「咸潮」的拼音、意思和解释

咸潮是一个开头的词语,它的拼音是xián cháo,这篇文章为您提供了咸潮拼音,读音,怎么拼读,同时为了让您在线轻松学习咸潮,我们收录了汉语辞典中咸潮的意义和释义,近义词,反义词,咸潮的五笔怎么打。

在线字典为您在线查询咸潮的词典内容如下,包括咸潮的拼音,读音,拼读;咸潮的意思和详细释义,咸潮的近反义词,咸潮的英语翻译,用咸潮这个词语怎么造句等内容。

咸潮读音/繁体/五笔/英文翻译

拼音 xián cháo 读音 跟我读
繁体 鹹潮 类型 词语大全
五笔 此词无五笔连打 平音 xianchao
词性 中性 语法
拼读 西(xi1)衣(yi1)啽(an2),咸(xian2)|吃(chi1)熬(ao2),潮(chao2)
英语翻译 salt tide

咸潮是什么意思?

· 基本释义

海潮。海水咸,故称。

· 详细释义

海潮。海水咸,故称。

清 谢元淮 《鹾言》诗之七:“砖池汲咸潮,盬盐出之晒。”

咸潮的近反义词?

咸潮近义词:抱歉,查无咸潮的近义词

咸潮反义词:抱歉,查无咸潮的反义词

咸潮词语接龙

(~咸潮~)在开头的接龙:潮剧,潮流,潮解,潮位,潮信,潮气,潮头,潮音,潮勇,潮烟,潮搐,潮骚,潮波,潮妈,潮动,潮鸡,潮满,潮爆,潮种,潮涛

(~咸潮~)在结尾的接龙:涨潮,弄潮,新潮,回潮,寒潮,春潮,浪潮,小潮,赤潮,红潮,怒潮,暗潮,人潮,低潮,热潮,防潮,返潮,风潮,大潮,落潮

暂时无法为您进行咸潮的词语顺序接龙!

用咸潮怎么造句?

您好,暂未查询到咸潮造句的内容。

由于上溯属于沿海地区一种特有的季候性自然现象,多发于枯水季节、干旱时期。

As a unique seasonal natural phenomenon along the coastal areas, Salty Tide usually occurs in the dry season or the period of drought.

当地水务局的官员称,上海市的自来水供应不会受到持续干旱和随之而来的咸潮入侵的影响。

Shanghai's tap water supply will not be undermined by the lingering drought and the consequent intrusion of saltwater, a local official from the water authority has said.

同时阐述了长江引水三期工程建成后,在入侵期间对上海市(中心城区)供水调度的改善。

Meanwhile, it also expounds that the completion of the Third Changjiang River Diversion Project will improve Shanghai (central urban area) water supply and Distribution Control during salt tide.

闸的基本功能是挡,综合功能包括防挡入侵,远期预留参与流域行洪调度、水质调度的功能。

Its main effects include preventing tide and salt water, satisfying the shipping and controlling flood and water quality.

据预测,珠江流域2006—2007年度枯水期来水依然偏枯,珠江三角洲地区将因继续面临严峻的供水局面。

According to forecast, water flow shall be low during dry period of 2006-2007 and water supply in the Pearl River Delta shall be threatened by salty tide again.

自来水泵站抽的都是盐分含量极高的水,因此,日常的饮用水都带有海腥的味,即进入学科上称“”的季节。

Water pumped by the water Stations contains high salinity. Therefore, the daily drinking water tastes salt and fishy. That is the season scientifically called Salty Tide.

陡山沱组盖帽碳酸盐岩形成于温暖条件下、微化海水沉积环境,属间—下台地前缘斜坡和浅海盆地之间的过渡带。

The precipitation of Doushantuo cap carbonates was deposited in warm, brackish water, and between the intertidal-subtidal inner ramp and shallow basin.

陡山沱组盖帽碳酸盐岩形成于温暖条件下、微化海水沉积环境,属间—下台地前缘斜坡和浅海盆地之间的过渡带。

The precipitation of Doushantuo cap carbonates was deposited in warm, brackish water, and between the intertidal-subtidal inner ramp and shallow basin.

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