Run-of-river hydro generation in presence of sub-daily source flow variations

The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Roy, Sanjoy [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	Energie / Energieökonomik / Energietechnik / Energiemanagement / Energieforschung
Schlagwörter:	Hydraulic turbines Hydroelectric power generation Hydrodynamics Water resources Meteorology

Übergeordnetes Werk:	Enthalten in: Energy - Amsterdam [u.a.] : Elsevier Science, 1976, 172, Seite 1268-1276
Übergeordnetes Werk:	volume:172 ; pages:1268-1276

DOI / URN:	10.1016/j.energy.2019.01.121

Katalog-ID:	ELV001982192

Internformat


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520			\|a The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency make the conventional estimate open to errors.
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allfields	10.1016/j.energy.2019.01.121 doi (DE-627)ELV001982192 (ELSEVIER)S0360-5442(19)30129-X DE-627 ger DE-627 rda eng 600 DE-600 50.70 bkl Roy, Sanjoy verfasserin (orcid)0000-0002-8849-2374 aut Run-of-river hydro generation in presence of sub-daily source flow variations 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency make the conventional estimate open to errors. 1.1\x Energie (DE-2867)14175-2 stw 1.2\x Energieökonomik (DE-2867)18350-4 stw 1.3\x Energietechnik (DE-2867)18353-5 stw 1.4\x Energiemanagement (DE-2867)18349-3 stw 1.5\x Energieforschung (DE-2867)18348-5 stw Hydraulic turbines Hydroelectric power generation Hydrodynamics Water resources Meteorology Enthalten in Energy Amsterdam [u.a.] : Elsevier Science, 1976 172, Seite 1268-1276 Online-Ressource (DE-627)320597903 (DE-600)2019804-8 (DE-576)116451815 1873-6785 nnns volume:172 pages:1268-1276 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 50.70 Energie: Allgemeines AR 172 1268-1276
spelling	10.1016/j.energy.2019.01.121 doi (DE-627)ELV001982192 (ELSEVIER)S0360-5442(19)30129-X DE-627 ger DE-627 rda eng 600 DE-600 50.70 bkl Roy, Sanjoy verfasserin (orcid)0000-0002-8849-2374 aut Run-of-river hydro generation in presence of sub-daily source flow variations 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency make the conventional estimate open to errors. 1.1\x Energie (DE-2867)14175-2 stw 1.2\x Energieökonomik (DE-2867)18350-4 stw 1.3\x Energietechnik (DE-2867)18353-5 stw 1.4\x Energiemanagement (DE-2867)18349-3 stw 1.5\x Energieforschung (DE-2867)18348-5 stw Hydraulic turbines Hydroelectric power generation Hydrodynamics Water resources Meteorology Enthalten in Energy Amsterdam [u.a.] : Elsevier Science, 1976 172, Seite 1268-1276 Online-Ressource (DE-627)320597903 (DE-600)2019804-8 (DE-576)116451815 1873-6785 nnns volume:172 pages:1268-1276 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 50.70 Energie: Allgemeines AR 172 1268-1276
allfields_unstemmed	10.1016/j.energy.2019.01.121 doi (DE-627)ELV001982192 (ELSEVIER)S0360-5442(19)30129-X DE-627 ger DE-627 rda eng 600 DE-600 50.70 bkl Roy, Sanjoy verfasserin (orcid)0000-0002-8849-2374 aut Run-of-river hydro generation in presence of sub-daily source flow variations 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency make the conventional estimate open to errors. 1.1\x Energie (DE-2867)14175-2 stw 1.2\x Energieökonomik (DE-2867)18350-4 stw 1.3\x Energietechnik (DE-2867)18353-5 stw 1.4\x Energiemanagement (DE-2867)18349-3 stw 1.5\x Energieforschung (DE-2867)18348-5 stw Hydraulic turbines Hydroelectric power generation Hydrodynamics Water resources Meteorology Enthalten in Energy Amsterdam [u.a.] : Elsevier Science, 1976 172, Seite 1268-1276 Online-Ressource (DE-627)320597903 (DE-600)2019804-8 (DE-576)116451815 1873-6785 nnns volume:172 pages:1268-1276 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 50.70 Energie: Allgemeines AR 172 1268-1276
allfieldsGer	10.1016/j.energy.2019.01.121 doi (DE-627)ELV001982192 (ELSEVIER)S0360-5442(19)30129-X DE-627 ger DE-627 rda eng 600 DE-600 50.70 bkl Roy, Sanjoy verfasserin (orcid)0000-0002-8849-2374 aut Run-of-river hydro generation in presence of sub-daily source flow variations 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency make the conventional estimate open to errors. 1.1\x Energie (DE-2867)14175-2 stw 1.2\x Energieökonomik (DE-2867)18350-4 stw 1.3\x Energietechnik (DE-2867)18353-5 stw 1.4\x Energiemanagement (DE-2867)18349-3 stw 1.5\x Energieforschung (DE-2867)18348-5 stw Hydraulic turbines Hydroelectric power generation Hydrodynamics Water resources Meteorology Enthalten in Energy Amsterdam [u.a.] : Elsevier Science, 1976 172, Seite 1268-1276 Online-Ressource (DE-627)320597903 (DE-600)2019804-8 (DE-576)116451815 1873-6785 nnns volume:172 pages:1268-1276 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 50.70 Energie: Allgemeines AR 172 1268-1276
