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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>1</volume_number>
		<volume_title>Kleinheubacher Berichte 2002</volume_title>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/ars-1-99-2003</doi>
	<article_url>http://www.adv-radio-sci.net/1/99/2003/</article_url>
	<abstract_html>http://www.adv-radio-sci.net/1/99/2003/ars-1-99-2003.html</abstract_html>
	<fulltext_pdf>http://www.adv-radio-sci.net/1/99/2003/ars-1-99-2003.pdf</fulltext_pdf>
	<start_page>99</start_page>
	<end_page>104</end_page>
	<publication_date>2003-05-05</publication_date>
	<article_title content_type="html">A hybrid method combining the FDTD and a time domain boundary-integral equation marching-on-in-time algorithm</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Becker</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>V. Hansen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Lehrstuhl für Theoretische Elektrotechnik der Universität Wuppertal, Rainer-Gruenter-Str. 21, 42119 Wuppertal, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">In this paper a hybrid method combining
the FDTD/FIT with a Time Domain Boundary-Integral
Marching-on-in-Time Algorithm (TD-BIM) is presented. Inhomogeneous
regions are modelled with the FIT-method, an
alternative formulation of the FDTD. Homogeneous regions
(which is in the presented numerical example the open space)
are modelled using a TD-BIM with equivalent electric and
magnetic currents flowing on the boundary between the inhomogeneous
and the homogeneous regions. The regions are
coupled by the tangential magnetic fields just outside the inhomogeneous
regions. These fields are calculated by making
use of a Mixed Potential Integral Formulation for the magnetic
field. The latter consists of equivalent electric and magnetic
currents on the boundary plane between the homogeneous
and the inhomogeneous region. The magnetic currents
result directly from the electric fields of the Yee lattice. Electric
currents in the same plane are calculated by making use
of the TD-BIM and using the electric field of the Yee lattice
as boundary condition. The presented hybrid method only
needs the interpolations inherent in FIT and no additional interpolation.
A numerical result is compared to a calculation
that models both regions with FDTD.</abstract>
	<references>
	</references>
</article>

