isobaric 中文意思是什麼

isobaric 解釋
adj. 形容詞 1. 【氣象學】等壓線的。
2. 【化學】同量異位的。

  1. Isobaric analyses can be quickly performed.

    等壓線分析可以很快地完成。
  2. The positive storm - relative helicity center is accompany with low - level jet in 850 - hpa isobaric surface fields

    通過分析我們發現了正的相對螺旋度中心與850hpa低空急流的演變過程是一致的。
  3. Continuous blade curve of isobaric pital of spherical milling cutter

    關于球頭銑刀的等螺距連續刃口曲線
  4. Multi - mode isobaric water supply system consist of fuji vp inverter and pod

    觸摸屏的多模式恆壓供水系統
  5. Isobaric weight - change determination

    等壓重量變化測定
  6. Isobaric mass - change determination

    等壓質量變化測定
  7. Study on isobaric vapor - liquid equilibrium of methanol - propionic acid - h2o multisystems

    水多元系汽液平衡研究
  8. Isobaric weight - change curve

    等壓重量變化曲線
  9. Standard isobaric surfaces

    標準等壓面
  10. Isobaric heat capacity

    等壓熱容
  11. Study on isobaric vapor - liquid equilibrium for vinyltrichlorosilane vinyltrimethoxysilane binary system

    乙烯基三甲氧基硅烷二元體系等壓汽液平衡研究
  12. The neutron halo structure of the first excited state of i3c and the neutron - proton halo structure of the second excited state of 6li, which is the isobaric analog state of the ground state of 6he, were considered the most probable candidates to search for

    前者的中子暈結構已為實驗所證實，後者是中子暈核~ 6he （基態）的同位旋相似態，其中子-質子暈結構至今尚未被實驗證實。
  13. For " upper - air ", weather maps are usually drawn for isobaric ( i. e. equal pressure ) surfaces following the practice of conventional upper - air observations and analysis. air density and atmospheric pressure generally decrease as altitude increases

    至於高空方面，由於常規的高空觀測與大氣分析都是在標準等氣壓面上進行，所以高空天氣圖亦習慣在等壓面上繪制。
  14. We get several useful conclusions on isobaric evaporation, isothermal flash, isobaric condensation, isothermal compressed condensation. an analysis on the micro - layer evaporation model is also discussed in the paper

    在定壓汽化、定溫降壓自蒸發、定壓凝結、定溫加壓凝結、可用能、微層蒸發模型幾個方面得出了一些有用的結論。
  15. In view of the applied condition, the equations of state are assorted as follows : isothermal eos, isobaric eos, and high - temperature eos

    從適用的宏觀條件、范圍上來分，固體物態方程可分為三大類：等溫態方程，等壓態方程，高溫態方程（相對德拜溫度） 。
  16. We also compare the deduced new eos to the other famous eos. in chapter three, some common isobaric equations of state and the related parameters are introduced. we list some empirical eos and clarify their models of theory

    列出了一些常用的經驗物態方程，並闡述了它們的理論模型，同時也對本文提出的物態方程進行了驗證、比較。
  17. The elastic constants of bcc li, na and fcc al crystals have been evaluated as functions of pressure and temperature by using a new model together with ab initio electronic structure and total - energy calculations. in the model it is considered that the elastic constants of crystals at a given temperature and pressure can be calculated using a conventional density functional method but modified by a new set lattice constants due to the isobaric volumetric thermal expansion when temperature rise from absolute zero to the given one

    本文對高壓及有限溫度立方金屬彈性常數的計算方法進行了研究，建立了一種考慮溫度效應的物理模型，基於這個模型和從頭算方法，對典型的立方晶系金屬li 、 na 、 al在高壓及有限溫度（熔點以下溫度）彈性常數進行了計算，取得了與已有實驗結果較好相符的計算結果。
  18. Through analysis of potential vorticity in isobaric surface field, in low - troposphere a positive potential vorticity disturbance exist and form incline disturbance column northward before rainstorm generation, at the same time have also reflected positive potential vorticity disturbance for severe convection weather trigger role in lower - troposphere ; soon positive potential vorticity disturbance in high - troposphere downward, form one vertical disturbance column, now corresponding precipitation develop stage ; in the prosperous stage of rainstorm that maintains isolines of horizontal distribution and still have straight positive potential vorticity disturbance in 600 - 700 hpa isobaric surface field ; when near ground arises negative potential vorticity disturbance, precipitation also weaken

    通過對等壓面的位渦分析，發現了在暴雨發生前，在對流層低層有正位渦擾動存在並向北形成傾斜的擾動柱，同時也反映了對流層低層正位渦擾動對強對流天氣的觸發作用；隨后高層正位渦向下擾動，形成一個垂直擾動柱，這時對應降水的發展階段：在暴雨的鼎盛階段， 600 700hpa上空維持水平分佈的等值線，在其上還有正的位渦擾動；當近地面出現負的位渦擾動時，降水隨之也減弱。
  19. The potential vorticity ( pv ) on isobaric and isentropic surface was studied. furthermore, the pv structure of another rainstorm caused by the 9711 typhoon was compared with it and the difference of the two rainstorm was discussed

    另外又與1997年第11號臺風登陸北上造成山東全省大到暴雨過程的位渦場結構進行了對比分析，討論了兩次暴雨過程位渦場結構的異同。
  20. Isobaric identification with gf - tof method is based on the different time of flight caused by the different energy loss. the resolution of gf - tof is mainly affected by two factors. first, the rises time of current pulse from start and stop detector

    Gf - tof方法對同量異位素的分辨取決于e的不同而產生的時間不同，時間分辨僅來源於定時探測器電流脈沖上升時間的快慢和離子在氣體介質中的能量離散。
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