unsaturated air 中文意思是什麼

unsaturated air 解釋
不飽和空氣
  • unsaturated : adj. 未飽和的；不飽和的。 unsaturated compounds 不飽和化合物。 unsaturated steam 未飽和蒸汽。
  • air : n 1 空氣，大氣。2 天空，空中。3 微風，和風。4 態度，樣子，風度，氣派；〈pl 〉高傲的架子。5 傳播，...
  1. Smaller drops spend more time in the unsaturated air and, if too small, are unable to reach the ground before evaporating completely.

    較小的雨滴在非飽和空氣中耗費時間較長，如果太小則在到達地面之前就完全蒸發掉了。
  2. Thus, two air masses that are themselves unsaturated may mix to produce a supersaturated air mass, and a cloud which is just condensed water droplets usually forms

    所以，兩團氣各自不飽和，但混合后可能成為一飽和氣團，產生我們呼出的霧或凝結的小水點。
  3. Thus, two air masses that are themselves unsaturated may mix to produce a supersaturated air mass, and a cloud ( which is just condensed water droplets ) usually forms

    所以，兩團氣各自不飽和，但混合后可能成為一飽和氣團，產生我們呼出的霧或凝結的小水點。
  4. In recent years, it is obtained from experiments that water infiltration is affected by air pressure, the problem on one - dimensional water infiltration is soloed by many researchers. in this paper two - dimensional water infiltration with air - out is considered and numerical simulation is made. unsaturated infiltration is the process of factors coupling each other

    近年來，許多研究人員從實驗中得出了氣體壓力變化對水流入滲有影響，並對一維水流入滲問題進行了求解，本文將進行考慮氣體排出過程影響的二維水流入滲問題的數值求解。
  5. By comparing the numerical results of water infiltration with air and without air, it is shown that the method in this paper is more effective for solving problems of water infiltration in unsaturated soil. in this paper the forming process of oil - bearing basin is the main research object and the mathematic model of geology is built, in order to simulate the dynamic forming process of stratums especially oil - bearing stratum in geology history in the time and space concept, further to investigate the history of petroleum forming, transmitting, accumulating and predict the distributing rule and scope of petroleum, and offer an rapid, quantitative, exact, general choice for the researcher of petroleum geology. with denudation, poor - compactness and sedimentation hiatus, the stratum relations of sedimentation section is judged, and the ancient thickness and pressure of stratum layer are recovered by the inversion method of back stripping. the numerical simulation algorithm of recovery of geological history is also given

    為了利用現代化的計算技術再現含油氣盆地的地史演化發育過程，以便進一步定量化研究油氣的生成、運移和聚集的歷史以及預測油氣分佈規律、分佈范圍，為石油地質學家提供一個快速、準確、定量、綜合的研究手段，本文就含油氣盆地的地史演化發育過程為主要研究對象，建立了數學地質模型，運用優化理論與演算法，在考慮了剝蝕、欠壓實、沉積間斷等地質現象的情況下，採用回剝反演法，應用鉆井、測井、地震等方法獲得的地層物性資料，判別沉積剖面中地層的接觸關系，恢復地層的古厚度、古壓力，構造了地史恢復的數值模擬方法。
  6. Simulation of heat and mass transfer in unsaturated soil under solar radiation and air convection

    大氣對流下未飽和土壤中熱質遷移過程的實時模擬研究
  7. The pore air pressure gradually goes up with the developing of axial strain in the process of the dynamic torsional shear test of loess, but the pore water pressure hold the line or goes up a little in the last. the stress - strain dynamic constitutive relationship of intact loess and man - made loess show the hyperbolic model. there are some remarkable differences of strength and strain between unsaturated loess and saturated loess

    研究結果表明：非飽和黃土在動力扭剪試驗過程中，隨著軸向變形的發展，孔隙氣壓力逐漸上升，而孔隙水壓力則基本保持不變或後期略有升高；原狀黃土和重塑黃土的應力應變本構關系呈雙曲線型；非飽和黃土和飽和黃土的強度及變形特性存在明顯差異；進而分析了含水量、固結應力和固結應力比對黃土動力特性的影響本文最後對非飽和土的有效應力計算公式進行了討論。
  8. Advances in numerical simula tion of two - phase water and air flow in unsaturated zone

    氣二相流數值模擬研究進展
  9. Based on the generalized consolidation theory of unsaturated soils, coupled analysis of deformation of soil skeleton and movement of pore water and pore air in stiff fissured clay and swelling soil were performed for a selected slope

    在非飽和土廣義固結理論的基礎上，對某一邊坡進行了變形與孔隙水、孔隙氣流動的耦合分析。
  10. If the curve were a straight line, clouds would never form when two unsaturated air masses mix, irrespective of how different they are

    若線是直的，兩團不飽和氣團混和起來無論它們相差多遠，霧永不能產生。
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