溫查文明 的英文怎麼說

中文拼音 [wēnzhāwénmíng]
溫查文明 英文
vina culture
  • 溫 : Ⅰ形容詞（不冷不熱） warm; lukewarm; hot; gentle; mild Ⅱ名詞1 （溫度） temperature 2 （瘟） acute ...
  • 查 : 查名詞1. [植物學] （山查） hawthorn; haw2. （姓氏） a surname
  • 文 : Ⅰ名詞1 （字） character; script; writing 2 （文字） language 3 （文章） literary composition; wri...
  • 明 : 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...
  • 溫查 : vin
  • 文明 : 1. （文化） civilization; culture 2. （社會發展到較高階段和具有較高文化的） civilized
  1. Based on the two ctd data sets from the cruise of the summertime in 2000 and wintertime in 2001 in bohai sea and the collected historic observed thermohaline data, we analyse systemically the distributional characteristics of temperature, salinity and density in wintertime and summertime in the bohai sea and the results reveal that the current hydrologic characteristics of the bohai sea have some obvious variances relative to the previous research results. in summer there are three low - temperature centers in the middle - layer and underlayer of the middle parts of the bohai strait, liaodong bay - mouth and bohai bay - mouth, but there is a uniform high - temperature center in the middle part of the bohai sea. in winter the isotherms extend westward and northward to the bohai sea from the warm core of the bohai strait and a cold - water tongue off the qinhuangdao spreads southeastward out, so the saddle - like isotherm pattern is formed in the middle part of the bohai sea

    利用2000年夏季和2001年冬季渤海兩次ctd資料和以前收集的渤海溫鹽調查資料，分析了渤海冬、夏季溫鹽密度的分佈特徵，結果表明，渤海現有的水文特徵與以往研究結果相比發生了明顯的變異：夏季在渤海海峽、遼東灣口和渤海灣口中部中、下層存在三個低溫中心，在渤海中部則出現一個上下均勻一致的高溫中心；冬季等溫線以渤海海峽暖中心向西和向北兩個方向伸入渤海，而從秦皇島外海有一冷水舌向東南方向伸展，在渤海中部海域形成「馬鞍狀」等溫線結構。
  2. Based upon the analysis of the data obtained during the survey, it can be concluded that : 1 ) the number of biomass of macrobenthos in the yellow sea and the east china sea in autuma is higher than that in spring, while the number of density of macrobenthos in autumn is lower than that in spring ; 2 ) the number of biomass of macrobenthos in the yellow sea is higher than that in the east china sea ; 3 ) the number of species in the yellow sea is lower than that in the east china sea ; 4 ) one of the characteristics of distribution of macrobenthos in the east china sea is that the species richness increased from the coastal waters to the offshore deep waters, from the north to the south. 5 ) the species composition in the deeper part occupied by the cold water mass of the yellow sea is more stable than that in the coastal part of the yellow sea in the late 40 ~ 50 years

    通過以上幾方面的分析，結果表明： 1 ）黃東海調查海域的秋季總生物量均高於春季，總棲息密度則低於早春季； 2 ）黃東海春季生物多樣性指數高於秋季； 3 ）南黃海、東海的水文特點顯著不同：東海底溫顯著高於南黃海底溫，東海底鹽亦高於南黃海底鹽； 4 ）南黃海春秋季生物量分佈無一致規律，東海春秋季生物量除長江口外基本上自近岸向外海逐步降低； 5 ）東海大陸架大型底棲動物的種類組成較南黃海更豐富； 6 ）東海大型底棲動物的分佈特點之一為：種類數由北向南、由近岸（西部）向外海（東部）逐漸增多； 7 ）在黃海冷水團控制的海域，其底棲動物種類組成較近岸海域穩定； 8 ）幾個生物多樣性指數各有側重，都能較好地反映底棲動物的分佈特點
  3. Through field investigation and analysis indoor, with studying all hydrochemistry data in detail, including macro components and micro components, the author finds out the hydrochemistry feature of ground water. for further specifying the ground water system, with cluster analysis of macro components of surface water and ground water in total 147 samples and the analysis of micro components, including ree, the main ground water systems are distinguished by and large, especially the ground water system main of fault no. 7 and fault no. 15 water bearing belts which have differences at macro and micro components between the two ground water systems, moreover, the main hydrogeochemistry effects are established such as lixiviation, oxidization, precipitation and mixing effect, especially the mixing effect which result in the complexit y of the hydrochemistry of deep bearing tectonic fracture water. based on them, the hydro geological model of upper dam base is established, meanwhile the author summarizes the hydrochemistry feature of weathering crevice water, surface tectonic crevice water and deep tectonic crevice water

