Research on variation of thermal pressure along hugoniot of solids 线上热压变化的研究
Rankine - hugoniot condition 于戈尼奥条件
It is found that , the quasi - isentropic curve is located between the hungoniot curve and isentropic curve , and more close to the latter 它介于冲击hugoniot线和等熵线之间,并更接近于等熵线。
In chapter 2 , the basic theory of the principle hugoniot and the methods of fluid velocity measurement are briefly summarized 第二章是本工作的理论基础,简要讨论了测量和制靶的基本原理和方法。
In this work , oscilloscopes with high precision are used to record the time interval when shock wave passed through the porous sample . we have measured the hugoniot data of porous iron whose initial densities varies from 6 . 151 to 6 . 725 mg / m3 本文采用高精度的示波器作为时间间隔记录仪器,测量了初始密度为6 . 151 - 6 . 725g / cm ~ 3多孔铁的冲击压缩数据。