The influence of soil type on the magnetic susceptibility measured throughout soil profiles
Identifieur interne : 000D46 ( Istex/Corpus ); précédent : 000D45; suivant : 000D47The influence of soil type on the magnetic susceptibility measured throughout soil profiles
Auteurs : M. Hanesch ; R. ScholgerSource :
- Geophysical Journal International [ 0956-540X ] ; 2005-04.
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Abstract
The interpretation of soil susceptibility measurements depends on knowledge of a reference value. This reference value will be influenced by the type of soil. In the present study, data of various soil types, which formed on diverse parent material, are analysed. As the same data set has been used in a soil pollution study, we are able to estimate and exclude the influence of pollution. Susceptibility values of unpolluted soils turn out to significantly depend on the soil type. Chernozem samples yield the highest susceptibility values of the analysed soil types (50–90 × 10−8 m3 kg−1). Cambisol displays intermediate values (20–60 × 10−8 m3 kg−1) and waterlogged soils have the lowest values (5–20 × 10−8 m3 kg−1). The enrichment of topsoil susceptibility (0–20 cm depth) compared to subsoil susceptibility (40–50 cm depth) depends more on the parent material than on the soil type. Given the comparability of soil type and parent material, the values of this study can be used to identify soils with unusual susceptibility values, which may be further analysed in order to pinpoint soil pollution.
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DOI: 10.1111/j.1365-246X.2005.02577.x
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Hanesch</name><affiliation><mods:affiliation>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Peter Tunner Str. 25, 8700 Leoben, Austria. E-mail: hanesch@unileoben.ac.at</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: hanesch@unileoben.ac.at</mods:affiliation></affiliation></author><author><name sortKey="Scholger, R" sort="Scholger, R" uniqKey="Scholger R" first="R." last="Scholger">R. Scholger</name><affiliation><mods:affiliation>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Palaeomagnetic Laboratory, Gams 45, 8130 Frohnleiten, Austria. E-mail: scholger@unileoben.ac.at</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: scholger@unileoben.ac.at</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Geophysical Journal International</title><title level="j" type="abbrev">Geophys. J. 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This reference value will be influenced by the type of soil. In the present study, data of various soil types, which formed on diverse parent material, are analysed. As the same data set has been used in a soil pollution study, we are able to estimate and exclude the influence of pollution. Susceptibility values of unpolluted soils turn out to significantly depend on the soil type. Chernozem samples yield the highest susceptibility values of the analysed soil types (50–90 × 10−8 m3 kg−1). Cambisol displays intermediate values (20–60 × 10−8 m3 kg−1) and waterlogged soils have the lowest values (5–20 × 10−8 m3 kg−1). The enrichment of topsoil susceptibility (0–20 cm depth) compared to subsoil susceptibility (40–50 cm depth) depends more on the parent material than on the soil type. Given the comparability of soil type and parent material, the values of this study can be used to identify soils with unusual susceptibility values, which may be further analysed in order to pinpoint soil pollution.</div></front></TEI><istex><corpusName>oup</corpusName><author><json:item><name>M. Hanesch</name><affiliations><json:string>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Peter Tunner Str. 25, 8700 Leoben, Austria. E-mail: hanesch@unileoben.ac.at</json:string><json:string>E-mail: hanesch@unileoben.ac.at</json:string></affiliations></json:item><json:item><name>R. Scholger</name><affiliations><json:string>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Palaeomagnetic Laboratory, Gams 45, 8130 Frohnleiten, Austria. 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Susceptibility values of unpolluted soils turn out to significantly depend on the soil type. Chernozem samples yield the highest susceptibility values of the analysed soil types (50–90 × 10−8 m3 kg−1). Cambisol displays intermediate values (20–60 × 10−8 m3 kg−1) and waterlogged soils have the lowest values (5–20 × 10−8 m3 kg−1). The enrichment of topsoil susceptibility (0–20 cm depth) compared to subsoil susceptibility (40–50 cm depth) depends more on the parent material than on the soil type. 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J. Int.</title><idno type="pISSN">0956-540X</idno><idno type="eISSN">1365-246X</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="2005-04"></date><biblScope unit="volume">161</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="50">50</biblScope><biblScope unit="page" to="56">56</biblScope></imprint></monogr><idno type="istex">4CD88B9FDEC018582D0723856D30FD5ABCE1742A</idno><idno type="DOI">10.1111/j.1365-246X.2005.02577.x</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2005</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>The interpretation of soil susceptibility measurements depends on knowledge of a reference value. This reference value will be influenced by the type of soil. In the present study, data of various soil types, which formed on diverse parent material, are analysed. As the same data set has been used in a soil pollution study, we are able to estimate and exclude the influence of pollution. Susceptibility values of unpolluted soils turn out to significantly depend on the soil type. Chernozem samples yield the highest susceptibility values of the analysed soil types (50–90 × 10−8 m3 kg−1). Cambisol displays intermediate values (20–60 × 10−8 m3 kg−1) and waterlogged soils have the lowest values (5–20 × 10−8 m3 kg−1). The enrichment of topsoil susceptibility (0–20 cm depth) compared to subsoil susceptibility (40–50 cm depth) depends more on the parent material than on the soil type. Given the comparability of soil type and parent material, the values of this study can be used to identify soils with unusual susceptibility values, which may be further analysed in order to pinpoint soil pollution.