Research Article | Open Access
Nicolas Pinel, Cédric Le Bastard, Christophe Bourlier, Meng Sun, "Asymptotic Modeling of Coherent Scattering from Random Rough Layers: Application to Road Survey by GPR at Nadir", International Journal of Antennas and Propagation, vol. 2012, Article ID 874840, 9 pages, 2012. https://doi.org/10.1155/2012/874840
Asymptotic Modeling of Coherent Scattering from Random Rough Layers: Application to Road Survey by GPR at Nadir
This paper studies the coherent scattering from random rough layers made up of two uncorrelated random rough surfaces, by considering 2D problems. The results from a rigorous electromagnetic method called PILE (propagation-inside-layer expansion) are used as a reference. Also, two asymptotic analytical approaches are presented and compared to the numerical model for comparison. The cases of surfaces with both Gaussian and exponential correlations are studied. This approach is applied to road survey by GPR at nadir.
Scattering by random rough surfaces has been the subject of active research from 1960s, in various domains of physics like optics, remote sensing of natural surfaces (sea surfaces, soils, etc.), and so on. Then, this general field of research begins to be rather well known, so that research is now more focused on specific domains like scattering from sea surfaces at high winds (which includes modeling of whitecaps, breaking waves, etc.) or low-grazing angles propagation. Also, the study is generalized to the remote sensing of complex media, for instance by taking volume scattering into account when inhomogeneous media are considered or by dealing with multilayered media.
This paper focuses on the scattering from layered media made up of one or several random rough surfaces and more specifically on the coherent scattering. This can be useful for various applications: in studying indoor propagation at 60 GHz, by taking the roughness of the rendering of office walls into account [1–3], in optics to determine optical constants of films  and other applications [5–9], to calculate the grazing incidence forward (i.e., in the specular direction) radar propagation over sea surfaces [10, 11], and so on.
Here, the study is applied to ground penetrating radar (GPR) for nondestructive pavement survey [12, 13] by taking the roughness of the surfaces into account . Two asymptotic approaches are extended to rough layered media: the scalar Kirchhoff-tangent plane approximation (SKA) and the second-order small perturbation method (SPM2), for calculating the coherent scattering contribution. A numerical rigorous method, named PILE (propagation-inside-layer expansion) method , is used as a reference to validate these two asymptotic models. The study focuses on 2D problems with the so-called 1D surfaces, for computational ease of the reference numerical method. This approach is applied to rough layers with two slightly rough surfaces (usually called “two-layer media”) characterized by either Gaussian or exponential correlation functions. The height probability density function (PDF) is assumed to be Gaussian.
This paper is organized as follows. Section 2 presents the extension of both the SKA and the SPM2 to calculate the coherent fields scattered from random rough layers. Then, Section 3 presents the numerical results for different scenarios and focuses on the application of road survey by GPR at nadir (i.e., normal incidence).
2. Random Rough Layer Coherent Scattering: Asymptotic Modeling
The problem considers a 1D random rough layer made up of two random rough surfaces separating homogeneous media and (2D problem). An incident plane wave impinges inside upon the upper rough surface (see Figure 1). Owing to the two surfaces, multiple scattered fields back into occur: not only the field scattered by the upper rough surface , but also higher order fields resulting from the multiple reflections inside : , , and so on.
2.1. Coherent Scattering of Slightly Rough Layers: Extension of the Ament Model
To study the influence of surface roughness on the coherent scattered fields, the Rayleigh roughness parameter Ra, which is well known for the case of reflection from single rough interfaces , is used. Considering the reflection onto the upper interface , it is usually given by the relation [16, 17] with being the refractive index of the incidence medium , the RMS height of the upper surface , and the incidence angle relatively to zenith. Equation (1) corresponds to the Rayleigh roughness parameter associated to the scattered field (see Figure 1). Then, the coherent scattering is given by the ratio of the amplitude of the mean scattered field with the amplitude of the incident field as with being the Fresnel reflection coefficient at the upper surface, the statistical average operator, and the random rough surface heights variations; the term assumes time convention. Then, the coherent field attenuation due to the surface roughness is given by with being the scattered field amplitude for the equivalent perfectly flat surface, which is given by . It must be noted that this holds for either 2D or 3D problems. For Gaussian statistics (i.e., for a Gaussian height PDF), the above equation simplifies as
Recent work [17, 18] made it possible to extend the Rayleigh roughness parameter Ra to the case of reflection from a rough layer made up of two rough surfaces. For a Gaussian process (i.e., for rough surfaces with Gaussian height PDF) and a Gaussian autocorrelation function, a satisfactory agreement was found in [17, 19] between the extended Rayleigh roughness parameters and exact numerical results. Hereafter, the results of this approach are analyzed more thoroughly by studying its frequency behaviour and an extension to the case of surfaces with exponential correlation is tested.
