,反应时间4 h,固液比1∶20,与聚丙烯腈纤维反应,获得了聚丙烯腈-三乙烯四胺固态胺纤维。应用酸碱滴定法测得纤维的胺基含量为6.5 mmol/g,应用扫描电子显微镜和红外光谱仪表征纤维的表面形貌和官能团。在压强100 kPa、温度25.0℃、相对湿度80%、CO2浓度1.0%、纤维含水量100%条件下,30 min内测得纤维对CO2的吸附量为88.0 g/kg;103℃~105℃高温水蒸气再生10 min,循环吸附再生10次,纤维的再生效率为96.5%。 相似文献
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Identification and quantification of plankton bloom events in the Baltic Sea by continuous pCO2 and chlorophyll a measurements on a cargo ship 总被引:4,自引:1,他引:3
Continuous measurements of the surface water CO2 partial pressure (pCO2) and the chlorophyll a fluorescence were performed in the Baltic Sea using a fully automated measurement system deployed on a cargo ship. The ship commuted regularly at two day intervals between the Mecklenburg Bight (Luebeck) and the Gulf of Finland (Helsinki). The pCO2 data collected during June 2003 and September 2004 were used to identify biological production events such as the spring bloom and the midsummer cyanobacteria bloom in five different sub-regions. To quantify the net biomass production, the decrease of the total CO2, NCT (normalized to a uniform alkalinity), during the production periods was calculated using the pCO2, temperature and salinity records and the mean alkalinity. Taking into account the CO2 air/sea exchange and the formation of dissolved organic carbon, a simple mass balance yielded the net production of particulate organic carbon which represents the total biomass. The chlorophyll a concentrations obtained from the fluorescence data showed peaks that in most cases coincided with the production maxima and thus supported the interpretation of the pCO2 data. The production during both the spring bloom (2004) and the midsummer nitrogen fixation period (2003) increased by a factor of about three from the southwest to the northeast. For the spring bloom our estimates were significantly higher than those based on the winter nutrient supply and Redfield C / N and C / P ratios. This indicated the existence of additional nutrient sources such as dissolved organic nitrogen, early nitrogen fixation and preferential P mineralization. Midsummer NCT minima were observed only in 2003 and used to quantify the nitrogen fixation activity and to characterize its interannual variability. 相似文献
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In view of the wide range of estimates for the total primary production for the Southern Ocean south of the Subantarctic Front—current estimates range from 1.2 to 3.5 Gtonne C year−1—we have examined two indirect methods for assessing primary production. First, we have estimated the primary production needed to sustain the carbon requirements of the endotherm top predators in the ecosystem. Estimation of the carbon requirements for crabeater seals of about 7 Mtonne C year−1 is extrapolated to a value for all endotherm predators of 15–30 Mtonne C year−1. Current data indicate that 70–80% of the diet of this suite of predators is zooplankton (predominantly the euphausiid krill), making for highly efficient transfer from primary production to top predators. Our best estimate of Southern Ocean primary production by this method is of the order of 1.7 Gtonne C year−1, or an averaged areal primary production of about 30–40 g C m−2 year−1. Our second approach is to estimate primary production from the drawdown of inorganic nutrients, based on the limited suite of studies from which an annual nutrient deficit can be calculated. Again, this indicates annual primary production of the order of 1.5 Gtonne. Although both methods have inherent uncertainties, taken together they provide a relatively robust constraint on annual primary production. For both methods to underestimate primary production by the 1–1.5 Gtonne C implied by the higher current estimates, carbon export from the Southern Ocean pelagic ecosystem would need to be much higher than is normally found in other oceans. 相似文献
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Copepods were sampled by a multiple opening-closing net in the eastern Weddell Sea during various seasons (late winter/early spring, summer, autumn). Total copepod biomass integrated over the upper 1000 m varied seasonally between 1.7 mg C m−3 in late winter/early spring and 3.7 mg C m−3 in autumn. After the dark season the copepods were rather evenly distributed vertically and highest biomass levels were found in the mid-water layers between about 200 m and 500 m. By contrast, especially in summer but also in autumn copepod biomass concentrated in the uppermost water layer. A total of 64 calanoid species were identified in the upper 1000 m with maximum species numbers in the deepest layer. The large calanoids Calanus propinquus, Calanoides acutus, Metridia gerlachei, Euchaeta antarctica and the small calanoid Microcalanus pygmaeus prevailed and accounted for 60–70% of total copepod biomass, while the small poecilostomatoid Oncaea and the cyclopoid Oithona species comprised about 20%. Hence, the distribution pattern of the entire copepod biomass is strongly influenced by the life cycles of a few dominant species. 相似文献