Distribution of zinc and lead fractions within a forest spodosol
Soil processes play a critical role in the fate of trace metals in forest ecosystems. To explore the nature of soil-trace metal interactions, we estimated five fractions of Zn and Pb in Spodosols at the Hubbard Brook Experimental Forest in central New Hampshire: (i) soluble + exchangeable (EX); (ii)...
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| description | Soil processes play a critical role in the fate of trace metals in forest ecosystems. To explore the nature of soil-trace metal interactions, we estimated five fractions of Zn and Pb in Spodosols at the Hubbard Brook Experimental Forest in central New Hampshire: (i) soluble + exchangeable (EX); (ii) inorganically bound (IB); (iii) organically bound (ORG); (iv) amorphous oxide bound (AMOX); and (v) mineral lattice, or residual (RES). Organic matter is a critical factor in trace metal fractionation in Hubbard Brook soils; loss-on-ignition was strongly correlated to EX Zn (r = 0.91) and Pb (r = 0.85), and ORG Zn (r = 0.57) and Pb (r = 0.89). The Oa horizon accounted for only 1.9% of the soil mass above the C horizon, but contained 23% and 77%, respectively, of the EX Zn and Pb in the soil. Lead was more tightly held in the soil than Zn; the percentage of total metal in the EX fraction was greater for Zn than Pb in all horizons. Through biocycling, Zn is returned to the forest floor, helping to maintain labile pools in upper soil horizons. Nevertheless, the EX Zn pool (6.03 kg ha-1) is insufficient to replace the pool of Zn in aboveground tissues (6.87 kg ha-1). Lead, not a nutrient, has accumulated in the soil due to the combustion of leaded gasoline. Lead leached from the O horizon between 1926 and 1991 can account for 30% of the EX + IB + ORG Pb, or 14% of the labile Pb in the mineral soil |
| doi_str_mv | 10.2136/sssaj1998.03615995006200030035x |
| format | Article |
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(Syracuse Univ., Syracuse, NY.) ; Petras, R.J</creator><creatorcontrib>Johnson, C.E. (Syracuse Univ., Syracuse, NY.) ; Petras, R.J</creatorcontrib><description>Soil processes play a critical role in the fate of trace metals in forest ecosystems. To explore the nature of soil-trace metal interactions, we estimated five fractions of Zn and Pb in Spodosols at the Hubbard Brook Experimental Forest in central New Hampshire: (i) soluble + exchangeable (EX); (ii) inorganically bound (IB); (iii) organically bound (ORG); (iv) amorphous oxide bound (AMOX); and (v) mineral lattice, or residual (RES). Organic matter is a critical factor in trace metal fractionation in Hubbard Brook soils; loss-on-ignition was strongly correlated to EX Zn (r = 0.91) and Pb (r = 0.85), and ORG Zn (r = 0.57) and Pb (r = 0.89). The Oa horizon accounted for only 1.9% of the soil mass above the C horizon, but contained 23% and 77%, respectively, of the EX Zn and Pb in the soil. Lead was more tightly held in the soil than Zn; the percentage of total metal in the EX fraction was greater for Zn than Pb in all horizons. Through biocycling, Zn is returned to the forest floor, helping to maintain labile pools in upper soil horizons. Nevertheless, the EX Zn pool (6.03 kg ha-1) is insufficient to replace the pool of Zn in aboveground tissues (6.87 kg ha-1). Lead, not a nutrient, has accumulated in the soil due to the combustion of leaded gasoline. Lead leached from the O horizon between 1926 and 1991 can account for 30% of the EX + IB + ORG Pb, or 14% of the labile Pb in the mineral soil</description><identifier>ISSN: 0361-5995</identifier><identifier>EISSN: 1435-0661</identifier><identifier>DOI: 10.2136/sssaj1998.03615995006200030035x</identifier><identifier>CODEN: SSSJD4</identifier><language>eng</language><publisher>Madison, WI: Soil Science Society of America</publisher><subject>Agronomy. Soil science and plant productions ; AIR POLLUTION ; Animal, plant and microbial ecology ; Applied ecology ; Applied sciences ; BIOAVAILABILITY ; BIODISPONIBILIDAD ; BIODISPONIBILITE ; Biological and medical sciences ; Biological and physicochemical properties of pollutants. Interaction in the soil ; CICLO BIOGEOQUIMICO ; CINC ; CYCLE BIOGEOCHIMIQUE ; CYCLING ; Earth sciences ; Earth, ocean, space ; ECOSISTEMA ; ECOSYSTEME ; ECOSYSTEMS ; Ecotoxicology, biological effects of pollution ; Engineering and environment geology. Geothermics ; Exact sciences and technology ; Forest ecosystems ; FOREST SOILS ; Forests ; FRACCIONAMIENTO ; FRACTIONATION ; FRACTIONNEMENT ; Fundamental and applied biological sciences. Psychology ; LEAD ; MOVEMENT IN SOIL ; NEW HAMPSHIRE ; PERFIL DEL SUELO ; PLOMB ; PLOMO ; Pollution ; POLLUTION ATMOSPHERIQUE ; POLLUTION DU SOL ; Pollution, environment geology ; POLUCION DEL AIRE ; POLUCION DEL SUELO ; PROCESOS DE TRANSPORTE EN EL SUELO ; PROFIL DU SOL ; Soil and sediments pollution ; Soil and water pollution ; SOIL LEAD POOLS ; SOIL POLLUTION ; SOIL PROFILES ; Soil science ; SOIL TRANSPORT PROCESSES ; SOIL ZINC POOLS ; Soils ; SOL DE FORET ; SPODOSOL ; SPODOSOLES ; SPODOSOLS ; SUELO FORESTAL ; Terrestrial environment, soil, air ; Trace metals ; TRANSPORT DANS LE SOL ; ZINC</subject><ispartof>Soil Science Society of America journal, 1998-05, Vol.62 (3), p.782-789</ispartof><rights>1998 Soil Science Society of America</rights><rights>1998 INIST-CNRS</rights><rights>Copyright American Society of Agronomy May 1998</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c500X-41a83b093a062f7d4ebf0c9700fe39ae6d212654fdb17ee107e15a0c9f0a43323</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.2136%2Fsssaj1998.03615995006200030035x$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.2136%2Fsssaj1998.03615995006200030035x$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27903,27904,45553,45554</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=2393153$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Johnson, C.E. (Syracuse Univ., Syracuse, NY.)</creatorcontrib><creatorcontrib>Petras, R.J</creatorcontrib><title>Distribution of zinc and lead fractions within a forest spodosol</title><title>Soil Science Society of America journal</title><description>Soil processes play a critical role in the fate of trace metals in forest ecosystems. To explore the nature of soil-trace metal interactions, we estimated five fractions of Zn and Pb in Spodosols at the Hubbard Brook Experimental Forest in central New Hampshire: (i) soluble + exchangeable (EX); (ii) inorganically bound (IB); (iii) organically bound (ORG); (iv) amorphous oxide bound (AMOX); and (v) mineral lattice, or residual (RES). Organic matter is a critical factor in trace metal fractionation in Hubbard Brook soils; loss-on-ignition was strongly correlated to EX Zn (r = 0.91) and Pb (r = 0.85), and ORG Zn (r = 0.57) and Pb (r = 0.89). The Oa horizon accounted for only 1.9% of the soil mass above the C horizon, but contained 23% and 77%, respectively, of the EX Zn and Pb in the soil. Lead was more tightly held in the soil than Zn; the percentage of total metal in the EX fraction was greater for Zn than Pb in all horizons. Through biocycling, Zn is returned to the forest floor, helping to maintain labile pools in upper soil horizons. Nevertheless, the EX Zn pool (6.03 kg ha-1) is insufficient to replace the pool of Zn in aboveground tissues (6.87 kg ha-1). Lead, not a nutrient, has accumulated in the soil due to the combustion of leaded gasoline. Lead leached from the O horizon between 1926 and 1991 can account for 30% of the EX + IB + ORG Pb, or 14% of the labile Pb in the mineral soil</description><subject>Agronomy. Soil science and plant productions</subject><subject>AIR POLLUTION</subject><subject>Animal, plant and microbial ecology</subject><subject>Applied ecology</subject><subject>Applied sciences</subject><subject>BIOAVAILABILITY</subject><subject>BIODISPONIBILIDAD</subject><subject>BIODISPONIBILITE</subject><subject>Biological and medical sciences</subject><subject>Biological and physicochemical properties of pollutants. Interaction in the soil</subject><subject>CICLO BIOGEOQUIMICO</subject><subject>CINC</subject><subject>CYCLE BIOGEOCHIMIQUE</subject><subject>CYCLING</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>ECOSISTEMA</subject><subject>ECOSYSTEME</subject><subject>ECOSYSTEMS</subject><subject>Ecotoxicology, biological effects of pollution</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Exact sciences and technology</subject><subject>Forest ecosystems</subject><subject>FOREST