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101.
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冰海结构物通常装备抗冰锥等倾斜面的抗冰结构物,用来减小平整冰移动产生的推挤载荷。平整冰推挤载荷是冰海结构物的重要设计技术指标,准确模拟平整冰推挤结构物的载荷特征和破碎冰堆积形态等规律具有重要意义。本文采用FEM-SPH耦合方法和有限元法分别模拟了平整冰推挤抗冰锥结构的过程和现象,分析了抗冰锥水线面直径对碎冰堆积形态及推挤载荷的影响规律。研究表明,与有限元法相比,FEM-SPH耦合方法不仅可以准确预报平整冰推挤结构的动态载荷,还可以直观再现破碎冰的堆积现象,有助于理解和分析平整冰与结构物的相互作用规律。本文的FEM-SPH耦合算法模型和分析结论可为研究和设计冰海结构物提供参考。 相似文献
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韩国籍船舶“依祖玛”轮舵系损坏严重,经过厂方检查分析,确定了简便实用的维修方案,并对换新部件中国内没有的材料进行了替换,确保了周期,符合船东要求和船检的规范。 相似文献
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Using three years (2003 to 2005) of MODIS-Aqua normalized water-leaving radiance at 551 nm this paper shows a fortnightly cycle in the Tagus estuary turbid plume. The Tagus estuary is one of the largest estuaries of the west coast of Europe and is located in the most populated area of Portugal, including the capital Lisbon. The turbid plume has been detected by the backscattering characteristics of the surface waters in the vicinity of the estuary mouth. In fortnightly scales, the turbid plume has smaller dimensions during and after neap tides and higher dimensions during and after spring tides. This is most probably associated with the fortnightly spring–neap tidal cycle and the consequent increase in turbidity inside the estuary during spring tides. During the summer weak spring tides (tidal amplitude approximately 2.5 m) no turbid plume is observed for an entire fortnightly cycle. Outside the summer months, precipitation, river discharge and winds, were found to increase the turbid area, but the fortnightly cycle appears to be superimposed on the large time-scale variability, and present throughout the year. 相似文献
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介绍了一种以树脂胶粘剂为介质的新型缓粘结预应力体系的试验研究,其中包括能满足该体系要求的固化期在3、6、12个月左右、抗压强度50 MPa以上的胶粘剂组分及物理力学性能的研究;对预应力筋在不同时间张拉锚固作业中的κ和μ进行测量;缓粘结预应力筋在应力状态下进行了腐蚀试验;采用缓粘结预应力筋制作了8根预应力受弯构件进行试验,并与同条件制作的有粘结、无粘结预应力梁进行比较。结果表明,胶粘剂固化后的缓粘结预应力构件的工作性能,几乎和有粘结预应力构件相同。通过几个缓粘结预应力工程的施工,表明该体系的施工工艺与无粘结预应力施工工艺相近,简便易行。该体系将后张法中的无粘结和有粘结预应力混凝土体系相结合,使传统的预应力技术有了更新的发展。 相似文献
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自2008年第3季度以来,在历史罕见的全球经济危机的冲击下,美国、日本和西欧等发达国家和地区经济急剧下滑,巴西和中国等发展中国家经济也受到不同程度的影响。 相似文献
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Macrobenthic surveys are an expensive, slow and labour intensive means to establish the health of benthic communities. Sediment profile imagery (SPI) is a means of rapid reconnaissance for monitoring large areas of the benthos. SPI has often been used to monitor gross anthropogenic disturbance. The aim of this study is to determine if SPI can be used as a tool to reliably map change in communities along natural estuarine gradients. Macrobenthic sampling was carried out at five stations along an established estuarine gradient. This faunal data was analysed using standard multivariate techniques and to ground truth a concurrent SPI survey. Faunal analysis showed that habitat quality in Inner Galway Bay was generally good, with some localised disturbance from the River Corrib and the sewage out flow exterior to the city dock. Four distinct groups were identified with a degree of overlap occurring between stations 3 and 4. While existing SPI indices mapped habitat quality in the same manner as the faunal data for end member stations, the level of distinction between the habitats of an intermediate staging was found to be poor. This lack of distinction amongst the stage 2 and 3 stations was overcome by developing a tailored index, the Galway Bay index of habitat quality (GBHQ). This index was derived from the 5 observed variables in the SPI data that were determined to best match the faunal distribution by permutative mantel testing. The 5 observed variables from the SPI data were the depth of the apparent redox potential discontinuity (aRPD), the depth of penetration by the prism, and the presence/absence of infauna, surface faecal pellet layer and biogenic mounding. The GBHQ was able to distinguish between the 5 stations to a greater extent than previously described indices, showing clearly the separate groupings defined by the faunal data. The index was tested on a follow up SPI survey and shown to be applicable in mapping a broader range of habitats in Galway Bay. Indices generated for localised mapping of estuarine gradients should be derived from observed features and be ground truthed using faunal data. Some aspects of the GBHQ should be generally applicable to fine grained boreal estuarine sediments (aRPD/penetration), while others may be of limited utility in other locations depending on the digging characteristics of the particular SPI camera, and local factors influencing the persistence of biogenic features in the profile. This derivation technique provides a simple way to optimise SPI to particular studies and localities. 相似文献