Das Verhältnis der Stabilisotopen18O und16O zur Beurteilung von Auslandswein
Identifieur interne : 000C18 ( Istex/Corpus ); précédent : 000C17; suivant : 000C19Das Verhältnis der Stabilisotopen18O und16O zur Beurteilung von Auslandswein
Auteurs : Brigitte Holbach ; Hilmar Förstel ; Herbert Otteneder ; Heinz HützenSource :
- Zeitschrift für Lebensmittel-Untersuchung und Forschung [ 0044-3026 ] ; 1994-03-01.
Abstract
Abstract: The relation of the stabile isotopes18O/16O was determined as deviation from an internationally accepted standard (Delta-value in per mil.; standard SMOW) with SIRA in 359 wines of Tunis, Portugal, Greece, Italy, Spain and Hungary. The determined relation is primary influenced by the geografical latitude of the wine region. The influence of the year and the climatic effect of certain areas increases from the south to the north. The results of individual climatical homogeneous areas are combined. They can serve as provisional base of knowledge in order to indicate the addition of water and false declarations of the origin of wines. Furthermore, information is given about the Delta-values of the ground-water of different regions, which are completely negative. Examples were given how to quantify the addition of water by using the Delta-values of authentic wines and ground-water. Some examples for falsification of wines are described. What ist further needed for using the18O/16O-ratio in the routine analysis of wines is discussed.
Url:
DOI: 10.1007/BF01192599
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ISTEX:E10ABDBCC0585B696E7194A3EFB0FBE69DCAB8E2Le document en format XML
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The determined relation is primary influenced by the geografical latitude of the wine region. The influence of the year and the climatic effect of certain areas increases from the south to the north. The results of individual climatical homogeneous areas are combined. They can serve as provisional base of knowledge in order to indicate the addition of water and false declarations of the origin of wines. Furthermore, information is given about the Delta-values of the ground-water of different regions, which are completely negative. Examples were given how to quantify the addition of water by using the Delta-values of authentic wines and ground-water. Some examples for falsification of wines are described. What ist further needed for using the18O/16O-ratio in the routine analysis of wines is discussed.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Brigitte Holbach</name><affiliations><json:string>Chemisches Untersuchungsamt Trier, Maximineracht 11a, D-54295, Trier, Deutschland</json:string></affiliations></json:item><json:item><name>Hilmar Förstel</name><affiliations><json:string>Institut für Radioagronomie, Forschungszentrum Jülich, Postfach 1913, D-52425, Jülich, Deutschland</json:string></affiliations></json:item><json:item><name>Herbert Otteneder</name><affiliations><json:string>Chemisches Untersuchungsamt Trier, Maximineracht 11a, D-54295, Trier, Deutschland</json:string></affiliations></json:item><json:item><name>Heinz Hützen</name><affiliations><json:string>Institut für Radioagronomie, Forschungszentrum Jülich, Postfach 1913, D-52425, Jülich, Deutschland</json:string></affiliations></json:item></author><articleId><json:string>BF01192599</json:string><json:string>Art6</json:string></articleId><language><json:string>ger</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: The relation of the stabile isotopes18O/16O was determined as deviation from an internationally accepted standard (Delta-value in per mil.; standard SMOW) with SIRA in 359 wines of Tunis, Portugal, Greece, Italy, Spain and Hungary. The determined relation is primary influenced by the geografical latitude of the wine region. The influence of the year and the climatic effect of certain areas increases from the south to the north. The results of individual climatical homogeneous areas are combined. They can serve as provisional base of knowledge in order to indicate the addition of water and false declarations of the origin of wines. Furthermore, information is given about the Delta-values of the ground-water of different regions, which are completely negative. Examples were given how to quantify the addition of water by using the Delta-values of authentic wines and ground-water. Some examples for falsification of wines are described. What ist further needed for using the18O/16O-ratio in the routine analysis of wines is discussed.