風寒型 的英文怎麼說

中文拼音 [fēnghánxíng]
風寒型 英文
wind-cold type
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 寒 : Ⅰ形1 （冷） cold 2 （害怕; 畏懼） afraid; fearful; tremble （with fear） 3 （貧困） poor; needy 4...
  • 風寒 : wind chill; chill; cold; wind-cold
  1. Cushion plant a plant that forms a tight low hummock as an adaptation to cold and dry or windy situations

    墊狀植物：為了適應寒冷、乾旱以及風沙的氣候形成的低矮的植物類型。
  2. This paper describes characteristic succession of dolomitic limestone tempestites from middle - upper cambrian in huangshi, eastern hubei province

    摘要鄂東黃石地區中上寒武統中下部發育一套典型的白雲質風暴巖。
  3. Clinical observation on governor vessel daoqi method for treatment of dyssomnia in the patient of depression

    滯針法治療風寒濕阻型類風濕性關節炎臨床觀察
  4. The results showed that : the integrated ecological risk was presented symmetrically along brahmaputra, and was mitigated from valley farming area to mountain pastoral area ; the hazards of main risk sources to risk suffer in each sub - region was differently, drought was the common risk source and imperils farming and stock raising severely ; aimed at enhancing the ability of fighting drought, controlling flood and stabilizing sand engineering measures should be taken steps to prevent those hazards ; mountain hazards must be controlled in resident area and along arterial traffic ; manual work should be done to void hail in those area where hails attacked heavily ; there is need to promulgated risk knowledge to herdsmen for strengthening their risk consciousness and improve the ability of preventing risk and self - help after hazards happened in the pasturing area

    扎囊縣綜合生態風險沿雅魯藏布江呈現對稱型分佈，並由河谷農業區向高山牧業區逐漸降低；各亞區的主要風險源對風險受體的危害強度差異較大，乾旱是共同的風險源，造成的農牧業生產損失最為嚴重；抗風險措施主要有在河谷地帶採取工程措施以提高抗旱、防洪和固沙能力，在半山臺地加強治理居民點及交通沿線的山地災害，在多雹區進行人工消雹；在高寒牧區向牧民傳播風險知識，以加強其風險意識，提高規避風險和災后自救能力。
  5. Took sha - zhuyu and east shore of qing - hai lake as the examples and based on the mass of field survey and soil analyse, took comparative method, we carried through the researches on the causes of the desertification, the origin of sandy desertificational land substance, the development diversification and difference of soil characteristic in process of manual and spontaneous vegetation recovery in high frigid regions and make out the taxonomy of desertificational land in high frigid region of china. the result obtained are summarized as follows : 1. the development of the desertificational land in high frigid regions is caused by the manual and spontaneous factors

    論文首次對高寒地區的砂質荒漠化土壤進行系統研究，以沙珠玉和青海湖東岸為例，通過野外考察和土壤樣品室內化驗，採用對比分析的研究方法，對中國高寒地區荒漠化的成因和研究區砂質荒漠化土地的形成演變，土壤發生特性、人工植被恢復和自然植被恢復過程中土壤的發育差異和性質變化進行系統研究，並用系統分類體系對研究區土壤進行類型劃分，得到主要結論如下： 1 、高寒地區荒漠化的發生發展是在自然因素和人為因素共同作用下進行的，沙珠玉地區風沙土是就地產生的，青海湖東岸地區風沙土主要是由風從湖的西岸搬運而來的，兩地區砂質荒漠化發展仍然十分嚴重。
  6. There are some differences between air conditioning rooms and natural ventilation ones ; the same situation exists with their thermal comfort requirements. the paper, aiming for thermal environment characters of residential buildings in cold zone, in the first times by means of fuzzy evaluation, puts forward a fuzzy evaluating model of the thermal feelings in a natural ventilation room of residential houses, which is mainly based on studies of the subjective feelings from people living in such curtain houses and measures of objective data from investigation with questionnaires

    本文針對寒冷地區居住建築熱環境特徵，以實際居住建築中的人體主觀感覺為研究對象，伴隨客觀參數測量的問卷調查手段，首次以模糊評價方法給出居住建築自然通風房間熱感覺的模糊評判模型，在此基礎上給出熱環境綜合評價指標；針對居住建築空調開啟特性，根據住宅自然通風與空調臨界轉換條件，提出能耗修正系數以便對此類建築的能耗進行正確科學的評價。
  7. The climax development group is isohumosols after sandy soil fixed under vegetation recovery condition in research regions. there was no different in soil type after 40 years developed. this manifested that soil formation and development process is very slow in high frigid regions

    6 、研究區土壤在植被恢復條件下，風沙土被固定以後，經過40多年的發育，類型未發生明顯分化，表明在高寒地區土壤的形成發育過程相當緩慢，土地一旦發生荒漠化，恢復治理相當困難，所以荒漠化防治要以預防為主。
  8. A clinical observation of hanshibi pill for rheumatism of type of simultaneous occurrence of cold dampness syndromes

    寒濕痹片治療寒濕痹阻型風濕病的臨床觀察
  9. This paper describes unique succession of calcareous tempestite from the early cambrian qingxudong formation, northeastern guizhou province

    摘要在黔東北銅仁江口地區下寒武統清虛洞組下部發育一套特徵典型、序列特殊的鈣質風暴巖。
  10. The climate of haibei research station was dominated by southeast monsoon and high pressure of siberia. it has a continental monsoon type climate, with severe and long winters and short cool summers

    受東南季風和西伯利亞高壓的影響，海北實驗站地區呈現典型的大陸氣候，有較長且寒冷的冬季和較短而涼爽的夏季。
  11. Phosphate deposits are distributed along the margin, platform and basin in the west yangtze area. the analysis methods include the paleogeography, petrology, organic geochemistry, geochemistry. the conclusions are drawn that the source of phosphate deposits distributed along the margin originate from the weathering production of continent, while phosphate deposits along the platform and basin gain phosphorus through hot spring on the buttom of the sea floor, which is brought to the sedimentary environment by rising sea - fluid, then accumulated by the organism and microorganism, meanwhile, basin phosphorite keep relatively higher organic carbon content

    認為早寒武世早期古陸遭受風化，被剝蝕下來的產物成為潮坪型磷塊巖的主要磷質來源，在碳酸鹽巖臺地發生的熱點活動和上升洋流從盆底深部帶來的磷質，共同作為臺地型磷塊巖的磷源，盆地型磷塊巖的磷質同樣是由熱點活動和上升流攜帶至缺氧的沉積環境中，通過藻類或微生物的富集作用成巖，並保留了較高的有機碳含量。
  12. Synoptic weather patterns leading to the arrival of cold surges of the winter monsoon in hong kong are examined and typical patterns are identified for the reference of forecasters

    詳細分析過一些冬季季候風寒潮抵達香港之天氣圖形勢后，天文臺鑒定了典型的模式供預報員參考。
分享友人
分享到 Line

分享到臉書