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Derivation of Flow Duration Curves to Estimate Hydropower Generation Potential in Data-Scarce Regions

Reichel, Fabian ; Hack, Jochen (2017)
Derivation of Flow Duration Curves to Estimate Hydropower Generation Potential in Data-Scarce Regions.
In: Water, 2017, 9 (572)
Artikel, Zweitveröffentlichung

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Kurzbeschreibung (Abstract)

Small-scale hydropower is a robust and reliable form of sustainable energy supply in remote areas. On the one hand, the potential for hydropower generation depends on the specific climate in a given place, and precipitation above all. On the other hand, such potential also depends on the catchment’s characteristics, e.g., topography, land use, and soils. In the absence of discharge measurements, the available river flow for hydropower production can be estimated in the form of a flow duration curve based on these variables. In this study, the lumped rainfall-runoff method by Crawford and Thurin (1981) was modified to calculate a flow duration curve with a daily time step for an ungauged catchment in Nicaragua. Satisfactory results could be obtained by calibrating the method with the aid of a few discharge measurements. Best results were obtained with a parameter set for groundwater flow and recharge to groundwater from excess soil moisture of 0.014 and 0.6, respectively. Considering the climate and catchment characteristics of the study site, this parameterization can be physically reasoned.

Typ des Eintrags: Artikel
Erschienen: 2017
Autor(en): Reichel, Fabian ; Hack, Jochen
Art des Eintrags: Zweitveröffentlichung
Titel: Derivation of Flow Duration Curves to Estimate Hydropower Generation Potential in Data-Scarce Regions
Sprache: Englisch
Publikationsjahr: 2017
Ort: Darmstadt
Publikationsdatum der Erstveröffentlichung: 2017
Verlag: MDPI
Titel der Zeitschrift, Zeitung oder Schriftenreihe: Water
Jahrgang/Volume einer Zeitschrift: 9
(Heft-)Nummer: 572
URL / URN: urn:nbn:de:tuda-tuprints-69186
Zugehörige Links:
Herkunft: Zweitveröffentlichung aus gefördertem Golden Open Access
Kurzbeschreibung (Abstract):

Small-scale hydropower is a robust and reliable form of sustainable energy supply in remote areas. On the one hand, the potential for hydropower generation depends on the specific climate in a given place, and precipitation above all. On the other hand, such potential also depends on the catchment’s characteristics, e.g., topography, land use, and soils. In the absence of discharge measurements, the available river flow for hydropower production can be estimated in the form of a flow duration curve based on these variables. In this study, the lumped rainfall-runoff method by Crawford and Thurin (1981) was modified to calculate a flow duration curve with a daily time step for an ungauged catchment in Nicaragua. Satisfactory results could be obtained by calibrating the method with the aid of a few discharge measurements. Best results were obtained with a parameter set for groundwater flow and recharge to groundwater from excess soil moisture of 0.014 and 0.6, respectively. Considering the climate and catchment characteristics of the study site, this parameterization can be physically reasoned.

Freie Schlagworte: daily time steps; flow duration curve; lumped rainfall-runoff method; micro-hydropower; Nicaragua; ungauged catchments
URN: urn:nbn:de:tuda-tuprints-69186
Sachgruppe der Dewey Dezimalklassifikatin (DDC): 600 Technik, Medizin, angewandte Wissenschaften > 620 Ingenieurwissenschaften und Maschinenbau
Fachbereich(e)/-gebiet(e): 11 Fachbereich Material- und Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften > Fachgebiet Ingenieurökologie
13 Fachbereich Bau- und Umweltingenieurwissenschaften
13 Fachbereich Bau- und Umweltingenieurwissenschaften > Institut Wasserbau und Wasserwirtschaft
13 Fachbereich Bau- und Umweltingenieurwissenschaften > Institut Wasserbau und Wasserwirtschaft > Fachgebiet Ingenieurhydrologie und Wasserbewirtschaftung
Hinterlegungsdatum: 29 Okt 2017 20:55
Letzte Änderung: 01 Dez 2023 09:49
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