Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizing
Autor(a) principal: | |
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Data de Publicação: | 2012 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Coffee Science (Online) |
Texto Completo: | https://coffeescience.ufla.br/index.php/Coffeescience/article/view/522 |
Resumo: | The objective of this study was to characterize the soil pH in function of chemical fertilizing through irrigation, andmanually, under the canopy. The crop was drip irrigated during the whole year when water soil tension was 21 kPa. The depth of waterwas defined based on the average reading of soil water potential at 0.10 and 0.30m depths. Soil solution extractors were installed atdepths of 0.10, 0.20, 0.30, 0.40 and 0.50 m and distanced from the plant at 0.10, 0.20, 0.30, 0.40 and 0.50 m. The soil pH wasmonitored in the fertilizing period for 2 seasons (2008/2009 and 2009/2010). Evaluation was carried out 24 hours after eachapplication of fertilizer until at least sixty days after the last parceling. Exponential and spherical semi-variogram models wereadjusted applying minimum weighted square and maximum likelihood methodologies, testing the adherence based on spatial dependencedegree and cross validation. The mapping was done based on the best adjusted semi-variogram, using kriging. The results showedthat soil solution pH present spatial dependence in the area sampled. The sources and rates of fertilizer used promoted the alkalinizationof the solution. Soil solution pH tends to be lower in the area with fertigation. |
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Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizingVariabilidade espacial do pH em área com cafeeiro fertirrigado e sistema tradicionalDrip irrigationpHcoffea arabica L.nutrientsgeostatisticsGotejamentopHCoffea arabica L.nutrientesgeoestatísticaThe objective of this study was to characterize the soil pH in function of chemical fertilizing through irrigation, andmanually, under the canopy. The crop was drip irrigated during the whole year when water soil tension was 21 kPa. The depth of waterwas defined based on the average reading of soil water potential at 0.10 and 0.30m depths. Soil solution extractors were installed atdepths of 0.10, 0.20, 0.30, 0.40 and 0.50 m and distanced from the plant at 0.10, 0.20, 0.30, 0.40 and 0.50 m. The soil pH wasmonitored in the fertilizing period for 2 seasons (2008/2009 and 2009/2010). Evaluation was carried out 24 hours after eachapplication of fertilizer until at least sixty days after the last parceling. Exponential and spherical semi-variogram models wereadjusted applying minimum weighted square and maximum likelihood methodologies, testing the adherence based on spatial dependencedegree and cross validation. The mapping was done based on the best adjusted semi-variogram, using kriging. The results showedthat soil solution pH present spatial dependence in the area sampled. The sources and rates of fertilizer used promoted the alkalinizationof the solution. Soil solution pH tends to be lower in the area with fertigation.Objetivou-se, no trabalho, caracterizar o pH no perfil do solo em função da adubação química aplicada via fertirrigação e,manualmente, sob a copa da planta. A cultura foi irrigada por gotejamento. A irrigação foi realizada quando a tensão média observadaem sensores “Watermarck”, instalados a 0,10 m de profundidade atingia 21 kPa. Calculou-se a lâmina com base na média de leitura dopotencial de água no solo observada nas profundidades de 0,10 e 0,30 m. Sob a copa das plantas, na região do bulbo molhado, foraminstalados 25 extratores de solução do solo a 0,10; 0,20; 0,30; 0,40 e 0,50 m de profundidade e distantes da planta de 0,10; 0,20; 0,30,0,40 e 0,50 m. A amostragem foi realizada em plantas irrigadas e não irrigadas no período de adubação (outubro a março), durante doisanos (2008/2009 e 2009/2010). As avaliações de pH foram realizadas a partir de 24 horas após cada aplicação de adubo até, pelomenos, sessenta dias após o último parcelamento. Os modelos de semi-variograma exponencial e esférico foram ajustados pelosmétodos dos mínimos quadrados ponderados e máxima verossimilhança. O mapeamento foi feito utilizando-se o interpoladorgeoestatístico. Os resultados mostraram que, para as plantas irrigadas e não irrigadas, o pH da solução do solo apresentou dependênciaespacial. As fontes e doses de adubo utilizado promoveram a alcalinização da solução do solo, no período avaliado. O pH da soluçãodo solo tende a ser menor na área em que a aplicação dos fertilizante foi realizada via fertirrigação.Editora UFLA2012-10-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://coffeescience.ufla.br/index.php/Coffeescience/article/view/522Coffee Science - ISSN 1984-3909; Vol. 7 No. 3 (2012); 198-207Coffee Science; Vol. 7 Núm. 3 (2012); 198-207Coffee Science; v. 7 n. 3 (2012); 198-2071984-3909reponame:Coffee Science (Online)instname:Universidade Federal de Lavras (UFLA)instacron:UFLAporhttps://coffeescience.ufla.br/index.php/Coffeescience/article/view/522/372Copyright (c) 2012 Coffee Science - ISSN 1984-3909https://creativecommons.org/info:eu-repo/semantics/openAccessRezende, Fátima ConceiçãoRibeiro, Victor BarbiereÁvila, Leo FernandesFaria, Manoel Alves deSilva, Elio Lemos da2013-02-24T14:23:09Zoai:coffeescience.ufla.br:article/522Revistahttps://coffeescience.ufla.br/index.php/CoffeesciencePUBhttps://coffeescience.ufla.br/index.php/Coffeescience/oaicoffeescience@dag.ufla.br||coffeescience@dag.ufla.br|| alvaro-cozadi@hotmail.com1984-39091809-6875opendoar:2024-05-21T19:53:43.819737Coffee Science (Online) - Universidade Federal de Lavras (UFLA)true |
