流沙現象 的英文怎麼說

中文拼音 [liúshāxiànxiàng]
流沙現象 英文
quick sand phenomena
  • : Ⅰ動1 (液體移動; 流動) flow 2 (移動不定) drift; move; wander 3 (流傳; 傳播) spread 4 (向壞...
  • : 沙動詞[方言] (搖動以清除雜物) shake
  • : Ⅰ名詞1 (現在; 此刻) present; now; current; existing 2 (現款) cash; ready money Ⅱ副詞(臨時; ...
  • 流沙 : heaving sand; drift sand; blown sand; quicksand; running sand; shifting sand流沙固化 petrificatio...
  • 現象 : appearance (of things); phenomenon
  1. Baldly as he had stated it, in his eyes was a rich vision of that hot, starry night at salina cruz, the white strip of beach, the lights of the sugar steamers in the harbor, the voices of the drunken sailors in the distance, the jostling stevedores, the flaming passion in the mexican s face, the glint of the beast - eyes in the starlight, the sting of the steel in his neck, and the rush of blood, the crowd and the cries, the two bodies, his and the mexican s, locked together, rolling over and over and tearing up the sand, and from away off somewhere the mellow tinkling of a guitar

    話雖說得不好,他眼前卻浮出薩萊納克魯茲那個炎熱的星夜的豐富景。狹長的海灘的白影,港口運糖船的燈光,遠處喝醉了酒的水手們的哈喝,熙熙攘攘的碼頭苦力,墨西哥人那滿臉的怒氣,他的眼睛在星光下閃出野獸一般的兇光,鋼鐵在自己脖于上的刺痛和熱血的淌。人群,驚呼,他和墨西哥人軀體扭結,滾來滾去,踢起了塵。
  2. Our research analyzes desert phenomena and physiognomy characteristics with gas - solid hydromechanics principles. the typical phenomena include sand incipience, sand ripple and sand erode

    使用體力學的基本原理解釋漠中的粒起動、紋形成和蝕等常見和地貌特徵。
  3. In light of current using situation and drawing on the experience of many scholars researched methods and viewpoints, this thesis made com land, fallow land, orchard, grass land as experimental field in black soil region jlau, which carried out experiment by applying different amounts of n and p fertilization in corn field. by means of collecting the samples of rainfall runoff, erosion silt and surface layer soil before and after rainfall for one year nature precipitation in field, we study the effect of surface runoff on n and p nutrient and fertility degeneration. the results showed : ( l ) there are lots of factors which affect soil erosion and losses of n and p, in which rainfall and rainfall intensity were more important, while rainfall intensity is the most important meteorological phenomena factor

    針對當前黑土利用狀,本文借鑒眾多學者的研究方法和觀點,在吉林農大黑土區選擇利用方式不同的玉米地、休閑地、果園、草地,在玉米區進行了不同數量的施肥,通過野外試驗,採集一年自然降雨產及泥樣品,同時採集降雨前後的耕層土壤樣品,研究了黑土區地表徑對氮磷養分特徵及肥力退化的影響,結果表明:土壤侵蝕和氮磷的失受諸多因素的影響,降雨量、降雨強度是重要因子,而降雨強度是影響農田地表徑養分失的最重要的氣因子,特別是暴雨,暴雨徑中氮磷濃度較平時高得多;隨作物生長,覆蓋度逐漸增加以及不同利用方式下表的覆蓋度差異,氮磷失都表為顯著的差異。
  4. The quality of sand incipience involved with many kinds of parameters, such as incipient velocity, incipient angle etc. our research depends on the advantage of cross - knowledge and makes a research on this subject by gas - solid hydromechanics theory and ptv measure technology

    本論文發揮交叉學科的優勢,採用氣固兩相體力學理論和ptv測量技術研究這一,從新的角度認識粒起動和風結構,為風動的研究打開了新的思路。
  5. This paper intends to, from the perspectives of the aesthetics of reception, look into the phenomenon of the play, " shajiabang ", the transition from a model version to a romantic one, trying to expose the causes underlying the heated debate around it

    摘要自接受美學的視閾審視從「樣板戲」到「風版」的「家浜」,力圖對「家浜」中引發的尖銳爭論之原因做出深層解讀。
  6. Based on the relative data of density flow in xiaolangdi reservoir in flood period of 2001, and through analyzing on water - sediment condition of density flow formed and movement element of density current, the common movement law and special phenomenon on forming, operating and discharging sediment of density flow in xiaolangdi reservoir have been clarified in this paper. the relationship of sediment transport of density flow has been explored combining with theory analysis and formula deduction

    本文主要依據2001年洪水期小浪底水庫異重的有關資料,通過對形成異重的水條件、異重運動要素的分析,闡明了小浪底異重的形成、運行和排等方面的一般運動規律和特殊,結合理論分析和公式推導,探討了異重關系。
  7. The structures and dynamic changes of the artifical sand - fixing vegetation were studied based on the follow views : components of vegetation community, plant diversity, life - forms of vegetation, trends of plant growth, characteristics of the vertical and horizontal structure of vegetation, relationship between the vegetation community and environment ( including soil moisture temperature etc. ), relationship between the vegetation community and characteristics of plant physiological activities. some results were showed as follow : 1. components, diversity and life style of artificial vegetation in shapotou region the marked changes of artificial vegetation have taken place during more than 40 years, since the establishment of sand - fixing vegetation

