Stream Bank Protection and Erosion Damage Mitigation Measures
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Protection Against Wave-Based Erosion
Protection against Wavebased Erosion The guidelines below address the elements of shore structure design common to nearly all erosion control structures subject to direct wave action and run-up. 1. Minimize the extent waterward. Erosion control structures should be designed with the smallest waterward footprint possible. This minimizes the occupation of the lake bottom, limits habitat loss and usually results in a lower cost to construct the project. In the case of stone revetments, the crest width should be only as wide as necessary for a stable structure. In general, the revetment should follow the cross-section of the bluff or dune and be located as close to the bluff or dune as possible. For seawalls, the distance that the structure extends waterward of the upland must be minimized. If the seawall height is appropriately designed to prevent the majority of overtopping, there is no engineering rationale based only on erosion control which justifies extending a seawall out into the water. 2. Minimize the impacts to adjacent properties. The design of the structure must consider the potential for damaging adjacent property. Projects designed to extend waterward of the shore will affect the movement of littoral material, reducing the overall beach forming process which in turn may cause accelerated erosion on adjacent or down-drift properties with less protective beaches. Seawalls, (and to a lesser extent, stone revetments) change the direction (wave reflection) and intensity of wave energy along the shore. Wave reflection can cause an increase in the total energy at the seawall or revetment interface with the water, allowing sand and gravel to remain suspended in the water, which will usually prevent formation of a beach directly fronting the structure. -
Item Unit of Specification Description Number
ITEM UNIT OF SPECIFICATION DESCRIPTION NUMBER MEASURE YEAR REFERENCE ------- ----------------- --------- ------------------------ --------------------------------------------------------------------------- 0001.00 CAL DAY 08 SURVEILLANCE OF TEMPORARY TRAFFIC CONTROL DEVICES ------- ----------------- --------- ------------------------ --------------------------------------------------------------------------- 0001.04 DAY 08 ENDANGERED SPECIES DAILY SURVEYOR ------- ----------------- --------- ------------------------ --------------------------------------------------------------------------- 0001.06 BARR DAY 08 VERTICAL PANELS ------- ----------------- --------- ------------------------ --------------------------------------------------------------------------- 0001.08 BARR DAY 08 422.00 BARRICADE, TYPE II ------- ----------------- --------- ------------------------ --------------------------------------------------------------------------- 0001.10 BARR DAY 08 422.00 BARRICADE, TYPE III ------- ----------------- --------- ------------------------ --------------------------------------------------------------------------- 0001.20 EACH 08 BARRICADE, TYPE III ------- ----------------- --------- ------------------------ --------------------------------------------------------------------------- 0001.30 LIGHT DAY 08 422.00 TYPE B HIGH INTENSITY WARNING LIGHT ------- ----------------- --------- ------------------------ --------------------------------------------------------------------------- 0001.45 BARR DAY 08 REFLECTORIZED PLASTIC DRUM ------- -
Geomorphic Classification of Rivers
9.36 Geomorphic Classification of Rivers JM Buffington, U.S. Forest Service, Boise, ID, USA DR Montgomery, University of Washington, Seattle, WA, USA Published by Elsevier Inc. 9.36.1 Introduction 730 9.36.2 Purpose of Classification 730 9.36.3 Types of Channel Classification 731 9.36.3.1 Stream Order 731 9.36.3.2 Process Domains 732 9.36.3.3 Channel Pattern 732 9.36.3.4 Channel–Floodplain Interactions 735 9.36.3.5 Bed Material and Mobility 737 9.36.3.6 Channel Units 739 9.36.3.7 Hierarchical Classifications 739 9.36.3.8 Statistical Classifications 745 9.36.4 Use and Compatibility of Channel Classifications 745 9.36.5 The Rise and Fall of Classifications: Why Are Some Channel Classifications More Used Than Others? 747 9.36.6 Future Needs and Directions 753 9.36.6.1 Standardization and Sample Size 753 9.36.6.2 Remote Sensing 754 9.36.7 Conclusion 755 Acknowledgements 756 References 756 Appendix 762 9.36.1 Introduction 9.36.2 Purpose of Classification Over the last several decades, environmental legislation and a A basic tenet in geomorphology is that ‘form implies process.’As growing awareness of historical human disturbance to rivers such, numerous geomorphic classifications have been de- worldwide (Schumm, 1977; Collins et al., 2003; Surian and veloped for landscapes (Davis, 1899), hillslopes (Varnes, 1958), Rinaldi, 2003; Nilsson et al., 2005; Chin, 2006; Walter and and rivers (Section 9.36.3). The form–process paradigm is a Merritts, 2008) have fostered unprecedented collaboration potentially powerful tool for conducting quantitative geo- among scientists, land managers, and stakeholders to better morphic investigations. -
