Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, Argentina
- Autores
- González Comunian, Dubraska; Vivanco, Lucía; Morras, Hector; Buduba, Carlos Guillermo; La Manna, Ludmila
- Año de publicación
- 2026
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Early soil formation processes in recent volcanic ash deposits remain poorly understood, especially regarding the vegetation role in shaping their chemical and physical properties. This study investigates the initial evolution of rhyolitic ash influenced by two contrasting forest types—native cypress and planted ponderosa pine—through analysis of ash deposits and their interaction with organic matter. The ash originated from the 2008 eruption of the Chait´ en volcano in southern Chile and was deposited across western Chubut Province, Argentina, where volcanic soils predominate. Four sampling sites were selected along a west-east transect, where pine plantations neighbor cypress forests. Undisturbed soil profile samples were collected for micromorphological analyses, while ash samples underwent physical, chemical, and biological analyses. Results revealed that – fifteen years after the eruption - ash from cypress forests has significantly higher concentrations of OC, N, Ca, K, Mg, as well as higher microbial biomass, than ash from pine plantations. Cypress litter composition and morphology strongly influence organic matter incorporation into the volcanic ash, resulting in a higher degree of mixing with the O horizon. In contrast, in pine plantations, organic matter incorporation appears to be influenced by a stronger fungal mycelium activity, leading to the development of crumb microstructure, a lower degree of mixing with organic matter, and a higher incorporation of ash into the A horizon. In both vegetation types, the microstructure of the A horizon is replicated in the ash: granular in cypress and crumb in pine. This study highlights how vegetation shapes the course of soil formation from its earliest stages.
Instituto de Suelos
Fil: González Comunian, Dubraska. Universidad Nacional de la Patagonia San Juan Bosco. Facultad de Ingeniería. Centro de Estudios Ambientales Integrados (CEAI); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Vivanco, Lucía. Universidad de Buenos Aires. Facultad de Agronomía. Departamento de Recursos Naturales. Cátedra de Ecología; Argentina. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas vinculadas a la Agricultura (IFEVA); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Investigaciones Fisiológicas y Ecológicas vinculadas a la Agricultura (IFEVA); Argentina
Fil: Morras, Héctor José María. Instituto Nacional de Tecnología Agropecuaria (INTA). Instituto de Suelos; Argentina. Universidad del Salvador. Facultad de Ciencias Agrarias y Veterinarias; Argentina
Fil: Buduba, Carlos G. Universidad Nacional de la Patagonia San Juan Bosco. Facultad de Ingeniería. Centro de Estudios Ambientales Integrados (CEAI); Argentina. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agroforestal Esquel; Argentina
Fil: La Manna, Ludmila. Universidad Nacional de la Patagonia San Juan Bosco. Facultad de Ingeniería. Centro de Estudios Ambientales Integrados (CEAI); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina - Fuente
- Catena 270 : 110150. (August 2026)
- Materia
-
Bosques
Bosque Templado
Materia Orgánica del Suelo
Bosques Primarios
Forests
Temperate Forests
Soil Organic Matter
Primary Forests
Ceniza Volcánica
Región Patagónica
Bosques Nativos
Volcanic Ashes - Nivel de accesibilidad
- acceso restringido
- Condiciones de uso
- http://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
.jpg)
- Institución
- Instituto Nacional de Tecnología Agropecuaria
- OAI Identificador
- oai:localhost:20.500.12123/26472
Ver los metadatos del registro completo
| id |
INTADig_de002d60c52405dbd9913719385ce81d |
|---|---|
| oai_identifier_str |
oai:localhost:20.500.12123/26472 |
| network_acronym_str |
INTADig |
| repository_id_str |
l |
| network_name_str |
INTA Digital (INTA) |
| spelling |
Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, ArgentinaGonzález Comunian, DubraskaVivanco, LucíaMorras, HectorBuduba, Carlos GuillermoLa Manna, LudmilaBosquesBosque TempladoMateria Orgánica del SueloBosques PrimariosForestsTemperate ForestsSoil Organic MatterPrimary ForestsCeniza VolcánicaRegión PatagónicaBosques NativosVolcanic AshesEarly soil formation processes in recent volcanic ash deposits remain poorly understood, especially regarding the vegetation role in shaping their chemical and physical properties. This study investigates the initial evolution of rhyolitic ash influenced by two contrasting forest types—native cypress and planted ponderosa pine—through analysis of ash deposits and their interaction with organic matter. The ash originated from the 2008 eruption of the Chait´ en volcano in southern Chile and was deposited across western Chubut Province, Argentina, where volcanic soils predominate. Four sampling sites were selected along a west-east transect, where pine plantations neighbor cypress forests. Undisturbed soil profile samples were collected for micromorphological analyses, while ash samples underwent physical, chemical, and biological analyses. Results revealed that – fifteen years after the eruption - ash from cypress forests has significantly higher concentrations of OC, N, Ca, K, Mg, as well as higher microbial