河底下面的 的英文怎麼說
中文拼音 [hédexiàmiànde]
河底下面的
英文
subbottom- 河 : 1 (天然的和人工的大水道) river 2 (指銀河系) the milky way system; the galaxy 3 (特指黃河) t...
- 底 : 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」)
- 下 : 下動詞1. (用在動詞后,表示由高處到低處) 2. (用在動詞后, 表示有空間, 能容納) 3. (用在動詞后, 表示動作的完成或結果)
- 面 : Ⅰ名詞1 (頭的前部; 臉) face 2 (物體的表面) surface; top 3 (外露的一層或正面) outside; the ri...
- 的 : 4次方是 The fourth power of 2 is direction
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In the research area, the incised valley was formed during the sea level downwards and was provided source by the arenaceous river from qiaotou. it is stacked by 3 incised valleys formed in 3 different sequences
研究區內子洲鎮川堡地區發育的下切河谷形成於海平面下降時期,來源於橋頭的砂質河流沉積,為疊置的、形成於三個不同三級層序底部的下切河谷充填沉積。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、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇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,以較高的時間解析度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坡背景下,上升半旋迴低水位期通常發育有水下扇、湖底扇等陡岸近源特徵的沉積體系,下降半旋迴高水位期,扇三角洲相粗碎屑巖由北向南進積;在南部的凹陷緩坡背景下,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。What ' s more, we put forward some experienced formulas on the basis of the cortical analysis. the result of the research show that by installing diffluent piers with low ridge, we can eliminate the root of oscillatiny water jump, perfect the energy dissipation effect of water jump, also, we can improve the flow condition of down - stream. the fact that the main flow of down - stream is in the middle, not only effectively lower the speed of the bottom flow in the ridge rear, alleviate the erosion to the river bed, but also avoid the heavy wave resulted from the main flow in the surface, thus improve the surface wave of down - stream obviously. we can work out the body style parameters of diffluent piers with low ridge according to the project flow condition and experience formulas, and then reckon the down - stream surface wave condition for the protected building of the down - stream bank
研究結果表明:設置低坎分流墩后,消除了擺動水躍水舌擺動的根源,提高了水躍的消能效果,改善了下游水流流態。下游水體的主流在中部,既有效的降低了坎后水流底流速,減輕水流對河床的沖刷,又避免了主流位於表面導致波浪過大的結果,下游的水面波浪明顯得到削減。依據經驗公式,可根據工程水流條件設計出低坎分流墩的體型參數,進而估算出下游沿程的水面波浪,為下游岸邊的砌護提供依據。Based on the previous studies, the research in this paper was carried out, mainly including two parts as follows : ( 1 ) anammox bacteria and aerobic ammonia oxidizers were detected in situ in 6 sediment samples taken from jiangsu province. molecular techniques, such as fish, pcr, dna cloning and sequencing etc. were used for this purpose. ( 2 ) the continuous cultivation of anammox bacteria from sediment samples were studied, which provides experimental basis for the bioaugamentation of eutrophicated sediment applying anammox process
本論文在前人研究的基礎上,開展了以下兩個方面的工作: ( 1 )採用分子生物學技術熒光原位雜交( fish ) 、多聚酶鏈式反應( pcr ) 、 dna克隆和測序等對采自江蘇省蘇州市、東太湖、新沂河等6個底質樣品進行了厭氧氨氧化菌和傳統氨氧化菌的原位檢測; ( 2 )探討了以底質作為接種體進行厭氧氨氧化菌富集培養的可行性,為天然底質環境中厭氧氨氧化過程的強化,富營養化底質微生物修復的可行性提供一定的依據。( 2 ) according to the forming model of the deep pull cracks, they can be divided into three classes pulled cracks -, pressed cracks and sheared cracks. ( 3 ) based on the two - dimensional and three - dimensional finite element methods. the following results can be affirmed : in the slope excavating process, the base surface will rebound in the direction of the excavating surface ' s excerior normal. the maximal displacements of the left and right bank are + 3. 6cm and + 2. 4cm ; the arch abutment will rebound in the direction of the river valley, the maximal displacements of the two bank are + 3. 5cm and + 2. 2cm ; the upstream and downstream surface will rebound in the direction of the normal direction. the maximal displacements are + 2. 1cm and + 1. 7cm. ( 4 ) the natural slope is stable
( 3 )通過二維及三維有限元分析得知,左右岸拱肩槽邊坡在開挖過程中,開挖底面主要表現為朝開挖面外法線方向發生回彈,左右岸最大位移量分別為+ 3 . 6cm 、 + 2 . 4cm ;拱端面主要表現為向河谷方向發生側向回彈,左右岸最大位移量分別為+ 3 . 5cm 、 + 2 . 2cm ;上下游坡面主要表現為向臨空方向的回彈,左右岸最大位移量分別為+ 2 . 1cm 、 + 1 . 7cm ;開挖使巖體產生由卸荷回彈導致的傾倒拉裂現象。Furthermore the small stool under my buns was very boring, the small stools under our buns were all made of pure irons just for the sounds being full of power and grandeur when we put down our stools
另外還有就是屁股底下的小凳子,為了在放凳子的時候聲音能夠整齊劃一、氣吞山河,所以我們屁股下面的小凳子都是用純鐵做的。One could almost hear the roots sucking the earth, the stalks growing, the underground streams trickling.
