Interrelationship between soil depth and soil properties of Pieniny National Park forest (Poland)
The purpose of this research was to investigate the relationship between soil biota such as microbial activity, soil fauna (e.g., earthworms and enchytraeids), and soil physical and chemical properties. The study area was located in Pieniny National Park (PNP) in the Carpathian Mountains in southern...
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| Veröffentlicht in: | Journal of mountain science 2019-07, Vol.16 (7), p.1534-1545 |
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| creator | Sokołowska, Justyna Józefowska, Agnieszka Woźnica, Karolina Zaleski, Tomasz |
| description | The purpose of this research was to investigate the relationship between soil biota such as microbial activity, soil fauna (e.g., earthworms and enchytraeids), and soil physical and chemical properties. The study area was located in Pieniny National Park (PNP) in the Carpathian Mountains in southern Poland. Soil samples were collected from six forest monitoring areas of PNP from two soil layers (at 0–15 cm and 15–30 cm down, respectively). The investigated soils were classified to eutric cambisols and had silt or silt loam soil texture. Upon analysis, soil aggregate stability index was connected with other physical, chemical, and biological soil properties. It was noted that the stability index of 3 mm to 5 mm soil aggregates influenced pH and dissolved organic carbon. The stability index of 2 mm to 3 mm soil aggregates was positively correlated with dissolved organic carbon, soil moisture, microbial biomass carbon, total organic carbon, total nitrogen, and enchytraeid density, and negatively correlated with bulk density, particle density, porosity, and permanent wilting point. The stability index of 1 mm to 2 mm soil aggregates was positively correlated with total nitrogen, enchytraeid and earthworm density and negatively correlated with particle density, porosity, and permanent wilting point. The study has shown what factors create a stable soil structure in the forest soils of PNP. |
| doi_str_mv | 10.1007/s11629-019-5441-8 |
| format | Article |
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The study area was located in Pieniny National Park (PNP) in the Carpathian Mountains in southern Poland. Soil samples were collected from six forest monitoring areas of PNP from two soil layers (at 0–15 cm and 15–30 cm down, respectively). The investigated soils were classified to eutric cambisols and had silt or silt loam soil texture. Upon analysis, soil aggregate stability index was connected with other physical, chemical, and biological soil properties. It was noted that the stability index of 3 mm to 5 mm soil aggregates influenced pH and dissolved organic carbon. The stability index of 2 mm to 3 mm soil aggregates was positively correlated with dissolved organic carbon, soil moisture, microbial biomass carbon, total organic carbon, total nitrogen, and enchytraeid density, and negatively correlated with bulk density, particle density, porosity, and permanent wilting point. The stability index of 1 mm to 2 mm soil aggregates was positively correlated with total nitrogen, enchytraeid and earthworm density and negatively correlated with particle density, porosity, and permanent wilting point. The study has shown what factors create a stable soil structure in the forest soils of PNP.</description><identifier>ISSN: 1672-6316</identifier><identifier>EISSN: 1993-0321</identifier><identifier>EISSN: 1008-2786</identifier><identifier>DOI: 10.1007/s11629-019-5441-8</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Aggregates ; Biological activity ; Biological properties ; Biota ; Bulk density ; Carbon ; Chemical properties ; Chemicophysical properties ; Density ; Dissolved organic carbon ; Earth and Environmental Science ; Earth Sciences ; Ecology ; Environment ; Forest soils ; Forests ; Geography ; Loam ; Loam soils ; Microbial activity ; Microorganisms ; Mountains ; National forests ; National parks ; Nitrogen ; Organic chemistry ; Organic soils ; Particle density (concentration) ; Porosity ; Silt ; Silt loam ; Soil aggregates ; Soil analysis ; Soil chemistry ; Soil classification ; Soil depth ; Soil fauna ; Soil investigations ; Soil layers ; Soil moisture ; Soil porosity ; Soil properties ; Soil stability ; Soil structure ; Soil texture ; Stability analysis ; Texture ; Total organic carbon ; Wilting ; Wilting point</subject><ispartof>Journal of mountain science, 2019-07, Vol.16 (7), p.1534-1545</ispartof><rights>Science Press, Institute of Mountain Hazards and Environment, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2019</rights><rights>Science Press, Institute of Mountain Hazards and Environment, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2019.