Distinguished scaling and UTSD structure in weak shock reflection at nearly glancing incidence

Abstract We study weak shock reflection from a rigid wall in the joint limit of weak shock strength and nearly glancing incidence. In the distinguished scaling M = 1 + λα 2 , the inner reflection region is governed by the unsteady transonic small-disturbance ( utsd ) equation and is controlled, to leading order, by the single parameter <m:math xmlns:m="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <m:msub> <m:mrow> <m:mi>a</m:mi> </m:mrow> <m:mrow> <m:mn>0</m:mn> </m:mrow> </m:msub> <m:mo>=</m:mo> <m:mn>1</m:mn> <m:mo>/</m:mo> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:mn>2</m:mn> <m:msqrt> <m:mrow> <m:mi>λ</m:mi> </m:mrow> </m:msqrt> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> </m:math> ${a}_{0}=1/\left(2\sqrt{\lambda }\right)$ , independent of the ratio of specific heats γ . Thus the known utsd detachment value <m:math xmlns:m="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <m:msub> <m:mrow> <m:mi>a</m:mi> </m:mrow> <m:mrow> <m:mi>d</m:mi> </m:mrow> </m:msub> <m:mo>=</m:mo> <m:msqrt> <m:mrow> <m:mn>2</m:mn> </m:mrow> </m:msqrt> </m:math> ${a}_{d}=\sqrt{2}$ corresponds in this scaling to λ d = 1/8, with Guderley–Mach reflection for λ &gt; 1/8. The physical trajectory angle is obtained by multiplying the canonical utsd trajectory function g ( a ) by the Mach-number strength scale <m:math xmlns:m="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <m:mi>δ</m:mi> <m:mo>=</m:mo> <m:msqrt> <m:mrow> <m:mn>2</m:mn> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:msup> <m:mrow> <m:mi>M</m:mi> </m:mrow> <m:mrow> <m:mn>2</m:mn> </m:mrow> </m:msup> <m:mo>−</m:mo> <m:mn>1</m:mn> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> </m:mrow> </m:msqrt> </m:math> $\delta =\sqrt{2\left({M}^{2}-1\right)}$ , so that <m:math xmlns:m="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <m:msub> <m:mrow> <m:mi>χ</m:mi> </m:mrow> <m:mrow> <m:mtext>phys</m:mtext> </m:mrow> </m:msub> <m:mo>=</m:mo> <m:mi>δ</m:mi> <m:mi>g</m:mi> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:mi>a</m:mi> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> <m:mo>+</m:mo> <m:mi>O</m:mi> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:msup> <m:mrow> <m:mi>δ</m:mi> </m:mrow> <m:mrow> <m:mn>2</m:mn> </m:mrow> </m:msup> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> <m:mo>=</m:mo> <m:mn>2</m:mn> <m:msqrt> <m:mrow> <m:mi>λ</m:mi> </m:mrow> </m:msqrt> <m:mspace width="0.17em"/> <m:mi>α</m:mi> <m:mi>g</m:mi> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:msub> <m:mrow> <m:mi>a</m:mi> </m:mrow> <m:mrow> <m:mn>0</m:mn> </m:mrow> </m:msub> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> <m:mo>+</m:mo> <m:mi>O</m:mi> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:msup> <m:mrow> <m:mi>α</m:mi> </m:mrow> <m:mrow> <m:mn>3</m:mn> </m:mrow> </m:msup> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> </m:math> ${\chi }_{\text{phys}}=\delta g\left(a\right)+O\left({\delta }^{2}\right)=2\sqrt{\lambda } \alpha g\left({a}_{0}\right)+O\left({\alpha }^{3}\right)$ . We rederive the self-similar utsd reduction, sonic parabola, and shock polar in order to make the convention and the detachment map self-contained. We also record a formal adjoint solvability expression for the first correction H

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Journal
Transport Phenomena
Published
2026-07-23
DOI
https://doi.org/10.1515/tp-2026-0071
Primary Topic
High-pressure geophysics and materials
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article
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article

Distinguished scaling and UTSD structure in weak shock reflection at nearly glancing incidence

Justin Kin Jun Hew
Transport Phenomena
High-pressure geophysics and materials
article

