Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds

Autores
Avecilla, Fernando; Panebianco, Juan Esteban; Buschiazzo, Daniel Eduardo
Año de publicación
2017
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Soil wind erosion and consequent PM10 emission is a complex process that has been related to surface properties and meteorological conditions. Most of the studies have emphasized on the relationship between the surface conditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about the influence of meteorological variables on PM10 emission from agricultural soils. The objective of this study was to identify the most important meteorological variables involved in the emission of PM10, identify their threshold values, and to analyze their interaction with the soil surface conditions. Measurements were made on a loam soil (Entic Haplustoll) in the semiarid Argentinian Pampa. Horizontal mass transport (Q) and PM10 emission were measured during two years on a bare and flat surface that was tilled periodically. The meteorological variables measured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soil temperature. In 30% of the events, the PM10 concentration at 1.8 m height exceeded the average values allowed by the World Health Organization (50 μg m−3 for a 24 h period). Maximum values exceeded 1000 μg m−3. The slope of the PM10 concentration gradient changed between spring − summer and autumn − winter periods. Threshold values of the studied variables were set when PM10 concentration values at 1.8 m height were consistently above the 50 μg m−3 limit. The highest PM10 emission rates were observed when relative humidity values were below 20% and the air temperature was higher than 30 °C. In addition when the wind speed exceeded 8 m s−1, dust emission increased significantly. From a multiple regression analysis, results indicated that PM10 emission was well correlated (p < 0.001) with maximum wind speed, relative humidity, and air temperature. Maximum wind speed and relative humidity conditioned the PM10 emission in a synergistic way. However, the regression explained only 32% of the variability. Although higher average PM10 emission values were measured during events with a crusted surface, lower average values of Q were measured during events with a crust. Field observations indicated that the complex interaction between the weather conditions and soil surface properties such as soil crusts, aggregate size distribution, soil moisture and even the soil condition when the tilling is done, can produce a high variability and unpredictability, of the PM10 emission from bare agricultural soils.
EEA Anguil
Fil: Avecilla, Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Ciencias de la Tierra y Ambientales de La Pampa. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales de La Pampa; Argentina
Fil: Panebianco, Juan Esteban. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Ciencias de la Tierra y Ambientales de La Pampa. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales de La Pampa; Argentina
Fil: Buschiazzo, Daniel Eduardo. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Anguil; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Ciencias de la Tierra y Ambientales de La Pampa. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales de La Pampa; Argentina
Fuente
Agricultural and forest meteorology 244–245 : 21-32. (15 October 2017)
Materia
Erosión
Suelo Franco
Condiciones Atmosféricas
Loam Soils
Meteorological Factors
PM10
Fine Particles
Erodibility
Erosionabilidad
Nivel de accesibilidad
acceso restringido
Condiciones de uso
Repositorio
INTA Digital (INTA)
Institución
Instituto Nacional de Tecnología Agropecuaria
OAI Identificador
oai:localhost:20.500.12123/3940

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oai_identifier_str oai:localhost:20.500.12123/3940
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spelling Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholdsAvecilla, FernandoPanebianco, Juan EstebanBuschiazzo, Daniel EduardoErosiónSuelo FrancoCondiciones AtmosféricasLoam SoilsMeteorological FactorsPM10Fine ParticlesErodibilityErosionabilidadSoil wind erosion and consequent PM10 emission is a complex process that has been related to surface properties and meteorological conditions. Most of the studies have emphasized on the relationship between the surface conditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about the influence of meteorological variables on PM10 emission from agricultural soils. The objective of this study was to identify the most important meteorological variables involved in the emission of PM10, identify their threshold values, and to analyze their interaction with the soil surface conditions. Measurements were made on a loam soil (Entic Haplustoll) in the semiarid Argentinian Pampa. Horizontal mass transport (Q) and PM10 emission were measured during two years on a bare and flat surface that was tilled periodically. The meteorological variables measured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soil temperature. In 30% of the events, the PM10 concentration at 1.8 m height exceeded the average values allowed by the World Health Organization (50 μg m−3 for a 24 h period). Maximum values exceeded 1000 μg m−3. The slope of the PM10 concentration gradient changed between spring − summer and autumn − winter periods. Threshold values of the studied variables were set when PM10 concentration values at 1.8 m height were consistently above the 50 μg m−3 limit. The highest PM10 emission rates were observed when relative humidity values were below 20% and the air temperature was higher than 30 °C. In addition when the wind speed exceeded 8 m s−1, dust emission increased significantly. From a multiple regression analysis, results indicated that PM10 emission was well correlated (p < 0.001) with maximum wind speed, relative humidity, and air temperature. Maximum wind speed and relative humidity conditioned the PM10 emission in a synergistic way. However, the regression explained only 32% of the variability. Although higher average PM10 emission values were measured during events with a crusted surface, lower average values of Q were measured during events with a crust. Field observations indicated that the complex interaction between the weather conditions and soil surface properties such as soil crusts, aggregate size distribution, soil moisture and even the soil condition when the tilling is done, can produce a high variability and unpredictability, of the PM10 emission from bare agricultural soils.EEA AnguilFil: Avecilla, Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Ciencias de la Tierra y Ambientales de La Pampa. