Pyrogenic changes in iron-illuvial podzols in the middle taiga of the Komi Republic

The changes in the morphological, physicochemical, and chemical properties of iron-illuvial podzols under middle-taiga dwarf shrub-green moss pine forests in the first months after fires are examined. It is shown that forest fires are accompanied by changes in the morphology of the litter horizons,...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Eurasian soil science 2014-02, Vol.47 (2), p.47-56
Hauptverfasser: Dymov, A. A, Dubrovsky, Yu. A, Gabov, D. N
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 56
container_issue 2
container_start_page 47
container_title Eurasian soil science
container_volume 47
creator Dymov, A. A
Dubrovsky, Yu. A
Gabov, D. N
description The changes in the morphological, physicochemical, and chemical properties of iron-illuvial podzols under middle-taiga dwarf shrub-green moss pine forests in the first months after fires are examined. It is shown that forest fires are accompanied by changes in the morphology of the litter horizons, their compaction, and by changes in the chemical properties of the soils. The data on the polycyclic aromatic hydrocarbons (PAHs) indicate a significant increase in the contents of chrysene, fluorene, naphthalene, pyrene, and anthracene in the Opyr(L) horizon in comparison with the litters in the background pine forest. The total PAH content in the O(F)pyr horizon increases mainly at the expense of di- and tri-nuclear PAHs (naphthalene and fluorene). The mineral soil horizons in the burnt area become enriched in the most mobile amphiphilic fractions of the organic matter, which is seen from the increase in the absolute and relative contents of the hydrophilic fractions, which might be represented by the products of combustion of fresh plant remains and litter.
doi_str_mv 10.1134/S1064229314020045
format Article
fullrecord <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_1727694494</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A721809747</galeid><sourcerecordid>A721809747</sourcerecordid><originalsourceid>FETCH-LOGICAL-a435t-df999a572c6f478159d47d5f64a018d3e118111872b69e941938b183af94231e3</originalsourceid><addsrcrecordid>eNp9kVFL3jAUhsvYYE73A3a1wm52U81JTprkUmRTUVD2TdhdyNcmNZI235J2oL_eaHchG0gICed9nnDIqapPQA4BGB5tgLRIqWKAhBKC_E21B5y3DSj-6225l7h5yt9XH3K-I4RJiXKv2lzfpzjYyXd1d2umwebaT7VPcWp8CMsfb0K9i_1DDM_BfGvr0fd9sPVs_GDq6J5rF3H09Q-7W7bBdwfVO2dCth__nvvVzfdvP0_Omsur0_OT48vGIONz0zullOGCdq1DIYGrHkXPXYuGgOyZBZBQtqDbVlmFoJjcgmTGKaQMLNuvvq7v7lL8vdg869HnzoZgJhuXrEFQ0SpEhQX98g96F5c0le40oBKMcySqUIcrNZhgtZ9cnJPpyurt6Ls4WedL_VhQkEQJFEWAVehSzDlZp3fJjybdayD6aS76v7kUh65OLmz58PSilVekz6vkTNRmSD7rmw0lJSek5cAoewQgGJUl</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1497355409</pqid></control><display><type>article</type><title>Pyrogenic changes in iron-illuvial podzols in the middle taiga of the Komi Republic</title><source>SpringerLink Journals - AutoHoldings</source><creator>Dymov, A. A ; Dubrovsky, Yu. A ; Gabov, D. N</creator><creatorcontrib>Dymov, A. A ; Dubrovsky, Yu. A ; Gabov, D. N</creatorcontrib><description>The changes in the morphological, physicochemical, and chemical properties of iron-illuvial podzols under middle-taiga dwarf shrub-green moss pine forests in the first months after fires are examined. It is shown that forest fires are accompanied by changes in the morphology of the litter horizons, their compaction, and by changes in the chemical properties of the soils. The data on the polycyclic aromatic hydrocarbons (PAHs) indicate a significant increase in the contents of chrysene, fluorene, naphthalene, pyrene, and anthracene in the Opyr(L) horizon in comparison with the litters in the background pine forest. The total PAH content in the O(F)pyr horizon increases mainly at the expense of di- and tri-nuclear PAHs (naphthalene and fluorene). The mineral soil horizons in the burnt area become enriched in the most mobile amphiphilic fractions of the organic matter, which is seen from the increase in the absolute and relative contents of the hydrophilic fractions, which might be represented by the products of combustion of fresh plant remains and litter.