CLASS PLAN RIVER BEHAVIOR FLOW GAUGING MANNING’S EQUATION BANKFULL DISCHARGE DISCUSS MCPHEE.

Slides:



Advertisements
Similar presentations
9: Running Water Basins: land area that contributes water to a river system Divide: separates different drainage basins Ex. Drainage basin of Mississippi.
Advertisements

Characteristics of High Gradient Streams
Module 1 : The Fluvial Environment Fluvial: Relating to or occurring in a river.
River Systems - Runoff.
Exploring Geology Chapter 16 Rivers and Streams
Rivers. Where Do Rivers Get Their Water? 466 Drainage Basin – provides water for the river. Drainage Basin – provides water for the river.
FLOODS, STREAMS AND MEANDERS. GAUGING STATION On all major streams Measures Stream Height Height vs. Discharge (volume) Flood Stage and height above Flood.
Fluxes of water, sediment, and elements class 1.Introduce instrumentation and approach for surveying and flow gauging 2.Introduce and understand Manning’s.
Chapter 6.2 The Work of Streams.
Sculpting Earth’s Surface
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.
River morphology and process class 1.consider physics of flow and erosion 2.review river taxonomy 3.examine the germane processes that control the shape.
FIELD METHODS IN ENVIRONMENTAL GEOLOGY GEOS 3110.
Water Cycle - Running Water
Chapter 13 Surface Water.
Reynolds Number (Re) Re = R = A/P V = mean velocity  /  =  (which is kinematic viscosity) Re = VR(  /  ), where Driving Forces Resisting Force Re.
Fluvial processes As with most geomorphic processes, Rivers operate as a function of a dynamic equilibrium between - Driving forces and Resisting forces.
Fluvial Processes “the great sculptor of the landscape”
Streams Objectives: 1.Definition 2.Importance 3.Hydrologic Cycle 4.Geometry and Dynamics.
Unit 4: Gradational Processes Ms. Thind
Chapter 16: Running Water. Hydrologic cycle The hydrologic cycle is a summary of the circulation of Earth’s water supply Processes involved in the hydrologic.
Oregon Case Studies Ryan Johnson. Studies  The response of impounded sediment to a culvert replacement project on Sutter Creek, a tributary of Honey.
Sediment Yield and Channel Processes. Definitions Suspend Sediment – sediment (orgranic or inorganic) which remains in suspension in water for a considerable.
THE HYDROLOGIC CYCLE. The Hydrologic Cycle The Hydrologic Cycle - Fresh Water Storage Reservoir % of Total Fresh Water Glaciers (Frozen)76% Groundwater22%
Streams (Rivers). Runoff: H 2 0 that does not sink into ground Most ends up in streams.
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.
Rivers: Fluvial Processes
Surface Water Chapter 9 Notes.
Stream Erosion and Transport
The hydrologic cycle. Running water Streamflow Two types of flow determined primarily by velocity –Laminar flow –Turbulent flow Factors that determine.
River Systems. I. Water Distribution 1.36 billion cubic km of water 97.2%oceans 2.15% glacial ice 0.65% lakes, streams, ground water.
Rivers and Streams. What is the continental divide?
 These two agents: erosion and deposition are the most important agents that affect weathered materials.  Erosion involves the physical removal of weathered.
Percolation Condensation Solar radiation Evaporation Sea Salt water Ground water Precipitation Transpiration Runoff in streams Copyright: McGraw-Hill.
Less than.01% of Earth’s water is contained in rivers and lakes Streams begin as runoff Waters flows downhill because of gravity The steepness of the.
Rivers and Streams. River Systems A river or stream: any body of water flowing downhill in a well defined channel A river or stream: any body of water.
Section 3: Stream Deposition
River Terminology 10/17/00. Erosion The break up and transport of earth materials by moving natural agents. Natural agents: Glaciers, Wind and Moving.
Surface and Ground water Chapter 11. Hydrologic Cycle.
How Streams Transport Material 13.2 Stream Erosion & Deposition.
7. Bedforms in coarse-grained channels Step-pool units Cluster bedforms Riffle-pool sequences.
Sediment Transport Stream Capacity - The capacity of a stream or river is the total amount of sediment a stream is able to transport comprised of three.
(,rivers, brooks, creeks, etc.)
Journal #4 Why are river system constantly changing? The narrow depression that a stream follows downhill is called its _________. What causes the formation.
Aims today: To learn about: Channel Efficiency The Hydraulic Radius
1D Hydraulic Modeling w/ LiDAR Data Noah J. Finnegan 1 1 UC Santa Cruz, Earth & Planetary Sciences.
River Systems Section 2 Section 2: Stream Erosion Preview Key Ideas Parts of a River System Channel Erosion Development of River Channels Tributary, River.
River systems. Runoff vs. Infiltration Factors determining runoff, or infiltration 1.Soil composition & pore space Coarse-grains & lots of humus = good.
Stream Erosion & Deposition Chapter 6 sections 1 and 2.
TRANSPORTATION & DEPOSITION in a Stream System.
What is the Bradshaw model?
Interactions class Getting and understanding watershed flux data
“the great sculptor of the landscape”
Expression Session Summarise “stream discharge” and “river load” using diagrams to assist your answer.
4 channel types defined at reach scale, based on 3 features
Rivers.
Warm-up What are four things that impact INFILTRATION? (the answer is in your notes) After you finish the warm-up put your river basin project in the inbox.
Chapter 13 Surface Water.
DO NOW Pick up notes and Review #30. Have your turned your lab in?
4 channel types defined at reach scale, based on 3 features
River System Development
Streams and Rivers Video: Grand Canyon.
Summary In addition to the oceans, where else is water found on Earth?
The Work of Streams.
Discharge, stream flow & channel shape
15-3 Stream Deposition.
Stream Erosion.
CLASS PLAN RIVER BEHAVIOR FLOW GAUGING MANNING’S EQUATION
The Flow of Freshwater.
Journal #6 What is a stream gradient?
Presentation transcript:

CLASS PLAN RIVER BEHAVIOR FLOW GAUGING MANNING’S EQUATION BANKFULL DISCHARGE DISCUSS MCPHEE

RIVERS On Huntington, in water Warm clothes, food, $, Daily Bread Measure discharge - survey and velocity Trace flow Compare pools and riffles Field estimate of bankfull stage

Idealized flow patterns Alluvial, meandering river Dye tracing

Channel Mobility Watts Branch, MD

Downstream Organization Survey one of each type Calculate discharge for one of each type COMPARE

FLOW GAUGING QUANTIFY VOLUME OF WATER MOVING THROUGH CHANNEL NEED CHANNEL GEOMETRY NEED VELOCITY

Distance Velocity Water Depth Survey Across Stream

Flow meter for measuring water speed

Divide and Conquer

Add up the pieces

From counts to speed

Manning Equation

SLOPE

Wetted Perimeter

Flow Levels Bank full flow About once a year Try to define in field using observations

Extreme Floods How does the Huntington Fit?

DEFINE BASIN AREA COUNT BOXES OR USE DIGITIZER

Sediment Transport Through Rivers Bedload -- material moving along the bed, shear forces exerted by water sufficient to move clasts Suspended Load -- material kept in the water column by turbulence and lift forces Bedload usually <<< than suspended load and ignored Dissolved Load -- material kept in the water column by turbulence and lift forces Dissolved load varies, usually <<< than suspended load

Sampling for suspended load…….

Mass Loadings and Erosion Rate Estimation Integrate suspended load over all flows (mass/time) Integrate bedload load over all flows (mass/time) Integrate dissolved load over all flows (mass/time) + +

Integration over all flows is a non trivial problem! Need Rating Curves (suspended, dissolved, bedload)

Other Approaches…Reservoir trapping Nahal Yael, Negev Desert

SEDIMENT YIELD - What comes out SEDIMENT GENERATION - Material generated by erosion = or ≠ Timescale Steady state Human impact Episodic disturbance

1. Describe the Atchafalaya River 2. What is the geologic origin of southern Louisiana? 3. What is "capture"? 4. What is and how does the "hold by levee" philosophy work? Is this philosophy still followed today? John McPhee -- Control of Nature