Soil nitrogen cycling following montane forest conversion in Central Sulawesi, Indonesia
The lower montane forest zone of Indonesia is undergoing rapid conversion of indigenous forests to agriculture. In this tropical region, however, the effects of forest conversion on soil N processes have not been investigated. Corn (Zea mays L.) and cacao (Theobroma cacao L.)–coffee (Coffea canephora Pierre ex Froehner) agroforestry are the main land use types in cleared lower montane forests in Central Sulawesi, Indonesia. Our main objective was to compare the soil N dynamics under agroforest systems and corn cultivation with indigenous forest. We measured the gross rates of N transformation processes using 15N pool dilution. The agroforest systems and indigenous forests had higher gross N mineralization rates and faster turnover rates of NH41 and microbial N pools than the long-term cultivated corn sites. Faster soil N turnover rates in agroforest systems suggest a more dynamic soil N cycling. Leguminous shade trees, which are important components of these agroforest systems, may have influenced the fast microbial N cycling through release of N-rich root exudates and plant residues. Our results show that compared with corn, agroforestry is a better option in terms of sustainability in the N-supplying capacity of the soil. In addition, we measured higher 15 NH41 recoveries than 15NO32 recoveries after 15 min of 15N addition in all our sites. Our measured rates of gross nitrification were very low to negligible, due to rapid disappearance of added 15NO32. Such fast reaction of NO32 warrants further investigation, especially in tropical areas where 15N studies are very few.
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EUA Wiley
2006
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Subjects: | UTILIZACIÓN DE LA TIERRA, MECÁNICA DEL SUELO, ZEA MAYS, COFFEA CANEPHORA, CULTIVO MIGRATORIO, MINERALIZACIÓN, CICLO DEL NITROGENO, NITRIFICACIÓN, PLANTAS DE SOMBRA, NITRATOS, FIJACIÓN DEL NITRÓGENO, GLIRICIDIA SEPIUM, INDONESIA, |
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KOHA-OAI-BVE:1258772022-08-04T22:09:03ZSoil nitrogen cycling following montane forest conversion in Central Sulawesi, Indonesia 59156 Corre, M.D. 61727 Dechert, G. 128090 Veldkamp, E. autores/as EUA Wiley2006 enpdfThe lower montane forest zone of Indonesia is undergoing rapid conversion of indigenous forests to agriculture. In this tropical region, however, the effects of forest conversion on soil N processes have not been investigated. Corn (Zea mays L.) and cacao (Theobroma cacao L.)–coffee (Coffea canephora Pierre ex Froehner) agroforestry are the main land use types in cleared lower montane forests in Central Sulawesi, Indonesia. Our main objective was to compare the soil N dynamics under agroforest systems and corn cultivation with indigenous forest. We measured the gross rates of N transformation processes using 15N pool dilution. The agroforest systems and indigenous forests had higher gross N mineralization rates and faster turnover rates of NH41 and microbial N pools than the long-term cultivated corn sites. Faster soil N turnover rates in agroforest systems suggest a more dynamic soil N cycling. Leguminous shade trees, which are important components of these agroforest systems, may have influenced the fast microbial N cycling through release of N-rich root exudates and plant residues. Our results show that compared with corn, agroforestry is a better option in terms of sustainability in the N-supplying capacity of the soil. In addition, we measured higher 15 NH41 recoveries than 15NO32 recoveries after 15 min of 15N addition in all our sites. Our measured rates of gross nitrification were very low to negligible, due to rapid disappearance of added 15NO32. Such fast reaction of NO32 warrants further investigation, especially in tropical areas where 15N studies are very few. Incluye 35 referencias bibliográficas en las páginas 365-366The lower montane forest zone of Indonesia is undergoing rapid conversion of indigenous forests to agriculture. In this tropical region, however, the effects of forest conversion on soil N processes have not been investigated. Corn (Zea mays L.) and cacao (Theobroma cacao L.)–coffee (Coffea canephora Pierre ex Froehner) agroforestry are the main land use types in cleared lower montane forests in Central Sulawesi, Indonesia. Our main objective was to compare the soil N dynamics under agroforest systems and corn cultivation with indigenous forest. We measured the gross rates of N transformation processes using 15N pool dilution. The agroforest systems and indigenous forests had higher gross N mineralization rates and faster turnover rates of NH41 and microbial N pools than the long-term cultivated corn sites. Faster soil N turnover rates in agroforest systems suggest a more dynamic soil N cycling. Leguminous shade trees, which are important components of these agroforest systems, may have influenced the fast microbial N cycling through release of N-rich root exudates and plant residues. Our results