</p></abstract><textClass xml:lang="en"><keywords scheme="keyword"><list><head>Keywords</head><item><term>magnetic susceptibility</term></item><item><term>reference signal</term></item><item><term>soil</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2005-04">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><original>false</original><mimetype>text/plain</mimetype><extension>txt</extension><uri>https://api.istex.fr/document/4CD88B9FDEC018582D0723856D30FD5ABCE1742A/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="corpus oup" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0"</istex:xmlDeclaration><istex:docType PUBLIC="-//NLM//DTD Journal Publishing DTD v2.3 20070202//EN" URI="journalpublishing.dtd" name="istex:docType"></istex:docType><istex:document><article article-type="research-article"><front><journal-meta><journal-id journal-id-type="hwp">gji</journal-id><journal-id journal-id-type="publisher-id">gji</journal-id><journal-title>Geophysical Journal International</journal-title><abbrev-journal-title>Geophys. J. Int.</abbrev-journal-title><issn pub-type="ppub">0956-540X</issn><issn pub-type="epub">1365-246X</issn><publisher><publisher-name>Blackwell Publishing Ltd</publisher-name><publisher-loc>Oxford, UK</publisher-loc></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.1111/j.1365-246X.2005.02577.x</article-id><article-categories><subj-group subj-group-type="heading"><subject>Geomagnetism, rock magnetism and palaeomagnetism</subject></subj-group></article-categories><title-group><article-title>The influence of soil type on the magnetic susceptibility measured throughout soil profiles</article-title></title-group><contrib-group><contrib contrib-type="author"><name><surname>Hanesch</surname><given-names>M.</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author"><name><surname>Scholger</surname><given-names>R.</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref></contrib><aff id="aff1"><label>1</label>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Peter Tunner Str. 25, 8700 Leoben, Austria. E-mail: <email>hanesch@unileoben.ac.at</email></aff><aff id="aff2"><label>2</label>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Palaeomagnetic Laboratory, Gams 45, 8130 Frohnleiten, Austria. E-mail: <email>scholger@unileoben.ac.at</email></aff></contrib-group><pub-date pub-type="ppub"><month>4</month><year>2005</year></pub-date><volume>161</volume><issue>1</issue><fpage>50</fpage><lpage>56</lpage><history><date date-type="received"><day>27</day><month>10</month><year>2004</year></date><date date-type="accepted"><day>3</day><month>12</month><year>2004</year></date></history><permissions><copyright-statement>© 2005 RAS</copyright-statement><copyright-year>2005</copyright-year></permissions><abstract><title>Summary</title><p>The interpretation of soil susceptibility measurements depends on knowledge of a reference value. This reference value will be influenced by the type of soil. In the present study, data of various soil types, which formed on diverse parent material, are analysed. As the same data set has been used in a soil pollution study, we are able to estimate and exclude the influence of pollution. Susceptibility values of unpolluted soils turn out to significantly depend on the soil type. Chernozem samples yield the highest susceptibility values of the analysed soil types (50–90 × 10<sup>−8</sup> m<sup>3</sup> kg<sup>−1</sup>). Cambisol displays intermediate values (20–60 × 10<sup>−8</sup> m<sup>3</sup> kg<sup>−1</sup>) and waterlogged soils have the lowest values (5–20 × 10<sup>−8</sup> m<sup>3</sup> kg<sup>−1</sup>). The enrichment of topsoil susceptibility (0–20 cm depth) compared to subsoil susceptibility (40–50 cm depth) depends more on the parent material than on the soil type. Given the comparability of soil type and parent material, the values of this study can be used to identify soils with unusual susceptibility values, which may be further analysed in order to pinpoint soil pollution.</p></abstract><kwd-group xml:lang="en"><title>Keywords</title><kwd>magnetic susceptibility</kwd><kwd>reference signal</kwd><kwd>soil</kwd></kwd-group></article-meta></front></article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo><title>The influence of soil type on the magnetic susceptibility measured throughout soil profiles</title></titleInfo><titleInfo type="alternative" contentType="CDATA"><title>The influence of soil type on the magnetic susceptibility measured throughout soil profiles</title></titleInfo><name type="personal"><namePart type="given">M.</namePart><namePart type="family">Hanesch</namePart><affiliation>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Peter Tunner Str. 25, 8700 Leoben, Austria. E-mail: hanesch@unileoben.ac.at</affiliation><affiliation>E-mail: hanesch@unileoben.ac.at</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">R.</namePart><namePart type="family">Scholger</namePart><affiliation>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Palaeomagnetic Laboratory, Gams 45, 8130 Frohnleiten, Austria. E-mail: scholger@unileoben.ac.at</affiliation><affiliation>E-mail: scholger@unileoben.ac.at</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="research-article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><place><placeTerm type="text">Oxford, UK</placeTerm></place><dateIssued encoding="w3cdtf">2005-04</dateIssued><copyrightDate encoding="w3cdtf">2005</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract>The interpretation of soil susceptibility measurements depends on knowledge of a reference value. This reference value will be influenced by the type of soil. In the present study, data of various soil types, which formed on diverse parent material, are analysed. As the same data set has been used in a soil pollution study, we are able to estimate and exclude the influence of pollution. Susceptibility values of unpolluted soils turn out to significantly depend on the soil type. Chernozem samples yield the highest susceptibility values of the analysed soil types (50–90 × 10−8 m3 kg−1). Cambisol displays intermediate values (20–60 × 10−8 m3 kg−1) and waterlogged soils have the lowest values (5–20 × 10−8 m3 kg−1). The enrichment of topsoil susceptibility (0–20 cm depth) compared to subsoil susceptibility (40–50 cm depth) depends more on the parent material than on the soil type. Given the comparability of soil type and parent material, the values of this study can be used to identify soils with unusual susceptibility values, which may be further analysed in order to pinpoint soil pollution.</abstract><subject lang="en"><genre>Keywords</genre><topic>magnetic susceptibility</topic><topic>reference signal</topic><topic>soil</topic></subject><relatedItem type="host"><titleInfo><title>Geophysical Journal International</title></titleInfo><titleInfo type="abbreviated"><title>Geophys. J. 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