Distinguished scaling and UTSD structure in weak shock reflection at nearly glancing incidence

Justin Kin Jun Hew
article en

Abstract

Abstract We study weak shock reflection from a rigid wall in the joint limit of weak shock strength and nearly glancing incidence. In the distinguished scaling M = 1 + λα 2 , the inner reflection region is governed by the unsteady transonic small-disturbance ( utsd ) equation and is controlled, to leading order, by the single parameter <m:math xmlns:m="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <m:msub> <m:mrow> <m:mi>a</m:mi> </m:mrow> <m:mrow> <m:mn>0</m:mn> </m:mrow> </m:msub> <m:mo>=</m:mo> <m:mn>1</m:mn> <m:mo>/</m:mo> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:mn>2</m:mn> <m:msqrt> <m:mrow> <m:mi>λ</m:mi> </m:mrow> </m:msqrt> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> </m:math> ${a}_{0}=1/\left(2\sqrt{\lambda }\right)$ , independent of the ratio of specific heats γ . Thus the known utsd detachment value <m:math xmlns:m="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <m:msub> <m:mrow> <m:mi>a</m:mi> </m:mrow> <m:mrow> <m:mi>d</m:mi> </m:mrow> </m:msub> <m:mo>=</m:mo> <m:msqrt> <m:mrow> <m:mn>2</m:mn> </m:mrow> </m:msqrt> </m:math> ${a}_{d}=\sqrt{2}$ corresponds in this scaling to λ d = 1/8, with Guderley–Mach reflection for λ &gt; 1/8. The physical trajectory angle is obtained by multiplying the canonical utsd trajectory function g ( a ) by the Mach-number strength scale <m:math xmlns:m="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <m:mi>δ</m:mi> <m:mo>=</m:mo> <m:msqrt> <m:mrow> <m:mn>2</m:mn> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:msup> <m:mrow> <m:mi>M</m:mi> </m:mrow> <m:mrow> <m:mn>2</m:mn> </m:mrow> </m:msup> <m:mo>−</m:mo> <m:mn>1</m:mn> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> </m:mrow> </m:msqrt> </m:math> $\delta =\sqrt{2\left({M}^{2}-1\right)}$ , so that <m:math xmlns:m="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <m:msub> <m:mrow> <m:mi>χ</m:mi> </m:mrow> <m:mrow> <m:mtext>phys</m:mtext> </m:mrow> </m:msub> <m:mo>=</m:mo> <m:mi>δ</m:mi> <m:mi>g</m:mi> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:mi>a</m:mi> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> <m:mo>+</m:mo> <m:mi>O</m:mi> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:msup> <m:mrow> <m:mi>δ</m:mi> </m:mrow> <m:mrow> <m:mn>2</m:mn> </m:mrow> </m:msup> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> <m:mo>=</m:mo> <m:mn>2</m:mn> <m:msqrt> <m:mrow> <m:mi>λ</m:mi> </m:mrow> </m:msqrt> <m:mspace width="0.17em"/> <m:mi>α</m:mi> <m:mi>g</m:mi> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:msub> <m:mrow> <m:mi>a</m:mi> </m:mrow> <m:mrow> <m:mn>0</m:mn> </m:mrow> </m:msub> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> <m:mo>+</m:mo> <m:mi>O</m:mi> <m:mrow> <m:mo stretchy="false">(</m:mo> <m:mrow> <m:msup> <m:mrow> <m:mi>α</m:mi> </m:mrow> <m:mrow> <m:mn>3</m:mn> </m:mrow> </m:msup> </m:mrow> <m:mo stretchy="false">)</m:mo> </m:mrow> </m:math> ${\chi }_{\text{phys}}=\delta g\left(a\right)+O\left({\delta }^{2}\right)=2\sqrt{\lambda } \alpha g\left({a}_{0}\right)+O\left({\alpha }^{3}\right)$ . We rederive the self-similar utsd reduction, sonic parabola, and shock polar in order to make the convention and the detachment map self-contained. We also record a formal adjoint solvability expression for the first correction H

Transport PhenomenaVol. 1(3)
Australian National University (AU)
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High-pressure geophysics and materials
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