高明區 的英文怎麼說

中文拼音 [gāomíng]
高明區 英文
gaoming district
  • : Ⅰ形容詞1 (從下向上距離大; 離地面遠) tall; high 2 (在一般標準或平均程度之上; 等級在上的) above...
  • : Ⅰ形容詞1 (明亮) bright; brilliant; light 2 (明白;清楚) clear; distinct 3 (公開;顯露在外;不隱...
  • : 區名詞(姓氏) a surname
  • 高明 : brilliant; bright; wise; better qualified
  1. The research indicates that the modern sediment is divided three layers : polluted layer, transition zone and unpolluted layer. just the pollute layer cause dianchi lake environmental pollution. the high value district of ammoniac nitrogen distributes near northern part haigeng mainly, middle part increase slightly, have most lower near southern part, the content of ammoniac nitrogen of the polluted layer sediment lower than the lower layer ; the high value district of effective phosphorus distributes near haikou - jinning, from the north to the south, the content of effective phosphorus increases progressively, the content of effective phosphorus of the polluted layer sediment obviously higher than the lower layer

    研究結果表:滇池現代沉積物主要分為三層,污染層、過渡層和未污染的湖泊沉積層,其中污染層是對滇池環境污染造成影響的層位;氨氮的主要分佈在北部海埂附近,中部略有增,南部則最低,表層沉積物的氨氮含量低於下層;而有效磷的則分佈在海口?晉寧附近,由北向南,有效磷的含量依次遞增,表層有效磷的含量要於底層。
  2. Furthermore, the dq value ranges of profile multifarctal spectra in different landform types and in different directions of the same sections perform different properties and anisotrpies. it can be concluded that the landscape fractal properties depends closely on the int ensity, manner and inhomogenity of exogenic and inogenic processess, and with the properties, we can study quantatively the dynamic geomorphic process. by using the same methods just above, local fractal dimensions d, crossover length tc and the multifractal spectra dq - q of two large - scale landform profiles ( across and along tianshan mountain ranges respectively ) are calculated. the results show that in the studied scaling range the two profiles perform different scaling properties, and both of them can be divided to three evident different linear scaling subsections

    不同類型地貌二維地貌表面也表現出多度域分形特徵,而且隨著觀測尺度的增加,每個間的分維值均表現為依次減小,表外營力作用的影響逐漸被內營力作用所取代:不同類型地貌在相應間的分維值表現為中低山盆地,體現了不同類型地貌表面粗糙性或復雜性的差異,因此分維值大小可作為地貌表面外營力侵蝕作用強度的重要指標:利用標度的間斷點和各種地貌類型表面分維值或宏觀效應趨於一致,提出5 - 6km左右可作為地貌的宏觀臨界點,並且與利用地貌剖線研究所得到的5km這一數值是基本吻合的。
  3. In addition, the dq - q curves behave in different shapes. it can be concluded that the scaling properties depend colsely on the way, intensity. acting scale and distribution in space of inogenic and exogenic processes. according to the scaling natures of the two landform profiles, it is proposed that the 5km scale is the low limit of the inogenic process effects which begin to dominate landscape patterns in landform systems

    該結果對理論地貌研究具有重要意義:不同地貌類型表面的多重分形譜值域表現為中低山盆地的總體特徵,地貌表面多重分形譜特徵表了內外營力地貌作用類型和強度在空間上分佈的不均勻程度。
  4. The results of 2 - d resistivity inversion of the yishui - tangtou and the liujazhuang faults indicate that electrical structures on both sides of the fault zone present obvious difference, the resistivity of the hanging wall is low and partially high, while that of the foot wall is high, and the faults are high - obliquity faults

