Derivation of plaint growth coeficients for the use in wind erosion models in Argentina
- Autores
- Mendez, Mariano Javier; Buschiazzo, Daniel Eduardo
- Año de publicación
- 2008
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Relationships between wind erosion soil loss ratio (SLR, the quotient between the soil loss in a ground cover and a bare and smooth soil) and the percent of soil coverage with plant residues or canopy have been mostly obtained by means of wind tunnel experiments where fluid-dynamic parameters, driven in the nature by climatic conditions, can be maintained constant. To test the behavior of SLR under natural conditions, we compared wind erosion measured in the field in a semiarid environment of Argentina, during 3 sunflower (Helianthus annus) and 3 corn (Zea mays) growth periods, with wind erosion calculated with available equations. Results showed that the relationship between measured SLR and percentage of soil cover with flat residues fitted well to the already available equation SLRf = e, where SC is the soil cover with flat residues and a is a constant, but with an a coefficient of 0.0605 instead of the originally provided 0.0438. This resulted in an averaged difference in the SLR of 37% between both equations. The variation in SLR was attributed to differences in the highest speeds used for the derivation of the original a coefficient (16 m s) than wind speeds occurring during field measurements in this study (10.8 m s, in average). The relationship between SLR and soil coverage with flat residues for storms with erosion amounts higher than 100 kg ha had an a coefficient of 0.039, very close to the original a coefficient. Measured SLR as a function of soil cover with corn and sunflower canopy was quite similar to calculations made with the previously available equation, where cc is the fraction of soil surface covered with crop canopy. The published equation, where pgca and pgcb are constants and Pd the days after seeding, was not adequate to explain the evolution of the percentage of soil cover by the crops. This equation was replaced by, where a, b, and c are constants and x is the days after seeding. SLR calculated on the basis of field measurements was, as a function of the days after corn seeding, lower than SLR calculated with available equations at early-crop growth stages and higher at late-crop growth stages. At early-crop growth stages, a critical period for wind erosion occurrence due to the low soil coverage with plants, sunflower had a better wind erosion control efficiency than corn. Sunflower also increased its wind erosion control efficiency with favorable climatic conditions, whereas corn efficiency remained unchanged. Such differences were attributed to the canopy leaf arrangement of each crop (planophyles in sunflower and erectophyles in corn), which resulted in a more effective reduction of wind speed by sunflower leaves than by the narrow leaves of the corn at same growth stages. On the other hand, sunflower had a more efficient use of the solar radiation and a faster canopy growth. We conclude that the equations developed here for use in empirical wind erosion prediction models produce reliable results, even under variable climatic conditions. Such models are useful for sites like the semiarid Pampas, where detailed climatic information is lacking.
Fil: Mendez, Mariano Javier. 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 - Materia
-
Semiarid Regions
Soil Canopy Cover
Soil Plant Residue Cover
Wind Erosion - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/81738
Ver los metadatos del registro completo
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Derivation of plaint growth coeficients for the use in wind erosion models in ArgentinaMendez, Mariano JavierBuschiazzo, Daniel EduardoSemiarid RegionsSoil Canopy CoverSoil Plant Residue CoverWind Erosionhttps://purl.org/becyt/ford/4.1https://purl.org/becyt/ford/4Relationships between wind erosion soil loss ratio (SLR, the quotient between the soil loss in a ground cover and a bare and smooth soil) and the percent of soil coverage with plant residues or canopy have been mostly obtained by means of wind tunnel experiments where fluid-dynamic parameters, driven in the nature by climatic conditions, can be maintained constant. To test the behavior of SLR under natural conditions, we compared wind erosion measured in the field in a semiarid environment of Argentina, during 3 sunflower (Helianthus annus) and 3 corn (Zea mays) growth periods, with wind erosion calculated with available equations. Results showed that the relationship between measured SLR and percentage of soil cover with flat residues fitted well to the already available equation SLRf = e, where SC is the soil cover with flat residues and a is a constant, but with an a coefficient of 0.0605 instead of the originally provided 0.0438. This resulted in an averaged difference in the SLR of 37% between both equations. The variation in SLR was attributed to differences in the highest speeds used for the derivation of the original a coefficient (16 m s) than wind speeds occurring during field measurements in this study (10.8 m s, in average). The relationship between SLR and soil coverage with flat residues for storms with erosion amounts higher than 100 kg ha had an a coefficient of 0.039, very close to the original a coefficient. Measured SLR as a function of soil cover with corn and sunflower canopy was quite similar to calculations made with the previously available equation, where cc is the fraction of soil surface covered with crop canopy. The published equation, where pgca and pgcb are constants and Pd the days after seeding, was not adequate to explain the evolution of the percentage of soil cover by the crops. This equation was replaced by, where a, b, and c are constants and x is