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Article

Quantification of the Evaporation Rates from Six Types of Wetland Cover in Palo Verde National Park, Costa Rica

1
Department of Water Management, Water Resources Section, Delft University of Technology, 2628 CN Delft, The Netherlands
2
Escuela de Ingeniería Forestal, Tecnológico de Costa Rica, Barrio Los Ángeles, P.O. Box 159-7050, Cartago 30101, Costa Rica
3
Escuela de Biología, Universidad de Costa Rica, Montes de Oca 11501, Costa Rica
*
Author to whom correspondence should be addressed.
Water 2019, 11(4), 674; https://doi.org/10.3390/w11040674
Received: 9 January 2019 / Revised: 15 March 2019 / Accepted: 25 March 2019 / Published: 1 April 2019
(This article belongs to the Special Issue Ecological Assessment of Wetlands)
The hydrology of tropical seasonal wetlands is affected by changes in the land cover. Changes from open water towards a vegetated cover imply an increase in the total evaporation flux, which includes the evaporation from open water bodies and the transpiration from vegetated surfaces. This study quantified the total evaporation flux of six covers of the Palo Verde wetland during dry season. The selected wetland covers were dominated by Neptunia natans (L.f.) Druce, Thalia geniculata L., Typha dominguensis Pers., Eichhornia crassipes (Mart.) Solms, a mixture of these species, and open water conditions. The plants were collected from the wetland and placed in lysimeters (59.1 L) built from plastic containers. The lysimeters were located in an open area near the meteorological station of the Organization for Tropical Studies (OTS). The evaporated water volume and meteorological data were collected between December 2012–January 2013. A completely randomized design was applied to determine the total evaporation (E), reference evaporation ( E ref , Penman-Monteith method) and crop coefficient ( K c ) for all the covers. T. geniculata (E: 17.0 mm d 1 , K c : 3.43) and open water (E: 8.2 mm d 1 , K c : 1.65) showed the highest and lowest values respectively, for daily evaporation and crop coefficient. Results from the ANOVA indicate that E. crassipes and N. natans were statistically different (p = 0.05) from T. dominguensis and the species mixture, while the water and T. geniculata showed significant differences with regard to other plant covers. These results indicate that the presence of emergent macrophytes as T. geniculata and T. dominguensis will increase the evaporation flux during dry season more than the floating macrophytes or open water surfaces. View Full-Text
Keywords: lysimeters; macrophytes; transpiration; marshland; Guanacaste; Tempisque river; Costa Rica lysimeters; macrophytes; transpiration; marshland; Guanacaste; Tempisque river; Costa Rica
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MDPI and ACS Style

Jiménez-Rodríguez, C.D.; Esquivel-Vargas, C.; Coenders-Gerrits, M.; Sasa-Marín, M. Quantification of the Evaporation Rates from Six Types of Wetland Cover in Palo Verde National Park, Costa Rica. Water 2019, 11, 674. https://doi.org/10.3390/w11040674

AMA Style

Jiménez-Rodríguez CD, Esquivel-Vargas C, Coenders-Gerrits M, Sasa-Marín M. Quantification of the Evaporation Rates from Six Types of Wetland Cover in Palo Verde National Park, Costa Rica. Water. 2019; 11(4):674. https://doi.org/10.3390/w11040674

Chicago/Turabian Style

Jiménez-Rodríguez, César D., Catalina Esquivel-Vargas, Miriam Coenders-Gerrits, and Mahmood Sasa-Marín. 2019. "Quantification of the Evaporation Rates from Six Types of Wetland Cover in Palo Verde National Park, Costa Rica" Water 11, no. 4: 674. https://doi.org/10.3390/w11040674

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