Vegetation- and Environmental Changes on Non-Reclaimed Spoil Heaps in Southern Poland.
Identifieur interne : 000030 ( Main/Exploration ); précédent : 000029; suivant : 000031Vegetation- and Environmental Changes on Non-Reclaimed Spoil Heaps in Southern Poland.
Auteurs : Oimahmad Rahmonov [Pologne] ; Robert Krzysztofik [Pologne] ; Dorota Rodek [Pologne] ; Justyna Smolarek-Lach [Pologne]Source :
- Biology [ 2079-7737 ] ; 2020.
Abstract
The study focused on the changes in vegetation and soils on an undeveloped area of coal mine spoil heaps. The process of vegetation changes was evaluated on the basis of historical cartographic materials and fieldwork. Changes of vegetation in nearly 200 years are presented herein. The main purpose of this study is to present an analysis of spatio-temporal changes in vegetation and their influence on soil features. The diversity of ecological species in terms of habitat requirements, tendency of hornbeam communities formation, and the relationship between forest communities and soil features was found. The basic soil properties were examined under selected plant communities (pH, Corg, Nt), available forms of elements (P, K, Mg), and as plant nutrients and heavy metal occurrence (Fe, Zn, Mn, Co, Cd, Pb, Sr, Cr, Cu). The soil organic carbon (Corg) content varied from 3.17 ± 0.007% to 17.7 ± 0.21% and significant differences were observed between sites. The highest total nitrogen (Nt) content was recorded in the soils of the sites that were represented by Populus-Betula stands (0.60 ± 0.01%). Soil acidity (pH) varied greatly, ranging from acidic (pH = 4.1) to weakly acidic (pH = 5.9). The highest value for Mgavail (205.43 ± 0.5 mg·kg-1) was noted in the soils under Calamagrostis epegijos (L.) Roth community and for Pavail (184.07 ± 3.77) and Kavail (346.19 ± 2.92 mg·kg-1) under the Quercus-Pinus stand. On all sites, Zn was a dominant element and its concentration ranged from 526.1 to 1060.4 mg·kg-1. Obtained results show how important it is to study the issue of vegetation changes and the formation of the landscape within an industrial city. The described results are important for the management of urban greening issues. Human influence on the disintegration and development of the natural environment is clearly visible. Due to the diversity of former mining areas and their time of creation, the studied area is one of the most important experimental areas for the determination link between vegetation and soil.
DOI: 10.3390/biology9070164
PubMed: 32679749
PubMed Central: PMC7408371
Affiliations:
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Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</nlm:affiliation><country xml:lang="fr">Pologne</country><wicri:regionArea>Institute of Social and Economic Geography and Spatial Management, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec</wicri:regionArea><wicri:noRegion>41-200 Sosnowiec</wicri:noRegion></affiliation></author><author><name sortKey=" Rodek, Dorota" sort=" Rodek, Dorota" uniqKey=" Rodek D" first="Dorota" last=" Rodek">Dorota Rodek</name><affiliation wicri:level="1"><nlm:affiliation>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</nlm:affiliation><country xml:lang="fr">Pologne</country><wicri:regionArea>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec</wicri:regionArea><wicri:noRegion>41-200 Sosnowiec</wicri:noRegion></affiliation></author><author><name sortKey="Smolarek Lach, Justyna" sort="Smolarek Lach, Justyna" uniqKey="Smolarek Lach J" first="Justyna" last="Smolarek-Lach">Justyna Smolarek-Lach</name><affiliation wicri:level="1"><nlm:affiliation>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</nlm:affiliation><country xml:lang="fr">Pologne</country><wicri:regionArea>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec</wicri:regionArea><wicri:noRegion>41-200 Sosnowiec</wicri:noRegion></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">PubMed</idno><date when="2020">2020</date><idno type="RBID">pubmed:32679749</idno><idno type="pmid">32679749</idno><idno type="doi">10.3390/biology9070164</idno><idno type="pmc">PMC7408371</idno><idno type="wicri:Area/Main/Corpus">000188</idno><idno type="wicri:explorRef" wicri:stream="Main" wicri:step="Corpus" wicri:corpus="PubMed">000188</idno><idno type="wicri:Area/Main/Curation">000188</idno><idno type="wicri:explorRef" 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Krzysztofik</name><affiliation wicri:level="1"><nlm:affiliation>Institute of Social and Economic Geography and Spatial Management, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</nlm:affiliation><country xml:lang="fr">Pologne</country><wicri:regionArea>Institute of Social and Economic Geography and Spatial Management, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec</wicri:regionArea><wicri:noRegion>41-200 Sosnowiec</wicri:noRegion></affiliation></author><author><name sortKey=" Rodek, Dorota" sort=" Rodek, Dorota" uniqKey=" Rodek D" first="Dorota" last=" Rodek">Dorota Rodek</name><affiliation