JARAMA RIVER RESTORATION PROJECT (VALDETORRES): Case study
|
|
|
- Paul Nicholson
- 6 years ago
- Views:
Transcription
1 JARAMA RIVER RESTORATION PROJECT (VALDETORRES): Case study Ana Seves Diego García de Jalón Jarama River: middle reach El Molar (Madrid) 1
2 Jarama River: middle reach El Molar (Madrid) Altitude: 630 m Natural M.A. Flow: 15 m 3 /s Real M.A. Flow: 5 m 3 /s Native Fishery: Barbel Nase Cobitis río Jarama (Algete) 1940_ _1995 Oc Nv Dc En Fb Mz Ab My Jn Jl Ag Sp OBJECTIVES: Rehabilitate the fluvial ecosystem according to actual flow regulation and watershed conditions Implement a physical habitat structure self-regulated Defense and conservation of Natural values from future impacts Promote Public Use 2
3 Project Plan: Fluvial Ecosystem analysis Problematic Diagnostic: riparian and channel alterations by gravel extrctions Flow regulation by large reservoirs Fine sediments comming from upstream Design and proposal of Actuations Design Limitations: Water Authority forbids any change in the actual instream channel Only 1,2 km lenth FLUVIAL ECOSYSTEM ANALYSIS Geomoirphology and fluvial dynamics Hydrological and hydraulical conditions Water quality Biological conditions 3
4 Fotografía aérea de 1956 Fotografía aérea de 1995 River Jarama flow regime Caudales (m 3 /sg) Qm Qm River Jarama Mean monthly flow values from Blue line before the construction of large reservoirs (El Atazar, Pinilla & El Vado) 4
5 Natural Flow regime alteration: Summer lentic conditions Significant decrease of bakfull discharge But the probability of extraodinary floods still exists (reservoir false security) Geomorphology and Fluvial Dynamics STUDY OF A LONG RIVER SEGMENT Longitudinal profile Valley morphology Plant view ANALISYS OF PROJECT REACH Longitudinal profile Plant view Hydraulic Geometry 5
6 Long river segment Comparison between river Jarama reference condition (1956) and actual (1995) photo! Balance Area (Ha) Area(Ha) Width (m) Width (m) Total River Jarama Sinuosity (Leopold & Wolman): Comparison between 1956 and TRAMO Coeficiente de Clasificación sinuosidad (56) A 1.9 Meandriforme B 1.4 Sinuoso C 1.7 Meandriforme D 1.5 Sinuoso Media 1.6 Meandriforme TRAMO Coeficiente de Clasificación sinuosidad (95) A 1.5 Meandriforme B 1.1 Sinuoso C 1.3 Sinuoso D 1.2 Sinuoso Media 1.3 Sinuoso PROJECT REACH STUDY Longitudinal Profile Cota (m) Longitud del tramo (m) pendiente en 1990 pendiente en 1968 River Jarama base level lowered due to: Gravel extractions directly from river bed, and also from the riparian system Decrease of bed load and tranported sediments 6
7 Longitudinal profile of the project reach (43 sections) 623 Perfil longitudinal del tramo de proyecto proyecto Legend Ground Elevation (m) Main Channel Distance (m) Project reach Plant view Historical evolution: Sinuosity Surface Channel width Años Sinuosidad Longitud (m) Superficie Anchura del (ha) cauce (m) Planta presentada por el cauce en el tramo de estudio en 1956, 1968 y 1990 a través de los planos 1:5.000 de 1990 y 1968 y la fotografía aérea de
8 The project Hydraulic Geometry Changes on channel morphology Wider and shallow sections secundary channels reduction of lateral slopes vaciados Pre-project projected Study hydraulic conditions from topographic cross sections (pre-project) and from designed ones (HEC-RAS). 8
9 Remains of gravel industry infraestructure gravera in the riparian zone 9
10 Presence of many open holes, aisolated by dykes and covered by freatic vegetation Old levees & dykes 10
11 Flow entrance Jul-2003 Construction of river channel and wetlands
12 Lagoon construction Recovered natural channel, below the lagoon
13 Costruction of a secundary channel (conectivity and braided) Water quality at entrance and at out-let (2002) Eutrophication and water warming below main lagoon Fine sediments coming from upstream New water outlet Flood lamination No funds for monitoring results Problems 13
14 RESTORATION GOALS Recover old river channel (as seen on 56 photo) Rehabilitation of the riparian system Recover the conection of the river with its flood plain Redesign of a channel connecting the Jarama river with its affluent Arroyo de la Casilla. 14
Integrated methodology for assessing the effects of geomorphological river restoration on fish habitat and riparian vegetation
Integrated methodology for assessing the effects of geomorphological river restoration on fish habitat and riparian vegetation Judit Maroto *a, Miguel Marchamalo a,b, Diego García de Jalón a, Marta González
BASIS FOR RIVER RESTORATION PROJECT
The FLUVIO FCT-Doctoral Program Hydromorphological and Habitat Restoration Course Diego García de Jalón and Marta González del Tánago, UPM Madrid BASIS FOR RIVER RESTORATION PROJECT Throughout the course,
Stream Restoration and Environmental River Mechanics. Objectives. Pierre Y. Julien. 1. Peligre Dam in Haiti (deforestation)
Stream Restoration and Environmental River Mechanics Pierre Y. Julien Malaysia 2004 Objectives Brief overview of environmental river mechanics and stream restoration: 1. Typical problems in environmental
!"#$%&&'()*+#$%(,-./0*)%(!
