Soil processes related to organic matter modifications following Douglas-fir mature reforestation
The aim of the study was to analyse the pedological, chemical and biochemical properties of soil in order to assess the effect of plant cover species (chestnut, Douglas-fir and mixed vegetation) on soil processes. The selected area under Douglas-fir reforestation was homogeneous for climate, morphol...
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| Veröffentlicht in: | Biology and fertility of soils 2015-04, Vol.51 (3), p.277-287 |
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| creator | Falsone, G Marinari, S Vittori Antisari, L Vianello, G |
| description | The aim of the study was to analyse the pedological, chemical and biochemical properties of soil in order to assess the effect of plant cover species (chestnut, Douglas-fir and mixed vegetation) on soil processes. The selected area under Douglas-fir reforestation was homogeneous for climate, morphology and parent material. The study involved three soils: under chestnut forest (CS), Douglas-fir reforestation (DF) and the transition zone (T). A soil profile differentiation occurred after 50 years of Douglas-fir plantation. The thickness of soil horizons at the surface varied, and the OH horizon in T site was fourfold thicker than that in DF site. The A1 mineral horizon in T site was also thicker than that in DF site. The Munsell value of mineral horizons was significantly lower in DF than CS site. Morphological differences (thickness and colour) probably reflect soil organic matter quality changes: in DF higher values of humification index were found in surface layers (OF/OH or OH and A1) and lower in deep organo-mineral and transition horizons (A2 and BA or AB) with respect to CS site. Also, a slight increase of weathering process was observed under Douglas-fir reforestation. The morphological, chemical and biological properties of soil were effective to assess the impact of various vegetation types on soil organic matter properties related to pedogenetic process. The various methodological approaches allow studying soil processes using a small–medium spatial scale sampling scheme. |
| doi_str_mv | 10.1007/s00374-014-0971-2 |
| format | Article |
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The selected area under Douglas-fir reforestation was homogeneous for climate, morphology and parent material. The study involved three soils: under chestnut forest (CS), Douglas-fir reforestation (DF) and the transition zone (T). A soil profile differentiation occurred after 50 years of Douglas-fir plantation. The thickness of soil horizons at the surface varied, and the OH horizon in T site was fourfold thicker than that in DF site. The A1 mineral horizon in T site was also thicker than that in DF site. The Munsell value of mineral horizons was significantly lower in DF than CS site. Morphological differences (thickness and colour) probably reflect soil organic matter quality changes: in DF higher values of humification index were found in surface layers (OF/OH or OH and A1) and lower in deep organo-mineral and transition horizons (A2 and BA or AB) with respect to CS site. Also, a slight increase of weathering process was observed under Douglas-fir reforestation. The morphological, chemical and biological properties of soil were effective to assess the impact of various vegetation types on soil organic matter properties related to pedogenetic process. The various methodological approaches allow studying soil processes using a small–medium spatial scale sampling scheme.</description><identifier>ISSN: 0178-2762</identifier><identifier>EISSN: 1432-0789</identifier><identifier>DOI: 10.1007/s00374-014-0971-2</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer-Verlag</publisher><subject>Agriculture ; Biogeochemistry ; Biological properties ; Biomedical and Life Sciences ; Castanea ; Forest soils ; Humification ; Life Sciences ; Organic matter ; Original Paper ; Pseudotsuga menziesii ; Reforestation ; soil chemical properties ; soil formation ; Soil horizons ; Soil microorganisms ; Soil organic matter ; Soil profiles ; Soil properties ; Soil Science & Conservation ; Transition zone ; Vegetation ; vegetation types</subject><ispartof>Biology and fertility of soils, 2015-04, Vol.51 (3), p.277-287</ispartof><rights>Springer-Verlag Berlin Heidelberg 2014</rights><rights>Springer-Verlag Berlin Heidelberg 2015</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c443t-320893e5fc660e94aada548ddf354d42f3ea3919d6eb2acf87869aca252643b3</citedby><cites>FETCH-LOGICAL-c443t-320893e5fc660e94aada548ddf354d42f3ea3919d6eb2acf87869aca252643b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00374-014-0971-2$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00374-014-0971-2$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>315,781,785,27929,27930,41493,42562,51324</link.rule.ids></links><search><creatorcontrib>Falsone, G</creatorcontrib><creatorcontrib>Marinari, S</creatorcontrib><creatorcontrib>Vittori Antisari, L</creatorcontrib><creatorcontrib>Vianello, G</creatorcontrib><title>Soil processes related to organic matter modifications following Douglas-fir mature reforestation</title><title>Biology and fertility of soils</title><addtitle>Biol Fertil Soils</addtitle><description>The aim of the study was to analyse the pedological, chemical and biochemical properties of soil in order to assess the effect of plant cover species (chestnut, Douglas-fir and mixed vegetation) on soil processes. The selected area under Douglas-fir reforestation was homogeneous for climate, morphology and parent material. The study involved three soils: under chestnut forest (CS), Douglas-fir reforestation (DF) and the transition zone (T). A soil profile differentiation occurred after 50 years of Douglas-fir plantation. The thickness of soil horizons at the surface varied, and the OH horizon in T site was fourfold thicker than that in DF site. The A1 mineral horizon in T site was also thicker than that in DF site. The Munsell value of mineral horizons was significantly lower in DF than CS site. Morphological differences (thickness and colour) probably reflect soil organic matter quality changes: in DF higher values of humification index were found in surface layers (OF/OH or OH and A1) and lower in deep organo-mineral and transition horizons (A2 and BA or AB) with respect to CS site. Also, a slight increase of weathering process was observed under Douglas-fir reforestation. 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The various methodological approaches allow studying soil processes using a small–medium spatial scale sampling scheme.</description><subject>Agriculture</subject><subject>Biogeochemistry</subject><subject>Biological properties</subject><subject>Biomedical and Life Sciences</subject><subject>Castanea</subject><subject>Forest soils</subject><subject>Humification</subject><subject>Life Sciences</subject><subject>Organic matter</subject><subject>Original Paper</subject><subject>Pseudotsuga menziesii</subject><subject>Reforestation</subject><subject>soil chemical properties</subject><subject>soil formation</subject><subject>Soil horizons</subject><subject>Soil microorganisms</subject><subject>Soil organic matter</subject><subject>Soil profiles</subject><subject>Soil properties</subject><subject>Soil Science & Conservation</subject><subject>Transition zone</subject><subject>Vegetation</subject><subject>vegetation types</subject><issn>0178-2762</issn><issn>1432-0789</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</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>eNp9kT1v2zAQhomiAep8_IBOFZAli9Ljh0hxDNy0KWAgg52ZOFOkQEMWHVJC0H8fuupQdOhwuOV537t7j5DPFO4pgPqaAbgSNdBSWtGafSArKjirQbX6I1kBVW3NlGSfyGXOBwDatFSvCG5jGKpTitbl7HKV3ICT66opVjH1OAZbHXGaXKqOsQs-WJxCHHPl4zDEtzD21bc49wPm2od0RufkiomPyeXpN3tNLjwO2d386Vdk9_1xt36qN88_fq4fNrUVgk81Z9Bq7hpvpQSnBWKHjWi7zvNGdIJ57pBrqjvp9gytb1UrNVpkDZOC7_kVuVtsyy2vcxlujiFbNww4ujhnQ6XiXIPkTUFv_0EPcU5jWa5QkjWq7KIKRRfKpphzOcmcUjhi-mUomHPmZsnclMzNOXPDioYtmlzYsXfpL-f_iL4sIo_RYJ9CNi9bVh4EwEC0XPJ3QcGOjw</recordid><startdate>20150401</startdate><enddate>20150401</enddate><creator>Falsone, G</creator><creator>Marinari, S</creator><creator>Vittori Antisari, L</creator><creator>Vianello, G</creator><general>Springer-Verlag</general><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SN</scope><scope>7T7</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>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H95</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>LK8</scope><scope>M0K</scope><scope>M2P</scope><scope>M7P</scope><scope>P64</scope><scope>PATMY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7ST</scope><scope>7U6</scope></search><sort><creationdate>20150401</creationdate><title>Soil