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Post-fire Impacts to Drinking Water Treatment 1 Amanda Hohner Assistant Professor Washington State University [email protected]

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Page 1: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Post-fire Impacts to Drinking Water Treatment

1

Amanda HohnerAssistant Professor

Washington State [email protected]

Page 2: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Agenda• Case Study: High Park Fire in northern Colorado• Utility Response• Overview of three AWWA-WRF Wildfire projects

• Post-fire Monitoring of a Water Intake• Leaching of Wildfire-Affected Sediments• Laboratory Heating of Soil and Litter

• Summary and Recommendations

2

Page 3: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Watershed Response

Increased particle loads

Elevated nutrient levels• Algal blooms• Algal organic matter

Altered dissolved organic matter• Coagulation challenges• DBP formation & speciation

Treatment Implication3

• Infrastructure problems• Coagulation, filtration, &

disinfection challenges

Goal: connect post-fire water quality changes directly to impacts on treatment process performance and finished water quality

Page 4: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

The High Park wildfire burned the Cache la Poudre (CLP) watershed in northern Colorado

Burned from June 9th- July 1st, 2012 87,000 acres at mixed severities Burned ~10% of total watershed

The CLP River provides water to several northern Colorado communities

Case Study- High Park Wildfire

Photo Credit: Michael Menefee

4

Page 5: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Watershed Response• Extensive loss of vegetation • Moderate to high soil burn severity • Hydrology shifted from subsurface to surface flow • Even small, previously dry tributaries experienced very

high, “flashy” flows

5

Page 6: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Fort Collins Utility Response• Shut down CLP River water supply • Used alternate water source (Horsetooth Reservoir) for over 100 days• CLP River water was slowly blended back into drinking water source • When turbidity exceeded 100 NTU the river intake was shut off again• Rapidly designed and constructed a pre-sedimentation basin

6

Page 7: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Fort Collins Utility Response• Installed early warning system• Provides ~ 1 hour warning of highly turbid water • Allows operators to shut down pipeline and avoid large sediment loads

Page 8: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Research Approach

8

1. Post-fire monitoring of a drinking water intake

2. Leaching of wildfire-affected sediments

3. Controlled laboratory heating and leaching of soil and litter

Bench-scale Treatability Evaluation

Page 9: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Study 1. Post-fire Monitoring9

Water Intake

Reference Site

• Monitored bi-weekly during baseflow and snowmelt• Post-rainstorm samples collected from intake

Page 10: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Pre- and Post-fire Water Quality 10Hohner et al., 2016, Water Research

• Paired differences in water quality (intake – reference site)• Dashed line (difference = 0)• *Post-rainstorm samples were not included

Page 11: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Treatability Evaluation• Conventional treatment with aluminum sulfate

• Coagulant dose selected based on optimal DOC removal

• Raw and treated water samples were chlorinated and analyzed for disinfection byproduct formation (DBPs)• Carbonaceous DBPs

• Total trihalomethanes (TTHMs)• Five haloacetic acids (HAA5s)

• Nitrogenous DBPs• Haloacetonitriles (HANs)• Chloropicrin

11

Page 12: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Watershed Monitoring:Raw Water C-DBPs

TTHM formation (μg/L) was significantly higher at the water intake

C-DBP yields peaked with snowmelt

C-DBP yields were not significantly different following the wildfire

Post-rainstorm C-DBP yields were similar to baseflow & snowmelt samples

12

10

20

30

40

50

60

70

80

TTH

M Y

ield

(µg/

mgC

)

Pre-fire Intake Water Intake Reference Rainstorm Events

10

20

30

40

50

60

70

80

Apr

il-13

May

-13

June

-13

July

-13

Aug

ust-1

3

Sept

embe

r-13

Oct

ober

-13

HAA

5 Yi

eld

(µg/

mgC

)

Page 13: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Watershed Monitoring:Raw Water N-DBPs

HAN4 formation (μg/L) was significantly higher at the water intake

N-DBP yields did not follow the same seasonal trend as C-DBPs

N-DBP yields were similar for the water intake and reference site

Post-rainstorm N-DBP formation and yields were elevated

13

0

1

2

3

4

HAN

4 Yi

eld

(µg/

mgC

)