8:30 Sign in Hoosic River Revival Coalition!"#$%&&'()*+#$%(,-./0*)%(! 12-#30+4/#"5-(60 9:00 Welcome and Introductions 9:15 Goals for Today s Program: A Description of the Planning Process 9:30 First Session:
The Importance of Riparian Vegetation in Channel Restoration: Moving Towards Quantification in Design
The Importance of Riparian Vegetation in Channel Restoration: Moving Towards Quantification in Design Rob Millar Department of Civil Engineering The University of British Columbia "Nothing is as practical
CR AAO Bridge. Dead River Flood & Natural Channel Design. Mitch Koetje Water Resources Division UP District
CR AAO Bridge Dead River Flood & Natural Channel Design Mitch Koetje Water Resources Division UP District Old County Road AAO Bridge Map courtesy of Marquette County Silver Lake Basin McClure Basin
Wetland & Floodplain Functional Assessments and Mapping To Protect and Restore Riverine Systems in Vermont. Mike Kline and Laura Lapierre Vermont DEC
Wetland & Floodplain Functional Assessments and Mapping To Protect and Restore Riverine Systems in Vermont Mike Kline and Laura Lapierre Vermont DEC NWI+ Hydro-Geomorphic Characterization of Wetlands and
ADDRESSING GEOMORPHIC AND HYDRAULIC CONTROLS IN OFF-CHANNEL HABITAT DESIGN
ADDRESSING GEOMORPHIC AND HYDRAULIC CONTROLS IN OFF-CHANNEL HABITAT DESIGN Conor Shea - Hydrologist U.S. Fish and Wildlife Service Conservation Partnerships Program Arcata, CA Learning Objectives Examine
Why Geomorphology for Fish Passage
Channel Morphology - Stream Crossing Interactions An Overview Michael Love Michael Love & Associates mlove@h2odesigns.com (707) 476-8938 Why Geomorphology for Fish Passage 1. Understand the Scale of the
River Restoration and Rehabilitation. Pierre Y. Julien
River Restoration and Rehabilitation Pierre Y. Julien Department of Civil and Environmental Engineering Colorado State University Fort Collins, Colorado River Mechanics and Sediment Transport Lima Peru
Birch Creek Geomorphic Assessment and Action Plan
Birch Creek Geomorphic Assessment and Action Plan Jim Webster Tim Hanrahan, PhD, CFM Jesse Schwartz, PhD Zach Hill January 22, 2015 White Eagle Grange This Project is a First Step in Strategy Planning
Upper Drac River restoration project
Upper Drac River restoration project Restoration of a braided river bed incised in clay substratum through sediment reloading and bed widening SHF Conference, Nantes, 6 & 7 october 2014 Small scale morphological
Aquifer an underground zone or layer of sand, gravel, or porous rock that is saturated with water.
Aggradation raising of the streambed by deposition that occurs when the energy of the water flowing through a stream reach is insufficient to transport sediment conveyed from upstream. Alluvium a general
Stream Classification
Stream Classification Why Classify Streams? Communication Tool Describe Existing Conditions & Trends Describe Restoration Goals Research Tool Morphologic Stream Classification Systems Schumm (1977) Alluvial
Technical Memorandum No
Pajaro River Watershed Study in association with Technical Memorandum No. 1.2.10 Task: Evaluation of Four Watershed Conditions - Sediment To: PRWFPA Staff Working Group Prepared by: Gregory Morris and
NATURAL RIVER. Karima Attia Nile Research Institute
NATURAL RIVER CHARACTERISTICS Karima Attia Nile Research Institute NATURAL RIVER DEFINITION NATURAL RIVER DEFINITION Is natural stream of water that flows in channels with ih more or less defined banks.
