The Effects of Flooding on Structures. Or What to Expect when the Drought Ends Violently
|
|
- Rosanna Horn
- 5 years ago
- Views:
Transcription
1 The Effects of Flooding on Structures Or What to Expect when the Drought Ends Violently
2 Let s Define Flood Increase in discharge compared to normal level Direct runoff of rainfall (we re talking about Texas) Increase in discharge correlates with increase in depth of flow/ water surface elevation
3 Probability? Roughly 25,000 on-system stream crossing bridges Roughly 17,000 off-system stream crossing bridges Roughly 42,000 stream crossing BRIDGES (>20 open span) Unknown number of culverts too small to be in the database.
4 Probability? Assuming each stream crossing is located on a stream defining a unique watershed with unique characteristics, that s 42,000 opportunities for a damaging flood event at all times; Assuming a 1% annual exceedance event (simply for convenience), that s an expected value of 420 per year statewide
5 Probability? 420 per year- is that realistic? Probably not for a number of reasons, but you get the drift- the probability of seeing structures you have an interest in be subjected to major flooding is not insignificant. Should you consider behavior/ performance in the face of flooding? (I do)
6
7
8
9
10
11 Notice Anything?
12
13 To paraphrase Ron White- It ain t THAT the water is flowin!
14 Debris- Solid materials carried by floodwaters. Floating or relatively buoyant material originating in the watershed and transported by the stream. Might be houses, cars, boats, or other manmade materials, but most commonly is composed of trees, limbs, and other vegetative matter.
15 Debris- Solid materials carried by floodwaters. Structures may function as debris traps if they are not designed with debris in mind. Debris clogs the structure exacerbating flooding of adjacent land, as well as inducing large lateral loads due to flow impediment.
16 Debris Look at the watershed and stream. Try to visualize debris production potential. What kind of debris and how much might be produced? How might structure configuration accommodate or impede debris passage? There s no real standard answer.
17
18 Scour Anecdotally, since such records have been kept, Texas has not seen the prevalence of problems due to scour as it is predicted by HEC 18 and is apparently prevalent in other states. Why is this? What is it about Texas that is different?
19
20 Hypothesis: Much of Texas is subject to flash flooding that appears to be of extreme severity. Many bridges that were built on types of foundations that were most vulnerable (early 20 th century) were destroyed by floods before scour came to our attention. Texas was driven to the use of relatively scour-failure-resistant foundations decades ago by necessity.
21
22
23 Scour- What we DO see Erosion damage to headers and approach roadway is very common when a structure (bridge or culvert) is overtopped by floodwaters. Undermining is often invisible from the roadway!
24
25
26
27 Streambed Material Mobile bed material is present in many Texas streams. After the fact, it may present symptoms similar to the classical scour phenomenon about which so much is written. It actually involves much more extensive material transport upstream, downstream, and through a structure than we are used to thinking about.
28
29
30
31
32
33
34 Summary and Conclusion We are conditioned by process and education to think only about flowing water when we do hydraulic analyses of bridges. Solids transported by the flowing water are very often the actual vehicles of bridge damage.
35 Summary and Conclusions Acknowledgement of the transport of solids by floodwaters is essential to planning survivable structures. There is little guidance- our procedures treat only water. Streams ALWAYS transport more than just water. Solids might be anywhere in the water column.
36 Summary and Conclusions Allowing the passage of debris might encourage a designer to open up a stream cross section at the structure to pass water and debris. Opening up the stream cross section invariably results in the inhibition of bed sediment movement at relatively small flows; this destabilizes the stream.
37 Summary and Conclusions There is a delicate balance between the natural rating curve (stage/discharge) of the stream, the rating curve of the structure, the ability of the structure to pass debris, and the ability of the stream to move bed material that arrives from upstream past the structure.
38 Summary and Conclusions Failure to account for debris passage in the configuration and maintenance of a structure increases the risk of damage to the structure during large events. Failure to account for bed material movement in the configuration and maintenance of a structure often destabilizes the stream and results in chronic, long-term problems that are difficult to resolve.
