Abstract
We revisit the problem of recovering wave speeds and density across a curved interface from reflected wave amplitudes. Such amplitudes have been exploited for decades in (exploration) seismology in this context. However, the analysis in seismology has been based on linearization and mostly flat interfaces. Here, we present an analysis without linearization and allow curved interfaces, establish uniqueness and provide a reconstruction, while making the notion of amplitude precise through a procedure rooted in microlocal analysis.
Similar content being viewed by others
References
Bhattacharyya, S.: Local uniqueness of the density from partial boundary data for isotropic elastodynamics. Inverse Prob. 34(12), 125001–10 (2018). https://doi.org/10.1088/1361-6420/aade76
Caday, P., V. de Hoop, M., Katsnelson, V., Uhlmann, G.: Scattering control for the wave equation with unknown wave speed. Arch. Ration. Mech. Anal 231, 409–464 (2019) arXiv:1611.06994
Caday, P., de Hoop, M.V., Katsnelson, V., Uhlmann, G.: Recovery of discontinuous Lamé parameters from exterior Cauchy data. Commun. Partial Differ. Equ. 46(4), 680–715 (2021). https://doi.org/10.1080/03605302.2020.1857399
Červený, V., Langer, J., Pšenčík, I.: Computation of geometric spreading of seismic body waves in laterally inhomogeneous media with curved interfaces. Geophys. J. Int. 38(1), 9–19 (1974). https://doi.org/10.1111/j.1365-246X.1974.tb04105.x
Davydenko, M., Verschuur, D.: Joint imaging of angle-dependent reflectivity and estimation of the migration velocity model using multiple scattering. Geophysics 84, 1–37 (2019). https://doi.org/10.1190/geo2018-0637.1
de Hoop, M.V., Bleistein, N.: Generalized radon transform inversions for reflectivity in anisotropic elastic media. Inverse Prob. 13(3), 669–690 (1997). https://doi.org/10.1088/0266-5611/13/3/009
de Hoop, M.V., Nakamura, G., Zhai, J.: Unique recovery of piecewise analytic density and stiffness tensor from the elastic-wave dirichlet-to-neumann map. SIAM J. Appl. Math. 79(6), 2359–2384 (2019). https://doi.org/10.1137/18M1232802
Doúgan, G., Nochetto, R.H.: First variation of the general curvature-dependent surface energy. ESAIM: Mathematical Modelling and Numerical Analysis - Modélisation Mathématique et Analyse Numérique 46(1), 59–79 (2012). https://doi.org/10.1051/m2an/2011019
Eskin, G., Ralston, J.: On the inverse boundary value problem for linear isotropic elasticity. Inverse Prob. 18(3), 907–921 (2002). https://doi.org/10.1088/0266-5611/18/3/324
Hammad, H., Verschuur, D.: Slowness and reflection coefficient curves for laterally heterogeneous media 2019(1), 1–5 (2019). https://doi.org/10.3997/2214-4609.201901538
Hansen, S.: Solution of a hyperbolic inverse problem by linearization. Commun. Partial Differ. Equ. 16(2–3), 291–309 (1991). https://doi.org/10.1080/03605309108820760
Knott, C.G.: Reflexion and refraction of elastic waves, with seismological applications. Lond. Edinburgh Dublin Philos. Mag. J. Sci. 48(290), 64–97 (1899). https://doi.org/10.1080/14786449908621305
Kohn, R., Vogelius, M.: Determining conductivity by boundary measurements. Commun. Pure Appl. Math. 37(3), 289–298 (1984). https://doi.org/10.1002/cpa.3160370302
Montalto, C.: Stable determination of a simple metric, a covector field and a potential from the hyperbolic dirichlet-to-neumann map. Commun. Partial Differ. Equ. 39(1), 120–145 (2014). https://doi.org/10.1080/03605302.2013.843429
Nachman, A.I.: Global uniqueness for a two-dimensional inverse boundary value problem. Ann. Math. 143(1), 71–96 (1996)
Nakamura, G., Uhlmann, G.: Identification of lamé parameters by boundary measurements. Am. J. Math. 115(5), 1161–1187 (1993)