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales de La Pampa; ArgentinaFil: Panebianco, Juan Esteban. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Ciencias de la Tierra y Ambientales de La Pampa. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales de La Pampa; ArgentinaFil: Buschiazzo, Daniel Eduardo. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Anguil; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Ciencias de la Tierra y Ambientales de La Pampa. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales de La Pampa; ArgentinaElsevier2018-11-21T14:41:19Z2018-11-21T14:41:19Z2017-10-15info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://hdl.handle.net/20.500.12123/3940https://www.sciencedirect.com/science/article/pii/S0168192317301818?via%3Dihub0168-1923https://doi.org/10.1016/j.agrformet.2017.05.016Agricultural and forest meteorology 244–245 : 21-32. (15 October 2017)reponame:INTA Digital (INTA)instname:Instituto Nacional de Tecnología Agropecuariaenginfo:eu-repo/semantics/restrictedAccess2025-10-23T11:16:45Zoai:localhost:20.500.12123/3940instacron:INTAInstitucionalhttp://repositorio.inta.gob.ar/Organismo científico-tecnológicoNo correspondehttp://repositorio.inta.gob.ar/oai/requesttripaldi.nicolas@inta.gob.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:l2025-10-23 11:16:45.465INTA Digital (INTA) - Instituto Nacional de Tecnología Agropecuariafalse
dc.title.none.fl_str_mv Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds
title Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds
spellingShingle Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds
Avecilla, Fernando
Erosión
Suelo Franco
Condiciones Atmosféricas
Loam Soils
Meteorological Factors
PM10
Fine Particles
Erodibility
Erosionabilidad
title_short Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds
title_full Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds
title_fullStr Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds
title_full_unstemmed Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds
title_sort Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds
dc.creator.none.fl_str_mv Avecilla, Fernando
Panebianco, Juan Esteban
Buschiazzo, Daniel Eduardo
author Avecilla, Fernando
author_facet Avecilla, Fernando
Panebianco, Juan Esteban
Buschiazzo, Daniel Eduardo
author_role author
author2 Panebianco, Juan Esteban
Buschiazzo, Daniel Eduardo
author2_role author
author
dc.subject.none.fl_str_mv Erosión
Suelo Franco
Condiciones Atmosféricas
Loam Soils
Meteorological Factors
PM10
Fine Particles
Erodibility
Erosionabilidad
topic Erosión
Suelo Franco
Condiciones Atmosféricas
Loam Soils
Meteorological Factors
PM10
Fine Particles
Erodibility
Erosionabilidad
dc.description.none.fl_txt_mv Soil wind erosion and consequent PM10 emission is a complex process that has been related to surface properties and meteorological conditions. Most of the studies have emphasized on the relationship between the surface conditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about the influence of meteorological variables on PM10 emission from agricultural soils. The objective of this study was to identify the most important meteorological variables involved in the emission of PM10, identify their threshold values, and to analyze their interaction with the soil surface conditions. Measurements were made on a loam soil (Entic Haplustoll) in the semiarid Argentinian Pampa. Horizontal mass transport (Q) and PM10 emission were measured during two years on a bare and flat surface that was tilled periodically. The meteorological variables measured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soil temperature. In 30% of the events, the PM10 concentration at 1.8 m height exceeded the average values allowed by the World Health Organization (50 μg m−3 for a 24 h period). Maximum values exceeded 1000 μg m−3. The slope of the PM10 concentration gradient changed between spring − summer and autumn − winter periods. Threshold values of the studied variables were set when PM10 concentration values at 1.8 m height were consistently above the 50 μg m−3 limit. The highest PM10 emission rates were observed when relative humidity values were below 20% and the air temperature was higher than 30 °C. In addition when the wind speed exceeded 8 m s−1, dust emission increased significantly. From a multiple regression analysis, results indicated that PM10 emission was well correlated (p < 0.001) with maximum wind speed, relative humidity, and air temperature. Maximum wind speed and relative humidity conditioned the PM10 emission in a synergistic way. However, the regression explained only 32% of the variability. Although higher average PM10 emission values were measured during events with a crusted surface, lower average values of Q were measured during events with a crust. Field observations indicated that the complex interaction between the weather conditions and soil surface properties such as soil crusts, aggregate size distribution, soil moisture and even the soil condition when the tilling is done, can produce a high variability and unpredictability, of the PM10 emission from bare agricultural soils.
