顽火辉石 meaning in Chinese
bishopvillite
cladnite
e tatite
enstatite
protobasite
protobastite
Examples
- The relationship between shock wave velocity and particle velocity of no - porous enstatite can be expressed as : d = 3 . 771 + 1 . 516u where the unit of velocity is km / s
可以认为，从p phugongiot数据看，在50 160gpa范围内，顽火辉石的高压相是稳定的。 - ( 3 ) by using the new method put out in ( 2 ) , hugoniot data of no - porous samples of enstatite ( mg0 . 92 , fe0 . 08 ) sio3 which initial density is 3 . 273g / m3 , were reduced and the modified hugoniot data shows very small dispersivity
（ 3 ）用（ 2 ）中提出的新方法，对前人和本文的顽火辉石hugongiot实验数据进行了初始孔隙度修正。结果显示，不同研究者所得的hugongiot数据的分散性大大减小。 - So it is impossible for enstatite to decompose to oxides between 50 to 140gpa . ( 5 ) the bulk modulus k0s and its first derivative of pressure k0s " were calculated from the experimental hugoniot data , by using eularian limit strain theory
3 ）根据本文顽火辉石hugoniot实验数据（结合前人的实验数据l用欧拉有限应变理论计算得到的顽火辉石零压炸弹性模量及其对压力的一阶导数为： k叮一266gpa ， k ； ，二4 - The linear relationship between shock wave velocity d and particle velocity u of our samples were obtained : d = 3 . 701 + 1 . 527u there the unit of relocity is km / s . no phase transition shows for enstatite with perovskite structure according to the experimental linear d - u line up to 110gpa
实验结果表明，在80 115gpa压力范围内本文所用顽火辉石的冲击波速度d与粒子速度u可用线性关系： d = 3 . 247 + 1 . 626u来描述。 - Considering that no phase transition of enstatite with perovslite structure were found during these static high pressure experiments , the consistence of the bulk modulus also supports that the high pressure phase of perovskite structure of enstatite is stability between 50 - 140gpa
考虑到静高压下的数据是在实验中未发现顽火辉石高压相有相变的情况下得到的。因此，动高压与静高压实验数据的一致性支持了在80 ? 140gpa压力内预火辉石的高压相保持稳定的观点。