Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile
Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbat...
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description | Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbation at this location makes it an appropriate baseline site for ecosystem analysis. We measured soil bulk density, pH, soil organic C (SOC), total N, and NH₄Cl-exchangeable cations (Ca⁺², Mg⁺², K⁺, Na⁺, Al⁺³) in 0-10 and 10-40 cm depth samples from 72 soil profiles representing three vegetation zones: Fitzroya cupressoides Forest, Pilgerodendron uvifera-Tepualia stipularis Forest, and Magellanic Moorland. Fitzroya and Pilgerodendron-Tepualia Forests were indistinguishable for all measured soil characteristics (P > 0.05, Dunn's multiple comparison test on ranked data); these included very high median SOC concentrations (0-10 cm = 49.6%) and correspondingly low bulk density values (0-10 cm = 0.07). Moorland soil median values (0-10 cm) were significantly higher for bulk density (0.12) and lower for SOC (28.5%), but not for total N (Forests = 0.99%, Moorland = 0.95%), resulting in lower median C: N ratios for the moorland (Forests = 44.7; Moorland = 30.3). Across both depths and all three vegetation zones regression analysis indicated that SOC was an excellent predictor (R²= 0.93, P < 0.001) of ∑ (exchangeable Ca⁺² + Mg⁺² + K⁺ + Na⁺).Comparison with other old growth montane environments indicates that the Fitzroya and Pilgerodendron-Tepualia soil profiles are characterized by C:N ratios typical of other relatively unpolluted conifer forest soils (33.0-49.3). Soil profiles of representative polluted montane conifer forests have lower C:N ratios (16.2-23.5).Organic horizons from representative polluted montane conifer forests also retain fewer exchangeable base cations per unit SOC than are retained by organic horizons from the Cordillera de Piuchué forests. |
doi_str_mv | 10.1023/A:1004375920790 |
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(New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources) ; Johnson, A.H ; Thomas, S.M</creator><creatorcontrib>Zarin, D.J. (New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources) ; Johnson, A.H ; Thomas, S.M</creatorcontrib><description>Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbation at this location makes it an appropriate baseline site for ecosystem analysis. We measured soil bulk density, pH, soil organic C (SOC), total N, and NH₄Cl-exchangeable cations (Ca⁺², Mg⁺², K⁺, Na⁺, Al⁺³) in 0-10 and 10-40 cm depth samples from 72 soil profiles representing three vegetation zones: Fitzroya cupressoides Forest, Pilgerodendron uvifera-Tepualia stipularis Forest, and Magellanic Moorland. Fitzroya and Pilgerodendron-Tepualia Forests were indistinguishable for all measured soil characteristics (P > 0.05, Dunn's multiple comparison test on ranked data); these included very high median SOC concentrations (0-10 cm = 49.6%) and correspondingly low bulk density values (0-10 cm = 0.07). Moorland soil median values (0-10 cm) were significantly higher for bulk density (0.12) and lower for SOC (28.5%), but not for total N (Forests = 0.99%, Moorland = 0.95%), resulting in lower median C: N ratios for the moorland (Forests = 44.7; Moorland = 30.3). Across both depths and all three vegetation zones regression analysis indicated that SOC was an excellent predictor (R²= 0.93, P < 0.001) of ∑ (exchangeable Ca⁺² + Mg⁺² + K⁺ + Na⁺).Comparison with other old growth montane environments indicates that the Fitzroya and Pilgerodendron-Tepualia soil profiles are characterized by C:N ratios typical of other relatively unpolluted conifer forest soils (33.0-49.3). Soil profiles of representative polluted montane conifer forests have lower C:N ratios (16.2-23.5).Organic horizons from representative polluted montane conifer forests also retain fewer exchangeable base cations per unit SOC than are retained by organic horizons from the Cordillera de Piuchué forests.