    為此，本文以大崗山壩區水文地球化學問題為研究對象，通過野外調查和室內分析，詳細的研究了壩區水化學資料，包括宏量組分、微量組分，查明了壩區地下水水化學特徵，對採集的147個地表及地下水樣的宏量組分進行聚類分析，結合微量元素，稀土元素的研究，並應用二氧化硅地熱溫標確定了深部構造裂隙水的熱源深度，基本區分了壩區各個主要地下水水系，特別是以f7 、 f15斷裂含水帶為主的地下水系，它們的宏量組分、微量組分以及稀土等方面均存在差異，以此為基礎，結合壩區水文地質條件，建立了壩區的上壩址的水文地質模型，同時通過分析了壩區花崗巖區的水化學資料，確立了壩區主要的水文地球化學作用，分別為：溶濾作用、氧化作用、沉澱作用、以及混合作用，混合作用是導致深部承壓裂隙水水化學復雜的主要原因，並總結了壩區風化裂隙水、淺部構造裂隙水、深部構造裂隙水的水化學特徵。
  4. Abstract : the paper analyses damaging causes for fixed support of chongqing beibei chaoyang suspension bridge in high temperature in august 1992. it put forward the idea for changing fixed support into finite displacement supper support based on site and analyses for structural intemal force. it is practical for engineering

    文摘:分析重慶北碚朝陽吊橋在1992年8月高溫時，使固定支座破壞的原因，在現場調查和結構內力分析基礎上，提出了將固定支座改為有限位移橡膠墊板支座方案，實踐證明是可行的
  5. Based on the documents and my personal field research, i presented my view as below : in the first chapter, under the context of cultural anthropology, i address the issues of the general cultural study, research methodology, the current academic study of render ewenki people, the value of research and study, the traditional culture, the historical cultural transition of render ewenki people as well as their traditional living to demonstrate the significance of studying render ewenki people ; the 2nd chapter concerns the structure function, feature of their material culture ; the 3rd chapter focuses on language and culture, namely, mythology, legend, story, proverb, arts, e. g

    該論文以大量文獻資料以及本人田野調查的豐富的第一手資料為依據，分成以下四個部分具體分析和討論馴鹿鄂溫克人的傳統文化：第一章緒論部分從文化人類學的視角對馴鹿鄂溫克人文化的研究方法和理論進行科學闡述，同時概述了國內外對馴鹿鄂溫克人的研究狀況，指出了對馴鹿鄂溫克人傳統生產生活開展學術研究的緊迫性、現實性以及重要性，進而闡明了對馴鹿鄂溫克人優秀傳統文化研究的學術價值和理論意義。
  6. 1. h. ventricosa and more than three hosta cultivars, were applied in gardens and virescences in hangzhou, but showed worse in hot summer. it resulted in no correctly considering the factors, such as temperature, shading and air humidity during plant designing

    浙江人學碩十學位論文7 .玉瞥屬植物的應用調查表明，現今杭州也有玉瞥屬的紫尊以及3個以上園藝品種應用於園林綠化中，但夏季高溫時普遍長勢不好，主要原因來白于植物配置過程中沒有對溫度、遮陰和空氣濕度等因子予以正確的考慮。
  7. On the basis of the analysis of the topography, geomorphology, geological structure of geothermal area and surroundings in fuzhou city, and the survey of hydrogeological condition, and the distribution of geothermal drilling, and the geothermal water exploitation, and the groundwater regime, and the scale and distribution of land subsidence, the relationship between land subsidence and geothermal water regime was discussed. the result showed that land subsidence of geothermal area in fuzhou city was mainly induced by the excessive extraction of geothermal water in the thesis

    在分析研究福州市溫泉區及周圍的地形地貌、地質構造、水文地質條件的基礎上，對地熱井分佈、流量、水位、地下熱水開採的歷史與現狀以及對地面沉降的表現、規模、分佈規律進行了深入的調查；分析了地下熱水歷年水位、水量動態變化特徵，並探討地下熱水與地面沉降的相關關系，結果表明過量開采地下熱水是導致福州市溫泉區地面沉降的主要原因。
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