wicri:level="1"><nlm:affiliation>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</nlm:affiliation><country xml:lang="fr">Pologne</country><wicri:regionArea>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec</wicri:regionArea><wicri:noRegion>41-200 Sosnowiec</wicri:noRegion></affiliation></author><author><name sortKey="Smolarek Lach, Justyna" sort="Smolarek Lach, Justyna" uniqKey="Smolarek Lach J" first="Justyna" last="Smolarek-Lach">Justyna Smolarek-Lach</name><affiliation wicri:level="1"><nlm:affiliation>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</nlm:affiliation><country xml:lang="fr">Pologne</country><wicri:regionArea>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec</wicri:regionArea><wicri:noRegion>41-200 Sosnowiec</wicri:noRegion></affiliation></author></analytic><series><title level="j">Biology</title><idno type="ISSN">2079-7737</idno><imprint><date when="2020" type="published">2020</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The study focused on the changes in vegetation and soils on an undeveloped area of coal mine spoil heaps. The process of vegetation changes was evaluated on the basis of historical cartographic materials and fieldwork. Changes of vegetation in nearly 200 years are presented herein. The main purpose of this study is to present an analysis of spatio-temporal changes in vegetation and their influence on soil features. The diversity of ecological species in terms of habitat requirements, tendency of hornbeam communities formation, and the relationship between forest communities and soil features was found. The basic soil properties were examined under selected plant communities (pH, C<sub>org</sub>, N<sub>t</sub>), available forms of elements (P, K, Mg), and as plant nutrients and heavy metal occurrence (Fe, Zn, Mn, Co, Cd, Pb, Sr, Cr, Cu). The soil organic carbon (C<sub>org</sub>) content varied from 3.17 ± 0.007% to 17.7 ± 0.21% and significant differences were observed between sites. The highest total nitrogen (N<sub>t</sub>) content was recorded in the soils of the sites that were represented by <i>Populus-Betula</i> stands (0.60 ± 0.01%). Soil acidity (pH) varied greatly, ranging from acidic (pH = 4.1) to weakly acidic (pH = 5.9). The highest value for Mg<sub>avail</sub> (205.43 ± 0.5 mg·kg<sup>-1</sup>) was noted in the soils under <i>Calamagrostis epegijos</i> (L.) Roth community and for P<sub>avail</sub> (184.07 ± 3.77) and K<sub>avail</sub> (346.19 ± 2.92 mg·kg<sup>-1</sup>) under the <i>Quercus-Pinus</i> stand. On all sites, Zn was a dominant element and its concentration ranged from 526.1 to 1060.4 mg·kg<sup>-1</sup>. Obtained results show how important it is to study the issue of vegetation changes and the formation of the landscape within an industrial city. The described results are important for the management of urban greening issues. Human influence on the disintegration and development of the natural environment is clearly visible. Due to the diversity of former mining areas and their time of creation, the studied area is one of the most important experimental areas for the determination link between vegetation and soil.</div></front></TEI><pubmed><MedlineCitation Status="PubMed-not-MEDLINE" Owner="NLM"><PMID Version="1">32679749</PMID><DateRevised><Year>2020</Year><Month>09</Month><Day>28</Day></DateRevised><Article PubModel="Electronic"><Journal><ISSN IssnType="Print">2079-7737</ISSN><JournalIssue CitedMedium="Print"><Volume>9</Volume><Issue>7</Issue><PubDate><Year>2020</Year><Month>Jul</Month><Day>15</Day></PubDate></JournalIssue><Title>Biology</Title><ISOAbbreviation>Biology (Basel)</ISOAbbreviation></Journal><ArticleTitle>Vegetation- and Environmental Changes on Non-Reclaimed Spoil Heaps in Southern Poland.</ArticleTitle><ELocationID EIdType="pii" ValidYN="Y">E164</ELocationID><ELocationID EIdType="doi" ValidYN="Y">10.3390/biology9070164</ELocationID><Abstract><AbstractText>The study focused on the changes in vegetation and soils on an undeveloped area of coal mine spoil heaps. The process of vegetation changes was evaluated on the basis of historical cartographic materials and fieldwork. Changes of vegetation in nearly 200 years are presented herein. The main purpose of this study is to present an analysis of spatio-temporal changes in vegetation and their influence on soil features. The diversity of ecological species in terms of habitat requirements, tendency of hornbeam communities formation, and the relationship between forest communities and soil features was found. The basic soil properties were examined under selected plant communities (pH, C<sub>org</sub>, N<sub>t</sub>), available forms of elements (P, K, Mg), and as plant nutrients and heavy metal occurrence (Fe, Zn, Mn, Co, Cd, Pb, Sr, Cr, Cu). The soil organic carbon (C<sub>org</sub>) content varied from 3.17 ± 0.007% to 17.7 ± 0.21% and significant differences were observed between sites. The highest total nitrogen (N<sub>t</sub>) content was recorded in the soils of the sites that were represented by <i>Populus-Betula</i> stands (0.60 ± 