SOILS</subject><subject>Forests</subject><subject>FRACCIONAMIENTO</subject><subject>FRACTIONATION</subject><subject>FRACTIONNEMENT</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>LEAD</subject><subject>MOVEMENT IN SOIL</subject><subject>NEW HAMPSHIRE</subject><subject>PERFIL DEL SUELO</subject><subject>PLOMB</subject><subject>PLOMO</subject><subject>Pollution</subject><subject>POLLUTION ATMOSPHERIQUE</subject><subject>POLLUTION DU SOL</subject><subject>Pollution, environment geology</subject><subject>POLUCION DEL AIRE</subject><subject>POLUCION DEL SUELO</subject><subject>PROCESOS DE TRANSPORTE EN EL SUELO</subject><subject>PROFIL DU SOL</subject><subject>Soil and sediments pollution</subject><subject>Soil and water pollution</subject><subject>SOIL LEAD POOLS</subject><subject>SOIL POLLUTION</subject><subject>SOIL PROFILES</subject><subject>Soil science</subject><subject>SOIL TRANSPORT PROCESSES</subject><subject>SOIL ZINC POOLS</subject><subject>Soils</subject><subject>SOL DE FORET</subject><subject>SPODOSOL</subject><subject>SPODOSOLES</subject><subject>SPODOSOLS</subject><subject>SUELO FORESTAL</subject><subject>Terrestrial environment, soil, air</subject><subject>Trace metals</subject><subject>TRANSPORT DANS LE SOL</subject><subject>ZINC</subject><issn>0361-5995</issn><issn>1435-0661</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1998</creationdate><recordtype>article</recordtype><recordid>eNqV0d1rFDEQAPAgCp6tf4IQROzTtpPP3Txpqa0fFHw4C30Lud1Ec2w3Z-aOWv96Z7nSBymCEJKH_DIzmWHsSMCxFMqeIGJYC-e6Y1BWGOcMgJUAoGiZX0_YQmhlGrBWPGWL2TQzes5eIK4B6AXAgr3_kHFb82q3zWXiJfHfeep5mAY-xjDwVEM_3yC_zdsfeeKBp1IjbjluylCwjIfsWQojxpf35wG7ujj_dvapufz68fPZ6WXTU13XjRahUytwKlCRqR10XCXoXQuQonIh2kEKaY1Ow0q0MQpoozCBRIKglZLqgB3t425q-bmjCvxNxj6OY5hi2aFvtRJt1zkg-fafkrrndOsswdd_wXXZ1Yl-QcaC0VIbQu_2qK8FscbkNzXfhHrnBcyhrH8YhH90EBThzX2agH0YqaVTn_EhjFROCaOI-T27zWO8-98sfnn6RS6XtM_mMXJNGV7tM6RQfPheqYirJfEWnDSdUH8ArgSsNA</recordid><startdate>199805</startdate><enddate>199805</enddate><creator>Johnson, C.E. (Syracuse Univ., Syracuse, NY.)</creator><creator>Petras, R.J</creator><general>Soil Science Society of America</general><general>American Society of Agronomy</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7T7</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>P64</scope><scope>SOI</scope><scope>KR7</scope></search><sort><creationdate>199805</creationdate><title>Distribution of zinc and lead fractions within a forest spodosol</title><author>Johnson, C.E. (Syracuse Univ., Syracuse, NY.) ; Petras, R.J</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c500X-41a83b093a062f7d4ebf0c9700fe39ae6d212654fdb17ee107e15a0c9f0a43323</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1998</creationdate><topic>Agronomy. Soil science and plant productions</topic><topic>AIR POLLUTION</topic><topic>Animal, plant and microbial ecology</topic><topic>Applied ecology</topic><topic>Applied sciences</topic><topic>BIOAVAILABILITY</topic><topic>BIODISPONIBILIDAD</topic><topic>BIODISPONIBILITE</topic><topic>Biological and medical sciences</topic><topic>Biological and physicochemical properties of pollutants. Interaction in the soil</topic><topic>CICLO BIOGEOQUIMICO</topic><topic>CINC</topic><topic>CYCLE BIOGEOCHIMIQUE</topic><topic>CYCLING</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>ECOSISTEMA</topic><topic>ECOSYSTEME</topic><topic>ECOSYSTEMS</topic><topic>Ecotoxicology, biological effects of pollution</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Exact sciences and technology</topic><topic>Forest ecosystems</topic><topic>FOREST SOILS</topic><topic>Forests</topic><topic>FRACCIONAMIENTO</topic><topic>FRACTIONATION</topic><topic>FRACTIONNEMENT</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>LEAD</topic><topic>MOVEMENT IN SOIL</topic><topic>NEW HAMPSHIRE</topic><topic>PERFIL DEL SUELO</topic><topic>PLOMB</topic><topic>PLOMO</topic><topic>Pollution</topic><topic>POLLUTION ATMOSPHERIQUE</topic><topic>POLLUTION DU SOL</topic><topic>Pollution, environment geology</topic><topic>POLUCION DEL AIRE</topic><topic>POLUCION DEL SUELO</topic><topic>PROCESOS DE TRANSPORTE EN EL SUELO</topic><topic>PROFIL DU SOL</topic><topic>Soil and sediments pollution</topic><topic>Soil and water pollution</topic><topic>SOIL LEAD POOLS</topic><topic>SOIL POLLUTION</topic><topic>SOIL PROFILES</topic><topic>Soil science</topic><topic>SOIL TRANSPORT PROCESSES</topic><topic>SOIL ZINC POOLS</topic><topic>Soils</topic><topic>SOL DE FORET</topic><topic>SPODOSOL</topic><topic>SPODOSOLES</topic><topic>SPODOSOLS</topic><topic>SUELO FORESTAL</topic><topic>Terrestrial environment, soil, air</topic><topic>Trace metals</topic><topic>TRANSPORT DANS LE SOL</topic><topic>ZINC</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Johnson, C.E. (Syracuse Univ., Syracuse, NY.)