Soil moisture assessed by digital mapping techniques and its field validation

Digital techniques and tools can assist not only in the prediction of soil properties, such as soil moisture, but also in planning the use and management of areas for agriculture and, or, environmental purposes. In this sense, this work aimed to study wetness indexes methods, defining the spatial re...

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Main Authors: Bruno Montoani Silva, Sérgio Henrique Godinho Silva, Geraldo Cesár de Oliveira, Petrus Hubertus Caspar Rosa Peters, Walbert Júnior Reis dos Santos, Nilton Curi
Format: Article
Language:English
Published: Universidade Federal de Lavras 2014-04-01
Series:Ciência e Agrotecnologia
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1413-70542014000200005&lng=en&tlng=en
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author Bruno Montoani Silva
Sérgio Henrique Godinho Silva
Geraldo Cesár de Oliveira
Petrus Hubertus Caspar Rosa Peters
Walbert Júnior Reis dos Santos
Nilton Curi
author_facet Bruno Montoani Silva
Sérgio Henrique Godinho Silva
Geraldo Cesár de Oliveira
Petrus Hubertus Caspar Rosa Peters
Walbert Júnior Reis dos Santos
Nilton Curi
author_sort Bruno Montoani Silva
collection DOAJ
description Digital techniques and tools can assist not only in the prediction of soil properties, such as soil moisture, but also in planning the use and management of areas for agriculture and, or, environmental purposes. In this sense, this work aimed to study wetness indexes methods, defining the spatial resolution and selecting the estimation method that best correlates with water content data measured in the field, evaluating even moisture at different soil depths and seasons. This study was developed in a landscape with strongly undulated relief and covered with Nitosols at the summit and upper middle third, and Argisols at the low middle third, ranging in altitude from 845 to 890 m, located in the southern state of Minas Gerais, Brazil. It were performed analyses of Pearson linear correlation between soil moisture determined in the field, at depths of 10, 20, 30, 40, 60 and 100 cm and the water storage in 0-100 cm depth, and the topographic and SAGA wetness indexes, TWI and SWI, respectively, obtained from digital elevation models at different spatial resolutions. In most studied conditions, the TWI with resolution of 10 m provided better results, particularly for the dry season. In this study, only the depth of 100 cm resulted in a significant and positive correlation, suggesting that the moisture levels are suitable for water dynamic studies in the subsurface, assisting in studies of hydrological dynamics and planning the soil use and management, especially for perennial plants with deeper root systems.
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spelling doaj.art-225af4d520b244738b3704171cfdc81d2022-12-22T03:12:25ZengUniversidade Federal de LavrasCiência e Agrotecnologia1981-18292014-04-0138214014810.1590/S1413-70542014000200005S1413-70542014000200005Soil moisture assessed by digital mapping techniques and its field validationBruno Montoani Silva0Sérgio Henrique Godinho Silva1Geraldo Cesár de Oliveira2Petrus Hubertus Caspar Rosa Peters3Walbert Júnior Reis dos Santos4Nilton Curi5Universidade Federal de LavrasUniversidade Federal de LavrasUniversidade Federal de LavrasUniversidade Federal de LavrasCompanhia de Desenvolvimento dos Vales do São Francisco e do ParnaíbaUniversidade Federal de LavrasDigital techniques and tools can assist not only in the prediction of soil properties, such as soil moisture, but also in planning the use and management of areas for agriculture and, or, environmental purposes. In this sense, this work aimed to study wetness indexes methods, defining the spatial resolution and selecting the estimation method that best correlates with water content data measured in the field, evaluating even moisture at different soil depths and seasons. This study was developed in a landscape with strongly undulated relief and covered with Nitosols at the summit and upper middle third, and Argisols at the low middle third, ranging in altitude from 845 to 890 m, located in the southern state of Minas Gerais, Brazil. It were performed analyses of Pearson linear correlation between soil moisture determined in the field, at depths of 10, 20, 30, 40, 60 and 100 cm and the water storage in 0-100 cm depth, and the topographic and SAGA wetness indexes, TWI and SWI, respectively, obtained from digital elevation models at different spatial resolutions. In most studied conditions, the TWI with resolution of 10 m provided better results, particularly for the dry season. In this study, only the depth of 100 cm resulted in a significant and positive correlation, suggesting that the moisture levels are suitable for water dynamic studies in the subsurface, assisting in studies of hydrological dynamics and planning the soil use and management, especially for perennial plants with deeper root systems.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1413-70542014000200005&lng=en&tlng=enAtributos de terrenodeterminação do conteúdo de água no solorelevodinâmica da água
spellingShingle Bruno Montoani Silva
Sérgio Henrique Godinho Silva
Geraldo Cesár de Oliveira
Petrus Hubertus Caspar Rosa Peters
Walbert Júnior Reis dos Santos
Nilton Curi
Soil moisture assessed by digital mapping techniques and its field validation
Ciência e Agrotecnologia
Atributos de terreno
determinação do conteúdo de água no solo
relevo
dinâmica da água
title Soil moisture assessed by digital mapping techniques and its field validation
title_full Soil moisture assessed by digital mapping techniques and its field validation
title_fullStr Soil moisture assessed by digital mapping techniques and its field validation
title_full_unstemmed Soil moisture assessed by digital mapping techniques and its field validation
title_short Soil moisture assessed by digital mapping techniques and its field validation
title_sort soil moisture assessed by digital mapping techniques and its field validation
topic Atributos de terreno
determinação do conteúdo de água no solo
relevo
dinâmica da água
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1413-70542014000200005&lng=en&tlng=en
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