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Assessment of the Assessment of the Lycoming Creek Lycoming Creek Watershed Watershed by Brandon Ford

Assessment of the Lycoming Creek Watershed

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Assessment of the Lycoming Creek Watershed. by Brandon Ford. Overview. Previous studies Erosion Potential Sediment Load My work Water Chemistry Macroinvertebrate study. Erosion Evaluation. During the summer 2002, Lycoming college - PowerPoint PPT Presentation

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Page 1: Assessment of the Lycoming Creek Watershed

Assessment of the Assessment of the Lycoming Creek Lycoming Creek

WatershedWatershed

by Brandon Ford

Page 2: Assessment of the Lycoming Creek Watershed

OverviewOverview

• Previous studiesPrevious studies– Erosion PotentialErosion Potential– Sediment LoadSediment Load

• My workMy work– Water ChemistryWater Chemistry– Macroinvertebrate studyMacroinvertebrate study

Page 3: Assessment of the Lycoming Creek Watershed

Erosion EvaluationErosion Evaluation

• During the summer 2002, Lycoming college During the summer 2002, Lycoming college interns (Theresa Black and Amy Curry) walked or floated interns (Theresa Black and Amy Curry) walked or floated the entire stretchthe entire stretchof Lycoming Creek betweenof Lycoming Creek between

Roaring Branch (N 41° 34,294, W 76° 57.891) Roaring Branch (N 41° 34,294, W 76° 57.891)

And lower Heshbon Road (N 41° 16.127, W 77° 03.036).And lower Heshbon Road (N 41° 16.127, W 77° 03.036).

• Total of 28 miles Total of 28 miles

Page 4: Assessment of the Lycoming Creek Watershed

Erosion Evaluation FormErosion Evaluation Form

Page 5: Assessment of the Lycoming Creek Watershed
Page 6: Assessment of the Lycoming Creek Watershed

What they foundWhat they found

Page 7: Assessment of the Lycoming Creek Watershed

0

20

40

60

80

100

120

Number of

Structures

Bridges Mid-channelBars

DepositionBars

Pipes Rip Rap Tributaries ConcreteWalls

Dried Creekbed

TotalErosion sites

Structure

Disturbances Along Lycoming Creek

Disturbances

Page 8: Assessment of the Lycoming Creek Watershed

LYCOMING CREEK WATERSHEDLYCOMING CREEK WATERSHEDGEOMORPHIC ASSESSMENTGEOMORPHIC ASSESSMENT

• Rob Parker of Endless Mountains RC Rob Parker of Endless Mountains RC & D& D

• Walked all tributaries of Lycoming Walked all tributaries of Lycoming Creek with the help of Lycoming Creek with the help of Lycoming College InternsCollege Interns

• Surveyed all possible sites off erosion Surveyed all possible sites off erosion and took GPS locationand took GPS location

Page 9: Assessment of the Lycoming Creek Watershed

PURPOSEPURPOSE

• Physically inspect the tributaries and Physically inspect the tributaries and main stemmain stem

• Determine Determine sourcessources of instability of instability– i.e. watershed widei.e. watershed wide

• Development and prioritization of Development and prioritization of appropriate remediation strategies appropriate remediation strategies for each of the identified for each of the identified sites/reachessites/reaches

Page 10: Assessment of the Lycoming Creek Watershed

EquipmentEquipment

All waypoints were recorded using a All waypoints were recorded using a 3D Differential GPS unit (accuracy 3D Differential GPS unit (accuracy typically @6 ft.)typically @6 ft.)

Page 11: Assessment of the Lycoming Creek Watershed

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Penbryn

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Leolyn

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Yorktown

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Ellenton

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Bodines

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Marsh Hill

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Langdon

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Ralston

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Quiggleville

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Cogan Station# Balls Mills

# Hepburnville#

Oak Lynn

Way PointsIncluding

•Bridges

•Debris jams

•Sites of existing bank protection

•Erosion sites

Page 12: Assessment of the Lycoming Creek Watershed

Sediment LoadsSediment Loads

• Determined by inserting erosion site Determined by inserting erosion site lengths and stream discharge into a lengths and stream discharge into a computer program (BEHI) that computer program (BEHI) that models sediment loads lost from models sediment loads lost from erosion (tons/year)erosion (tons/year)

