Water Testing Project for the North Fork River

Slides:



Advertisements
Similar presentations
Erosion and Deposition
Advertisements

Riparian Zone Habitat Assessment Vegetation and More.
Aquatic Entomology ZOOL 484/584 Policies Course outline - website.
I.Running water: 1.Erosion: a. most erosion on earth is due to running water (streams and rivers). Image from
Objectives Describe how surface water can move weathered materials.
Watershed System Physical Properties Stream flow (cfs) Stream Channel Pattern Substrate Chemical Properties pH Dissolved Oxygen Temperature Nutrients Turbidity.
Bioassessment 1.0. Stream Visual Assessment Protocol 1. Turbidity 2. Plant growth 3. Channel Condition 4. Channel Flow Alteration 5. Percent Embeddedness.
“Habitat Assessment Using the QHEI “ Edward T. Rankin June 6 City of Columbus, Level 3 Training Course Columbus, Ohio Senior ResearchScientist
Rivers and streams A river and stream can be defined as. a natural stream of water that flows through land and empties into a body of water such as an.
Fundamentals of River Restoration and Salmonid Fisheries OWEB, 1999, Fundamentals of River Restoration and Salmonid Fisheries OWEB, 1999, Fundamentals.
STREAM ECOLOGY By Maggie Bell-McKinnon, biologist Washington Department of Ecology
Water Cycle - Running Water
Chapter 13 Surface Water.
Review Vocab: Aquatic Environments 4-1. a slow-moving body of water where the water seems to stand still; lakes, ponds; and wetlands lentic.
STREAM ECOSYSTEMS.
Materials Transport & NSCD Material Classes Velocity to Transport Relationships York NSCD Restoration PSY CCREP.
Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,
Natural Riparian Resources Water Landscape & SoilVegetation.
Aquatic Science Lotic Ecosystems.
Surface Water Chapter 9 Notes.
Flowing water.  vitally important geologically, biologically, historically and culturally.  contain only 0.001% of the total amount of the worlds water.
Section 13.1 Streams and Rivers
Stream Erosion and Transport
A stream is a body of water that carries rock particles and dissolved ions and flows down slope along a clearly defined path, called a channel. Thus, streams.
Water Quality and Water Testing. Studies of streams may involve the following measurements and analysis 1.Physical Parameters of the Stream 2.Biological.
Lec 11: Stream Ecology- Abiotic Features Lentic-Lotic Comparisons -Major influences & processes Hydrology, Morphology, & Discharge Human Alterations.
EROSION- The transport of weathered materials…. Major Erosive Agents: Running Water GLACIERS WIND OCEAN CURRENTS AND WAVES MASS WASTING (GRAVITY!)
13.1 Streams and Rivers Key Idea:
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.
River Systems. Objective  Students will describe factors that affect the erosive ability of a river and the evolution of a river system.
Streams and Rivers.
Watersheds This is an area where rain joins together to flow into streams, rivers, lakes, or wetlands. This is the drainage basin. The watershed boundary.
Journal #4 Why are river system constantly changing? The narrow depression that a stream follows downhill is called its _________. What causes the formation.
River Systems Section 2 Section 2: Stream Erosion Preview Key Ideas Parts of a River System Channel Erosion Development of River Channels Tributary, River.
Chapter 2: The Flow of Freshwater. Draw the water cycle diagram in your daybook and label it in your own words. p.41 in your text.
TRANSPORTATION & DEPOSITION in a Stream System.
Stream Ecology.
Fundamentals of River Restoration and Salmonid Fisheries OWEB, 1999, Fundamentals of River Restoration and Salmonid Fisheries Dylan Castle.
River Vocabulary Science 1.
Surface Water.
Erosion and Deposition
STREAMS & RIVERS Chapter 6 1.
Which Way to the Sea?.
Physical Characteristics of streams
Fluvial Geomorphology
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.
Surface Water. Surface Water Surface water notes: Where is all the water? 97.5% in Oceans 1.8 % in Ice .63% in groundwater .007% in salty lakes and.
Chapter 13 Surface Water.
DO NOW Pick up notes and Review #30. Have your turned your lab in?
by Maddie, Ty, McKinley, and Garrett
Erosional/Depositional Systems
Chapter 6.1 Running Water.
SOL 6.7 Ecosystems.
Chapter 13 Notes.
Stream Order & Watersheds
Stream Erosion.
Surface Water Chapter 9.
stream, river, lake, wetland, or ocean
Streams Hydrodynamics
Rivers & Watersheds.
Streams Hydrodynamics
Surface Water. Surface Water Surface water notes: Where is all the water? 97.5% in Oceans 1.8 % in Ice .63% in groundwater .007% in salty lakes and.
Surface Water. Surface Water Surface water notes: Where is all the water? 97.5% in Oceans 1.8 % in Ice .63% in groundwater .007% in salty lakes and.
Rivers and Streams Chapter 6.1 and 6.2.
The Flow of Freshwater.
The Flow of Water.
River Systems Chapter 15.
Rivers & Watersheds.
Stages in the Development of a River Valley
Presentation transcript:

Water Testing Project for the North Fork River Watershed System Physical Properties Stream flow (cfs) Stream Channel Pattern Substrate Chemical Properties pH Dissolved Oxygen Temperature Nutrients Turbidity Biological Properties Riparian Zones Macroinvertebrates Water testing day is FridayMay 11th at the North Arm Trailhead.

Physical Properties of a Watershed System Stream Shape Stream Flow

Stream Flow The amount of water that flows past a specific point in a stream over a period of time.

Natural Influences that affect Stream Flow Climate Season Watershed Meandering Substrate Groundwater Vegetation

Human influences affecting stream flow Dams Channelization Land use

Why do we care about Stream Flow? Water quality : affects turbidity (sediment load) and dissolved oxygen Aquatic life : creates different habitats for fish and bugs Vegetation: needs overbank flooding for nutrients Flooding: controlled for human structures Water storage: determines how and when water should be stored

Method to measure & calculate stream flow 1. Measure a 10 m section and mark it with rocks. 2. Throw a stick in above this section and use a stop watch to measure the time it takes the stick to travel the 10 m section 3 separate times. Average the times. 3. Divide the distance (m) by average time (s) to get the velocity (m/s). 4. Measure the depth (m) & width(m) to find an area (m2). 5. Stream flow = velocity (m/sec) x area (m2)

What influences stream shape? Substrate Type Stream Channel Pattern Riffle/ Run /Pool Ratio

Substrate Types Silt Cobble Sand Boulders Bedrock Gravel

Method for Recording observations of substrate Step into the stream, without looking bend down and pick up some sediment. Tell your partner the type of substrate you are holding, have them record the type with a tally mark. Take 50 samples in and along the river section. Tally your total number of observations for each type of substrate. Multiply the number of observations of each type by 2. This will equal the % out of 100 for each substrate.

Stream Channel Patterns Top View of Stream Cross-section view meandering straight braided

Meandering Stream Found in valley bottoms without much slope. Slower Velocity. Big pools, some riffles and runs Mixture of sand bars & suspended silt particles.

Straight Stream Steep gradient, fast flowing Substrate is predominantly cobble and gravel Mostly runs some riffles

Braided Stream River continually splits and rejoins. River moves across broad flat plains. Slow and fast velocities. Mostly runs and riffles. Mixture of silt, Sand, and gravel.

Habitat areas of a Stream Channel Run Run run

Pools where fish hide and rest from the current Riffles have high oxygen amounts essential for macroinvertabrates (bugs) and spawning fish. Runs where fish feed and travel Pools where fish hide and rest from the current

Method for Recording Riffle Run Pool Ratios 1. Take one step next to your river section, look across the river. Record a tally mark on your sheet that shows if you see a riffle, run, or pool 3. Make 50 observations. 4. Total the tally for each characteristic. 5. Multiply the totals by 2 to find the % riffle, run or pool that your river section contains.

Natural Influences affecting Stream Shape Friction created by substrate Velocity Vegetation

Human Influences affecting Stream Shape Development, logging, mining, grazing can destroy vegetation which causes more water and sediment to drain directly into a stream rather than being filter through groundwater. Channel alterations, ie. straightening of a stream along a highway or through a city center Dams prevent downstream flooding but then stream nutrients are not distributed throughout the floodplain to plants.

Why do we care about stream shape? Stream shape affects water quality Straightening of a stream increases velocity, which results in higher erosion rates and more turbidity Darker streams impact temperature and amount of sunlight that reaches plant life. Stream shape affects habitat. A straight stream does not have the variety of habitats found in a meandering stream Stream shape impacts flooding

How will you interpret your results? Physical Characteristics of the river will be correlated to the chemical and biological parameters. Some Examples: Channel pattern and shape will effect velocity and erosion which will in turn effect temperature and oxygen and/or nutrients. Substrate will be related to velocity and oxygen which will determine how many bugs are in the river. Riffle/Run/Pool ratio will indicate the diversity of the aquatic habitats and in relation to this the diversity of life in the stream. High diversity correlates to high water quality.