39
40
41 Questions? George R. Herrmann, P.E., P.H., CFM
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
More informationDegradation Concerns related to Bridge Structures in Alberta
Degradation Concerns related to Bridge Structures in Alberta Introduction There has been recent discussion regarding the identification and assessment of stream degradation in terms of how it relates to
More informationMonitoring Scour Critical Bridges During Floods For Local Bridge Owners. Presented by
Monitoring Scour Critical Bridges During Floods For Local Bridge Owners Presented by SAFETY FIRST DO NOT ENDANGER YOURSELF OR OTHERS WHILE MONITORING BRIDGES DO NOT ENTER FLOOD WATERS FLOOD WATERS INCLUDE
More informationWhy 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
More informationStream Simulation: A Simple Example
Stream Simulation: A Simple Example North Thompson Creek, CO Paul T. Anderson U.S.D.A. Forest Service Here s How We Started May 2011 2-1 USDA-Forest Service Here s How We Finished Forest Service Aquatic
More informationPENNSYLVANIA DEPARTMENT OF TRANSPORTATION ENGINEERING DISTRICT 3-0
PENNSYLVANIA DEPARTMENT OF TRANSPORTATION ENGINEERING DISTRICT 3-0 LYCOMING COUNTY S.R.15, SECTION C41 FINAL HYDROLOGIC AND HYDRAULIC REPORT STEAM VALLEY RUN STREAM RELOCATION DATE: June, 2006 REVISED:
More informationTechnical 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
More informationENGINEERING HYDROLOGY
ENGINEERING HYDROLOGY Prof. Rajesh Bhagat Asst. Professor Civil Engineering Department Yeshwantrao Chavan College Of Engineering Nagpur B. E. (Civil Engg.) M. Tech. (Enviro. Engg.) GCOE, Amravati VNIT,
More informationSCOPE 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
More informationDolores 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
More informationDebris Loads, Bridge/Culvert failure, and Climate Change Identifying stream reaches most susceptible to climate-exacerbated debris load
Debris Loads, Bridge/Culvert failure, and Climate Change Identifying stream reaches most susceptible to climate-exacerbated debris load Seth Lawler, Mathew Mampara, Kristine Mosuela, Mathini Sreetharan
More informationInstream Erosion Control General
Instream Erosion Control General EROSION CONTROL TECHNIQUES Revegetation Temperate Climates Short-Term Non Vegetation Wet Tropics Long-Term Weed Control [1] Semi-Arid Zones Permanent [1] Weed control attributes
More informationVINCENT COOPER Flood Hazard Mapping Consultant
FLOOD HAZARD MAPPING OF GRENADA FINAL REPORT (NON-TECHNICAL) By VINCENT COOPER Flood Hazard Mapping Consultant For the Caribbean Development Bank January, 2006 TABLE OF CONTENTS INTRODUCTION 1 METHODOLOGY
More informationNotes: We all know that Toulmins Spring Branch is a sub-watershed of Three Mile Creek watershed. Some part of it is in Mobile area and rest of it is
1 Notes: This presentation is about some of our findings from a study carried out over the last 3-4 months on stormwater management of Toulmins Spring Branch watershed by NEP. The objective of this study
More informationCASE STUDIES. Introduction
Introduction The City of Winston-Salem faces the challenge of maintaining public infrastructure (e.g., water and sewer lines, storm drains, roads, culverts and bridges) while minimizing the potential impacts
More informationCatastrophic Events Impact on Ecosystems
Catastrophic Events Impact on Ecosystems Hurricanes Hurricanes An intense, rotating oceanic weather system with sustained winds of at least 74 mph and a welldefined eye Conditions for formation: Warm water
More informationGully Erosion Part 1 GULLY EROSION AND ITS CAUSES. Introduction. The mechanics of gully erosion
Gully Erosion Part 1 GULLY EROSION AND ITS CAUSES Gully erosion A complex of processes whereby the removal of soil is characterised by incised channels in the landscape. NSW Soil Conservation Service,
More informationWhy Stabilizing the Stream As-Is is Not Enough
Why Stabilizing the Stream As-Is is Not Enough Several examples of alternatives to the County s design approach have been suggested. A common theme of these proposals is a less comprehensive effort focusing
More informationLEVEE DESIGN FOR FLOOD PROTECTION ON ALLUVIAL FANS
LEVEE DESIGN FOR FLOOD PROTECTION ON ALLUVIAL FANS BRUCE M. PHILLIPS 1 ABSTRACT The dynamic nature of alluvial fans in arid environments offers numerous floodplain management challenges primarily due to
More informationMODELING OF LOCAL SCOUR AROUND AL-KUFA BRIDGE PIERS Saleh I. Khassaf, Saja Sadeq Shakir
ISSN 2320-9100 11 International Journal of Advance Research, IJOAR.org Volume 1, Issue 8,August 2013, Online: ISSN 2320-9100 MODELING OF LOCAL SCOUR AROUND AL-KUFA BRIDGE PIERS Saleh I. Khassaf, Saja Sadeq