Page 13: Assessment of the Lycoming Creek Watershed

• 86 Sites86 Sites

• 31555’ Length31555’ Length

• 12862 Tons 12862 Tons per yearper year

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Union Center

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Ogdensburg

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Eastpoint#

Penbryn

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Leolyn

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Yorktown

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Ellenton

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Bodines

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Marsh Hill

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Langdon

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Ralston

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Gray#

Trout Run#

Powys

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Quiggleville

#Perryville #

Cogan Station

# Balls Mills# Hepburnville

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Oak Lynn

EROSION SITES

Page 14: Assessment of the Lycoming Creek Watershed

My WorkMy Work

• During Summer of 2004During Summer of 2004• Collected water samples and Collected water samples and

macroinvertebrate samples from macroinvertebrate samples from fives sites on Lycoming Creek and fives sites on Lycoming Creek and from sites on 14 of its tribs.from sites on 14 of its tribs.

• Samples were also taken from 3 Samples were also taken from 3 control sites; Grays Run, Rock Run, control sites; Grays Run, Rock Run, and Pleasant Streamand Pleasant Stream

Page 15: Assessment of the Lycoming Creek Watershed

Water Water ChemistChemistry and ry and

BiologicBiological al

SamplinSampling Sitesg Sites

Page 16: Assessment of the Lycoming Creek Watershed

Water ChemistryWater Chemistry

• Samples were collected in plastic Samples were collected in plastic containerscontainers– Each container was rinsed twice before Each container was rinsed twice before

fillingfilling

• Several biological and metal tests Several biological and metal tests were run on water samples including:were run on water samples including:– pH levelpH level– AluminumAluminum

Page 17: Assessment of the Lycoming Creek Watershed

Lycoming CreekLycoming Creek

• My data along with Amy and My data along with Amy and Theresa’s Theresa’s – Summer pH was generally higher than Summer pH was generally higher than

Spring pHSpring pH– Large decrease in alkalinity between Large decrease in alkalinity between

Summer and Spring samplingSummer and Spring sampling– Slight increase in pH from Summer ’02 Slight increase in pH from Summer ’02

to Summer ’04to Summer ’04

Page 18: Assessment of the Lycoming Creek Watershed

Averaged #’s for Water Averaged #’s for Water Chem.Chem.

Stream Name (Site Number) Roaring Branch Ralston Camp Susque Powys Bowmans Field

pH lab 7.03 6.60 6.66 6.77 7.00

Conductivity (us) 102.47 80.73 51.50 82.97 84.50

Alkalinity (ppm) 15.12 10.90 4.35 14.17 14.20

Orthophosphate 1.26 1.50 1.94 0.19 0.22

Phosphorous 0.31 0.27 0.84 2.05 0.33

Nitrate 9.62 9.95 8.01 7.67 6.38

Nitrite 0.02 0.02 3.29 0.02 0.02

DO (ppm) 8.97 10.72 10.62 10.88 10.48

Temp (C ) 79.83 12.27 12.00 12.25 13.63

TDS (ppm) 57.40 43.63 45.23 47.03 47.53

Page 19: Assessment of the Lycoming Creek Watershed

Sampled SitesSampled Sites

Page 20: Assessment of the Lycoming Creek Watershed

Average pH levelsAverage pH levels

• Average pH level of Pa streams 6.5 – 8.5Average pH level of Pa streams 6.5 – 8.5

Average pH of the Tribs and Control Sites

0

5

10

pH

Page 21: Assessment of the Lycoming Creek Watershed

How pH Effects Stream LifeHow pH Effects Stream Life• Acidic water allows leaching of many toxic chemicals Acidic water allows leaching of many toxic chemicals

• pH levels around 4 or below may destroy larva and eggs, pH levels around 4 or below may destroy larva and eggs, result in fish kills, and/or cause mutations. result in fish kills, and/or cause mutations.

