Mechanisms and Measurement of Fluvial-Coal Transport Coal Mining and the Aquatic Environment Abingdon, VA, Sept. 6-7, 2007 John R. Gray

Slides:



Advertisements
Similar presentations
The concept of the WATER application was born from the need in Kentucky to quantify water availability in areas of the Commonwealth with limited long-term.
Advertisements

IMPROVING ESTIMATES OF SUSPENDED SEDIMENT CONCENTRATION AND FLUX IN THE LITTLE BEAR RIVER Brant Whiting, Jeffery S. Horsburgh and Amber S. Jones Utah Water.
Irene Seco Manuel Gómez Alma Schellart Simon Tait Erosion resistance and behaviour of highly organic in-sewer sediment 7th International Conference on.
U.S. Department of the Interior U.S. Geological Survey Welcome to the USGS Webinar: New Science and Online Management Tools to Help Guide Action on Nutrients.
BASIC FLUVIAL SEDIMENT CONCEPTS Introduction to Sediment Sampling USGS Technical training in Support of Native American Relations (TESNAR) 2011 Klamath,
Introduction to Sediment Sampling USGS Technical training in Support of Native American Relations (TESNAR) 2011 Klamath, Warm Springs, Yurok, and Karuk.
Sedimentary Petrology GEO 333 Lab (1) Introduction2009 Mansour Al-Hashim.
Entrainment and non-uniform transport of fine-sediment in coarse-bedded rivers Paul E. Grams & Peter R. Wilcock, Johns Hopkins University Stephen M. Wiele,
DRASTIc Groundwater Vulnerability map of Tennessee
Evaluation of Street Sweeping as a Water Quality Management Tool in Three Residential Basins in Madison, WI Bill Selbig USGS – WRD Middleton, WI Bill Selbig.
SPARROW Modeling in the Mississippi River Basin Iowa Science Assessment Davenport, IA Nov. 14, 2012 (608) By Dale M. Robertson*
15. Physics of Sediment Transport William Wilcock (based in part on lectures by Jeff Parsons) OCEAN/ESS
1D SEDIMENT TRANSPORT MORPHODYNAMICS with applications to RIVERS AND TURBIDITY CURRENTS © Gary Parker November, CHAPTER 13: THE QUASI-STEADY APPROXIMATION.
1D SEDIMENT TRANSPORT MORPHODYNAMICS with applications to RIVERS AND TURBIDITY CURRENTS © Gary Parker November, CHAPTER 12: BULK RELATIONS FOR TRANSPORT.
CLASS PLAN RIVER BEHAVIOR FLOW GAUGING MANNING’S EQUATION BANKFULL DISCHARGE DISCUSS MCPHEE.
1D SEDIMENT TRANSPORT MORPHODYNAMICS with applications to RIVERS AND TURBIDITY CURRENTS © Gary Parker November, CHAPTER 24: APPROXIMATE FORMULATION.
Lecture ERS 482/682 (Fall 2002) Erosion and sediment transport ERS 482/682 Small Watershed Hydrology.
Suspended Load Above certain critical shear stress conditions, sediment particles are maintained in suspension by the exchange of momentum from the fluid.
Hydrologic Issues in Mountaintop Mining Areas Ronald Evaldi, USGS-WSC, Charleston, WV Daniel Evans, USGS-WSC, Louisville, KY Hugh Bevans, USGS-WSC, Charleston,
Gold By: Mohammed.a Panning Panning – Was a simple technique used to find alluvial gold, which was small nuggets of gold that were found in creek beds.
Using field exercises to develop critical thinking skills in hydrology students Eric W. Peterson Department of Geography-Geology.
Sediment transport in wadi systems
What Does It All Mean Siletz River near Siletz, OR May 20-23, 2013.
SAMPLING TECHNIQUES FOR SUSPENDED SEDIMENT Introduction to Sediment Sampling USGS Technical training in Support of Native American Relations (TESNAR) 2013.
APPLICATION OF THE FAST THEORY TO THE SEDIMENTOLOGY OF THE PAWMPAWM RIVER, GHANA Divine Odame Appiah, Dept. of Geography and Rural Dev’t, KNUST, Kumasi.
Garey A. Fox, Ph.D., P.E., Derek M. Heeren, Michael A. Kizer, Ph.D. Oklahoma State University Evaluation of Alluvial Well Depletion Analytical Solutions.
Reynolds Number (Re) Re = R = A/P V = mean velocity  /  =  (which is kinematic viscosity) Re = VR(  /  ), where Driving Forces Resisting Force Re.
Regional/National Sediment Yields: Application of Fundamental Fluvial Geomorphic Techniques for TMDLs National Sedimentation Laboratory Andrew Simon USDA-ARS.
Fluvial Processes “the great sculptor of the landscape”
Stream Stability and Sediment Transport Environmental Hydrology Lecture 21.
Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,
Collaborative Monitoring in the Great Lakes: Revisiting the Lake Michigan Mass Balance Project Collaborative Monitoring in the Great Lakes: Revisiting.
