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71.
We investigated the water structure and nutrient distribution in the Suruga Bay from April 2000 to July 2002, especially the Offshore Water, which occupies a large part of the bay. The maximum salinity in the upper 200 m varied between 34.49 and 34.71, indicating a temporal change in the influence of Kuroshio Water on the Offshore Water. Seasonal variation in nutrient concentrations was largest from surface to 50 m. On the other hand, the variance in nutrient concentrations within each season was largest in the subsurface layer of 100–300 m in spring, summer and fall. In the Offshore Water, the change of nutrients was negatively correlated with that of salinity in each season. This suggests that an increasing intrusion of saline water brings about a lower nutrient concentration in the Offshore Water. Likewise, negative correlations were observed between the change of the maximum salinity and chlorophyll a (Δ [chl.a-int])/nutrients integrated in the upper 200 m. Δ[chl.a-int] was significantly correlated with the changes of nitrate and phosphorus, but there were no significant correlations between Δ[chl.a-int] and the change of silicate. These results suggest that the concentrations of chlorophyll a and nutrients in the Offshore Water were decreased due to the increasing intrusion of Kuroshio Water. The Offshore Water is likely to be related to the regulation of primary production by nitrate.  相似文献   
72.
Surface waves are the roughness element of the ocean surface. The parameterization of the drag coefficient of the ocean surface is simplified by referencing to wind speed at an elevation proportional to the characteristic wavelength. The dynamic roughness is analytically related to the drag coefficient. Under the assumption of fetch limited wave growth condition, various empirical functions of the dynamic roughness can be converted to equivalent expressions for comparison. For datasets covering a wide range of the dimensionless frequency (inverse wave age), it is important to account for the variable rate of wave development at different wave ages. As a result, the dependence of the Charnock parameter on wave age is nonmonotonic. Finally, the analysis presented here suggests that the significant wave steepness is a sensitive property of the ocean surface and a single variable normalization of the dynamic roughness using a wavelength or wave height parameter actually produces more robust functions than bi-variable normalizations using wave height and wave slope.  相似文献   
73.
Total mass flux, size distribution of sediment particles and some chemical components such as total carbon (TC), total nitrogen (TN) and calcium carbonate (CaCO3) were monitored monthly using a multi-cup sediment traps at seven coral reef sites (6 reef flat and 1 reef slope) of the Marine Protected Areas around Ishigaki, Kohama, Kuroshima and Iriomote Islands in the southern Ryukyus, Japan from September 2000 to September 2001. The size distribution of trapped sediments revealed mostly uni-modal fine sand to mud in the reef flat and gravelly to coarse sand in the reef slope. The total mass flux ranged between 0.54 to 872 gm−2d−1, and showed a pronounced seasonality (high in summer-autumn and low in spring) at each site, which was consistent with the rainfall and typhoon regime. Exceptionally high values were observed on the reef slope (Iriomote) in February–March 2001 (1533 gm−2d−1) owing to a large amount of bottom sediment re-suspension. On the reef flat (Todoroki South and North; Ishigaki), values obtained in July–August 2001 (872 gm−2d−1) and August–September 2001 (800 gm− 2d−1) indicate the high terrestrial discharge from Todoroki River. Trapped sediment particles consist of CaCO3 (1.2–27.1%) and a non-carbonate fraction (98.8–72.9%), which contains total carbon (4.9–26%), carbonate carbon (CO2-C) (0.2–3.1%) and non-carbonate carbon (NC-C) (7.9–25.6%). Total nitrogen content was in the range 0.02–0.48%. TN is contained mainly in the carbonate fraction and NC-C may be contained in the non-carbonate fraction. The low TN/OC ratio of the trapped sediments suggests that they were mostly of terrestrial origin and that both fractions migrated. The high total mass flux derived from Todoroki River exceeded the threshold at which a lethal effect on coral community is caused. The results stress the importance of conducting seasonal studies of sedimentation over more than one year and at more than one location in south Japan coral reef ecosystems to gain an understanding of the processes controlling the total mass fluxes and their nutrients content, also to develop an awareness of how to prevent the damage of coral reef ecosystems and, if it does occur, to allow mitigation measures to be undertaken.  相似文献   
74.