Page 22: Assessment of the Lycoming Creek Watershed

Tributaries with High pH Tributaries with High pH LevelsLevels

• Many streams had a pH level under 5.0

• Frozen Run, Red Run, Miners Run, Yellow Dog Run, Hound Run, Doe Run, and Upper Long Run

Average Summer Trib. pH's (Relative to 5)

8

7Above 5

Below 5

Page 23: Assessment of the Lycoming Creek Watershed

Average Aluminum LevelsAverage Aluminum Levels• Levels increase due to low pH levelsLevels increase due to low pH levels

• Pa State Drinking Limit is 0.2 mg/LPa State Drinking Limit is 0.2 mg/L

0

0.1

0.2

0.30.4

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0.6

0.7

0.8

mg

/L

Page 24: Assessment of the Lycoming Creek Watershed

How Does Aluminum Effect How Does Aluminum Effect Stream LifeStream Life

• Accumulates on gills restricting Accumulates on gills restricting breathingbreathing

• Al levels of 0.5 mg/L combined with Al levels of 0.5 mg/L combined with pH levels under 5.5 are lethal to most pH levels under 5.5 are lethal to most fish and aquatic macroinvertebratesfish and aquatic macroinvertebrates

• A level of 0.1 mg/L Al, independent of A level of 0.1 mg/L Al, independent of pH, has been set as a “stress level” pH, has been set as a “stress level” for aquatic organismsfor aquatic organisms

Page 25: Assessment of the Lycoming Creek Watershed

Tributaries with High Levels Tributaries with High Levels (>0.1mg/l) of Al(>0.1mg/l) of Al

• Several tribs had pH levels over 0.1 mg/lSeveral tribs had pH levels over 0.1 mg/l– Frozen Run, Red Run, Miners Run, Yellow Dog Run, Frozen Run, Red Run, Miners Run, Yellow Dog Run,

Hound Run, Doe Run, Long Run, Abbott Run, and Upper Hound Run, Doe Run, Long Run, Abbott Run, and Upper Long RunLong Run

– Abbott Run was above .5 mg/lAbbott Run was above .5 mg/lSummer Al levels for Tributaries

85

1

above .1 - .5

below .1

above .5

Page 26: Assessment of the Lycoming Creek Watershed

What do these measurements What do these measurements tells us?tells us?

• High levels of any of these High levels of any of these measurements indicate some type of measurements indicate some type of acid impactacid impact– Acid precipitationAcid precipitation– Acid mine drainageAcid mine drainage

• Many of the sample tribs. lie below Many of the sample tribs. lie below abandoned minesabandoned mines

Page 27: Assessment of the Lycoming Creek Watershed

Acid Mine Drainage (AMD)Acid Mine Drainage (AMD)

• Occurs in streams below old surface Occurs in streams below old surface and deep minesand deep mines

• Pyrite (FeSPyrite (FeS22) is present in coal seams ) is present in coal seams and the rock layers between coal and the rock layers between coal seemsseems

• Result of the reaction that occurs Result of the reaction that occurs when pyrite encounters water and airwhen pyrite encounters water and air

Page 28: Assessment of the Lycoming Creek Watershed

The ReactionThe Reaction

• FeS2 + 3.75 O2 + 3.5 H2O Fe(OH)3 + 2 FeS2 + 3.75 O2 + 3.5 H2O Fe(OH)3 + 2 H2SO4 H2SO4 – Yielding iron hydroxide and sulfuric acidYielding iron hydroxide and sulfuric acid

• The acid increases pH which leads to the leaching The acid increases pH which leads to the leaching of Al, Fe, and Mn from soilsof Al, Fe, and Mn from soils

• These metals dissolve in stream water but These metals dissolve in stream water but precipitate out when pH levels increaseprecipitate out when pH levels increase– Most of the tribs. with low pH values also had high Al Most of the tribs. with low pH values also had high Al

levelslevels

Page 29: Assessment of the Lycoming Creek Watershed

Metal PrecipitatesMetal Precipitates

• Fe leads to Fe leads to characteristic Red -characteristic Red -Orange or Orange -Orange or Orange -Yellow colorYellow color– Yellow BoyYellow Boy

• Al is White and Mn Al is White and Mn is Blackis Black

Page 30: Assessment of the Lycoming Creek Watershed

Metal PrecipitatesMetal Precipitates

• Precipitates fall to stream beds Precipitates fall to stream beds coating them and the rocks coating them and the rocks macroinvertebrates live undermacroinvertebrates live under

• Coating smothers macroinverts and Coating smothers macroinverts and restricts their breathing restricts their breathing

• Leads to fish kills as fish feed on the Leads to fish kills as fish feed on the macroinvertsmacroinverts

Page 31: Assessment of the Lycoming Creek Watershed

Macroinvertebrate Macroinvertebrate CollectionCollection

• Samples collected by means of a kick Samples collected by means of a kick netnet