Geography for the IB DIPLOMA
OXFORD IB STUDY GUIDES Garrett Nagle Briony Cooke Geography FOR THE IB DIPLOMA 2nd edition OPTION A FRESHWATER – DRAINAGE BASINS 1 DRAINAGE BASIN HYDROLOGY AND GEOMORPHOLOGY The drainage basin DEFINITIONS Evaporation is the physical process by which a liquid becomes a gas. It is a function of: The drainage basin is an area that is drained by a river • vapour pressure and its tributaries. Drainage basins have inputs, stores, • air temperature processes and outputs. The inputs and outputs cross the • wind boundary of the drainage basin, hence the drainage basin • rock surface, for example, bare soils and rocks have is an open system. The main input is precipitation, which is high rates of evaporation compared with surfaces regulated by various means of storage. The outputs include which have a protective tilth where rates are low. evaporation and transpiration. Flows include infiltration, throughflow, overland flow and base flow, and stores Transpiration is the loss of water from vegetation. include vegetation, soil, aquifers and the cryosphere (snow Evapotranspiration is the combined loss of water and ice). from vegetation and water surfaces to the atmosphere. Drainage basin hydrology Potential evapotranspiration is the rate of water loss from an area if there were no shortage of water. PRECIPITATION Channel Interception precipitation 1. VEGETATION FLOWS Stemflow & throughfall Infiltration is the process by which water sinks into the Overland flow 2. SURFACE STORAGE 5. CHANNEL ground. Infiltration capacity refers to the amount of Floods moisture that a soil can hold. By contrast, the infiltration Capilliary Infiltration rise rate refers to the speed with which water can enter the Interflow 3. -
Linktm Gabions and Mattresses Design Booklet
LinkTM Gabions and Mattresses Design Booklet www.globalsynthetics.com.au Australian Company - Global Expertise Contents 1. Introduction to Link Gabions and Mattresses ................................................... 1 1.1 Brief history ...............................................................................................................................1 1.2 Applications ..............................................................................................................................1 1.3 Features of woven mesh Link Gabion and Mattress structures ...............................................2 1.4 Product characteristics of Link Gabions and Mattresses .........................................................2 2. Link Gabions and Mattresses .............................................................................. 4 2.1 Types of Link Gabions and Mattresses .....................................................................................4 2.2 General specification for Link Gabions, Link Mattresses and Link netting...............................4 2.3 Standard sizes of Link Gabions, Mattresses and Netting ........................................................6 2.4 Durability of Link Gabions, Link Mattresses and Link Netting ..................................................7 2.5 Geotextile filter specification ....................................................................................................7 2.6 Rock infill specification .............................................................................................................8 -
Shoreline Management in Chesapeake Bay C
Shoreline Management In Chesapeake Bay C. S. Hardaway, Jr. and R. J. Byrne Virginia Institute of Marine Science College of William and Mary 1 Cover Photo: Drummond Field, Installed 1985, James River, James City County, Virginia. This publication is available for $10.00 from: Sea Grant Communications Virginia Institute of Marine Science P. O. Box 1346 Gloucester Point, VA 23062 Special Report in Applied Marine Science and Ocean Engineering Number 356 Virginia Sea Grant Publication VSG-99-11 October 1999 Funding and support for this report were provided by... Virginia Institute of Marine Science Virginia Sea Grant College Program Sea Grant Contract # NA56RG0141 Virginia Coastal Resource Management Program NA470Z0287 WILLIAM& MARY Shoreline Management In Chesapeake Bay By C. Scott Hardaway, Jr. and Robert J. Byrne Virginia Institute of Marine Science College of William and Mary Gloucester Point, Virginia 23062 1999 4 Table of Contents Preface......................................................................................7 Shoreline Evolution ................................................................8 Shoreline Processes ..............................................................16 Wave Climate .......................................................................16 Shoreline Erosion .................................................................20 Reach Assessment ................................................................23 Shoreline Management Strategies ......................................24 Bulkheads and Seawalls -
Flood Hazard of Dunedin's Urban Streams