the days after seeding. SLR calculated on the basis of field measurements was, as a function of the days after corn seeding, lower than SLR calculated with available equations at early-crop growth stages and higher at late-crop growth stages. At early-crop growth stages, a critical period for wind erosion occurrence due to the low soil coverage with plants, sunflower had a better wind erosion control efficiency than corn. Sunflower also increased its wind erosion control efficiency with favorable climatic conditions, whereas corn efficiency remained unchanged. Such differences were attributed to the canopy leaf arrangement of each crop (planophyles in sunflower and erectophyles in corn), which resulted in a more effective reduction of wind speed by sunflower leaves than by the narrow leaves of the corn at same growth stages. On the other hand, sunflower had a more efficient use of the solar radiation and a faster canopy growth. We conclude that the equations developed here for use in empirical wind erosion prediction models produce reliable results, even under variable climatic conditions. Such models are useful for sites like the semiarid Pampas, where detailed climatic information is lacking.Fil: Mendez, Mariano Javier. 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; ArgentinaLippincott Williams2008-08info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/81738Mendez, Mariano Javier; Buschiazzo, Daniel Eduardo; Derivation of plaint growth coeficients for the use in wind erosion models in Argentina; Lippincott Williams; Soil Science; 173; 8; 8-2008; 468-4790038-075XCONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://journals.lww.com/soilsci/Abstract/2008/07000/DERIVATION_OF_PLANT_GROWTH_COEFFICIENTS_FOR_THE.5.aspxinfo:eu-repo/semantics/altIdentifier/doi/10.1097/SS.0b013e31817b666cinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:21:48Zoai:ri.conicet.gov.ar:11336/81738instacron: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:34982025-10-22 11:21:48.557CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Derivation of plaint growth coeficients for the use in wind erosion models in Argentina |
| title |
Derivation of plaint growth coeficients for the use in wind erosion models in Argentina |
| spellingShingle |
Derivation of plaint growth coeficients for the use in wind erosion models in Argentina Mendez, Mariano Javier Semiarid Regions Soil Canopy Cover Soil Plant Residue Cover Wind Erosion |
| title_short |
Derivation of plaint growth coeficients for the use in wind erosion models in Argentina |
| title_full |
Derivation of plaint growth coeficients for the use in wind erosion models in Argentina |
| title_fullStr |
Derivation of plaint growth coeficients for the use in wind erosion models in Argentina |
| title_full_unstemmed |
Derivation of plaint growth coeficients for the use in wind erosion models in Argentina |
| title_sort |
Derivation of plaint growth coeficients for the use in wind erosion models in Argentina |
| dc.creator.none.fl_str_mv |
Mendez, Mariano Javier Buschiazzo, Daniel Eduardo |
| author |
Mendez, Mariano Javier |
| author_facet |
Mendez, Mariano Javier Buschiazzo, Daniel Eduardo |
| author_role |
author |
| author2 |
Buschiazzo, Daniel Eduardo |
| author2_role |
author |
| dc.subject.none.fl_str_mv |
Semiarid Regions Soil Canopy Cover Soil Plant Residue Cover Wind Erosion |
| topic |
Semiarid Regions Soil Canopy Cover Soil Plant Residue Cover Wind Erosion |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/4.1 https://purl.org/becyt/ford/4 |
| dc.description.none.fl_txt_mv |
Relationships between wind erosion soil loss ratio (SLR, the quotient between the soil loss in a ground cover and a bare and smooth soil) and the percent of soil coverage with plant residues or canopy have been mostly obtained by means of wind tunnel experiments where fluid-dynamic parameters, driven in the nature by climatic conditions, can be maintained constant. To test the behavior of SLR under natural conditions, we compared wind erosion measured in the field in a semiarid environment of Argentina, during 3 sunflower (Helianthus annus) and 3 corn (Zea mays) growth periods, with wind erosion calculated with available equations. Results showed that the relationship between measured SLR and percentage of soil cover with flat residues fitted well to the already available equation SLRf = e, where SC is the soil cover with flat residues and a is a constant, but with an a coefficient of 0.0605 instead of the originally provided 0.0438. This resulted in an averaged difference in the SLR of 37% between both equations. The variation in SLR was attributed to differences in the highest speeds used for the derivation of the original a coefficient (16 m s) than wind speeds occurring during field measurements in this study (10.8 m s, in average). The relationship between SLR and soil coverage with flat residues for storms with erosion amounts higher than 100 kg ha had an a coefficient of 0.039, very close to the original a coefficient. Measured SLR as a function of soil cover with corn and sunflower canopy was quite similar to calculations made with the previously available equation, where cc is the fraction of soil surface covered with crop canopy. The published equation, where pgca and pgcb are constants and Pd the days after seeding, was not adequate to explain the evolution of the percentage of soil cover by the crops. This equation was replaced by, where a, b, and c are constants and x is the days after seeding. SLR calculated on the basis of field measurements was, as a function of the days after corn seeding, lower than SLR calculated with available equations at early-crop growth stages and higher at late-crop growth stages. At early-crop growth stages, a critical period for wind erosion occurrence due to the low soil coverage with