Nakamura, G., Uhlmann, G.: Global uniqueness for an inverse boundary problem arising in elasticity. Invent. Math. 118, 457–474 (1994). https://doi.org/10.1007/BF01231541DO
Nakamura, G., Uhlmann, G.: Erratum: Global uniqueness for an inverse boundary value problem arising in elasticity (inventiones mathematicae (1994) 118 (457–474)). Invent. Math. 152, 205–207 (2003). https://doi.org/10.1007/s00222-002-0276-1
Neves, F.A., de Hoop, M.V.: Some remarks on nonlinear amplitude versus scattering angle-azimuth inversion in anisotropic media. Geophysics 65(1), 158–166 (2000). https://doi.org/10.1190/1.1444706
Oksanen, L., Salo, M., Stefanov, P., Uhlmann, G.: Inverse problems for real principal type operators. 2001–07599 (2020) arXiv:2001.07599 [math.AP]
Rachele, L.V.: Boundary determination for an inverse problem in elastodynamics. Commun. Partial Differ. Equ. 25(11–12), 1951–1996 (2000)
Rachele, L.V.: Uniqueness in inverse problems for elastic media with residual stress. Commun. Partial Differ. Equ. 28(11–12), 1787–1806 (2003). https://doi.org/10.1081/PDE-120025485
Rachele, L.V.: Uniqueness of the density in an inverse problem for isotropic elastodynamics. Trans. Am. Math. Soc. 355(12), 4781–4806 (2003). https://doi.org/10.1090/S0002-9947-03-03268-9
Skopintseva, L., Aizenberg, A., Ayzenberg, M., Landro, M.: The effect of interface curvature on avo inversion of near-critical and postcritical pp-reflections. Geophysics (2012). https://doi.org/10.1190/GEO2011-0298.1
Stefanov, P., Uhlmann, G.: Thermoacoustic tomography arising in brain imaging. Inverse Prob. 27(4), 045004–26 (2011). https://doi.org/10.1088/0266-5611/27/4/045004
Stefanov, P., Yang, Y.: The inverse problem for the dirichlet-to-neumann map on lorentzian manifolds. Anal. PDE 11(6), 1381–1414 (2018). https://doi.org/10.2140/apde.2018.11.1381
Stefanov, P., Uhlmann, G., Vasy, A.: The transmission problem in linear isotropic elasticity. Pure Appl. Anal. 3(1), 109–161 (2021). https://doi.org/10.2140/paa.2021.3.109
Sylvester, J., Uhlmann, G.: A global uniqueness theorem for an inverse boundary value problem. Ann. Math. 125(1), 153–169 (1987)
Sylvester, J., Uhlmann, G.: Inverse boundary value problems at the boundary-continuous dependence. Commun. Pure Appl. Math. 41(2), 197–219 (1988). https://doi.org/10.1002/cpa.3160410205
Sylvester, J., Uhlmann, G.: Inverse problems in anisotropic media. Contemp. Math. 122, 105–117 (1991). https://doi.org/10.1090/conm/122/1135861
Taylor, M.E.: Reflection of singularities of solutions to systems of differential equations. Commun. Pure Appl. Math. 28(4), 457–478 (1975)
Yamamoto, K.: Elastic waves in two solids as propagation of singularities phenomenon. Nagoya Math. J. 116, 25–42 (1989)
Zhou, Y., E., Y., Zhu, L., Qi, M., Xu, X., Bai, J., Ren, Z., Wang, L.: Terahertz wave reflection impedance matching properties of graphene layers at oblique incidence. Carbon (2015). https://doi.org/10.1016/j.carbon.2015.10.063
Zoeppritz, K.: Über reflection und durchgang seismischer wellen durch unstetigkeitsflchen. Nachrichten con der Gesellschaft der Wissenschaften zu Gttingen, Mathematisch-Physikalische Klasse 1919, 66–84 (1919)
Acknowledgements
M.V.d.H. gratefully acknowledges support from the Simons Foundation under the MATH + X program, the National Science Foundation under Grant DMS-1815143, and the corporate members of the Geo-Mathematical Imaging Group at Rice University. G.U. was partly supported by NSF, a Walker Family Endowed Professorship at UW and a Si-Yuan Professorship at IAS, HKUST. S.B. was partly supported by Project No.: 16305018 of the Hong Kong Research Grant Council. The authors greatly appreciate the detailed suggestions made by two anonymous referees which improved this paper.
