A model to validate effective waves in random particulate media: spherical symmetry
Artur L. Gower,
Stuart C. Hawkins,
Gerhard Kristensson
Abstract:There has not been a satisfying numerical validation of the theory of effective waves in random particulate materials. Validation has been challenging because the theoretical methods for effective waves have been limited to random particulate media in infinite slabs or half-spaces, which require a very large number of particles to perform accurate numerical simulations. This paper offers a solution by providing, from first principles, a method to calculate effective waves for a sphere filled with particles for… Show more
“…Finally, substituting ( 57) into (48), we conclude the extinction theorem w inc (r) = 0 for r that satisfies (35). That is, there is no term in the average transmitted wave that satisfies the background wave equation.…”
Section: The Average Of the Incident Fieldmentioning
confidence: 82%
“…The distance b 12 appears in (11) and is sometimes called the correlation length. Our analysis shows that when (35) is true, the transmitted field ( 31) is a sum of effective waves, and the incident wave is no more.…”
Section: Deducing the Average Transmitted Wavementioning
confidence: 89%
“…In papers such as [24] that calculate the average field from first principals, it is not clear that w inc = 0. Here we remove any doubt by proving that when sufficiently inside the material, given by condition (35), we have that w inc := 0 for any incident field, any material region R, any frequency, and all types of particles. Using the results from section 4.1, we collect the terms in equation ( 36) that satisfy the background wave equation to obtain:…”
Section: The Average Of the Incident Fieldmentioning
confidence: 98%
“…As in this case each frequency has only one mode: the plane-wave. An alternate approach to validate the theory of effective waves is to do Monte-Carlo simulations of particles within a sphere [35], or circular particles within a circle [36]. These have the added benefit of requiring a finite computational domain, though the transmitted fields are more complex.…”
Section: A Plate Filled With Particlesmentioning
confidence: 99%
“…Using equations (B.13) and (34) in the integral (B.12), and swapping the order of integration leads to: where we used that B(r; a) is completely contained in R 1 for every r 2 due to (35). There are values for r 1 for which the integral in equation (B.15) is zero.…”
Section: B3 the Transmitted Scattered Fieldmentioning
Microwave remote sensing is significantly altered when passing through clouds or dense ice. This phenomenon isn't unique to microwaves; for instance, ultrasound is also disrupted when traversing through heterogeneous tissues. Understanding the average transmission in particle-filled environments is central to improve data extraction or even to create materials that can selectively block or absorb certain wave frequencies. Most methods that calculate the average transmitted field assume that it satisfies a wave equation with a complex effective wavenumber. However, recent theoretical work has predicted more than one effective wave propagating even in a material which is statistically isotropic and for scalar waves. In this work we provide the first clear evidence of these predicted multiple effective waves by using high-fidelity Monte-Carlo simulations that do not make any statistical assumptions. To achieve this, it was necessary to fill in a missing link in the theory for particulate materials: we prove that the incident wave does not propagate within the material, which is usually taken as an assumption called the Ewald-Oseen extinction theorem. By proving this we conclude that the extinction length - the distance it takes for the incident wave to be extinct - is equal to the correlation length between the particles.
“…Finally, substituting ( 57) into (48), we conclude the extinction theorem w inc (r) = 0 for r that satisfies (35). That is, there is no term in the average transmitted wave that satisfies the background wave equation.…”
Section: The Average Of the Incident Fieldmentioning
confidence: 82%
“…The distance b 12 appears in (11) and is sometimes called the correlation length. Our analysis shows that when (35) is true, the transmitted field ( 31) is a sum of effective waves, and the incident wave is no more.…”
Section: Deducing the Average Transmitted Wavementioning
confidence: 89%
“…In papers such as [24] that calculate the average field from first principals, it is not clear that w inc = 0. Here we remove any doubt by proving that when sufficiently inside the material, given by condition (35), we have that w inc := 0 for any incident field, any material region R, any frequency, and all types of particles. Using the results from section 4.1, we collect the terms in equation ( 36) that satisfy the background wave equation to obtain:…”
Section: The Average Of the Incident Fieldmentioning
confidence: 98%
“…As in this case each frequency has only one mode: the plane-wave. An alternate approach to validate the theory of effective waves is to do Monte-Carlo simulations of particles within a sphere [35], or circular particles within a circle [36]. These have the added benefit of requiring a finite computational domain, though the transmitted fields are more complex.…”
Section: A Plate Filled With Particlesmentioning
confidence: 99%
“…Using equations (B.13) and (34) in the integral (B.12), and swapping the order of integration leads to: where we used that B(r; a) is completely contained in R 1 for every r 2 due to (35). There are values for r 1 for which the integral in equation (B.15) is zero.…”
Section: B3 the Transmitted Scattered Fieldmentioning
Microwave remote sensing is significantly altered when passing through clouds or dense ice. This phenomenon isn't unique to microwaves; for instance, ultrasound is also disrupted when traversing through heterogeneous tissues. Understanding the average transmission in particle-filled environments is central to improve data extraction or even to create materials that can selectively block or absorb certain wave frequencies. Most methods that calculate the average transmitted field assume that it satisfies a wave equation with a complex effective wavenumber. However, recent theoretical work has predicted more than one effective wave propagating even in a material which is statistically isotropic and for scalar waves. In this work we provide the first clear evidence of these predicted multiple effective waves by using high-fidelity Monte-Carlo simulations that do not make any statistical assumptions. To achieve this, it was necessary to fill in a missing link in the theory for particulate materials: we prove that the incident wave does not propagate within the material, which is usually taken as an assumption called the Ewald-Oseen extinction theorem. By proving this we conclude that the extinction length - the distance it takes for the incident wave to be extinct - is equal to the correlation length between the particles.
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