May 7, Roger Leventhal, P.E. Marin County Public Works Laurel Collins Watershed Sciences
May 7, 2013 Roger Leventhal, P.E. Marin County Public Works Laurel Collins Watershed Sciences Background Funded in 2009 under EPA 2100 Grant for $30k and managed by SFEP Project Goals: Update original
Perspectives on river restoration science, geomorphic processes, and channel stability
Perspectives on river restoration science, geomorphic processes, and channel stability Stream Restoration Forum: Science and Regulatory Connections Andrew C. Wilcox Department of Geosciences University
Field Methods to Determine/ Verify Bankfull Elevation, XS Area & Discharge
Module # 6 Field Methods to Determine/ Verify Bankfull Elevation, XS Area & Discharge Iowa s River Restoration Toolbox Level 1 / Base Training Overview of Basic Field Data Collection Site Map Cross Sections
Geomorphology Studies
Geomorphology Studies Technical Workgroup Meeting February 14, 2012 Prepared by: Tetra Tech Prepared for: Alaska Energy Authority Overall Goal Geomorphology Studies Two studies Geomorphology Study (RSP
What discharge (cfs) is required to entrain the D 84 (84 th percentile of sediment size distribution) in Red Canyon Wash?
Gregory Indivero 31 October 2011 What discharge (cfs) is required to entrain the D 84 (84 th percentile of sediment size distribution) in Red Canyon Wash? What discharge was required to deposit observed
OBJECTIVES. Fluvial Geomorphology? STREAM CLASSIFICATION & RIVER ASSESSMENT
STREAM CLASSIFICATION & RIVER ASSESSMENT Greg Babbit Graduate Research Assistant Dept. Forestry, Wildlife & Fisheries Seneca Creek, Monongahela National Forest, West Virginia OBJECTIVES Introduce basic
Diagnostic Geomorphic Methods for Understanding Future Behavior of Lake Superior Streams What Have We Learned in Two Decades?
Diagnostic Geomorphic Methods for Understanding Future Behavior of Lake Superior Streams What Have We Learned in Two Decades? Faith Fitzpatrick USGS WI Water Science Center, Middleton, WI fafitzpa@usgs.gov
A MULTI-CRITERIA APPROACH SUPPORTING THE INVESTIGATION OF A FLOODPLAIN POTENTIALLY CONTAMINATED BY PESTICIDES
A MULTI-CRITERIA APPROACH SUPPORTING THE INVESTIGATION OF A FLOODPLAIN POTENTIALLY CONTAMINATED BY PESTICIDES L ZILIANI, B GROPPELLI, S CECCON, F COLOMBO (RAMBOLL ENVIRON) D BOCCHIOLA, M C RULLI, G RAVAZZANI,
The River Restoration Centre therrc.co.uk. Understanding Fluvial Processes: supporting River Restoration. Dr Jenny Mant
The River Restoration Centre therrc.co.uk Understanding Fluvial Processes: supporting River Restoration Dr Jenny Mant Jenny@therrc.co.uk Understanding your catchment Hydrology Energy associated with the
Step 5: Channel Bed and Planform Changes
Step 5: Channel Bed and Planform Changes When disturbed, streams go through a series of adjustments to regain equilibrium with the flow and sediment supply of their watersheds. These adjustments often
Mississippi River and Tributaries Project Mississippi River Geomorphology and Potamology Program
Mississippi River and Tributaries Project Mississippi River Geomorphology and Potamology Program Barb Kleiss, Mississippi Valley Division Freddie Pinkard, Vicksburg District June, 2016 Program Objectives
GLG362/GLG598 Geomorphology K. Whipple October, 2009 I. Characteristics of Alluvial Channels
I. Characteristics of Alluvial Channels Self-formed morphology set by entrainment, transport, and deposition They move unconsolidated sedimentary materials present in the valley fill flood plain/bank flow
Technical Memorandum No Sediment Model
Pajaro River Watershed Study in association with Technical Memorandum No. 1.2.9 Sediment Model Task: Development of Sediment Model To: PRWFPA Staff Working Group Prepared by: Gregory Morris and Elsie Parrilla
3/3/2013. The hydro cycle water returns from the sea. All "toilet to tap." Introduction to Environmental Geology, 5e
Introduction to Environmental Geology, 5e Running Water: summary in haiku form Edward A. Keller Chapter 9 Rivers and Flooding Lecture Presentation prepared by X. Mara Chen, Salisbury University The hydro
Field Observations and One-Dimensional Flow Modeling of Summit Creek in Mack Park, Smithfield, Utah
Intermountain Center for River Rehabilitation and Restoration, Utah State University 31 July 2018 Field Observations and One-Dimensional Flow Modeling of Summit Creek in Mack Park, Smithfield, Utah I.
