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tidal creek in Chinese

Pronunciation:
How to pronounce "tidal creek""tidal creek" in a sentence

Translationmobile phoneMobile

  • 潮溝
  • 潮溪

Examples

  • So the tidal creeks must be managed in order to recover the salt marshes
    為了恢復鹽沼,必須對這些潮溝進行整治。
  • In some coast , the revolution of salt marshes are influenced by the moving of the tidal creeks , especially that parallel to the salt marsh edge would move landward , which will make the salt marshes eroded
    在某些岸段,鹽沼受潮溝運移的影響,尤其是平行于鹽沼外緣的潮溝向岸擺動,將侵蝕鹽沼草灘。
  • The prograding rate of the spartina alterniflora vertical to the coast is slower and the prograding rate parallel to the coast is quicker through it also will be slower when expanding across the tidal creeks
    它垂直于海岸的擴展速度較慢,平行于海岸的擴展速度較快,但在越過潮溝擴展時,速度也會變慢。
  • There are five genetic classifications of tidal creeks as follows : tidal creek scoured by the currents of ebb tide ; tidal creek eroded by stream from land ; tidal creek scoured by conflux of rainwater ; new tidal creek formed when the old moving ; tidal creek scoured by the flood
    在形成上共分為四種成因類型,即落潮水流沖刷型、陸源水流侵蝕型、雨水匯流型、潮溝遷移殘留型和潮流輻聚侵蝕型。
  • The sediment of tidal flat affect tidal creek greatly too , especially affect the development of curve current of tidal creek . on the upper tidal flat , the clay is abundance , and the sediment is much more viscous , so the curve current develops well
    灘面沉積物的組成對潮溝的發(fā)育也有較大的影響,尤其是潮溝曲流的發(fā)育,愈向潮灘的上部,粘土的含量愈多,沉積物的粘結作用也越強,潮溝越易發(fā)育曲流。
  • This thesis studies the tidal creek system on the prograding mud flat in jiangsu province based on 16 pieces of mss , tm and spot images from 1973 to 2001 , and analyses the growth , genetic classification , evolution and affecting factors of tidal creeks
    本文結合1973年至2001年共16張不同時相的衛(wèi)星影像對江蘇淤長型淤泥質潮灘上的潮溝系統(tǒng)進行了研究,對潮溝的發(fā)育、形成、演化和影響因素進行了初步探討。
  • Tide is the primary dynamic factor in building tidal flat ; it must be affect tidal creek system on mud flat . therefore , based on the raster image of the year of 2000 , the thesis has built correlation equations between average tidal ranges and the density of tidal creeks , the ratio of the width of outlet to the length of low tidal shore , the ratio of the area of tidal creek to tidal basin respectively . the result shows that the former is high well - marked correlation ; the two latter are well - marked correlation
    潮汐是塑造潮灘的主要動力因素,它必然與淤泥質潮灘上潮溝系統(tǒng)的發(fā)育有密切的關系,為此,本文以2000年的衛(wèi)片作底圖,對潮溝系的密度、溝口寬度占低潮線長度的比值以及潮溝面積與潮盆面積的比值,分別與平均潮差建立了相關關系,結果發(fā)現(xiàn),潮溝系的密度與平均潮差之間存在著高度顯著的相關性,溝口寬度占低潮線長度的比值和潮溝面積與潮盆面積的比值與平均潮差之間存在著顯著的相關性。
  • After analyzing , the author got the basic character of tidal flat hydrodynamic : the time of flooding on bare flat and ebbing is basically the same and the time of flooding on pioneer zone of salt marsh is a little short ; the process curve of current speed on bare flat did not appear peak value on the beginning of flooding and at the end of ebbing but presented double peak , that is , it presented double peak in winter and spring and ebbing peak value disappeared in summer and autumn , salt marsh presented single peak character in a year and the process curve in tidal creek presented double peak ; all current direction on every spot presented gyration current and the current speed changed rapidly during the high water level without obvious slack water period
    分析得到了潮灘水動力基本特征:光灘水位漲潮和落潮時間基本相等,而鹽沼前緣帶水位漲潮時間略短;光灘流速過程線在漲潮初和落潮末出現(xiàn)峰值,呈現(xiàn)“雙峰型”特征,鹽沼前緣帶則冬、春季節(jié)呈現(xiàn)“雙峰型” ,夏、秋季節(jié)落潮峰值消失,鹽沼帶四季呈現(xiàn)單峰特征,潮溝內過程線為“雙峰型” ;各測點流向均呈現(xiàn)回轉流特征,在高水位時流向迅速改變,不存在明顯的憩流。
  • There are four characteristics of the evolution of tidal creek as follows : ( 1 ) in the initial stages , tidal creek develops by continuous eroding trace to the source and depriving of the top of other tidal creeks . ( 2 ) the transverse moving of tidal creek occur mostly in the lower part , the middle part and the outlet take second place , and the upper part is more stability . ( 3 ) the different level branches of tidal creek transform into each other in the whole evolution course
    潮溝的演變具有以下特點: ( 1 )潮溝在形成初期,不斷進行溯源侵蝕和襲奪以擴大集水面積而發(fā)展壯大, ( 2 )潮溝的側向移動主要發(fā)生在潮溝的下段,中段和口門次之,上段最為穩(wěn)定( 3 )不同級別的支潮溝之間處在不斷地相互轉化過程之中。
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