Water Intake Reference Rainstorm Events

0

1

2

3

4

Apr

il-13

May

-13

June

-13

July

-13

Aug

ust-1

3

Sept

embe

r-13

Oct

ober

-13

Chl

orop

icrin

Yie

ld (µ

g/m

gC)

Page 14: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Watershed Monitoring: Treatment Response

• During baseflow and snowmelt significantly higher alum dose (10 mg/L) required for water intake

• Post-rainstorm samples presented treatment challenges, and even at high alum doses (>65 mg/L) showed minimal DOC removal (< 10%)

• Post-fire samples had high initial turbidity (>200 ntu) and high DOC

• Five post-rainstorm samples exceeded DBP MCLs

14

0

1

2

3

4

5

6

0 50 100

DOC

(mgC

/L)

Alum Dose (mg/L)

PNF 5/4

PBR 5/4IntakeReference

Page 15: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Study 2. Wildfire-affected Sediment Leaching• Source Water Leachates:

• Sediments added to source waters for two utilities• Fort Collins (baseline)• Denver Water (baseline)

• LCT Leachates:• Sediments added to low-carbon tap-water (LCT)

• Treatment processes evaluation:• Coagulation• Pre-oxidation/Coagulation• Powdered activated carbon (PAC) + Coagulation• Biofiltration/Coagulation• Ozonation/Coagulation/Biofiltration

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Page 16: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

CLP River Water and Sediment Leachate Comparison 16

Page 17: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Sediment Leachates: Coagulation Response17

0

1

10

100

1000

0 20 40 60

Log

Turb

idity

(ntu

)

Alum Dose (mg/L)

Baseline WatersSource Water LeachatesLCT Leachates

0

2

4

6

8

10

0 10 20 30 40 50 60

DO

C (m

g C/L

)

Alum Dose (mg/L)

Hohner et al., 2017, Environmental Science: Water Research & Technology

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Sediment Leachates: C-DBP Formation18

Solid symbols represent raw samples and open symbols show treated samples Trends were significant for all sample groups (p < 0.001) Slopes for different sample groups were not significantly different (p > 0.05)

0

50

100

150

200

250

300

350

400

450

0 2 4 6 8 10

TTHM

(μg/

L)

DOC (mgC/L)

Baseline WatersSource Water LeachatesLCT Leachates

0

50

100

150

200

250

300

350

400

0 2 4 6 8 10

HAA

5 (μ

g/L)

DOC (mgC/L)

Baseline WatersSource Water LeachatesLCT Leachates

Page 19: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Sediment Leachates: N-DBP Formation19

HAN4 trend was significant (p < 0.001) for the LCT leachates Slopes for the different sample groups were significantly different (p > 0.05) Sediment leachates appear enriched in N-DBP precursors

0

5

10

15

20

25

0 2 4 6 8 10

HAN

4 (μ

g/L)

DOC (mgC/L)

Baseline WatersSource Water LeachatesLCT Leachates

0

5

10

15

20

25

30

0 2 4 6 8 10

Chlo

ropi

crin

(μg/

L)

DOC (mgC/L)

Baseline WatersSource Water LeachatesLCT Leachates

Page 20: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

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1. DBP MCLs were used to assess treatability of the sediment leachates

2. DBP Yields were used for comparison of samples with varying

DOC

3. Required DOC threshold values for the point of chlorination were

determined

4. The more restrictive DOC threshold was chosen (TTHM or HAA5)-lower required treated water DOC concentration for meeting MCLs