dc.title.none.fl_str_mv |
Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizing Variabilidade espacial do pH em área com cafeeiro fertirrigado e sistema tradicional |
title |
Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizing |
spellingShingle |
Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizing Rezende, Fátima Conceição Drip irrigation pH coffea arabica L. nutrients geostatistics Gotejamento pH Coffea arabica L. nutrientes geoestatística |
title_short |
Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizing |
title_full |
Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizing |
title_fullStr |
Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizing |
title_full_unstemmed |
Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizing |
title_sort |
Spatial variability of pH in coffee plants under fertigation and traditional system of fertilizing |
author |
Rezende, Fátima Conceição |
author_facet |
Rezende, Fátima Conceição Ribeiro, Victor Barbiere Ávila, Leo Fernandes Faria, Manoel Alves de Silva, Elio Lemos da |
author_role |
author |
author2 |
Ribeiro, Victor Barbiere Ávila, Leo Fernandes Faria, Manoel Alves de Silva, Elio Lemos da |
author2_role |
author author author author |
dc.contributor.author.fl_str_mv |
Rezende, Fátima Conceição Ribeiro, Victor Barbiere Ávila, Leo Fernandes Faria, Manoel Alves de Silva, Elio Lemos da |
dc.subject.por.fl_str_mv |
Drip irrigation pH coffea arabica L. nutrients geostatistics Gotejamento pH Coffea arabica L. nutrientes geoestatística |
topic |
Drip irrigation pH coffea arabica L. nutrients geostatistics Gotejamento pH Coffea arabica L. nutrientes geoestatística |
description |
The objective of this study was to characterize the soil pH in function of chemical fertilizing through irrigation, andmanually, under the canopy. The crop was drip irrigated during the whole year when water soil tension was 21 kPa. The depth of waterwas defined based on the average reading of soil water potential at 0.10 and 0.30m depths. Soil solution extractors were installed atdepths of 0.10, 0.20, 0.30, 0.40 and 0.50 m and distanced from the plant at 0.10, 0.20, 0.30, 0.40 and 0.50 m. The soil pH wasmonitored in the fertilizing period for 2 seasons (2008/2009 and 2009/2010). Evaluation was carried out 24 hours after eachapplication of fertilizer until at least sixty days after the last parceling. Exponential and spherical semi-variogram models wereadjusted applying minimum weighted square and maximum likelihood methodologies, testing the adherence based on spatial dependencedegree and cross validation. The mapping was done based on the best adjusted semi-variogram, using kriging. The results showedthat soil solution pH present spatial dependence in the area sampled. The sources and rates of fertilizer used promoted the alkalinizationof the solution. Soil solution pH tends to be lower in the area with fertigation. |
publishDate |
2012 |
dc.date.none.fl_str_mv |
2012-10-05 |
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 |
https://coffeescience.ufla.br/index.php/Coffeescience/article/view/522 |
url |
https://coffeescience.ufla.br/index.php/Coffeescience/article/view/522 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://coffeescience.ufla.br/index.php/Coffeescience/article/view/522/372 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2012 Coffee Science - ISSN 1984-3909 https://creativecommons.org/ info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2012 Coffee Science - ISSN 1984-3909 https://creativecommons.org/ |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Editora UFLA |
publisher.none.fl_str_mv |
Editora UFLA |
dc.source.none.fl_str_mv |
Coffee Science - ISSN 1984-3909; Vol. 7 No. 3 (2012); 198-207 Coffee Science; Vol. 7 Núm. 3 (2012); 198-207 Coffee Science; v. 7 n. 3 (2012); 198-207 1984-3909 reponame:Coffee Science (Online) instname:Universidade Federal de Lavras (UFLA) instacron:UFLA |
instname_str |
Universidade Federal de Lavras (UFLA) |
instacron_str |
UFLA |
institution |
UFLA |
reponame_str |
Coffee Science (Online) |
collection |
Coffee Science (Online) |
repository.name.fl_str_mv |
Coffee Science (Online) - Universidade Federal de Lavras (UFLA) |
repository.mail.fl_str_mv |
coffeescience@dag.ufla.br||coffeescience@dag.ufla.br|| alvaro-cozadi@hotmail.com |
_version_ |
1799874919593410560 |