EEA Anguil
Fil: Avecilla, Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Ciencias de la Tierra y Ambientales de La Pampa. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales de La Pampa; Argentina
Fil: Panebianco, Juan Esteban. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Ciencias de la Tierra y Ambientales de La Pampa. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales de La Pampa; Argentina
Fil: Buschiazzo, Daniel Eduardo. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Anguil; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Ciencias de la Tierra y Ambientales de La Pampa. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales de La Pampa; Argentina
description Soil wind erosion and consequent PM10 emission is a complex process that has been related to surface properties and meteorological conditions. Most of the studies have emphasized on the relationship between the surface conditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about the influence of meteorological variables on PM10 emission from agricultural soils. The objective of this study was to identify the most important meteorological variables involved in the emission of PM10, identify their threshold values, and to analyze their interaction with the soil surface conditions. Measurements were made on a loam soil (Entic Haplustoll) in the semiarid Argentinian Pampa. Horizontal mass transport (Q) and PM10 emission were measured during two years on a bare and flat surface that was tilled periodically. The meteorological variables measured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soil temperature. In 30% of the events, the PM10 concentration at 1.8 m height exceeded the average values allowed by the World Health Organization (50 μg m−3 for a 24 h period). Maximum values exceeded 1000 μg m−3. The slope of the PM10 concentration gradient changed between spring − summer and autumn − winter periods. Threshold values of the studied variables were set when PM10 concentration values at 1.8 m height were consistently above the 50 μg m−3 limit. The highest PM10 emission rates were observed when relative humidity values were below 20% and the air temperature was higher than 30 °C. In addition when the wind speed exceeded 8 m s−1, dust emission increased significantly. From a multiple regression analysis, results indicated that PM10 emission was well correlated (p < 0.001) with maximum wind speed, relative humidity, and air temperature. Maximum wind speed and relative humidity conditioned the PM10 emission in a synergistic way. However, the regression explained only 32% of the variability. Although higher average PM10 emission values were measured during events with a crusted surface, lower average values of Q were measured during events with a crust. Field observations indicated that the complex interaction between the weather conditions and soil surface properties such as soil crusts, aggregate size distribution, soil moisture and even the soil condition when the tilling is done, can produce a high variability and unpredictability, of the PM10 emission from bare agricultural soils.
publishDate 2017
dc.date.none.fl_str_mv 2017-10-15
2018-11-21T14:41:19Z
2018-11-21T14:41:19Z
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/20.500.12123/3940
https://www.sciencedirect.com/science/article/pii/S0168192317301818?via%3Dihub
0168-1923
https://doi.org/10.1016/j.agrformet.2017.05.016
url http://hdl.handle.net/20.500.12123/3940
https://www.sciencedirect.com/science/article/pii/S0168192317301818?via%3Dihub
https://doi.org/10.1016/j.agrformet.2017.05.016
identifier_str_mv 0168-1923
dc.language.none.fl_str_mv eng
language eng
dc.rights.none.fl_str_mv info:eu-repo/semantics/restrictedAccess
eu_rights_str_mv restrictedAccess
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 Agricultural and forest meteorology 244–245 : 21-32. (15 October 2017)
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
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