The influence of soil type on the magnetic susceptibility measured throughout soil profiles
Identifieur interne : 000893 ( Main/Exploration ); précédent : 000892; suivant : 000894The influence of soil type on the magnetic susceptibility measured throughout soil profiles
Auteurs : M. Hanesch [Autriche] ; R. Scholger [Autriche]Source :
- Geophysical Journal International [ 0956-540X ] ; 2005-04.
English descriptors
- KwdEn :
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.
Url:
DOI: 10.1111/j.1365-246X.2005.02577.x
Affiliations:
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 000D46
- to stream Istex, to step Curation: 000909
- to stream Istex, to step Checkpoint: 000315
- to stream Main, to step Merge: 000903
- to stream Main, to step Curation: 000893
Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title>The influence of soil type on the magnetic susceptibility measured throughout soil profiles</title><author><name sortKey="Hanesch, M" sort="Hanesch, M" uniqKey="Hanesch M" first="M." last="Hanesch">M. Hanesch</name></author><author><name sortKey="Scholger, R" sort="Scholger, R" uniqKey="Scholger R" first="R." last="Scholger">R. Scholger</name></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:4CD88B9FDEC018582D0723856D30FD5ABCE1742A</idno><date when="2005" year="2005">2005</date><idno type="doi">10.1111/j.1365-246X.2005.02577.x</idno><idno type="url">https://api.istex.fr/document/4CD88B9FDEC018582D0723856D30FD5ABCE1742A/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000D46</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000D46</idno><idno type="wicri:Area/Istex/Curation">000909</idno><idno type="wicri:Area/Istex/Checkpoint">000315</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Checkpoint">000315</idno><idno type="wicri:doubleKey">0956-540X:2005:Hanesch M:the:influence:of</idno><idno type="wicri:Area/Main/Merge">000903</idno><idno type="wicri:Area/Main/Curation">000893</idno><idno type="wicri:Area/Main/Exploration">000893</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a">The influence of soil type on the magnetic susceptibility measured throughout soil profiles</title><author><name sortKey="Hanesch, M" sort="Hanesch, M" uniqKey="Hanesch M" first="M." last="Hanesch">M. Hanesch</name><affiliation wicri:level="1"><country wicri:rule="url">Autriche</country><wicri:regionArea>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Peter Tunner Str. 25, 8700 Leoben</wicri:regionArea><wicri:noRegion>8700 Leoben</wicri:noRegion></affiliation><affiliation wicri:level="1"><country wicri:rule="url">Autriche</country></affiliation></author><author><name sortKey="Scholger, R" sort="Scholger, R" uniqKey="Scholger R" first="R." last="Scholger">R. Scholger</name><affiliation wicri:level="1"><country wicri:rule="url">Autriche</country><wicri:regionArea>Chair of Geophysics, Department for Geosciences and Geophysics, University of Leoben, Palaeomagnetic Laboratory, Gams 45, 8130 Frohnleiten</wicri:regionArea><wicri:noRegion>8130 Frohnleiten</wicri:noRegion></affiliation><affiliation wicri:level="1"><country wicri:rule="url">Autriche</country></affiliation></author></analytic><monogr></monogr><series><title level="j">Geophysical Journal International</title><title level="j" type="abbrev">Geophys. J. Int.</title><idno type="ISSN">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">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><idno type="ISSN">0956-540X</idno></series><idno type="istex">4CD88B9FDEC018582D0723856D30FD5ABCE1742A</idno><idno type="DOI">10.1111/j.1365-246X.2005.02577.x</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0956-540X</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>magnetic susceptibility</term><term>reference signal</term><term>soil</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="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.</div></front></TEI><affiliations><list><country><li>Autriche</li></country></list><tree><country name="Autriche"><noRegion><name sortKey="Hanesch, M" sort="Hanesch, M" uniqKey="Hanesch M" first="M." last="Hanesch">M. Hanesch</name></noRegion><name sortKey="Hanesch, M" sort="Hanesch, M" uniqKey="Hanesch M" first="M." last="Hanesch">M. Hanesch</name><name sortKey="Scholger, R" sort="Scholger, R" uniqKey="Scholger R" first="R." last="Scholger">R. Scholger</name><name sortKey="Scholger, R" sort="Scholger, R" uniqKey="Scholger R" first="R." last="Scholger">R. Scholger</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Terre/explor/CobaltMaghrebV1/Data/Main/Exploration
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000893 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Main/Exploration/biblio.hfd -nk 000893 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Terre
|area= CobaltMaghrebV1
|flux= Main
|étape= Exploration
|type= RBID
|clé= ISTEX:4CD88B9FDEC018582D0723856D30FD5ABCE1742A
|texte= The influence of soil type on the magnetic susceptibility measured throughout soil profiles
}}
| This area was generated with Dilib version V0.6.32. |  |