Observation Method to Predict Meander Migration and Vertical Degradation of Rivers
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River Dynamics 101 - Fact Sheet River Management Program Vermont Agency of Natural Resources
River Dynamics 101 - Fact Sheet River Management Program Vermont Agency of Natural Resources Overview In the discussion of river, or fluvial systems, and the strategies that may be used in the management of fluvial systems, it is important to have a basic understanding of the fundamental principals of how river systems work. This fact sheet will illustrate how sediment moves in the river, and the general response of the fluvial system when changes are imposed on or occur in the watershed, river channel, and the sediment supply. The Working River The complex river network that is an integral component of Vermont’s landscape is created as water flows from higher to lower elevations. There is an inherent supply of potential energy in the river systems created by the change in elevation between the beginning and ending points of the river or within any discrete stream reach. This potential energy is expressed in a variety of ways as the river moves through and shapes the landscape, developing a complex fluvial network, with a variety of channel and valley forms and associated aquatic and riparian habitats. Excess energy is dissipated in many ways: contact with vegetation along the banks, in turbulence at steps and riffles in the river profiles, in erosion at meander bends, in irregularities, or roughness of the channel bed and banks, and in sediment, ice and debris transport (Kondolf, 2002). Sediment Production, Transport, and Storage in the Working River Sediment production is influenced by many factors, including soil type, vegetation type and coverage, land use, climate, and weathering/erosion rates. -
Stream Restoration, a Natural Channel Design
Stream Restoration Prep8AICI by the North Carolina Stream Restonltlon Institute and North Carolina Sea Grant INC STATE UNIVERSITY I North Carolina State University and North Carolina A&T State University commit themselves to positive action to secure equal opportunity regardless of race, color, creed, national origin, religion, sex, age or disability. In addition, the two Universities welcome all persons without regard to sexual orientation. Contents Introduction to Fluvial Processes 1 Stream Assessment and Survey Procedures 2 Rosgen Stream-Classification Systems/ Channel Assessment and Validation Procedures 3 Bankfull Verification and Gage Station Analyses 4 Priority Options for Restoring Incised Streams 5 Reference Reach Survey 6 Design Procedures 7 Structures 8 Vegetation Stabilization and Riparian-Buffer Re-establishment 9 Erosion and Sediment-Control Plan 10 Flood Studies 11 Restoration Evaluation and Monitoring 12 References and Resources 13 Appendices Preface Streams and rivers serve many purposes, including water supply, The authors would like to thank the following people for reviewing wildlife habitat, energy generation, transportation and recreation. the document: A stream is a dynamic, complex system that includes not only Micky Clemmons the active channel but also the floodplain and the vegetation Rockie English, Ph.D. along its edges. A natural stream system remains stable while Chris Estes transporting a wide range of flows and sediment produced in its Angela Jessup, P.E. watershed, maintaining a state of "dynamic equilibrium." When Joseph Mickey changes to the channel, floodplain, vegetation, flow or sediment David Penrose supply significantly affect this equilibrium, the stream may Todd St. John become unstable and start adjusting toward a new equilibrium state. -
Chapter 4: Land Degradation
Final Government Distribution Chapter 4: IPCC SRCCL 1 Chapter 4: Land Degradation 2 3 Coordinating Lead Authors: Lennart Olsson (Sweden), Humberto Barbosa (Brazil) 4 Lead Authors: Suruchi Bhadwal (India), Annette Cowie (Australia), Kenel Delusca (Haiti), Dulce 5 Flores-Renteria (Mexico), Kathleen Hermans (Germany), Esteban Jobbagy (Argentina), Werner Kurz 6 (Canada), Diqiang Li (China), Denis Jean Sonwa (Cameroon), Lindsay Stringer (United Kingdom) 7 Contributing Authors: Timothy Crews (The United States of America), Martin Dallimer (United 8 Kingdom), Joris Eekhout (The Netherlands), Karlheinz Erb (Italy), Eamon Haughey (Ireland), 9 Richard Houghton (The United States of America), Muhammad Mohsin Iqbal (Pakistan), Francis X. 10 Johnson (The United States of America), Woo-Kyun Lee (The Republic of Korea), John Morton 11 (United Kingdom), Felipe Garcia Oliva (Mexico), Jan Petzold (Germany), Mohammad Rahimi (Iran), 12 Florence Renou-Wilson (Ireland), Anna Tengberg (Sweden), Louis Verchot (Colombia/The United 13 States of America), Katharine Vincent (South Africa) 14 Review Editors: José Manuel Moreno Rodriguez (Spain), Carolina Vera (Argentina) 15 Chapter Scientist: Aliyu Salisu Barau (Nigeria) 16 Date of Draft: 07/08/2019 17 Subject to Copy-editing 4-1 Total pages: 186 Final Government Distribution Chapter 4: IPCC SRCCL 1 2 Table of Contents 3 Chapter 4: Land Degradation ......................................................................................................... 4-1 4 Executive Summary ........................................................................................................................ -