For uncorrelated rough surfaces, the extended Rayleigh roughness parameter associated to the second-order scattered field is given for lossless media and by [17, 19] with where is the refractive index of , is the RMS height of the lower surface , and is the propagation angle inside the inner medium .
Then, for Gaussian statistics, the so-called coherent field attenuation associated to is given by
This derivation can be extended to any order of reflection from a two-layer medium . As a consequence, for Gaussian statistics, the coherent field attenuation associated to the th order scattered field is given by where with This model is then an extension of the so-called Ament model to random rough layers, and which corresponds to using the scalar Kirchhoff-tangent plane approximation (SKA). It is recalled that the above equations are valid for both 2D and 3D problems.
2.2. Coherent Scattering under an Extended SPM2 Model
It is well known that under the SPM2 (second-order small perturbation method) model, the amplitude attenuation of the coherent scattered field is given for 2D problems and for Gaussian statistics by the relation  Comparing the classical SPM2 model with the Ament model (SKA model) for a single rough surface , it can be easily seen that the SPM2 model for describing the coherent field attenuation can be written in terms of the Rayleigh roughness parameter as By comparing (12) with (4), in vacuum (), it can be noted that the SPM2 and SKA models become equivalent when the Rayleigh roughness parameter , which occurs for all if the surface RMS height , with the EM wavelength in vacuum. It also occurs, for instance, for rougher surfaces, as soon as is large enough (). Besides, let us note that the criterion corresponds to the validity domain of the SPM2 model; thus, when the SPM model begins to be invalid, the SKA model is expected to depart from the SPM2 model. Hopefully, we expect the SKA model to be still valid in this region.
Then, at least in the domain where the Ament model (or SKA model) and the SPM2 model are both valid, the SPM2 model for describing the amplitude attenuation of the coherent scattered fields of rough two-layer media can be written as Then, the remark for a single rough interface for comparing the SPM2 and SKA models can be extended to the two-layer case: the SPM2 and SKA models become equivalent when the Rayleigh roughness parameter .
In what follows, both asymptotic extended models are compared to a numerical reference method to study their validity domain.
3. Numerical Validation
In order to compute the fields scattered from the rough layer, a numerical method, based on the method of moments (MoM), is used as a reference to validate the above two asymptotic methods for 2D problems. This method, called PILE (propagation-inside-layer expansion) method , is a rigorous numerical method that can be speeded up by the acceleration methods [21, 22]. In this study, the PILE method is accelerated by the Forward-Backward method (FB)  together with the Spectral Acceleration (FB-SA) [24–26] and denoted by PILE + FB-SA .
Contrary to other MoM-based reference numerical methods which generally can calculate only the total scattered field from rough layers , the PILE method is able to rigorously compute each scattered field contribution (, , and so on, see Figure 1).
3.1. Application to Pavement Survey by GPR at Nadir
The simulation parameters are chosen to match to the conventional GPR configuration used for pavement survey at traffic speed (e.g., ), that is, air-coupled radar configuration at vertical incidence (nadir, ). It is assumed that the scope of probing is limited to the first two layers of the pavement structure, which corresponds to the two rough surfaces represented in Figure 1.
