Wind action should be primarily influenced on the open shore segment and aerial-marine shore segment, and it's sensitive for the response of the processes of the shadow shore segment to the tide action.

弧形海岸過(guò)程的動(dòng)力機(jī)理通過(guò)對(duì)南灣海灘近岸的動(dòng)力作用分析表明：1）波浪動(dòng)力是影響華南弧形海岸過(guò)程的決定性因子婷婷网色色图，近岸海區(qū)的波浪場(chǎng)與海灘場(chǎng)具有明顯的相關(guān)區(qū)69网在线观看免费，關(guān)鍵區(qū)主要位于海灘的中間岸段及其海區(qū)的近岸帶和海灣上国产老色批在线观看视频、下岬角連線的鄰近區(qū)域。2）風(fēng)應(yīng)力及其潮汐是影響整個(gè)華南弧形海岸時(shí)空變化過(guò)程的重要?jiǎng)恿σ蜃硬豢ü谙撸渲泄鷄v表兄妹，風(fēng)應(yīng)力主要偏重于對(duì)海灘開(kāi)敞岸段及其水上岸段的影響，遮蔽岸段的海灘過(guò)程對(duì)潮汐動(dòng)力作用的響應(yīng)較為敏感www欧美操逼视频。3）臺(tái)風(fēng)大浪及其冬季冷空氣南下導(dǎo)致的動(dòng)力作用加強(qiáng)是海灘過(guò)程急遽變化的重要因子这久久精品。

The outside sea wave streams into near the shore and shallow water area, being subjected to a submarine friction function, the wave 鋒 becomes abrupt, the trough of wave become slowly, the fluid matter orders sport track to present back and forth fluxion, and to shore enter the current velocity degree is usually bigger than offshore reflux speed, causing bottom sediment clean to shore porterage, and is aroused a shore wave of ascend the blunt water current take to the seashore on-line pile up.

外海波浪傳入近岸淺水區(qū)，受到海底的摩擦作用一级a爱做片2，波鋒變陡激情无码一区、波谷變緩，水質(zhì)點(diǎn)運(yùn)動(dòng)軌跡呈現(xiàn)往復(fù)流動(dòng)最近免费中文字幕视频在线MV，而且向岸進(jìn)流速度通常大于離岸回流速度，導(dǎo)致底部泥沙凈向岸搬運(yùn)久久国国产免费999，并被激岸浪的上沖水流帶至海濱線上堆積久久精品一二三美女。

After that the fractures in the right dam foundation slope were stretched at the beginning of the Quaternary Period because in the period Yakouhoushan mountain quaquaversal dome was blowups quickly. At the same time, the valley trenching of Lancang River reach to 800-1000 meter in altitude at the right bank in Nuozadu dam site. This two reason accelerated the groundwater infiltration in the right bank slope. So, the weathering agency could have invaded deeply in the right bank slope.

導(dǎo)致右岸巖體復(fù)雜化的成因是，右岸巖體在早期遭受了多期構(gòu)造作用和巖體蝕變的基礎(chǔ)上可以永久免费观看的一级视频，第四紀(jì)早期丫口后山穹隆的快速隆起與當(dāng)時(shí)河谷下切至800m～1000m高程這一特殊因素組合引起了右岸巖體沿原有的斷裂張開(kāi)91在线视频第一页，使地下水等風(fēng)化營(yíng)力能夠到達(dá)坡體較深部位，經(jīng)過(guò)長(zhǎng)期的風(fēng)化卸荷作用嫩草久久久久久久精品99，形成了右岸復(fù)雜巖體有人有片在线观看视频。

The thickness of the ice cover on the wall surface heat transfer is greater than the thickness of it on the air heat transfer form. The thickness of the ice cover on the wall surface heat transfer along the way changes slowly, but it on the air heat transfer along the way changes significantly. Reducing the entrance velocity, lowering the wall surface or air temperature, the formation of the thickness of the ice cover will increase; in the 3D circumstances, The thickness of the ice cover was relatively uniform in the import of the U-turn model, the ice cover was gradual accumulation in the convex bank when the stream traversed the import of the U-turn model, the thickness of the ice cover in the convex bank was significantly bigger than the thickness in the concave bank. The temperature field under the ice cover tends to be complex because of the existence of the secondary flows. The temperature in the convex bank is greater than it in the concave bank. Compared with the data from experiments, the laws in the numerical simulation are similar with them in the experiments