    沂水湯頭斷裂、劉家莊斷裂的二維電阻率反演結果表,斷裂帶兩側的電性結構呈現出整體性的差異,正斷層的上盤為低阻和局部、低阻擾動;而斷層下盤多為均勻的;斷層為角度斷層。
  5. ( 2 ) the liman problem is normally adopted to check the liability of numerical method. the calculation error was within 9 % by comparison with the theoretic solutions of liman problem in the following case, the dimensionless calculation length was 2 with high pressure zone 0. 8, and the dimensionless state parameters were p1 = 2, p2 = 1, p1 = p2 = 1, u1 = u2 = 0. experiment results in literature [ 8 ] were used to check the adaptability of the numerical model developed here for unconfined gas cloud explosions and the calculation error was within 13 %

    ( 2 )數值方法的可靠性通常用黎曼問題的解析解檢驗,本文以無量綱計算長度為2 ,長度為0 . 8 ,狀態參數為p _ 1 = 2 , p _ 2 = 1 , _ 1 = _ 2 = 1 , u _ 1 = u _ 2 = 0條件下的黎曼問題解析解對所編制的爆炸場計算程序進行了考核,結果表該程序的計算誤差在9以內;為考核本文計算模型預測開敞空間氣雲爆炸的適用性,以文獻[ 8 ]的實驗數據進行了校核,計算誤差在13以內。
  6. Further more, the coherence between circulation and olr are calculated and analyzed. the results show that there is positive correlation between australian high and the precipitation of middle and low reaches of yangtze rivers, and negative correlation between okhotsk and the precipitation of middle and low reaches of yangtze rivers

    由相關分析得出,春季鄂霍次克海與澳大利亞和長江中下游地夏季olr值分別表現出較好的正相關和負相關,表這兩個地位勢度場的變化與夏季長江中下游地降水多少有著密切的關系。
  7. The research shows that : 1 ) the ductility of the hsc bending members constructed is much greater than 5 ; 2 ) increasing the vertical links and distribution steel can increase the deflection under ultimate moment ; 3 ) with appropriate compressive bars, vertical links and distribution steel the increase of moment after yield and the decrease of moment under ultimate moment can be ignored, so the ductility of the hsc bending member is much larger ; 3 ) the width / depth ratio of hsc bending member has no obvious effect on the ultimate compressive strain of concrete ; 4 ) the method used here to calculate the deflection is applicable ; 5 ) the location of crack coincides with the location of vertical links and distribution steel ; 6 ) the bending property of the hsc structure under the blast load can meet the demand of protective engineering

    研究表:本文研究的梁、板構件的延性比遠大於5 ;增加箍筋(鉤筋、分佈筋)含量,可以提混凝土剝落時的撓度;在適當的受壓筋、箍筋(鉤筋、分佈筋)含量下,可以忽略壓混凝土剝落瞬間的承載力下降,從而大大提構件的延性;受彎構件的寬比對壓混凝土極限應變的影響不顯;受彎構件的裂縫間距受箍筋(鉤筋、分佈筋)的布置影響;文中所用的承載力和變形計算方法是可行的。化爆試驗表強混凝土構件的動載抗彎性能能夠滿足防護結構的要求。
  8. The studies of in - layer heterogeneity are as follows : the text depicts the characteristics of heterogeneity by calculating the coefficient of variability, kmax / k and k. max / k. min of sand layers of different sedimentous microfacies ; divides interlayer into two types, and counts their numbers, thickness, frequency and density of a single sand layer according to the characteristics of lithology and logging, finally summarizes the characteristics of interlayer distributing ; sets up five in - layer heterogeneity models and points out that the primary models are model a and c. the studies of between - layer heterogeneity are as follows : the text depicts sand layers " growth and distributing conditions by calculating the lamination factor, sandstone density and overlap coefficient ; makes certain the lithology and thickness of interlayer by the method of contrasting the typical curves

