TDR Technique for Estimating the Intensity of Evapotranspiration of Turfgrasses

The paper presents a method for precise estimation of evapotranspiration of selected turfgrass species. The evapotranspiration functions, whose domains are only two relatively easy to measure parameters, were developed separately for each of the grass species. Those parameters are the temperature an...

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Main Authors: Grzegorz Janik, Karol Wolski, Anna Daniel, Małgorzata Albert, Wojciech Skierucha, Andrzej Wilczek, Paweł Szyszkowski, Amadeusz Walczak
Format: Article
Language:English
Published: Wiley 2015-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1155/2015/626545
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author Grzegorz Janik
Karol Wolski
Anna Daniel
Małgorzata Albert
Wojciech Skierucha
Andrzej Wilczek
Paweł Szyszkowski
Amadeusz Walczak
author_facet Grzegorz Janik
Karol Wolski
Anna Daniel
Małgorzata Albert
Wojciech Skierucha
Andrzej Wilczek
Paweł Szyszkowski
Amadeusz Walczak
author_sort Grzegorz Janik
collection DOAJ
description The paper presents a method for precise estimation of evapotranspiration of selected turfgrass species. The evapotranspiration functions, whose domains are only two relatively easy to measure parameters, were developed separately for each of the grass species. Those parameters are the temperature and the volumetric moisture of soil at the depth of 2.5 cm. Evapotranspiration has the character of a modified logistic function with empirical parameters. It assumes the form ETRθ2.5 cm,T2.5 cm=A/1+B·e-C·θ2.5 cm·T2.5 cm, where: ETRθ2.5 cm,T2.5 cm is evapotranspiration [mm·h−1], θ2.5 cm is volumetric moisture of soil at the depth of 2.5 cm [m3·m−3], T2.5 cm is soil temperature at the depth of 2.5 cm [°C], and A, B, and C are empirical coefficients calculated individually for each of the grass species [mm·h1], and [—], [(m3·m−3·°C)−1]. The values of evapotranspiration calculated on the basis of the presented function can be used as input data for the design of systems for the automatic control of irrigation systems ensuring optimum moisture conditions in the active layer of lawn swards.
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institution Kabale University
issn 2356-6140
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language English
publishDate 2015-01-01
publisher Wiley
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spelling doaj-art-a99dbbbf60684720a1163ed9cdf79dbe2025-02-03T01:11:37ZengWileyThe Scientific World Journal2356-61401537-744X2015-01-01201510.1155/2015/626545626545TDR Technique for Estimating the Intensity of Evapotranspiration of TurfgrassesGrzegorz Janik0Karol Wolski1Anna Daniel2Małgorzata Albert3Wojciech Skierucha4Andrzej Wilczek5Paweł Szyszkowski6Amadeusz Walczak7Institute of Environmental Protection and Development, Wrocław University of Environmental and Life Sciences, Plac Grunwaldzki 24, 50-363 Wrocław, PolandDepartment of Agroecosystems and Green Areas Management, Wrocław University of Environmental and Life Sciences, Plac Grunwaldzki 24, 50-363 Wrocław, PolandDistance Learning Center, Wrocław University of Environmental and Life Sciences, Plac Grunwaldzki 24A, 50-365 Wrocław, PolandInstitute of Environmental Protection and Development, Wrocław University of Environmental and Life Sciences, Plac Grunwaldzki 24, 50-363 Wrocław, PolandDepartment of Metrology and Modelling of Agrophysical Processes, Institute of Agrophysics of the Polish Academy of Sciences, Doświadczalna 4, 20-290 Lublin, PolandDepartment of Metrology and Modelling of Agrophysical Processes, Institute of Agrophysics of the Polish Academy of Sciences, Doświadczalna 4, 20-290 Lublin, PolandInstitute of Landscape Architecture, Wrocław University of Environmental and Life Sciences, Plac Grunwaldzki 24A, 50-365 Wrocław, PolandInstitute of Environmental Protection and Development, Wrocław University of Environmental and Life Sciences, Plac Grunwaldzki 24, 50-363 Wrocław, PolandThe paper presents a method for precise estimation of evapotranspiration of selected turfgrass species. The evapotranspiration functions, whose domains are only two relatively easy to measure parameters, were developed separately for each of the grass species. Those parameters are the temperature and the volumetric moisture of soil at the depth of 2.5 cm. Evapotranspiration has the character of a modified logistic function with empirical parameters. It assumes the form ETRθ2.5 cm,T2.5 cm=A/1+B·e-C·θ2.5 cm·T2.5 cm, where: ETRθ2.5 cm,T2.5 cm is evapotranspiration [mm·h−1], θ2.5 cm is volumetric moisture of soil at the depth of 2.5 cm [m3·m−3], T2.5 cm is soil temperature at the depth of 2.5 cm [°C], and A, B, and C are empirical coefficients calculated individually for each of the grass species [mm·h1], and [—], [(m3·m−3·°C)−1]. The values of evapotranspiration calculated on the basis of the presented function can be used as input data for the design of systems for the automatic control of irrigation systems ensuring optimum moisture conditions in the active layer of lawn swards.http://dx.doi.org/10.1155/2015/626545
spellingShingle Grzegorz Janik
Karol Wolski
Anna Daniel
Małgorzata Albert
Wojciech Skierucha
Andrzej Wilczek
Paweł Szyszkowski
Amadeusz Walczak
TDR Technique for Estimating the Intensity of Evapotranspiration of Turfgrasses
The Scientific World Journal
title TDR Technique for Estimating the Intensity of Evapotranspiration of Turfgrasses
title_full TDR Technique for Estimating the Intensity of Evapotranspiration of Turfgrasses
title_fullStr TDR Technique for Estimating the Intensity of Evapotranspiration of Turfgrasses
title_full_unstemmed TDR Technique for Estimating the Intensity of Evapotranspiration of Turfgrasses
title_short TDR Technique for Estimating the Intensity of Evapotranspiration of Turfgrasses
title_sort tdr technique for estimating the intensity of evapotranspiration of turfgrasses
url http://dx.doi.org/10.1155/2015/626545
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