Carbon and hydrogen isotopes of n-alkanes in soils reconstructed after mining disturbance.
Identifieur interne : 000531 ( Main/Exploration ); précédent : 000530; suivant : 000532Carbon and hydrogen isotopes of n-alkanes in soils reconstructed after mining disturbance.
Auteurs : Alexia Paul [Canada] ; Sylvie A. Quideau [Canada]Source :
- Journal of environmental quality [ 1537-2537 ] ; 2020.
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- MESH :
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- geographic : Canada.
English descriptors
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Abstract
Ecosystem reconstruction after mining disturbance is a challenge considering the multitude of factors that affect soil formation and revegetation. In the boreal forest of western Canada, peat material is often used as the organic amendment for land reclamation to upland forest. Carbon and water dynamics of peat-dominated ecosystems differ from natural upland forest soils. The objective of this work was to evaluate the evolution of soils reconstructed after mining disturbance using 13 C and 2 H analyses of n-alkane tracers. Ten soils from natural ecosystems were sampled (0-10 cm) and compared with 11 soils from novel ecosystems ranging in age from 0 to 30 yr, as well as a fresh peat sample. Soils supported different vegetation, including pine (Pinus spp.), aspen (Populus spp.), and white spruce [Picea glauca (Moench) Voss]. Despite overlaps for some individual n-alkanes, we found a dominance of n-C25 in reconstructed soils, also dominant in the peat material, and a dominance of n-C27 in natural soils, one of the dominant n-alkanes in natural forest vegetation. In addition, there was a significant difference in odd n-alkane δ2 H and δ13 C values between natural and reconstructed soils (p < .05). Differences in δ2 H values, more negative for reconstructed soils than for natural soils, were attributed to changes in soil moisture, from wetter peat-dominated soils to drier upland forests; among forest types, δ2 H values were most negative under pine vegetation. The δ13 C composition of odd n-alkanes, in particular n-C27 , was significantly related to tree age (p < .05). Overall, both 2 H and 13 C isotopic signatures of odd n-alkanes exhibited differences between natural and reconstructed soils. However, within the reconstructed soils, neither isotopic signature showed a clear evolution with age since reclamation.
DOI: 10.1002/jeq2.20069
PubMed: 33016403
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Quideau</name><affiliation wicri:level="1"><nlm:affiliation>Dep. of Renewable Resources, Univ. of Alberta, 442 Earth Sciences Building, Edmonton, AB, T6G 2E3, Canada.</nlm:affiliation><country xml:lang="fr">Canada</country><wicri:regionArea>Dep. of Renewable Resources, Univ. of Alberta, 442 Earth Sciences Building, Edmonton, AB, T6G 2E3</wicri:regionArea><wicri:noRegion>T6G 2E3</wicri:noRegion></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">PubMed</idno><date when="2020">2020</date><idno type="RBID">pubmed:33016403</idno><idno type="pmid">33016403</idno><idno type="doi">10.1002/jeq2.20069</idno><idno type="wicri:Area/Main/Corpus">000070</idno><idno type="wicri:explorRef" wicri:stream="Main" wicri:step="Corpus" wicri:corpus="PubMed">000070</idno><idno type="wicri:Area/Main/Curation">000070</idno><idno type="wicri:explorRef" wicri:stream="Main" wicri:step="Curation">000070</idno><idno type="wicri:Area/Main/Exploration">000070</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en">Carbon and hydrogen isotopes of n-alkanes in soils reconstructed after mining disturbance.</title><author><name sortKey="Paul, Alexia" sort="Paul, Alexia" uniqKey="Paul A" first="Alexia" last="Paul">Alexia Paul</name><affiliation wicri:level="1"><nlm:affiliation>Dep. of Renewable Resources, Univ. of Alberta, 442 Earth Sciences Building, Edmonton, AB, T6G 2E3, Canada.</nlm:affiliation><country xml:lang="fr">Canada</country><wicri:regionArea>Dep. of Renewable Resources, Univ. of Alberta, 442 Earth Sciences Building, Edmonton, AB, T6G 2E3</wicri:regionArea><wicri:noRegion>T6G 2E3</wicri:noRegion></affiliation></author><author><name sortKey="Quideau, Sylvie A" sort="Quideau, Sylvie A" uniqKey="Quideau S" first="Sylvie A" last="Quideau">Sylvie A. Quideau</name><affiliation wicri:level="1"><nlm:affiliation>Dep. of Renewable Resources, Univ. of Alberta, 442 Earth Sciences Building, Edmonton, AB, T6G 2E3, Canada.