人幾乎能聽到植物的根在吸收大地養料,莖干在長高,地面底下的小河在汩汩地流著。Based on the analysis of satellite images of various periods, landform data and river channel transverse section evolution in the lower yellow river, the characteristics of the river channel boundary condition changes at different location are clarified as middle flood channel flood transport width and area are evidently decreased especially for the main channel with comparison to 1950s, beach area that is unimpeded before become blocked because of road, irrigation channel constructed on it, and consequently intensify high edge of beach and lowering dyke and river
在現場查勘的基礎上,通過對丹江口水庫和小浪底水庫攔沙初期下遊河道演變、排洪能力變化特點的對比,分析了黃河下游防洪面臨的新形勢:小浪底水庫攔沙初期,下遊河道發生沖刷,但艾山以下窄河段沖淤變化不大,近年來形成的淤積萎縮的狀況難以很快改觀,游蕩性河段調整劇烈,工程出險機遇增大,河道水位流量關系中水流量以下部分同流量水位明顯降低,中水流量以上部分水位降低幅度可能會明顯偏小,防洪形勢仍不容樂觀。About the kolotcha, in borodino, and both sides of it, especially to the left where the voina runs through swampy ground into the kolotcha, a mist still hung over the scene, melting, parting, shimmering with light in the bright sunshine, and giving fairy - like beauty to the shapes seen through it
在科洛恰河上面,在波羅底諾村及其兩邊,特別是左邊,也就是沃伊納河在沼澤地帶入科洛恰河的地方,彌漫著晨霧,霧在融化,消散,在剛升起的明亮的太陽的照耀下變得透明起來,霧中一切可以看見的景物神奇地變得五光十色,只勾勒出那些東西的清晰的輪廓。Experimental process shows that variance of underwater distributary channel and declining rate of lake plane are closely related to moving intension of motive soleplate
實驗過程顯示,水下分流河道的變遷與湖平面的下降速率及活動底板的運動強度密切相關。According to the documentation collected from domestic and abroad wang wei dong who works in huadong architect and structure institute utilizes the similar work property between the underground continuous wall and pile subjected the vertical loads, and introduces poulos method of elasticity and plastic which applies to pile foundation into the calculation for subsidence of underground continuous wall. pujialiu and yu yuzhou from water and electronic engineering of qinghua university, according to the result of three axes, define the concrete parameter utilize the model of non - linear e - b combined with the design cross section of dam in xiaolangdi, yellow river accept the total stress programme of thepd dam, and we analyze the stress and displacement of plastic concrete diaphragm wall by finite element method in comparison with the result of common concrete one. at same time, we consider the effect of the character of plastic concrete diaphragm wall which is composed of different gradients and adopting the level of stress and pulling stress infers whether the plastic concrete diaphragm wall is safe or not
地下連續墻是一種歷史較短的施工方法,目前,砼防滲墻的設計還是以傳統的設計方法為主,根據查找國內外文獻資料,華東建築設計院王衛東利用地下連續墻與樁在豎向荷載作用下的工作性能有相似性,將適用於樁基的poulos彈性理論引入對地下連續墻的沉降計算中;清華大學水利水電工程系濮家騮、于玉貞根據三軸試驗結果確定混凝土的參數,利用非線性e - b模型,結合黃河小浪底土石壩設計剖面,採用thepd土石壩總應力程序,對深覆蓋層塑性混凝土防滲墻的應力、位移進行有限元分析,並與普通混凝土防滲墻計算結果加以對比,同時分析了不同配比塑性混凝土特性的影響,並採用應力水平和拉應力數值來判斷塑性混凝土防滲墻的安全程度。These are the words which moses spoke to all israel across the jordan in the wilderness, in the arabah opposite suph, between paran and tophel, laban, hazeroth, and dizahab