</description><identifier>ISSN: 1064-2293</identifier><identifier>EISSN: 1556-195X</identifier><identifier>DOI: 10.1134/S1064229314020045</identifier><language>eng</language><publisher>Boston: Springer-Verlag</publisher><subject>Analysis ; Anthracene ; Biogeochemistry ; Chemical properties ; combustion ; Coniferous forests ; Earth and Environmental Science ; Earth Sciences ; Forest &amp; brush fires ; Forest fires ; Forest soils ; Genesis and Geography of Soils ; Geotechnical Engineering &amp; Applied Earth Sciences ; Litter ; mineral soils ; Naphthalene ; Organic matter ; physicochemical properties ; Podzols ; Polycyclic aromatic hydrocarbons ; Soil horizons ; Soil properties ; Soil sciences ; taiga</subject><ispartof>Eurasian soil science, 2014-02, Vol.47 (2), p.47-56</ispartof><rights>Pleiades Publishing, Ltd. 2014</rights><rights>COPYRIGHT 2014 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a435t-df999a572c6f478159d47d5f64a018d3e118111872b69e941938b183af94231e3</citedby><cites>FETCH-LOGICAL-a435t-df999a572c6f478159d47d5f64a018d3e118111872b69e941938b183af94231e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1064229314020045$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1064229314020045$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,777,781,27905,27906,41469,42538,51300</link.rule.ids></links><search><creatorcontrib>Dymov, A. A</creatorcontrib><creatorcontrib>Dubrovsky, Yu. A</creatorcontrib><creatorcontrib>Gabov, D. N</creatorcontrib><title>Pyrogenic changes in iron-illuvial podzols in the middle taiga of the Komi Republic</title><title>Eurasian soil science</title><addtitle>Eurasian Soil Sc</addtitle><description>The changes in the morphological, physicochemical, and chemical properties of iron-illuvial podzols under middle-taiga dwarf shrub-green moss pine forests in the first months after fires are examined. It is shown that forest fires are accompanied by changes in the morphology of the litter horizons, their compaction, and by changes in the chemical properties of the soils. The data on the polycyclic aromatic hydrocarbons (PAHs) indicate a significant increase in the contents of chrysene, fluorene, naphthalene, pyrene, and anthracene in the Opyr(L) horizon in comparison with the litters in the background pine forest. The total PAH content in the O(F)pyr horizon increases mainly at the expense of di- and tri-nuclear PAHs (naphthalene and fluorene). The mineral soil horizons in the burnt area become enriched in the most mobile amphiphilic fractions of the organic matter, which is seen from the increase in the absolute and relative contents of the hydrophilic fractions, which might be represented by the products of combustion of fresh plant remains and litter.</description><subject>Analysis</subject><subject>Anthracene</subject><subject>Biogeochemistry</subject><subject>Chemical properties</subject><subject>combustion</subject><subject>Coniferous forests</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Forest &amp; brush fires</subject><subject>Forest fires</subject><subject>Forest soils</subject><subject>Genesis and Geography of Soils</subject><subject>Geotechnical Engineering &amp; Applied Earth Sciences</subject><subject>Litter</subject><subject>mineral soils</subject><subject>Naphthalene</subject><subject>Organic matter</subject><subject>physicochemical properties</subject><subject>Podzols</subject><subject>Polycyclic aromatic hydrocarbons</subject><subject>Soil horizons</subject><subject>Soil properties</subject><subject>Soil sciences</subject><subject>taiga</subject><issn>1064-2293</issn><issn>1556-195X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kVFL3jAUhsvYYE73A3a1wm52U81JTprkUmRTUVD2TdhdyNcmNZI235J2oL_eaHchG0gICed9nnDIqapPQA4BGB5tgLRIqWKAhBKC_E21B5y3DSj-6225l7h5yt9XH3K-I4RJiXKv2lzfpzjYyXd1d2umwebaT7VPcWp8CMsfb0K9i_1DDM_BfGvr0fd9sPVs_GDq6J5rF3H09Q-7W7bBdwfVO2dCth__nvvVzfdvP0_Omsur0_OT48vGIONz0zullOGCdq1DIYGrHkXPXYuGgOyZBZBQtqDbVlmFoJjcgmTGKaQMLNuvvq7v7lL8vdg869HnzoZgJhuXrEFQ0SpEhQX98g96F5c0le40oBKMcySqUIcrNZhgtZ9cnJPpyurt6Ls4WedL_VhQkEQJFEWAVehSzDlZp3fJjybdayD6aS76v7kUh65OLmz58PSilVekz6vkTNRmSD7rmw0lJSek5cAoewQgGJUl</recordid><startdate>20140201</startdate><enddate>20140201</enddate><creator>Dymov, A. A</creator><creator>Dubrovsky, Yu. A</creator><creator>Gabov, D. N</creator><general>Springer-Verlag</general><general>Springer US</general><general>Springer</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QL</scope><scope>7ST</scope><scope>7T7</scope><scope>7U9</scope><scope>7UA</scope><scope>7X2</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H94</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M0K</scope><scope>M2P</scope><scope>M7N</scope><scope>P64</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>20140201</creationdate><title>Pyrogenic changes in iron-illuvial podzols in the middle taiga of the Komi