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-32db5c6e5ce6a37987c33a1172189bc8e024377b57b93e431d78fbe7fa108a263</citedby><cites>FETCH-LOGICAL-c316t-32db5c6e5ce6a37987c33a1172189bc8e024377b57b93e431d78fbe7fa108a263</cites><orcidid>0000-0002-9785-3784 ; 0000-0003-4922-2037 ; 0000-0003-1255-4150 ; 0000-0002-6816-9342</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11629-019-5441-8$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11629-019-5441-8$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Sokołowska, Justyna</creatorcontrib><creatorcontrib>Józefowska, Agnieszka</creatorcontrib><creatorcontrib>Woźnica, Karolina</creatorcontrib><creatorcontrib>Zaleski, Tomasz</creatorcontrib><title>Interrelationship between soil depth and soil properties of Pieniny National Park forest (Poland)</title><title>Journal of mountain science</title><addtitle>J. Mt. Sci</addtitle><description>The purpose of this research was to investigate the relationship between soil biota such as microbial activity, soil fauna (e.g., earthworms and enchytraeids), and soil physical and chemical properties. The study area was located in Pieniny National Park (PNP) in the Carpathian Mountains in southern Poland. Soil samples were collected from six forest monitoring areas of PNP from two soil layers (at 0–15 cm and 15–30 cm down, respectively). The investigated soils were classified to eutric cambisols and had silt or silt loam soil texture. Upon analysis, soil aggregate stability index was connected with other physical, chemical, and biological soil properties. It was noted that the stability index of 3 mm to 5 mm soil aggregates influenced pH and dissolved organic carbon. The stability index of 2 mm to 3 mm soil aggregates was positively correlated with dissolved organic carbon, soil moisture, microbial biomass carbon, total organic carbon, total nitrogen, and enchytraeid density, and negatively correlated with bulk density, particle density, porosity, and permanent wilting point. The stability index of 1 mm to 2 mm soil aggregates was positively correlated with total nitrogen, enchytraeid and earthworm density and negatively correlated with particle density, porosity, and permanent wilting point. The study has shown what factors create a stable soil structure in the forest soils of PNP.</description><subject>Aggregates</subject><subject>Biological activity</subject><subject>Biological properties</subject><subject>Biota</subject><subject>Bulk density</subject><subject>Carbon</subject><subject>Chemical properties</subject><subject>Chemicophysical properties</subject><subject>Density</subject><subject>Dissolved organic carbon</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Environment</subject><subject>Forest soils</subject><subject>Forests</subject><subject>Geography</subject><subject>Loam</subject><subject>Loam soils</subject><subject>Microbial activity</subject><subject>Microorganisms</subject><subject>Mountains</subject><subject>National forests</subject><subject>National parks</subject><subject>Nitrogen</subject><subject>Organic chemistry</subject><subject>Organic soils</subject><subject>Particle density (concentration)</subject><subject>Porosity</subject><subject>Silt</subject><subject>Silt loam</subject><subject>Soil aggregates</subject><subject>Soil analysis</subject><subject>Soil chemistry</subject><subject>Soil classification</subject><subject>Soil depth</subject><subject>Soil fauna</subject><subject>Soil investigations</subject><subject>Soil layers</subject><subject>Soil moisture</subject><subject>Soil porosity</subject><subject>Soil properties</subject><subject>Soil stability</subject><subject>Soil structure</subject><subject>Soil texture</subject><subject>Stability analysis</subject><subject>Texture</subject><subject>Total organic carbon</subject><subject>Wilting</subject><subject>Wilting point</subject><issn>1672-6316</issn><issn>1993-0321</issn><issn>1008-2786</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1kD1PwzAQhi0EEqXwA9gsscBg8NmN7Yyo4qNSBR1gtpzkQlNCHOxUqP8elyAxMd2d9D6nRy8h58CvgXN9EwGUyBmHnGWzGTBzQCaQ55JxKeAw7UoLpiSoY3IS44ZzpXMDE-IW3YAhYOuGxndx3fS0wOELsaPRNy2tsB_W1HXVePbB9xiGBiP1NV012DXdjj79wK6lKxfeae0DxoFernybuKtTclS7NuLZ75yS1_u7l_kjWz4_LOa3S1Ymq4FJURVZqTArUTmZ5HQppQPQAkxelAa5mEmti0wXucSZhEqbukBdO-DGCSWn5GL8mxw_t8nAbvw2JKtohciE1jwzJqVgTJXBxxiwtn1oPlzYWeB236Qdm7SpSbtv0u4ZMTIxZbs3DH-f_4e-AQf7dmk</recordid><startdate>20190701</startdate><enddate>20190701</enddate><creator>Sokołowska, Justyna</creator><creator>Józefowska, Agnieszka</creator><creator>Woźnica, Karolina</creator><creator>Zaleski, Tomasz</creator><general>Science Press</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-9785-3784</orcidid><orcidid>https://orcid.org/0000-0003-4922-2037</orcidid><orcidid>https://orcid.org/0000-0003-1255-4150</orcidid><orcidid>https://orcid.org/0000-0002-6816-9342</orcidid></search><sort><creationdate>20190701</creationdate><title>Interrelationship between soil depth and soil properties of Pieniny National Park forest (Poland)</title><author>Sokołowska, Justyna ; Józefowska, Agnieszka ; Woźnica, Karolina ; Zaleski, Tomasz</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c316t-32db5c6e5ce6a37987c33a1172189bc8e024377b57b93e431d78fbe7fa108a263</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Aggregates</topic><topic>Biological activity</topic><topic>Biological properties</topic><topic>Biota</topic><topic>Bulk