水底坡度 的英文怎麼說

中文拼音 [shuǐde]
水底坡度 英文
underwater gradient
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • : 底助詞(用在定語后, 表示定語和中心詞之間是領屬關系, 現在多寫作「的」)
  • : Ⅰ名詞(地面傾斜的地方) slope Ⅱ形容詞(傾斜) sloping; slanting
  • : 度動詞[書面語] (推測; 估計) surmise; estimate
  • 坡度 : falling gradient; slope; inclination; declivity; pitch; batter
  1. Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area

    詳細的沉積相研究發現,紅獅地區第三系發育有沖積扇、下沖積扇、河流、三角洲、扇三角洲、湖泊和湖扇7種主要沉積相類型,並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖,以較高的時間解析揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律,比如在北部的凹陷陡背景下,上升半旋迴低位期通常發育有下扇、湖扇等陡岸近源特徵的沉積體系,下降半旋迴高位期,扇三角洲相粗碎屑巖由北向南進積;在南部的凹陷緩背景下,上升半旋迴主要發育辮狀河流相,下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相沉積和鹽類沉積。
  2. The model of vertical eco - landscape was designed according to the slope and contour line : in the top land over 25, trees were planted to form a water - conserving forest ; in the slope land between 15 and 25, peach trees were planted ; between 5 and 15, loquats trees were planted ; less than 5, special species of fruit trees, melons and vegetables were planted ; the bottom field was characterized with water area of " rice and fish ", " lotus and fish "

    其垂直生態景觀模式按和等高線布置:在大於25的山頂形成保林木區,上15 25的陡種植桃樹,中5 15的斜種植枇杷,下小於5的緩地帶種植特種果、瓜類及蔬菜,形成「稻魚」和「藕魚」特色域區。
  3. In this paper, the marine route survey factors, such as water depth, bottom slope, soil shearing strength, tidal current and thunderstorm and their roles in the submarine fibre - optic cable engineering are introduced, and their roles and necessities in the cable construction are also appraised, which will make the combination of marine route survey with construction demand closer and the marine route survey be aimed at the cable engineering practice

    摘要介紹了深、海、土壤剪切張以及潮流、雷暴等海洋路由各勘測要素及其在海光纜通信施工中的作用,並對它們在施工中的作用及其必要性進行了評價,從而使海洋路由勘測與施工的需要結合得更緊密,更具有針對性。
  4. Through discussion of numerical solution, the author get the effect of height of filled soil, size of culvert, width of valley, property of filled soil, construction procedure and techniques on soil stress of the culvert top ; 3. through the centrifuge test, the paper validates the reliability of numerical calculating on high - stack soil ; 4. the paper puts forward the simplified calculating method of soil stress of the culvert top on the foundation of numerical simulating and centrifuge modeling

    通過對數值解的討論,得到填土高,涵洞截面尺寸,溝谷部寬,溝壁角,填築體性狀,施工速,地下對豎向位移場及涵洞頂部土壓力的影響情況; 3通過離心機的模擬試驗,驗證了數值計算對高路堤的計算結果的可靠性; 4在數值模擬和室內離心機模型試驗的基礎上,提出了高填方涵洞頂部土壓力簡化計算方法。
  5. This kind of instability bulk movement is induced by wave cyclic loading, as a result the slope of bottom bed decrease, water depth increase, and instability bulk movement has the character of subregion, regularity and head erosion, thus it will influence evolvement of region of interest landform, and change flow field and bottom stratum condition continually, so will lead to dynamic influence on structure foundation soil

    這種不穩定塊體運動由波浪循環荷載誘發,其結果使床整體減緩,深加大,而且不穩定的塊體運動具有小區域、多發性和溯源侵蝕的特點,將繼續影響著海域以後的深地形的發展演化,並不斷改變著該區的流場與床地層條件,對構築物地基土的穩定性產生著動態的影響。
  6. Through analyzing bed ' s response to wave, in the condition that super - stratum is more hard and second - stratum is more soft in region of interest, super static interstitial hydraulic pressure amplitude die away rapidly between stratums, before in sight of boundary between hard and soft stratum, plane effective pressure increase to max. shear stress reach peak value when bed thickness is approximately 2. 7 meters, then it will decrease to the minimum on the place where the flexible soil has a common boundary with the rigidity, so the boundary is the most destroy plane on engineering. on the basis of reconnaissance in situ, in normal situation of sea, the structure slides to the basin along the boundary

    通過對床在波浪下的響應分析,對于研究區床上層較硬而第二層較軟的情況,超靜孔隙壓力幅值在層間交界處迅速衰減,在臨近硬、軟地層交界處前,平有效應力增至最大,剪切應力在床厚大約2 . 7米左右達到峰值,然後減小,到硬、軟層土交界位置,達到最小,因此這個界面就是最容易發生破壞的工程軟弱面,現場勘查證明,即使在正常海況下,構築物也會沿以此交界面為滑動面,緩慢向「盆」滑動。
  7. It decreased with the increase of the gradient. the soil moisture in sunlit slope is greater than that in sunless slope, and changes as the following order in the slope : top < middle < lower

    面,隨著的增加,土壤含量逐漸降低;陰的土壤含量高於陽;而在同一向,土壤含量從頂遞減。
  8. This discovery lends credence to the controversial idea of forcefully injecting water or steam into faults at the base of an unstable flank to trigger the stress - relieving earthquakes needed to let it down slowly

    這項發現無疑為一個爭議性的構想打了一劑強心針:在不穩固邊部的斷層,強行注入或蒸氣,目的是引發地震、釋放應力,以緩慢降低邊
  9. Through analysis, we conclude that washing action of wave and flow is main power of evolvement of region of interest landform, structure lead to the fact that water area around shallow structure in cheng dao sea field has an increase about 0. 3m / a through actual measurement, water depth increase rate around foundation is 0. 25m / a, slope gradient of side slope averagely has a decrease of 5 % o a year, however marine hydropower wash rate through compute is 0. 2m / a on underwater bottom, the wash rate on structure foundation is 0. 35m / a

    分析認為,浪流的沖刷作用是研究區深地形演化的主要動力,構築物的存在,使埕島海域淺區人工構築物周邊域實測年深增加幅約0 . 3m a ,地基附近深增加速率0 . 25m a ,邊平均每年以5減緩,而計算得出的海洋動力沖蝕速率在為0 . 2m a ,在構築物地基沖蝕速率達0 . 35m a 。
  10. The model for non - linear long wave and the mild slope equation are respectively applied to simulation wave propagation on a classical topography for small size waters - submerged shoal with concentric contours. the differences between them in wave propagation are got through comparing the numerical solutions. and the results are accordant with actual cases

    並將非線性長波傳播模型和緩方程,分別應用於非線性作用較摘要強、地形為平與圓形暗礁的組合這一經典物模實驗,比較了二者應用於小尺域范圍內波浪傳播變形的具體差別。
  11. The bottom slope source terms is treated with surface gradient method so as to obtain the high - order accuracy result in the scheme

    採用這種演算法並對淺方程的源項按面梯法進行處理,可以獲得較高精的模擬結果。
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