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The Regulation of Peace River : a Case Study for River Management.

This book presents a comprehensive overview of the first longitudinal study of the downstream response of a major river to the establishment of a large hydropower facility and dams. Peace River, a northward flowing boreal river in northwestern Canada was dammed in 1967 and the book describes the mor...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Church, Michael
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Hoboken : Wiley, 2014.
Temas:
Acceso en línea:Texto completo

MARC

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035 |a (OCoLC)893332985 
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049 |a UAMI 
100 1 |a Church, Michael. 
245 1 4 |a The Regulation of Peace River :  |b a Case Study for River Management. 
260 |a Hoboken :  |b Wiley,  |c 2014. 
300 |a 1 online resource (291 pages) 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
588 0 |a Print version record. 
505 0 |a The Regulation of Peace River; Contents; Contributing authors; Preface; 1 On regulated rivers; 1.1 Setting a context; 1.2 Peace River; 1.3 Some precedents; 1.4 The program; References; 2 The regulation of Peace River; 2.1 Introduction; 2.2 Hydrology; 2.2.1 Hydrography and runoff sources; 2.2.2 Climate and runoff; 2.2.3 Flood regime; 2.2.4 Competent flows; 2.3 Sediment transport; 2.3.1 Suspended sediment in the upper river; 2.3.2 Suspended sediment in the lower river; 2.3.3 The suspended sediment record at the Town of Peace River; 2.3.4 Bedload; 2.4 Discussion and conclusions; Acknowledgments. 
504 |a References3 Downstream channel gradation in the regulated Peace River; 3.1 Introduction; 3.2 Reach description; 3.3 Methods; 3.3.1 Cross-sections; 3.3.2 Specific gauge; 3.3.3 Planform analysis; 3.3.4 Tributary confluence effect; 3.4 Observations; 3.4.1 Cross-sections; 3.4.2 Specific gauge; 3.4.3 Planform analysis; 3.4.4 Confluences; 3.5 Discussion; 3.5.1 Absence of channel degradation; 3.5.2 Spatial variability of channel gradation; 3.5.3 Channel cross-sectional morphology; 3.5.4 Confluences; 3.5.5 Channel gradation and planform change: implications for channel gradient; 3.6 Conclusions. 
505 8 |a AcknowledgmentsReferences; 4 Tributary channel gradation due to regulation of Peace River; 4.1 Introduction; 4.2 Study sites; 4.3 Potential tributary gradation; 4.4 Methods; 4.4.1 Air photo interpretation; 4.4.2 Surveying; 4.4.3 Dendrochronology; 4.4.4 Specific gauge analysis; 4.5 Observations; 4.5.1 Farrell Creek; 4.5.2 Halfway River; 4.5.3 Moberly River; 4.5.4 Pine River; 4.5.5 Beatton River; 4.5.6 Kiskatinaw River; 4.5.7 Alces River; 4.5.8 Hines Creek; 4.5.9 Smoky River; 4.5.10 Summary of channel gradation observations; 4.6 Discussion; 4.6.1 Timing and fates of channel gradation. 
505 8 |a 4.6.2 Tributary gradation pattern downstream4.7 Conclusions; Acknowledgments; References; 5 The hydraulic geometry of Peace River; 5.1 Introduction; 5.2 Hydraulic geometry; 5.3 Methods; 5.4 At-a-station hydraulic geometry; 5.4.1 Peace River at Taylor, British Columbia (WSC Stn. 07FD002); 5.4.2 Peace River at Alces River, British Columbia (WSC Stn. 07FD010); 5.4.3 Peace River at Dunvegan Bridge (WSC Stn. 07FD003); 5.4.4 Peace River at Carcajou (WSC Stn. 07HD001); 5.4.5 Peace River at Fort Vermilion (WSC Stn. 07HF001); 5.4.6 Hydraulic geometry at WSC Stn. 07KC001, Peace River at Peace Point. 
505 8 |a 5.4.7 Summary on at-a-station hydraulic geometry5.5 Downstream hydraulic geometry; 5.5.1 Formative flows; 5.5.2 Downstream changes; 5.6 Resistance to flow; 5.7 Some tests for channel pattern; 5.8 Discussion; 5.9 Conclusions; Acknowledgments; References; 6 Ice on Peace River: effects on bank morphology and riparian vegetation; 6.1 Introduction; 6.2 The ice regime; 6.2.1 An introduction to river ice; 6.2.2 Ice on Peace River; 6.3 Methods; 6.3.1 River datum; 6.3.2 Vegetation damage; 6.3.3 Riparian vegetation; 6.3.4 Bank morphology and sedimentary features. 
500 |a 6.4 Ice-jam location, magnitude, and frequency from the scar record. 
520 |a This book presents a comprehensive overview of the first longitudinal study of the downstream response of a major river to the establishment of a large hydropower facility and dams. Peace River, a northward flowing boreal river in northwestern Canada was dammed in 1967 and the book describes the morphological response of the 1200 km downstream channel and the response of riparian vegetation to the change in flow regime over the first forty years of regulated flows. Beginning with a description of the effect of regulation on the flow and sediment regimes of the river, the book proceeds to stud. 
590 |a ProQuest Ebook Central  |b Ebook Central Academic Complete 
650 0 |a Watershed management  |z Peace River Watershed (B.C. and Alta.) 
650 0 |a Riparian ecology  |z Peace River Watershed (B.C. and Alta.) 
651 0 |a Peace River (B.C. and Alta.)  |x Watershed  |x Environmental conditions. 
650 6 |a Bassins hydrographiques  |x Gestion  |z Paix, Bassin de la rivière de la (C.-B. et Alb.) 
650 6 |a Écologie ripicole  |z Paix, Bassin de la rivière de la (C.-B. et Alb.) 
650 7 |a Riparian ecology  |2 fast 
650 7 |a Watershed management  |2 fast 
651 7 |a Canada  |z Peace River  |2 fast 
651 7 |a Canada  |z Peace River Watershed  |2 fast 
758 |i has work:  |a The regulation of Peace River (Text)  |1 https://id.oclc.org/worldcat/entity/E39PCFK6JGkRFHhYQFbyypkTwP  |4 https://id.oclc.org/worldcat/ontology/hasWork 
776 0 8 |i Print version:  |a Church, Michael.  |t Regulation of Peace River : A Case Study for River Management.  |d Hoboken : Wiley, ©2014  |z 9781118906149 
856 4 0 |u https://ebookcentral.uam.elogim.com/lib/uam-ebooks/detail.action?docID=1813818  |z Texto completo 
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938 |a ProQuest Ebook Central  |b EBLB  |n EBL1813818 
994 |a 92  |b IZTAP