潜艇舱室固态胺CO2清除技术的动力学分析

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。     

潜艇舱室固态胺CO2清除技术的动力学分析

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.     

固态胺纤维吸附CO2速率实验研究

模拟核潜艇环境工况条件,对固态胺纤维吸附CO2进行研究。实验测定了环境温度25℃、环境压力101kPa、气相中CO2含量0.5%时,固态胺纤维有水存在下吸附CO2的速率为5.57×10-4mmolig-1is-1。理论分析了吸附速率的控制过程,结果表明固态胺纤维吸附CO2总速率受双膜理论的液膜控制。     

固态胺清除二氧化碳技术研究

本文介绍了固态胺树脂的一般物化性能，研究了固态胺树脂作为可再生的二氧化碳吸收剂用于清除空气中低浓度（0．2％－0．4％）二氧化碳的原理及工艺技术，并与乙醇胺吸收CO2法进行性能比较。     

潜艇舱室固态胺CO2清除技术的动力学分析

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.     

新型固态胺二氧化碳吸收剂的制备及性能

采用丙烯酸酯类为单体,二乙烯苯为交联剂,悬浮聚合制备大孔交联共聚物基质,胺解制备了一种新型固态胺二氧化碳吸收剂一聚丙烯酰多乙烯多胺型树脂,研究了单体种类、功能基结构和含量、胺解条件等对树脂吸收二氧化碳性能的影响.模拟条件试验表明,该树脂吸收二氧化碳活性高,寿命长.     

潜艇舱室固态胺CO2清除技术的化学热力学分析

依据有关文献提供的热力学状态函数值,分水蒸气再生和真空再生2种工况,近似计算了标准状态和实际状况下固态胺吸附与解吸CO2反应的平衡与程度,并讨论了温度、湿度和CO2分压等对其所产生的影响。     

潜艇舱室固态胺CO2清除技术的化学热力学分析

依据有关文献提供的热力学状态函数值,分水蒸汽再生和真空再生两种工况,近似计算了标准状态和实际状况下固态胺吸附与解吸CO2反应的平衡与程度,并讨论了温度、湿度和二氧化碳分压等对其所产生的影响。     

潜艇舱室固态胺CO2清除技术的基础理论分析

简述了国内外潜艇舱室CO2的清除方法,指出了固态胺技术将是未来发展的主要方向之一,分析了固态胺吸附与再生的理论基础,给出了成功应用该技术需要优先解决的系列问题。     

载人深潜器二氧化碳清除方式研究

比较了各种类型水下运载器如潜艇、载人深潜器等对载人密闭舱室内二氧化碳气体浓度的不同要求。针对载人深潜器载人舱内的客观条件,从动力、空间大小、二氧化碳浓度要求等方面分析其对二氧化碳清除的特殊要求。分析了常见的几种密闭环境二氧化碳清除方式如一乙醇胺、固态胺、分子筛、碱石灰、氢氧化锂等技术各自的优缺点,在此基础上,开发出一种二氧化碳清除技术及研制了样机。使用该样机进行封闭空间内的有人二氧化碳吸收试验,以验证该项技术的效果。试验结果证明了这种技术的有效性。在完成样机试验后,又将样机随潜水器进行海试。海试的圆满成功进一步证实了样机的有效性。     

CO2脱除机在白灵菇种植场所的应用研究

白灵菇是一种营养丰富的食用菌,目前在国内市场供不应求,而在其反季节种植过程中,存在着冷库内CO2浓度逐步升高,影响产量和形状的问题。为解决这些问题,介绍了新研制的一种新型的CO2脱除机,可以较好的控制反季种植中冷库内的CO2浓度。测试了冷库内不同生长阶段白灵菇产生的CO2浓度,考察了冷库内不同高度时的CO2浓度的梯度变化,以及在试验中后期冷库内CO2浓度的变化速度。提出了白灵菇反季节种植冷库中CO2脱除机的运行方式。     

Identification and quantification of plankton bloom events in the Baltic Sea by continuous pCO2 and chlorophyll a measurements on a cargo ship

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, ^NC_T (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 ^NC_T minima were observed only in 2003 and used to quantify the nitrogen fixation activity and to characterize its interannual variability.     

LiOH药粒的粉尘抑制技术现状与展望

LiOH是密闭空间中一种重要的CO2吸收剂。针对LiOH药粒在使用过程中易产生刺激性粉尘的缺点,本文主要介绍了几种LiOH药粒粉尘抑制技术的技术原理,分析了各种技术的主要特点,展望了LiOH粉尘抑制技术的研究前景。     

CO2电催化还原的研究

以混合的金属氧化物RuO_2、TiO_2、Ag_2O和SnO_2对钛表面进行了修饰,得到了四个不同氧化物组成的钛电极,即RuO_2 TiO_2/Ti(35:65,A)、RuO_2 TiO_2/Ti(25:75,B)、RuO_2 TiO_2 Ag_2O/Ti(C)和RuO_2 TiO_2 SnO2/Ti(D),采用循环伏安法研究了其常温常压下在0.1mol/L的KHCO3水溶液中的电化学行为,在-900mV的恒定电位下进行了CO2的还原,分析了电极的稳定性和还原产物的情况。结果表明,金属氧化物电极对CO2还原产生了很好的催化作用,-900mV下对甲酸和甲醇有高的选择性,还原的液相产物中仅发现了甲酸和甲醇,电极A、B、C和D上生成甲酸和甲醇的总电流效率分别为84.4%、57.4%、93.1%和88.1%,且长时间电解过程中电极具有很好的稳定性,是有很好应用前景的催化电极材料。     

