DOCSLIB.ORG

Geomorphic Response of Rivers Below Dams by Sediment Replenishment Technique

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Geomorphic Response of Rivers Below Dams by Sediment Replenishment Technique River Flow 2010 - Dittrich, Koll, Aberle & Geisenhainer (eds) - © 2010 Bundesanstalt für Wasserbau ISBN 978-3-939230-00-7 Geomorphic response of rivers below dams by sediment replenishment technique S. A. Kantoush & T. Sumi Water Resources Research Center, Disaster Prevention Research Institute, Kyoto University, Japan A. Kubota Kizugawa Dams Integrated Operation & Management Office, Japan Water Agency, Japan ABSTRACT: Sedimentation problems on regulated rivers are considerably different from natural rivers. An effective means of reservoir sediment management is to excavate deposited sediments within reser- voir and transport to the river downstream of a dam. The flood is designed to erode the placed sediment at the banks of Nunome River, in an effort to restore the lower reach of the river to a more natural ecosys- tem. Since 2004, six attempts of sediment replenishment to rebuilding vital sediment sand bars below Nunome dam are in progressing. Monitoring measurements pre- and post- replenishment show the effect of improvements in riverbed formation, grain size distribution, and erosion processes. Actual field expe- riments are presented and compared with scaled laboratory experiments, with the objective of identifying parameters and process of sediment replenishment characteristics. The paper investigates the influence of sediment replenishment below Nunome Dam on changes of river bed. Appropriate sediment materials, which are excavated and treated from the upper part of the Nunome reservoir, and supplied to down- stream rivers contributes to rebuilt sand bars, mitigate the armouring of river bed, and management of re- servoir sedimentation. With the field experiments, the processes are directly visible and a wealth of valu- able data is obtained, and will be used for numerical modeling in future application. Keywords: Dam impacts, Reservoir sediment replenishment, Sediment management, River restoration, Revitalization of regulated rivers, Sediment feeding, Geomorphic response 1 INTRODUCTION Dam Impacts on: 1.1 Dam Impacts Morphological Hydrological Ecological Loss of aquatic and River bank Water table lowering Dams greatly influence flow and sediment dis- instability riparian habitats charge regimes and can have significant impacts on downstream reaches below dam. Bed load se- Bed armouring Reduction in overall flows oxygen stratification diment management is required to preserve the River incision and Changes in flood capabilities of water resources facilities and to bed degradation Nutrient exchange frequency and magnitude conserve the environment in rivers downstream of Impacts on the reservoir. The sediment deficit produces a infrastructures Changes in seasonal flow Gas-bubble disease large variety of physical, ecological and environ- Sediment deficit to Adverse effect on mental effects. To mitigate that coarse sediments, coastal zones Changes hydrodynamic within estuaries water quality by grain diameter, with specific grain size distri- butions artificially replenished to satisfy the river Figure 1. Possible impacts due to lack of sediment transport bed load capacity (sediment replenishment). Fig- in the downstream reach below dams ure 1 classifies the impacts of sediment deficit be- In addition, dams alter the downstream flow low dams to three groups; morphological, hydro- regime of rivers (Williams and Wolman, 1984), logical, and ecological effects. Sediment deficit is which controls many physical and ecological as- not only an environmental issue but also a socio- pects of river form and processes, including sedi- economic problem, for instance due to loss of re- ment transport and nutrient exchange (Poff et al., servoir capacity (Fan and Springer, 1993). 1997). Morphological effects on the river channel 1155 (e.g., Kondolf and Matthews, 1993; Shields et al., geometry are influenced by variability in water 2000) that includes riverbed incision, riverbank and sediment release. Sediment replenishment instability, upstream erosion in tributaries, dam- scenarios may, induce undesirable morphological age to bridges, embankments and levees (e.g., and ecological consequences as well as significant Kondolf, 1997), and changes in channel width channel adjustments that can result in failure of (e.g., Wilcock et al., 1996). Hydrological effects the restoration project itself. That is, it is neces- caused by dams include changes in flood frequen- sary to better understand reversibility, direction cy and magnitude, reduction in overall flows, and time scale of changes, and the sustainability changes in seasonal flows, and altered timing of of a replenishment intervention before it is im- releases (Ligon et al., 1995). plemented. 