模擬結(jié)果顯示：二維情況下，運(yùn)用壁面?zhèn)鳠嵝纬傻谋w厚度大于運(yùn)用空氣傳熱形成的冰蓋厚度黄色视频直接进，壁面?zhèn)鳠嵝纬傻谋w厚度沿程變化緩慢~级黄色视频高清视频，而空氣傳熱形成的冰蓋厚度沿程變化明顯，減小入口流速亚洲人成A片在线观看尤物，降低壁面或空氣溫度等性一级录像视频网站免费大全，形成冰蓋的厚度都會(huì)增大；三維情況下免费无码黄视瓶，彎道入口處凸av黄色在线观看免费、凹岸形成的冰蓋厚度基本相同，進(jìn)入彎道后亚洲R在线，凸岸形成的冰蓋厚度逐漸增大1024色婬免费视频，而凹岸的冰蓋厚度逐漸減小，受橫向環(huán)流的影響，冰蓋下水流的溫度場(chǎng)趨向復(fù)雜A级黄色网站免费看，并且凸岸的溫度小于凹岸的溫度国产操av；與實(shí)驗(yàn)室實(shí)驗(yàn)所得數(shù)據(jù)相比較，數(shù)值模擬研究得到的規(guī)律基本符合實(shí)驗(yàn)規(guī)律理论日韩中文。

Hased on the field data and the typical investigation of hydrodynamical effect on collapse in reser voir banks, tihs paper analyses the mechanism of reservoir banks collapse and deeply studies some speical relationships between wave Height.

本文以影響庫(kù)岸坍塌變形的水動(dòng)力學(xué)因素作為主要研究對(duì)象超碰在线欧美精品，選取三峽工程重慶河段庫(kù)岸為原型，通過(guò)模型試驗(yàn)研究欧美又大又粗一区二区，分析了庫(kù)岸坍塌變形與波高偷拍视频无码、岸坡坡度、岸坡土質(zhì)等要素的關(guān)系亚洲色欲综合网在线观看A，對(duì)更深入欧美一级视频网站免费在线观看、全面的進(jìn)行庫(kù)岸坍塌機(jī)理的研究提供了可靠的依據(jù)

Chapter 2 discusses the necessity of the establishment and development of Shanghai offshore financial market and focuses on its influence to Chinese economy and the construction of Shanghai international finical center.

本文共分四章，結(jié)構(gòu)安排如下：第一章成年无码av网站天堂网，離岸金融市場(chǎng)概述介紹了離岸金融市場(chǎng)的含義久久精彩视频7、特點(diǎn)及發(fā)展情況，主要闡述離岸金融市場(chǎng)的發(fā)展及其發(fā)展的國(guó)際經(jīng)驗(yàn)黄片aaav免费。

The Fourth part analyzed the necessity and conditional foundation of offshore financial market, combined abroad experience of development of offshore financial market, such as choosing mode which suit oneself etc. This part also analyzed the present condition of Chinese offshore financial market and problem which appeared during the development of Chinese offshore financial market.

第四部分在分析了中國(guó)建立離岸金融市場(chǎng)的必要性和條件的基礎(chǔ)上亚洲欧洲黄色搞j国产网站VV级，結(jié)合國(guó)外發(fā)展離岸金融市場(chǎng)的經(jīng)驗(yàn)如選擇適合自身的模式等，分析了中國(guó)離岸金融市場(chǎng)的現(xiàn)狀色欲天天婬色婬香综，剖析了中國(guó)離岸金融市場(chǎng)在發(fā)展過(guò)程中出現(xiàn)的問(wèn)題欧美一级专区。

When three gorge sluiced,bank slide between 135m and 175m must be instable,namely reservoir bank collapse.so the department concerning order to carry out special reaserch about bank collapse geological investigate, bank collapse prognosticate.bank collapse prevention and bank prevention information manage system and decision system.

