水汽壓 的英文怎麼說

中文拼音 [shuǐ]
水汽壓 英文
aqueous vapor pressure
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • : 名詞1. (由液體或某些固體變成的氣體) vapour2. (水蒸氣) steam
  • : 壓構詞成分。
  1. The paper reports concisely the technology development of pretreatment and subsequence treatment of acidic water stripping installation now, the technology of pretreatment of acidic water include : remove waste gas, waste oil, suspending solid, effluvium and safety measure taken, the technology of subsequence treatment of acidic water include : the technology of return use of srripped water and the technology of sbr and the technology of ion exchange of denitrification, especially the proprietary technology of fripp in the field

    摘要簡述了目前煉油廠酸性提裝置的上下游處理技術及其研究進展,上游技術主要包括:酸性脫氣、除油、脫懸浮物、惡臭氣體脫臭和應採取的安全防護措施;下游技術主要包括:提凈化的回用、 sbr法、離子交換法除氨等工藝,並簡要介紹了撫順石油化工研究院在本領域上的專有技術。
  2. Ice possesses a lower equilibrium vapour pressure than water.

    冰具有比低的平衡蒸
  3. Over the range of air temperature, the saturation vapor pressure fluctuates from less than 1 / 10 to over 100 millibars, or by a factor of 1000

    在氣溫變化范圍內,飽和水汽壓在小於1毫巴到超過100毫巴(即大於1000倍)間變動。
  4. Using the ground humidity parameter data, the precipitable water of single station was more accurate than the data retrieved from satellite data. but it was of low spatial and temporal resolutions compared with that retrieved from satellite data

    用地面濕度參量資料(地面水汽壓)估算晴空大氣可降量,其單站的估算結果比用衛星資料反演的結果要精確,但是估算的場時空解析度不如衛星資料反演的高。
  5. Using outputs of ground temperature, vapor pressure, wind speed and low cloudage. middle cloudage as well as high cloudage from mm5v36, and ground direct radiation and out - going scattered radiation from modtran3

    利用數值預報模式mm5v36輸出地面氣溫、水汽壓、風速和低雲量、中雲量及高雲量等氣象要素。利用大氣輻射傳輸模式modtran3 . 0輸出地面太陽直接輻射和射向天空的散射輻射以及總輻射。
  6. This paper studies the spatial distrihution of water vapor press in the mountain areas of chongqing, with the month average data of water vapor press of climatic reorganized data including 34 meteorological observing stations in chongqing and 4 around it from 1971 to 2000 and 7 meteorological sentries in it from 1997 to 1999, and 100mx 100m dem of chongqing. according to the theory of mountain climate and basing on gis, it analysises the influencing factors to water vapor press decreasing coefficients in chongqing, and studies the relations among water vapor press longitude latitude and sea level elevation, and founds the water vapor press spatial distribution model in chongqing, and calculates the spatial distribution of the month average and the year average water vapor press in chongqing, and completes the cartographies of the water vapor press spatial distribution of chongqing

    本文利用重慶地區34個及其周圍4個常規氣象觀測站1971 2000年30年和7個氣象哨1997 1999年3年氣候整編的月平均水汽壓資料,以及重慶地區100m 100mdem數據,對重慶地區山地水汽壓空間分佈進行研究根據山地氣候學原理,利用gis技術,分析重慶地區水汽壓遞減系數的影響因子,研究水汽壓與經度緯度和海拔高度等因子的關系,建立重慶地區水汽壓空間分佈模型,計算重慶市月平均和年平均水汽壓空間分佈,並完成重慶市水汽壓空間分佈的制圖。
  7. Water vapor press decreasing coefficients are different in different time

    水汽壓遞減系數在不同時間是不相同的。
  8. Saturation vapour pressure

    飽和水汽壓
  9. Spatially explicit distribution of water vapor pressure over chongqing under real terrain

    起伏地形下重慶市水汽壓的空間分佈
  10. Geographical situation and sea level elevation are the main influencing factors to the spatial distribution of water vapor press

    地理位置和海拔高度是水汽壓空間分佈的主要影響因子。
  11. Monthly relative humidity, dew point, web - bulb temperature and vapour pressure recorded at the observatory between 1961 - 1990