1.2 Sediment Replenishment Projects in Japan 1.3 Objectives Large Japanese rivers are often trained to a large The study focuses on the design criteria for sedi- extent, to maintain services such as navigation, ment replenishment project in Japan to improve hydropower generation and flood defense. Okano river bed conditions. The investigations are based et al., (2004) summarized sediment replenishment on field and laboratory experiments. The objec- projects in Japanese Rivers, such as Tenryu, Ota- tives of this paper are: (a) to make a general re- kine, Abukuma, Ara, Oi, Naka, Kuzuryu, Yodo, view of impacts of dam on downstream reach; (b) Kanna, and Tone, have been conducted by Minis- to discuss the role of different factors influencing try of Land, Infrastructure and Transport (MLIT). the sediment replenishment research; (c) to illu- Kantoush et al. (2010) investigated the morpho- strate and analyze the sediment replenishment logical evolution and corresponding flow field through a regulated fluvial system during actual during replenishment experiments in Uda River, field tests. Japan. Sediment treatment system is applied by Sumi et al. (2009), to produce appropriate grain sized material with less turbidity. Seto et al. 2 FIELD EXPERIMENTS FOR SEDIMENT (2009), analyzed sediment replenishment effects REPLENISHMENT IN NUNOME RIVER on the downstream river of Yahagi dam. 2.1 Test Procedure and Replenishing Concept Factors of Sediment Replenishment In Japan, it is common practice to remove accu- Sediment Flow Physical River Physical Replenishment Monitoring Economics mulated coarse sediment by excavation and dredg- Physical Characteristics Characteristics Characteristics Characteristics Characteristics Characteristics ing, and to make effective use of the removed se- Flood flow Initial bed Placed sediment Water quality Excavation and Porosity and discharges (Flood morphology and volume and (turbidity, Ph, sediment diment. Sediment replenishment method is one of density hydrographs) slopes geometry shape temperature, treatment costs new measures of sediment management. In this Bed material size, Submerged or Environmental (fish Sediment type and Flow water depths gradation and partial or un species, stream Transportation cost method, trapped sediment is periodically exca- cohesion permeability submerged state invertebrates, algae) vated and then transported to be placed temporari- Grain size Flow duration Sediment rating Locations and Flow field and distribution, and curve and curve (suspended placement Feeding cost ly downstream of the dam. In a manner decided percentage of fine frequency and bed loads) arrangement along vertical velocity sediment the river profiles according to the sediment transport capacity of the Treatment of Flow patterns and River bank Cross sectional Frequency of Monitoring cost excavated and velocity profiles vegetation feeding per year survey and precise channel and the environmental conditions. There- dredged sediment and season surveying of riffles and pools fore, the sediment is returned to the channel Indirect (side bank Erosion rate and Volume of Trapped feeding) or direct Visual inspection Sediment source type (side bank or sediment in (in river) feeding and grain size Project benefits downstream in the natural flooding processes. The vortex types) reservoirs method analysis procedure of the experiments consists of four Figure 2. Main groups of sediment replenishment characte- steps: (1) extracting mechanically the accumu- ristics and managing factors lated sediment at check dam; (2) transporting it by Sediment transport and associated channel bed truck to downstream river; (3) placing the sedi- mobility are recognized as key processes for ment with specific geometry (Figure 3), and (4) creating and maintaining physical habitats, aquatic monitoring flow, sediment, and environmental pa- and riparian ecosystems. In Japan, sediment rep- rameters. lenishment projects are undertaking with different Placed sediment configurations and characteristics of sediment and geometry discharges. Figure 2 summarizes factors that in- Flood stage fluence the