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1)  silt-sandy beach
粉沙质海岸
1.
Sand movement of silt-sandy beach and the outer navigation siltation;
粉沙质海岸的泥沙运动和外航道淤积
2.
Method of calculating return period of suddenly siltation on a silt-sandy beach
粉沙质海岸航道骤淤重现期的确定方法
3.
Definition of silt-sandy beach and its characteristics of sediment movement
粉沙质海岸的界定及其泥沙运动特点
2)  silt sandy beach
粉沙质海岸
1.
Sediment movement along silt sandy beach and calculation of siltation;
粉沙质海岸泥沙运动和淤积分析计算
2.
A Statistical probability model for calculating deposition amount is proposed on the basis of depositing features of the open channel on a silt sandy beach.
针对粉沙质海岸开敞航道的回淤特点提出了一个计算航道回淤的统计概化模型。
3)  silty coast
粉沙质海岸
1.
In recent years, with the increase of the port constructions on the silty coast, the problems of the sediment transport, especially the channel siltation become more and more prominent.
近年来,随着粉沙质海岸港口建设的发展,粉沙质海岸泥沙问题,特别是航道淤积问题越来越突出。
2.
Combined with research work for several years on silt of Huanghua harbor,the research experience and learning including the seacoast division,the sudden siltation condition in the outer channel on silty coast,the movement form of silt,the characteristics of silty coast research and the regulation of sudden siltation in outer channel on silty coast were also introduced.
结合几年来参与黄骅港泥沙研究工作,介绍了研究过程中的经验和体会,包括关于海岸的性质划分、粉沙质海岸航道骤淤的条件和泥沙运动形式、粉沙质海岸泥沙研究的特点和粉沙质海岸航道泥沙骤淤的治理。
4)  silty mud coast
粉沙淤泥质海岸
1.
But the computation method of the siltation thickness in approach channels derived from the mud coast can be used in the silty mud coast by considering the different hydrodynamic characters of brea.
回顾了淤泥质海岸航道淤积厚度的计算方法,其中,特别对破波与非破波产生的含沙量作出的比较表明,它们之间的差别非常之大,但只要考虑了破波和正常波的不同水动力特性、粉沙淤泥质泥沙与淤泥质泥沙之间的不同运动特性,则淤泥质海岸航道的淤积计算方法,就可以用于粉沙淤泥质海岸。
5)  sandy coast
沙质海岸
1.
There are different forms of the beds on the natural sandy coast, on which the propagation process of the wave is a typical nonlinear one.
 天然沙质海岸上存在着不同形状的床面,波浪在其上面的传播过程是一典型的非线性演化过程· 以此为工程背景,利用摄动方法对小幅度非均匀倾斜床面上波浪的非线性传播过程进行了探讨,给出了解析的表达式,并与相关的实验资料进行了比较分析,结果表明,所建立的波浪演化模型能够反映实际情况·
2.
The construction of breakwaters or groins on sandy coasts could change the local flow field,leading to adjustment of beach erosion and accretion.
在沙质海岸上修建导流堤、丁坝等会引起局部海域水沙动力条件的改变和海床冲淤调整,因此准确预测沿岸输沙率是海岸工程建设前进行优化设计的基础条件之一。
6)  sandy beach
沙质海岸
1.
It shows that the cape-bay coast and barrier-lagoon coast are the major types of Quanzhou sandy beach.
研究表明泉州市沙质海岸以岬控岸和沙坝——泻湖为主,岬控岸的沉积物和剖面表现为中细粒沉积和岸坡由近岸向海变平缓,而沙坝——泻湖岸则以粗粒沉积和岸坡起伏不平为特征,沉积物特征、沿岸输沙、平衡剖面及动力地貌均反映了泉州砂质海岸的侵蚀状况。
补充资料:粉沙
土壤中介于沙与黏土之间的细颗粒,捏在手中像面粉,细腻而不粘手。含粉沙的土壤保水能力好,适于种植马铃薯、花生等。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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