Effect of burning of tropical deciduous forest soil in Mexico on the microbial degradation of organic matter
Slash and burn conversion of tropical deciduous forest can result in significant disruption of soil nutrient cycling, particularly in terms of the dynamics of microbial populations. This study deals with the effect of fire and ash input on microbial respiration and on distribution of C within water-...
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| Veröffentlicht in: | Plant and soil 1999-09, Vol.206 (1), p.29-36 |
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| creator | Garcia-Oliva, F. (Denver Univ., Denver, CO (USA). Dept. of Biology Science) Sanford, R.L Kelly, E |
| description | Slash and burn conversion of tropical deciduous forest can result in significant disruption of soil nutrient cycling, particularly in terms of the dynamics of microbial populations. This study deals with the effect of fire and ash input on microbial respiration and on distribution of C within water-stable aggregate in soils during a long-term incubation experiment (164 days). In 0-2 cm samples, the forest soil with ash had the lowest total CO₂-C evolved during incubation. In the top 2 cm soil burned samples, grass amendment did not increase respiration; it did increase respiration, however, in the undisturbed forest soil. Our results suggest that the fire affected microbial activity through both soil heating and chemical changes. As indicated by the results of the grass amendment to burned sample treatment the high temperature killed some soil microorganisms, mainly those associated with the use of newly added C. In addition, ash input appears to have constrained microbial activity through changes in soil chemistry. Soil heating and ash input also affected the distribution of C across different size fractions of soil aggregates. Labile C associated with macroaggregates (>250 µm) was destroyed during fire and did not represent an important source of available labile C for microbial activity. We concluded that the combination of organic C redistribution among size-aggregate fractions and microbial communities alteration by fire are critical for soil C dynamic under pasture condition. |
| doi_str_mv | 10.1023/A:1004390202057 |
| format | Article |
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(Denver Univ., Denver, CO (USA). Dept. of Biology Science) ; Sanford, R.L ; Kelly, E</creator><creatorcontrib>Garcia-Oliva, F. (Denver Univ., Denver, CO (USA). Dept. of Biology Science) ; Sanford, R.L ; Kelly, E</creatorcontrib><description>Slash and burn conversion of tropical deciduous forest can result in significant disruption of soil nutrient cycling, particularly in terms of the dynamics of microbial populations. This study deals with the effect of fire and ash input on microbial respiration and on distribution of C within water-stable aggregate in soils during a long-term incubation experiment (164 days). In 0-2 cm samples, the forest soil with ash had the lowest total CO₂-C evolved during incubation. In the top 2 cm soil burned samples, grass amendment did not increase respiration; it did increase respiration, however, in the undisturbed forest soil. Our results suggest that the fire affected microbial activity through both soil heating and chemical changes. As indicated by the results of the grass amendment to burned sample treatment the high temperature killed some soil microorganisms, mainly those associated with the use of newly added C. In addition, ash input appears to have constrained microbial activity through changes in soil chemistry. Soil heating and ash input also affected the distribution of C across different size fractions of soil aggregates. Labile C associated with macroaggregates (>250 µm) was destroyed during fire and did not represent an important source of available labile C for microbial activity. We concluded that the combination of organic C redistribution among size-aggregate fractions and microbial communities alteration by fire are critical for soil C dynamic under pasture condition.