沖淤特性 的英文怎麼說

中文拼音 [chōngxìng]
沖淤特性 英文
erosional and depositional behavior
  • : Ⅰ動詞1 (淤積) become silted up 2 (血液不流通) (of blood) stagnateⅡ名詞(淤積的泥沙) silt Ⅲ...
  • : Ⅰ形容詞(特殊; 超出一般) particular; special; exceptional; unusual Ⅱ副詞1 (特別) especially; v...
  • : Ⅰ名詞1 (性格) nature; character; disposition 2 (性能; 性質) property; quality 3 (性別) sex ...
  • 特性 : characteristic(s); character; performance; features; properties; behaviour; response; character...
  1. It is mainly by analyzing the features of sediment concentration distribution in vertical in this paper, and then the problems of effect of headwork gates on sediment prevention, relation between distribution of sediment deposition in irrigated areas and its treatment and utilization, estimating the influence of withdrawing water and sediment on channel deposition and erosion in lower yellow river, and treatment and utilization of the sediment entered into canals are discussed

    本文主要從分析計算含沙量沿垂線分佈點,探討渠首防沙的作用,分析灌區泥沙積分佈與泥沙處理利用的關系,分析計算引水引沙對黃河下遊河道影響及入渠泥沙的處理利用等問題。
  2. 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,下遊河道發生刷,但艾山以下窄河段變化不大,近年來形成的積萎縮的狀況難以很快改觀,游蕩河段調整劇烈,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。
  3. Make a comprehensive view of all study results about the flood channel, a model of formation and evolution of the flood channels was proposed. according to this model, not all flood channels formed by ebb channels divided by sand spit develop toward death, some of them may be keeping the current situation or transform to the reserve channel with the change of runoff and sediment concentration from upper reach

    用gis方法計算1861 - 2002年新橋水道區域的變化,可定量表達漲潮槽在不同時間尺度形成演化規律,結合漲潮槽巖芯沉積物垂向的沉積變化,可闡明漲潮槽的形成機理與演化過程,並提出不同種類型漲潮槽的形成演化模式。
  4. Supported by the state natural science foundation project " formation mechanism and evolution processes of flood channels in the changjiang estuary ", this paper study systematically the formation and evolution, erosion and deposition, and features of dynamic sediment of flood channels in the changjiang estuary, and put forward a development model of the different flood channels

    本文依託國家自然科學基金課題《長江河口漲潮槽形成的機理與演化過程的定量研究》 ,以長江河口的漲潮槽為研究對象,採用沉積和地貌,定和定量相結合的方法,運用gis技術對河口漲潮槽的形成機理、演化模式、動力沉積徵以及變化等問題進行了系統的研究。
  5. Cour and silting characteristics of debris flows - because of resistance decrease due to supernormal pore water pressure, intermittent debris flows can be accelerated on mild slope in the superimposable processes of several debris flows

    ?泥石流的變化?泥石流多陣迭加過程中出現超載孔隙水壓力使龍頭阻力降低,在緩坡上能夠加速運動,說明泥石流龍頭迭加具有加速效應。
  6. Runoff characteristics of cao ' e river and its effect on processes of the estuary

    曹娥江徑流及其對河口的影響
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