Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880
Main Author: | |
---|---|
Publication Date: | 2008 |
Other Authors: | , |
Format: | Article |
Language: | por |
Source: | Acta Scientiarum. Agronomy (Online) |
DOI: | 10.4025/actasciagron.v26i2.1880 |
Download full: | http://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1880 |
Summary: | The multiple evaluation forms of erosive individual-storm for the national researchers are undeniable. Therefore, the criteria to classify the erosive individual-storm, used in rainfall erosivity factor, as well as to study the correlation of the EI30 index with the erosion soil losses, were investigated in Sao Paulo State, Brazil. To study, analysis of simple individual-storm in Campinas, Mococa and Pindorama Experimental Stations (IAC). To study the correlation, analysis of simple linear regression, between the rainfall EI30 indexes and the respectives soil losses, were done to research the necessary statistical treatments to the establishment of the criteria of the erosive individual-storm. The conclusive analysis, were destined to two purposes. In the first case, with a view to study the correlation of the EI30 index with the erosion soil losses, the following criteria must be used: 1) to compute the EI30 index for all storms equal or greater than 10.0mm; 2) to compute the EI30 index for storms of less than 10.0mm only if they to show a precipitation equal or greater than 6.0mm in 15 minutes, and 3) to compute the EI30 index for all storms with erosion soil losses and/or runoff. Otherwise, with a view to determine the rainfall erosivity factor (R), to use the following criteria: 1) to compute the EI30 index for all storms equal or greater than 10.0mm, and 2) to compute the EI30 index for storms of less than 10.0mm only if they to show a precipitation equal or greater than 6.0mm in 15 minutes. |
id |
UEM-5_71b0af45cf7494ad735d575a6ad35103 |
---|---|
oai_identifier_str |
oai:periodicos.uem.br/ojs:article/1880 |
network_acronym_str |
UEM-5 |
network_name_str |
Acta Scientiarum. Agronomy (Online) |
spelling |
Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880Critérios de classificação de chuva individual erosiva para o Estado de São Paulo - DOI: 10.4025/actasciagron.v26i2.1880equação universal de perda de soloerosividade da chuvafator erosividade da chuvaerosão do solo5.00.00.00-4 Ciências AgráriasThe multiple evaluation forms of erosive individual-storm for the national researchers are undeniable. Therefore, the criteria to classify the erosive individual-storm, used in rainfall erosivity factor, as well as to study the correlation of the EI30 index with the erosion soil losses, were investigated in Sao Paulo State, Brazil. To study, analysis of simple individual-storm in Campinas, Mococa and Pindorama Experimental Stations (IAC). To study the correlation, analysis of simple linear regression, between the rainfall EI30 indexes and the respectives soil losses, were done to research the necessary statistical treatments to the establishment of the criteria of the erosive individual-storm. The conclusive analysis, were destined to two purposes. In the first case, with a view to study the correlation of the EI30 index with the erosion soil losses, the following criteria must be used: 1) to compute the EI30 index for all storms equal or greater than 10.0mm; 2) to compute the EI30 index for storms of less than 10.0mm only if they to show a precipitation equal or greater than 6.0mm in 15 minutes, and 3) to compute the EI30 index for all storms with erosion soil losses and/or runoff. Otherwise, with a view to determine the rainfall erosivity factor (R), to use the following criteria: 1) to compute the EI30 index for all storms equal or greater than 10.0mm, and 2) to compute the EI30 index for storms of less than 10.0mm only if they to show a precipitation equal or greater than 6.0mm in 15 minutes.As múltiplas formas de conceituação da chuva individual erosiva pelos pesquisadores nacionais são notórias. Neste trabalho, foram estudados os critérios para conceituação de chuva individual erosiva para o Estado de São Paulo, destinados ao estudo do fator erosividade da chuva, como também para o estudo da correlação do EI30 com as perdas de solo por erosão. Foram analisadas as chuvas das Estações Experimentais de Conservação do Solo de Campinas, Mococa e Pindorama (IAC). Para o estudo de correlação, foram feitas análises de regressão linear simples, entre os EI30 das chuvas e as respectivas perdas de solo, de forma a investigar as situações estatísticas necessárias ao estabelecimento dos critérios conceituais de chuva individual erosiva. A análise final possibilitou concluir que, quando o propósito do estudo for o de correlação do EI30 com as perdas de solo por erosão, devem ser adotados os seguintes critérios: 1) considerar todas as chuvas maiores ou iguais a 10,0mm; 2) considerar aquelas menores do que 10,0mm se apresentarem uma quantidade maior ou igual a 6,0mm em 15 minutos e 3) considerar todas as que apresentaram perda de solo por erosão e/ou enxurrada. Por outro lado, quando o propósito do estudo for o de determinação do fator erosividade da chuva , tais critérios devem ser: 1) considerar todas as chuvas maiores ou iguais a 10,0mm e 2) considerar aquelas menores do que 10,0mm se apresentarem uma quantidade maior ou igual a 6,0mm em 15 minutos.Universidade Estadual de