河道坡度 的英文怎麼說

中文拼音 [dào]
河道坡度 英文
stream gradient
  • : 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...
  • : Ⅰ名詞(道路) road; way; route; path 2 (水流通過的途徑) channel; course 3 (方向; 方法; 道理) ...
  • : 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
  • 河道 : river course; streamway; covalency; runway; cut; river channel河道變遷 channel change; migration ...
  • 坡度 : falling gradient; slope; inclination; declivity; pitch; batter
  1. From sedimentology symbol such as rock assembled, sediment gradus, sandstone grading analysis, protogene sedimentary structure, ichnofossile and logging facies etc and palaeoenvironment background, it is confirmed that shen84 - an12block s34 segment is braid river delta system, not fan delta system ( abrupt slope ). then it can be more partition as braid river delta plain sedimentary assembled, delta front sedimentary assembled and prodelta sedimentary assembled on core and log assembled. and delta plain sedimentary assembled can be identified four microfacies : braided distributary channel, crevasse splay, overbank deposits and interdistributary bay

    沉積微相研究是儲層非均質性研究的基礎,研究區有豐富的巖芯資料和測井資料,通過巖石組合、沉積韻律,砂巖粒分析、沉積構造、古生物遺跡和測井相等沉積學標志,結合古環境背景,確定沈84 ?安12塊s _ 3 ~ 4段為辮狀三角洲體系,而不是前人所認為的扇三角洲(陡型)體系,在巖芯和測井組合上可進一步劃分為辮狀三角洲平原沉積組合、三角洲前緣沉積組合和前三角洲沉積組合,其中三角洲平原沉積組合又可識別出辮狀分流、決口扇、分流邊部和分流間灣四種微相類型;三角洲前緣沉積組合識別出水下分流、水下分流邊部和分流口壩三種微相。
  2. When catchment area, average channel gradient and catchment shape factor of designed culvert or bridge are known, a user can be convenient to get local parameters c, e and b from standard contour charts and easy to calculate flood flow just by a calculator. design period of flood flow is enormously shortened as well as a high precision. estimated flood flow through culvert or small bridge by new calculation model is generally less than by traditional methods, so that much cost is cut down a s reducing the span of culvert or small bridge

    以75000km ~ 2的川中丘陵地區為試點研究區,繪制了該地區新模型的參數等值線圖,率定了不同設計頻率的改正系數,使設計者只需在地形圖上獲取集水面積,平均降和流域形狀系數,在參數等值線圖上查得橋涵所在地的相應參數,使用計算器即可迅速計算出設計流量,大大縮短了設計周期,且精較高,設計的洪水流量一般低於傳統方法,從而可減小橋涵跨徑,節省投資。
  3. A new method is presented. the travel time, including the time delays associated with overland folw pathways, is obtained. it is expected that the hillslope velocity and the stream velocity are different, and different equation is used. in the method, the fact that velocity increases going downstream in river systems is taken into account. after the travel time of each cell being calculated, the frequency distribution of the times of arrival of individual water droplets at the catchment outlet - giuh, is obtained

    提出了一種匯流時間計算方法,匯流時間中包括地漫流時間和匯流時間。方法中地單元的匯流速單元的匯流速採用不同的計算公式,同時考慮流速沿向下游的變化。流域中每一個網格單元的匯流時間得到后,將其看作隨機變量,進行統計分析后,得到匯流時間的頻率分佈? giuh 。
  4. Product function : soft soil subgrade strengthening, reinforced embankment & slope, strengthening separation, bounding deformation of foundation, prevent road from reflection crack, increasing the intensity of subgrade. it can strengthen soft subgrade of kinds of roads and railways ; prevent road from reflection crack ; enhance the strength of subgrade ; reinforcedriverbank, embankment and slope ; homogenize the stress ; adjust settlement ; improve the stability and bearing capacity of the basement ; strengthen road and bridge tops

    產品功能:軟土路基加強,路堤邊加筋,加強隔離,約束地基變形,防止路反射裂體,提高路基的強.各種路、鐵路等軟路基加強,增強路基的強岸、路堤、邊起加筋,均化應力,調整沉降,提高基底穩定和承載力;路橋臺面的加強。
  5. The arch dams locate at such areas which have high mounain, deep valley, steep slope, narrow riverway and high seismic intensity. the aseismic capabilities of high arch dams have relationship with lives and properties of people and productions of industry and agriculture, so the eanhquake becomes the main factor of arch darns design

    這些大壩所在地區山高谷深,岸陡峻,狹窄,地處高地震烈區,高壩的抗震性能關繫到下游廣大地區工農業生產和人民生命財產的安全,考慮地震因素成為大壩設計中的控制工況。
  6. There is sharp gradient in top and small gradient in bottom. the ability of removing flood is high in top and it is small in bottom correspondingly. sediment silt up continually, so the bed of river is jacked up year by year and become the famous river on land

    由於泥沙含量高,現行已行水140餘年,山東段床上寬下窄,上陡下緩,排洪能力上大下小,在泥沙淤積作用下,床逐年抬高,成為世界上著名的地上「懸」 。
  7. Thirdly, there are many river bends and shoals in the inner mongolia reach. ice flood will occur in these places at the break - up time. it is valuable and meaningful to make factor analysis for ice flood and model research for freeze - up time and break - up time

    第三,內蒙段成幾字型大彎曲,其間淺灘彎疊出,變緩,逶迤曲折,中多夾心灘,分流竄溝,解凍開時,常在的曲灣或山寬變窄的狹窄段產生凌汛。
  8. The geomorphological instantaneous unit hydrograph ( giuh ) is viewed as the frequency distribution of the times of arrival of individual water deoplets at the catchment outlet. the travel path, for a typical hillslope cell. consists of a hillslope fraction, corresponding to overland flow and a stream fraction, corresponding to concentrated channeled flow. to obtain the time of travel, velocities must be defined. hillslope and stream velocities vary with location and must be strongly correlated with slope, and therefore a spatial distribution of velocities and hence of travel times could be obtained. the present methods of giuh neglect any time delays associated with overland flow pathways

    地貌單位線被看作是流域上各水質點在弱相互作用下,到達流域出口匯流時間的頻率分佈。對於一個典型的山型網格單元,匯流路徑由兩部分組成,即地部分和部分,為了得到匯流時間,必須首先確定匯流速地和的匯流速隨著區域位置而變,並且必然與有關,因此,可首先計算流速的空間分佈,進而得到匯流時間的空間分佈。
  9. Therefore, nowadays major problem is how to reduce the slope cultivated land ' s soil erosion and sediment concentration transporting to three gorges reservoir in order to prolong the three gorges engineering ' s use time and protect the safety of the middle and lower reaches channel of yangtze river

    因此當前的主要問題是如何臧輕耕地土壤侵蝕,減少進入三峽庫區的泥沙量,延長三峽工程的運轉時間,保障長江中下遊的安全。另外,按土壤平均厚78 。
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