More informationA Simple Procedure for Estimating Loss of Life from Dam Failure. Wayne J. Graham, P.E. 1
A Simple Procedure for Estimating Loss of Life from Dam Failure Wayne J. Graham, P.E. 1 INTRODUCTION Evaluating the consequences resulting from a dam failure is an important and integral part of any dam
More informationStep 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
More informationMonte Carlo Simulations for Probabilistic Flood Hazard Assessment
Monte Carlo Simulations for Probabilistic Flood Hazard Assessment Jemie Dababneh, Ph.D., P.E., 1 and Mark Schwartz, P.E. 1 1 RIZZO Associates, Monroeville, Pennsylvania Presentation to PSA 2017 International
More informationCase Study 14. Rocky Creek Vented Box Culvert Ford
Case Study. Rocky Creek Vented Box Culvert Ford Location West Central Arkansas. Ouachita National Forest; Oden Ranger District. Rocky Creek crossing on Forest Road 887 (Muddy Gibbs Road). Crossing Description
More informationCE415L Applied Fluid Mechanics Laboratory
Applied Fluid Mechanics Laboratory Learning Objective Following completion of this experiment and the analysis of the data, you should be able to 1. generalize results of introducing changes to a natural
More informationForest Service AOP Meeting Objectives of Stream Simulation: Examples and Talking Points
Forest Service AOP Meeting Objectives of Stream Simulation: Examples and Talking Points Traci Sylte, P.E. Hydrology/Fluvial Geomorphology Lolo National Forest Is It True? Are Road Crossings a Dam with
More informationDevelopment and application of demonstration MIKE 21C morphological model for a bend in Mekong River
Development and application of demonstration MIKE 21C morphological model for a bend in Mekong River September 2015 0 Table of Contents 1. Introduction... 2 2. Data collection... 3 2.1 Additional data...
More informationModeling Great Britain s Flood Defenses. Flood Defense in Great Britain. By Dr. Yizhong Qu
Modeling Great Britain s Flood Defenses AIRCurrents Editor s note: AIR launched its Inland Flood Model for Great Britain in December 2008. The hazard module captures the physical processes of rainfall-runoff
More informationSediment Transport Analysis for Stream Restoration Design: The Good, the Bad, and the Ugly.
Sediment Transport Analysis for Stream Restoration Design: The Good, the Bad, and the Ugly. Brett Jordan Phd, PE HydroGeo Designs LLC. Land and Water Services Inc. THE GOOD THE BAD THE UGLY THE GOOD THE
More informationStandards for Soil Erosion and Sediment Control in New Jersey May 2012
STANDARD FOR SEDIMENT BASIN Definition A barrier, dam, excavated pit, or dugout constructed across a waterway or at other suitable locations to intercept and retain sediment. Basins created by construction
More informationAppendix F Channel Grade Control Structures
Stream Simulation Appendix F Channel Grade Control Structures This appendix briefly describes permanent grade control structures that are sometimes needed in the upstream and/or downstream reaches adjacent
More information[1] Performance of the sediment trap depends on the type of outlet structure and the settling pond surface area.
Sediment Trench SEDIMENT CONTROL TECHNIQUE Type 1 System Sheet Flow Sandy Soils Type 2 System [1] Concentrated Flow Clayey Soils Type 3 System [1] Supplementary Trap Dispersive Soils [1] Performance of
More informationCase Study 2: Twenty-mile Creek Rock Fords
Case Study : Twenty-mile Creek Rock Fords Location Crossing Description Washington. Okanagan National Forest. Methow Valley Ranger District. Chewuch river basin, East Chewuch Road. The Twenty-mile Creek
More informationThe effectiveness of check dams in controlling upstream channel stability in northeastern Taiwan
Erosion, Debris Mows and Environment in Mountain Regions (Proceedings of the Chengdu Symposium, July 1992). IAHS Publ. no. 209, 1992. 423 The effectiveness of check dams in controlling upstream channel
More informationGrant 0299-NEP: Water Resources Project Preparatory Facility
Document Produced under Grant Project Number: 45206 May 2016 Grant 0299-NEP: Water Resources Project Preparatory Facility Final Report Volume 3 East Rapti (1 of 9) Prepared by Pvt. Ltd. For Ministry of
More informationCountermeasure Calculations and Design
Countermeasure Calculations and Design Summarized from Bridge Scour and Stream Instability Countermeasures, Experience, Selection, and Design Guidance, Second Edition, Publication No. FHWA NHI 01-003,
More informationStream 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
More informationHow Can DOT Operations and Maintenance Prepare for Extreme Weather Events?
