- 更多网络例句与滩脊相关的网络例句 [注：此内容来源于网络，仅供参考]
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Sediment from river is not the main source of the Rushan Bay now any more ,which leads to the change of balance of sedimentation power. Sediment will transport because of the drive of hydrodynamic elements in macroscopic view .Direction of suspended load is basicly the same as tidal current .Flood tide makes suspended load transport to tip of the inner Bay and to the Mouth in exterior Bay .The direction of longside sediment transport in two sides of the Mouth mainly focus in the Mouth .Because the coastline along the exterior Bay is very meandering and it belongs to the type of bedrock ,besides some sediment going into the inner Bay ,so actual net sediment discharge rate is less than calculation .It develops an ebb delta out of the Mouth and forms tidal sand ridge ,tidal washing canal ,barrier bar and marine physiognomy ;The result of model simulation disclosures that differences of sediment erosion and siltation between single tidal action and wave-current action are very big .From the analysis of sediment composition、sediment sources and stability of beach and ridge ,this article gets the conclusion that the channel has the possibility to silt ,though the course maybe very slow.
通过分析研究文章得出如下结论：沉积物平面分布与水动力的时空变化存在很好的相关性；口门外发育落潮流三角洲，形成潮流沙脊、潮流冲刷槽、浅滩、拦门沙等水下动力地貌；乳山湾河流来沙已不是湾内泥沙主要来源导致沉积水动力平衡发生改变，宏观上表现在泥沙受水动力驱动发生不断运移；悬沙运移方向与涨潮流方向基本一致，湾内涨潮流带来的悬移质泥沙向湾顶运移，湾外悬移质泥沙主要向口门方向运移；湾口两侧岸段沿岸输沙方向均指向口门方向，由于乳山湾外海岸线曲折，两侧岸段以基岩为主，加之部分泥沙进入湾内，实际净输沙量小于计算值；数值模拟发现潮流单独作用与波流共同作用下泥沙蚀淤模拟差别较大；从沉积物组成、泥沙来源及滩槽稳定性三个方面分析，文章认为研究区存在航道淤积的可能性，但过程相对较慢。
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The basal geomorphology structure of the Tidal-Basin System of the Tiaozini Sandbanks is watershed and tidal creek system. We analyses its formation, evolvement, geomorphology characters and development and discusses the main influence factors which is water, sediment and space. We divide the evolution phases which is formation phase, autumn phase and contabescence phase. In the end we confirms its main functions, which is discharging the folium water on the tidal flat of the Tidal-Basin in the end of the ebb-tide, transporting sediment to Tidal-Basin through tidal creek systems, confining the swing range of the dynamical axis of flood tide or ebb tide, balancing the dynamical status of the South and North. At the same time, we compare coastal tidal-basin and sandbanks tidal-basin on geomorphology characters, formation causes, style and so on.
条子泥潮盆—潮沟系统的基本地貌结构为分水滩脊和潮沟系统，本文分别对它们的形成与发育、地貌特点及动态变化进行了分析，并探讨了影响其发育的主要因素，即来水条件、来沙条件、空间条件，划定了其主要发育阶段，即形成期、成熟期、衰亡期；在上述分析的基础上确定了潮盆—潮沟系统的主要功能，即通过潮沟系统渲泄落潮后期滞留在其潮盆范围内的滩面薄层水、通过潮沟系向潮盆内部输入或输出泥沙、限制涨落潮动力主轴摆动范围、平衡南北两侧动力状态；同时针对岸滩潮盆—潮沟系统与沙洲潮盆—潮沟系统的地貌特征、成因类型等进行了对比分析。
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So, there are still much more debate on the relationships among river sediment supply and water discharge, mud flat and radiative tidal sandy ridges, and on their responses to geological tectonic movements, sea level changes and human activities.
因此，对河流、潮滩、辐射沙脊群三者之间的相互关系，及其在构造运动、海面变化和人类活动等作用影响下所产生的变化等与海陆相互作用有关的问题，目前还存在相当多的争论。
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Cheniers are generally related to the deltaic environment.
滩脊一般与三角洲环境有关。
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Phragmites Australis, Ael uropus liitoralis, Zoysiamacrostachya, Messerschmidia sibirica, Limonium bicolor were the main vegetation types in the chenier seaside, but in the chenier plain, Artemisia annua, Artemisia mongolica and Herba Heteropappi Altaici occurred frenquently.
通过对无棣贝沙堤植物多样性的分析发现，样方内共出现物种20余种；同时，贝沙堤向海面和贝壳滩脊、向陆一面分别分布着以芦苇、獐茅、大穗结缕草、二色补血草、砂引草以及以青蒿、蒙古蒿、阿尔泰紫菀为优势种的群落。
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This region is manifested with marine terrace, sand dunes, beach ridges, estuaries, floodplains, beaches, mangroves, peneplains, uplands, sea cliff, etc.
该区显示为海成阶地、沙丘、滩脊、河口、洪积平原、海滩、红树林、准平原、高地、海蚀崖等等。
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The basal geomorphology structure of the Tidal-Basin System of the Tiaozini Sandbanks is watershed and tidal cr...
条子泥潮盆-潮沟系统的基本地貌结构为分水滩脊和潮沟系统，本文分别对它们的形成与发育、地貌特点及动态变化进行了分析，并探讨了影响其发育的主要因素，即来水条件、来沙条件、空间条件，划定了其主要发育阶段，即形成期、成熟期、衰亡期；在上述分析的基础上确定了潮盆-潮沟系统的主要功能，即通过潮沟系统渲泄落潮后期滞留在其潮盆范围内的滩面薄层水、通过潮沟系向潮盆内部输入或输出泥沙、限制涨落潮动力主。。。
- 更多网络解释与滩脊相关的网络解释 [注：此内容来源于网络，仅供参考]
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beach ridge：滩脊
beach reef 滩礁 | beach ridge 滩脊 | beach rock 海滩岩
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beach ridge：海滩脊,滩脊,沿岸堤,滨岸堤,海滩堤
滩脊 beach rampart | 海滩脊,滩脊,沿岸堤,滨岸堤,海滩堤 beach ridge | 滩崖,滩坎 beach scarp
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backshore beach ridge：滨后滩脊
backshaft 后轴 | backshore beach ridge 滨后滩脊 | backshore beach 滨后滩
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beach ridge; fulls：滩脊
滩潭 beach pool | 滩脊 beach ridge; fulls | 滩沙 beach sand
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fulls; beach ridge：滩脊
满岸期 fullbank stage | 漂白土 fuller's earth | 滩脊 fulls; beach ridge
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beach rampart：滩脊
beach price 海底原油在海上处理后之陆上价格 | beach rampart 滩脊 | beach reef 滩礁
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accretionary ridge：外展滩脊;加积砂岭
accretionary prism加积棱柱 | accretionary ridge外展滩脊;加积砂岭 | accretionary subduction complex加积俯冲复合体
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accretionary ridge：增积砂岭,外展滩脊,堆积脊
"增积岩体","accretionary prism" | "增积砂岭,外展滩脊,堆积脊","accretionary ridge" | "增积隐没复合体,加积俯冲复合体,加积俯冲带杂岩","accretionary subduction complex"
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accretionary ridge：外展滩脊
accretionary limestone | 加积石灰岩 | accretionary ridge | 外展滩脊 | accroach | 非法占有,强占
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fulls：滩脊;沿岸堤
fullrheologicalcurve 全流变曲线 | fulls 滩脊;沿岸堤 | fullsaturationdivingprocedure 全饱和潜水法