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<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>12</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/npg-12-101-2005</doi>
	<article_url>http://www.nonlin-processes-geophys.net/12/101/2005/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/12/101/2005/npg-12-101-2005.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/12/101/2005/npg-12-101-2005.pdf</fulltext_pdf>
	<start_page>101</start_page>
	<end_page>115</end_page>
	<publication_date>2005-01-27</publication_date>
	<article_title content_type="html">Quasiadiabatic description of nonlinear particle dynamics in typical magnetotail configurations</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>D. L. Vainchtein</name>
		</author>
		<author numeration="2" affiliations="3">
			<name>J. Büchner</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>A. I. Neishtadt</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>L. M. Zelenyi</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Space Research Institute, ul.Profsouznaya, 84/32, Moscow, Russia, GSP-7, 117997</affiliation>
		<affiliation numeration="2" content_type="html">Department of Mechanical &amp; Environmental Engineering, University of California, Santa Barbara, CA 93106, USA</affiliation>
		<affiliation numeration="3" content_type="html">Max Planck Institut für Aeronomie, Max-Planck-Str. 2, D-37191 Katlenburg-Lindau, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">In the present paper we discuss the motion of charged particles in three different regions of the
Earth magnetotail: in the region with magnetic field reversal and in the vicinities of neutral line
of &lt;i&gt;X&lt;/i&gt;- and &lt;i&gt;O&lt;/i&gt;-types. The presence of small parameters (ratio of characteristic length scales in
and perpendicular to the equatorial plane and the smallness of the electric field) allows us to
introduce a hierarchy of motions and use methods of perturbation theory. We propose a parameter
that plays the role of a measure of mixing in the system.</abstract>
	<references>
	</references>
</article>