1以下是摩西在約但河東的曠野,疏弗對面的亞拉巴,在巴蘭和陀弗、拉班、哈洗錄、底撒哈之間,向以色列眾人所說的話。These are the words which moses spoke to all israel across the jordan in the wilderness, in the arabah opposite suph, between paran and tophel and laban and hazeroth and dizahab
申1 : 1以下所記的、是摩西在約但河東的曠野、疏弗對面的亞拉巴、就是巴蘭、陀弗、拉班、哈洗錄、底撒哈中間、向以色列眾人所說的話。These be the words which moses spake unto all israel on this side jordan in the wilderness, in the plain over against the red sea, between paran, and tophel, and laban, and hazeroth, and dizahab
1以下所記的,是摩西在約旦河東的曠野,疏弗對面的亞拉巴,就是巴蘭,陀弗,拉班,哈洗錄,底撒哈中間,向以色列眾人所說的話。These are the words which moses said to all israel on the far side of jordan, in the waste land in the arabah opposite suph, between paran on the one side, and tophel, laban, hazeroth, and dizahab on the other
以下所記的、是摩西在約但河東的曠野、疏弗對面的亞拉巴、就是巴蘭、陀弗、拉班、哈洗錄、底撒哈中間、向以色列眾人所說的話。I have me my summer vacation in a town last year. since whose are there. some of my relations, there have a good view for the mountain and river, i think it ' s a great place be to rest, one day when i ride my bike on the small path, this river catch my eye for very clearly but like very deeply, becauese i can ' t see the end of the water, then. some chap shouting make me look at, they catch a a short boy and thow he in the water with a heavily, waiting for a moment yet the boy not up the water, i ' m very worry and jumping in the river, i want float out but some watergrass be enteine my leg and the body is deeper at every movey, i don ' t know past how long time, i feeling one small hand help me break up the watergrass and push me to the surface of the rive, after that i just kown they are hvae a playing who can sit in the swim and make a long time in deep water, but i want cry for the joking, becauese i couldn ' t swim but i have a forget
去年我在一個小鎮上度暑假,因為那裡有我的親戚,我認為那裡有好山好水是一個靜休的好地方.一天當我在小路上騎著自行車時,一條非常清澈但好像也挺深的小河吸引了我的視線,因為我好像看不到河的底端,這時,一些小孩的叫喊聲因起了我的注意,他們抓住一個矮小的小男孩然後重重的扔進了水裡,待了一小會這個男孩沒有露出水面,我非常擔心就跳進了水裡,我想浮出來,但一些水草纏住我了的腿,我每動一動身體就會越往下沉,我不知道過了多常時間,我感覺有一雙小手幫我弄掉腿上的水草並往水面推著我的身體,后來我才知道他們是在玩看誰在水底呆的時間長的游戲比賽,但我對于著樣的笑話想哭因為我忘記自己了不會游泳When choosing evaluative indexes, we take four aspects of fatalness of sea level rise hazards, vulnerability of land system, socio - economic and ecological vulnerability, and defending ability. we draw the map based on the relief map and the land utilizing map of 1 : 100000 scale, gain altitude values ( range of 1 km 1 km ) and the fundamental data of evaluation in the studied area using the software of mapinfo and socio - economic statistic data
運用mapinfo軟體和社會經濟統計數據,以盤錦市1 : 100000地形圖和土地利用圖作為底圖,獲得地面1km 1km范圍高程值以及評估單元基礎數據,並計算出在沒有防護、不同潮位背景、海平面上升不同高度的條件下,遼河三角洲未來海平面上升將淹沒的土地面積、受災人口和經濟損失,以及不同土地利用類型的淹沒面積及相應的經濟價值。分享友人