sediment replenishment research. These factors are classified in six groups as shown Normal stage in Figure 2. Several significant gaps in the scien- tific understanding of these processes remain, par- Figure 3. Concept of sediment replenishment and placed se- ticularly concerning how riverbed deposition and diment geometry on the bank of Nunome River 1156 The replenished sediment is placed at such an 2.4 Case Study of Nunome Dam Actual Sediment elevation; in order to reduce the turbidity during Replenishment Tests normal flow period. The top of the sediment is ad- Since 2004, six experiments of sediment reple- justed so that the sediment is completely sub- nishment projects with different sediment volumes merged during flood at several
Load more

Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Planning, Design and Estimation of a Check Dam B.H
    ISSN XXXX XXXX © 2017 IJESC Research Article Volume 7 Issue No.4 Planning, Design and Estimation of a Check Dam B.H. Ramathilagam1, S. Murugesan2, M. Manikandan3, A. Arumugaraja4, Assistant professor1, U. G. student2, 3, 4 Department of Civil Sethu institute of technology, Virudhunagar, India Abstract To overcome these issues on a global scale, water erosion is the most severe type of soil erosion. It occurs mostly in the form of running water. This study was to develop information from dam which check dam can be adopted for the purpose of ground water recharge. Dams are constructions built across a river or a stream and used to interrupt and store water for special purpose. Check dams are comparatively smaller and more temporary to other types of dams for the purpose of ground water recharge. The Study consisted of a site selection phase, a surveying phase, an planning phase, an design phase and estimation analysis. .This Particular scheme lies in highly favourable zone for recharge as classified in the zonation map for Ground water recharge. By implementing this scheme, with in the zone of influence of about 1 km radius from the check dam site will be benefitted by way of percolation. Increase the Ground water level and increase the revenue through the ayacut . Totally 185.02.0 Ha Ayacut is benefitted through Seventy Eight No’s of wells. Moreover, all the wells (both domestic and agricultural wells) within the zone of influence will be recharged. The length of the check dam is 106m. The design and Estimation of the structure is done using the software Ms-Excel.
    [Show full text]
  • CHAPTER 5 Temporary Runoff Control
    CHAPTER 5 Temporary Runoff Control Temporary runoff control is important designer and contractor recognize these on developing sites to minimize on-site opportunities to reduce site runoff. erosion and to prevent off-site sediment Sediment laden water must be routed to discharge. Temporary runoff control an appropriate sediment control device primarily consists of two main strate- before leaving the site. Conveying run- gies: keeping off site water clean and off through stabilized temporary diver- managing on site sediment laden water. sions and slope drains not only directs Off site water that passes through an muddy water to treatment devices but active construction site should be kept also reduces further erosion and pre- as clean as possible. This is accom- vents costly re-grading associated with plished by routing this flow through gully development. Effective runoff the site without opportunity to mix control also makes re-vegetation easier with untreated site runoff or by divert- and less costly. ing clean water can be diverted around The practices outlined in this chapter construction areas. Sediment control will significantly increase the effective- practices generally will be more effec- ness of a sediment and erosion control tive, less expensive and require less plan. maintenance by not incorporating off site water. Diversions and temporary crossings are examples of runoff con- trols that are designed to keep off site water clean. Once construction begins, erosion will occur. To minimize erosion, site 5.1 Rock Check Dam ....................................3 runoff must be managed. This starts by minimizing the amount of disturbance 5.2 Slope Drain ..............................................7 and maintaining existing vegetation as 5.3 Temporary Diversion ..............................10 much as possible to reduce the volume 5.4 Stream Utility Crossing ..........................15 of runoff generated and subsequent 5.5 Temporary Stream Crossing ..................23 erosion.
