Site Selection and Security Considerations Mark Heggli Innovative Hydrology, Inc. Consultant To The World Bank Expert Real-Time Hydrology Information Systems.

Slides:



Advertisements
Similar presentations
Safety Absolutes Green Lake
Advertisements

WATER QUALITY ANALYSIS for ANTIDEGRADATION
HYDROMETRIC SITE SELECTION Training for PNG Power Port Moresby July 2012.
Application of the Continuous Slope-Area Method for Determining Stream Discharge and Development of Rating Curves in Ephemeral Channels Navajo Nation Hydroclimate.
A section has been added regarding Stream Restoration Design Criteria: A. Designs for stream restoration try to mimic natural conditions present in stable.
Mark Heggli Consultant to the World Bank Expert Real-time Hydrology Information Systems Workshop Module 4: Data Management Solutions for a Modernized HIS.
Weirs and Canal Intakes By: Nell Kolden and Taylor Barnett Thursday April 12, 2012 CIVE 717.
COURSE COORDINATOR: DR. J. O. ADEJUWON OFFICE LOCATION: ROOM B203, COLERM BUILDING OTHER LECTURERS: DR. GRACE O. OLUWASANYA.
CHAPTER FOUR Stream flow measurement
Streamflow and Runoff The character, amount, and timing of discharge from a basin tells a lot about flow paths within the basin Therefore, important to.
Detention / Infiltration Structure. Figure 21–1 Point Discharge and Downstream Stability Analysis Procedure.
Hydroelectric Relicensing in Vermont Brian Fitzgerald Vermont Agency of Natural Resources.
River Studies. Outline of Events During your river field work you will be visiting two different sites in the lower course of the river. At each site.
6.13 Design experiences in Tigray:
Subwatershed Outlet (B1 project area) Hydrological Monitoring Institutional strengthening The newly established Tana Basin Organisation have been trained.
Hydrological Information System Module 20 – Integrated Reservoir Monitoring System.
RQ30 RADAR SYSTEM (An Australian Perspective) RQ30 RADAR SYSTEM (An Australian Perspective) Malaysia JPS Offices Ampang, Kuala Lumpur 8 th May 2012.
Koktuli River Instream Flow Reservation Cathy Flanagan Bristol Bay Native Association.
How do we measure how much water is in a stream?
FLOODS, STREAMS AND MEANDERS. GAUGING STATION On all major streams Measures Stream Height Height vs. Discharge (volume) Flood Stage and height above Flood.
HEC-RAS US Army Corps of Engineers Hydrologic Engineering Center
Stage – Discharge Rating Numerical relationship between water elevation (stage) and discharge at a location in a flowing system. Expressed as an equation,
Part 2 Some Basic Aspects of CHANNEL HYDRAULICS. The volume of water that passes by any given point along a watercourse is called “Q”, for quantity of.
Discharge Measurement Concepts September 2011 – Glen Hess,TESNAR, Oregon (Many slides from USGS Surface Water Field Techniques May 2008 Class)
Hydrology and Water Resources RG744 Institute of Space Technology December 11, 2013.
Discharge Measurement Concepts September 2012 – Glen Hess,TESNAR, Oregon (Many slides from USGS Surface Water Field Techniques May 2008 Class)
1 Toggle Fullscreen mode with this button above Audio also available via phone: For assistance, call: If.
Abstract Background Conclusion Stream Bed Morphology and Discharge Rates of Deckers Creek Data was collected at 5 different points along a 100 meter transect.
Hydraulic Engineering
Final Presentation UNSA, Nice HydroEurope 05 th March, 2010.
Site Selection and Security Considerations Mark Heggli Innovative Hydrology, Inc. Consultant To The World Bank Expert Real-Time Hydrology Information Systems.
Workshop Mark Heggli Consultant to the World Bank Expert Real-time Hydrology Information Systems Module 11: Managing HIS During Warranty Period.