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
Funding
M.V.d.H. gratefully acknowledges support from the Simons Foundation under the MATH + X program, the National Science Foundation under Grant DMS-1815143, and the corporate members of the Geo-Mathematical Imaging Group at Rice University. G.U. was partly supported by NSF, a Walker Family Endowed Professorship at UW and a Si-Yuan Professorship at IAS, HKUST. S.B. was partly supported by Project No.: 16305018 of the Hong Kong Research Grant Council.
Conflict of interest
Financial interests: The authors declare they have no financial interests. Non-financial interests: The authors declare they have no non-financial interests.
Availability of data and material
Not applicable.
Code availability
Not applicable.
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
A Proofs of lemmas and propositions from Section 2
A Proofs of lemmas and propositions from Section 2
These are proofs of the main statements in the acoustic case. Since they are a simpler, yet more lucid version of the elastic case, we relegate them to this appendix.
1.1 A.1 Zeroth order recovery of the parameters at the interface
Proof of Lemma 2.1
By solving (2.4), we get
where we denote \(f = \xi _I/\xi _T, a = \mu ^{(-)}, b = \mu ^{(+)}.\) Note that \(f = f(|\xi ' |/\tau )\) i.e. it is a function of the parameter \(|\xi ' |/\tau \) while a, b only depend on x. Now, since \((a_R)_0 = ({\tilde{a}}_R)_0\) and assuming \(\mu ^{(-)} = {\tilde{\mu }}^{(-)}\) (i.e. \(a=\tilde{a}\)) on \(\Gamma \) we obtain
Varying \(|\xi ' |/\tau \) keeping everything else constant, we get
where \(f_1\) is f evaluated at different value of \(|\xi ' |/\tau \). Thus,
where we used \(c^{(-)}_S = {\tilde{c}}^{(-)}_S\) and labelled \(d = |\xi ' |/\tau \), \(d_1 = |\xi '_1 |/\tau _1\). Cross multiplying we get the algebraic equation
Note that, as long as we pick \(d_1 \ne \pm d\), we recover \(c_S^{(+)} = \tilde{c}_S^{(+)}\). Then going back to (A.1) one gets \(b=\tilde{b}\), that is \(\mu ^{(+)} = {{\tilde{\mu }}}^{(+)}\) on \(\Gamma \). \(\square \)
Remark A.1
In geophysical experiments, one often only has access to relative amplitudes where the amplitude is normalized to be 1 for an incident wave hitting the interface at a fixed particular angle. Concretely, for a fixed, \((x',\tau _1, \xi '_1)\) in the hyperbolic set, suppose one instead measures \(R:= (a_R)_0(x',\tau ,\xi ')/ (a_R)_0(x',\tau _1,\xi '_1)\). The questions is can one recover \(\mu ^{(+)}\) and \(c_S^{(+)}\) at \(x'\) from R at various incident angles (i.e. varying \(\tau , \xi '\) in the hyperbolic set)?
In order to recover a single unknown parameter such as \(\mu ^{(+)}\), then this can be done with elementary means, but disentangling two material parameters is less clear. For the uniqueness question, ignoring spacial variables, assume
Then one can show \(\mu ^{(+)} = {{\tilde{\mu }}}^{(+)}\) and \(c_S^{(+)} = {\tilde{c}}_S^{(+)}\) with a similar argument as above.
One can even obtain a partial reconstruction algorithm directly from R. Via computation, one can show that
where \(a,b,f,f_1\) are as in the lemma. By solving a quadratic equation, we compute
where \(\alpha = 2a(f-f_1), \beta = a^2ff_1\) are independent of b. Since b is independent of those variable, one can vary \(\tau , \xi '\) within the hyperbolic set to obtain a nonlinear equation that needs to be solved for \(c_S\) only (without any terms involving \(b= \mu ^{(+)}\)), but it is unclear whether this can be done by elementary means. If it can, then our approach shows how one can do the recovery even with reflected amplitudes, and there is a reconstruction formula.