0.01%). Soil acidity (pH) varied greatly, ranging from acidic (pH = 4.1) to weakly acidic (pH = 5.9). The highest value for Mg<sub>avail</sub> (205.43 ± 0.5 mg·kg<sup>-1</sup>) was noted in the soils under <i>Calamagrostis epegijos</i> (L.) Roth community and for P<sub>avail</sub> (184.07 ± 3.77) and K<sub>avail</sub> (346.19 ± 2.92 mg·kg<sup>-1</sup>) under the <i>Quercus-Pinus</i> stand. On all sites, Zn was a dominant element and its concentration ranged from 526.1 to 1060.4 mg·kg<sup>-1</sup>. Obtained results show how important it is to study the issue of vegetation changes and the formation of the landscape within an industrial city. The described results are important for the management of urban greening issues. Human influence on the disintegration and development of the natural environment is clearly visible. Due to the diversity of former mining areas and their time of creation, the studied area is one of the most important experimental areas for the determination link between vegetation and soil.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Rahmonov</LastName><ForeName>Oimahmad</ForeName><Initials>O</Initials><Identifier Source="ORCID">0000-0003-4883-3784</Identifier><AffiliationInfo><Affiliation>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Krzysztofik</LastName><ForeName>Robert</ForeName><Initials>R</Initials><Identifier Source="ORCID">0000-0002-2330-8994</Identifier><AffiliationInfo><Affiliation>Institute of Social and Economic Geography and Spatial Management, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Środek</LastName><ForeName>Dorota</ForeName><Initials>D</Initials><AffiliationInfo><Affiliation>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Smolarek-Lach</LastName><ForeName>Justyna</ForeName><Initials>J</Initials><AffiliationInfo><Affiliation>Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, 41-200 Sosnowiec, Poland.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2020</Year><Month>07</Month><Day>15</Day></ArticleDate></Article><MedlineJournalInfo><Country>Switzerland</Country><MedlineTA>Biology (Basel)</MedlineTA><NlmUniqueID>101587988</NlmUniqueID><ISSNLinking>2079-7737</ISSNLinking></MedlineJournalInfo><KeywordList Owner="NOTNLM"><Keyword MajorTopicYN="N">anthropogenic soil</Keyword><Keyword MajorTopicYN="N">coal post-industrial sites</Keyword><Keyword MajorTopicYN="N">soil–vegetation link</Keyword><Keyword MajorTopicYN="N">urban forest</Keyword><Keyword MajorTopicYN="N">vegetation succession</Keyword></KeywordList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2020</Year><Month>06</Month><Day>10</Day></PubMedPubDate><PubMedPubDate PubStatus="revised"><Year>2020</Year><Month>07</Month><Day>06</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2020</Year><Month>07</Month><Day>10</Day></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2020</Year><Month>7</Month><Day>19</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2020</Year><Month>7</Month><Day>19</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2020</Year><Month>7</Month><Day>19</Day><Hour>6</Hour><Minute>1</Minute></PubMedPubDate></History><PublicationStatus>epublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">32679749</ArticleId><ArticleId IdType="pii">biology9070164</ArticleId><ArticleId IdType="doi">10.3390/biology9070164</ArticleId><ArticleId IdType="pmc">PMC7408371</ArticleId></ArticleIdList><ReferenceList><Reference><Citation>Environ Pollut. 2003;124(2):247-56</Citation><ArticleIdList><ArticleId IdType="pubmed">12713924</ArticleId></ArticleIdList></Reference><Reference><Citation>Sci Total Environ. 2006 Mar 1;356(1-3):154-64</Citation><ArticleIdList><ArticleId IdType="pubmed">15941578</ArticleId></ArticleIdList></Reference><Reference><Citation>Proc Natl Acad Sci U S A. 2007 Dec 26;104(52):20684-9</Citation><ArticleIdList><ArticleId IdType="pubmed">18093933</ArticleId></ArticleIdList></Reference><Reference><Citation>Environ Sci Pollut Res Int. 2013 Nov;20(11):7680-5</Citation><ArticleIdList><ArticleId IdType="pubmed">23436061</ArticleId></ArticleIdList></Reference><Reference><Citation>Front Microbiol. 2018 Feb 23;9:149</Citation><ArticleIdList><ArticleId IdType="pubmed">29527192</ArticleId></ArticleIdList></Reference></ReferenceList></PubmedData></pubmed><affiliations><list><country><li>Pologne</li></country></list><tree><country name="Pologne"><noRegion><name sortKey="Rahmonov, Oimahmad" sort="Rahmonov, Oimahmad" uniqKey="Rahmonov O" first="Oimahmad" last="Rahmonov">Oimahmad Rahmonov</name></noRegion><name sortKey=" Rodek, Dorota" sort=" Rodek, Dorota" uniqKey=" Rodek D" first="Dorota" last=" Rodek">Dorota Rodek</name><name sortKey="Krzysztofik, Robert" sort="Krzysztofik, Robert" uniqKey="Krzysztofik R" first="Robert" last="Krzysztofik">Robert Krzysztofik</name><name sortKey="Smolarek Lach, Justyna" sort="Smolarek Lach, Justyna" uniqKey="Smolarek Lach J" first="Justyna" last="Smolarek-Lach">Justyna Smolarek-Lach</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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