Use of the Time Domain Reflectometry to evaluate the nitrate distribution in fertirrigated soils columns

The monitoring of spatial and temporal variation of the soil water content (θ), of the soil bulk electric conductivity (CEs), of the soil solution electric conductivity (CEss) and of the ion concentration (Ci) enables to estimate the water loss by deep percolation and evapotranspiration, to determin...

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Main Authors: Rubens Alves de Oliveira, Antonio Teixeira de Matos, Mauro Aparecido Martinez, Marcelo Rocha dos Santos, João Henrique Zonta
Format: Article
Language:English
Published: Instituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi) 2009-12-01
Series:Revista Ambiente & Água
Subjects:
TDR
Online Access:http://www.ambi-agua.net/seer/index.php/ambi-agua/article/view/296
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spelling doaj-ef4ceb78163d49b6b0a551ac4eab7b6d2020-11-25T00:52:43ZengInstituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi)Revista Ambiente & Água1980-993X2009-12-0143678110.4136/ambi-agua.296Use of the Time Domain Reflectometry to evaluate the nitrate distribution in fertirrigated soils columnsRubens Alves de OliveiraAntonio Teixeira de MatosMauro Aparecido MartinezMarcelo Rocha dos SantosJoão Henrique ZontaThe monitoring of spatial and temporal variation of the soil water content (θ), of the soil bulk electric conductivity (CEs), of the soil solution electric conductivity (CEss) and of the ion concentration (Ci) enables to estimate the water loss by deep percolation and evapotranspiration, to determine the areas of nutrients extraction by plants and the possible nutrients loss by leaching. The of objective this work was to evaluate, using the TDR technique, the nitrate distribution in Typic Quartzipsamment (RQ) and Oxisol (LV) soil columns fertirrigated with calcium nitrate. Nitrate fertirrigations were accomplished in the columns, and the soil water content (θ) and the soil bulk electric conductivity (CEs) obtained with TDR. The nitrate concentration was estimated using the values of θ and of CEs. In the RQ soil, the nitrate reached 30, 21 e 12 cm when the fertirrigations were done at the beginning, at the middle and at the end of the irrigation period, respectively. In the LV soil, independently of the moment of the fertirrigation, the nitrate was retained in the layer from 0 to 12 cm deep.http://www.ambi-agua.net/seer/index.php/ambi-agua/article/view/296FertirrigationNitrate movementTDR
collection DOAJ
language English
format Article
sources DOAJ
author Rubens Alves de Oliveira
Antonio Teixeira de Matos
Mauro Aparecido Martinez
Marcelo Rocha dos Santos
João Henrique Zonta
spellingShingle Rubens Alves de Oliveira
Antonio Teixeira de Matos
Mauro Aparecido Martinez
Marcelo Rocha dos Santos
João Henrique Zonta
Use of the Time Domain Reflectometry to evaluate the nitrate distribution in fertirrigated soils columns
Revista Ambiente & Água
Fertirrigation
Nitrate movement
TDR
author_facet Rubens Alves de Oliveira
Antonio Teixeira de Matos
Mauro Aparecido Martinez
Marcelo Rocha dos Santos
João Henrique Zonta
author_sort Rubens Alves de Oliveira
title Use of the Time Domain Reflectometry to evaluate the nitrate distribution in fertirrigated soils columns
title_short Use of the Time Domain Reflectometry to evaluate the nitrate distribution in fertirrigated soils columns
title_full Use of the Time Domain Reflectometry to evaluate the nitrate distribution in fertirrigated soils columns
title_fullStr Use of the Time Domain Reflectometry to evaluate the nitrate distribution in fertirrigated soils columns
title_full_unstemmed Use of the Time Domain Reflectometry to evaluate the nitrate distribution in fertirrigated soils columns
title_sort use of the time domain reflectometry to evaluate the nitrate distribution in fertirrigated soils columns
publisher Instituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi)
series Revista Ambiente & Água
issn 1980-993X
publishDate 2009-12-01
description The monitoring of spatial and temporal variation of the soil water content (θ), of the soil bulk electric conductivity (CEs), of the soil solution electric conductivity (CEss) and of the ion concentration (Ci) enables to estimate the water loss by deep percolation and evapotranspiration, to determine the areas of nutrients extraction by plants and the possible nutrients loss by leaching. The of objective this work was to evaluate, using the TDR technique, the nitrate distribution in Typic Quartzipsamment (RQ) and Oxisol (LV) soil columns fertirrigated with calcium nitrate. Nitrate fertirrigations were accomplished in the columns, and the soil water content (θ) and the soil bulk electric conductivity (CEs) obtained with TDR. The nitrate concentration was estimated using the values of θ and of CEs. In the RQ soil, the nitrate reached 30, 21 e 12 cm when the fertirrigations were done at the beginning, at the middle and at the end of the irrigation period, respectively. In the LV soil, independently of the moment of the fertirrigation, the nitrate was retained in the layer from 0 to 12 cm deep.
topic Fertirrigation
Nitrate movement
TDR
url http://www.ambi-agua.net/seer/index.php/ambi-agua/article/view/296
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