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71.
CO2减排是国际关注的热点问题。将CO2注入地下地质构造永久封存是CO2减排的有效途径。挪威Sleipner气田盐水层CO2封存工程是世界上第一个完全为了对CO2进行地质封存而实施的商业项目,为CO2的海上捕集、地质存储及其监测提供了极其宝贵的经验。详细介绍Sleipner气田海上平台MDEA法天然气分离CO2技术及CO2高压密相回注工艺,为我国南海莺歌海盆地天然气田伴生二氧化碳的埋存和利用提供参考。 相似文献
72.
介绍蓄电池分类及特点,放电浓度、硫酸浓度、温度等是影响船用铅酸蓄电池使用寿命的主要因素;提出在日常使用中要常检查铅酸蓄电池在支架上的固定螺栓,保持蓄电池盖上的气孔畅通无阻等正确的维护方法。 相似文献
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基于实际运用中深圳地铁车辆紧急启动控制电路及操作方法存在的问题,简要介绍该车辆紧急启动以及蓄电池充电机控制电路的基本原理,分析了电路上及操作方法上存在的问题,提出了相应的改进方法。 相似文献
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Igor P. Semiletov Irina I. Pipko Irina Repina Natalia E. Shakhova 《Journal of Marine Systems》2007,66(1-4):204
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. 相似文献
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本文对触摸屏MT6000系列进行了介绍,并描述了电池管理系统组成及触摸屏MT6070iH在该系统中的应用,通过实例讨论了MT6070iH的设计开发方法。 相似文献
78.
为了从大量记录筛选出一致性较好的电池进行配组,本文提出一种基于SQL数据库的方案实现电池配组功能,无需复杂的算法,开发效率高,具有良好可扩展性并支持标准用户接口,并在实际应用中取得了良好效果。 相似文献
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