Carbonate chemistry dynamics and carbon dioxide fluxes across the atmosphere–ice–water interfaces in the Arctic Ocean: Pacific sector of the Arctic

Climatic changes in the Northern Hemisphere have led to remarkable environmental changes in the Arctic Ocean, which is surrounded by permafrost. These changes include significant shrinking of sea-ice cover in summer, increased time between sea-ice break-up and freeze-up, and Arctic surface water freshening and warming associated with melting sea-ice, thawing permafrost, and increased runoff. These changes are commonly attributed to the greenhouse effect resulting from increased atmospheric carbon dioxide (CO₂) concentration and other non-CO₂ radiatively active gases (methane, nitrous oxide). The greenhouse effect should be most pronounced in the Arctic where the largest air CO₂ concentrations and winter–summer variations in the world for a clean background environment were detected. However, the air–land–shelf interaction in the Arctic has a substantial impact on the composition of the overlying atmosphere; as the permafrost thaws, a significant amount of old terrestrial carbon becomes available for biogeochemical cycling and oxidation to CO₂. The Arctic Ocean's role in determining regional CO₂ balance has been ignored, because of its small size (only  4% of the world ocean area) and because its continuous sea-ice cover is considered to impede gaseous exchange with the atmosphere so efficiently that no global climate models include CO₂ exchange over sea-ice. In this paper we show that: (1) the Arctic shelf seas (the Laptev and East-Siberian seas) may become a strong source of atmospheric CO₂ because of oxidation of bio-available eroded terrestrial carbon and river transport; (2) the Chukchi Sea shelf exhibits the strong uptake of atmospheric CO₂; (3) the sea-ice melt ponds and open brine channels form an important spring/summer air CO₂ sink that also must be included in any Arctic regional CO₂ budget. Both the direction and amount of CO₂ transfer between air and sea during open water season may be different from transfer during freezing and thawing, or during winter when CO₂ accumulates beneath Arctic sea-ice; (4) direct measurements beneath the sea ice gave two initial results. First, a drastic pCO₂ decrease from 410 μatm to 288 μatm, which was recorded in February–March beneath the fast ice near Barrow using the SAMI-CO₂ sensor, may reflect increased photosynthetic activity beneath sea-ice just after polar sunrise. Second, new measurements made in summer 2005 beneath the sea ice in the Central Basin show relatively high values of pCO₂ ranging between 425 μatm and 475 μatm, values, which are larger than the mean atmospheric value in the Arctic in summertime. The sources of those high values are supposed to be: high rates of bacterial respiration, import of the Upper Halocline Water (UHW) from the Chukchi Sea (CS) where values of pCO₂ range between 400 and 600 μatm, a contribution from the Lena river plume, or any combination of these sources.     

Atmospheric CO2 measurements and error analysis on seasonal air–sea CO2 fluxes in the Bay of Biscay

Atmospheric molar fraction of CO₂ (xCO₂^atm) measurements obtained on board of ships of opportunity are used to parameterize the seasonal cycle of atmospheric xCO₂ (xCO₂^atm) in three regions of the eastern North Atlantic (Galician and French offshore and Bay of Biscay). Three selection criteria are established to eliminate spurious values and identify xCO₂^atm data representative of atmospheric background values. The filtered data set is fitted to seasonal curve, consisting of an annual trend plus a seasonal cycle. Although the fitted curves are consistent with the seasonal evolution of xCO₂^atm data series from land meteorological stations, only ship-board measurements can report the presence of winter xCO₂^atm minimum on Bay of Biscay. Weekly air–sea CO₂ flux differences (mmol C·m^− 2 day^− 1) produced by the several options of xCO₂^atm usually used (ship-board measurements, data from land meteorological stations and annually averaged values) were calculated in Bay of Biscay throughout 2003. Flux error using fitted seasonal curve relative to on board measurements was minimal, whereas land stations and annual means yielded random (− 0.2 ± 0.3 mmol C·m^− 2·day^− 1) and systematic (− 0.1 ± 0.4 mmol C·m^− 2 day^− 1), respectively. The effect of different available sources of sea level pressure, wind speed and transfer velocity were also evaluated. Wind speed and transfer velocity parameters are found as the most critical choice in the estimate of CO₂ fluxes reaching a flux uncertainty of 7 mmol C·m^− 2·day^− 1 during springtime. The atmospheric pressure shows a notable relative effect during summertime although its influence is quantitatively slight on annual scale (0.3 ± 0.2 mmol C·m^− 2·day^− 1). All results confirms the role of the Bay of Biscay as CO₂ sink for the 2003 with an annual mean CO₂ flux around − 5 ± 5 mmol C m^− 2 day^− 1.