</abstract><qualityIndicators><score>4.862</score><pdfVersion>1.3</pdfVersion><pdfPageSize>594 x 785 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1053</abstractCharCount><pdfWordCount>2942</pdfWordCount><pdfCharCount>19875</pdfCharCount><pdfPageCount>7</pdfPageCount><abstractWordCount>160</abstractWordCount></qualityIndicators><title>Das Verhältnis der Stabilisotopen18O und16O zur Beurteilung von Auslandswein</title><refBibs><json:item><host><author><json:item><name>Muscadet Bordeaux Chablis Montepulciano</name></json:item><json:item><name> Frascati</name></json:item></author><publicationDate>1991</publicationDate></host></json:item><json:item><author><json:item><name>J Dunbar</name></json:item></author><host><volume>174</volume><pages><last>359</last><first>355</first></pages><author></author><title>Z Lebensm Unters Forsch</title><publicationDate>1982</publicationDate></host><publicationDate>1982</publicationDate></json:item><json:item><author><json:item><name>H F6rstel</name></json:item><json:item><name>H Hfitzen</name></json:item></author><host><volume>120</volume><pages><last>76</last><first>71</first></pages><author></author><title>Weinwirtsch</title><publicationDate>1984</publicationDate></host><publicationDate>1984</publicationDate></json:item><json:item><author></author><host><volume>72</volume><pages><last>455</last><first>449</first></pages><author></author><title>F6rstel H Naturwissenschaften</title><publicationDate>1985</publicationDate></host><publicationDate>1985</publicationDate></json:item><json:item><author><json:item><name>H F6rstel</name></json:item><json:item><name>H Hfitzen</name></json:item></author><host><volume>122</volume><pages><last>16</last><first>13</first></pages><author></author><title>Weinwirtsch</title><publicationDate>1986</publicationDate></host><publicationDate>1986</publicationDate></json:item><json:item><author></author><host><volume>122</volume><pages><last>208</last><first>202</first></pages><author></author><title>F6rstel H Weinwirtsch</title><publicationDate>1986</publicationDate></host><publicationDate>1986</publicationDate></json:item><json:item><author><json:item><name>S Epstein</name></json:item><json:item><name>T Mayeda</name></json:item></author><host><volume>4</volume><pages><first>213</first></pages><author></author><title>Geochim Cosmochim Acta</title><publicationDate>1953</publicationDate></host><publicationDate>1953</publicationDate></json:item><json:item><author><json:item><name>P Horn</name></json:item><json:item><name> Schaafp</name></json:item><json:item><name>B Holbach</name></json:item><json:item><name>S H61zl</name></json:item><json:item><name>H Eschnauer</name></json:item></author><host><volume>196</volume><pages><last>409</last><first>407</first></pages><author></author><title>Z Lebensm Unters Forsch</title><publicationDate>1993</publicationDate></host><publicationDate>1993</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>198</volume><pages><last>229</last><first>223</first></pages><issn><json:string>0044-3026</json:string></issn><issue>3</issue><subject><json:item><value>Analytical Chemistry</value></json:item><json:item><value>Biotechnology</value></json:item><json:item><value>Food Science</value></json:item><json:item><value>Agriculture</value></json:item><json:item><value>Forestry</value></json:item></subject><journalId><json:string>217</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1438-2385</json:string></eissn><title>Zeitschrift für Lebensmittel-Untersuchung und Forschung</title><publicationDate>1994</publicationDate><copyrightDate>1994</copyrightDate></host><categories><wos></wos><scienceMetrix><json:string>applied sciences</json:string><json:string>agriculture, fisheries & forestry</json:string><json:string>food science</json:string></scienceMetrix></categories><publicationDate>1994</publicationDate><copyrightDate>1994</copyrightDate><doi><json:string>10.1007/BF01192599</json:string></doi><id>E10ABDBCC0585B696E7194A3EFB0FBE69DCAB8E2</id><score>0.54200613</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/E10ABDBCC0585B696E7194A3EFB0FBE69DCAB8E2/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/E10ABDBCC0585B696E7194A3EFB0FBE69DCAB8E2/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/E10ABDBCC0585B696E7194A3EFB0FBE69DCAB8E2/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="de">Das Verhältnis der Stabilisotopen18O und16O zur Beurteilung