scholarly journals Propagation of a Spherical Wave in Elastoplastic Medium with Complex Equations of State

2021 ◽  
pp. 403-420
Author(s):  
Sherzod Khudainazarov ◽  
Burkhon Donayev
2021 ◽  
Vol 264 ◽  
pp. 02041
Author(s):  
Sherzod Khudainazarov ◽  
Burkhon Donayev ◽  
B Ashirov

The propagation of a spherical wave in the soil is solved in an analytically inverse way for soils with more complex equations of state. The results are obtained to propagate a spherical shock wave in soil with a more complex equation of state for the shape change in the medium. The study shows that taking into account the nonlinear elastic shock waves of the annular stress leads to an increase compared to the elastic medium. Note that in using a complicated equation of state of the soil, a spherical shock wave propagates in the soil, behind the front of which, in the disturbance region, the medium is unloaded.


2000 ◽  
Vol 98 (24) ◽  
pp. 2045-2052
Author(s):  
Keshawa P. Shukla, Walter G. Chapman
Keyword(s):  

1986 ◽  
Vol 47 (C8) ◽  
pp. C8-31-C8-35
Author(s):  
J. J. REHR ◽  
R. C. ALBERS ◽  
C. R. NATOLI ◽  
E. A. STERN
Keyword(s):  

1986 ◽  
Vol 47 (C8) ◽  
pp. C8-213-C8-216
Author(s):  
J. J. REHR ◽  
J. MUSTRE DE LEON ◽  
C. R. NATOLI ◽  
C. S. FADLEY
Keyword(s):  

1986 ◽  
Vol 47 (C8) ◽  
pp. C8-89-C8-92 ◽  
Author(s):  
R. V. VEDRINSKII ◽  
L. A. BUGAEV

AIAA Journal ◽  
1998 ◽  
Vol 36 ◽  
pp. 515-521 ◽  
Author(s):  
Charles L. Merkle ◽  
Philip E. O. Buelow ◽  
Sankaran Venkateswaran ◽  
Jennifer Y. Sullivan
Keyword(s):  

Author(s):  
Natalia Andrulionis ◽  
Natalia Andrulionis ◽  
Ivan Zavialov ◽  
Ivan Zavialov ◽  
Elena Kovaleva ◽  
...  

This article presents a new method of laboratory density determination and construction equations of state for marine waters with various ionic compositions and salinities was developed. The validation of the method was performed using the Ocean Standard Seawater and the UNESCO thermodynamic equation of state (EOS-80). Density measurements of water samples from the Aral Sea, the Black Sea and the Issyk-Kul Lake were performed using a high-precision laboratory density meter. The obtained results were compared with the density values calculated for the considered water samples by the EOS-80 equation. It was shown that difference in ionic composition between Standard Seawater and the considered water bodies results in significant inaccuracies in determination of water density using the EOS-80 equation. Basing on the laboratory measurements of density under various salinity and temperature values we constructed a new equation of state for the Aral Sea and the Black Sea water samples and estimated errors for their coefficients.


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