density</topic><topic>Carbon</topic><topic>Chemical properties</topic><topic>Chemicophysical properties</topic><topic>Density</topic><topic>Dissolved organic carbon</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecology</topic><topic>Environment</topic><topic>Forest soils</topic><topic>Forests</topic><topic>Geography</topic><topic>Loam</topic><topic>Loam soils</topic><topic>Microbial activity</topic><topic>Microorganisms</topic><topic>Mountains</topic><topic>National forests</topic><topic>National parks</topic><topic>Nitrogen</topic><topic>Organic chemistry</topic><topic>Organic soils</topic><topic>Particle density (concentration)</topic><topic>Porosity</topic><topic>Silt</topic><topic>Silt loam</topic><topic>Soil aggregates</topic><topic>Soil analysis</topic><topic>Soil chemistry</topic><topic>Soil classification</topic><topic>Soil depth</topic><topic>Soil fauna</topic><topic>Soil investigations</topic><topic>Soil layers</topic><topic>Soil moisture</topic><topic>Soil porosity</topic><topic>Soil properties</topic><topic>Soil stability</topic><topic>Soil structure</topic><topic>Soil texture</topic><topic>Stability analysis</topic><topic>Texture</topic><topic>Total organic carbon</topic><topic>Wilting</topic><topic>Wilting point</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sokołowska, Justyna</creatorcontrib><creatorcontrib>Józefowska, Agnieszka</creatorcontrib><creatorcontrib>Woźnica, Karolina</creatorcontrib><creatorcontrib>Zaleski, Tomasz</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Journal of mountain science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sokołowska, Justyna</au><au>Józefowska, Agnieszka</au><au>Woźnica, Karolina</au><au>Zaleski, Tomasz</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Interrelationship between soil depth and soil properties of Pieniny National Park forest (Poland)</atitle><jtitle>Journal of mountain science</jtitle><stitle>J. Mt. Sci</stitle><date>2019-07-01</date><risdate>2019</risdate><volume>16</volume><issue>7</issue><spage>1534</spage><epage>1545</epage><pages>1534-1545</pages><issn>1672-6316</issn><eissn>1993-0321</eissn><eissn>1008-2786</eissn><abstract>The purpose of this research was to investigate the relationship between soil biota such as microbial activity, soil fauna (e.g., earthworms and enchytraeids), and soil physical and chemical properties. The study area was located in Pieniny National Park (PNP) in the Carpathian Mountains in southern Poland. Soil samples were collected from six forest monitoring areas of PNP from two soil layers (at 0–15 cm and 15–30 cm down, respectively). The investigated soils were classified to eutric cambisols and had silt or silt loam soil texture. Upon analysis, soil aggregate stability index was connected with other physical, chemical, and biological soil properties. It was noted that the stability index of 3 mm to 5 mm soil aggregates influenced pH and dissolved organic carbon. The stability index of 2 mm to 3 mm soil aggregates was positively correlated with dissolved organic carbon, soil moisture, microbial biomass carbon, total organic carbon, total nitrogen, and enchytraeid density, and negatively correlated with bulk density, particle density, porosity, and permanent wilting point. The stability index of 1 mm to 2 mm soil aggregates was positively correlated with total nitrogen, enchytraeid and earthworm density and negatively correlated with particle density, porosity, and permanent wilting point. The study has shown what factors create a stable soil structure in the forest soils of PNP.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11629-019-5441-8</doi><tpages>12</tpages><orcidid>https://orcid.org/0000-0002-9785-3784</orcidid><orcidid>https://orcid.org/0000-0003-4922-2037</orcidid><orcidid>https://orcid.org/0000-0003-1255-4150</orcidid><orcidid>https://orcid.org/0000-0002-6816-9342</orcidid></addata></record> |
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| ispartof | Journal of mountain science, 2019-07, Vol.16 (7), p.1534-1545 |
| issn | 1672-6316 1993-0321 1008-2786 |
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| source | Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings |
| subjects | Aggregates Biological activity Biological properties Biota Bulk density Carbon Chemical properties Chemicophysical properties Density Dissolved organic carbon Earth and Environmental Science Earth Sciences Ecology Environment Forest soils Forests Geography Loam Loam soils Microbial activity Microorganisms Mountains National forests National parks Nitrogen Organic chemistry Organic soils Particle density (concentration) Porosity Silt Silt loam Soil aggregates Soil analysis Soil chemistry Soil classification Soil depth Soil fauna Soil investigations Soil layers Soil moisture Soil porosity Soil properties Soil stability Soil structure Soil texture Stability analysis Texture Total organic carbon Wilting Wilting point |
| title | Interrelationship between soil depth and soil properties of Pieniny National Park forest (Poland) |
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