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1023/A:1004390202057</identifier><identifier>CODEN: PLSOA2</identifier><language>eng</language><publisher>Dordrecht: Kluwer Academic Publishers</publisher><subject>Aggregates ; Agronomy. Soil science and plant productions ; Ash ; Ashes ; Biochemistry and biology ; BIODEGRADACION ; BIODEGRADATION ; Biological activity ; Biological and medical sciences ; BOSQUE ESTACIONAL TROPICAL ; BRULAGE ; BURNING ; Carbon dioxide ; Chemical, physicochemical, biochemical and biological properties ; CICLO BIOGEOQUIMICO ; Coarse textured soils ; CYCLE BIOGEOCHIMIQUE ; CYCLING ; Deciduous forests ; ELIMINATION DES REMANENTS ; Forest fires ; FOREST SOILS ; Forests ; FORET SAISONNIERE TROPICALE ; Fractions ; Fundamental and applied biological sciences. Psychology ; Grasses ; Heating ; High temperature ; MATERIA ORGANICA DEL SUELO ; MATIERE ORGANIQUE DU SOL ; MEXICO ; MEXIQUE ; Microbial activity ; Microbial degradation ; Microbiology ; Microorganisms ; Mineral soils ; Nutrient cycles ; Nutrient dynamics ; Organic matter ; Pasture ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Population studies ; QUEMA ; Respiration ; Slash and burn ; SLASH DISPOSAL ; Soil aggregates ; Soil chemistry ; Soil dynamics ; Soil microorganisms ; Soil nutrients ; SOIL ORGANIC MATTER ; Soil samples ; Soil science ; SOIL STRUCTURAL UNITS ; Soil temperature ; Soil water ; Soils ; SOL DE FORET ; SUELO FORESTAL ; TRATAMIENTO DE LOS RESTOS DE CORTAS ; Tropical forests ; TROPICAL SEASONAL FORESTS ; Tropical soils ; UNIDADES ESTRUCTURALES DE SUELOS ; UNITE STRUCTURALE DU SOL</subject><ispartof>Plant and soil, 1999-09, Vol.206 (1), p.29-36</ispartof><rights>1999 Kluwer Academic Publishers</rights><rights>1999 INIST-CNRS</rights><rights>Kluwer Academic Publishers 1998.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c330t-4d54dfebfcf123ce728e7802e37edd41d0164c4f104d880a8be66db4261675b53</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/42949433$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/42949433$$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=1835979$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Garcia-Oliva, F. (Denver Univ., Denver, CO (USA). Dept. of Biology Science)</creatorcontrib><creatorcontrib>Sanford, R.L</creatorcontrib><creatorcontrib>Kelly, E</creatorcontrib><title>Effect of burning of tropical deciduous forest soil in Mexico on the microbial degradation of organic matter</title><title>Plant and soil</title><description>Slash and burn conversion of tropical deciduous forest can result in significant disruption of soil nutrient cycling, particularly in terms of the dynamics of microbial populations. This study deals with the effect of fire and ash input on microbial respiration and on distribution of C within water-stable aggregate in soils during a long-term incubation experiment (164 days). In 0-2 cm samples, the forest soil with ash had the lowest total CO₂-C evolved during incubation. In the top 2 cm soil burned samples, grass amendment did not increase respiration; it did increase respiration, however, in the undisturbed forest soil. Our results suggest that the fire affected microbial activity through both soil heating and chemical changes. As indicated by the results of the grass amendment to burned sample treatment the high temperature killed some soil microorganisms, mainly those associated with the use of newly added C. In addition, ash input appears to have constrained microbial activity through changes in soil chemistry. Soil heating and ash input also affected the distribution of C across different size fractions of soil aggregates. Labile C associated with macroaggregates (>250 µm) was destroyed during fire and did not represent an important source of available labile C for microbial activity. We concluded that the combination of organic C redistribution among size-aggregate fractions and microbial communities alteration by fire are critical for soil C dynamic under pasture condition.</description><subject>Aggregates</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Ash</subject><subject>Ashes</subject><subject>Biochemistry and biology</subject><subject>BIODEGRADACION</subject><subject>BIODEGRADATION</subject><subject>Biological activity</subject><subject>Biological and medical sciences</subject><subject>BOSQUE ESTACIONAL TROPICAL</subject><subject>BRULAGE</subject><subject>BURNING</subject><subject>Carbon dioxide</subject><subject>Chemical, physicochemical, biochemical and biological properties</subject><subject>CICLO BIOGEOQUIMICO</subject><subject>Coarse textured soils</subject><subject>CYCLE BIOGEOCHIMIQUE</subject><subject>CYCLING</subject><subject>Deciduous forests</subject><subject>ELIMINATION DES REMANENTS</subject><subject>Forest fires</subject><subject>FOREST SOILS</subject><subject>Forests</subject><subject>FORET SAISONNIERE