The studied pavement structure is made up of a layer medium of ultra-thin asphalt surfacing (UTAS) of mean thickness mm , overlying a rolling band of same general composition (see Figure 1 with ). The two asymptotic methods are compared with the numerical model in a much wider frequency band than in  (here, GHz), in order to study the frequency limits of the two asymptotic methods. Also, the influence of the correlation length of the surfaces on the validity of the models is studied. The UTAS and the rolling band are assumed to be equivalent to homogeneous media at normal incidence and at the frequency band under study [13, 29, 30]. Their relative permittivities typically range between 4 and 8 [29, 31], and their conductivities between and S/m . For the simulations, we take and , respectively, and S/m and S/m, respectively. Then, by considering nondispersive media, the complex relative permittivity can be calculated as  with F/m the permittivity inside the vacuum. For instance, for GHz, the complex relative permittivities are and . The two rough interfaces and are assumed to have a Gaussian height PDF. About the height autocorrelation function, some studies showed that it is closer to an exponential function than a Gaussian one [33, 34]. Then, it is interesting to look at the influence of the choice of correlation on the accuracy of the asymptotic models. In particular, as the so-called Ament model is based on the scalar Kirchhoff-tangent plane approximation (SKA) which is valid for locally flat surfaces, its performances should degrade for changing from Gaussian correlation to exponential correlation. By contrast, the SPM2 model can deal with nonlocally flat surfaces but is limited to slightly rough surfaces; for random rough layers, this corresponds to the following generalized criterion:
For the upper surface , the root mean square (RMS) height is of the order of 0.6–1 mm, and the correlation length of the order of 5–10 mm [33, 34]. For the lower surface , the RMS height and the correlation length are a bit greater. For the first scenario to be studied here, chosen simulation parameters are mm, mm, mm, and mm. The two rough surfaces are assumed to be uncorrelated .
The antenna is assumed to radiate a vertically polarized plane wave in the far field of probed pavement like in : the antenna is about 400 mm above the sand surface, for which the far-field condition has been checked from data. The antenna is thus located beyond the Fraunhofer distance with respect to the probed pavement.
The typical width of probed surface antenna footprint is of the order of 300–500 mm [35, 36]. Then, for the simulations, surfaces of length mm are considered, illuminated by a Thorsos beam of attenuation parameter  (the Thorsos beam is a tapered plane wave, whose tapering has a Gaussian shape; the tapering is used to reduce the incident field to near zero at the ends of the surface realizations and thereby to reduce the edge effects to negligible levels). The two rough interfaces are sampled with a sampling step , with the wavelength inside . A normal () incident wave is taken, and the first two orders of the reflected fields by the rough layer and are calculated by the PILE method at the different frequencies over the GPR band, that is, GHz.
3.2. Numerical Results
In Figure 2, the frequency behavior of the amplitude attenuation of and in vertical (V) polarization is investigated for Gaussian correlation in the whole range of the band GHz, for which Monte-Carlo processes were used.
As expected, for both contributions, the influence of the roughness of the interfaces continuously increases with frequency, inducing a decrease of the scattered magnitude at nadir. This is confirmed by the Rayleigh roughness parameters and which increase as the frequency increases. The decrease in amplitude is stronger for than for , as predicted by Ra expressions. Moreover, for the first-order , a general very good agreement of both the SKA and SPM2 models can be found with the PILE reference method. In particular, a perfect match is found for the lower frequencies and for both asymptotic models. Slight differences between the SKA and the SPM2 occur with increasing frequencies, from approximately 8 GHz. For the second-order , a general excellent agreement of only the SKA model can be found with the PILE reference method. Indeed, the SPM2 model significantly deviates from the PILE method, starting from approximately 3.5–4 GHz. This can be attributed to the fact that is much higher than ; then, the general condition for the SPM2 to be valid occurs for lower frequencies. As a comparison, for GHz, , whereas . By using a least square method on the PILE results, a Gaussian fit is also applied as a test for comparison. This fitting process confirms that the PILE method for describing the attenuation of the coherent field amplitude can be approximated by a Gaussian attenuation with respect to the frequency; the agreement is particularly good for the second-order .
Figure 3 presents the numerical results for the same parameters as in Figure 2, but for surfaces with exponential correlation. The same general comments and conclusions as for Gaussian correlation can be made here. Indeed, the results of the PILE code do not change significantly from Gaussian to exponential correlation: there is only a slight decrease for the higher frequencies here. Then, both the SKA and SPM2 models show a good agreement for , and the SKA model shows a very good agreement for . Then, it is interesting to notice that the agreement is even better for the second-order contribution, which validates the proposed approach for random rough layers. These results lead us to the conclusion that for this typical configuration, the coherent scattering of random rough layers does not change significantly from Gaussian to exponential correlation, as predicted by the SKA and SPM2 models.