John Hoffmann Introduction to USGS Arizona Program and Hydrology USGSGeologyMappingBiologyWater Water-Science Centers.
A Limnological Assessment: The Lucas Pond Christian Brown Dylan Gollen Taylor Lasley John Novak.
Sediment Transport over Ripples and Dunes Stephen R McLean, UC Santa Barbara Jonathan Nelson, USGS, Denver, CO Thanks to: Sandro Orlandi, University of.
U.S. Department of the Interior U.S. Geological Survey The Mississippi River Sediment and QW Data Information Network Phil Turnipseed, PE for John R. Gray.
Update on IMPROVE Light Extinction Equation and Natural Conditions Estimates Tom Moore, WRAP Technical Coordinator May 23, 2006.
Basic Hydrology Water Quality: Sediment production and transport.
U.S. Department of the Interior U.S. Geological Survey Water-Quality Monitoring: Data Collection and Analysis Strategies for Designing Program.
Modelisation of suspended sediment transport in rivers Master thesis Véronique Briguet 2011 Alain Recking, Oldrich Navratil, Nicolle Mathys.
Sediment Yield and Channel Processes. Definitions Suspend Sediment – sediment (orgranic or inorganic) which remains in suspension in water for a considerable.
Bedload-transport measurements with geophones
U.S. Department of the Interior U.S. Geological Survey Determination of Daily Sediment, Nutrient, and Sediment-Associated Chemical Concentrations and Loads.
EFFECT OF ORGANIC MATTER ON WAVE- INDUCED RESUSPENSION OF FINE SEDIMENT.
Flow Energy PE + KE = constant between any two points  PE (loss) =  KE (gain) Rivers are non-conservative; some energy is lost from the system and can.
Sediment transport Part 2: transport rate GEOL/CE/EEB 8601 Intro to Stream Restoration.
 Not all channels are formed in sediment and not all rivers transport sediment. Some have been carved into bedrock, usually in headwater reaches of streams.
Water Movement Below Surface
Gary R. Wall and Timothy F. Hoffman U.S. Geological Survey
Regional Integrated Science Projects - Opequon Creek/Shenandoah River Basins Agencies Involved – USGS Water, Geology, GIO/ Geography, and Biology Disciplines,
15. Physics of Sediment Transport William Wilcock (based in part on lectures by Jeff Parsons) OCEAN/ESS 410.
Estimating the Volume of Fine-Grained Sediments Behind Four Low-Head Dams, Kalamazoo River, Michigan. In cooperation with the Michigan Department of Environmental.
Intro to Geomorphology (Geos 450/550) Lecture 7: channel geometry and sediment transport power laws in channel geometry bed load sediment transport Rouse.
SPARROW: A Model Designed for Use With Monitoring Networks Richard A. Smith, Gregory E. Schwarz, and Richard B. Alexander US Geological Survey, Reston,
A river flowing between banks composed of coarse material with numerous protrusions and over a bed of large, angular rocks meets with more resistance than.
USGS ACTIVITY: Estimating suspended-sediment load continuously for 2 years using turbidity *, hydroacoustic, and LISST instruments, all proxy technologies.
SUBCOMMITTEE ON SEDIMENTATION Proposal to become a subgroup under the ACWI September 9, 2003.
Sedimentology Lecture #6 Class Exercise The Fenton River Exercise.
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.
Water-quality trends for selected sites at and near the Idaho National Laboratory, Idaho Roy Bartholomay USGS INL Project Office
U.S. Department of the Interior U.S. Geological Survey Proposed National Sediment and Water-Quality Monitoring Program Piloted in the Mississippi River.
Bedload transport Jens Turowski, WSL Bedload transport Lecture for Hydrological Processes and Modelling 24th June 2011 Jens M. Turowski, Swiss Federal.
Sedimentology Assessment 1 Due: Tuesday Feb 1, at midnight (Use your lecture slides and the text book) Instructions: Use text boxes to place your answers.
1 Hydroacoustic Sediment Surrogates and Methods —test results for a small urban river— Mark N Landers, Federal Interagency Sedimentation.
Redahegn Sileshi1, Robert Pitt2 , and Shirley Clark3
Exercise 1: Fenton River Floodplain Exercise
Suction Dredging Introduction
OCEAN/ESS Physics of Sediment Transport William Wilcock (based in part on lectures by Jeff Parsons)
Sediment Guidance Workgroup
Presentation transcript:

Mechanisms and Measurement of Fluvial-Coal Transport Coal Mining and the Aquatic Environment Abingdon, VA, Sept. 6-7, 2007 John R. Gray USGS Office of Surface Water Reston, Virginia

COAL MINING & THE AQUATIC ENVIRONMENT ?Fluvial Coal Transport/Fate? “Coal…is observed in the riverbed for months…but seems to disappear for a long time” “How and where coal moves in river systems?” “How to know where coal moves?” (Braven Beaty, 5/2007 )

Overview of mechanisms, fluvial-sediment transport Coal movement and storage in streams as a special case of fluvial-sediment transport Suspended-sediment and bedload measurement – equipment and techniques USGS-BLM Coal-Hydrology Program, COAL MINING & THE AQUATIC ENVIRONMENT Ergo, My Overview:

NICKEL PRIMER ON FLUVIAL SEDIMENTOLOGY

Density (mass per unit volume). –wood <1 –water 1.0 (pure, 4° C) –coal (~1.3, eastern U.S. coal – W. Orem) –quartz & feldspar ~2.65 (prevalent minerals in nature) –iron 7.9 –lead11.4 –mercury13.5 –gold19.3 PHYSICAL CHARACTERISTICS OF SEDIMENT

Categories of Sediment Transport

0.062 mm2 mm0.002 mm SandsSilts Clays

C mean = ~930 mg/l BC=1.03 BC=~1 Box Coefficient (BC) = C mean /C point BC=~1.1 Culbertson et al., 1964

C mean = ~1,360 mg/l BC=~1.7 Box Coefficient (BC) = C mean /C point BC=~5 BC=~4 BC=~1.5 Mean Values Culbertson et al., 1964

Measuring Coal Transport Using FISP Sediment Samplers ► Suspended Sediment: - Isokinetic samplers deployed by flow-weighting techniques of the Federal Interagency Sedimentation Project - Pumping samplers - Turbidity and other surrogate techniques might work*. ► Bedload: US BLH-84 or US BL-84 bedload samplers deployed by Equal-Width or Unequal-Width Techniques ► Bottom Material: US BM or US BMH bottom-material samplers, or if material larger than medium gravel, Cooper Scooper, pipe dredge, or another ‘bulk-sampling’ technique

Sampled & Unsampled Zones with an Isokinetic Sampler

FISPFISP TM US D-74

FISPFISPTM US D-96

US BL-84FISPFISPTM

U.S. BMH-80

U.S. BM-54

(Singer, Cepello, Henderson, 2006, 8FISC, p 328) The Cooper Scooper 36 x 23 x 28 cm 16 kg dry weight Contact Michael Singer,

(Singer, Cepello, Henderson, 2006, 8FISC, p 328) The Cooper Scooper

Analyzing Coal Samples ►USGS Kentucky Science Center Sediment Laboratory Libby Shreve Chief Standard sediment-lab services, plus - % coal in bed material, loss-on-ignition ►See next plot from Bill Orem, USGS, on % organics in bed material of eastern coal region rivers.

Coal Mussel Study TN/VA/WV Rivers From Bill Orem, USGS, on % organics in bed material of eastern coal region rivers. Mean value excluding 14.8% outlier

Predicting Coal Transport ► For bedload, empirical equations such as Meyer-Peter Mueller, Smith-Wiberg, Yalin, Parker, etc. work. Requires sediment density -- OK ►For suspended load, coal-settling velocity must be known. That can be derived for eastern coal -- OK ►Both cases, the size distribution of coal bed material must be known. USGS Louisville, Kentucky, Laboratory performs such analyses -- OK “If gravel-size material, should be pretty easy to predict mobility using USGS_MD SWMS Interface – J. Nelson, USGS, Golden, CO”

USGS-BLM Coal-Hydrology Program, ►Collect information and study hydrologic processes related to development and mining of coal. ►More than 500 reports produced. ►West Virginia: “A mined basin sediment yield was 240X > unmined (Parker, PP 1464, p. 157). Statistics also for VA, TN, KY that show as mined area increases, sediment yields increase.

USGS-BLM Coal-Hydrology Program,

Parker, USGS Professional Paper 1464, p. 159

COAL MINING & THE AQUATIC ENVIRONMENT Good News!: Measuring and estimating coal transport Wealth of historical information from the USGS-BLM Coal-Hydrology Program that might be ‘mined’ before considering more data collection. Wealth of capabilities for monitoring sediment transport; specific coal-monitoring protocols needed. Modeling capabilities appear to be up-to-the-task. Thanks for loaning me your ears and eyes…

The END?