allfieldsSound	10.1016/j.energy.2019.01.121 doi (DE-627)ELV001982192 (ELSEVIER)S0360-5442(19)30129-X DE-627 ger DE-627 rda eng 600 DE-600 50.70 bkl Roy, Sanjoy verfasserin (orcid)0000-0002-8849-2374 aut Run-of-river hydro generation in presence of sub-daily source flow variations 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency make the conventional estimate open to errors. 1.1\x Energie (DE-2867)14175-2 stw 1.2\x Energieökonomik (DE-2867)18350-4 stw 1.3\x Energietechnik (DE-2867)18353-5 stw 1.4\x Energiemanagement (DE-2867)18349-3 stw 1.5\x Energieforschung (DE-2867)18348-5 stw Hydraulic turbines Hydroelectric power generation Hydrodynamics Water resources Meteorology Enthalten in Energy Amsterdam [u.a.] : Elsevier Science, 1976 172, Seite 1268-1276 Online-Ressource (DE-627)320597903 (DE-600)2019804-8 (DE-576)116451815 1873-6785 nnns volume:172 pages:1268-1276 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 50.70 Energie: Allgemeines AR 172 1268-1276
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author	Roy, Sanjoy
spellingShingle	Roy, Sanjoy ddc 600 bkl 50.70 stw Energie stw Energieökonomik stw Energietechnik stw Energiemanagement stw Energieforschung misc Hydraulic turbines misc Hydroelectric power generation misc Hydrodynamics misc Water resources misc Meteorology Run-of-river hydro generation in presence of sub-daily source flow variations
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topic_title	600 DE-600 50.70 bkl Run-of-river hydro generation in presence of sub-daily source flow variations 1.1\x Energie (DE-2867)14175-2 stw 1.2\x Energieökonomik (DE-2867)18350-4 stw 1.3\x Energietechnik (DE-2867)18353-5 stw 1.4\x Energiemanagement (DE-2867)18349-3 stw 1.5\x Energieforschung (DE-2867)18348-5 stw Hydraulic turbines Hydroelectric power generation Hydrodynamics Water resources Meteorology
topic	ddc 600 bkl 50.70 stw Energie stw Energieökonomik stw Energietechnik stw Energiemanagement stw Energieforschung misc Hydraulic turbines misc Hydroelectric power generation misc Hydrodynamics misc Water resources misc Meteorology
topic_unstemmed	ddc 600 bkl 50.70 stw Energie stw Energieökonomik stw Energietechnik stw Energiemanagement stw Energieforschung misc Hydraulic turbines misc Hydroelectric power generation misc Hydrodynamics misc Water resources misc Meteorology
topic_browse	ddc 600 bkl 50.70 stw Energie stw Energieökonomik stw Energietechnik stw Energiemanagement stw Energieforschung misc Hydraulic turbines misc Hydroelectric power generation misc Hydrodynamics misc Water resources misc Meteorology
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title	Run-of-river hydro generation in presence of sub-daily source flow variations
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title_full	Run-of-river hydro generation in presence of sub-daily source flow variations
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title_sort	run-of-river hydro generation in presence of sub-daily source flow variations
title_auth	Run-of-river hydro generation in presence of sub-daily source flow variations
abstract	The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency make the conventional estimate open to errors.
abstractGer	The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency make the conventional estimate open to errors.
abstract_unstemmed	The power output by a small hydropower generation unit (SHP) is conventionally estimated as a product of the net head, admitted flow, and a typical value of efficiency. In case of run of river (RoR) units however, sub-daily variability of stream flow together with consequent variation of efficiency make the conventional estimate open to errors.
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title_short	Run-of-river hydro generation in presence of sub-daily source flow variations
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doi_str	10.1016/j.energy.2019.01.121
up_date	2024-07-06T23:13:36.488Z
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Run-of-river hydro generation in presence of sub-daily source flow variations

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