Maringá2008-04-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/188010.4025/actasciagron.v26i2.1880Acta Scientiarum. Agronomy; Vol 26 No 2 (2004); 175-183Acta Scientiarum. Agronomy; v. 26 n. 2 (2004); 175-1831807-86211679-9275reponame:Acta Scientiarum. Agronomy (Online)instname:Universidade Estadual de Maringá (UEM)instacron:UEMporhttp://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1880/1293Carvalho, Morel de Passos eFreddi, Onã da SilvaVeronese Junior, Valdenirinfo:eu-repo/semantics/openAccess2022-11-23T18:37:35Zoai:periodicos.uem.br/ojs:article/1880Revistahttp://www.periodicos.uem.br/ojs/index.php/ActaSciAgronPUBhttp://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/oaiactaagron@uem.br||actaagron@uem.br|| edamasio@uem.br1807-86211679-9275opendoar:2022-11-23T18:37:35Acta Scientiarum. Agronomy (Online) - Universidade Estadual de Maringá (UEM)false |
dc.title.none.fl_str_mv |
Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 Critérios de classificação de chuva individual erosiva para o Estado de São Paulo - DOI: 10.4025/actasciagron.v26i2.1880 |
title |
Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 |
spellingShingle |
Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 Carvalho, Morel de Passos e equação universal de perda de solo erosividade da chuva fator erosividade da chuva erosão do solo 5.00.00.00-4 Ciências Agrárias Carvalho, Morel de Passos e equação universal de perda de solo erosividade da chuva fator erosividade da chuva erosão do solo 5.00.00.00-4 Ciências Agrárias |
title_short |
Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 |
title_full |
Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 |
title_fullStr |
Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 |
title_full_unstemmed |
Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 |
title_sort |
Classification criteria of erosive individual-storm in the São Paulo state - DOI: 10.4025/actasciagron.v26i2.1880 |
author |
Carvalho, Morel de Passos e |
author_facet |
Carvalho, Morel de Passos e Carvalho, Morel de Passos e Freddi, Onã da Silva Veronese Junior, Valdenir Freddi, Onã da Silva Veronese Junior, Valdenir |
author_role |
author |
author2 |
Freddi, Onã da Silva Veronese Junior, Valdenir |
author2_role |
author author |
dc.contributor.author.fl_str_mv |
Carvalho, Morel de Passos e Freddi, Onã da Silva Veronese Junior, Valdenir |
dc.subject.por.fl_str_mv |
equação universal de perda de solo erosividade da chuva fator erosividade da chuva erosão do solo 5.00.00.00-4 Ciências Agrárias |
topic |
equação universal de perda de solo erosividade da chuva fator erosividade da chuva erosão do solo 5.00.00.00-4 Ciências Agrárias |
description |
The multiple evaluation forms of erosive individual-storm for the national researchers are undeniable. Therefore, the criteria to classify the erosive individual-storm, used in rainfall erosivity factor, as well as to study the correlation of the EI30 index with the erosion soil losses, were investigated in Sao Paulo State, Brazil. To study, analysis of simple individual-storm in Campinas, Mococa and Pindorama Experimental Stations (IAC). To study the correlation, analysis of simple linear regression, between the rainfall EI30 indexes and the respectives soil losses, were done to research the necessary statistical treatments to the establishment of the criteria of the erosive individual-storm. The conclusive analysis, were destined to two purposes. In the first case, with a view to study the correlation of the EI30 index with the erosion soil losses, the following criteria must be used: 1) to compute the EI30 index for all storms equal or greater than 10.0mm; 2) to compute the EI30 index for storms of less than 10.0mm only if they to show a precipitation equal or greater than 6.0mm in 15 minutes, and 3) to compute the EI30 index for all storms with erosion soil losses and/or runoff. Otherwise, with a view to determine the rainfall erosivity factor (R), to use the following criteria: 1) to compute the EI30 index for all storms equal or greater than 10.0mm, and 2) to compute the EI30 index for storms of less than 10.0mm only if they to show a precipitation equal or greater than 6.0mm in 15 minutes. |
publishDate |
2008 |
dc.date.none.fl_str_mv |
2008-04-11 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1880 10.4025/actasciagron.v26i2.1880 |
url |
http://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1880 |
identifier_str_mv |
10.4025/actasciagron.v26i2.1880 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
http://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1880/1293 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Estadual de Maringá |
publisher.none.fl_str_mv |
Universidade Estadual de Maringá |
dc.source.none.fl_str_mv |
Acta Scientiarum. Agronomy; Vol 26 No 2 (2004); 175-183 Acta Scientiarum. Agronomy; v. 26 n. 2 (2004); 175-183 1807-8621 1679-9275 reponame:Acta Scientiarum. Agronomy (Online) instname:Universidade Estadual de Maringá (UEM) instacron:UEM |
instname_str |
Universidade Estadual de Maringá (UEM) |
instacron_str |
UEM |
institution |
UEM |
reponame_str |
Acta Scientiarum. Agronomy (Online) |
collection |
Acta Scientiarum. Agronomy (Online) |
repository.name.fl_str_mv |
Acta Scientiarum. Agronomy (Online) - Universidade Estadual de Maringá (UEM) |
repository.mail.fl_str_mv |
actaagron@uem.br||actaagron@uem.br|| edamasio@uem.br |
_version_ |
1822182768368418816 |
dc.identifier.doi.none.fl_str_mv |
10.4025/actasciagron.v26i2.1880 |