How Can DOT Operations and Maintenance Prepare for Extreme Weather Events? Gregory C. Johnson, P.E. Chief Operations Officer Michigan Department of Transportation November 17, 2012 Michigan s Climate Four
More informationTom 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
More informationFish Passage at Road Crossings
Fish Passage at Road Crossings 1 Crossing Design Workshop Outline 1:00 to 2:00 Intro, Design Overview, Channel Width 2:00 to 2:15 Break 2:15 to 3:15 No-Slope, Stream Simulation Design 3:15 to 3:30 Break
More informationComparative Analysis of Hurricane Vulnerability in New Orleans and Baton Rouge. Dr. Marc Levitan LSU Hurricane Center. April 2003
Comparative Analysis of Hurricane Vulnerability in New Orleans and Baton Rouge Dr. Marc Levitan LSU Hurricane Center April 2003 In order to compare hurricane vulnerability of facilities located in different
More informationUGRC 144 Science and Technology in Our Lives/Geohazards
UGRC 144 Science and Technology in Our Lives/Geohazards Flood and Flood Hazards Dr. Patrick Asamoah Sakyi Department of Earth Science, UG, Legon College of Education School of Continuing and Distance Education
More informationAPPROACH 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
More informationLecture Note for Open Channel Hydraulics
Chapter -one Introduction to Open Channel Hydraulics 1.1 Definitions Simply stated, Open channel flow is a flow of liquid in a conduit with free space. Open channel flow is particularly applied to understand
More informationSwift Creek Sediment Management Action Plan (SCSMAP)
Swift Creek Sediment Management Action Plan (SCSMAP) PHASE 2 PROJECT PLAN PROPOSAL Whatcom County Public Works Department 322 N. Commercial Street, Suite 210 Bellingham, WA 98225 (360) 676-6692 June 2013
More informationEvaluation of Scour Depth around Bridge Piers with Various Geometrical Shapes
Evaluation of Scour Depth around Bridge Piers with Various Geometrical Shapes Dr. P. D. Dahe * Department of Civil Engineering, SGGSIE&T, Vishnupuri, Nanded (Maharashtra) S. B. Kharode Department of Civil
More informationRock Sizing for Batter Chutes
Rock Sizing for Batter Chutes STORMWATER MANAGEMENT PRACTICES Photo 1 Rock-lined batter chute Photo 2 Rock-lined batter chute 1. Introduction In the stormwater industry a chute is a steep drainage channel,
More informationProbabilistic Evaluation of a Meandering Low-Flow Channel. February 24 th, UMSRS
Probabilistic Evaluation of a Meandering Low-Flow Channel February 24 th, 2014 2014 UMSRS 1 2 acknowledgments Low- Flow Channel (LFC) overview Proposed Diversion Channel collects runoff from: The Rush
More informationAppendix E Guidance for Shallow Flooding Analyses and Mapping
Appendix E Guidance for Shallow Flooding Analyses and Mapping E.1 Introduction Different types of shallow flooding commonly occur throughout the United States. Types of flows that result in shallow flooding
More informationTABLE OF CONTENTS LIST OF TABLES. Page
TABLE OF CONTENTS Page 11.0 EFFECTS OF THE ENVIRONMENT ON THE PROJECT... 11-1 11.1 Weather Conditions... 11-1 11.2 Flooding... 11-2 11.3 Forest Fires... 11-2 11.4 Permafrost and Subsidence Risk... 11-3
More informationNational Hydrology committee of Afghanistan (NHCA) Sedimentation in Reservoire
National Hydrology committee of Afghanistan (NHCA) Sedimentation in Reservoire OCt.2007 Prof. Mohammad Qasem Seddeqy KPU بسم االله الرحمن الرحيم وجعلنامن الماءکل شي ء حی 30 واز ا ب هر چيزی رازنده گردانيدیم
