Short grass actual evapotranspiration and its dependence on soil water status

Rebeca Hernandez Gomis

Diplomová práce

Abstract:

A weighable Smart-Field Lysimeter (30 cm diameter, 30 cm depth) located in the experimental field of the Czech University of Life Science in Suchdol, Prague, was used to measure directly the daily actual evapotranspiration (ETa) of a short grass surface, neither artificially irrigated nor fertilized, during a period of two years, 26 April, 2013 to May 1, 2015. The primary data recorded by the lysimeter contain periods of rain or snowfall and also some the noise and gaps. In this project, only daily actual evapotranspiration sums from midnight to midnight were calculated and only for rainless days.Secondly, using daily meteorological data from the weather station at the experimental site, the reference crop evapotranspiration (ETo) was calculated with the FAO 56 Penman-Monteith method. At last, the calculated actual evapotranspiration from the lysimeter has been contrasted with the reference evapotranspiration and their ratio was related to the soil water content at 5 cm.The actual evapotranspiration measured with the lysimeter has a seasonal behaviour similar to that of the reference crop evapotranspiration. However, the ratio or the difference of the two does not have a pronounced seasonal behaviour. It is recommended that for continuity of this study, the original Penman-Monteith equation should be applied to estimate the impact of the bulk surface resistance and LAI on ET.

Keywords

lysimeter, soil water content, actual evapotranspiration, reference crop evapotranspiration, FAO56 Penman-Monteith equation

Jazyk práce: angličtina

Datum vytvoření / odevzdání či podání práce: 14. 4. 2016

Obhajoba závěrečné práce

• Vedoucí: Ing. František Doležal, CSc.

Česká zemědělská univerzita v Praze

Fakulta agrobiologie, potravinových a přírodních zdrojů

Magisterský studijní program / obor:
Natural Resources and Environment / Natural Resources and Environment