biomass, than ash from pine plantations. Cypress litter composition and morphology strongly influence organic matter incorporation into the volcanic ash, resulting in a higher degree of mixing with the O horizon. In contrast, in pine plantations, organic matter incorporation appears to be influenced by a stronger fungal mycelium activity, leading to the development of crumb microstructure, a lower degree of mixing with organic matter, and a higher incorporation of ash into the A horizon. In both vegetation types, the microstructure of the A horizon is replicated in the ash: granular in cypress and crumb in pine. This study highlights how vegetation shapes the course of soil formation from its earliest stages.Instituto de SuelosFil: González Comunian, Dubraska. Universidad Nacional de la Patagonia San Juan Bosco. Facultad de Ingeniería. Centro de Estudios Ambientales Integrados (CEAI); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Vivanco, Lucía. Universidad de Buenos Aires. Facultad de Agronomía. Departamento de Recursos Naturales. Cátedra de Ecología; Argentina. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas vinculadas a la Agricultura (IFEVA); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Investigaciones Fisiológicas y Ecológicas vinculadas a la Agricultura (IFEVA); ArgentinaFil: Morras, Héctor José María. Instituto Nacional de Tecnología Agropecuaria (INTA). Instituto de Suelos; Argentina. Universidad del Salvador. Facultad de Ciencias Agrarias y Veterinarias; ArgentinaFil: Buduba, Carlos G. Universidad Nacional de la Patagonia San Juan Bosco. Facultad de Ingeniería. Centro de Estudios Ambientales Integrados (CEAI); Argentina. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agroforestal Esquel; ArgentinaFil: La Manna, Ludmila. Universidad Nacional de la Patagonia San Juan Bosco. Facultad de Ingeniería. Centro de Estudios Ambientales Integrados (CEAI); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaElsevier2026-06-03T14:08:17Z2026-06-03T14:08:17Z2026-08info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://hdl.handle.net/20.500.12123/26472https://www.sciencedirect.com/science/article/abs/pii/S03418162260036070341-8162https://doi.org/10.1016/j.catena.2026.110150Catena 270 : 110150. (August 2026)reponame:INTA Digital (INTA)instname:Instituto Nacional de Tecnología Agropecuariaenginfo:eu-repo/semantics/restrictedAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)2026-06-04T09:46:26Zoai:localhost:20.500.12123/26472instacron:INTAInstitucionalhttp://repositorio.inta.gob.ar/Organismo científico-tecnológicoNo correspondehttp://repositorio.inta.gob.ar/oai/requesttripaldi.nicolas@inta.gob.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:l2026-06-04 09:46:26.111INTA Digital (INTA) - Instituto Nacional de Tecnología Agropecuariafalse |
| dc.title.none.fl_str_mv |
Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, Argentina |
| title |
Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, Argentina |
| spellingShingle |
Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, Argentina González Comunian, Dubraska Bosques Bosque Templado Materia Orgánica del Suelo Bosques Primarios Forests Temperate Forests Soil Organic Matter Primary Forests Ceniza Volcánica Región Patagónica Bosques Nativos Volcanic Ashes |
| title_short |
Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, Argentina |
| title_full |
Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, Argentina |
| title_fullStr |
Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, Argentina |
| title_full_unstemmed |
Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, Argentina |
| title_sort |
Evolution of recent volcanic ash deposits under native and planted temperate forest in Patagonia, Argentina |
| dc.creator.none.fl_str_mv |
González Comunian, Dubraska Vivanco, Lucía Morras, Hector Buduba, Carlos Guillermo La Manna, Ludmila |
| author |
González Comunian, Dubraska |
| author_facet |
González Comunian, Dubraska Vivanco, Lucía Morras, Hector Buduba, Carlos Guillermo La Manna, Ludmila |
| author_role |
author |
| author2 |
Vivanco, Lucía Morras, Hector Buduba, Carlos Guillermo La Manna, Ludmila |
| author2_role |
author author author author |
| dc.subject.none.fl_str_mv |
Bosques Bosque Templado Materia Orgánica del Suelo Bosques Primarios Forests Temperate Forests Soil Organic Matter Primary Forests Ceniza Volcánica Región Patagónica Bosques Nativos Volcanic Ashes |
| topic |
Bosques Bosque Templado Materia Orgánica del Suelo Bosques Primarios Forests Temperate Forests Soil Organic Matter Primary Forests Ceniza Volcánica Región Patagónica Bosques Nativos Volcanic Ashes |
| dc.description.none.fl_txt_mv |