Republic</title><author>Dymov, A. A ; Dubrovsky, Yu. A ; Gabov, D. N</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a435t-df999a572c6f478159d47d5f64a018d3e118111872b69e941938b183af94231e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Analysis</topic><topic>Anthracene</topic><topic>Biogeochemistry</topic><topic>Chemical properties</topic><topic>combustion</topic><topic>Coniferous forests</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Forest &amp; brush fires</topic><topic>Forest fires</topic><topic>Forest soils</topic><topic>Genesis and Geography of Soils</topic><topic>Geotechnical Engineering &amp; Applied Earth Sciences</topic><topic>Litter</topic><topic>mineral soils</topic><topic>Naphthalene</topic><topic>Organic matter</topic><topic>physicochemical properties</topic><topic>Podzols</topic><topic>Polycyclic aromatic hydrocarbons</topic><topic>Soil horizons</topic><topic>Soil properties</topic><topic>Soil sciences</topic><topic>taiga</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Dymov, A. A</creatorcontrib><creatorcontrib>Dubrovsky, Yu. A</creatorcontrib><creatorcontrib>Gabov, D. N</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Virology and AIDS Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Agricultural Science Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Agricultural Science Database</collection><collection>Science Database</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Eurasian soil science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Dymov, A. A</au><au>Dubrovsky, Yu. A</au><au>Gabov, D. N</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Pyrogenic changes in iron-illuvial podzols in the middle taiga of the Komi Republic</atitle><jtitle>Eurasian soil science</jtitle><stitle>Eurasian Soil Sc</stitle><date>2014-02-01</date><risdate>2014</risdate><volume>47</volume><issue>2</issue><spage>47</spage><epage>56</epage><pages>47-56</pages><issn>1064-2293</issn><eissn>1556-195X</eissn><abstract>The changes in the morphological, physicochemical, and chemical properties of iron-illuvial podzols under middle-taiga dwarf shrub-green moss pine forests in the first months after fires are examined. It is shown that forest fires are accompanied by changes in the morphology of the litter horizons, their compaction, and by changes in the chemical properties of the soils. The data on the polycyclic aromatic hydrocarbons (PAHs) indicate a significant increase in the contents of chrysene, fluorene, naphthalene, pyrene, and anthracene in the Opyr(L) horizon in comparison with the litters in the background pine forest. The total PAH content in the O(F)pyr horizon increases mainly at the expense of di- and tri-nuclear PAHs (naphthalene and fluorene). The mineral soil horizons in the burnt area become enriched in the most mobile amphiphilic fractions of the organic matter, which is seen from the increase in the absolute and relative contents of the hydrophilic fractions, which might be represented by the products of combustion of fresh plant remains and litter.</abstract><cop>Boston</cop><pub>Springer-Verlag</pub><doi>10.1134/S1064229314020045</doi><tpages>10</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1064-2293
ispartof Eurasian soil science, 2014-02, Vol.47 (2), p.47-56
issn 1064-2293
1556-195X
language eng
recordid cdi_proquest_miscellaneous_1727694494
source SpringerLink Journals - AutoHoldings
subjects Analysis
Anthracene
Biogeochemistry
Chemical properties
combustion
Coniferous forests
Earth and Environmental Science
Earth Sciences
Forest & brush fires
Forest fires
Forest soils
Genesis and Geography of Soils
Geotechnical Engineering & Applied Earth Sciences
Litter
mineral soils
Naphthalene
Organic matter
physicochemical properties
Podzols
Polycyclic aromatic hydrocarbons
Soil horizons
Soil properties
Soil sciences
taiga
title Pyrogenic changes in iron-illuvial podzols in the middle taiga of the Komi Republic
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-17T13%3A05%3A48IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Pyrogenic%20changes%20in%20iron-illuvial%20podzols%20in%20the%20middle%20taiga%20of%20the%20Komi%20Republic&rft.jtitle=Eurasian%20soil%20science&rft.au=Dymov,%20A.%20A&rft.date=2014-02-01&rft.volume=47&rft.issue=2&rft.spage=47&rft.epage=56&rft.pages=47-56&rft.issn=1064-2293&rft.eissn=1556-195X&rft_id=info:doi/10.1134/S1064229314020045&rft_dat=%3Cgale_proqu%3EA721809747%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1497355409&rft_id=info:pmid/&rft_galeid=A721809747&rfr_iscdi=true