von Auslandswein</title><title level="a" type="alt" xml:lang="en">The stable-isotope-ratio of18O and16O as a mean to evaluate foreign wine</title><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Springer-Verlag</publisher><pubPlace>Berlin/Heidelberg</pubPlace><availability><p>Springer-Verlag, 1994</p></availability><date>1993-08-24</date></publicationStmt><notesStmt><note>Originalarbeit</note></notesStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="de">Das Verhältnis der Stabilisotopen18O und16O zur Beurteilung von Auslandswein</title><title level="a" type="alt" xml:lang="en">The stable-isotope-ratio of18O and16O as a mean to evaluate foreign wine</title><author xml:id="author-1"><persName><forename type="first">Brigitte</forename><surname>Holbach</surname></persName><affiliation>Chemisches Untersuchungsamt Trier, Maximineracht 11a, D-54295, Trier, Deutschland</affiliation></author><author xml:id="author-2"><persName><forename type="first">Hilmar</forename><surname>Förstel</surname></persName><affiliation>Institut für Radioagronomie, Forschungszentrum Jülich, Postfach 1913, D-52425, Jülich, Deutschland</affiliation></author><author xml:id="author-3" corresp="yes"><persName><forename type="first">Herbert</forename><surname>Otteneder</surname></persName><affiliation>Chemisches Untersuchungsamt Trier, Maximineracht 11a, D-54295, Trier, Deutschland</affiliation></author><author xml:id="author-4"><persName><forename type="first">Heinz</forename><surname>Hützen</surname></persName><affiliation>Institut für Radioagronomie, Forschungszentrum Jülich, Postfach 1913, D-52425, Jülich, Deutschland</affiliation></author></analytic><monogr><title level="j">Zeitschrift für Lebensmittel-Untersuchung und Forschung</title><title level="j" type="abbrev">Z Lebensm Unters Forch</title><idno type="journal-ID">217</idno><idno type="pISSN">0044-3026</idno><idno type="eISSN">1438-2385</idno><idno type="issue-article-count">15</idno><idno type="volume-issue-count">6</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>Berlin/Heidelberg</pubPlace><date type="published" when="1994-03-01"></date><biblScope unit="volume">198</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="223">223</biblScope><biblScope unit="page" to="229">229</biblScope></imprint></monogr><idno type="istex">E10ABDBCC0585B696E7194A3EFB0FBE69DCAB8E2</idno><idno type="DOI">10.1007/BF01192599</idno><idno type="ArticleID">BF01192599</idno><idno type="ArticleID">Art6</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1993-08-24</date></creation><langUsage><language ident="de">de</language></langUsage><abstract xml:lang="en"><p>Abstract: The relation of the stabile isotopes18O/16O was determined as deviation from an internationally accepted standard (Delta-value in per mil.; standard SMOW) with SIRA in 359 wines of Tunis, Portugal, Greece, Italy, Spain and Hungary. The determined relation is primary influenced by the geografical latitude of the wine region. The influence of the year and the climatic effect of certain areas increases from the south to the north. The results of individual climatical homogeneous areas are combined. They can serve as provisional base of knowledge in order to indicate the addition of water and false declarations of the origin of wines. Furthermore, information is given about the Delta-values of the ground-water of different regions, which are completely negative. Examples were given how to quantify the addition of water by using the Delta-values of authentic wines and ground-water. Some examples for falsification of wines are described. What ist further needed for using the18O/16O-ratio in the routine analysis of wines is discussed.</p></abstract><abstract xml:lang="de"><p>Zusammenfassung: Das Verhältnis der stabilen Isotopen18O/16O wurde als Abweichung von einem Standard (Delta-Wert in Promille; Standard SMOW) mittels SIRA an insgesamt 359 Weinproben aus Tunesien, Portugal, Griechenland, Italien, Spanien und Ungarn bestimmt. Das ermittelte Verhältnis wird primär von der geographischen Breite des Anbaugebietes beeinflußt. Der Einfluß des Jahrgangs und des Kleinklimas bestimmter Anbauzonen nehmen vom Süden nach Norden zu. Die Ergebnisse einzelner, klimatisch einheitlicher Zonen werden zusammengefaßt. Sie sollen als vorläufige Beurteilungsgrundlage dienen, eventuelle Wasserzusätze oder falsche Angaben zur Herkunft von Weinen zu erkennen. Weiterhin werden die Delta-Werte von Grundwasser unterschiedlichster Herkunft angegeben. Sie liegen ausschließlich im negativen Bereich. Es wird aufgezeigt, wie sich anhand der Delta-Werte authentischer Weine und des Grundwassers Wasserzusätze erkennen und quantitativ abschätzen lassen. Einzelne Beispiele für Weinfälschungen aus der Praxis werden vorgestellt. Die Voraussetzungen für die routinemäßige Anwendung des18O/16O-Verhältnisses werden diskutiert.