Flood hazard of Dunedin’s urban streams Review of Dunedin City District Plan: Natural Hazards Otago Regional Council Private Bag 1954, Dunedin 9054 70 Stafford Street, Dunedin 9016 Phone 03 474 0827 Fax 03 479 0015 Freephone 0800 474 082 www.orc.govt.nz © Copyright for this publication is held by the Otago Regional Council. This publication may be reproduced in whole or in part, provided the source is fully and clearly acknowledged. ISBN: 978-0-478-37680-7 Published June 2014 Prepared by: Michael Goldsmith, Manager Natural Hazards Jacob Williams, Natural Hazards Analyst Jean-Luc Payan, Investigations Engineer Hank Stocker (GeoSolve Ltd) Cover image: Lower reaches of the Water of Leith, May 1923 Flood hazard of Dunedin’s urban streams i Contents 1. Introduction ..................................................................................................................... 1 1.1 Overview ............................................................................................................... 1 1.2 Scope .................................................................................................................... 1 2. Describing the flood hazard of Dunedin’s urban streams .................................................. 4 2.1 Characteristics of flood events ............................................................................... 4 2.2 Floodplain mapping ............................................................................................... 4 2.3 Other hazards ...................................................................................................... -
Erosion-1.Pdf
R E S O U R C E L I B R A R Y E N C Y C L O P E D I C E N T RY Erosion Erosion is the geological process in which earthen materials are worn away and transported by natural forces such as wind or water. G R A D E S 6 - 12+ S U B J E C T S Earth Science, Geology, Geography, Physical Geography C O N T E N T S 9 Images For the complete encyclopedic entry with media resources, visit: http://www.nationalgeographic.org/encyclopedia/erosion/ Erosion is the geological process in which earthen materials are worn away and transported by natural forces such as wind or water. A similar process, weathering, breaks down or dissolves rock, but does not involve movement. Erosion is the opposite of deposition, the geological process in which earthen materials are deposited, or built up, on a landform. Most erosion is performed by liquid water, wind, or ice (usually in the form of a glacier). If the wind is dusty, or water or glacial ice is muddy, erosion is taking place. The brown color indicates that bits of rock and soil are suspended in the fluid (air or water) and being transported from one place to another. This transported material is called sediment. Physical Erosion Physical erosion describes the process of rocks changing their physical properties without changing their basic chemical composition. Physical erosion often causes rocks to get smaller or smoother. Rocks eroded through physical erosion often form clastic sediments. -
The Biology and Management of the River Dee
THEBIOLOGY AND MANAGEMENT OFTHE RIVERDEE INSTITUTEofTERRESTRIAL ECOLOGY NATURALENVIRONMENT RESEARCH COUNCIL á Natural Environment Research Council INSTITUTE OF TERRESTRIAL ECOLOGY The biology and management of the River Dee Edited by DAVID JENKINS Banchory Research Station Hill of Brathens, Glassel BANCHORY Kincardineshire 2 Printed in Great Britain by The Lavenham Press Ltd, Lavenham, Suffolk NERC Copyright 1985 Published in 1985 by Institute of Terrestrial Ecology Administrative Headquarters Monks Wood Experimental Station Abbots Ripton HUNTINGDON PE17 2LS BRITISH LIBRARY CATALOGUING-IN-PUBLICATIONDATA The biology and management of the River Dee.—(ITE symposium, ISSN 0263-8614; no. 14) 1. Stream ecology—Scotland—Dee River 2. Dee, River (Grampian) I. Jenkins, D. (David), 1926– II. Institute of Terrestrial Ecology Ill. Series 574.526323'094124 OH141 ISBN 0 904282 88 0 COVER ILLUSTRATION River Dee west from Invercauld, with the high corries and plateau of 1196 m (3924 ft) Beinn a'Bhuird in the background marking the watershed boundary (Photograph N Picozzi) The centre pages illustrate part of Grampian Region showing the water shed of the River Dee. Acknowledgements All the papers were typed by Mrs L M Burnett and Mrs E J P Allen, ITE Banchory. Considerable help during the symposium was received from Dr N G Bayfield, Mr J W H Conroy and Mr A D Littlejohn. Mrs L M Burnett and Mrs J Jenkins helped with the organization of the symposium. Mrs J King checked all the references and Mrs P A Ward helped with the final editing and proof reading. The photographs were selected by Mr N Picozzi. The symposium was planned by a steering committee composed of Dr D Jenkins (ITE), Dr P S Maitland (ITE), Mr W M Shearer (DAES) and Mr J A Forster (NCC). -
Cumulative Effective Stream Power and Bank Erosion on the Sacramento River, California, Usa1