</creatorcontrib><creatorcontrib>Petras, R.J</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environment Abstracts</collection><collection>Civil Engineering Abstracts</collection><jtitle>Soil Science Society of America journal</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Johnson, C.E. (Syracuse Univ., Syracuse, NY.)</au><au>Petras, R.J</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Distribution of zinc and lead fractions within a forest spodosol</atitle><jtitle>Soil Science Society of America journal</jtitle><date>1998-05</date><risdate>1998</risdate><volume>62</volume><issue>3</issue><spage>782</spage><epage>789</epage><pages>782-789</pages><issn>0361-5995</issn><eissn>1435-0661</eissn><coden>SSSJD4</coden><abstract>Soil processes play a critical role in the fate of trace metals in forest ecosystems. To explore the nature of soil-trace metal interactions, we estimated five fractions of Zn and Pb in Spodosols at the Hubbard Brook Experimental Forest in central New Hampshire: (i) soluble + exchangeable (EX); (ii) inorganically bound (IB); (iii) organically bound (ORG); (iv) amorphous oxide bound (AMOX); and (v) mineral lattice, or residual (RES). Organic matter is a critical factor in trace metal fractionation in Hubbard Brook soils; loss-on-ignition was strongly correlated to EX Zn (r = 0.91) and Pb (r = 0.85), and ORG Zn (r = 0.57) and Pb (r = 0.89). The Oa horizon accounted for only 1.9% of the soil mass above the C horizon, but contained 23% and 77%, respectively, of the EX Zn and Pb in the soil. Lead was more tightly held in the soil than Zn; the percentage of total metal in the EX fraction was greater for Zn than Pb in all horizons. Through biocycling, Zn is returned to the forest floor, helping to maintain labile pools in upper soil horizons. Nevertheless, the EX Zn pool (6.03 kg ha-1) is insufficient to replace the pool of Zn in aboveground tissues (6.87 kg ha-1). Lead, not a nutrient, has accumulated in the soil due to the combustion of leaded gasoline. Lead leached from the O horizon between 1926 and 1991 can account for 30% of the EX + IB + ORG Pb, or 14% of the labile Pb in the mineral soil</abstract><cop>Madison, WI</cop><pub>Soil Science Society of America</pub><doi>10.2136/sssaj1998.03615995006200030035x</doi><tpages>8</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0361-5995 |
| ispartof | Soil Science Society of America journal, 1998-05, Vol.62 (3), p.782-789 |
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| source | Wiley Online Library Journals Frontfile Complete |
| subjects | Agronomy. Soil science and plant productions AIR POLLUTION Animal, plant and microbial ecology Applied ecology Applied sciences BIOAVAILABILITY BIODISPONIBILIDAD BIODISPONIBILITE Biological and medical sciences Biological and physicochemical properties of pollutants. Interaction in the soil CICLO BIOGEOQUIMICO CINC CYCLE BIOGEOCHIMIQUE CYCLING Earth sciences Earth, ocean, space ECOSISTEMA ECOSYSTEME ECOSYSTEMS Ecotoxicology, biological effects of pollution Engineering and environment geology. Geothermics Exact sciences and technology Forest ecosystems FOREST SOILS Forests FRACCIONAMIENTO FRACTIONATION FRACTIONNEMENT Fundamental and applied biological sciences. Psychology LEAD MOVEMENT IN SOIL NEW HAMPSHIRE PERFIL DEL SUELO PLOMB PLOMO Pollution POLLUTION ATMOSPHERIQUE POLLUTION DU SOL Pollution, environment geology POLUCION DEL AIRE POLUCION DEL SUELO PROCESOS DE TRANSPORTE EN EL SUELO PROFIL DU SOL Soil and sediments pollution Soil and water pollution SOIL LEAD POOLS SOIL POLLUTION SOIL PROFILES Soil science SOIL TRANSPORT PROCESSES SOIL ZINC POOLS Soils SOL DE FORET SPODOSOL SPODOSOLES SPODOSOLS SUELO FORESTAL Terrestrial environment, soil, air Trace metals TRANSPORT DANS LE SOL ZINC |
| title | Distribution of zinc and lead fractions within a forest spodosol |
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