More informationEngineering Hydrology
Engineering Hydrology Prof. Rajesh Bhagat Asst. Professor Civil Engineering Department Yeshwantrao Chavan College Of Engineering Nagpur B. E. (Civil Engg.) M. Tech. (Enviro. Engg.) GCOE, Amravati VNIT,
More informationAPPENDIX 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,
More informationGEOMORPHIC CHANGES IN LOWER CACHE CREEK 2012
GEOMORPHIC CHANGES IN LOWER CACHE CREEK 2012 Eric W. Larsen Technical Memorandum Prepared for Cache Creek Technical Advisory Committee Natural Resources Program Yolo County Board of Supervisors 2012 Prepared
More informationAlso, when Cascade volcanoes do erupt, high-speed avalanches of pyroclastic flows
INTRODUCTION A volcano is a vent through which molten rock escapes to the Earth s surface. Unlike other mountains, which are pushed up from below, volcanoes are built by surface accumulation of their eruptive
More informationRock Sizing for Bank Stabilisation
Rock Sizing for Bank Stabilisation WATERWAY MANAGEMENT PRACTICES Photo 1 Lower bank rock stabilisation with voids filled with small rocks Photo 2 Rock stabilisation with plants introduced at time of rock
More informationGeomorphology 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
More informationCONCEPTUAL AND TECHNICAL CHALLENGES IN DEFINING FLOOD PLANNING AREAS IN URBAN CATCHMENTS
CONCEPTUAL AND TECHNICAL CHALLENGES IN DEFINING FLOOD PLANNING AREAS IN URBAN CATCHMENTS C Ryan 1, D Tetley 2, C Kinsey 3 1 & 2 Catchment Simulation Solutions, NSW 3 Co-ordinator Stormwater and Structural
More informationDo 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,
More informationDam Removal Analysis Guidelines for Sediment
A review of: Dam Removal Analysis Guidelines for Sediment Joe Rathbun (Retired) rathbunj@sbcglobal.net Some Potential Sediment Issues Reservoir restoration Downstream water quality Downstream deposition
More informationSurface Water and Stream Development
Surface Water and Stream Development Surface Water The moment a raindrop falls to earth it begins its return to the sea. Once water reaches Earth s surface it may evaporate back into the atmosphere, soak
More informationRiver Nith restoration, cbec UK Ltd, October 2013 APPENDIX A
APPENDIX A FLUVIAL AUDIT METHOD STATEMENT Fluvial Audit Methodology INTRODUCTION The procedure used to characterize the geomorphic and sedimentary regimes of the River Till is an adaptation of the Fluvial
More informationSessom Creek Sand Bar Removal HCP Task 5.4.6
Sessom Creek Sand Bar Removal HCP Task 5.4.6 Prepared by: Dr. Thomas Hardy Texas State University Dr. Nolan Raphelt Texas Water Development Board January 6, 2013 DRAFT 1 Introduction The confluence of
More informationErosion Surface Water. moving, transporting, and depositing sediment.
+ Erosion Surface Water moving, transporting, and depositing sediment. + Surface Water 2 Water from rainfall can hit Earth s surface and do a number of things: Slowly soak into the ground: Infiltration
More informationRock Sizing for Multi-Pipe & Culvert Outlets
Rock Sizing for Multi-Pipe & Culvert Outlets STORMWATER AND WATERWAY MANAGEMENT PRACTICES Photo 1 Rock pad outlet structure at end of a duel stormwater pipe outlet Photo 2 Rock pad outlet structure at
More informationTSEGI WASH 50% DESIGN REPORT
TSEGI WASH 50% DESIGN REPORT 2/28/2014 Daniel Larson, Leticia Delgado, Jessica Carnes I Table of Contents Acknowledgements... IV 1.0 Project Description... 1 1.1 Purpose... 1 Figure 1. Erosion of a Headcut...