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Chemistry</head><item><term>Analytical Chemistry</term></item><item><term>Biotechnology</term></item><item><term>Food Science</term></item><item><term>Agriculture</term></item><item><term>Forestry</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1993-08-24">Created</change><change when="1994-03-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-11-23">References added</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-01-21">References added</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/E10ABDBCC0585B696E7194A3EFB0FBE69DCAB8E2/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Springer, Publisher found" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" encoding="UTF-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//Springer-Verlag//DTD A++ V2.4//EN" URI="http://devel.springer.de/A++/V2.4/DTD/A++V2.4.dtd" name="istex:docType"></istex:docType><istex:document><Publisher><PublisherInfo><PublisherName>Springer-Verlag</PublisherName><PublisherLocation>Berlin/Heidelberg</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>217</JournalID><JournalPrintISSN>0044-3026</JournalPrintISSN><JournalElectronicISSN>1438-2385</JournalElectronicISSN><JournalTitle>Zeitschrift für Lebensmittel-Untersuchung und Forschung</JournalTitle><JournalAbbreviatedTitle>Z Lebensm Unters Forch</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Chemistry</JournalSubject><JournalSubject Type="Secondary">Analytical Chemistry</JournalSubject><JournalSubject Type="Secondary">Biotechnology</JournalSubject><JournalSubject Type="Secondary">Food Science</JournalSubject><JournalSubject Type="Secondary">Agriculture</JournalSubject><JournalSubject Type="Secondary">Forestry</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>198</VolumeIDStart><VolumeIDEnd>198</VolumeIDEnd><VolumeIssueCount>6</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>3</IssueIDStart><IssueIDEnd>3</IssueIDEnd><IssueArticleCount>15</IssueArticleCount><IssueHistory><CoverDate><Year>1994</Year><Month>3</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Springer-Verlag</CopyrightHolderName><CopyrightYear>1994</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art6"><ArticleInfo Language="De" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF01192599</ArticleID><ArticleDOI>10.1007/BF01192599</ArticleDOI><ArticleSequenceNumber>6</ArticleSequenceNumber><ArticleTitle Language="De">Das Verhältnis der Stabilisotopen<Superscript>18</Superscript>O und<Superscript>16</Superscript>O zur Beurteilung von Auslandswein</ArticleTitle><ArticleTitle Language="En">The stable-isotope-ratio of<Superscript>18</Superscript>O and<Superscript>16</Superscript>O as a mean to evaluate foreign wine</ArticleTitle><ArticleCategory>Originalarbeit</ArticleCategory><ArticleFirstPage>223</ArticleFirstPage><ArticleLastPage>229</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2005</Year><Month>2</Month><Day>3</Day></RegistrationDate><Received><Year>1993</Year><Month>8</Month><Day>24</Day></Received></ArticleHistory><ArticleCopyright><CopyrightHolderName>Springer-Verlag</CopyrightHolderName><CopyrightYear>1994</CopyrightYear></ArticleCopyright><ArticleGrants Type="Regular"><MetadataGrant Grant="OpenAccess"></MetadataGrant><AbstractGrant Grant="OpenAccess"></AbstractGrant><BodyPDFGrant Grant="Restricted"></BodyPDFGrant><BodyHTMLGrant Grant="Restricted"></BodyHTMLGrant><BibliographyGrant Grant="Restricted"></BibliographyGrant><ESMGrant Grant="Restricted"></ESMGrant></ArticleGrants><ArticleContext><JournalID>217</JournalID><VolumeIDStart>198</VolumeIDStart><VolumeIDEnd>198</VolumeIDEnd><IssueIDStart>3</IssueIDStart><IssueIDEnd>3</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Brigitte</GivenName><FamilyName>Holbach</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff2"><AuthorName DisplayOrder="Western"><GivenName>Hilmar</GivenName><FamilyName>Förstel</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1" CorrespondingAffiliationID="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Herbert</GivenName><FamilyName>Otteneder</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff2"><AuthorName