Ways To Identify Background Verses Accelerated Erosion
Ways To Identify Background Verses Accelerated Erosion Establish Background Condition From Old Ground Photos, Aerial Photos, and Maps Compare Rate Over Time At the Same Location, or for Reaches Channel
Riparian Assessment. Steps in the right direction... Drainage Basin/Watershed: Start by Thinking Big. Riparian Assessment vs.
Riparian Assessment vs. Monitoring Riparian Assessment What is a healthy stream? Determine stream/riparian health Determine change or trend, especially in response to mgmt Classification = designation
MATHEMATICAL MODELING OF FLUVIAL SEDIMENT DELIVERY, NEKA RIVER, IRAN. S.E. Kermani H. Golmaee M.Z. Ahmadi
JOURNAL OF ENVIRONMENTAL HYDROLOGY The Electronic Journal of the International Association for Environmental Hydrology On the World Wide Web at http://www.hydroweb.com VOLUME 16 2008 MATHEMATICAL MODELING
Case Studies in River Management
Case Studies in River Management Pierre Y. Julien Colorado State University 1) Case Studies of River Management in the US 2) Interesting River Management Issues in South Korea Middle Rio Grande, USA Camby
Dolores River Watershed Study
CHAPTER 4: RIVER AND FLOODPLAIN ISSUES The Dolores River falls into a category of streams in Colorado that share some unique characteristics. Like some other mountain streams in the state, it has a steep
Tom Ballestero University of New Hampshire. 1 May 2013
Tom Ballestero University of New Hampshire 1 May 2013 1 Hydrology 2 Basic Hydrology Low flows most common Flows that fill the stream to the banks and higher are much less common Filling the stream to the
Analysis of coarse sediment connectivity in semiarid river channels
Sediment Transfer tlirongh the Fluviai System (Proceedings of a symposium held in Moscow, August 2004). IAHS Publ. 288, 2004 269 Analysis of coarse sediment connectivity in semiarid river channels J. M.
Sediment and nutrient transport and storage along the urban stream corridor
Sediment and nutrient transport and storage along the urban stream corridor Greg Noe, Cliff Hupp, Ed Schenk, Jackie Batson, Nancy Rybicki, Allen Gellis What is the role of floodplains everywhere? Noe 2013,
Do you think sediment transport is a concern?
STREAM RESTORATION FRAMEWORK AND SEDIMENT TRANSPORT BASICS Pete Klingeman 1 What is Your Restoration Project Like? k? Do you think sediment transport is a concern? East Fork Lewis River, WA Tidal creek,
Stream Geomorphology. Leslie A. Morrissey UVM July 25, 2012
Stream Geomorphology Leslie A. Morrissey UVM July 25, 2012 What Functions do Healthy Streams Provide? Flood mitigation Water supply Water quality Sediment storage and transport Habitat Recreation Transportation
Restoration Goals TFG Meeting. Agenda
San Joaquin River Restoration Program Restoration Goals TFG Meeting Reach 2B Update April 28, 2010 Agenda 1. Introductions 2. Program Restoration Goal Context 3. Program Update a) Interim Flows b) EIS/EIR
How Do Human Impacts and Geomorphological Responses Vary with Spatial Scale in the Streams and Rivers of the Illinois Basin?