Early soil formation processes in recent volcanic ash deposits remain poorly understood, especially regarding the vegetation role in shaping their chemical and physical properties. This study investigates the initial evolution of rhyolitic ash influenced by two contrasting forest types—native cypress and planted ponderosa pine—through analysis of ash deposits and their interaction with organic matter. The ash originated from the 2008 eruption of the Chait´ en volcano in southern Chile and was deposited across western Chubut Province, Argentina, where volcanic soils predominate. Four sampling sites were selected along a west-east transect, where pine plantations neighbor cypress forests. Undisturbed soil profile samples were collected for micromorphological analyses, while ash samples underwent physical, chemical, and biological analyses. Results revealed that – fifteen years after the eruption - ash from cypress forests has significantly higher concentrations of OC, N, Ca, K, Mg, as well as higher microbial biomass, than ash from pine plantations. Cypress litter composition and morphology strongly influence organic matter incorporation into the volcanic ash, resulting in a higher degree of mixing with the O horizon. In contrast, in pine plantations, organic matter incorporation appears to be influenced by a stronger fungal mycelium activity, leading to the development of crumb microstructure, a lower degree of mixing with organic matter, and a higher incorporation of ash into the A horizon. In both vegetation types, the microstructure of the A horizon is replicated in the ash: granular in cypress and crumb in pine. This study highlights how vegetation shapes the course of soil formation from its earliest stages. Instituto de Suelos Fil: González Comunian, Dubraska. Universidad Nacional de la Patagonia San Juan Bosco. Facultad de Ingeniería. Centro de Estudios Ambientales Integrados (CEAI); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Vivanco, Lucía. Universidad de Buenos Aires. Facultad de Agronomía. Departamento de Recursos Naturales. Cátedra de Ecología; Argentina. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas vinculadas a la Agricultura (IFEVA); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Investigaciones Fisiológicas y Ecológicas vinculadas a la Agricultura (IFEVA); Argentina Fil: Morras, Héctor José María. Instituto Nacional de Tecnología Agropecuaria (INTA). Instituto de Suelos; Argentina. Universidad del Salvador. Facultad de Ciencias Agrarias y Veterinarias; Argentina Fil: Buduba, Carlos G. Universidad Nacional de la Patagonia San Juan Bosco. Facultad de Ingeniería. Centro de Estudios Ambientales Integrados (CEAI); Argentina. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agroforestal Esquel; Argentina Fil: La Manna, Ludmila. Universidad Nacional de la Patagonia San Juan Bosco. Facultad de Ingeniería. Centro de Estudios Ambientales Integrados (CEAI); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina |
| description |
Early soil formation processes in recent volcanic ash deposits remain poorly understood, especially regarding the vegetation role in shaping their chemical and physical properties. This study investigates the initial evolution of rhyolitic ash influenced by two contrasting forest types—native cypress and planted ponderosa pine—through analysis of ash deposits and their interaction with organic matter. The ash originated from the 2008 eruption of the Chait´ en volcano in southern Chile and was deposited across western Chubut Province, Argentina, where volcanic soils predominate. Four sampling sites were selected along a west-east transect, where pine plantations neighbor cypress forests. Undisturbed soil profile samples were collected for micromorphological analyses, while ash samples underwent physical, chemical, and biological analyses. Results revealed that – fifteen years after the eruption - ash from cypress forests has significantly higher concentrations of OC, N, Ca, K, Mg, as well as higher microbial biomass, than ash from pine plantations. Cypress litter composition and morphology strongly influence organic matter incorporation into the volcanic ash, resulting in a higher degree of mixing with the O horizon. In contrast, in pine plantations, organic matter incorporation appears to be influenced by a stronger fungal mycelium activity, leading to the development of crumb microstructure, a lower degree of mixing with organic matter, and a higher incorporation of ash into the A horizon. In both vegetation types, the microstructure of the A horizon is replicated in the ash: granular in cypress and crumb in pine. This study highlights how vegetation shapes the course of soil formation from its earliest stages. |
| publishDate |
2026 |
| dc.date.none.fl_str_mv |
2026-06-03T14:08:17Z 2026-06-03T14:08:17Z 2026-08 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/20.500.12123/26472 https://www.sciencedirect.com/science/article/abs/pii/S0341816226003607 0341-8162 https://doi.org/10.1016/j.catena.2026.110150 |
| url |
http://hdl.handle.net/20.500.12123/26472 https://www.sciencedirect.com/science/article/abs/pii/S0341816226003607 https://doi.org/10.1016/j.catena.2026.110150 |
| identifier_str_mv |
0341-8162 |
| dc.language.none.fl_str_mv |
eng |
| language |
eng |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/restrictedAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
| eu_rights_str_mv |
restrictedAccess |
| rights_invalid_str_mv |
http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.none.fl_str_mv |
Elsevier |
| publisher.none.fl_str_mv |
Elsevier |
| dc.source.none.fl_str_mv |
Catena 270 : 110150. (August 2026) reponame:INTA Digital (INTA) instname:Instituto Nacional de Tecnología Agropecuaria |
| reponame_str |
INTA Digital (INTA) |
| collection |
INTA Digital (INTA) |
| instname_str |
Instituto Nacional de Tecnología Agropecuaria |
| repository.name.fl_str_mv |
INTA Digital (INTA) - Instituto Nacional de Tecnología Agropecuaria |
| repository.mail.fl_str_mv |
tripaldi.nicolas@inta.gob.ar |
| _version_ |
1867091752951742464 |
| score |
13.343132 |