Recent observations suggest that the annual mean southward transport of the East Sakhalin Current (ESC) is significantly larger than the annual mean Sverdrup transport. Motivated by this observational result, transport of a western boundary current has been investigated using a simple numerical model with a western slope. This transport is defined as the instantaneous barotropic transport integrated from the western boundary to the offshore point where the barotropic velocity vanishes. The model, forced by seasonally varying wind stress, exhibits an annual mean of the western boundary current transport that is larger than that of the Sverdrup transport, as observed. The southward transport from October to March in the model nearly equals the instantaneous Sverdrup transport, while the southward transport from April to September decreases slowly. Although the Sverdrup transport in July vanishes, the southward transport in summer nearly maintains the annual mean Sverdrup transport, because the barotropic Rossby wave cannot intrude on the western slope. This summer transport causes the larger annual mean. Although there are some uncertainties in the estimation of the Sverdrup transport in the Sea of Okhotsk, the seasonal variation of the southward transport in the model is qualitatively similar to the observations.  相似文献   
75.
厦门港潮汐水流及浑水悬沙整体物理模型于1989年建成后,已进行了不少有意义的试验研究工作,取得较好效果。本文主要介绍模型的设计思想、相似准则、浑水悬沙相似理论的探讨、模型设计方法以及模型沙的选择等。  相似文献   
76.
上海潮滩沉积物重金属的动力学累积特征   总被引:65,自引:3,他引:65  
1993年7-8月,在上海长江口南岸和杭州湾北岸淤泥质潮滩不同地貌部位,采集表层沉积物和柱状沉积物样品,采用筛析法,离心法、火焰原子吸收法,^210Pb法等分别对沉积物粒度、重金属总量,不同粒级重金属含量以及沉积速率等进行了和测定。结果表明,潮滩沉积物重金属的空间分布格局并不受沿岸排污的直接影响,而与沉积动力作用密切相关。在水动力条件较弱的淤涨岸段和高潮滩部位,伴随着细颗粒起泥沙的大量堆积,Cu,  相似文献   
77.
本文介绍了智能潜器集成仿真系统的硬、软件结构.通过这一系统所展示的水下虚拟仿真环境能够在研究和开发智能潜器的控制体系结构、潜器载体的水动力学、信息融合和目标识别等工作中发挥巨大作用  相似文献   
78.
主要对1983-1996年间关于鱼类生长激素的体内代谢、分泌调控和作用机制的研究进展予以综合评述。通过鱼类划性放射免疫测定法的建立和体风代谢动力学研究,证实,外源生长激素在鱼体内不会产生积累。鱼类生长激素的分泌调控受下丘脑分泌的生长激素释放因子(GHRF)和释放抑制因子(SRIF)的双重;促性腺激素释放激素(GnRH)、雌二醇(E2)、促甲状腺素释放激素(TRH)和神经肽(NYP)对鱼类生长激素的  相似文献   
79.
有机氯农药(DDT,BHC)和多氯联苯(PCBs)是人工合成的有机氯化合物。它们的化学性质稳定,在环境中能持久地残留并不易受环境中各种因素的作用而降解,它们在生物体内的累积和生物链中的浓缩已构成对人类和生态系统的潜在危害,早已引起世界各国的关注,并公认为全球性的环境污染物。许多国家的学者对不同海区、各大洋海水、沿岸海水、沉积物以及海洋生物体内的DDT, BHC, PCBs作了广泛深入的调查研究(Elear, 1976; Edwand et al, 1975; Ehrhardt, 1981; Harvey, 1973; Osterroht, 1977;Robert, 1976)。我国对近海海域有机氯农药污染状况作过一些调查,但对多氯联苯未见有过报道。、1980年8月作者在渤海湾采集了26个站位的海水样品,22个站位的沉积物样品和8个毛蚶(Arasubcrenata Lischke)样品,分析了其中DDT, BHC, PCBs的含量水平,并对其在渤海湾中的分布特征作了初步探讨。  相似文献   
80.
黄、渤海海岸风沙地貌类型及其分布规律和发育模式   总被引:24,自引:0,他引:24  
于1990-1994年,对黄,渤海海岸风沙地貌,风沙沉积,风沙灾害和土地沙漠化现象进行详细的外业调查,测量和填图,在此基础上,利用GIS技术原理,对海岸岗沙地貌进行系统的分类研究,对海岸风沙地貌分布规律和发育模式进行较深入的探讨,结果表明,研究区风沙地貌,风沙灾害和土地沙漠化现象主要分布在冬,春季气候干旱,风力强而持久,砂源丰富的渤海海岸和山东半岛半岸的砂质海岸地区,海岸沙丘和风成砂地总面积达70  相似文献   
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