How Do Human Impacts and Geomorphological Responses Vary with Spatial Scale in the Streams and Rivers of the Illinois Basin? Bruce Rhoads Department of Geography University of Illinois at Urbana-Champaign
Watershed concepts for community environmental planning
Purpose and Objectives Watershed concepts for community environmental planning Dale Bruns, Wilkes University USDA Rural GIS Consortium May 2007 Provide background on basic concepts in watershed, stream,
Mangyeong River Hydraulic Modeling Analysis
Mangyeong River Hydraulic Modeling Analysis Draft Prepared For: Korea Institute of Construction Technology, Republic of Korea by: Dr. Pierre Y. Julien Jaehoon Kim Colorado State University Engineering
Lower South Fork McKenzie River Floodplain Enhancement Project
Lower South Fork McKenzie River Floodplain Enhancement Project McKenzie River Ranger District Willamette National Forest Project Location The project is located in the South Fork McKenzie River Watershed,
Summary of Hydraulic and Sediment-transport. Analysis of Residual Sediment: Alternatives for the San Clemente Dam Removal/Retrofit Project,
Appendix N SUMMARY OF HYDRAULIC AND SEDIMENT-TRANSPORT ANALYSIS OF RESIDUAL SEDIMENT: ALTERNATIVES FOR THE SAN CLEMENTE DAM REMOVAL/RETROFIT PROJECT, CALIFORNIA the San Clemente Dam Removal/Retrofit Project,
Influence of the Major Drainages to the Mississippi River and Implications for System Level Management
Influence of the Major Drainages to the Mississippi River and Implications for System Level Management Brian M. Vosburg Geologist Louisiana Coastal Protection and Restoration Authority brian.vosburg@la.gov
River Response. Sediment Water Wood. Confinement. Bank material. Channel morphology. Valley slope. Riparian vegetation.
River Response River Response Sediment Water Wood Confinement Valley slope Channel morphology Bank material Flow obstructions Riparian vegetation climate catchment vegetation hydrological regime channel
Fluvial Driven Alluvial Fans
Fluvial Driven Alluvial Fans Restoration Project Evaluations - Examples from the Russian and Napa River Watersheds Mia Docto Masters Thesis UC Berkeley 1. Basic Fan Description 2. Fluvial Driven Fan Characteristics
Business. Meteorologic monitoring. Field trip? Reader. Other?
Business Meteorologic monitoring Field trip? Reader Other? Classification Streams Characterization Discharge measurements Why classify stream channels? Why Classify Stream Channels? Provides a common language
APPROACH TO THE SPANISH WATER ORGANISATION IMPROVING FLOOD HAZARD MAPPING, LAWS AND AUTHORITIES COORDINATION
"Workshop On Land Use Planning And Water Management, With Focus On Flood Risk Management Oslo, Norway. Wednesday 31 January and Thursday 1 February 2007 APPROACH TO THE SPANISH WATER ORGANISATION IMPROVING
Technical Supplement 3E. Rosgen Stream Classification Technique Supplemental Materials. (210 VI NEH, August 2007)
Technical Supplement 3E (210 VI NEH, August 2007) Issued August 2007 Cover photo: The Rosgen stream classification system uses morphometric data to characterize streams. Advisory Note Techniques and approaches
SCOPE OF PRESENTATION STREAM DYNAMICS, CHANNEL RESTORATION PLANS, & SEDIMENT TRANSPORT ANALYSES IN RELATION TO RESTORATION PLANS
DESIGN METHODS B: SEDIMENT TRANSPORT PROCESSES FOR STREAM RESTORATION DESIGN PETER KLINGEMAN OREGON STATE UNIVERSITY CIVIL ENGINEERING DEPT., CORVALLIS 2 ND ANNUAL NORTHWEST STREAM RESTORATION DESIGN SYMPOSIUM
Natural Shoreline Landscapes on Michigan Inland Lakes
Natural Shoreline Landscapes on Michigan Inland Lakes Excerpts from Chapters 2 and 3 Photo Photo by Jane by Jane Herbert Herbert Did you know? Twenty-four species of amphibians, 25 species of reptiles,
Restoration Modeling Analysis for Abandoned Channels of the Mangyeong River
1) 한국환경과학회지제20권 ( 제5호 ), 555~564, 2011 Journal of the Environmental Sciences DOI: 10.5322/JES.2011.20.5.555 Restoration Modeling Analysis for Abandoned Channels of the Mangyeong River Jaehoon Kim, Pierre
Four Mile Run Levee Corridor Stream Restoration
Four Mile Run Levee Corridor Stream Restoration 30% Design Summary U.S. Army Corps of Engineers, Baltimore District Presentation Outline Four Mile Run 1.) Historic Perspective 2.) Existing Conditions 3.)