1.2 A.2 Recovery of the derivatives of the parameters at the interface
Proof of Lemma 2.2
Observe that for \(J=0\), from (2.6) and (2.8) one obtains
In order to calculate the term \(P\phi _{\bullet } = (\rho \partial _t^2 - \nabla _x\cdot \mu \nabla _x)\phi _{\bullet }\), we start with
Therefore, \( \partial _{x_3} \phi _\bullet = \pm \sqrt{c^{-2}_{S}| \partial _{t}\phi _{\bullet } |^2 - | \partial _{x'}\phi _{\bullet } |^2}\) can be recovered from \(c_S\) and the tangential derivatives of \(\phi _{\bullet }\) on \(\Gamma \). In other words, \( \partial _{x_3} \phi _\bullet \) at \(\Gamma \) is a \(R_0\) term. Taking one more derivative of (A.3) in the normal direction we get
Here the last two terms above are determined by \(c_S\), \(\phi _{\bullet }\) and their tangential derivatives on \(\Gamma \). Hence, we have
If we take one more normal derivative of \(\phi _{\bullet }\), then \( \partial _{x_3}E_0\) can have at most one derivative of \(c_S\) as well as the term \(c_S^{-2}\xi _{3, \bullet }^{-1}| \partial _t \phi _\bullet |^2\). Thus, we obtain
In general, one obtains
Now we calculate
Also note that \( \partial ^2_t \phi _{\bullet } = \partial ^2_t\left( -\tau t + x'\cdot \xi '\right) = 0\) on \(\Gamma \). Thus, from a direct calculation, we obtain
Therefore, going back to (A.2) we get
so that
\(\square \)
Remark A.2
Observe that \( \partial _{x_3}(a_{I})_0\) and \( \partial _{x_3}(a_{R})_0\) are indeed \(R_0\) terms, because \(\rho ^{(-)}\) and \(c_{S}^{(-)}\) are known on the \(\Omega _{-}\) region and so are \( \partial _{x_3}\rho ^{(-)}\), \( \partial _{x_3}c_{S}^{(-)}\) on \(\Gamma \). The rest of the terms in the expression of \( \partial _{x_3}(a_{I})_0\) and \( \partial _{x_3}(a_{R})_0\) can be determined from the 0-th order transmission condition (2.4). On the other hand \( \partial _{x_3}(a_{T})_0\) is not \(R_0\) but \(R_1\) since it involves \(\rho ^{(+)}\) and \(c_{S}^{(+)}\), which cannot be determined from (2.4).
We provide the proofs of several claims made in the elastic case.
Proof of Lemma 2.3
We start with the transmission conditions for \((a_R)_{-1}\). From (2.5) for \(J=-1\), we get
Note that \(\mu ^{(+)}\) can be determined by the 0-th order transmission condition (see Lemma 2.1), therefore, \(\left( \mu ^{(-)}\xi _{3, I} + \mu ^{(+)}\xi _{3, T}\right) ^{-1}\) is a \(R_0\) quantity. Furthermore, thanks to Lemma 2.2, \(\mu ^{(-)} \partial _{x_3}(a_I)_0\) and \(\mu ^{(-)} \partial _{x_3}(a_R)_0\) are \(R_0\), see Remark A.2. From (A.5) and (2.9) one obtains
We denote \(f=f(|\xi ' |/\tau ) = \left( 1 - \frac{( \partial _t \phi _T)^2}{2(c_S^{(+)})^2 \xi ^2_{3,T}}\right) \). If we have \({\tilde{\rho }}^{(-)} = \rho ^{(-)}\), \({\tilde{\mu }}^{(-)} = \mu ^{(-)}\) on \(\Omega _{-}\) and \(\tilde{R} = R\) on \(\Gamma \), then one gets \(\tilde{R}_0 = R_0\) and \((\tilde{a}_R)_{-1} = (a_R)_{-1}\) on \(\Gamma \). Therefore, we obtain
Note that \((a_T)_0 \ne 0\) on the hyperbolic set when solving (2.4), which implies
Observe that f is a \(R_0\) quantity so that \(f=\tilde{f}\). Furthermore, \(\rho ^{(+)}\), \({\tilde{\rho }}^{(+)}\) depends only on x, hence by varying \((|\xi ' |/\tau )\) we obtain
where f and \(f_1\) are evaluated in different values of \(|\xi ' |/\tau \). Note that \(c_S^{(+)} = \tilde{c}_S^{(+)}\) on \(\Gamma \) (see Lemma 2.1). If we take two values of \(|\xi ' |/\tau \) such a way that \(f \ne f_1\) on \(\Gamma \), then (A.7) implies
Going back to (A.6) we obtain \( \partial _{x_3}\rho ^{(+)} = \partial _{x_3}{\tilde{\rho }}^{(+)}\) and thus \( \partial _{x_3}\mu ^{(+)} = \partial _{x_3}{\tilde{\mu }}^{(+)}\) on \(\Gamma \). \(\square \)
Proof of Lemma 2.4
We prove this lemma via an iterative argument. First we note that for \(J=0,-1\) we already have Lemma 2.1 and Lemma 2.3.