DisplayOrder="Western"><GivenName>Heinz</GivenName><FamilyName>Hützen</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgName>Chemisches Untersuchungsamt Trier</OrgName><OrgAddress><Street>Maximineracht 11a</Street><Postcode>D-54295</Postcode><City>Trier</City><Country>Deutschland</Country></OrgAddress></Affiliation><Affiliation ID="Aff2"><OrgDivision>Institut für Radioagronomie</OrgDivision><OrgName>Forschungszentrum Jülich</OrgName><OrgAddress><Postbox>Postfach 1913</Postbox><Postcode>D-52425</Postcode><City>Jülich</City><Country>Deutschland</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>The relation of the stabile isotopes<Superscript>18</Superscript>O/<Superscript>16</Superscript>O was determined as deviation from an internationally accepted standard (Delta-value in per mil.; standard SMOW) with SIRA in 359 wines of Tunis, Portugal, Greece, Italy, Spain and Hungary. The determined relation is primary influenced by the geografical latitude of the wine region. The influence of the year and the climatic effect of certain areas increases from the south to the north. The results of individual climatical homogeneous areas are combined. They can serve as provisional base of knowledge in order to indicate the addition of water and false declarations of the origin of wines.</Para><Para>Furthermore, information is given about the Delta-values of the ground-water of different regions, which are completely negative. Examples were given how to quantify the addition of water by using the Delta-values of authentic wines and ground-water. Some examples for falsification of wines are described. What ist further needed for using the<Superscript>18</Superscript>O/<Superscript>16</Superscript>O-ratio in the routine analysis of wines is discussed.</Para></Abstract><Abstract ID="Abs2" Language="De"><Heading>Zusammenfassung</Heading><Para>Das Verhältnis der stabilen Isotopen<Superscript>18</Superscript>O/<Superscript>16</Superscript>O wurde als Abweichung von einem Standard (Delta-Wert in Promille; Standard SMOW) mittels SIRA an insgesamt 359 Weinproben aus Tunesien, Portugal, Griechenland, Italien, Spanien und Ungarn bestimmt. Das ermittelte Verhältnis wird primär von der geographischen Breite des Anbaugebietes beeinflußt. Der Einfluß des Jahrgangs und des Kleinklimas bestimmter Anbauzonen nehmen vom Süden nach Norden zu. Die Ergebnisse einzelner, klimatisch einheitlicher Zonen werden zusammengefaßt. Sie sollen als vorläufige Beurteilungsgrundlage dienen, eventuelle Wasserzusätze oder falsche Angaben zur Herkunft von Weinen zu erkennen. Weiterhin werden die Delta-Werte von Grundwasser unterschiedlichster Herkunft angegeben. Sie liegen ausschließlich im negativen Bereich. Es wird aufgezeigt, wie sich anhand der Delta-Werte authentischer Weine und des Grundwassers Wasserzusätze erkennen und quantitativ abschätzen lassen. Einzelne Beispiele für Weinfälschungen aus der Praxis werden vorgestellt. Die Voraussetzungen für die routinemäßige Anwendung des<Superscript>18</Superscript>O/<Superscript>16</Superscript>O-Verhältnisses werden diskutiert.</Para></Abstract></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="de"><title>Das Verhältnis der Stabilisotopen18O und16O zur Beurteilung von Auslandswein</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="de"><title>Das Verhältnis der Stabilisotopen18O und16O zur Beurteilung von Auslandswein</title></titleInfo><titleInfo lang="en"><title>The stable-isotope-ratio of18O and16O as a mean to evaluate foreign wine</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>The stable-isotope-ratio of18O and16O as a mean to evaluate foreign wine</title></titleInfo><name type="personal"><namePart type="given">Brigitte</namePart><namePart type="family">Holbach</namePart><affiliation>Chemisches Untersuchungsamt Trier, Maximineracht 11a, D-54295, Trier, Deutschland</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Hilmar</namePart><namePart type="family">Förstel</namePart><affiliation>Institut für Radioagronomie, Forschungszentrum Jülich, Postfach 1913, D-52425, Jülich, Deutschland</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal" displayLabel="corresp"><namePart type="given">Herbert</namePart><namePart type="family">Otteneder</namePart><affiliation>Chemisches Untersuchungsamt Trier, Maximineracht 11a, D-54295, Trier, Deutschland</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Heinz</namePart><namePart