Classifying Rivers - Three Stages of River Development
Classifying Rivers - Three Stages of River Development River Characteristics - Sediment Transport - River Velocity - Terminology The illustrations below represent the 3 general classifications into which rivers are placed according to specific characteristics. These categories are: Youthful, Mature and Old Age. A Rejuvenated River, one with a gradient that is raised by the earth's movement, can be an old age river that returns to a Youthful State, and which repeats the cycle of stages once again. A brief overview of each stage of river development begins after the images. A list of pertinent vocabulary appears at the bottom of this document. You may wish to consult it so that you will be aware of terminology used in the descriptive text that follows. Characteristics found in the 3 Stages of River Development: L. Immoor 2006 Geoteach.com 1 Youthful River: Perhaps the most dynamic of all rivers is a Youthful River. Rafters seeking an exciting ride will surely gravitate towards a young river for their recreational thrills. Characteristically youthful rivers are found at higher elevations, in mountainous areas, where the slope of the land is steeper. Water that flows over such a landscape will flow very fast. Youthful rivers can be a tributary of a larger and older river, hundreds of miles away and, in fact, they may be close to the headwaters (the beginning) of that larger river. Upon observation of a Youthful River, here is what one might see: 1. The river flowing down a steep gradient (slope). 2. The channel is deeper than it is wide and V-shaped due to downcutting rather than lateral (side-to-side) erosion. -
Land Degradation
SPM4 Land degradation Coordinating Lead Authors: Lennart Olsson (Sweden), Humberto Barbosa (Brazil) Lead Authors: Suruchi Bhadwal (India), Annette Cowie (Australia), Kenel Delusca (Haiti), Dulce Flores-Renteria (Mexico), Kathleen Hermans (Germany), Esteban Jobbagy (Argentina), Werner Kurz (Canada), Diqiang Li (China), Denis Jean Sonwa (Cameroon), Lindsay Stringer (United Kingdom) Contributing Authors: Timothy Crews (The United States of America), Martin Dallimer (United Kingdom), Joris Eekhout (The Netherlands), Karlheinz Erb (Italy), Eamon Haughey (Ireland), Richard Houghton (The United States of America), Muhammad Mohsin Iqbal (Pakistan), Francis X. Johnson (The United States of America), Woo-Kyun Lee (The Republic of Korea), John Morton (United Kingdom), Felipe Garcia Oliva (Mexico), Jan Petzold (Germany), Mohammad Rahimi (Iran), Florence Renou-Wilson (Ireland), Anna Tengberg (Sweden), Louis Verchot (Colombia/ The United States of America), Katharine Vincent (South Africa) Review Editors: José Manuel Moreno (Spain), Carolina Vera (Argentina) Chapter Scientist: Aliyu Salisu Barau (Nigeria) This chapter should be cited as: Olsson, L., H. Barbosa, S. Bhadwal, A. Cowie, K. Delusca, D. Flores-Renteria, K. Hermans, E. Jobbagy, W. Kurz, D. Li, D.J. Sonwa, L. Stringer, 2019: Land Degradation. In: Climate Change and Land: an IPCC special report on climate change, desertification, land degradation, sustainable land management, food security, and greenhouse gas fluxes in terrestrial ecosystems [P.R. Shukla, J. Skea, E. Calvo Buendia, V. Masson-Delmotte, H.-O. Pörtner, D. C. Roberts, P. Zhai, R. Slade, S. Connors, R. van Diemen, M. Ferrat, E. Haughey, S. Luz, S. Neogi, M. Pathak, J. Petzold, J. Portugal Pereira, P. Vyas, E. Huntley, K. Kissick, M. Belkacemi, J. Malley, (eds.)]. In press. -
Belt Width Delineation Procedures
Belt Width Delineation Procedures Report to: Toronto and Region Conservation Authority 5 Shoreham Drive, Downsview, Ontario M3N 1S4 Attention: Mr. Ryan Ness Report No: 98-023 – Final Report Date: Sept 27, 2001 (Revised January 30, 2004) Submitted by: Belt Width Delineation Protocol Final Report Toronto and Region Conservation Authority Table of Contents 1.0 INTRODUCTION......................................................................................................... 1 1.1 Overview ............................................................................................................... 1 1.2 Organization .......................................................................................................... 2 2.0 BACKGROUND INFORMATION AND CONTEXT FOR BELT WIDTH MEASUREMENTS …………………………………………………………………...3 2.1 Inroduction............................................................................................................. 3 2.2 Planform ................................................................................................................ 4 2.3 Meander Geometry................................................................................................ 5 2.4 Meander Belt versus Meander Amplitude............................................................. 7 2.5 Adjustments of Meander Form and the Meander Belt Width ............................... 8 2.6 Meander Belt in a Reach Perspective.................................................................. 12 3.0 THE MEANDER BELT AS A TOOL FOR PLANNING PURPOSES............................... -