    [Show full text]
  • Engineering and Mitigation
    Engineering and Mitigation 919 7th International Conference on Debris-Flow Hazards Mitigation Predicting debris-flow scour depth downstream from a check dam Hua-Yong Chena,b,c*, Xiao-Qing Chena,b,c, Jian-Gang Chena,b,c, and Jin-Bo Tanga,b a Key Laboratory of Mountain Hazards and Earth Surface Process/Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China b University of Chinese Academy of Sciences, Beijing 100049, China c CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences (CAS), Beijing, 100101, China Abstract Debris flows often pose great threats to people’s lives and property in mountainous regions. For example on August 8, 2010, a debris flow with a volume of 220×104 m3 occurred in ZhouQu county, Gansu province, China. The debris flow resulted in not only significant loss of farmlands, but also in 1,248 deaths and 496 people missing. The construction of check dams in debris- flow valleys is a useful way to mitigate deaths and damages. Herein, we investigate scour downstream from check dam spillway structures. We propose that the main parameters which determine scour depth of a scour hole downstream from check dams, include flow density, flow depth, flow discharge per unit width, and acceleration due to gravity. Physical experiments were also carried out to investigate debris flow movement and scour characteristics. In addition, a theoretical expression was deduced to predict the maximum scour depth downstream from check dams. There was a good correlation between experimental data and results predicted from theory. The results obtained in this paper can provide constraints for the design of check dams in mountainous areas.
    [Show full text]
  • Section 6 - Structural Bmps Volume/Peak Rate Reduction by Infiltration Bmps BMP 6.7: Constructed Filter
    Section 6 - Structural BMPs Volume/Peak Rate Reduction by Infiltration BMPs BMP 6.7: Constructed Filter Filters are structures or excavated areas containing a layer of sand, compost, organic material, peat, or other filter media that reduce pollutant levels in stormwater runoff by filtering sediments, metals, hydrocarbons, and other pollutants. Key Design Elements Potential Applications • Drain down – should empty within 72 hrs Residential: LIMITED Commercial: YES Ultra Urban: YES • Minimum permeability of filtration medium required Industrial: YES Retrofit: YES • Minimum depth of filtering medium = 18" Highway/Road: YES • Perforated pipes (4" min) in stone Stormwater Functions • May be designed to collect and convey filtered runoff down-gradient Volume Reduction: Low-Med* Recharge: Low-Med* • May be designed to infiltrate Peak Rate Control: Low/High Water Quality: High • Pretreatment for debris and sediment may be needed *If Infiltration Used • Must be sized for drainage area Pollutant Removal TSS: 85% • Regular inspection and maintenance required for TP: 85% continued functioning NO3: 30% • Positive overflow is required Other Considerations • Certain applications may warrant spill containment • Infiltration Systems Guidelines and Soil Investigation Guidelines should be followed, see Section 6.8. Draft Pennsylvania Stormwater Management Manual 6-277 Section 6 - Structural BMPs Description A stormwater filter is a structure or excavation filled with material and designed to filter stormwater runoff to improve water quality. The filter media may be comprised of materials such as sand, peat, compost, granular activated carbon (GAC), perlite, or other material. In some applications the stormwater runoff flows through an open air, “pretreatment” chamber to allow the large particles and debris to settle out (sedimentation).