TROPICALE</subject><subject>Fractions</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Grasses</subject><subject>Heating</subject><subject>High temperature</subject><subject>MATERIA ORGANICA DEL SUELO</subject><subject>MATIERE ORGANIQUE DU SOL</subject><subject>MEXICO</subject><subject>MEXIQUE</subject><subject>Microbial activity</subject><subject>Microbial degradation</subject><subject>Microbiology</subject><subject>Microorganisms</subject><subject>Mineral soils</subject><subject>Nutrient cycles</subject><subject>Nutrient dynamics</subject><subject>Organic matter</subject><subject>Pasture</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>Population studies</subject><subject>QUEMA</subject><subject>Respiration</subject><subject>Slash and burn</subject><subject>SLASH DISPOSAL</subject><subject>Soil aggregates</subject><subject>Soil chemistry</subject><subject>Soil dynamics</subject><subject>Soil microorganisms</subject><subject>Soil nutrients</subject><subject>SOIL ORGANIC MATTER</subject><subject>Soil samples</subject><subject>Soil science</subject><subject>SOIL STRUCTURAL UNITS</subject><subject>Soil temperature</subject><subject>Soil water</subject><subject>Soils</subject><subject>SOL DE FORET</subject><subject>SUELO FORESTAL</subject><subject>TRATAMIENTO DE LOS RESTOS DE CORTAS</subject><subject>Tropical forests</subject><subject>TROPICAL SEASONAL FORESTS</subject><subject>Tropical soils</subject><subject>UNIDADES ESTRUCTURALES DE SUELOS</subject><subject>UNITE STRUCTURALE DU SOL</subject><issn>0032-079X</issn><issn>1573-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1999</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>eNpdkctLAzEQxoMoWKtnT0IQ8baa52bjrYgvqHpR8LZk86gp201NsqD_vdGKgkyYJHy_-ZhMADjE6AwjQs9nFxghRiUiJbjYAhPMBa04ovU2mCBESYWEfNkFeykt0dcd1xPQXzlndYbBwW6Mgx8WX8ccw9pr1UNjtTdjGBN0IdqUYQq-h36A9_bd6wDDAPOrhSuvY-j8d8EiKqOyL0oxCnGhBq_hSuVs4z7YcapP9uBnn4Ln66uny9tq_nhzdzmbV5pSlCtmODPOdk47TKi2gjRWNIhYKqwxDBuEa6aZw4iZpkGq6Wxdm46RGteCd5xOwenGdx3D21jablc-adv3arDlLS0WVAhZ8hQc_wOXoUyh9NYKjiUpixbo5AdSqczERTVon9p19CsVP1rcUC6FLNjRBlumHOKvzIhkklH6pzsVWrWIxeJhjqWU5Sskb-gnR4iHSg</recordid><startdate>19990901</startdate><enddate>19990901</enddate><creator>Garcia-Oliva, F. 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Dept. of Biology Science)</creator><creator>Sanford, R.L</creator><creator>Kelly, E</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>19990901</creationdate><title>Effect of burning of tropical deciduous forest soil in Mexico on the microbial degradation of organic matter</title><author>Garcia-Oliva, F. (Denver Univ., Denver, CO (USA). Dept. of Biology Science) ; Sanford, R.L ; Kelly, E</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c330t-4d54dfebfcf123ce728e7802e37edd41d0164c4f104d880a8be66db4261675b53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1999</creationdate><topic>Aggregates</topic><topic>Agronomy. Soil science and plant productions</topic><topic>Ash</topic><topic>Ashes</topic><topic>Biochemistry and biology</topic><topic>BIODEGRADACION</topic><topic>BIODEGRADATION</topic><topic>Biological activity</topic><topic>Biological and medical sciences</topic><topic>BOSQUE ESTACIONAL TROPICAL</topic><topic>BRULAGE</topic><topic>BURNING</topic><topic>Carbon dioxide</topic><topic>Chemical, physicochemical, biochemical and biological properties</topic><topic>CICLO BIOGEOQUIMICO</topic><topic>Coarse textured soils</topic><topic>CYCLE BIOGEOCHIMIQUE</topic><topic>CYCLING</topic><topic>Deciduous forests</topic><topic>ELIMINATION DES REMANENTS</topic><topic>Forest fires</topic><topic>FOREST SOILS</topic><topic>Forests</topic><topic>FORET SAISONNIERE TROPICALE</topic><topic>Fractions</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Grasses</topic><topic>Heating</topic><topic>High temperature</topic><topic>MATERIA ORGANICA DEL SUELO</topic><topic>MATIERE ORGANIQUE DU SOL</topic><topic>MEXICO</topic><topic>MEXIQUE</topic><topic>Microbial activity</topic><topic>Microbial degradation</topic><topic>Microbiology</topic><topic>Microorganisms</topic><topic>Mineral soils</topic><topic>Nutrient cycles</topic><topic>Nutrient dynamics</topic><topic>Organic matter</topic><topic>Pasture</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>Population studies</topic><topic>QUEMA</topic><topic>Respiration</topic><topic>Slash and burn</topic><topic>SLASH DISPOSAL</topic><topic>Soil aggregates</topic><topic>Soil chemistry</topic><topic>Soil dynamics</topic><topic>Soil microorganisms</topic><topic>Soil nutrients</topic><topic>SOIL ORGANIC MATTER</topic><topic>Soil samples</topic><topic>Soil science</topic><topic>SOIL STRUCTURAL UNITS</topic><topic>Soil temperature</topic><topic>Soil water</topic><topic>Soils</topic><topic>SOL DE FORET</topic><topic>SUELO FORESTAL</topic><topic>TRATAMIENTO DE LOS RESTOS DE CORTAS</topic><topic>Tropical forests</topic><topic>TROPICAL SEASONAL FORESTS</topic><topic>Tropical soils</topic><topic>UNIDADES ESTRUCTURALES DE SUELOS</topic><topic>UNITE STRUCTURALE DU SOL</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Garcia-Oliva, F. 