Modification of Meander Migration by Bank Failures
JournalofGeophysicalResearch: EarthSurface RESEARCH ARTICLE Modification of meander migration by bank failures 10.1002/2013JF002952 D. Motta1, E. J. Langendoen2,J.D.Abad3, and M. H. García1 Key Points: 1Department of Civil and Environmental Engineering, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA, • Cantilever failure impacts migration 2National Sedimentation Laboratory, Agricultural Research Service, U.S. Department of Agriculture, Oxford, Mississippi, through horizontal/vertical floodplain 3 material heterogeneity USA, Department of Civil and Environmental Engineering, University of Pittsburgh, Pittsburgh, Pennsylvania, USA • Planar failure in low-cohesion floodplain materials can affect meander evolution Abstract Meander migration and planform evolution depend on the resistance to erosion of the • Stratigraphy of the floodplain floodplain materials. To date, research to quantify meandering river adjustment has largely focused on materials can significantly affect meander evolution resistance to erosion properties that vary horizontally. This paper evaluates the combined effect of horizontal and vertical floodplain material heterogeneity on meander migration by simulating fluvial Correspondence to: erosion and cantilever and planar bank mass failure processes responsible for bank retreat. The impact of D. Motta, stream bank failures on meander migration is conceptualized in our RVR Meander model through a bank [email protected] armoring factor associated with the dynamics of slump blocks produced by cantilever and planar failures. Simulation periods smaller than the time to cutoff are considered, such that all planform complexity is Citation: caused by bank erosion processes and floodplain heterogeneity and not by cutoff dynamics. Cantilever Motta, D., E. J. Langendoen, J. D. Abad, failure continuously affects meander migration, because it is primarily controlled by the fluvial erosion at and M. -
Meander Bend Migration Near River Mile 178 of the Sacramento River
Meander Bend Migration Near River Mile 178 of the Sacramento River MEANDER BEND MIGRATION NEAR RIVER MILE 178 OF THE SACRAMENTO RIVER Eric W. Larsen University of California, Davis With the assistance of Evan Girvetz, Alexander Fremier, and Alex Young REPORT FOR RIVER PARTNERS December 9, 2004 - 1 - Meander Bend Migration Near River Mile 178 of the Sacramento River Executive summary Historic maps from 1904 to 1997 show that the Sacramento River near the PCGID-PID pumping plant (RM 178) has experienced typical downstream patterns of meander bend migration during that time period. As the river meander bends continue to move downstream, the near-bank flow of water, and eventually the river itself, is tending to move away from the pump location. A numerical model of meander bend migration and bend cut-off, based on the physics of fluid flow and sediment transport, was used to simulate five future migration scenarios. The first scenario, simulating 50 years of future migration with the current conditions of bank restraint, showed that the river bend near the pump site will tend to move downstream and pull away from the pump location. In another 50-year future migration scenario that modeled extending the riprap immediately upstream of the pump site (on the opposite bank), the river maintained contact with the pump site. In all other future migration scenarios modeled, the river migrated downstream from the pump site. Simulations that included removing upstream bank constraints suggest that removing bank constraints allows the upstream bend to experience cutoff in a short period of time. Simulations show the pattern of channel migration after cutoff occurs. -
TRCA Meander Belt Width
Belt Width Delineation Procedures Report to: Toronto and Region Conservation Authority 5 Shoreham Drive, Downsview, Ontario M3N 1S4 Attention: Mr. Ryan Ness Report No: 98-023 – Final Report Date: Sept 27, 2001 (Revised January 30, 2004) Submitted by: Belt Width Delineation Protocol Final Report Toronto and Region Conservation Authority Table of Contents 1.0 INTRODUCTION......................................................................................................... 1 1.1 Overview ............................................................................................................... 1 1.2 Organization .......................................................................................................... 2 2.0 BACKGROUND INFORMATION AND CONTEXT FOR BELT WIDTH MEASUREMENTS …………………………………………………………………...3 2.1 Inroduction............................................................................................................. 3 2.2 Planform ................................................................................................................ 4 2.3 Meander Geometry................................................................................................ 5 2.4 Meander Belt versus Meander Amplitude............................................................. 7 2.5 Adjustments of Meander Form and the Meander Belt Width ............................... 8 2.6 Meander Belt in a Reach Perspective.................................................................. 12 3.0 THE MEANDER BELT AS A TOOL FOR PLANNING PURPOSES............................... -
