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871.
A time-series sediment trap was deployed from December 1994 to February 2002 at the mouth of Tokyo Bay (35°03′ N, 139°40′
E; water depth, 850 m). Sinking particles were obtained with a time interval of one week at a depth of approximately 100 m
above the sea floor. Observed total mass fluxes varied from 3.3 to 226.7 g/m2/day with an average of 28.0 g/m2/day. Concentrations of rare earth elements, Al, Ca and Si in particulate materials were measured. The combustible fraction
at 450°C is assumed to be equivalent to the organic matter content. Contents of biogenic materials, namely organic matter,
opal and calcium carbonate, were about 30% and the content of lithogenic material was about 70%. Using La/Yb ratios of particles
from the sediment trap and Tama-gawa River and surface sediment of Tokyo Bay, it was estimated that about 50% of the lithogenic
particles collected in the sediment trap at the mouth of Tokyo Bay originated from resuspended surface sediment in Tokyo Bay.
An increasing trend of Opal/CaCO3 ratio in the sinking particles was found in the spring season. It is suggested that the relative increase of diatoms is due
to the decreasing dissolved inorganic nitrogen input into Tokyo Bay. 相似文献
872.
873.
Numerical experiments were performed in order to investigate the effects of variations of the transport through the Korea/Tsushima Strait, an inlet of the Japan/East Sea, on the upper layer circulation in the JES based on a 10-month transport observation from May 1999 to March 2000 (Perkins et al., 2000). All external forcings to the model were annual mean fields, except the transport variation through the Korea Strait. In the experiments where the periodic variation of the transport repeated continuously sinusoidally by several periods, strong variability of sea surface height (SSH) was detected in the region extending from the Korea Strait to the Japanese coast due to the geostrophy of the buoyancy forcing at the Korea Strait. The region along the Korean coast is more sensitive to the long-term variations than the short-term (≤60-day period) ones. In two experiments forced by realistic and monthly mean transport, the difference of rms of sea surface height was largest at the Japanese coast and relatively large at the East Korean Warm Current separation region (128∼130°E, 39∼41°N) and to the east of Yamato Rise. The distribution of difference of eddy kinetic energy at 100 m depth between the two experiments was similar to that of the rms of SSH. In the distributions of mean SSH and mean kinetic energy at 100 m depth the realistic transport invokes eddy variability to interact with mean current resulting in the changes of the mean SSH and the mean kinetic energy at the East Korean Warm Current separation region, but it does not produce conspicuous changes in the mean fields of entire JES compared with the mean fields forced by the seasonal transport. 相似文献
874.
二维悬沙长期输运速度的定义和机理分析 总被引:2,自引:0,他引:2
将悬沙和水体的长期输运分离研究,给出二维悬沙长期输运速度的定义。从理论上分析了各种物理过程对二维悬沙长期输运速度的影响机理。采用部分观测资料,对长江口二维悬沙长期输运速度及其机理作了初步的计算分析,结果表明:在最大浑浊带,悬沙和水体长期输运有明显的差别;在描述悬沙长期输运时,二维悬沙长期输运速度比二维水体长期输运速度更合理;潮泵作用和垂向切变作用是造成两者差别的主要原因。 相似文献
875.
876.
An even–odd signal decomposition is performed on a complex shoreline having a longshore sediment transport gradient. The expected impact of erosion due to a navigation channel and structures is discussed and implications of the transport gradient on the decomposed shoreline signal are noted. 相似文献
877.
在该海域潮流计算的基础上,利用有限元法建立了二维的拉格朗日余流模型,得出了威海及烟台南部海域的拉格朗日余流分布。跟踪了文登、乳山、海阳、莱阳近岸主要排污口的污水输运轨迹,为沿岸县市污水排放的选址提供理论依据。 相似文献
878.
879.
在沙纹床面输沙过程中,假设水流从涡中取出并搬运的悬移质数量与推移质运动的沙星成比例,由12组细沙实验结果得到了沙纹床面净输沙的方向和输沙强度公式,并与他人的实验结果进行对比。 相似文献
880.
苏北中部滨海平原成陆机制研究 总被引:8,自引:0,他引:8
苏北中部滨海平原位于废黄河三角洲和长江三角洲之间,其形成与全新世最大海侵之后长江、古黄河的供沙历史和供沙状况密切相关,并且现今海域南黄海辐射沙洲的辐聚点也位于这段海岸,故探讨其成陆机制具有重要意义。本文数值模拟了公元8世纪时该区的M2潮汐、潮流,在此基础上,计算了7种粒径泥沙在当时潮流场中的净输运状况,划分了海底冲淤区。计算结果表明,公元8世纪时苏北岸外存在大致以东台为顶点的辐射状古潮流场,其分布格局与现今苏北岸外大致以京港为顶点的辐射关潮流场基本一致,该辐射状潮流场的存在是由当时台东岸外的独特驻潮波波腹所决定的。进入苏北岸外古辐射状潮流场中的泥沙,在辐聚、辐散的潮流作用下,每一个潮周期均自NE、SE方向向东台附近海域净输运泥沙,在东台附近海域发生淤积。由此认为,苏北中部滨海平原是大致以东台为顶点的辐聚、辐散潮 相似文献