454 IEEE GEOSCIENCE AND REMOTE SENSING LETTERS, VOL. 14, NO. 3, MARCH 2017
A Simple and Effective Inverse Source
Reconstruction With Minimum A
Priori Information on the Source
Adriana Brancaccio, Member, IEEE, and Marco Donald Migliore, Member, IEEE
Abstract— A simple and effective two-step method to detect
and localize scattering objects from the measurements of the total
electric field, collected at a single frequency on a planar domain,
is presented. The first step consists in solving a linear inverse
source problem, looking for surface equivalent currents on a
plane located between the measurement surface and the objects
themselves. Thus, the equivalent currents associated with both the
scatterer presence and the background contribution are obtained.
In the second step, the support of the equivalent currents
associated with the objects is separated from the background by
exploiting the low-rank property of the background field. The
proposed method does not require information on the source,
except for its frequency, and it is easily implementable and entails
a low computational burden. Experimental results validate the
method.
Index Terms— Electromagnetic scattering inverse problems,
microwave imaging, sparse matrices.
I. I NTRODUCTION
T
HE aim of this letter is to introduce a simple and effective
two-step method to detect and localize objects from the
measurements of the electric field, collected on a planar
surface placed at some distances from them, in the presence
of an external source providing the incident field. As is
well known, one of the main difficulties in inverse scattering
problems is to evaluate the “scattered” field, that is defined as
the difference between the total field (quantity that is actually
measured in practice) and the field in the absence of the
scattering objects, that is the so-called “background” field [1].
The latter can be measured easily in laboratory conditions by
removing the scatterers, but not in the case of realistic in situ
measurement configurations [2]. In principle, the incident field
can be simulated numerically. However, this would require
detailed information about the illuminating source and the
background geometry and parameters (for instance, terrain
permittivity in the case of buried scatterers).
The proposed method overcomes this problem by a two-
step procedure. In the first step, the total measured field is
related to the field radiated by equivalent surface currents
Manuscript received July 26, 2016; revised September 23, 2016,
November 13, 2016, and December 15, 2016; accepted December 24, 2016.
Date of publication January 24, 2017; date of current version February 23,
2017. This work was supported by the European Union’s Seventh Framework
Program for research, technological development, and demonstration under
Grant 284996.
A. Brancaccio is with DIII, Second University of Napoli, 81031 Aversa,
Italy (e-mail: adriana.brancaccio@unina2.it).
M. D. Migliore is with DIEI, University of Cassino and Southern Lazio,
03043 Cassino, Italy (e-mail: mdmiglio@unicas.it).
Color versions of one or more of the figures in this letter are available
online at http://ieeexplore.ieee.org.
Digital Object Identifier 10.1109/LGRS.2017.2649938
located on an “investigation” plane close to the scatterers.
The support of such equivalent currents is assumed as the
unknown of the inverse problem. It is useful to note that the
reconstruction of the equivalent currents has been discussed
in a previous paper [3], but with reference to far-field mea-
surements. Its extension to near-field data was presented at
a conference [4] with reference to scattered field data. Its
application to total field data is discussed for the first time
in this letter.
Usually, direct and inverse electromagnetic problems
approaches using equivalent currents refer to volumetric cur-
rents in the case of dielectric objects [5] and to surface
currents in the case of metallic objects [6]–[8]. In both the
cases, the current in the volume or on the surface of the
object is considered. Our approach is significantly different.
We consider 2-D equivalent currents for any kind of object
(dielectric or metallic and 3-D). Furthermore, the equivalent
current is evaluated on a surface that is different from the
object surface. These characteristics allow to greatly reduce
the computational burden of the algorithm.
The aim of the second step is to distinguish the equiva-
lent currents associated with the scattering objects from the
ones related to the background contribution. To this end, the
algorithm exploits the low-rank properties of the background
field and the sparse properties of the field scattered by the
objects [9]. The latter property holds for localized small
scatterers. This procedure was briefly discussed in [10] and
included among the examples of applications of the minimum
trace norm regularization technique, but it was never experi-
mentally tested earlier.
In brief, the proposed algorithm requires a linear inversion
for the first step, while the second step can be performed using
efficient convex minimization programs [11]. Thus, from a
numerical point of view, the method proves to be both fast and
easy to program into MATLAB, and it is easy to implement in
that it does not require information on the source. In addition,
the sparse representation of the scattered field characteristic
makes it applicable to fields such as demining, as shown
in [10].
II. SCATTERING MODEL
We assume that objects (either metallic or dielectric) are at
some distances from the measurement plane and illuminated
by an external source. The tangent component of the field is
measured over a finite domain of the measurement plane.
In the following, we suppose that the objects stand in
free space, according to the experimental configuration used
in Sections IV and V. Consequently, the background field
is the incident field radiated by the source. However, the
proposed approach also works in the case of objects buried
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