4.17 Spain. Catalonia
4.17 Spain Catalonia In Spain, inundation studies are the responsibility of the respective Hydrographic Confederations of each river basin (River Basin Authorities). The actual status of inundation studies
Topic Page: Floodplains
Topic Page: Floodplains Definition: f loodplain from The Penguin English Dictionary a low-lying area beside a river that is composed of sedimentary deposits and is subject to periodic flooding. Summary
Application of Fluvial Geomorphologic Techniques At Abandoned Mine Sites 1. David A. Greenfield 2 Dennis M. Palladino 3
Application of Fluvial Geomorphologic Techniques At Abandoned Mine Sites 1 David A. Greenfield 2 Dennis M. Palladino 3 ABSTRACT Watersheds that have been severely impacted by mining can no longer transport
Fluvial Geomorphology
Geomorphic Components of Riparian Ecosystems W. Barry Southerland, Ph.D. Fluvial Geomorphologist, CPESC #514 West National Technology Support Center Water Quality and Quantity Technology Development Team
Important Copyright Information
Important Copyright Information The following content is provided for educational purposes by the workshop presenter. This content may or may not have been peer reviewed. Information, opinions and recommendations
Assessment. Assessment
2001 SPRINGBROOK CREEK RESTORATION - THREE YEAR POST-CONSTRUCTION REVIEW - Presented by Bruce Henderson and Andy Harris 2005 River Restoration Northwest Symposium Skamania Lodge, Washington www.hendersonlandservices.com
River Morphology. EAD 511 River management
River Morphology EAD 511 River management Introduction FLUVIAL GEOMORPHOLOGY Webster's New World Dictionary defines fluvial as: of, found in, or produced by a river or rivers. The same reference defines
Consequences of river regulation works: altered fluvial processes + increasing flood hazard
Consequences of river regulation works: altered fluvial processes + increasing flood hazard Dr. Tímea Kiss assistant professor Department of Physical Geography and Geoinformatics, University of Szeged,
Ground Water Control of Tree Island Origin, Genesis and Destruction. By John F. Meeder and Peter W. Harlem SERC,FIU
Ground Water Control of Tree Island Origin, Genesis and Destruction By John F. Meeder and Peter W. Harlem SERC,FIU Functional Definition Our functional definition of a Tree Island is; an isolated scrub
Nutrient and Sediment Cycling and Retention in Urban Floodplain Wetlands
Nutrient and Sediment Cycling and Retention in Urban Floodplain Wetlands Greg Noe, Cliff Hupp, Nancy Rybicki, Ed Schenk, and Jackie Batson National Research Program, Reston VA U.S. Department of the Interior
Sediment Transport in Stream Assessment and Design July 31 August 4, Logan, Utah
DEPARTMENT OF WATERSHED SCIENCES Sediment Transport in Stream Assessment and Design July 31 August 4, Logan, Utah This course is intended for those who wish to understand and apply the principles of sediment
Water quality needs: Flow, velocity. Fish biologists need: Critical depth or velocity. Hydrology gives flows m 3 /s or day
Environmental Water Allocation Hydraulics Dr L Beevers Heriot Watt University, it UK l.beevers@hw.ac.uk Overview Why hydraulics in EWA? Different types of flows Theory Case studies Review Why do we need
Kootenai River Habitat Restoration Program Update
Kootenai River Habitat Restoration Program Update Kootenai Tribe of Idaho Kootenai Valley Resource Initiative November 19, 2012 Bonners Ferry, Idaho Changes to Kootenai Basin Beaver trapping Floodplain
Vegetation effects on river hydraulics. Johannes J. (Joe) DeVries David Ford Consulting Engineers, Inc. Sacramento, CA
Vegetation effects on river hydraulics Johannes J. (Joe) DeVries David Ford Consulting Engineers, Inc. Sacramento, CA jjdevries@ford-consulting.com SAC05 D2P31 RM 99.0L VIEW UPSTREAM AT UPSTREAM END DWR
Licca Liber - the free Lech
Licca Liber - the free Lech Source: W. Schilling WWA Donauwörth The river Lech an overview Hydrography / Hydrology catchment area 4000 km² Length 256 km Delta H 1100 m Slope Ø 0,4 % discharge in Augsburg
Strategies for managing sediment in dams. Iwona Conlan Consultant to IKMP, MRCS
Strategies for managing sediment in dams Iwona Conlan Consultant to IKMP, MRCS 1 Sediment trapping by dams Active storage capacity Dead storage coarse material (bed load) Fine materials (suspension) Francis
Upper Truckee River Restoration Lake Tahoe, California Presented by Brendan Belby Sacramento, California
Upper Truckee River Restoration Lake Tahoe, California Presented by Brendan Belby Sacramento, California Mike Rudd (Project Manager), Charley Miller & Chad Krofta Declines in Tahoe s Water Clarity The
LANDFORMS OF THE LOWER YUBA RIVER
LOWER YUBA RIVER ACCORD MONITORING AND EVALUATION PROGRAM LANDFORMS OF THE LOWER YUBA RIVER APRIL 2012 Prepared for: The Lower Yuba Accord River Management Team by Josh Wyrick, PhD., and Greg Pasternack,
Coarse Sediment Augmentation on Regulated Rivers. Scott McBain McBain & Trush, Inc.