三峽蓄水后，必然引起沿江兩岸135m～175m范圍庫(kù)岸邊坡的不穩(wěn)定黄色成人网站在线观看，即水庫(kù)塌岸或邊岸再造国产A级高清视频毛片。鑒于此，國(guó)家相關(guān)部門(mén)下達(dá)對(duì)三峽庫(kù)區(qū)兩岸進(jìn)行塌岸地質(zhì)調(diào)查国产精品区最新视频、塌岸預(yù)測(cè)国产盗摄一区、塌岸防治的工程技術(shù)以及塌岸防治信息管理系統(tǒng)與決策支持系統(tǒng)等專題研究。

The paper analyze the influence factor in water level, ground-water, river current, ground structure, bank aspects, wave action and vegetation condition with qualitative method.

分析得出：區(qū)域(1)-a庫(kù)岸再造的主要影響因素是河道縱向水流的沖刷作用网址在线观看国产日韩视频；區(qū)域(1)庫(kù)岸再造的影響因素是高水位時(shí)波浪的沖刷日韩乱伦字幕中文一区，水位降落時(shí)覆土層的剝離，以及水位變化造成基巖的風(fēng)化www.rihanav、崩塌黄色一级片大相焦；區(qū)域(2)、區(qū)域(3)庫(kù)岸再造的主要影響因素是暴雨和水位降落時(shí)岸坡的失穩(wěn)滑塌中文字幕制服丝袜第57页，次要影響因素是高水位時(shí)波浪的沖刷爱爱视频a，水位降落時(shí)覆土層的剝離，水位變化造成基巖的風(fēng)化精品日本一区二区三区免费；區(qū)域：(4)庫(kù)岸再造的影響因素是高水位時(shí)波浪的沖刷毛片A片在线观看免费在线观看，水位降落時(shí)覆土層的剝離。

When the soil behind and/or beneath such a wall liquefies, the pressure it exerts on the wall can increase greatly - enough to cause the wall to slide and/or tilt toward the water.

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ANGELO：岸皆路

龍之夢(mèng)日本岸皆路(ANGELO)專柜[龍之夢(mèng)日本岸皆路(ANGELO)打折]龍之夢(mèng)日本岸皆路(ANGELO)專柜--部分5折[龍之夢(mèng)日本岸皆路(ANGELO)專柜]

lee shore：下風(fēng)岸,背風(fēng)岸

lake shore 湖岸,湖濱 | lee shore 下風(fēng)岸,背風(fēng)岸 | pole shore 立柱頂撐

on a lee shore：船在下風(fēng)岸(即迎風(fēng)岸

on a lay 船長(zhǎng)包船拆帳制 | on a lee shore 船在下風(fēng)岸(即迎風(fēng)岸 | on a wind 迎風(fēng)航駛

marginal quay：順岸式碼頭;順岸碼頭

marginal beam 邊緣梁 | marginal quay 順岸式碼頭;順岸碼頭 | marginal terrain 僅及安全的地帶;不易發(fā)展的地帶;僅及安全的地勢(shì);不易發(fā)展的地勢(shì)

marginal quay：順岸式碼頭;順岸碼頭kLi中國(guó)學(xué)習(xí)動(dòng)力網(wǎng)

marginal beam 邊緣梁kLi中國(guó)學(xué)習(xí)動(dòng)力網(wǎng) | marginal quay 順岸式碼頭;順岸碼頭kLi中國(guó)學(xué)習(xí)動(dòng)力網(wǎng) | mariculture zone 海產(chǎn)養(yǎng)殖區(qū)kLi中國(guó)學(xué)習(xí)動(dòng)力網(wǎng)

rip current channel：離岸流水道

rip channel 離岸流水道 | rip current channel 離岸流水道 | rip tide 離岸流

stony shore：粗石子石岸

stony shore 粗礫石岸 | stony shore 粗石子石岸 | stony shore 粗石子石岸石岸

rip tide：離岸流

rip saw 粗齒鋸 | rip tide 離岸流 | rip tide 離岸流每次浪沖上海灘后形成的)離岸流

rip tide：離岸流每次浪沖上海灘后形成的)離岸流

rip tide 離岸流 | rip tide 離岸流每次浪沖上海灘后形成的)離岸流 | rip 暗礁引起的水花;挖掉木甲板縫的舊捻絮

shore cover：岸到岸全程保險(xiǎn)

shore control system 岸控系統(tǒng) | shore cover 岸到岸全程保險(xiǎn) | shore current 沿岸流