Estuaries in the Balance: the Copano/Aransas Estuary Curriculum Guide
Estuaries in the Balance: The Copano/Aransas Estuary Curriculum Guide Development of this curriculum was made possible by funding from the Texas General Land Office Coast- al Management Program. The curriculum was developed and modified from “Project PORTS”, created by Lisa Calvo at Rutgers University and available at http://hsrl.rutgers.edu/~calvo/PORTS/Welcome.html. PRIMER DISCOVERING THE 1 COPANO/ARANSAS BAY SYSTEM The Copano/Aransas Estuary is the region where waters from the Mis- sion and Aransas Rivers flow into the Copano Bay, and from there, to the RELATED VOCABULARY Aransas Bay and then the Gulf of Mexico. Estuaries are dynamic sys- tems where tidal and river currents mix fresh river water with salty ocean Estuary—an area partially surrounded by land where fresh water and salt water meet. water. As a result the salt content, or salinity, of estuarine waters varies from fresh to brackish to salt water. Copano Bay, fed by the Mission and Watershed—an area of land drained by a river Aransas Rivers and Copano Creek, covers about 65 square miles. The or other body of water. Copano Bay watershed drains an area of 1,388,781 square miles. It Salinity—the salt content of water. Estuarine connects to Aransas Bay, which has an area of 70 square miles and is waters vary from fresh (no salt) to marine (salty ocean water). in turn bordered on the east by San Jose Island, a 21-mile long barrier island. Density—the mass (amount of material) in a certain volume of matter. Estuaries serve as vital habitats and critical nursery grounds for many Euryhaline—describing species which can toler- species of plants and animals. -
2008 Basin Summary Report San Antonio-Nueces Coastal Basin Nueces River Basin Nueces-Rio Grande Coastal Basin
2008 Basin Summary Report San Antonio-Nueces Coastal Basin Nueces River Basin Nueces-Rio Grande Coastal Basin August 2008 Prepared in cooperation with the Texas Commission on Environmental Quality Clean Rivers Program Table of Contents List of Acronyms ................................................................................................................................................... ii Executive Summary ............................................................................................................................................. 1 Significant Findings ......................................................................................................................................... 1 Recommendations .......................................................................................................................................... 4 1.0 Introduction ................................................................................................................................................... 5 2.0 Public Involvement ....................................................................................................................................... 6 Public Outreach .............................................................................................................................................. 6 3.0 Water Quality Reviews .................................................................................................................................. 8 3.1 Water Quality Terminology -
General Manager Position Profile
General Manager Position Profile Organization overview The San Antonio River Authority is an award-winning agency dedicated to preserving, protecting, and managing the resources and environment of the San Antonio River basin (Bexar, Goliad, Karnes, and Wilson counties.) It is involved in flood control, water quality, parks, wastewater services, and conservation. In 1937, the Texas legislature created what is now the San Antonio River Authority, which has authority to impose an ad valorem tax, proceeds from which can only be used for planning, operations, and maintenance. The current tax rate is set at $0.01858 per $100 assessed property valuation; average annual tax on a residential homestead is $40.20. The River Authority’s 2020-2021 budget is $374 million and it has more than 300 employees. The River Authority is governed by 12 elected directors – six from Bexar County and two each from the other counties. “Committed to Safe, Clean, Enjoyable Creeks and Rivers” is the mission statement of the River Authority. Examples of actions the River Authority has taken toward the mission statement include: Safe • Providing project management and technical expertise on flood mitigation. • Constructing, operating, and maintaining flood control dams. • Helping to update and maintain floodplain maps. • Developing predictive flood technology. • Creating and maintaining watershed master plans; partnering with other agencies in the regional watershed management program. • Managing such major projects as the San Antonio River Improvements Project (13 miles of the San Antonio River in urban San Antonio) and the San Pedro Creek Improvements Project (unique urban greenspace in downtown San Antonio). • Removing debris to maintain flow capacity of waterways.