More informationB-1. Attachment B-1. Evaluation of AdH Model Simplifications in Conowingo Reservoir Sediment Transport Modeling
Attachment B-1 Evaluation of AdH Model Simplifications in Conowingo Reservoir Sediment Transport Modeling 1 October 2012 Lower Susquehanna River Watershed Assessment Evaluation of AdH Model Simplifications
More informationTarbela Dam in Pakistan. Case study of reservoir sedimentation
Tarbela Dam in Pakistan. HR Wallingford, Wallingford, UK Published in the proceedings of River Flow 2012, 5-7 September 2012 Abstract Reservoir sedimentation is a main concern in the Tarbela reservoir
More informationCrows Landing Naval Base Easement
1 of 15 West Stanislaus Resource Conservation District Crows Landing Naval Base Easement Annual Reserve Monitoring Report Jamie McFarlin 11/112012 2 of 15 West Stanislaus Resource Conservation District
More informationRock Sizing for Waterway & Gully Chutes
Rock Sizing for Waterway & Gully Chutes WATERWAY MANAGEMENT PRACTICES Photo 1 Rock-lined waterway chute Photo 2 Rock-lined gully chute 1. Introduction A waterway chute is a stabilised section of channel
More informationSedimentation in the Nile River
Advanced Training Workshop on Reservoir Sedimentation Sedimentation in the Nile River Prof. Dr. Abdalla Abdelsalam Ahmed 10-16 Oct. 2007, IRTCES, Beijing, China CWR,Sudan 1 Water is essential for mankind
More informationThe last three sections of the main body of this report consist of:
Threatened and Endangered Species Geological Hazards Floodplains Cultural Resources Hazardous Materials A Cost Analysis section that provides comparative conceptual-level costs follows the Environmental
More informationFluvial Erosion Impacts on Infrastructure Along Indiana Rivers and Streams
Fluvial Erosion Impacts on Infrastructure Along Indiana Rivers and Streams Siavash Beik, Robert Barr, Brian Meunier 2017 Purdue Road School March 6-9, 2017 In June 2008, flooding damaged or destroyed
More informationStream 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
More informationVolcanoes. Introduction
Volcanoes Introduction Display Slide V-0 Explain that a volcano is a vent through which molten rock escapes to the Earth s surface. Unlike other mountains, which are pushed up from below, volcanoes are
More informationFigure 1. Map of drainages above Beatty s property.
July 13, 2011, corrected Observations of post-monument Fire flows at, Miller Canyon, Coronado National Forest, July 11 th, 2011 Ann Youberg, AZGS Tom Beatty reported 1.05 of rain at his house on July 10
More informationEach basin is surrounded & defined by a drainage divide (high point from which water flows away) Channel initiation
DRAINAGE BASINS A drainage basin or watershed is defined from a downstream point, working upstream, to include all of the hillslope & channel areas which drain to that point Each basin is surrounded &
More informationIMPACTS OF SECONDARY FLOOD EMBANKMENTS ON THE WAIMAKARIRI FLOODPLAIN, NEW ZEALAND
IMPACTS OF SECONDARY FLOOD EMBANKMENTS ON THE WAIMAKARIRI FLOODPLAIN, NEW ZEALAND Terry van Kalken (1), Tony Oliver (2), Ian Heslop (2), Tony Boyle (2) (1) DHI Water & Environment, e-centre, Oaklands Road,
More informationAASHTO Extreme Weather Events Symposium Vermont s Road and Rivers - Managing for the Future
AASHTO Extreme Weather Events Symposium Vermont s Road and Rivers - Managing for the Future May 22, 2013 PLANET EARTH 2 2 MANY MANYYEARS AGO 23,000 years ago there was more than 8,000 feet of glacier over
More informationGENERAL 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,
More informationDetermination of River Water Level Exceedance Frequency Curves
Swiss Federal Nuclear Safety Inspectorate ENSI Determination of River Water Level Exceedance Frequency Curves G. M. Schoen, R. C. Hausherr, A. Ramezanian PSA 2017 International Topical Meeting on Probabilistic
More informationCONCEPTS Conservational Channel Evolution and Pollutant Transport System
CONCEPTS Conservational Channel Evolution and Pollutant Transport System Eddy J. Langendoen Watershed Physical Processes Research Unit National Sedimentation Laboratory USDA Agricultural Research Service
More informationGIS Techniques for Floodplain Delineation. Dean Djokic
GIS Techniques for Floodplain Delineation Dean Djokic (ddjokic@esri.com) Content What is a floodplain? How to get a floodplain? What can GIS do for floodplain modeling? Simple GIS techniques for floodplain
