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11.
While there is already a comprehensive understanding of the effects of environmental variables, such as dissolved oxygen, temperature and salinity, on the structure, biomass and metabolism of aquatic biota in estuarine habitats, the effect of sedimentation, a harmful underlying factor, remains unclear. The aim of this study was to assess the differences in fish assemblages along the freshwater to salt water gradient of a large tropical estuary, and to evaluate the effects on them of habitat disturbance associated with shallow water sedimentation in the intertidal areas. Fish and environmental variables were recorded in the upper, middle and lower salinity zones of the estuary at ebb tide in both the dry and wet seasons. Sediment samples associated with different levels of habitat disturbance were analysed using granulometry, and their organic content and dissolved oxygen levels were quantified. Water temperature, salinity, pH and dissolved oxygen levels were also measured. Habitat disturbance was found to be correlated with the density, biomass and richness of fish assemblages. A total of 77 species were recorded, forming two distinct fish assemblages, with the Eleotridae family dominating in the upper zone, and Gerreidae, Gobiidae and Tetraodontidae the most common in the middle and lower estuary. Changes in the structure of fish assemblages, including reductions in density, biomass and richness, were associated with disturbance to natural features, where muddy sediment was replaced by sandy sediment and the quantity of organic matter fell. Atherinella brasiliensis was the species which showed a preference for the disturbed areas in the middle and lower zones, while Dormitator maculatus showed a preference for them in the upper estuary. They may be taken as indicators of habitat disturbance due to shallow sedimentation. 相似文献
12.
AbstractBlast response of submerged pipelines has been a research focus in recent years. In this article, a three-dimensional numerical model is established to investigate dynamic response of pipelines due to underwater explosion. The u–p approximation is integrated into finite element method (FEM) to simulate pore water effect in the seabed. Numerical continuity between hydraulic pressure in the flow field and pore pressure in the marine sediment is guaranteed to realize the blast response of submerged pipelines in ocean environment. Both fluid–structure interaction (FSI) and pipeline–seabed interaction (PSI) have been considered in the proposed model simultaneously. A comprehensive parametric study is carried out after validation of the present model with test data from underground explosion and underwater explosion, respectively. The effect of embedment depth, TNT equivalent, stand-off distance, pipeline diameter, and pipeline thickness to blast response of the submerged pipelines is investigated based on numerical results. Variation of deformation patterns and stress distribution of the pipeline with various installation and structure parameters has been illustrated and discussed to facilitate engineering practice. 相似文献
13.
选取史灌河流域上游黄泥庄站以上集水区域为研究流域,以地面站点观测为基准数据,评估TRMM 3B42V7版本卫星降水数据的精度,并采用上述两种降水数据驱动栅格型新安江模型,模拟黄泥庄站日径流和月径流过程。结果表明:2001~2010年TRMM 3B42V7降水数据与雨量站数据累积量的偏差不大,仅为1.71%,但相关系数较低,采用TRMM降水数据模拟的日径流能基本再现黄泥庄站的日径流过程,但对洪峰的模拟精度较低;TRMM月降水数据精度较高,相关系数为0.96,能够较为精确地模拟黄泥庄站的月径流过程。 相似文献
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Systematic studies of the ophiolites and associated volcanics stretching more than 1500 km from the Derni-Nanping-Pipasi-Kangxian area in the west to the Qingshuihe area of the south Dabie Mountains in the east indicate the existence of a suture zone (the Mianl(u)e suture)and a vanished paleo-ocean basin (the Mianlue paleo-ocean basin) in the region. From west to east, ophiolitic melange associations distribute discontinuously along the suture. Rock assemblages include ophiolite, island arc and oceanic island rock series. The Mianlue paleo-ocean basin experienced its major formation and expending episode during the Carboniferous-Permian period. The finding of the suture zone and the paleo-ocean basin is tectonically significant in timing the collision between the North China-Qinling and Yangtze blocks and determining the formation and evolution of the Qinling orogenic belt. 相似文献
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Meng Fancong Yang Jingsui Zhang Jianxin Wu Cailai Shi Rendeng Li Haibing Li Tianfu WT ”BX 《地学前缘》2000,(Z1)
CRETACEOUS (?) VOLCANIC ROCKS ON THE NORTH END OF THE ALTYN TAGH FAULT:CHARACTERISTICS AND TECTONIC IMPLICATIONS1 PanGuitang ,WangPeisheng ,XuYaorong ,etal.CenozoictectonicevolutionofQinghai Tibetplateau[M] .Beijing :Geo logicalPublishingHouse ,1990 .32~ 6 8(inChinese) .
2 ZhengXiangshen ,BianQiantao,ZhengJiankang .OntheCenozoicvolcanicrocksinHohxildisreict,QinghaiProvince[A] .ActaPetrologicaSinica,1996 ,12 ( 4) :530~ 54 5(inChinesewith… 相似文献
19.
编队飞行是多颗卫星在共同控制律下动力学状态的耦合。利用卫星编队来实现光学稀疏孔径,是下一代空间光学遥感发展的新方向。阐述了光学稀疏孔径的概念及成像原理,讨论了空间光学遥感成像的干涉模式选择问题,并分析了菲索干涉对卫星编队的要求。 相似文献
20.
张北6.2级地震序列特征 总被引:1,自引:0,他引:1
1998年1月10日张北6.2级地震后,我们根据《地震现场工作大纲和震情分析指南》用b值h值、u值,k值对该次地震序列进行了综合判定。结果认为此次地震为主震余震型。张北地震序列在衰减过程中出现以4级地震为峰值有节律的起伏,在时间上有较规则的准周期,且每一组起伏前密集-平静规律十分明显。 相似文献