plants, sunflower had a better wind erosion control efficiency than corn. Sunflower also increased its wind erosion control efficiency with favorable climatic conditions, whereas corn efficiency remained unchanged. Such differences were attributed to the canopy leaf arrangement of each crop (planophyles in sunflower and erectophyles in corn), which resulted in a more effective reduction of wind speed by sunflower leaves than by the narrow leaves of the corn at same growth stages. On the other hand, sunflower had a more efficient use of the solar radiation and a faster canopy growth. We conclude that the equations developed here for use in empirical wind erosion prediction models produce reliable results, even under variable climatic conditions. Such models are useful for sites like the semiarid Pampas, where detailed climatic information is lacking. Fil: Mendez, Mariano Javier. 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 |
| description |
Relationships between wind erosion soil loss ratio (SLR, the quotient between the soil loss in a ground cover and a bare and smooth soil) and the percent of soil coverage with plant residues or canopy have been mostly obtained by means of wind tunnel experiments where fluid-dynamic parameters, driven in the nature by climatic conditions, can be maintained constant. To test the behavior of SLR under natural conditions, we compared wind erosion measured in the field in a semiarid environment of Argentina, during 3 sunflower (Helianthus annus) and 3 corn (Zea mays) growth periods, with wind erosion calculated with available equations. Results showed that the relationship between measured SLR and percentage of soil cover with flat residues fitted well to the already available equation SLRf = e, where SC is the soil cover with flat residues and a is a constant, but with an a coefficient of 0.0605 instead of the originally provided 0.0438. This resulted in an averaged difference in the SLR of 37% between both equations. The variation in SLR was attributed to differences in the highest speeds used for the derivation of the original a coefficient (16 m s) than wind speeds occurring during field measurements in this study (10.8 m s, in average). The relationship between SLR and soil coverage with flat residues for storms with erosion amounts higher than 100 kg ha had an a coefficient of 0.039, very close to the original a coefficient. Measured SLR as a function of soil cover with corn and sunflower canopy was quite similar to calculations made with the previously available equation, where cc is the fraction of soil surface covered with crop canopy. The published equation, where pgca and pgcb are constants and Pd the days after seeding, was not adequate to explain the evolution of the percentage of soil cover by the crops. This equation was replaced by, where a, b, and c are constants and x is the days after seeding. SLR calculated on the basis of field measurements was, as a function of the days after corn seeding, lower than SLR calculated with available equations at early-crop growth stages and higher at late-crop growth stages. At early-crop growth stages, a critical period for wind erosion occurrence due to the low soil coverage with plants, sunflower had a better wind erosion control efficiency than corn. Sunflower also increased its wind erosion control efficiency with favorable climatic conditions, whereas corn efficiency remained unchanged. Such differences were attributed to the canopy leaf arrangement of each crop (planophyles in sunflower and erectophyles in corn), which resulted in a more effective reduction of wind speed by sunflower leaves than by the narrow leaves of the corn at same growth stages. On the other hand, sunflower had a more efficient use of the solar radiation and a faster canopy growth. We conclude that the equations developed here for use in empirical wind erosion prediction models produce reliable results, even under variable climatic conditions. Such models are useful for sites like the semiarid Pampas, where detailed climatic information is lacking. |
| publishDate |
2008 |
| dc.date.none.fl_str_mv |
2008-08 |
| 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 |
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article |
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publishedVersion |
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http://hdl.handle.net/11336/81738 Mendez, Mariano Javier; Buschiazzo, Daniel Eduardo; Derivation of plaint growth coeficients for the use in wind erosion models in Argentina; Lippincott Williams; Soil Science; 173; 8; 8-2008; 468-479 0038-075X CONICET Digital CONICET |
| url |
http://hdl.handle.net/11336/81738 |
| identifier_str_mv |
Mendez, Mariano Javier; Buschiazzo, Daniel Eduardo; Derivation of plaint growth coeficients for the use in wind erosion models in Argentina; Lippincott Williams; Soil Science; 173; 8; 8-2008; 468-479 0038-075X CONICET Digital CONICET |
| dc.language.none.fl_str_mv |
eng |
| language |
eng |
| dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://journals.lww.com/soilsci/Abstract/2008/07000/DERIVATION_OF_PLANT_GROWTH_COEFFICIENTS_FOR_THE.5.aspx info:eu-repo/semantics/altIdentifier/doi/10.1097/SS.0b013e31817b666c |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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openAccess |
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https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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application/pdf application/pdf |
| dc.publisher.none.fl_str_mv |
Lippincott Williams |
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Lippincott Williams |
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reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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