Coarse Sediment Augmentation on Regulated Rivers Scott McBain McBain & Trush, Inc. scott@mcbaintrush.com Components Some geomorphic and ecological considerations Conceptual approach at understanding augmentation
APPENDIX B Hydraulic Considerations for Pipeline Crossings of Stream Channels
APPENDIX B Hydraulic Considerations for Pipeline Crossings of Stream Channels B-1 B-2 APPENDIX B HYDRAULIC CONSIDERATIONS FOR PIPELINE CROSSINGS OF STREAM CHANNELS Pipeline crossings of perennial, intermittent,
Avoiding Geohazards in the Mid-Atlantic Highlands by Using Natural Stream Principles
Avoiding Geohazards in the Mid-Atlantic Highlands by Using Natural Stream Principles J. Steven Kite, WVU Neal Carte, WVDOT Will Harman, Michael Baker Corp. Donald D. Gray, WVU Photo: W. Gillespie North
Fact sheet: Glacial rivers (all Europe)
Fact sheet: Glacial rivers (all Europe) General description Valleyplanform Hydrology and The valley form varies from a gorge to a V-shaped valley and the single-thread channel is mainly characterized by
Vermont Stream Geomorphic Assessment. Appendix E. River Corridor Delineation Process. VT Agency of Natural Resources. April, E0 - April, 2004
Vermont Stream Geomorphic Assessment Appendix E River Corridor Delineation Process Vermont Agency of Natural Resources - E0 - River Corridor Delineation Process Purpose A stream and river corridor delineation
Sprague River Basin Restoration Post Project Evaluations: Lessons Learned and Future Applications
River Restoration Northwest, 2015 Sprague River Basin Restoration Post Project Evaluations: Lessons Learned and Future Applications Mark R. Tompkins, P.E., Ph.D. ACKNOWLEDGEMENTS The Klamath Tribes Larry
Updated Fluvial Geomorphology Modeling Approach
(FERC No. 14241) Updated Fluvial Geomorphology Modeling Approach Technical Memorandum Prepared for Prepared by Tetra Tech Original Submitted June 30, 2013 Updated May 2014 Page intentionally left blank
Rapid Geomorphic Assessments: RGA s
Establishing Current Reference Conditions Rates and concentrations of suspended-sediment transport vary over time and space due to factors such as precipitation characteristics and discharge, geology,
Hydraulic and Sediment Transport Modeling Strategy
Appendix B Hydraulic and Sediment Transport Modeling Strategy May 2014 Technical Memorandum Channel Capacity Report January 2015 San Joaquin River Restoration Program Hydraulic and Sediment Transport Modeling
Determining the Suitable Sediment extraction Locations of Existing Sand and Gravel Mines on Boshar River in Iran using HEC-RAS Modeling
ICSE6-134 Determining the Suitable Sediment extraction Locations of Existing Sand and Gravel Mines on Boshar River in Iran using HEC-RAS Modeling Mohammad GHARESIFARD 1, Ali JAHEDAN 2, Bahar MOLAZEM 3
The Effects of Geomorphology and Watershed Land Use on Spawning Habitat
The Effects of Geomorphology and Watershed Land Use on Spawning Habitat By Evan Buckland INTRODUCTION The distribution and frequency of large geomorphic features in a watershed govern where suitable spawning
Thank you to all of our 2015 sponsors: Media Partner
Thank you to all of our 2015 sponsors: Media Partner Fluvial System Concepts and Their Application in Greenfield Stream Corridor Realignment Dr. Paul Villard, P.Geo. GEO Morphix Ltd. Overview Major realignment
Geomorphology Geology 450/750 Spring Fluvial Processes Project Analysis of Redwood Creek Field Data Due Wednesday, May 26