For studying the validity domain of extended SKA and SPM2 models, another set of simulations is led for a different configuration. We chose to reduce the correlation length of both surfaces and : we took mm and mm and kept other parameters constant (in particular, the surface RMS heights), in order to increase the surface slopes. Indeed, as the SPM2 model is valid for small surface slopes and the SKA model is valid for negligible slopes, increasing the RMS slopes should degrade the agreement. Then, as both the SKA and SPM2 models do not depend on the surface correlation length, their results do not change with the configuration.
Associated results for Gaussian correlation can be found in Figure 4. Let us note that for Gaussian surfaces, this modification implies changing the surfaces RMS slopes from and to and . Compared to Figure 2, it can be noted that the results of the PILE method slightly decrease for the first echo , and that this decrease gets stronger as the frequency increases. This decrease may be attributed to the increase of the surface slopes, which induces a broadening of the scattered field in regions away from the specular direction, which in consequence may decrease the coherent specular scattered field. Besides, despite the decrease of the PILE results, both SKA and SPM2 models show a general good agreement with the PILE method, and in particular for the lower frequencies. For the second echo , the PILE results do not change significantly: there is a slight decrease for the lower frequencies, but a slight increase for the higher frequencies. Then, the SKA model remains in a very good agreement with the PILE method.
The same analysis is made on surfaces with exponential correlation in Figure 5. Similar comments can be made here by comparing Figure 5 with Figure 2: for the first echo, the PILE code slightly decreases, and this decrease gets stronger as increases. Then, for exponential correlation here, the difference of both the SKA and SPM2 models with the PILE method begins to be rather significant for the higher frequencies, and in particular for tending to 10GHz. For the second echo, there is also a slight decrease of the PILE code for the lower frequencies. Thus, the SKA model remains in a (very) good agreement with the PILE method in the whole frequency range, even for the higher frequencies where the coherent attenuation is significant.
At last, 2 more sets of simulations for both Gaussian and exponential surfaces are studied: first, by increasing again the correlation lengths (mm and mm) in Figures 6 and 7 and second, by increasing the RMS heights (mm and mm) and correlation lengths kept constant (mm and mm) in Figures 8 and 9. First, by decreasing again the correlation lengths, as expected the agreement of both SKA and SPM models is poorer in general, and in particular for the first-order . The overestimation by both SKA and SPM models increases as the frequency increases (the SPM model gives slightly better agreements) and becomes significant for the higher frequencies. This is not surprising, as here the RMS slopes are significant: . Besides, the agreement is better for exponential correlation than for Gaussian correlation. For the second-order , for both correlations, slight differences occur in the range 1–4 GHz, owing to the increase of the RMS slopes ( here). However, the SKA model shows a general good agreement in the whole frequency range.
Second, this time (Figures 8 and 9) by increasing the RMS heights with correlation lengths kept constant (mm and mm) compared to Figures 4 and 5, the results are similar to the reference configuration (mm and mm). Here, this corresponds to RMS slopes and . The main observable differences occur in the second-order where the SKA model slightly overestimates the reference method for the lower frequencies, like in Figures 6 and 7. Nevertheless, here the agreement is better, and in particular for the first-order .
As a consequence, it can be concluded that the agreement is less sensitive to the RMS heights than the correlation lengths. The main difference is in the frequency validity domain of the SPM model: as predicted by theory, it decreases as the RMS heights increases (see in particular ). Thus, the SKA model is in a general (very) good agreement with the PILE method in the whole frequency range for both Gaussian and exponential correlations. Its main limitations are the small correlation lengths in the higher frequencies for the first-order scattered field .
This paper presented the extension of both the SKA and SPM2 models to coherent scattering from random rough layers, where the two random rough surfaces are uncorrelated. An application is then presented for dealing with the pavement survey by GPR at nadir, in a large frequency range (GHz), and for surfaces with both Gaussian and exponential correlations. The comparisons with a numerical reference method made it possible to validate both asymptotic models in their validity domains for 2D problems. For 3D problems, similar results and conclusions are expected, as the SKA model for describing the attenuation of the coherent scattering owing to the surface roughness is the same for 2D and 3D problems.
In particular, the SKA model was shown to correctly predict the coherent scattered field for typical configurations in pavement survey by GPR at nadir. By taking into account the time delay of each echoes in this new model, this direct simple EM model can be a good candidate for its use in signal processing algorithms for the estimation of physical parameters of the pavement like its thickness [13, 14] and also and more important, for the estimation of the RMS heights of the rough surfaces and simultaneously.
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