    本文以騰格里漠東南緣寧夏中衛縣坡頭地區人工固植被作為研究對,採用傳統生態學的野外調查方法,從植被群落的組成、多樣性、生活型、群落生長動態、垂直結構特徵、水平結構特徵、群落結構與周圍環境(土壤含水量、溫度)相互關系及其與植物自身生理生態適應特徵關系等多個角度研究了人工植被群落的結構及其動態變化,取得了如下研究結果: 1 、植被群落組成、多樣性及生活型:坡頭地區人工植被經過近50年的演變,從丘到固定地,地植被的動態變化經歷了從人工植被到人工?自然植被的轉變,從人工植被建立初期的少數幾種引種植物到有30多種植物,隨著固定地時間的延長,植物種類日趨豐富,並且人工植被在15 25年、 40 50年兩個階段,物種的周轉速率最大,即群落結構變化最大。
  8. The main result is as follows : 1. after erosion, the content of organic matter, total nitrogen and the available nitrogen in the sediment is more than that of soil sample. namely the enrichment phenomenon of organic matter, total nitrogen and the available nitrogen in slope cultivated land erosion soil is obvious

    黃?土受侵蝕后,泥樣中有機質、全氮和堿解氮的含量都高於雨前採集的坡地表層土樣,即黃?土坡耕地水土失中有機質、全氮和堿解氮失的「富集」明顯,而全磷和速效磷卻無明顯的「富集」
  9. Due to the influence of climate drought and human activities, the ecological environment of qinghai province is in an increasingly grave condition, namely, climate abnormal events occurring frequently, grassland degenerating, ground sanding, glacier shrinking, water level of lakes descending and river runoff decreasing, and so on. in the basis of extensively collecting and analyzing the data of qinghai ecological environmental factors such as climate, water resource and grassland resource etc., the further basic research is performed on the ecological environment characters of main climate factors, surface runoff, water resource, lcc and their correlation to coordinate with the basic, strategic and precursory research for the development of china west part and provide the scientific foundation for corresponding development both ecological environment and social economy, and persistent utilization of natural environment resource

    本研究針對當前在氣候乾旱化和人類活動的共同影響下青海省生態環境中氣候異常事件即氣災害頻繁發生、草場退化、土地化、冰川萎縮、湖泊水位下降和河量減少等生態環境退化日益嚴重的實際,在廣泛收集和整理青海省氣候、水資源、草地資源等生態環境因子基礎資料的基礎上,對青海的主要氣候要素、地表徑、水資源、植被的演替及其相互間的關系等主要生態環境變化特徵進行了基礎性的研究。
  10. Due to irrational land utilization, absurd assarting and herding, a series of environmental problems, such as sandy soil, grassland degeneration, soil and water loss, appeared, which severely threatened to survival and development of human being. it was proved that biomic - measure was the radical measure of ecology environment construction and harnessing. thus, a research on choosing a kind of grass, which was good, stronger stress resistance and faster growth velocity, was carried out

    黃土高原半乾旱區多年來由於不合理的土地利用和濫墾濫牧等,致使土壤化,草地退化,水土失等一系列生態環境問題嚴重威脅著人類的生存與發展,多年的研究已證明,生物措施是生態環境建設與治理的根本性措施,因此,針對目前的自然狀,選擇抗逆性強、生長快、生產中急需的優良牧草進行了定位試驗研究。
  11. For dilute solid - liquid two - phase flow, the mechanism of particle motion driven by fluid is the main subject, especially the particle motion in the near wall region. the bursting phenomenon and coherent structure of turbulence play an important role on the motion of particles in the near wall region

    明槽紊近壁區的顆粒運動與紊動猝發及紊相干結構有著密切的關系,開展近壁區顆粒與紊相互作用的機理研究對于體力學和泥運動力學都有著重要的理論意義和實際價值。
  12. Our research observes the wind - sand flow phenomena in outside field. then establish a wind - blown - sand flow experimental set and reformulate the phenomena in lab

    本文建立了風實驗裝置,對自然界中的風進行野外觀測和實驗室模擬。
  13. After the implementation of water regulation, the river course in delta reaches the minimum ecological flux, and no flow interruption take place ; the runoff flowing into the sea and the transporting sediment increase ; the areas of fresh water wetland is also increased gradually ; species variety get instauration obviously

    結果表明,黃河水量統一調度后,河口三角洲最小河道生態基在非汛期基本得到滿足,斷不再發生,徑入海率和輸入海量有所增加,淡水濕地面積逐漸增多,物種多樣性明顯得到改善。
  14. It is concluded that the phenomena of replacement of spatial and temporal process is typical in the erosion development, the coarsen of riverbeds, the sediment concentration and the change of river regime, etc

    分析表明,河再造床過程在沖刷延展、河床粗化、含量及其特徵、岸灘侵蝕以及河型變化等方面具有較典型的時空演替
  15. During the sand - dust storm, the high pv spreads evidently downward from the upper troposphere

    塵暴期間,對層高層大值位渦下傳十分明顯。
分享友人