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tide water相关的网络例句

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与 tide water 相关的网络例句 [注:此内容来源于网络,仅供参考]

Taking the Cangdongpian inning area on the west side of Tiaozini Sand as a case study,the paper analyzed the compages and validity of ebb tide water to maintain the flood discharge creek below the tide lock for different projects of seawall line.

文章以条子泥西侧岸滩仓东片匡围为例,探讨了不同堤线方案下邻近闸下流槽各种落潮水量组成及其维护闸下排水能力的有效性。

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。

in pearl river delta region,water environmental contamination featured big amount and mixed types and centralization of pollutant discharge with latent combined pollutants,striding boundary pollution,severe municipal pollution,the trend of regional pollution being extended from cities to rural area,infall of salty tide in recent years.as a result,the unwatered complexion was hastened due to bad water quality.the factors of water environmental contamination were analyzed as the natural factors including especial hydrographic net distributed pattern,water body runoff characteristic,water resource distributive regional difference,infall of ocean tide,and so forth; the artificial factors as inconsequence of economic development mode and distribution of industry and cities planning,lagging environmental infrastructure,indifferency of environmental consciousness,dissonance of economic development and environmental protection.

珠江三角洲地区水环境污染特点表现为:污染物排放量大、类型杂且集中,潜在复合污染出现,跨界污染突出,城市污染依然严重,并呈现出从城市向农村蔓延的区域性污染趋势,加上近几年咸潮入侵加剧,使区域水质型缺水的局面更趋紧张。造成这种污染局面的因素:一方面受控于区域内特殊的河网分布格局,水体径流特征、水资源分配的地区性差异以及海潮入侵等自然因素;另一方面也反映了区域经济发展模式,工业布局和城市规划不尽合理,环境基础设施滞后,环境意识淡薄,经济发展与环境保护不协调等人为因素所致。

The" high water","middle water",and "Low water" in some mangrove literature should be " high water spring tide"," high water middle tide", and "high water neap tide" in tidology terminolo-gy.

潮汐和浸淹形成的环境梯度控制了红树林在潮滩上的总体分布和群落结构,是红树林能量特征最重要的组成部分「,成为红树林生态学研究的重要内容。

The results showed that the quasi-period of floes diameter in the surface water during the spring tide included 7.86 h, 3.93h and 2.95h; those in the same water during the neap tide included 8.38h and 3.14h; those in the bottom water during the spring tide included 3.33h and 1.19h.

分析表明,长江口徐六泾处细颗粒泥沙絮凝体粒径存在着明显的变化周期:大潮表层存在7.86h, 3.93h和2.95h的变化周期;小潮表层存在8.38h和3.14h的变化周期;大潮底层存在3.33h和1.19h的变化周期。

Results show that floes' VC and D at the surface water were closely related to current velocity; and the peaks of VC lag those of the current velocity. The lag variation during ebb and flood tides is 10-30min and 30-50 min, respectively. Current velocity at 50 cm/s is a turning point of D vs. vertical average current velocity, before the point, Dm increases with current velocity, and decreases after the point. Similarly, VC at 75μl/L becomes a critical point in the surface water, below the point, D increases with VC, and above the point, D stabilizes.Δp is D dependent, larger floes have much lower Δp than smaller floes. Both D and Δp of floes affect ω. In the surface water during spring tide and neap tide, a power exponent relationship exists between Δp and D, and ω and D.

研究表明:①长江口徐六泾表层絮凝体体积浓度主要受水流流速影响,再悬浮现象明显,体积浓度过程线滞后流速过程线,落潮期间滞后10-30min,涨潮则滞后30-50min;②小于一定流速时絮凝体平均粒径随流速增大而增大,大于一定流速时絮凝体平均粒径则随流速增大而减小,徐六泾夫、小潮表层絮凝体在50cm/s的垂线平均流速时出现平均粒径与垂线平均流速关系的转折;③徐六注大、小潮表层絮凝体平均粒径在体积浓度75μl/L时出现平均粒径与体积浓度关系的转折,体积浓度小于75μl/L时粒径随体积浓度增加而增大,超过75μl/L时粒径随体积浓度的增加变化不明显;④絮凝体有效密度由粒径大小控制,粒径大,有效密度小,反之亦然,粒径和有效密度共同决定絮凝体静水沉速,有效密度和沉速与平均粒径之间均存在良好的幂指数关系。

Soft tide of sand of Na Daihe bathing place is smooth, beach wide gentle, tide is douce, highest tide 1.66 meters, neap 0.66 meters, tide differs 1 meter or so, water Wen Kuo is spent, safe and comfortable; Marine sanded fine softness, without reef shiver, without mud sodden grass; Seawater is clear and transparent, free from contamination.

南戴河海滨浴场沙软潮平,滩宽和缓,潮汐稳静,最高潮位1.66米,最低潮位0.66米,潮差1米左右,水温适度,安全舒适;海底沙细柔软,无礁石碎块,无污泥烂草;海水清亮透明,无污染。

By coordinate transformation,specifically,by using orthogonal coordinate system to obtain vertical high resolution ratio in superstratum water of Beibu Gulf and making use of Sigma coordinate system to match terrain in bottom water,the authors intend to set up Beibu Gulf Physical Oceanic Model and use the model to simulate partial tide M\-2,partial tide K\-1 and partial tide O\-1 respectively.

采用坐标变换方法,在北部湾上层海洋采用正交坐标系以获得垂向高分辨率,在底层水体采用 Sigma坐标系以拟合地形,建立北部湾的物理海洋模型,并利用建立的模型分别模拟北部湾的 M2 、K1 、O1 分潮。

In tide of coastal waters bare and respect of laky eutrophication prevention and cure, obtain bare of the East China Sea material of whole process of tide happening, succession, confirm crucial physics process forms primary value in bare tide, consider to make clear, the Yangtse River pours fresh water or composition of salt of nutrition of area of tall hair of tide of bare of the East China Sea reachs content to be planted to bare tide choose He Chichao to form have conclusive effect.

在近海赤潮和湖泊富营养化防治方面,获得东海赤潮发生、演替全过程资料,证实关键物理过程在赤潮形成初期的重要性,探究表明,长江冲淡水或东海赤潮高发区营养盐组成及含量对赤潮种遴选和赤潮形成具有决定性功能。

They are inversing tide water swimming.

他们逆着潮水游泳。

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