In order to prove the lemma for \(J<-1\) we study the transport equation (2.6). For \(J<0\), in the transport equations (2.6), we encounter the term \(P(t,x,D_{t,x})(a_\bullet )_J = \rho \partial _t^2(a_\bullet )_J - \nabla \cdot \mu \nabla (a_\bullet )_J\). We calculate
Using the equation earlier for \( \partial _{x_3}(a_\bullet )_0\), we see the second term is in fact \(R_1\). Thus, we obtain
Now, from the transport equation (2.6) and the relation (2.7) ,(A.8) we get
Since the microlocal transmission conditions (2.5) helps us to connect \((a_R)_{-2}\) to \( \partial _{x_3}(a_T)_{-1}\), using the same argument as in Lemma 2.3 we see that \((a_R)_{-2}\) uniquely determines \( \partial ^2_{x_3} \rho ^{(+)}\) and \( \partial ^2_{x_3} \mu ^{(+)}\) at \(\Gamma \). Iterating the above argument gives us
Then we get from the \(|J |\)-th order transmission conditions
so that
Using the same argument as above, and noting that the transmission conditions already determine \((a_T)_{J+1}\) from knowledge of \((a_R)_{J+1}\), shows that \((a_R)_J\) determines \( \partial ^{|J |}_{x_3} \rho ^{(+)}\) and \( \partial ^{|J |}_{x_3} \mu ^{(+)}\) at \(\Gamma \). \(\square \)
This completes the proof of Theorem 1.1. The essential piece to make this work is verifying that \((a_R)_J\) at \(\Gamma \) only depends on at most \(|J |\) normal derivatives of the material parameters using the transmission conditions to continue unique recovery inductively. We finish this section by the following remark.
Remark A.3
Note that the recovery of the parameters on the boundary is obtained directly from the principal symbol of the reflection operator R, whereas recovering the higher order derivatives one relies on the recursive equations obtained from the interface conditions for the lower order terms of the asymptotic expansion of the geometric optics solution.
1.3 A.3 Proofs of several lemmas in the elastic case
Lastly in this appendix, we provide the remaining proof of lemma 3.1, which is similar to our previous computations and the
Remaining proof of lemma 3.1
Having \(r_{11} = \tilde{r}_{11}\) we obtain
Here we use that fact that so far we have \(\rho ^{(\pm )} = {\tilde{\rho }}^{(\pm )}\), \(\mu ^{(\pm )} = {\tilde{\mu }}^{(\pm )}\), \(c_S^{(\pm )} = \tilde{c_S}^{(\pm )}\) on \(\Gamma \) and therefore, \(\xi _{3,\bullet ,S} = {\tilde{\xi }}_{3,\bullet ,S}\). Equating the coefficient of \({\hat{\tau }}^8\) on the both sides of the above equation we obtain
After a cross multiplication and simplification, on \(\Gamma \) we obtain
Since \(c_P^{(+)}\) and \(\tilde{c}_P^{(+)}\) are wave speeds and cannot be negative, hence, we obtain \(c_P^{(+)} = \tilde{c}_P^{(+)}\) on \(\Gamma \). \(\square \)
We also finish the proof of proposition 4.5 in the elastic case.
proof of proposition 4.5 in the elastic case:
First, we need the following operator appearing in the elastic transport equations (see (Rachele 2000, equation (25)))
The divergence term is computed exactly as in the acoustic case with the mean curvature appearing, which is still an \(R_0\) term.