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1023/A:1004375920790</identifier><identifier>CODEN: PLSOA2</identifier><language>eng</language><publisher>Dordrecht: Kluwer Academic Publishers</publisher><subject>Acid soils ; Agronomy. Soil science and plant productions ; Air pollution ; AZOTE ; Biological and medical sciences ; BOSQUE SUBALPINO ; CARBON ; CARBONE ; CARBONO ; Cations ; Chemical, physicochemical, biochemical and biological properties ; CHILE ; CHILI ; Coniferous forests ; CUPRESSACEAE ; DISPONIBILIDAD DE NUTRIENTES ; DISPONIBILITE D'ELEMENT NUTRITIF ; Ecosystem studies ; FERTILIDAD DEL SUELO ; FERTILITE DU SOL ; Forest ecosystems ; FOREST SOILS ; Forest watersheds ; FORET SUBALPINE ; Fundamental and applied biological sciences. Psychology ; MATERIA ORGANICA DEL SUELO ; MATIERE ORGANIQUE DU SOL ; Mineral components. Ionic and exchange properties ; Montane environments ; Montane forests ; Moorlands ; NITROGEN ; NITROGENO ; NUTRIENT AVAILABILITY ; Nutrient status ; Old growth ; Old growth forests ; Organic carbon ; Organic soils ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Regression analysis ; Soil density ; SOIL FERTILITY ; Soil nutrients ; SOIL ORGANIC MATTER ; Soil pollution ; Soil profiles ; Soil science ; SOL DE FORET ; SUBALPINE FORESTS ; SUELO FORESTAL ; Temperate forests ; Vegetation</subject><ispartof>Plant and soil, 1998-04, Vol.201 (2), p.251-258</ispartof><rights>1998 Kluwer Academic Publishers</rights><rights>1998 INIST-CNRS</rights><rights>Kluwer Academic Publishers 1998</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c330t-25425a499aa998bf6637c8c632368ad8b5246fa02654ebaae64e1007ff248c203</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/42948326$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/42948326$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27924,27925,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=2370648$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Zarin, D.J. (New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources)</creatorcontrib><creatorcontrib>Johnson, A.H</creatorcontrib><creatorcontrib>Thomas, S.M</creatorcontrib><title>Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile</title><title>Plant and soil</title><description>Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbation at this location makes it an appropriate baseline site for ecosystem analysis. We measured soil bulk density, pH, soil organic C (SOC), total N, and NH₄Cl-exchangeable cations (Ca⁺², Mg⁺², K⁺, Na⁺, Al⁺³) in 0-10 and 10-40 cm depth samples from 72 soil profiles representing three vegetation zones: Fitzroya cupressoides Forest, Pilgerodendron uvifera-Tepualia stipularis Forest, and Magellanic Moorland. Fitzroya and Pilgerodendron-Tepualia Forests were indistinguishable for all measured soil characteristics (P > 0.05, Dunn's multiple comparison test on ranked data); these included very high median SOC concentrations (0-10 cm = 49.6%) and correspondingly low bulk density values (0-10 cm = 0.07). Moorland soil median values (0-10 cm) were significantly higher for bulk density (0.12) and lower for SOC (28.5%), but not for total N (Forests = 0.99%, Moorland = 0.95%), resulting in lower median C: N ratios for the moorland (Forests = 44.7; Moorland = 30.3). Across both depths and all three vegetation zones regression analysis indicated that SOC was an excellent predictor (R²= 0.93, P < 0.001) of ∑ (exchangeable Ca⁺² + Mg⁺² + K⁺ + Na⁺).Comparison with other old growth montane environments indicates that the Fitzroya and Pilgerodendron-Tepualia soil profiles are characterized by C:N ratios typical of other relatively unpolluted conifer forest soils (33.0-49.3). Soil profiles of representative polluted montane conifer forests have lower C:N ratios (16.2-23.5).Organic horizons from representative polluted montane conifer forests also retain fewer exchangeable base cations per unit SOC than are retained by organic horizons from the Cordillera de Piuchué forests.</description><subject>Acid soils</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Air pollution</subject><subject>AZOTE</subject><subject>Biological and medical sciences</subject><subject>BOSQUE SUBALPINO</subject><subject>CARBON</subject><subject>CARBONE</subject><subject>CARBONO</subject><subject>Cations</subject><subject>Chemical, physicochemical, biochemical and biological properties</subject><subject>CHILE</subject><subject>CHILI</subject><subject>Coniferous forests</subject><subject>CUPRESSACEAE</subject><subject>DISPONIBILIDAD DE NUTRIENTES</subject><subject>DISPONIBILITE D'ELEMENT NUTRITIF</subject><subject>Ecosystem studies</subject><subject>FERTILIDAD DEL SUELO</subject><subject>FERTILITE DU SOL</subject><subject>Forest ecosystems</subject><subject>FOREST