    層內非均質性研究,通過計算不同沉積微相砂體滲透率的變異系數、突進系數以及級差來說主要儲集微相的非均質特徵;據巖性及電性特徵,將層內夾層分為兩類,統計單砂層段內夾層的個數、累積夾層厚度、夾層頻率及夾層密度,並且根據夾層頻率及密度平面分布圖統計出每層的頻率相對和低值,總結夾層分佈特徵;根據物性參數隨深度的變化趨勢建立了五種儲層層內物性非均質模式,指出研究內以a型和c型模式為主。
  9. The new area of kaifeng named " bianxi " locates in jinming district, west to the city dike, east to zhongmu boundary, north to 310 national highway and south to lianluo highway

    開封市汴西新位於金腹地,東至護城大堤,西至中牟邊界,南至310國道,北至連霍速公路。
  10. The analysis of the large - scale synoptic situation shows that strong precipitation is closely related to the explosion of monsoon and the intensification of cross - equatorial flow which bring a lot of vapor and meet with cold masses at the eastern of northwest district on 8th, june causing extremely heavy rainfall ; that subtropical high - level jet at 200hpa, subtropical high at 500hpa and low - level jet at 850hpa are the weather backgrounds favorable to strong precipitation ; that the pattern of eastern highs and western lows and the establishment of a low - level jet and the coupling between upper - and low - level patterns that determine that the rain occurred in the east of the northwest china ( on average, this is the rainy season for the south of china, but not for the northwest china ) ; that water vapor comes from southerly and easterly flow which converge at the eastern of northwest district with convergence mainly in lower levels and pbl ; that the high value of the whole - level apparent heat source < q1 > is near the area of large rainfall in the direction of northeasterly - southwesterly agreeable to shear line very well and the condensation latent heat releasing is main heat source with vertical advection item playing key role in q1 and q2 ; that there is a vertical secondary circulation crossing low - lever jet whose ascending branch is at the area of large rainfall ; that the construction of convection instability and conditional symmetry instability results that there is not only deep thermal instability, but also moisture influx and triggering mechanism of thermal instability causing strong torrential rain

    作為對比,本文還對2002年6月24 - 25日發生在北京地的強地形雨進行了分析,並討論陜南、北京地兩地暴雨的異同點以及地形作用的共性和個性,為兩地暴雨預報提供有益的參考,得出了一些很有意義的結果: 1大尺度環流背景分析表: ( 1 ) 「 02 . 6 」強降水與6月上旬越赤道氣流和季風爆發密切相關,攜帶大量水汽的偏南氣流與冷空氣於6月8日交匯在西北地東部,導致了這次強降水的發生; ( 2 ) 200hpa的副熱帶西風急流、 500hpa副以及850hpa的低空急流的配置非常有利於本文分析之陜西強降水的發展與維持。大尺度形勢分析表,東西低形勢場、低空急流的建立和低空形勢的配置決定了這場降雨出現在西北地東部。與暴雨相聯系,存在一支橫越低空急流的經向垂直環流,暴雨處于該垂直環流的上升支; ( 3 )偏南和偏東氣流水汽通道在西北地東部交匯,水汽的輻合積聚主要在對流層低層和行星邊界層內完成; ( 4 )整層的視熱源< q _ 1 >在暴雨附近呈東北-西南向分佈,與切變線走向非常一致,降水產生的凝結潛熱釋放是強降水大氣的主要熱源。
  11. ( 5 ) the hazard map is got by two kinds of methods of hazard assessment. after the analysis two kinds of assessment results both show that the most dangerous area in main urban area of wanzhou distributes the area along both sides of zhuxihe and the left side of yangtze river. this result agrees with the actual distribution of landslide, which proves that the assessment result is effective

    ( 5 )通過使用兩種危險性評價方法,得到危險性圖,對其分析發現兩種評價的結果都顯示,萬州主城危險性最域主要分佈在苎溪河兩岸和長江的左岸,這與實際的滑坡分佈基本吻合,這充分說了評價結果的有效性。
  12. Shenyang gao xin district awarded “ civilization enterprise ” ect. honors