Next, we let \(\nabla \) be the Levi-Civita connection and \(e_\alpha = \partial _{{\tilde{x}}_\alpha }\) a basis for \(T\Omega \) near \(\Gamma \) for \(\alpha = 1, 2, 3\), and dual basis \(\{{\hat{e}}_\alpha \}\). Note that \( \partial _{{\tilde{x}}_3} = \partial _\nu \) when restricted to \(\Gamma \) by fixing a unit normal \(\nu \) with the correspending sign. Then \(\nabla _x \phi = \partial _{{\tilde{x}}_\alpha }\phi \ e_\alpha \) with the usual summation convention and
where in particular, the last term is the only new term we have from the flat case and it is an \(R_0\) term. An analogous calculation applies to \(( \nabla _x \otimes \mu \nabla _x \phi )^t\). Let \(N = \nabla \phi _P/|\nabla \phi _P |\) and observe that
Since \(\Gamma ^3_{3 j} = 0\) in our coordinates, if we pick \(\xi _{tan} = 0\) (normal incidence wave), then the quantity above vanishes at \(\Gamma \). Thus,
where for \(\xi _{tan} = 0\), \(R_0\) contains no curvature terms when restricted to \(\Gamma \).
Following (Rachele 2000, equation (34)), we also need to compute the term
restricted to \(\Gamma \) where p is the principal symbol of Q. We will also choose \(\xi _{tan} = 0\) initially. Observe that \( \partial _{\tilde{\xi }_1} ( {\tilde{\xi }}\otimes {\tilde{\xi }}) = {\tilde{\xi }}\otimes e_1 + e_1 \otimes {\tilde{\xi }}\) so that when restricted to \( {\tilde{\xi }}= d\phi _P\), at \(\Gamma \), for \(\xi _{tan} =0 \) (we assume all statements in this subsection are with this restriction)
Using that \(\langle \nu , \nabla _\nu \nu \rangle = 0\), we get
where H(x) is from before and proportional to the mean curvature at \(\Gamma \). Similarly,
One may also check that the quantity \(N^t ( \partial _{ {\tilde{\xi }}} | {\tilde{\xi }} |^2 I) \cdot \partial _{ \tilde{x}}N\) has no curvature terms when we restrict to \(\Gamma \) and \(\xi _{tan} = 0\). Then from (Rachele 2000, equation (50)), we get
where \(R_0\) also does not contain any curvature terms and can be compute from the values of the parameters and not their normal derivative. Combining these calculations, we obtain from (Rachele 2000, lemma 3.5)
where \(R_0\) does not depend on curvature when restricted to \(\Gamma \) and \(\xi _{tan} = 0\), and \(b_\bullet \) is a fixed constant whose sign is dependent on \(\bullet .\) One may derive an analogous formula for \( \partial _\nu (\alpha _{k,\bullet })_0\) for \(k=1,2\) using (Rachele 2000, lemma 3.5) as well. To recover the mean curvature as in the acoustic case, we use the transmission conditions (3.13) for the lower order symbols and this produces an additional term:
where we denoted by D the matrix appearing in (3.13) which does not depend on curvature. The right hand side of the above equation will contain curvature terms in the form of \( \partial _{ \tilde{x}_i}N_{\bullet }\) and \( \partial _{ \tilde{x}_i}N_{\bullet ,k}\). However, when \(\xi _{tan} = 0\) and restricted to \(\Gamma \), the inner product of these vectors with \(N_\bullet \) will not have curvature terms since \(\Gamma ^3_{3l} = 0\). Thus, by setting \(J = -1\) and taking the inner product of the equation for \((\mathcal {A}_R)_{-1}\) in (A.17) with \(N_R\), then we can recover the mean curvature from \((\mathcal {A}_R)_{-1}\) as in the acoustic case by using (A.16). After a long computation similar to the one above, we may then recover \( \partial _\nu H(x)\) at the boundary from \((\mathcal {A}_R)_{-2}\) as in the acoustic case and invoke lemma 4.3, keeping in mind that H(x) and \(\kappa \) are proportional. \(\square \)
Rights and permissions
About this article
Cite this article
Bhattacharyya, S., de Hoop, M.V., Katsnelson, V. et al. Recovery of wave speeds and density of mass across a heterogeneous smooth interface from acoustic and elastic wave reflection operators. Int J Geomath 13, 9 (2022). https://doi.org/10.1007/s13137-022-00199-1
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s13137-022-00199-1