Geomorphology Geology 450/750 Spring 2004 Fluvial Processes Project Analysis of Redwood Creek Field Data Due Wednesday, May 26 This exercise is intended to give you experience using field data you collected
CHANNEL GEOMORPHIC RESPONSES TO DISTURBANCES ASSESSED USING STREAMGAGE INFORMATION
CHANNEL GEOMORPHIC RESPONSES TO DISTURBANCES ASSESSED USING STREAMGAGE INFORMATION Kyle E. Juracek, Research Hydrologist, U.S. Geological Survey, Lawrence, KS, kjuracek@usgs.gov; Mark W. Bowen, Ph.D. candidate,
Deliverable 2.1: Multi-scale framework and indicators of hydromorphological processes and forms
3. THE HIERACHICAL FRAMEWORK Many hierarchical approaches have been proposed to support better understanding of the functioning of river catchments, corridors and networks. In chronological order, some
Implementing a Project with 319 Funds: The Spring Brook Meander Project. Leslie A. Berns
Implementing a Project with 319 Funds: The Spring Brook Meander Project Leslie A. Berns "...to acquire... and hold lands... for the purpose of protecting and preserving the flora, fauna and scenic beauties...
Environmental Geology Chapter 9 Rivers and Flooding
Environmental Geology Chapter 9 Rivers and Flooding Flooding in Pakistan 2010-1600 killed/20000 affected The hydrologic cycle is powered by the Sun The cycle includes evaporation, precipitation, infiltration,
Beaver Creek Corridor Design and Analysis. By: Alex Previte
Beaver Creek Corridor Design and Analysis By: Alex Previte Overview Introduction Key concepts Model Development Design Accuracy Conclusion Refresh v = Beaver Creek Site = Wittenberg Introduction Low head
Brief outline of the presentation
EGS AGU - EUG Joint Assembly, Nice, France, April 2003 Session HS9 - Sediment dynamics and channel change in rivers and estuaries Channel change and sediment movement after a major level drawdown at Kremasta
Assignment 1. Measuring River Characteristics- Vernon Creek. Applied Fluvial Geomorphology Field Techniques EESc 435
Assignment 1 Measuring River Characteristics- Vernon Creek Applied Fluvial Geomorphology Field Techniques EESc 435 Amanda Jardine 30100093 Jaime McDonald 14177083 Erica Massey 50870088 April 28, 2012 Introduction
DAM IMPACTS ON AND RESTORATION OF AN ALLUVIAL RIVER RIO GRANDE, NEW MEXICO
A. Reservoir Effects of Stream Channels DAM IMPACTS ON AND RESTORATION OF AN ALLUVIAL RIVER RIO GRANDE, NEW MEXICO Gigi RICHARD 1 and Pierre JULIEN 2 ABSTRACT The impact of construction of dams and reservoirs
GENERAL SUMMARY BIG WOOD RIVER GEOMORPHIC ASSESSMENT BLAINE COUNTY, IDAHO
GENERAL SUMMARY BIG WOOD RIVER GEOMORPHIC ASSESSMENT BLAINE COUNTY, IDAHO Prepared For Trout Unlimited 300 North Main Street, Hailey, Idaho, 83333 Prepared By P. O. Box 8578, 140 E. Broadway, Suite 23,
Technical Review of Pak Beng Hydropower Project (1) Hydrology & Hydraulics and (2) Sediment Transport & River Morphology
Technical Review of Pak Beng Hydropower Project (1) Hydrology & Hydraulics and (2) Sediment Transport & River Morphology The 2 nd Regional Stakeholder Forum The Pak Beng Hydropower Project 5 th May 2017
Mapping of Future Coastal Hazards. for Southern California. January 7th, David Revell, Ph.D. E.
Mapping of Future Coastal Hazards for Southern California January 7th, 2014 David Revell, Ph.D. drevell@esassoc.com E. Vandebroek, 2012 Outline Coastal erosion hazard zones Flood hazard zones: Coastal
Lab Final Review 4/16/18
Lab Final Review 4/16/18 Overall goals from lab Think about geology on recent timescales, predict the direction change Be able to identify how different landforms or patterns (e.g. drainage patterns, dune