</nlm:affiliation><country xml:lang="fr">Canada</country><wicri:regionArea>Dep. of Renewable Resources, Univ. of Alberta, 442 Earth Sciences Building, Edmonton, AB, T6G 2E3</wicri:regionArea><wicri:noRegion>T6G 2E3</wicri:noRegion></affiliation></author></analytic><series><title level="j">Journal of environmental quality</title><idno type="eISSN">1537-2537</idno><imprint><date when="2020" type="published">2020</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Alkanes (MeSH)</term><term>Canada (MeSH)</term><term>Carbon (MeSH)</term><term>Ecosystem (MeSH)</term><term>Hydrogen (MeSH)</term><term>Isotopes (MeSH)</term><term>Soil (MeSH)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Alcanes (MeSH)</term><term>Canada (MeSH)</term><term>Carbone (MeSH)</term><term>Hydrogène (MeSH)</term><term>Isotopes (MeSH)</term><term>Sol (MeSH)</term><term>Écosystème (MeSH)</term></keywords><keywords scheme="MESH" type="chemical" xml:lang="en"><term>Alkanes</term><term>Carbon</term><term>Hydrogen</term><term>Isotopes</term><term>Soil</term></keywords><keywords scheme="MESH" type="geographic" xml:lang="en"><term>Canada</term></keywords><keywords scheme="MESH" xml:lang="en"><term>Ecosystem</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Alcanes</term><term>Canada</term><term>Carbone</term><term>Hydrogène</term><term>Isotopes</term><term>Sol</term><term>Écosystème</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Canada</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Ecosystem reconstruction after mining disturbance is a challenge considering the multitude of factors that affect soil formation and revegetation. In the boreal forest of western Canada, peat material is often used as the organic amendment for land reclamation to upland forest. Carbon and water dynamics of peat-dominated ecosystems differ from natural upland forest soils. The objective of this work was to evaluate the evolution of soils reconstructed after mining disturbance using <sup>13</sup> C and <sup>2</sup> H analyses of n-alkane tracers. Ten soils from natural ecosystems were sampled (0-10 cm) and compared with 11 soils from novel ecosystems ranging in age from 0 to 30 yr, as well as a fresh peat sample. Soils supported different vegetation, including pine (Pinus spp.), aspen (Populus spp.), and white spruce [Picea glauca (Moench) Voss]. Despite overlaps for some individual n-alkanes, we found a dominance of n-C<sub>25</sub> in reconstructed soils, also dominant in the peat material, and a dominance of n-C<sub>27</sub> in natural soils, one of the dominant n-alkanes in natural forest vegetation. In addition, there was a significant difference in odd n-alkane δ<sup>2</sup> H and δ<sup>13</sup> C values between natural and reconstructed soils (p < .05). Differences in δ<sup>2</sup> H values, more negative for reconstructed soils than for natural soils, were attributed to changes in soil moisture, from wetter peat-dominated soils to drier upland forests; among forest types, δ<sup>2</sup> H values were most negative under pine vegetation. The δ<sup>13</sup> C composition of odd n-alkanes, in particular n-C<sub>27</sub> , was significantly related to tree age (p < .05). Overall, both <sup>2</sup> H and <sup>13</sup> C isotopic signatures of odd n-alkanes exhibited differences between natural and reconstructed soils. However, within the reconstructed soils, neither isotopic signature showed a clear evolution with age since reclamation.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" IndexingMethod="Automated" Owner="NLM"><PMID Version="1">33016403</PMID><DateCompleted><Year>2020</Year><Month>10</Month><Day>06</Day></DateCompleted><DateRevised><Year>2020</Year><Month>10</Month><Day>06</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1537-2537</ISSN><JournalIssue CitedMedium="Internet"><Volume>49</Volume><Issue>3</Issue><PubDate><Year>2020</Year><Month>May</Month></PubDate></JournalIssue><Title>Journal of environmental quality</Title><ISOAbbreviation>J Environ Qual</ISOAbbreviation></Journal><ArticleTitle>Carbon and hydrogen isotopes of n-alkanes in soils reconstructed after mining disturbance.</ArticleTitle><Pagination><MedlinePgn>688-699</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1002/jeq2.20069</ELocationID><Abstract><AbstractText>Ecosystem reconstruction after mining disturbance is a challenge considering the multitude of factors that affect soil formation and revegetation. In the boreal forest of western Canada, peat material is often used as the organic amendment for land reclamation to upland forest. Carbon and water dynamics of peat-dominated ecosystems differ from natural upland forest soils. The objective of this work was to evaluate the evolution of soils reconstructed after mining disturbance using <sup>13</sup> C and <sup>2</sup> H analyses of n-alkane tracers. Ten soils from natural ecosystems were sampled (0-10 cm) and compared with 11 soils from novel ecosystems ranging in age from 0 to 30 yr, as well as a fresh peat sample. Soils supported different vegetation, including pine (Pinus spp.), aspen (Populus spp.), and white spruce [Picea glauca (Moench) Voss]. Despite overlaps for some individual n-alkanes, we found a dominance of n-C<sub>25</sub> in reconstructed soils, also dominant in the peat material, and a dominance of n-C<sub>27</sub> in natural soils, one of the dominant n-alkanes in natural forest vegetation. In addition, there was a significant difference in odd n-alkane δ<sup>2</sup> H and δ<sup>13</sup> C values between natural and reconstructed soils (p < .05). Differences in δ<sup>2</sup> H values, more negative for reconstructed soils than for natural soils, were attributed to changes in soil moisture, from wetter peat-dominated soils to drier upland forests; among forest types, δ<sup>2</sup> H values were most negative under pine vegetation. The δ<sup>13</sup> C composition of odd n-alkanes, in particular n-C<sub>27</sub> , was significantly related to tree age (p < .05). Overall, both <sup>2</sup> H and <sup>13</sup> C isotopic signatures of odd n-alkanes exhibited differences between natural and reconstructed soils. However, within the reconstructed soils, neither isotopic signature showed a clear evolution with age since reclamation.</AbstractText><CopyrightInformation>© 2020 The Authors. Journal of Environmental Quality © 2020 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.</CopyrightInformation></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Paul</LastName><ForeName>Alexia</ForeName><Initials>A</Initials><Identifier Source="ORCID">https://orcid.org/0000-0003-1048-8305</Identifier><AffiliationInfo><Affiliation>Dep. of Renewable Resources, Univ. of Alberta, 442 Earth Sciences Building, Edmonton, AB, T6G 2E3, Canada.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Quideau</LastName><ForeName>Sylvie A</ForeName><Initials>SA</Initials><AffiliationInfo><Affiliation>Dep. of Renewable Resources, Univ. of Alberta, 442 Earth Sciences Building, Edmonton, AB, T6G 2E3, Canada.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><GrantList CompleteYN="Y"><Grant><GrantID>462352-2014</GrantID><Agency>Natural Sciences and Engineering Research Council of Canada</Agency><Country></Country></Grant><Grant><Agency>Canadian Oil Sands Network for Research and Development</Agency><Country></Country></Grant><Grant><Agency>Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada</Agency><Country></Country></Grant></GrantList><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2020</Year><Month>03</Month><Day>20</Day></ArticleDate></Article><MedlineJournalInfo><Country>United States</Country><MedlineTA>J Environ Qual</MedlineTA><NlmUniqueID>0330666</NlmUniqueID><ISSNLinking>0047-2425</ISSNLinking></MedlineJournalInfo><ChemicalList><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D000473">Alkanes</NameOfSubstance></Chemical><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D007554">Isotopes</NameOfSubstance></Chemical><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D012987">Soil</NameOfSubstance></Chemical><Chemical><RegistryNumber>7440-44-0</RegistryNumber><NameOfSubstance UI="D002244">Carbon</NameOfSubstance></Chemical><Chemical><RegistryNumber>7YNJ3PO35Z</RegistryNumber><NameOfSubstance UI="D006859">Hydrogen</NameOfSubstance></Chemical></ChemicalList><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D000473" MajorTopicYN="N">Alkanes</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D002170" MajorTopicYN="N" Type="Geographic">Canada</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D002244" MajorTopicYN="Y">Carbon</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D017753" MajorTopicYN="N">Ecosystem</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D006859" MajorTopicYN="N">Hydrogen</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D007554" MajorTopicYN="N">Isotopes</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D012987" MajorTopicYN="Y">Soil</DescriptorName></MeshHeading></MeshHeadingList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2019</Year><Month>05</Month><Day>21</Day></PubMedPubDate><PubMedPubDate PubStatus="revised"><Year>2019</Year><Month>12</Month><Day>10</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2020</Year><Month>02</Month><Day>21</Day></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2020</Year><Month>10</Month><Day>5</Day><Hour>8</Hour><Minute>43</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2020</Year><Month>10</Month><Day>6</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2020</Year><Month>10</Month><Day>7</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>ppublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">33016403</ArticleId><ArticleId IdType="doi">10.1002/jeq2.20069</ArticleId></ArticleIdList><ReferenceList><Title>REFERENCES</Title><Reference><Citation>Adhikari, K., & Hartemink, A. 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