    [Show full text]
  • Technical Supplement 14P--Gullies and Their Control
    Technical Gullies and Their Control Supplement 14P (210–VI–NEH, August 2007) Technical Supplement 14P Gullies and Their Control Part 654 National Engineering Handbook Issued August 2007 Cover photo: Gully erosion may be a significant source of sediment to the stream. Gullies may also form in the streambanks due to uncontrolled flows from the flood plain (valley trenches). Advisory Note Techniques and approaches contained in this handbook are not all-inclusive, nor universally applicable. Designing stream restorations requires appropriate training and experience, especially to identify conditions where various approaches, tools, and techniques are most applicable, as well as their limitations for design. Note also that prod- uct names are included only to show type and availability and do not constitute endorsement for their specific use. (210–VI–NEH, August 2007) Technical Gullies and Their Control Supplement 14P Contents Purpose TS14P–1 Introduction TS14P–1 Classical gullies and ephemeral gullies TS14P–3 Gullying processes in streams TS14P–3 Issues contributing to gully formation or enlargement TS14P–5 Land use practices .........................................................................................TS14P–5 Soil properties ................................................................................................TS14P–6 Climate ............................................................................................................TS14P–6 Hydrologic and hydraulic controls ..............................................................TS14P–6
    [Show full text]
  • Gully Prevention and Control
    Gully Rehabilitation Principle: “Prevention is better than Cure” 2012 Nile Basin Initiative Eastern Nile Subsidiary Action Program (ENSAP) Eastern Nile Technical Regional Office (ENTRO) Eastern Nile Watershed Management Project A Field Guide on Gully Prevention and Control March 2012 Prepared by: LAKEW DESTA & BELAYNEH ADUGNA P.O. Box 27173‐1000, Addis Ababa, Ethiopia Tel. +251 (11) 646 1130/646 1132, fax: +251 (11) 645 9407 Email: [email protected] or [email protected] Web site: www.nilebasin.org/entro Gully Rehabilitation Principle: “Prevention is better than Cure” 2012 Table of Contents 1. Introduction ................................................................................................................................................ 1 2. Process of Soil Erosion and Gully Formation ............................................................................................ 4 3. Factors Affecting Gully Formation ............................................................................................................ 8 3.1. Man-made factors .............................................................................................................................. 9 3.1.1. Improper land use....................................................................................................................... 9 3.1.2. Forest and grass fires .................................................................................................................. 9 3.1.3. Overgrazing/Free grazing .......................................................................................................
    [Show full text]
  • Erosion & Sediment: ES-13
    ACTIVITY: Check Dams ES – 13 Targeted Constituents Significant Benefit Partial Benefit Low or Unknown Benefit Sediment Heavy Metals Floatable Materials Oxygen Demanding Substances Nutrients Toxic Materials Oil & Grease Bacteria & Viruses Construction Wastes Description Small temporary dams, constructed across a swale or drainage ditch, reduce the velocity of concentrated stormwater flows. This reduces erosion of the swale or ditch, and also promotes sedimentation behind the dam. Check dams are usually constructed from large rocks or stones, but other materials can also be used. This practice is likely to create a significant reduction in sediment. Suitable Temporary erosion and sediment control in small open channels that typically drain 5 Applications acres or less. During the establishment of permanent vegetation in drainage ditches or channels. On steep channels where stormwater runoff velocities must be reduced. Approach Check dams are used to prevent erosion by reducing the velocity of channel flow in small drainage channels and swales. Check dams control sediment by allowing sediment to settle out above the check dam, and by allowing stormwater to flow through a rock filter. Check dams are primarily used in small, steep channels where runoff velocities need to be reduced. Check dams must be sized and constructed correctly and maintained properly, in order to prevent material from washing out. Check dams are usually constructed from large aggregate or riprap. Other materials may be used, such as natural logs or sandbags filled with gravel, which can withstand the stormwater flow velocities and forces. Do not use creosote railroad ties or telephone poles. Check dams in drainage channels are not usually constructed from straw bales or silt fences, since concentrated flows quickly wash out these materials.
    [Show full text]
  • BMP 31.00 – 33.00. Temporary Check Dam
    BMP 31.00 – 33.00. Temporary Check Dam These instructions include BMP 31.00, 32.00, and • Check dams are used in narrow ditches. 33.00. • Steep channel slopes reduce effectiveness. DESIGN CONSIDERATIONS • Coupling check dams with a small adjacent upstream sump improves velocity slowing and Objectives sediment trapping ability. Temporary Check Dams are used to reduce scour, reduce velocity, dissipate energy, prevent erosion, • The area downstream from the last dam should and settle sediment behind the weir structure in an be stabilized or flow diverted. unlined channel or vegetative swale. • Check dam rocks interfere with the establishment of vegetation. Description A Temporary Check Dam can be constructed of a • Some Temporary Check Dams are left as a variety of materials and is placed perpendicular to permanent control measure. Removal may be flow in a ditch or channel. It is placed so that it indicated because of unsightliness or extends higher than the water level on both sides of interference with maintenance (grass mowing) the flow path and is lower in the center to allow activities. water to flow through a controlled path. Design Temporary Check Dams can be constructed from The design of Temporary Check Dams (high at angular rock, fiber rolls, prefabricated foam barriers, channel banks, lower in the middle) directs sandbags, or compost socks. When rock is used, overtopping flows centrally to avert scouring of small sediment particles become lodged in the check channel surfaces. The check dam is keyed into dam’s interior. channel slopes to prevent bank undercut and erosion. Other Names Check dam structures are sized to stay in place In-Stream/Channel Energy Dissipater, Velocity during peak flow.