• Placed in plastic container and Placed in plastic container and preserved w/ % ethanolpreserved w/ % ethanol

• Samples were then counted and Samples were then counted and identifiedidentified

Page 32: Assessment of the Lycoming Creek Watershed

RBA of MacroinvertebratesRBA of Macroinvertebrates

• Samples were analyzed using the Samples were analyzed using the EPA’s Rapid Bioassessment protocolEPA’s Rapid Bioassessment protocol

• Based onBased on– # of taxa# of taxa– # of EPT# of EPT– Hilsenhoff Biotic IndexHilsenhoff Biotic Index– % Tolerant and % Intolerant Taxa% Tolerant and % Intolerant Taxa– Shannon-weiner Diversity Shannon-weiner Diversity

Page 33: Assessment of the Lycoming Creek Watershed

RBA of MacroinvertebratesRBA of Macroinvertebrates

• Categories are scored 1-5, 5 being Categories are scored 1-5, 5 being goodgood

• Add up the 6 category scores for a Add up the 6 category scores for a site score (0-30)site score (0-30)– 6-10 – very poor6-10 – very poor– 11-16 – poor11-16 – poor– 17-22 – fair17-22 – fair– 23-30 - good 23-30 - good

Page 34: Assessment of the Lycoming Creek Watershed

Metrics for Red RunMetrics for Red Run

Red Run (S1)* Red Run (S2)* Red Run (S3)* Red Run (S4)*

Total Taxa 11 9 15 5

EPT Taxa 6 4 7 0

Hilsenhoff Biotic Index 2.43 1.76 2.79 5.93

% Intolerant 0.63 0.74 0.56 0

% Tolerant 0 0 0.04 0

Shannon Diversity 2.173 2.201 2.326 0.5237

         

Metric Scores        

Total Taxa 3 3 5 1

EPT Taxa 5 3 5 1

Hilsenhoff Biotic Index 5 5 5 3

% Intolerant 5 5 5 1

% Tolerant 5 5 5 5

Shannon Diversity 5 5 5 1

         

Site Score 28 26 30 12

Relative Health Good Good Good Poor

Page 35: Assessment of the Lycoming Creek Watershed

Average Site Score for Tributaries

05

101520253035

Site

Sco

re

Page 36: Assessment of the Lycoming Creek Watershed

ResultsResults

• Only one trib. (West Hills Run) had a Only one trib. (West Hills Run) had a fair health sore when its site scores fair health sore when its site scores where averagedwhere averaged

• However, many individual sites had However, many individual sites had fair scores and one had a poor scorefair scores and one had a poor score– Bottle Run 4, West Hills Run, Miners Run Bottle Run 4, West Hills Run, Miners Run

2 & 3, and Doe Run 1 all had fair scores2 & 3, and Doe Run 1 all had fair scores– Red Run 4 had a poor scoreRed Run 4 had a poor score

Page 37: Assessment of the Lycoming Creek Watershed

ResultsResults

• Although many Although many streams streams appeared to be appeared to be impaired when impaired when there waters are there waters are chemically chemically tested, tested, macroinvertebramacroinvertebrate communities te communities are relatively are relatively unimpairedunimpaired

Page 38: Assessment of the Lycoming Creek Watershed

Future WorkFuture Work

• More water testing is being More water testing is being performed this Springperformed this Spring– More severe pH levels are present in More severe pH levels are present in

streams during the winter/spring streams during the winter/spring melting/runoff process due to the high melting/runoff process due to the high acidity of PA precipitationacidity of PA precipitation

• More work will also be performed this More work will also be performed this summersummer

Page 39: Assessment of the Lycoming Creek Watershed

Hound Run Summer/SpringHound Run Summer/Spring

• pH dropped in spring and Al levels pH dropped in spring and Al levels increasedincreased

  Summer pH Spring pH Summer Al Spring Al

Site 1 4.835 2.79 0.192 0.215

Site 2 4.78 3.34 0.275 0.35

Site 3 5.06 3.17 0.163 0.171

Page 40: Assessment of the Lycoming Creek Watershed

AcknowledgementsAcknowledgements

• Zimm and the rest of the Biology Zimm and the rest of the Biology StaffStaff

• Rob ParkerRob Parker

• Drew Zimmerman, Amy Curry, Jim Drew Zimmerman, Amy Curry, Jim Rodgers, and Heather EdelsteinRodgers, and Heather Edelstein

• MattMatt