show that compared with corn, agroforestry is a better option in terms of sustainability in the N-supplying capacity of the soil. In addition, we measured higher 15 NH41 recoveries than 15NO32 recoveries after 15 min of 15N addition in all our sites. Our measured rates of gross nitrification were very low to negligible, due to rapid disappearance of added 15NO32. Such fast reaction of NO32 warrants further investigation, especially in tropical areas where 15N studies are very few. UTILIZACIÓN DE LA TIERRAMECÁNICA DEL SUELOZEA MAYSCOFFEA CANEPHORACULTIVO MIGRATORIOMINERALIZACIÓNCICLO DEL NITROGENONITRIFICACIÓNPLANTAS DE SOMBRANITRATOSFIJACIÓN DEL NITRÓGENOGLIRICIDIA SEPIUMINDONESIASoil Science Society of America Journal (EUA) https://doi.org/10.2136/sssaj2005.0061 |
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UTILIZACIÓN DE LA TIERRA MECÁNICA DEL SUELO ZEA MAYS COFFEA CANEPHORA CULTIVO MIGRATORIO MINERALIZACIÓN CICLO DEL NITROGENO NITRIFICACIÓN PLANTAS DE SOMBRA NITRATOS FIJACIÓN DEL NITRÓGENO GLIRICIDIA SEPIUM INDONESIA UTILIZACIÓN DE LA TIERRA MECÁNICA DEL SUELO ZEA MAYS COFFEA CANEPHORA CULTIVO MIGRATORIO MINERALIZACIÓN CICLO DEL NITROGENO NITRIFICACIÓN PLANTAS DE SOMBRA NITRATOS FIJACIÓN DEL NITRÓGENO GLIRICIDIA SEPIUM INDONESIA |
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UTILIZACIÓN DE LA TIERRA MECÁNICA DEL SUELO ZEA MAYS COFFEA CANEPHORA CULTIVO MIGRATORIO MINERALIZACIÓN CICLO DEL NITROGENO NITRIFICACIÓN PLANTAS DE SOMBRA NITRATOS FIJACIÓN DEL NITRÓGENO GLIRICIDIA SEPIUM INDONESIA UTILIZACIÓN DE LA TIERRA MECÁNICA DEL SUELO ZEA MAYS COFFEA CANEPHORA CULTIVO MIGRATORIO MINERALIZACIÓN CICLO DEL NITROGENO NITRIFICACIÓN PLANTAS DE SOMBRA NITRATOS FIJACIÓN DEL NITRÓGENO GLIRICIDIA SEPIUM INDONESIA 59156 Corre, M.D. 61727 Dechert, G. 128090 Veldkamp, E. autores/as Soil nitrogen cycling following montane forest conversion in Central Sulawesi, Indonesia |
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The lower montane forest zone of Indonesia is undergoing rapid conversion of indigenous forests to agriculture. In this tropical region, however, the effects of forest conversion on soil N processes have not been investigated. Corn (Zea mays L.) and cacao (Theobroma cacao L.)–coffee (Coffea canephora Pierre ex Froehner) agroforestry are the main land use types in cleared lower montane forests in Central Sulawesi, Indonesia. Our main objective was to compare the soil N dynamics under agroforest systems and corn cultivation with indigenous forest. We measured the gross rates of N transformation processes using 15N pool dilution. The agroforest systems and indigenous forests had higher gross N mineralization rates and faster turnover rates of NH41 and microbial N pools than the long-term cultivated corn sites. Faster soil N turnover rates in agroforest systems suggest a more dynamic soil N cycling. Leguminous shade trees, which are important components of these agroforest systems, may have influenced the fast microbial N cycling through release of N-rich root exudates and plant residues. Our results show that compared with corn, agroforestry is a better option in terms of sustainability in the N-supplying capacity of the soil. In addition, we measured higher 15 NH41 recoveries than 15NO32 recoveries after 15 min of 15N addition in all our sites. Our measured rates of gross nitrification were very low to negligible, due to rapid disappearance of added 15NO32. Such fast reaction of NO32 warrants further investigation, especially in tropical areas where 15N studies are very few.
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UTILIZACIÓN DE LA TIERRA MECÁNICA DEL SUELO ZEA MAYS COFFEA CANEPHORA CULTIVO MIGRATORIO MINERALIZACIÓN CICLO DEL NITROGENO NITRIFICACIÓN PLANTAS DE SOMBRA NITRATOS FIJACIÓN DEL NITRÓGENO GLIRICIDIA SEPIUM INDONESIA |
author |
59156 Corre, M.D. 61727 Dechert, G. 128090 Veldkamp, E. autores/as |
author_facet |
59156 Corre, M.D. 61727 Dechert, G. 128090 Veldkamp, E. autores/as |
author_sort |
59156 Corre, M.D. |
title |
Soil nitrogen cycling following montane forest conversion in Central Sulawesi, Indonesia |
title_short |
Soil nitrogen cycling following montane forest conversion in Central Sulawesi, Indonesia |
title_full |
Soil nitrogen cycling following montane forest conversion in Central Sulawesi, Indonesia |
title_fullStr |
Soil nitrogen cycling following montane forest conversion in Central Sulawesi, Indonesia |
title_full_unstemmed |
Soil nitrogen cycling following montane forest conversion in Central Sulawesi, Indonesia |
title_sort |
soil nitrogen cycling following montane forest conversion in central sulawesi, indonesia |
publisher |
EUA Wiley |
publishDate |
2006 |
work_keys_str_mv |
AT 59156corremd soilnitrogencyclingfollowingmontaneforestconversionincentralsulawesiindonesia AT 61727dechertg soilnitrogencyclingfollowingmontaneforestconversionincentralsulawesiindonesia AT 128090veldkampeautoresas soilnitrogencyclingfollowingmontaneforestconversionincentralsulawesiindonesia |
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1756064848264822784 |