Workshop Mark Heggli Consultant to the World Bank Expert Real-time Hydrology Information Systems Module 6: Operations & Maintenance and Training.
Workshop Mark Heggli Innovative Hydrology, Inc. Consultant to the World Bank Expert Real-time Hydrology Information Systems Module 6: Training, Operations.
Mark Heggli Innovative Hydrology, Inc. Consultant to the World Bank Expert Real-time Hydrological Technology Module 1: Essential Elements of a Hydrological.
WORKSHOP Mark Heggli Innovative Hydrology, Inc. Consultant to the World Bank Expert Real-time Hydrology Information Systems Module 9: Equipment Delivery.
Urban Storm Drain Design: Pump Station Design. Purposes To lift stormwater to higher elevation when discharge of local collection system lies below regional.
INTRODUCTION Mark Heggli, Meteorologist/Hydrologist Expert Real-time Hydrology Information Systems Innovative Hydrology, Inc. Consultant to the World Bank.
Corby Weir Investigation Project. Corby Weir Investigations and significant events Background and History - Weir construction and Purpose Concerns raised.
Prepared by: Burnham – Floodplain Study October 23, 2009 Presented by: Marty Spongberg, PhD, PE, PG AMEC Geomatrix, Inc.
March 2003HEC-RAS Version 3.1 Other Features of HEC-RAS- part 2 Cross Section Interpolation Multiple Plans Supporting Pictures.
Measuring velocity profiles above different substrates on the Glinščica stream Maja Koprivšek 1, Mitja Brilly 1, Mihael Jožef Toman 2 1 University of Ljubljana,
7. Bedforms in coarse-grained channels Step-pool units Cluster bedforms Riffle-pool sequences.
Stream Classification. What factors affect stream morphology? Width Depth Slope Velocity Discharge Flow resistance Sediment size Sediment load Leopold.
Why use Index-Velocity Methods? Traditional Sites – Stage vs Discharge is predictable.
6.12a DESIGN APPROACH ON BILILO SPATE IRRIGATION PROJECT Presented by Eyob Yehayis.
Lesson Understanding Soil Drainage Systems. Interest Approach Ask students the question, “What determines how fast water will flow through a funnel?”
13. Sediment and aquatic habitat in rivers (a)Benthic organisms and bed sediments (b)Fish and bed sediments (c)Reach classification based on bed material.
Basic Hydraulics: Rating curve. Definition & terminology Rating curve, also known as stage–discharge curve, is a graph showing the relation between the.
Hydrology and Water Resources RG744 Institute of Space Technology November 13, 2015.
Think about answering the questions: Who? What? Where? When? Why? How? Before your volunteers begin collecting data.
permitting.
Habitat suitability and availability for rainbow trout Oncorhynchus mykiss in the Canyon Reservoir tailrace Greg Cummings.
Mark Heggli Innovative Hydrology, Inc. Consultant to the World Bank Expert Real-time Hydrology Information Systems Module 12: Assuming Management of an.
What is the Bradshaw model?
Bridges Reach analysis Fundamental tool for design
Presented by Harry C. Elinsky, Jr. Filtech, Inc.
Basic Hydrology & Hydraulics: DES 601
Hydrological Information System
6.1 BASIC ENGINEERING New ‘modernised’ diversion structures have promoted larger inequity in the distribution of irrigation water between upstream and.
Integrated River Basin Management Tools and methods for IRBM Monitoring, Acquisition and processing of Water Resource Data.
HP-II Workshop on Real-time Hydrological Information Systems
Streams Hydrodynamics
CLASS PLAN RIVER BEHAVIOR FLOW GAUGING MANNING’S EQUATION
REGULATION WORK UNIT – 10 LECTURER IN CIVIL ENGG. GP MEHAM SANDEEP.
Longitudinal Profile Survey for Successful Culvert Replacement
Scour Analysis on the west fork of the Duchesne River
In-Stream Structures & Grade Control
Introduction: Real-time Hydrology Information System
Introduction: Real-time Hydrology Information System
Presentation transcript:

Site Selection and Security Considerations Mark Heggli Innovative Hydrology, Inc. Consultant To The World Bank Expert Real-Time Hydrology Information Systems

Examples that refer to products are intended for illustrative purposes only, and do not imply an endorsement or recommendation of any particular product

Site Selection and Security Consideration  Site selection Define the Site Purpose Site Survey/ Field Visit  Security considerations for all sites

Site Selection: Define The Site Purpose  Establish the purpose of the site What are you trying to measure? ○ Water Level ○ Discharge ○ Water Temperature ○ Water Quality ○ Rainfall ○ Other How crucial is the data? ○ Logging needs ○ Frequency of Data Collection  Consideration of future needs Additional sensors, additional telemetry

Site Selection: Site Survey/Field Visit  Why is it important to complete a site survey? Ease and safe accessibility Understand the characteristics of the area being measured ○ Understanding the characteristics will help in the decision making of proper equipment to make accurate measurements ○ A mismatch between local conditions and appropriate technology can result in: Poor quality of data High maintenance requirements for both field and office procedures

Site Survey/Field Visit: Accessibility and Safety  Safe access to site Road to Drive Walking Path Boat Aircraft  Minimization of risk during install, ongoing operation and maintenance Personnel, sub-contractors, public

Site Survey/Field Visit: Water Level and Discharge Sites  Stream characteristics Control Upstream and downstream considerations Contained and subterranean flow Streambed and banks Gauging sections

Stream Characteristics: Control  What is a control? Control needs to be stable and sensitive Minimum change in discharge with minimum change in stage Cease to flow point should not be affected by sedimentation or weed growth Try to find a site with an existing natural control  Types of Control Natural control Man made control

Stream Characteristics: Upstream and Downstream Considerations  Straight section of stream According to the WMO, the general course of the stream is straight for about 10 times the stream width, upstream and downstream from the gauge site if the control is a river reach (channel control). Approach velocities are evenly distributed Minimize possibility of sedimentation fill  Downstream Effects Evaluate downstream effects ( tidal effects, water shortages, future civil works/dams)

Stream Characteristics: Contained and Subterranean Flow  Contained Flow Section needs to contain all flow including maximum flood flow No possibility of over bank or side channel flow  Subterranean Flow Evaluation should include possibility of subterranean upstream, causing bypassing of flow (prevalent in underground mining areas)

Stream Characteristics: Stable Stream Bed and Banks  Stable Stream Bed Minimal infill or scour  Stable Stream Banks Avoid locations with bank scour or erosion

Stream Characteristics: Gauging Sections  Gauging Sections Feasibility ○ Low flow wading ○ Boat measurement ○ Unmanned cableways

Rainfall Site Selection  Obstruction  Wind  Slopes  Height of gauge Wind velocities increase with height High enough to prevent splashing from the ground 1 m is standard according to WMO

Site Selection: Location of Instrumentation  Power AC DC- Generator or Battery Solar needs a clear access to sunlight  Telemetry Landline GPRS/GSM Coverage Radio Link Satellite Access  Housing of Equipment Location of instrumentation must be above maximum flood

Security Considerations  All Sites Locks Fencing Disguise

Suggestions  Rarely will an ideal site be found for a gauging station and judgment must be exercised in choosing between adequate sites, each of which may have some shortcomings  Often adverse conditions may exist at all possible sites for installing a required gauging station and a poor site must be accepted. For example, all streams in a given region may have unstable beds and banks, which result in continually changing stage- discharge relations.

QUIZ

Thank You  WMO Site Selection 1044 Volume 1  The ideal gauge site satisfies the following criteria, many of which are defined in ISO : (a) The general course of the stream is straight for about 10 times the stream width, upstream and downstream from the gauge site if the control is a river reach (channel control). If the control is a section control, the downstream conditions must be such that the control is not drowned. The water entering a section control should have low velocity (see (f) below); (b) The total flow is confined to one channel at all stages and no flow bypasses the site as subsurface flow; (c) The stream-bed is not subject to scour and fill and is relatively free of aquatic vegetation; (d) Banks are permanent, high enough to contain floods, and are free of brush; (e) Unchanging natural controls are present in the form of a bedrock outcrop or other stable riffle for low flow and a channel constriction for high flow – or a waterfall or cascade that is unsubmerged at all stages. If a natural control is not available, then channel conditions should allow for the construction of an artificial control such as a weir or flume (see Chapter 3); (f) A pool is present upstream from the control at extremely low stages to ensure a recording of stage at extremely low flow, and to avoid high velocities at the streamward end of stage recorder intakes, transducers, or manometer orifice during periods of high flow. The sensitivity of the control should be such that any significant change in discharge shall result in a measurable change in stage; (g) The gauge site is far enough upstream from the confluence with another stream or from tidal effect to avoid any variable influence the other stream or the tide may have on the stage at the gauge site; (h) A satisfactory reach for measuring discharge at all stages is available within reasonable proximity of the gauge site. It is not necessary for low and high flows to be measured at the same stream cross-section; (i) The site is readily accessible for ease in installation and operation of the gauging station; (j) Within reach of a suitable telemetry system; (k) Good conditions for discharge measurements at all stages; (l) Instruments, shelter, and housing above all flood levels. Sensors with a range to measure floods and drought.  Rarely will an ideal site be found for a gauging station and judgment must be exercised in choosing between adequate sites, each of which may have some shortcomings. Often adverse conditions may exist at all possible sites for installing a required gauging station and a poor site must be accepted. For example, all streams in a given region may have unstable beds and banks, which result in continually changing stage-discharge relations.