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isobath相关的网络例句

查询词典 isobath

与 isobath 相关的网络例句 [注:此内容来源于网络,仅供参考]

In summer, distribution of Pro paralleled the 50m isobath, presenting in most areas of the East China Sea.

在垂直分布上,超微型浮游植物的分hi与水柱的分层、营养状况都有关系。

Shelf break at depths between 20 to 550 meters, with an average of 130 meters, also has the 200-meter isobath as the lower limit of the continental shelf.

陆架坡折处的水深在20~550米间,平均为130米,也有把200米等深线作为陆架下限的。

By comparing different series of topography data, scouring and sedimentation are calculated in a more accurate way. By analyzing the shift of the isobath and shore line, the evolution of typical cross section, a preliminary study of the response to the changes of upstream runoff and sediment are carried out, due to the effect of the construction of the Three Gorges Project.

分别对北支、南支和南汇边滩的横向、纵向变化情况进行了分析,对各自的冲淤进行了定量的计算,获得地形冲淤变化的强度和空间分布,并探讨了长江口地区的冲淤演变对三峡工程引起的长江供沙量变化的响应情况。

The west of Qiandao port, that is near the Qiandao Village, the depth of water condition is good, the isobath of -5 meters is 3200 meters to the bank.

前岛港西部即前岛村附近水深条件较好,-5米等深线距岸3200米,开挖后可建设万吨级泊位。

Advantage of the natural conditions:① Hankou port -6 m isobath offshore 1 km,-10 m isobath offshore 5 kilometers, the planned routes for various types of ships enter out, without tidal restrictions.

自然条件优势:①韩口港区-6米等深线离岸1公里,-10米等深线离岸5公里,规划的航道可供各类船只随进随出,不受潮水限制。

Animal taxonomists described as a "living fossil" of the amphioxus, in the shallow water near the 15 m isobath density of 1035 / m, think about with these "living fossils" with swimming in a region, which can not but make you feel shock.

被动物分类学家誉为"活化石"的文昌鱼,在浅海15米等深线附近密度达到1035尾/平方米,想想能够与这些"活化石"同在一个区域游泳,这不能不使你感到震撼。

It is shown from the analysis results that the average retrogradation rate of the south coastline of the Laizhou Bay during 1958 to 2004 was 27 m/a,the average retreating rate of the 0 m isobath was in the range of 27 to 65 m/a,and the average cutting rate of beach face was 2.1 cm/a.

结果表明,1958-1984年,莱州湾南岸岸线平均侵蚀后退速率为27 m/a,0 m等深线后退速率为27~65 m/a,岸滩平均蚀低速率为2.1 cm/a.1984-2004年,莱州湾南岸岸线位置基本无变化,岸滩平均蚀低速率为1.04 cm/a,水深5 m以浅的区域表层沉积物变粗。

The different grains of the deposited materials are basically parallel to the isobaths, sand lower than–3m isobath and silty clay deeper than–3m isobath.

2数值模型要定量预测海湾填海工程可能引起的海底冲淤影响,建立数学模型是最有效的方法。

Changes of erosion and accumulation of the seabed before and after the project The general characteristics of the pattern of erosion and accumulation of the seabed near the scheduled project both before and after the scheduled project are as the following: accumulation occurs at the areas lower than–10 isobath; some suspended sediment is deposited near the coast due to the relatively small tidal current with a monthly accumulation rate of 2-6 mm; while a slight erosion occurs in the areas deeper than–10 isobath with a monthly accumulation rate of .2 mm.

5工程前后海底冲淤变化工程前后海底冲淤相同的地方是:大致沿-10m等深线向近岸呈淤积状态,近岸由于潮流流速小,一些悬沙落淤,月淤积量在近岸附近约2-6mm;而-10m等深线以深基本上呈轻微冲刷状态,月冲刷量一般在0.2mm以下。

The deep water deposition means the deposition in the area where the water depth is larger than 30 meters, in which the major sediments are coarse sand and gravel. This kind of deposition is the relic deposition formed by the Pleistocene alluvial-lacustine deposition reworked under modern channel currents actions, and ususally the Holocene acummulation lack in the deep waters. The transitional zone deposition is the deposition between the low tidal level line and the 30 meters isobath, where the sediment types is changeable and the grain sizes are gradually coarsening from the low tidal line to the deep water area. This kind of deposition is developed by the deep water eroded sediments sorting under the transitional zone current action. The different types distributed along the isobath. The tidal flat deposition is the fine sediment deposition on the tidal flat which is flo sedimentation of the silty clay under the tidal flat dynamic action and ususally developed fluid mud on the lower tidal flat. The channel mouth deposition is the deposition in the channel mouth area. According to the sediment types, it includes sand deposition where there are coarse sediments supply and silt deposition where there are only fine sediments surpport.

峡道深水区沉积是指水深大于30米的峡道底部沉积,它以粗颗粒砂砾石沉积为特色,是现代峡道水动力对第四纪海退时发育的冲洪积和坡积物进行改造形成的蚀余沉积,全新世沉积地层往往缺失;峡道过渡带沉积是指水深介于低潮位线至30米水深线之间发育的峡道边坡沉积,该带沉积以沉积物类型多样为特色,自低潮位线至30米水深线,沉积物粒级逐渐变粗,由粉砂质粘土逐渐递变为中粗砂,是峡道深水区沉积物经多次分选沉积而发育的,基本平行于等深线分布的条带状沉积,在岸坡较陡岸段,过渡带下部可发育重力沉积;峡道潮滩沉积是指在低潮线与海岸线之间发育的细颗粒沉积,它是粘性细颗粒泥沙在潮滩动力作用下,发生动水絮凝沉积而形成的粉砂质粘土沉积,在低潮滩可发育浮泥;峡道口门区沉积则是在峡道汇入大海或海湾时,在峡道出口水流影响所及范围的沉积,根据峡道口门区供给泥沙的特性,峡道口门区沉积有粉砂质淤泥沉积和砂质沉积两种类型。

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