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 propertiesand meteorological conditions. Most of the studies have emphasized on the relationship between the surfaceconditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about theinfluence of meteorological variables on PM10 emission from agricultural soils. The objective of this study was toidentify the most important meteorological variables involved in the emission of PM10, identify their thresholdvalues, 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 weremeasured during two years on a bare and flat surface that was tilled periodically. The meteorological variablesmeasured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soiltemperature. In 30% of the events, the PM10 concentration at 1.8 m height exceeded the average values allowedby the World Health Organization (50 μg m−3 for a 24 h period). Maximum values exceeded 1000 μg m−3. Theslope 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 wereconsistently above the 50 μg m−3 limit. The highest PM10 emission rates were observed when relative humidityvalues were below 20% and the air temperature was higher than 30 °C. In addition when the wind speedexceeded 8 m s−1, dust emission increased significantly. From a multiple regression analysis, results indicatedthat PM10 emission was well correlated (p< 0.001) with maximum wind speed, relative humidity, and airtemperature. 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 valueswere measured during events with a crusted surface, lower average values of Q were measured during eventswith a crust. Field observations indicated that the complex interaction between the weather conditions and soilsurface properties such as soil crusts, aggregate size distribution, soil moisture and even the soil condition whenthe tilling is done,
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. 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. Instituto Nacional de Tecnología Agropecuaria; Argentina
Materia
Fine
Particles
Erodibility
Meterological
Variables
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/44165

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network_name_str CONICET Digital (CONICET)
spelling Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholdsAvecilla, FernandoPanebianco, Juan EstebanBuschiazzo, Daniel EduardoFineParticlesErodibilityMeterologicalVariableshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Soil wind erosion and consequent PM10 emission is a complex process that has been related to surface propertiesand meteorological conditions. Most of the studies have emphasized on the relationship between the surfaceconditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about theinfluence of meteorological variables on PM10 emission from agricultural soils. The objective of this study was toidentify the most important meteorological variables involved in the emission of PM10, identify their thresholdvalues, 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 weremeasured during two years on a bare and flat surface that was tilled periodically. The meteorological variablesmeasured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soiltemperature. In 30% of the events, the PM10 concentration at 1.8 m height exceeded the average values allowedby the World Health Organization (50 μg m−3 for a 24 h period). Maximum values exceeded 1000 μg m−3. Theslope 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 wereconsistently above the 50 μg m−3 limit. The highest PM10 emission rates were observed when relative humidityvalues were below 20% and the air temperature was higher than 30 °C. In addition when the wind speedexceeded 8 m s−1, dust emission increased significantly. From a multiple regression analysis, results indicatedthat PM10 emission was well correlated (p< 0.001) with maximum wind speed, relative humidity, and airtemperature. 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 valueswere measured during events with a crusted surface, lower average values of Q were measured during eventswith a crust. Field observations indicated that the complex interaction between the weather conditions and soilsurface properties such as soil crusts, aggregate size distribution, soil moisture and even the soil condition whenthe tilling is done,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; 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. 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. Instituto Nacional de Tecnología Agropecuaria; ArgentinaElsevier Science2017-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/44165Avecilla, Fernando; Panebianco, Juan Esteban; Buschiazzo, Daniel Eduardo; Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds; Elsevier Science; Agricultural And Forest Meteorology; 244; 5-2017; 21-320168-1923CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.agrformet.2017.05.016info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0168192317301818info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-11-26T08:40:09Zoai:ri.conicet.gov.ar:11336/44165instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-11-26 08:40:10.288CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
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
Fine
Particles
Erodibility
Meterological
Variables
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 Fine
Particles
Erodibility
Meterological
Variables
topic Fine
Particles
Erodibility
Meterological
Variables
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Soil wind erosion and consequent PM10 emission is a complex process that has been related to surface propertiesand meteorological conditions. Most of the studies have emphasized on the relationship between the surfaceconditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about theinfluence of meteorological variables on PM10 emission from agricultural soils. The objective of this study was toidentify the most important meteorological variables involved in the emission of PM10, identify their thresholdvalues, 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 weremeasured during two years on a bare and flat surface that was tilled periodically. The meteorological variablesmeasured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soiltemperature. In 30% of the events, the PM10 concentration at 1.8 m height exceeded the average values allowedby the World Health Organization (50 μg m−3 for a 24 h period). Maximum values exceeded 1000 μg m−3. Theslope 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 wereconsistently above the 50 μg m−3 limit. The highest PM10 emission rates were observed when relative humidityvalues were below 20% and the air temperature was higher than 30 °C. In addition when the wind speedexceeded 8 m s−1, dust emission increased significantly. From a multiple regression analysis, results indicatedthat PM10 emission was well correlated (p< 0.001) with maximum wind speed, relative humidity, and airtemperature. 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 valueswere measured during events with a crusted surface, lower average values of Q were measured during eventswith a crust. Field observations indicated that the complex interaction between the weather conditions and soilsurface properties such as soil crusts, aggregate size distribution, soil moisture and even the soil condition whenthe tilling is done,
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. 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. Instituto Nacional de Tecnología Agropecuaria; Argentina
description Soil wind erosion and consequent PM10 emission is a complex process that has been related to surface propertiesand meteorological conditions. Most of the studies have emphasized on the relationship between the surfaceconditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about theinfluence of meteorological variables on PM10 emission from agricultural soils. The objective of this study was toidentify the most important meteorological variables involved in the emission of PM10, identify their thresholdvalues, 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 weremeasured during two years on a bare and flat surface that was tilled periodically. The meteorological variablesmeasured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soiltemperature. In 30% of the events, the PM10 concentration at 1.8 m height exceeded the average values allowedby the World Health Organization (50 μg m−3 for a 24 h period). Maximum values exceeded 1000 μg m−3. Theslope 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 wereconsistently above the 50 μg m−3 limit. The highest PM10 emission rates were observed when relative humidityvalues were below 20% and the air temperature was higher than 30 °C. In addition when the wind speedexceeded 8 m s−1, dust emission increased significantly. From a multiple regression analysis, results indicatedthat PM10 emission was well correlated (p< 0.001) with maximum wind speed, relative humidity, and airtemperature. 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 valueswere measured during events with a crusted surface, lower average values of Q were measured during eventswith a crust. Field observations indicated that the complex interaction between the weather conditions and soilsurface properties such as soil crusts, aggregate size distribution, soil moisture and even the soil condition whenthe tilling is done,
publishDate 2017
dc.date.none.fl_str_mv 2017-05
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/11336/44165
Avecilla, Fernando; Panebianco, Juan Esteban; Buschiazzo, Daniel Eduardo; Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds; Elsevier Science; Agricultural And Forest Meteorology; 244; 5-2017; 21-32
0168-1923
CONICET Digital
CONICET
url http://hdl.handle.net/11336/44165
identifier_str_mv Avecilla, Fernando; Panebianco, Juan Esteban; Buschiazzo, Daniel Eduardo; Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds; Elsevier Science; Agricultural And Forest Meteorology; 244; 5-2017; 21-32
0168-1923
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.agrformet.2017.05.016
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0168192317301818
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier Science
publisher.none.fl_str_mv Elsevier Science
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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