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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ANGEO</journal-id>
<journal-title-group>
<journal-title>Annales Geophysicae</journal-title>
<abbrev-journal-title abbrev-type="publisher">ANGEO</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1432-0576</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/angeo-20-1509-2002</article-id>
<title-group>
<article-title>Solar wind heating by an embedded quasi-isothermal pick-up ion fluid</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fahr</surname>
<given-names>H. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institut für Astrophysik und Extraterrestrische Forschung der Universität Bonn Auf dem Hügel 71, D-53121 Bonn, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Correspondence to: H. J. Fahr (hfahr@astro.uni-bonn.de)</addr-line>
</aff>
<pub-date pub-type="epub">
<day>30</day>
<month>11</month>
<year>1999</year>
</pub-date>
<volume>20</volume>
<issue>10</issue>
<fpage>1509</fpage>
<lpage>1518</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
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<self-uri xlink:href="http://www.ann-geophys.net/20/1509/2002/angeo-20-1509-2002.pdf">The full text article is available as a PDF file from http://www.ann-geophys.net/20/1509/2002/angeo-20-1509-2002.pdf</self-uri>
<abstract>
<p>It is well known that the solar wind plasma
 consists of primary ions of solar coronal origin and secondary ions of
 interstellar origin. Interstellar H-atoms penetrate into the inner heliosphere
 and when ionized there are converted into secondary ions. These are implanted
 into the magnetized solar wind flow and are essentially enforced to co-move
 with this flow. By nonlinear interactions with wind-entrained Alfvén waves the
 latter are processed in the co-moving velocity space. This pick-up process,
 however, also causes actions back upon the original solar wind flow, leading to
 a deceleration, as well as a heating of the solar wind plasma. The resulting
 deceleration is not only due to the loading effect, but also due to the action
 of the pressure gradient. To calculate the latter, it is important to take into
 account the stochastic acceleration that suffers at their convection out of the
 inner heliosphere by the quasi-linear interactions with MHD turbulences. Only
 then can the presently reported VOYAGER observations of solar wind
 decelerations and heatings in the outer heliosphere be understood in terms of
 the current, most likely values of interstellar gas parameters. In a consistent
 view of the thermodynamics of the solar wind plasma, which is composed of
 secondary ions and solar wind protons, we also derive that the latter are
 globally heated at their motion to larger solar distances. The arising heat
 transfer is due to the action of suprathermal ions which drive MHD waves that
 are partially absorbed by solar wind protons and thereby establish their
 observed quasi-polytropy. We obtain a quantitative expression for the solar
 wind proton pressure as a function of solar distance. This expression clearly
 shows the change from an adiabatic to a quasi-polytropic behaviour with a
 decreasing polytropic index at increasing distances, as has been observed by
 the VOYAGERS. This also allows one to calculate the average percentage of the
 intitial energy fed into the thermal proton energy. In a first-order evaluation
 of this expression we can estimate that under stationary flow conditions about
 10% of the initial injection energy is eventually transfered to solar wind
 protons, independent of the actual injection rate.&amp;nbsp;&lt;br&gt;&lt;br&gt;&lt;b&gt;Key words.&lt;/b&gt; Interplanetary physics (energetic
 particles; interstellar gas; solar wind plasma)</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
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