supercooled 中文意思是什麼

supercooled 解釋
adj. 形容詞 【化學】過冷（的），（不凝結而）冷卻到冰點以下的。

  1. Release of silver iodide ( agi ) into an existing supercooled cloud ( i. e., air temperature between - 39 and - 5 celsius ) can convert water vapor to ice crystals, which is called sublimation

    將碘化銀播灑至已形成的過冷卻雲中（既空氣溫度在- 39攝氏度? - 5攝氏度）能將水汽轉化為冰晶，這個轉化過程被稱為凝華。
  2. Glass and pitch behave like supercooled liquids of very high viscosity.

    玻璃和瀝青的行為很像具有極高粘滯性的過冷液體。
  3. What happens to rubber when it ' s supercooled

    橡膠在超低溫的環境下會怎麼樣？
  4. Study on the measure of reducing condensate ' s supercooled degree

    減少凝結水過冷度措施的研究
  5. Microforming progress of bulk amorphous alloys in supercooled liquid region

    大塊非晶合金在過冷液相區微塑性成形的研究進展
  6. To raise the freezing temperature of supercooled water in encapsulated ice storage requires some additives into the water

    在封裝式蓄冰技術中，為提高過冷水開始結冰的溫度，需向水中加入合適的成核添加劑。
  7. Application the retrieval coefficients of the city of changchun in april to a field experiments in jilin province, on april 22 demonstrate the airborne up - looking microwave radiometer can detect cloud liquid water and supercooled liquid water content

    此外，本文將求得的長春地區4月的反演系數應用到長春4月22日的一次飛行實驗中，結果表明，能夠探測出雲中液態水和過冷水含量及其變化。
  8. When snow crystals strike supercooled droplets, the droplets will immediately freeze onto them. this process, called riming, forms soft particles known as snow pellets or grains. in temperate zones, the melting of snow pellets provides much of the rainfall from cumulus clouds

    每當雪晶碰到過冷的水點時，它們會立刻凝固在一起，形成的軟粒子便是雪小球，而整個過程被稱為"蒙霜" ;在溫和的區域里
  9. Cloud liquid water content is always one of the most important quantities in many subjects and operations, particularly in modification weather the conditions of cloud liquid water and supercooled liquid water content are the predetermination conditions of seeding clouds

    雲中液態水含量一直是多種學科和業務中都極其重要的量，尤其是人工影響天氣領域，雲中雲水含量及過冷水條件是決定可播性的先決條件。
  10. The paper works out the ice crystal spectrum distributing in the different macroscopic and micro - backgroud of the cloud ( ie, the thickness, the temperature and the supersaturation with respect to ice of the nucleation layer ). this paper also works out the amount of catalyst which is allowed in the cloud nucleation layer according to the different quantity of the supercooled water, the density of the supersaturation of the vapor with respect to ice. simultaneously, the paper discusses the i nfluence of remaining time when seeding artificial ice nucleus in the different ascending - velocity and altitude, and elicits the proper seeding altitude of the catalyst

    以此解為依據，得出了不同均流時，人工引入冰核在核化層存留時間，再以此時間作為人工冰核凝華增長時間，求出不同的雲宏微觀背景（如核化層厚度、溫度、冰面過飽和度等）下的冰晶譜分佈，經和實際資料比對符合相當好。進而求出核化層中不同過冷水量、冰面過飽和水汽密度下雲核化層可允許的催化用量。同時討論了不同升速，不同高度引入人工冰核時對其存留時間的影響。
  11. The results show that the auto - conversion of frozen drops and graupels ( cnfh, cngh ) are the main sources of the hailstones in the strong convective storm studied in the paper, but the contribution of frozen drops is greater than that of graupels. hailstones mainly depend on the processes of collecting supercooled water ( clch, clrh ) to grow. the relatively simple mass continuous equation was used to calculate vertical velocity, and use radial projection relation of dual - doppler radar to retrieve the case ' s three - dimensional wind field

    同時模擬分析了冰雹形成的微物理過程，結果表明，本個例模擬雹雲中，冰雹粒子主要由凍滴和霰轉化（ cnfh ， cngh ）形成，但凍滴對冰雹形成的貢獻要比霰大得多，冰雹含水量中心的發展演變與凍滴含水量中心的發展演變相一致，冰雹主要是通過撞凍過冷水過程（ clch ， clrh ）而進一步長大的。
  12. Finally, it briefly discusses the feasibility, the applying foreground and the approach with regard to the calculating method about the amount of catalyst provided in this paper by integrating the ascending - velocity field and cloud water field in the possible working section abstracted from the mm5 mesoscale model with the thickness of the ice crystal particles in nucleation layer and supercooled water quantity which is surveyed by the plane

    得出適合的催化劑引入高度等。最後，簡要討論了用mm5中尺度區域模式提取可能作業區的升速場和雲水量場，並結合飛機實測核化層冰晶粒子濃度、過冷水量等，探討了本文提出的催化劑用量計算方法的可行性，應用前景和途徑。
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