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901.
Carbon cycling in the Weddell Sea was investigated during the ANT X/7 cruise with `FS Polarstern' December 1992–January 1993. Samples were taken on a cross section from Kapp Norvegia to Joinville Island, and on a section from the Larsen Ice Shelf to the northeast. The following quantities were measured: total carbon dioxide (TCO2), fluorescence from humic substances and total organic carbon. The distribution of TCO2 was strongly positively correlated to the time elapsed since the various water masses were last ventilated. In general, humic substance fluorescence was positively correlated with TCO2, with the exception of the productive part of the western Weddell Sea, where the correlation was negative in the surface mixed layer. The increased fluorescence at the surface is suggested to be a result of biological production. The distribution of total organic carbon showed less structure, since this quantity includes a particulate component, which is subject to dispersion processes different from those of the dissolved components TCO2 and humic substances. The mean total organic carbon concentration below the surface mixed layer was 50 μmol l−1. At some stations, a steep TOC maximum around 2000 m depth was observed. This was interpreted to result from mass sinking of phytoplankton blooms. Total organic carbon had a maximum in surface water, and at some stations also a second subsurface maximum. In the Warm Deep Water (WDW), TCO2 and fluorescence had their maximum values, while total organic carbon tended to be low. In low productivity surface water in the eastern part of the Kapp Norvegia–Joinville Island section, the lowest flourescence was found. Surface water is eventually formed from Warm Deep Water, which had the highest fluorescence values, and therefore it is concluded that humic substances were removed in situ from surface water. In the central area of the Weddell Sea, TCO2 and fluorescence showed the highest Warm Deep Water maxima, while total organic carbon was low. The Warm Deep Water in this area is part of the so-called Central Intermediate Water which circulates for a long time within the Weddell Gyre. Reduced total organic carbon, which coincides with the most pronounced Central Intermediate Water characteristics, and high TCO2 can thus both be accounted for by continued degradation of organic matter in this water mass. The associated fluorescence maximum implies that humic substances are also produced during mineralisation. Recently formed bottom water, by contrast, could be seen as patches of low TCO2, low fluorescence and high total organic carbon along the western slope of the Weddell Sea. 相似文献
902.
周贤全 《变流技术与电力牵引》2005,(5):13-17
从运用的观点来看,受电弓弓头碳基滑板的安装方法是非常重要的.碳滑板一般用带贴紧钢套包层的楔型榫制成,或用能夹紧整个碳滑板的金属装配架制作,用螺栓固定在受电弓弓头上.作者开发了其他3种新的安装方法.并阐述了日本在过去20多年里对碳基滑板材料所进行的开发,以及对所开发的安装方法进行试验室试验或现场试验的结果. 相似文献
903.
904.
采用四氯化碳为有机溶剂代替酒精,清洗掉了雷达机柜内金属线路板表面铬金属膜上的甲基硅油保护液,使三防漆能够均匀地涂敷在金属线路板表面,可以充分发挥三防漆对雷达机柜内电子装备的防护作用。从实用性和化学热力学的角度分析了选择四氯化碳作为甲基硅油清洗剂的原因。 相似文献
905.
潜艇密闭舱室二氧化碳清除措施探析 总被引:3,自引:0,他引:3
二氧化碳是潜艇舱室的主要有害气体,主要由人员呼吸产生。介绍了潜艇密闭舱室二氧化碳的几种清除措施的原理和优缺点,分析了国外潜艇二氧化碳清除技术的发展过程、最新技术和未来发展趋势。 相似文献
906.
本文介绍了MARPOL73/78公约附则VI《防止船舶造成大气污染规则》,概括了船用柴油机排放控制技术,主要阐述了新型船用低速电控柴油机利用共轨系统控制并优化燃烧过程,降低排放的措施与试验,并得出船用电控柴油机的排放完全符合IMO排放规则的结论。 相似文献
907.
908.
简要介绍了NJ2机车电子燃油喷射系统的工作原理、组成和功用,列举了该型机车在青藏高原实测的燃油消耗率和排放指标,对NJ2机车和DF4B机车的实际燃油单耗进行了对比,表明NJ2机车燃烧过程得到优化,燃油消耗率较低。 相似文献
909.
Late-Quaternary changes in productivity of the Southern Ocean 总被引:1,自引:0,他引:1
R.F. Anderson N. Kumar R.A. Mortlock P.N. Froelich P. Kubik B. Dittrich-Hannen M. Suter 《Journal of Marine Systems》1998,17(1-4)
Paleoceanographic records based on new proxies of export production have been constructed for the South Atlantic sector of the Southern Ocean. A radionuclide-ratio proxy of particle flux (10Be/230Th) and the accumulation rate of authigenic uranium, which responds to the flux of organic carbon to the sea bed, both indicate a dramatic increase, compared to the present, in the export production of the Subantarctic zone (approximately the region between the present-day positions of the Subtropical Convergence and the Antarctic Polar Front) during glacial periods. If the South Atlantic is representative of the entire Southern Ocean, then export production in the Southern Ocean during the Last Glacial Maximum was substantially greater than at present. Previous studies, focusing on the burial of biogenic opal, failed to recognize the glacial increase in export production of the Southern Ocean because of a strong non-linearity between accumulation rates of opal and of organic carbon. 相似文献
910.