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(Denver Univ., Denver, CO (USA). Dept. of Biology Science)</au><au>Sanford, R.L</au><au>Kelly, E</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effect of burning of tropical deciduous forest soil in Mexico on the microbial degradation of organic matter</atitle><jtitle>Plant and soil</jtitle><date>1999-09-01</date><risdate>1999</risdate><volume>206</volume><issue>1</issue><spage>29</spage><epage>36</epage><pages>29-36</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><coden>PLSOA2</coden><abstract>Slash and burn conversion of tropical deciduous forest can result in significant disruption of soil nutrient cycling, particularly in terms of the dynamics of microbial populations. This study deals with the effect of fire and ash input on microbial respiration and on distribution of C within water-stable aggregate in soils during a long-term incubation experiment (164 days). In 0-2 cm samples, the forest soil with ash had the lowest total CO₂-C evolved during incubation. In the top 2 cm soil burned samples, grass amendment did not increase respiration; it did increase respiration, however, in the undisturbed forest soil. Our results suggest that the fire affected microbial activity through both soil heating and chemical changes. As indicated by the results of the grass amendment to burned sample treatment the high temperature killed some soil microorganisms, mainly those associated with the use of newly added C. In addition, ash input appears to have constrained microbial activity through changes in soil chemistry. Soil heating and ash input also affected the distribution of C across different size fractions of soil aggregates. Labile C associated with macroaggregates (>250 µm) was destroyed during fire and did not represent an important source of available labile C for microbial activity. We concluded that the combination of organic C redistribution among size-aggregate fractions and microbial communities alteration by fire are critical for soil C dynamic under pasture condition.</abstract><cop>Dordrecht</cop><pub>Kluwer Academic Publishers</pub><doi>10.1023/A:1004390202057</doi><tpages>8</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0032-079X |
| ispartof | Plant and soil, 1999-09, Vol.206 (1), p.29-36 |
| issn | 0032-079X 1573-5036 |
| language | eng |
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| source | Jstor Complete Legacy; SpringerLink Journals - AutoHoldings |
| subjects | Aggregates Agronomy. Soil science and plant productions Ash Ashes Biochemistry and biology BIODEGRADACION BIODEGRADATION Biological activity Biological and medical sciences BOSQUE ESTACIONAL TROPICAL BRULAGE BURNING Carbon dioxide Chemical, physicochemical, biochemical and biological properties CICLO BIOGEOQUIMICO Coarse textured soils CYCLE BIOGEOCHIMIQUE CYCLING Deciduous forests ELIMINATION DES REMANENTS Forest fires FOREST SOILS Forests FORET SAISONNIERE TROPICALE Fractions Fundamental and applied biological sciences. Psychology Grasses Heating High temperature MATERIA ORGANICA DEL SUELO MATIERE ORGANIQUE DU SOL MEXICO MEXIQUE Microbial activity Microbial degradation Microbiology Microorganisms Mineral soils Nutrient cycles Nutrient dynamics Organic matter Pasture Physics, chemistry, biochemistry and biology of agricultural and forest soils Population studies QUEMA Respiration Slash and burn SLASH DISPOSAL Soil aggregates Soil chemistry Soil dynamics Soil microorganisms Soil nutrients SOIL ORGANIC MATTER Soil samples Soil science SOIL STRUCTURAL UNITS Soil temperature Soil water Soils SOL DE FORET SUELO FORESTAL TRATAMIENTO DE LOS RESTOS DE CORTAS Tropical forests TROPICAL SEASONAL FORESTS Tropical soils UNIDADES ESTRUCTURALES DE SUELOS UNITE STRUCTURALE DU SOL |
| title | Effect of burning of tropical deciduous forest soil in Mexico on the microbial degradation of organic matter |
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