More informationHydro-engineers.ch HEC-RAS ANALAYSIS. River: L Aïre Mesfin Tewolde. Hydro-engineers.ch 23 oct. 2017
Hydro-engineers.ch HEC-RAS ANALAYSIS River: L Aïre Mesfin Tewolde 17 Hydro-engineers.ch 23 oct. 2017 PREPARED BY MESFIN TEWOLDE [TEMPORARY MISSION] Hydro-engineers.ch HEC-RAS ANALYSIS [January- March 2014]
More informationAn environmentally sensitive erosion control technique in the Mekong River Delta: 10 years on
7 th Australian Stream Management Conference - Full Paper An environmentally sensitive erosion control technique in the Mekong River Delta: 10 years on John Tilleard 1, Tony Ladson 2 1 Moroka Pty Ltd,
More informationHistorical channel change on the Upper Gila River, Arizona and New Mexico in response to anthropogenic modifications and extreme floods
Historical channel change on the Upper Gila River, Arizona and New Mexico in response to anthropogenic modifications and extreme floods www.archives.gov www.paztcn.wr.usgs.gov wrh.noaa.gov Upper Gila River
More informationDevelopment of a Fluvial Erosion Hazard Mitigation Program for Indiana
Development of a Fluvial Erosion Hazard Mitigation Program for Indiana Indiana Watersheds Webinar Series October 12,2011 Robert Barr Center for Earth and Environmental Science Department of Earth Sciences
More informationStone Outlet Sediment Trap
3.12 Sediment Control Description: A stone outlet sediment trap is a small detention area formed by placing a stone embankment with an integral stone filter outlet across a drainage swale for the purpose
More informationBig Wood River. General Information
General Information The flows out of the southern portion of the Sawtooth National Recreation Area in central Idaho. The study reach is about a,200 ft length of river about.5 miles upstream from the discontinued
More information3/3/2013. 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
More informationSection 4: Model Development and Application
Section 4: Model Development and Application The hydrologic model for the Wissahickon Act 167 study was built using GIS layers of land use, hydrologic soil groups, terrain and orthophotography. Within
More informationSediment Trap. A temporary runoff containment area, which promotes sedimentation prior to discharge of the runoff through a stabilized spillway.
Sediment Trap SC-15 Source: Caltrans Construction Site Best Management Practices Manual, 2003. Description A temporary runoff containment area, which promotes sedimentation prior to discharge of the runoff
More informationSolutions to Flooding on Pescadero Creek Road
Hydrology Hydraulics Geomorphology Design Field Services Photo courtesy Half Moon Bay Review Solutions to Flooding on Pescadero Creek Road Prepared for: San Mateo County Resource Conservation District
More informationImportant 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
More informationHYDROLOGIC AND HYDRAULIC REPORT FOR SR. 0522, SECTION 5BN ALONG BLACKLOG CREEK CROMWELL TOWNSHIP HUNTINGDON COUNTY. Prepared for:
HYDROLOGIC AND HYDRAULIC REPORT FOR SR. 0522, SECTION 5BN ALONG BLACKLOG CREEK CROMWELL TOWNSHIP Prepared for: KCI Technologies, Inc. Mechanicsburg, PA and Pennsylvania Department of Transportation Engineering
More informationSubject Name: SOIL AND WATER CONSERVATION ENGINEERING 3(2+1) COURSE OUTLINE
Subject Name: SOIL AND WATER CONSERVATION ENGINEERING 3(2+1) COURSE OUTLINE (Name of Course Developer: Prof. Ashok Mishra, AgFE Department, IIT Kharagpur, Kharagpur 721 302) Module 1: Introduction and
More informationMonitoring Headwater Streams for Landscape Response to
Monitoring Headwater Streams for Landscape Response to Climate Change Matthew Connor, PhD Connor nvironmental, nc. www.oe-i.com icom Healdsburg, California verview Headwater stream geomorphology Response
More informationThe 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
More informationRemedial works against debris flows after floods in the State of Vargas, Venezuela
River Basin Management IV 127 Remedial works against debris flows after floods in the State of Vargas, Venezuela P. Di Pietro 1, G. Morassutti 2 & G. Fracassi 3 1 Maccaferri, Italy 2 Consultant, Italy
More informationFour Beetles Project Mendocino National Forest
Four Beetles Project Mendocino National Forest Jose Chavez Bakersfield College 06/07/2016-08/02/2016 District Archeologist Curtis Fair & District Hydrologist John Kelley 2016 Acknowledgements: This project
More information