type="family">Hützen</namePart><affiliation>Institut für Radioagronomie, Forschungszentrum Jülich, Postfach 1913, D-52425, Jülich, Deutschland</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Springer-Verlag</publisher><place><placeTerm type="text">Berlin/Heidelberg</placeTerm></place><dateCreated encoding="w3cdtf">1993-08-24</dateCreated><dateIssued encoding="w3cdtf">1994-03-01</dateIssued><copyrightDate encoding="w3cdtf">1994</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">de</languageTerm><languageTerm type="code" authority="iso639-2b">ger</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Abstract: The relation of the stabile isotopes18O/16O was determined as deviation from an internationally accepted standard (Delta-value in per mil.; standard SMOW) with SIRA in 359 wines of Tunis, Portugal, Greece, Italy, Spain and Hungary. The determined relation is primary influenced by the geografical latitude of the wine region. The influence of the year and the climatic effect of certain areas increases from the south to the north. The results of individual climatical homogeneous areas are combined. They can serve as provisional base of knowledge in order to indicate the addition of water and false declarations of the origin of wines. Furthermore, information is given about the Delta-values of the ground-water of different regions, which are completely negative. Examples were given how to quantify the addition of water by using the Delta-values of authentic wines and ground-water. Some examples for falsification of wines are described. What ist further needed for using the18O/16O-ratio in the routine analysis of wines is discussed.</abstract><abstract lang="de">Zusammenfassung: Das Verhältnis der stabilen Isotopen18O/16O wurde als Abweichung von einem Standard (Delta-Wert in Promille; Standard SMOW) mittels SIRA an insgesamt 359 Weinproben aus Tunesien, Portugal, Griechenland, Italien, Spanien und Ungarn bestimmt. Das ermittelte Verhältnis wird primär von der geographischen Breite des Anbaugebietes beeinflußt. Der Einfluß des Jahrgangs und des Kleinklimas bestimmter Anbauzonen nehmen vom Süden nach Norden zu. Die Ergebnisse einzelner, klimatisch einheitlicher Zonen werden zusammengefaßt. Sie sollen als vorläufige Beurteilungsgrundlage dienen, eventuelle Wasserzusätze oder falsche Angaben zur Herkunft von Weinen zu erkennen. Weiterhin werden die Delta-Werte von Grundwasser unterschiedlichster Herkunft angegeben. Sie liegen ausschließlich im negativen Bereich. Es wird aufgezeigt, wie sich anhand der Delta-Werte authentischer Weine und des Grundwassers Wasserzusätze erkennen und quantitativ abschätzen lassen. Einzelne Beispiele für Weinfälschungen aus der Praxis werden vorgestellt. Die Voraussetzungen für die routinemäßige Anwendung des18O/16O-Verhältnisses werden diskutiert.</abstract><note>Originalarbeit</note><relatedItem type="host"><titleInfo><title>Zeitschrift für Lebensmittel-Untersuchung und Forschung</title></titleInfo><titleInfo type="abbreviated"><title>Z Lebensm Unters Forch</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1994-03-01</dateIssued><copyrightDate encoding="w3cdtf">1994</copyrightDate></originInfo><subject><genre>Chemistry</genre><topic>Analytical Chemistry</topic><topic>Biotechnology</topic><topic>Food Science</topic><topic>Agriculture</topic><topic>Forestry</topic></subject><identifier type="ISSN">0044-3026</identifier><identifier type="eISSN">1438-2385</identifier><identifier type="JournalID">217</identifier><identifier type="IssueArticleCount">15</identifier><identifier type="VolumeIssueCount">6</identifier><part><date>1994</date><detail type="volume"><number>198</number><caption>vol.</caption></detail><detail type="issue"><number>3</number><caption>no.</caption></detail><extent unit="pages"><start>223</start><end>229</end></extent></part><recordInfo><recordOrigin>Springer-Verlag, 1994</recordOrigin></recordInfo></relatedItem><identifier type="istex">E10ABDBCC0585B696E7194A3EFB0FBE69DCAB8E2</identifier><identifier type="DOI">10.1007/BF01192599</identifier><identifier type="ArticleID">BF01192599</identifier><identifier type="ArticleID">Art6</identifier><accessCondition type="use and reproduction" contentType="copyright">Springer-Verlag, 1994</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Springer-Verlag, 1994</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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