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<article language="en">
	<journal>
		<journal_title>Advances in Radio Science</journal_title>
		<journal_url>www.adv-radio-sci.net</journal_url>
		<issn>1684-9965</issn>
		<eissn>1684-9973</eissn>
		<volume_number>3</volume_number>
		<volume_title>Kleinheubacher Berichte 2004</volume_title>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/ars-3-219-2005</doi>
	<article_url>http://www.adv-radio-sci.net/3/219/2005/</article_url>
	<abstract_html>http://www.adv-radio-sci.net/3/219/2005/ars-3-219-2005.html</abstract_html>
	<fulltext_pdf>http://www.adv-radio-sci.net/3/219/2005/ars-3-219-2005.pdf</fulltext_pdf>
	<start_page>219</start_page>
	<end_page>225</end_page>
	<publication_date>2005-05-12</publication_date>
	<article_title content_type="html">Time-Domain Techniques for Computation and Reconstruction of One-Dimensional Profiles</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Rahman</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. Marklein</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Fachgebiet Theoretische Elektrotechnik, Fachbereich Elektrotechnik/Informatik, Universit&amp;#x00E4;t Kassel (UNIK), 34109 Kassel, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">This paper presents a time-domain technique to compute the electromagnetic fields and to
reconstruct the permittivity profile within a one-dimensional medium of finite length.
The medium is characterized by a permittivity as well as conductivity profile which vary
only with depth. The discussed scattering problem is thus one-dimensional. The modeling
tool is divided into two different schemes which are named as the forward solver and
the inverse solver.
The task of the forward solver is to compute the internal fields of the specimen which
is performed by Green’s function approach. When a known electromagnetic wave is incident
normally on the media, the resulting electromagnetic field within the media can be calculated
by constructing a Green’s operator. This operator maps the incident field on either side
of the medium to the field at an arbitrary observation point. It is nothing but a matrix of
integral operators with kernels satisfying known partial differential equations. The
reflection and transmission behavior of the medium is also determined from the boundary
values of the Green&apos;s operator.
The inverse solver is responsible for solving an inverse scattering problem by reconstructing
the permittivity profile of the medium. Though it is possible to use several algorithms to solve this
problem, the invariant embedding method, also known as the layer-stripping method, has been
implemented here due to the advantage that it requires a finite time trace of reflection data.
Here only one round trip of reflection data is used, where one round trip is defined by the time required by the pulse to
propagate through the medium and back again. The inversion process
begins by retrieving the reflection kernel from the reflected wave
data by simply using a deconvolution technique. The rest of the task
can easily be performed by applying a numerical approach to
determine different profile parameters.
Both the solvers have been found to have the ability to deal with different types of slabs and
incident electromagnetic pulses. Slabs having continuous and discontinuous relative permittivity
have already been tested successfully. The tested electromagnetic pulses are a Dirac, Gaussian and
sinusoidal pulse. Due to sampling, the resolution of the system also plays a significant role in
obtaining better outputs from this scheme.</abstract>
	<references>
	</references>
</article>