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION AUGUST AMERICAN WATER RESOURCES ASSOCIATION 2006 CUMULATIVE EFFECTIVE STREAM POWER AND BANK EROSION ON THE SACRAMENTO RIVER, CALIFORNIA, USA1 Eric W. Larsen, Alexander K. Fremier, and Steven E. Greco2 ABSTRACT: Bank erosion along a river channel determines the INTRODUCTION pattern of channel migration. Lateral channel migration in large alluvial rivers creates new floodplain land that is essential for Natural rivers and their surrounding areas consti- riparian vegetation to get established. Migration also erodes tute some of the world’s most diverse, dynamic, and existing riparian, agricultural, and urban lands, sometimes complex terrestrial ecosystems (Naiman et al., 1993). damaging human infrastructure (e.g., scouring bridge founda- Land deposition on the inside bank of a curved river tions and endangering pumping facilities) in the process. channel is a process that creates opportunities for Understanding what controls the rate of bank erosion and asso- vegetation to colonize the riparian corridor (Hupp and ciated point bar deposition is necessary to manage large allu- Osterkamp, 1996; Mahoney and Rood, 1998). Point vial rivers effectively. In this study, bank erosion was bar deposition and outside bank erosion are tightly proportionally related to the magnitude of stream power. Linear coupled. These physical processes (which constitute regressions were used to correlate the cumulative stream channel migration) maintain ecosystem heterogeneity power, above a lower flow threshold, with rates of bank erosion in floodplains over space and time (Malanson, 1993). at 13 sites on the middle Sacramento River in California. Two Channel migration structures and sustains riparian forms of data were used: aerial photography and field data. -
Tennessee Erosion & Sediment Control Handbook
TENNESSEE EROSION & SEDIMENT CONTROL HANDBOOK A Stormwater Planning and Design Manual for Construction Activities Fourth Edition AUGUST 2012 Acknowledgements This handbook has been prepared by the Division of Water Resources, (formerly the Division of Water Pollution Control), of the Tennessee Department of Environment and Conservation (TDEC). Many resources were consulted during the development of this handbook, and when possible, permission has been granted to reproduce the information. Any omission is unintentional, and should be brought to the attention of the Division. We are very grateful to the following agencies and organizations for their direct and indirect contributions to the development of this handbook: TDEC Environmental Field Office staff Tennessee Division of Natural Heritage University of Tennessee, Tennessee Water Resources Research Center University of Tennessee, Department of Biosystems Engineering and Soil Science Civil and Environmental Consultants, Inc. North Carolina Department of Environment and Natural Resources Virginia Department of Conservation and Recreation Georgia Department of Natural Resources California Stormwater Quality Association ~ ii ~ Preface Disturbed soil, if not managed properly, can be washed off-site during storms. Unless proper erosion prevention and sediment control Best Management Practices (BMP’s) are used for construction activities, silt transport to a local waterbody is likely. Excessive silt causes adverse impacts due to biological alterations, reduced passage in rivers and streams, higher drinking water treatment costs for removing the sediment, and the alteration of water’s physical/chemical properties, resulting in degradation of its quality. This degradation process is known as “siltation”. Silt is one of the most frequently cited pollutants in Tennessee waterways. The division has experimented with multiple ways to determine if a stream, river, or reservoir is impaired due to silt. -
Defining the Moment of Erosion
Earth Surface Processes and Landforms EarthDefining Surf. the Process. moment Landforms of erosion 30, 1597–1615 (2005) 1597 Published online in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/esp.1234 Defining the moment of erosion: the principle of thermal consonance timing D. M. Lawler* School of Geography, Earth and Environmental Sciences, The University of Birmingham, Birmingham B15 2TT, UK *Correspondence to: Abstract D. M. Lawler, School of Geography, Earth and Geomorphological process research demands quantitative information on erosion and deposi- Environmental Sciences, tion event timing and magnitude, in relation to fluctuations in the suspected driving forces. University of Birmingham, This paper establishes a new measurement principle – thermal consonance timing (TCT) Birmingham B15 2TT. – which delivers clearer, more continuous and quantitative information on erosion and E-mail: [email protected] deposition event magnitude, timing and frequency, to assist understanding of the controlling mechanisms. TCT is based on monitoring the switch from characteristically strong tempera- ture gradients in sediment, to weaker gradients in air or water, which reveals the moment of erosion. The paper (1) derives the TCT principle from soil micrometeorological theory; (2) illustrates initial concept operationalization for field and laboratory use; (3) presents experimental data for simple soil erosion simulations; and (4) discusses initial application of TCT and perifluvial micrometeorology principles in the delivery of timing solutions for two bank erosion events on the River Wharfe, UK, in relation to the hydrograph. River bank thermal regimes respond, as soil temperature and energy balance theory pre- dicts, with strong horizontal thermal gradients (often >>>1Kcm−−−1 over 6·8 cm).