processes related to organic matter modifications following Douglas-fir mature reforestation</title><author>Falsone, G ; Marinari, S ; Vittori Antisari, L ; Vianello, G</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c443t-320893e5fc660e94aada548ddf354d42f3ea3919d6eb2acf87869aca252643b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Agriculture</topic><topic>Biogeochemistry</topic><topic>Biological properties</topic><topic>Biomedical and Life Sciences</topic><topic>Castanea</topic><topic>Forest soils</topic><topic>Humification</topic><topic>Life Sciences</topic><topic>Organic matter</topic><topic>Original Paper</topic><topic>Pseudotsuga menziesii</topic><topic>Reforestation</topic><topic>soil chemical properties</topic><topic>soil formation</topic><topic>Soil horizons</topic><topic>Soil microorganisms</topic><topic>Soil organic matter</topic><topic>Soil profiles</topic><topic>Soil properties</topic><topic>Soil Science & Conservation</topic><topic>Transition zone</topic><topic>Vegetation</topic><topic>vegetation types</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Falsone, G</creatorcontrib><creatorcontrib>Marinari, S</creatorcontrib><creatorcontrib>Vittori Antisari, L</creatorcontrib><creatorcontrib>Vianello, G</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</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 Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>Proquest Central</collection><collection>Natural 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>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Science Database</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environmental 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><collection>Sustainability Science Abstracts</collection><jtitle>Biology and fertility of soils</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Falsone, G</au><au>Marinari, S</au><au>Vittori Antisari, L</au><au>Vianello, G</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soil processes related to organic matter modifications following Douglas-fir mature reforestation</atitle><jtitle>Biology and fertility of soils</jtitle><stitle>Biol Fertil Soils</stitle><date>2015-04-01</date><risdate>2015</risdate><volume>51</volume><issue>3</issue><spage>277</spage><epage>287</epage><pages>277-287</pages><issn>0178-2762</issn><eissn>1432-0789</eissn><abstract>The aim of the study was to analyse the pedological, chemical and biochemical properties of soil in order to assess the effect of plant cover species (chestnut, Douglas-fir and mixed vegetation) on soil processes. The selected area under Douglas-fir reforestation was homogeneous for climate, morphology and parent material. The study involved three soils: under chestnut forest (CS), Douglas-fir reforestation (DF) and the transition zone (T). A soil profile differentiation occurred after 50 years of Douglas-fir plantation. The thickness of soil horizons at the surface varied, and the OH horizon in T site was fourfold thicker than that in DF site. The A1 mineral horizon in T site was also thicker than that in DF site. The Munsell value of mineral horizons was significantly lower in DF than CS site. Morphological differences (thickness and colour) probably reflect soil organic matter quality changes: in DF higher values of humification index were found in surface layers (OF/OH or OH and A1) and lower in deep organo-mineral and transition horizons (A2 and BA or AB) with respect to CS site. Also, a slight increase of weathering process was observed under Douglas-fir reforestation. 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| subjects | Agriculture Biogeochemistry Biological properties Biomedical and Life Sciences Castanea Forest soils Humification Life Sciences Organic matter Original Paper Pseudotsuga menziesii Reforestation soil chemical properties soil formation Soil horizons Soil microorganisms Soil organic matter Soil profiles Soil properties Soil Science & Conservation Transition zone Vegetation vegetation types |
| title | Soil processes related to organic matter modifications following Douglas-fir mature reforestation |
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