Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in...

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The Physical Impact of Mining Yacuambi River Basin, Southern Ecuador May 2011 Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier, Department of Fish & Wildlife Resources, University of Idaho Carlos Iñiguez A. Instituto de Ecología Universidad Técnica Particular de Loja

Transcript of Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in...

Page 1: Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,

The Physical Impact of Mining Yacuambi River Basin, Southern EcuadorMay 2011

Emily Shimada, Environmental Science, University of IdahoResearch Team B: Watershed Management in the Andean ParamoFaculty Advisors: Dr. Alex Fremier, Department of Fish & Wildlife Resources, University of Idaho

Carlos Iñiguez A. Instituto de Ecología Universidad Técnica Particular de Loja

Page 2: Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,

Introduction: Sediment in Fluvial Environments

Bedload (D>1mm)Suspended load (D<0.05mm)Wash load (D<0.0063mm)

Name Diameter (mm)

BouldersCobblesGravelSandSiltClay

>25664-256

2-640.062-2

.004-.062<0.004

Texture Classification

Page 3: Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,

Introduction: Cause & Effect of Increased Fluvial Sediment

Source ImpactNatural Anthropogenic Course grain/ Bedload Fine grain/ Suspended load

ClimateVegetationTopographyGeology & soilTectonicsBase levelSurface erodibilityTime/history

MiningAgricultureDeforestationUrbanizationDamsTraffic/Roads/

ConstructionGrazing

Increased water levelFlooding potentialAlterations in channel

dimensionsAlterations in the

stream substratesAlterations in aquatic

organism habitat

Increased flow viscosity & reduced settling velocity ->increase transport grain size & bedload

Reduced depth for sunlight penetration ->hinders photosynthesis

Page 4: Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,

Background: Tropical Mountain Stream Ecosystems

Source Impact

Natural Anthropogenic MiningCourse sedient build up-> increases channel bed elevation (decreasing flow)Decreased aquatic biological activity

Steep topography Tropical Climate High rainfall Abundant vegetation

Land use managementMining activities

Page 5: Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,

Research Objectives1. What is the observed grain size distribution in:Streams considered “un-impacted” from human land use activities

(mining) Impacted stream

Above & Below sites with changes in land use

2. What is the predicted grain size distribution based on measurable stream dimensions in:

Streams considered “un-impacted” from human land use activities (mining)

Impacted stream- Above & Below sites with changes in land use

3. Is there a relationship between: Observed & predicted D50 in different streams and stream reachesLand use gradient & observed grain size distributionPhysical stream properties & ecological functioning of the stream?

Study Site

Page 6: Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,

Site SelectionImpacted & un-impactedAbove & Below areas of distinct land use differences (mining) Establish sites at the Stream Reach scale

Length = approx. 10X Width

Relatively uniform slope, dimensions, velocity

Methods: 1) Field Work

Sediment Property MeasurementsPebble Count Median Grain Size (D50)

Wet Sieving Median Grain Size (D50)

For sediment diameters 1mm & 2mm

64mm

1mm

General Stream MeasurementsVelocityCross-sectional Area Wetted PerimeterTurbiditySlopeDepthBankfull width

Page 7: Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,

Methods: 2) Analytical Work1) Predicted grain size distribution:

D50 that moves at observed flow

D50 that moves at bankfull flowbf = gRS

τ cr = ηg(ρ s − ρ)π

6D tanφ

Additional Measurements•Discharge Q=VA•Turbidity•Manning’s roughness

n =k(R2/3S1/2)

V

Initiation of Motion

2) Establish relationship between predicted & observed D50:

Between & within un-impacted stream reachesBetween & within impacted stream reaches

(above and below land use site)

3) Compare grain size distribution between impacted & un-impacted streamsIs there a clear correlation of grain size

distribution to land use gradient?Is there an ecological impact?

D50 =τ

τ cr (ρ s − ρ)g

G = gRS

(shear stress)

Page 8: Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,

Relevance & Connection

Physical Impact of current land uses

Bio-indicator Framework

Current watershed uses & policies

Cultural & political Perceptions of watershed use & resulting impacts

Is there an observed ecological impact?

What is the relationship between land use and

ecological impact?What needs to be done?

Is there an interest and/or agenda for

watershed protection?

What can be done at the local & international level order to accommodate cultural values and stakeholders’ interests,

while promoting sustainable land use practices and policies?

Watershed use & policy jurisdiction

(stakeholders)

Societal/Political affect on watershed use & the ecosystem

Page 9: Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,

Thanks & References Images: http://www.amazonrainforestnews.com/2011_04_01_archive.html http://www.nativerevegetation.org/learn/manual/ch_5.aspx http://www.amazonconservation.org/news/newsletter/0812/index.html http://www.uwsp.edu/geo/faculty/lemke/geomorphology/lectures/03_stream_sediment.html