SOILS</subject><subject>Forest watersheds</subject><subject>FORET SUBALPINE</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>MATERIA ORGANICA DEL SUELO</subject><subject>MATIERE ORGANIQUE DU SOL</subject><subject>Mineral components. Ionic and exchange properties</subject><subject>Montane environments</subject><subject>Montane forests</subject><subject>Moorlands</subject><subject>NITROGEN</subject><subject>NITROGENO</subject><subject>NUTRIENT AVAILABILITY</subject><subject>Nutrient status</subject><subject>Old growth</subject><subject>Old growth forests</subject><subject>Organic carbon</subject><subject>Organic soils</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>Regression analysis</subject><subject>Soil density</subject><subject>SOIL FERTILITY</subject><subject>Soil nutrients</subject><subject>SOIL ORGANIC MATTER</subject><subject>Soil pollution</subject><subject>Soil profiles</subject><subject>Soil science</subject><subject>SOL DE FORET</subject><subject>SUBALPINE FORESTS</subject><subject>SUELO FORESTAL</subject><subject>Temperate forests</subject><subject>Vegetation</subject><issn>0032-079X</issn><issn>1573-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1998</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>eNpdkM1rGzEQxUVoIW7Sc04BEUpP2WRW0uqjt2D6ETDNIS30toxlyZZZS6kkE_LfV05CCz0NM-_H470h5KyHqx4Yv7751AMIrgbDQBk4IrN-ULwbgMs3ZAbAWdfuv47Ju1K2cNh7OSPxPoWJprzGGCy1mJcpUowrGvc1BxcrLRXrvtAQaZpW3Tqnx7qhuxQrRkdtisG7nBrgU3al0kesLpeNW5VLelsmpPNNmJK7fJ7ulLz1OBX3_nWekJ9fPv-Yf-sWd19v5zeLznIOtWODYAMKYxCN0UsvJVdWW8kZlxpXejkwIT0Ck4NwS0QnhWvtlfdMaMuAn5CPL74POf3et1zjLhTrpqmFbmHHXvVaKziAF_-B27TPsWUb1dD-CtqYBn14hbBYnHzGaEMZH3LYYX4aGVcghW7Y-Qu2LTXlv7JgpolM_tM9phHXuVl8X_StIMChGf8DDbiHRg</recordid><startdate>19980401</startdate><enddate>19980401</enddate><creator>Zarin, D.J. (New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources)</creator><creator>Johnson, A.H</creator><creator>Thomas, S.M</creator><general>Kluwer Academic Publishers</general><general>Springer</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>IQODW</scope><scope>3V.</scope><scope>7SN</scope><scope>7ST</scope><scope>7T7</scope><scope>7X2</scope><scope>88A</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>FR3</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>LK8</scope><scope>M0K</scope><scope>M7P</scope><scope>P64</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>RC3</scope><scope>SOI</scope></search><sort><creationdate>19980401</creationdate><title>Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile</title><author>Zarin, D.J. (New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources) ; Johnson, A.H ; Thomas, S.M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c330t-25425a499aa998bf6637c8c632368ad8b5246fa02654ebaae64e1007ff248c203</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1998</creationdate><topic>Acid soils</topic><topic>Agronomy. Soil science and plant productions</topic><topic>Air pollution</topic><topic>AZOTE</topic><topic>Biological and medical sciences</topic><topic>BOSQUE SUBALPINO</topic><topic>CARBON</topic><topic>CARBONE</topic><topic>CARBONO</topic><topic>Cations</topic><topic>Chemical, physicochemical, biochemical and biological properties</topic><topic>CHILE</topic><topic>CHILI</topic><topic>Coniferous forests</topic><topic>CUPRESSACEAE</topic><topic>DISPONIBILIDAD DE NUTRIENTES</topic><topic>DISPONIBILITE D'ELEMENT NUTRITIF</topic><topic>Ecosystem studies</topic><topic>FERTILIDAD DEL SUELO</topic><topic>FERTILITE DU SOL</topic><topic>Forest ecosystems</topic><topic>FOREST SOILS</topic><topic>Forest watersheds</topic><topic>FORET SUBALPINE</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>MATERIA ORGANICA DEL SUELO</topic><topic>MATIERE ORGANIQUE DU SOL</topic><topic>Mineral components. Ionic and exchange properties</topic><topic>Montane environments</topic><topic>Montane forests</topic><topic>Moorlands</topic><topic>NITROGEN</topic><topic>NITROGENO</topic><topic>NUTRIENT AVAILABILITY</topic><topic>Nutrient status</topic><topic>Old growth</topic><topic>Old growth forests</topic><topic>Organic carbon</topic><topic>Organic soils</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>Regression analysis</topic><topic>Soil density</topic><topic>SOIL FERTILITY</topic><topic>Soil nutrients</topic><topic>SOIL ORGANIC MATTER</topic><topic>Soil