Seminar talk, 18 September 2024: Difference between revisions

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We present general case for <math>n=1</math> and several systems for <math>n=2</math> and <math>3</math>. The key is that the Riemann invariant at the microscale is the "flux" rather than "density". It allows for exact solutions of several 1D problems: "smoothing" of shocks and "sharpening" of rarefaction waves into shocks due to microscale <math>x</math>- and <math>t</math>-dependencies, flows in piecewise homogeneous media. It also allows formulating an upscaling algorithm based on the analytical solutions and its invariant properties.
We present general case for <math>n=1</math> and several systems for <math>n=2</math> and <math>3</math>. The key is that the Riemann invariant at the microscale is the "flux" rather than "density". It allows for exact solutions of several 1D problems: "smoothing" of shocks and "sharpening" of rarefaction waves into shocks due to microscale <math>x</math>- and <math>t</math>-dependencies, flows in piecewise homogeneous media. It also allows formulating an upscaling algorithm based on the analytical solutions and its invariant properties.
| video =  
| video = https://video.gdeq.org/GDEq-zoom-seminar-20240918-Pavel_Bedrikovetsky.mp4
| slides =  
| slides = [[Media:Moscow_Osja_240918.pdf|Moscow_Osja_240918.pdf]]
| references =  
| references = [[Media:f(s,x)_exact_upscaling_240918.pdf|f(s,x)_exact_upscaling_240918.pdf]]
| 79YY-MM-DD = 7975-90-81
| 79YY-MM-DD = 7975-90-81
}}
}}

Latest revision as of 08:40, 4 January 2025

Speaker: Pavel Bedrikovetsky

Title: Exact solutions and upscaling in conservation law systems

Abstract:
Numerous transport processes in nature and industry are described by n×n conservation law systems ut+f(u)x=0, u=(u1,,un). This corresponds to upper scale, like rock or core scale in porous media, column length in chemical engineering, or multi-block scale in city transport. The micro heterogeneity at lower scales introduces x- or t-dependencies into the large-scale conservation law system, like f=f(u,x) or f(u,t). Often, numerical micro-scale modelling highly exceeds the available computational facilities in terms of calculation time or memory. The problem is a proper upscaling: how to "average" the micro-scale x-dependent f(u,x) to calculate the upper-scale flux f(u)?

We present general case for n=1 and several systems for n=2 and 3. The key is that the Riemann invariant at the microscale is the "flux" rather than "density". It allows for exact solutions of several 1D problems: "smoothing" of shocks and "sharpening" of rarefaction waves into shocks due to microscale x- and t-dependencies, flows in piecewise homogeneous media. It also allows formulating an upscaling algorithm based on the analytical solutions and its invariant properties.

Video
Slides: Moscow_Osja_240918.pdf

References:
f(s,x)_exact_upscaling_240918.pdf