    1961 - 1990年天文臺錄得相對濕度露點濕球溫度和水汽壓之月平均值
  12. Monthly relative humidity, dew point, web - bulb temperature and vapour pressure recorded at the observatory between 1971 - 2000

    1971 - 2000年天文臺錄得相對濕度露點濕球溫度和水汽壓之月平均值
  13. The relations between soil surface resistance and evaporating time, and difference of vapour pressure between evaporating plane and atmosphere were simulated. simulating result of the latter was better than that of the former

    同時,還對土壤表面阻力與蒸發時間的關系、與蒸發時間及土壤蒸發面和大氣間水汽壓差的關系進行了模擬,結果后一種比前一種模擬更符合實際。
  14. Reference crop evapotranspiration ( rce ) characterized by its nonlinearity and multi - time scale feature, may vary with the change of time under the influence of stochastic variation of meteorological factors such as temperature, sunlight, wind speed, vapor pressure and so on

    摘要受氣溫、日照、風速、水汽壓等因子隨機變化的影響,參考作物騰發量時序過程具有非線性、多時間尺度變化等特性。
  15. It looks something like the equilibrium curve in figure 1 below. figure 1

    像以下的均衡曲線圖一,想想氣溫與水汽壓力的關系。
  16. Recall the relationship between air temperature and vapour pressure ( i. e. water vapour pressure ). it looks something like the equilibrium curve in figure 1 below

    像以下的均衡曲線圖一,想想氣溫與水汽壓力的關系。
  17. You ll notice that the equilibrium curve in figure 1 curves upward, that is, the equilibrium vapour pressure increases faster at higher temperatures

    你會留意圖一的均衡曲線是向上弧的,這樣,均衡水汽壓力在較高溫度時上升較快。
  18. The results showed that soil surface resistance often increased with evaporation time and cumulative evaporation, but the relation might be changed by variation of difference of vapour pressure between evaporating plane and atmosphere ; difference of vapour pressure between evaporating plane and atmosphere was one of the major factors for determining the soil surface resistance

    結果表明,土壤表面阻力總趨勢是隨蒸發時間的延長和累積蒸發量的增加而增大,但這種關系有可能被土壤蒸發面和大氣間水汽壓差的改變所打破,土壤蒸發面和大氣間水汽壓差是決定土壤表面阻力的主要因素之一。
  19. The month average and the year average water vapor press in chongqing both show that : the water vapor press decreases with the increasing of sea level elevation ; the water vapor press values in north - west and middle hill areas are middle and high ; the water vapor press values in north - east and south - east mountain areas are relatively low. the sea level elevation in north - east and south - east mountain areas of chongqing is higher, especially the north - east mountains are more rugged than the north - west mountains, and the decreasing of water vapor press with the increasing of sea level elevation is more distinct, so the lowest value often appears in the north - east mountains not in the north - west mountains. the seasonal change of water vapor press in chongqing is also distinct : the values of water vapor press are low mostly in winter, and the high values are relatively less ; the values of water vapor press are middle and high mostly in summer, and the low values are relatively less, the values in spring and autumn are between them

    重慶市全年各月月平均和年平均水汽壓都表現出:隨著海拔高度的增加,水汽壓逐漸減小;西北部和中部的丘陵低山地區一般為水汽壓的中高值區;東北部與東南部的山地地區的水汽壓則相對較小重慶市東北東南山地地區海拔高度較高,尤其是東北山區的山地較東南山區的起伏更大,水汽壓隨海拔高度的減小更加明顯,因此各月的最小值往往出現在東北山區而非東南山區重慶市水汽壓的季節變化也很明顯:冬季水汽壓多為小值,大值較少;而夏季多為中、大值,小值較少;春秋季則介於兩者之間。
  20. The mountain water vapor press decreases as a e index with the increasing of sea level elevation ; the constant item and the once items of longitude and latitude are important to the spatial distribution of water vapor press ; the twice items of longitude and latitude are less important to the spatial distribution of water vapor press

    山區水汽壓隨著海拔高度的增加呈e指數減小;經度和緯度的常數項和一次項對水汽壓空間分佈的影響比較大,經度和緯度的二次項對水汽壓空間分佈的影響比較小。
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