1) Denzhou shoal
登州浅滩
1.
Based on field observed data and historical data and charts, the geographic information system technique and interpolation method were used to calculate and analyze the recent changes in the Denzhou shoal, the causes for its geomorphological evolution were analyzed, and its evolutional regularity in the future was predicted.
在野外实际测量和历史资料与图件收集的基础上,以地理信息系统技术为支持对大量数据进行了计算分析;应用数学插值等方法,计算分析了登州浅滩近期变化情况,分析研究了地貌形态演变原因,并对其以后的演变规律做出了预测。
2) Wenzhou shoal
温州浅滩
1.
By means of mathematical models of wave, tidal flow and sediment, numerical study is carried out on deposit-promoting schemes in the reclamation project of Wenzhou shoal at Oujiang estuary.
建立了波浪潮流泥沙数学模型,对瓯江口温州浅滩围涂促淤工程效果进行了数值模拟研究。
2.
On the basis of model verification and calibration by field data,wave field,tidal flow field,salinity field,suspended sediment field and seabed erosion and deposition field of Oujiang Estuary,where large-scale reclamation project of Wenzhou Shoal will occur,are numerically simulated.
建立了波浪、潮流、盐度、悬沙、底床冲淤等多种因素数学模型,在模型验证的基础上,对瓯江口温州浅滩围涂工程海区的波浪场、潮流场、盐度场、悬沙场、底床冲淤场进行了数值模拟研究,对温州浅滩围涂工程对瓯江泄洪、瓯江南北口分流比、乐清湾养殖业、瓯江口港口航道及状元岙深水区、南口口外滩地的影响进行了分析论证。
3) Laizhou shoal
莱州浅滩
1.
The result shows that the sediment resource of the Laizhou gulf is made up of the Yellow River mouth sandspit and the Laizhou shoal, which origin from the Yellow river sediment and the river sediment of the north-west Shandong peninsula.
结果表明 ,莱州湾泥沙资源主要包括黄河口沙嘴和莱州浅滩两部分 ,分别来源于黄河和山东半岛西北部河流输沙。
2.
Based on field work and historical geomorphic analysis, and supported by GIS and RS, this paper has researched the geomorphic dynamic characteristics and evolution rules and the artificial effects on erosion and deposition of the Laizhou shoal since 1958, when many reservoirs were built, and a great amount of sand began to be reduced.
在野外观测和历史地貌调查的基础上,利用地理信息系统和遥感技术,研究了现代莱州浅滩的地貌演变规律和人类活动对浅滩地貌冲淤动态的影响。
3.
It’s study the dynamic geomorphology, dynamic deposition and the relation withheavy metals in surface sediments of the Laizhou shoal for the first time.
本文首次对莱州浅滩动力地貌、动力沉积及其与沉积物中重金属含量分布之间的关系进行了研究。
4) secche
浅滩浅滩
5) shoals
[英][ʃəul] [美][ʃol]
浅滩
1.
The middle and lower reaches of the Yangtze River is typical bending braided river which have many shoals and the riverbed evolution of these reaches is serious.
我国长江中下游是典型的河槽分汊型河流,浅滩众多,河床演变剧烈,主槽与支汊交替转化,碍航问题突出,成为制约航运发展的“瓶颈”。
6) shoal
[英][ʃəʊl] [美][ʃol]
浅滩
1.
Evolution characteristics of the shoals of the second and third generation alluvial islands in the Changjiang Estuary;
长江口第二、三代冲积岛浅滩演变特征分析
2.
The exposed and unexposed shoals and their bearings on the carbonate reservoirs in the Feixianguan Formation in the northeastern part of the Sichuan Basin;
四川盆地东北部飞仙关组暴露浅滩、非暴露浅滩与储层关系
3.
Combining with the moving characteristic of water and sediment,mechanism of shoal s navigation-obstru.
文章基于对该河段建库以后原型观测资料,分析了兴隆至新泗港这一宽浅弯道段河道的冲淤变化情况,并结合本河段的水流泥沙运动特性,阐述了该河段浅滩碍航机理。
补充资料：登州泉
济南众多的泉水中，喷涌的形态各不相同，但看起来最与众不同的应是登州泉了。
游走于趵突泉公园和万竹园之间，翠竹瑟瑟，忽见平地凸起一池，且泉池造型独特，长方形的泉池中池中有池，外池内壁刻有“登州泉”三个苍翠的大字，泉水从内池溢出后，沿内池四边跌落于外池之中，状如满溢的一盘琼浆，水面如镜，光洁如缎，落水如珠，丽影扬辉。
“登州泉”一名的来源，是因为传说此泉的水脉来自东海边的登州。古人曾有诗曰：“文登一脉透谭城，澄彻全无蜃气腥。安得雪堂苏学土，朗吟万竹濯清冷。”其实，登州泉与趵突泉应为同—水脉，均来源于济南市的南部山区。
登州泉为金代《名泉碑》和明晏璧《七十二泉诗》所著录的济南七十二名泉之一。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条