    [Show full text]
  • A Case Study of Long-Term Field Performance of Check-Dams In
    Environ Geol (2009) 58:897–911 DOI 10.1007/s00254-008-1570-z ORIGINAL ARTICLE A case study of long-term field performance of check-dams in mitigation of soil erosion in Jiangjia stream, China Q. L. Zeng Æ Z. Q. Yue Æ Z. F. Yang Æ X. J. Zhang Received: 2 April 2008 / Accepted: 22 September 2008 / Published online: 16 October 2008 Ó Springer-Verlag 2008 Abstract This paper examines the long-term field perfor- erosion; and (d) vegetations on bank slopes. The field data mance of the check-dams in mitigation of soil erosion in the demonstrate that the check-dams have had the following Duozhao catchment of Jiangjia stream, southwest China. good functions for mitigation of soil erosion: (1) restricting Since their construction between 1979 and 1982, the check- the channel depth and lateral erosions, (2) protecting the dams have been functioning effectively. The examination is channel erosion base, (3) reducing the bed gradients of made via comparisons between the environmental condi- debris-flow channels, (4) fixing the channel bed, (5) stabi- tions of the Duozhao catchment with its adjacent Menqian lizing the bank slopes, as well as (6) facilitating the growth of catchment in the stream, because no check dams were con- vegetations. structed in the Menqian catchment. The examination is based on recent field investigations and aerial photograph analyses, Keywords Check-dam Á Debris flow Á Soil erosion Á and covers four aspects: (a) bed gradients of catchment Environmental management Á Jiangjia stream Á Case studies channels; (b) stability of bank slopes; (c) rates of land Introduction Electronic supplementary material The online version of this Soil erosion is a common natural phenomenon in moun- article (doi:10.1007/s00254-008-1570-z) contains supplementary tainous regions.
    [Show full text]
  • Appendix C Excerpt from MDOT Drainage Manual (Chapter 9
    Appendix C Excerpt from MDOT Drainage Manual (Chapter 9 Stormwater BMPs – Page 9-13 through 9-34 ) Michigan Department of Transportation C-1 7/1/02-6/30/03 Annual Report October 1, 2003 Stormwater Best Management Practices (BMPs) 9.4.2 MDOT-Approved BMPs The following two sections describe MDOT-approved BMPs. Section 9.4.2.1 lists approved BMPs in a table format, and Section 9.4.2.2 lists the BMPs in alphabetical order along with their definition and applications. 6.4.2.1 Summary List for BMP Selection Table 9-1 gives an alphabetized listing of BMPs, which can be used on MDOT projects. These BMPs are taken from the SESC Manual and the MDOT SWMP. BMPs which need more explanation than is provided in the SESC Manual are discussed in Section 9.4.2.2; otherwise, for design details, see the references given in Table 9-1. Copies of details identified can be found in the SESC Manual. Estimated costs are provided in Appendix 9-B. When selecting BMPs, use those given in Table 9-1. Additionally, there are some BMPs selection guidelines, listed below, which should always be used to help accomplish MDOT goals. 1. Preserve the natural drainage system. 2. Control source pollutants by: • Maximizing green space. • Protecting riparian buffer. • Stabilizing disturbed areas. • Identifying proper use of fertilizers and pesticides. • Identifying proper use of snow and ice control operations. 3. Evaluate site according to project delivery steps outlined in Section 9.4.1.2. 4. Use SESC details, outlined in the SESC Manual, for evaluation during construction.
    [Show full text]