pollution</topic><topic>Soil profiles</topic><topic>Soil science</topic><topic>SOL DE FORET</topic><topic>SUBALPINE FORESTS</topic><topic>SUELO FORESTAL</topic><topic>Temperate forests</topic><topic>Vegetation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zarin, D.J. (New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources)</creatorcontrib><creatorcontrib>Johnson, A.H</creatorcontrib><creatorcontrib>Thomas, S.M</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Agricultural Science Collection</collection><collection>Biology 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>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Genetics Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Plant and soil</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zarin, D.J. (New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources)</au><au>Johnson, A.H</au><au>Thomas, S.M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile</atitle><jtitle>Plant and soil</jtitle><date>1998-04-01</date><risdate>1998</risdate><volume>201</volume><issue>2</issue><spage>251</spage><epage>258</epage><pages>251-258</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><coden>PLSOA2</coden><abstract>Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbation at this location makes it an appropriate baseline site for ecosystem analysis. We measured soil bulk density, pH, soil organic C (SOC), total N, and NH₄Cl-exchangeable cations (Ca⁺², Mg⁺², K⁺, Na⁺, Al⁺³) in 0-10 and 10-40 cm depth samples from 72 soil profiles representing three vegetation zones: Fitzroya cupressoides Forest, Pilgerodendron uvifera-Tepualia stipularis Forest, and Magellanic Moorland. Fitzroya and Pilgerodendron-Tepualia Forests were indistinguishable for all measured soil characteristics (P > 0.05, Dunn's multiple comparison test on ranked data); these included very high median SOC concentrations (0-10 cm = 49.6%) and correspondingly low bulk density values (0-10 cm = 0.07). Moorland soil median values (0-10 cm) were significantly higher for bulk density (0.12) and lower for SOC (28.5%), but not for total N (Forests = 0.99%, Moorland = 0.95%), resulting in lower median C: N ratios for the moorland (Forests = 44.7; Moorland = 30.3). Across both depths and all three vegetation zones regression analysis indicated that SOC was an excellent predictor (R²= 0.93, P < 0.001) of ∑ (exchangeable Ca⁺² + Mg⁺² + K⁺ + Na⁺).Comparison with other old growth montane environments indicates that the Fitzroya and Pilgerodendron-Tepualia soil profiles are characterized by C:N ratios typical of other relatively unpolluted conifer forest soils (33.0-49.3). Soil profiles of representative polluted montane conifer forests have lower C:N ratios (16.2-23.5).Organic horizons from representative polluted montane conifer forests also retain fewer exchangeable base cations per unit SOC than are retained by organic horizons from the Cordillera de Piuchué forests.</abstract><cop>Dordrecht</cop><pub>Kluwer Academic Publishers</pub><doi>10.1023/A:1004375920790</doi><tpages>8</tpages></addata></record> |
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language | eng |
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subjects | Acid soils Agronomy. Soil science and plant productions Air pollution AZOTE Biological and medical sciences BOSQUE SUBALPINO CARBON CARBONE CARBONO Cations Chemical, physicochemical, biochemical and biological properties CHILE CHILI Coniferous forests CUPRESSACEAE DISPONIBILIDAD DE NUTRIENTES DISPONIBILITE D'ELEMENT NUTRITIF Ecosystem studies FERTILIDAD DEL SUELO FERTILITE DU SOL Forest ecosystems FOREST SOILS Forest watersheds FORET SUBALPINE Fundamental and applied biological sciences. Psychology MATERIA ORGANICA DEL SUELO MATIERE ORGANIQUE DU SOL Mineral components. Ionic and exchange properties Montane environments Montane forests Moorlands NITROGEN NITROGENO NUTRIENT AVAILABILITY Nutrient status Old growth Old growth forests Organic carbon Organic soils Physics, chemistry, biochemistry and biology of agricultural and forest soils Regression analysis Soil density SOIL FERTILITY Soil nutrients SOIL ORGANIC MATTER Soil pollution Soil profiles Soil science SOL DE FORET SUBALPINE FORESTS SUELO FORESTAL Temperate forests Vegetation |
title | Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile |
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