    沈陽授予的「文單位」等榮譽稱號。
  13. The initial challenge to researchers and advisors is to recognize that crop production, especially at consistently high yield levels, is a complex problem that requires a team effort to unleash creative thinking from various disciplines that can be combined to increase crop yields

    研究工作者和農業顧問的首要任務是認識並了解作物生產,特別要了解的生產是一個復雜的問題,需要一個綜合性課題組的共同努力,發揮各自的聰才智,為提作物的產量而努力。
  14. After that, the multifractal spectra dq - q are computed by fixed - mass method. the results show that in the studied scaling range different types of landscapes and profiles in different directions perform different fractal properties, that is, the d value and crossover length ^ decrease in turns with the landform type from high - moutain, mid - low mountain to basin, and the profile parallel to wear grooves often has lower d values ( < 1. 5 ) than those perpendicular to wear grooves do ( 1. 5 ) in the same section

    提出以地貌分形特點和渡越長度為依據的地貌層次界定方案,研究指出了5km左右應為宏觀臨界點:不同構造地貌、不同取向的剖線的多重分形譜值域范圍寬窄表現出中低山盆地,垂直構造地貌斜坡方向斜交方向平行方向的特點,表了內外營力作用的不均勻性和方向性。
  15. Research points out that the three key factors, which determine the nox emissions, are maximum peak temperature, rich oxygen concentration and the duration in which combustion products stay at high temperature zone

    船舶柴油機的氮氧化物主要是山于大氣中的氮在柴油機燃燒過程中被氧化而成。研究表溫、富氧以及燃燒產物在的停留時間是決定氮氧化物排放量的三個決定因素。
  16. Senior port health officer of the dh, dr henry kong said if travellers could not avoid going to places of high incidence of meningococcal infection, they are advised to wear surgical masks and use anti - bacterial hand sanitizer when necessary

    ?生署級港口?生主任江永醫生說,若旅遊人士無可避免要到腦膜炎雙球菌,有需要時應戴上口罩及以殺菌消毒液洗手。
  17. The results demonstrate that the upper limit of permafrost in this area had declined from 1970s to the middle phase of 1990, and permafrost has appeared degenerate tendecy, but since middle 1990s, permafrost have a stable state ; ground temperature of roadbed near the earth surface is higher than that of the natural ground, thawing time of roadbed near the earth surface is longer than that of the natural ground, the heat income within the permafrost is greater than the heat release from the permafrost during anannual period, the heat accumulation within the permafrost is temporarily appeared as temperature rising, but with the heat accumulation within permafrost growing up year by year, permafrost temperature will become higher gradually, and strong thawing of permafrost could be happened in the region

    結果表:風火山地從20世紀70年代到90年代中期凍土上限下降,凍土出現退化現象,從90年代至今凍土趨于穩定;路基近地表地溫於對應天然地表下的地溫,路基近地表經歷的融化期長于對應天然地表,進入多年凍土的熱收支也呈現出吸熱顯大於放熱的周期性變化,進入多年凍土的熱積累暫時以增地溫耗熱為主,但隨著凍土吸熱量的逐年積累、凍土溫度的不斷升,本凍土可能發生強烈融化。
  18. Add : san ming road, cangjiang industrial park, gaoming district, foshan city, guangdong province, china

    地址:廣東省佛山市高明區滄江工業園三
  19. Which boasts the title of rear garden of guangzhou city, our company, foshan jiedali metallic products co., ltd. is a sino - foreign joint venture

    佛山市捷達利金屬製品有限公司位於佛山市高明區楊和鎮人和工業開發
  20. Foshan gaoming yadi plastic board factory imports advance producing art, aims to serve customers with high quality and honesty

    佛山市高明區亞迪塑料板材廠以先進的生產工藝、優質的產品質量、誠信的服務宗旨多年來贏得國內外客戶的支持和信任。
分享友人