Page 21: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

21

Sample Name

DOC Threshold(mgC/L) Best Treatment

OptionConventional

TreatmentEnhanced

Coagulation PAC Chlorine Dioxide

Pre-ozonation Biofiltration

Pre-ozonation/

BiofiltrationB

asel

ine

Wat

ers

Fort Collins(FC) 2.6 2.8 2.3 2.6 2.7 2.6 3.0 Pre-ozonation/

Biofiltration

Denver Water(DW) 3.1 3.3 2.8 4.8 3.0 2.7 3.3 Chlorine Dioxide

Average increase in DOC threshold 0.2 -0.3 0.8 0.0 -0.2 0.3

Sour

ce W

ater

Lea

chat

es

A- FC 2.0 2.0 1.8 1.8 2.4 1.4 2.2 Pre-ozonation

B- DW 1.7 2.1 1.8 1.8 3.0 1.6 2.6 Pre-ozonation

C- DW 2.1 2.8 2.1 2.1 2.8 2.4 2.1 Enhanced Coag& Pre-ozonation

D- FC 1.8 2.4 1.3 2.0 2.4 1.8 2.3 Enhanced Coag& Pre-ozonation

LC

T L

each

ates

A- LCT 2.0 2.3 1.8 2.1 2.6 1.6 2.4 Pre-ozonation

B- LCT 1.6 2.1 2.0 2.0 1.7 1.7 2.1 Enhanced Coag & Pre-ozonation/Bio

C- LCT 1.4 1.9 2.1 1.7 3.0 1.5 2.1 Pre-ozonation

D- LCT 2.1 2.0 1.8 2.2 2.7 1.6 2.5 Pre-ozonation

Average Increase in DOC threshold 0.4 0.0 0.1 0.7 -0.1 0.5 Pre-ozonation

Page 22: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Study 3: Controlled Heating22

• Objective: Understand the effects of a low-moderate severity wildfire on dissolved organic matter and treatability

• Surface litter and soil samples were collected from three source watersheds

DW

WM

NY

Page 23: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Controlled Laboratory Heating23

• Materials were heated in a furnace at 225°C for two hours • Soil and litter were composited• Unheated (control) and heated materials were leached for 24 hours in LCT water• Leachates were diluted to a DOC concentration = 5.0 ± 1.0 mgC/L

Page 24: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Controlled Heating: Dissolved Organic Matter (DOM)

• Heating altered the DOM character:• Nitrogen enriched: DOC:DON ↓• More aromatic: SUVA254 ↑ • Lower molecular weight compounds

24

Page 25: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Controlled Heating: Jar Test Response25

0.0

0.1

1.0

10.0

100.0

0 20 40 60 80

Log

Turb

idity

(ntu

)

Alum Dose (mg/L)

WM Control WM HeatedDW Control DW HeatedNY Control NY Heated

1

2

3

4

5

6

7

0 20 40 60 80 100 120

DO

C (m

g C/L

)

Alum Dose (mg/L)

Page 26: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Controlled Heating: Treated Water DBP Levels26

0

20

40

60

80

100

120

140

160

0 1 2 3 4 5

HAA

5 Fo

rmat

ion

(μg/

L)

DOC (mgC/L)

MCLControlHeated

0

20

40

60

80

100

120

140

160

0 1 2 3 4 5

TTH

M F

orm

atio

n (μ

g/L)

DOC (mgC/L)

MCLControlHeated

0

2

4

6

8

10

12

0 1 2 3 4 5

HAN

4 Fo

rmat

ion

(μg/

L)

DOC (mgC/L)

0

2

4

6

8

10

12

14

16

0 1 2 3 4 5C

hlor

opic

rin F

orm

atio

n (μ

g/L)

DOC (mgC/L)

Page 27: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Research Summary• A small wildfire may impact water quality and treatment

• Post-rainstorm samples presented the greatest treatment challenges

• Additional treatment may be required to meet DBP MCLs

• Attention should be given to post-fire N-DBP precursors

• DOM character may be altered by wildfire heating

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Page 28: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Recommendations Capital Investment Considerations Expanding water storage capacity Exploring additional supplies Increasing monitoring Constructing pre-sedimentation basins

Treatment Operations Increase coagulant dose to account for higher turbidity and DOM Increased solids loading, greater costs, shorter filter runs Difficulty meeting DBP regulations

*Small, single source water treatment systems may be at greatest risk*

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Page 29: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

AcknowledgmentsWater Research Foundation Colorado Department of Public Health & Environment Hazen & SawyerWater Utilities Denver Water, NYC Department of Environmental Protection, City of

Westminster, San Francisco Public Utilities Commission, Truckee Meadows Water Authority, Metropolitan Water District of Southern California, City of Fort Collins

University of Colorado Jeffrey Writer, Dorothy Noble, Kaelin Cawley, Jack Webster, Leigh Gilmore, Eli

Townsend, Ariel Retuta, Garrett McKay, Andrew Moscovich, Wade Godman

Page 30: Post-fire Impacts to Drinking Water Treatment · 2018-10-23 · HAN4 formation (μg/L) was significantly higher at the water intake N-DBP yields did not follow the same seasonal trend

Additional Resources30

• Becket et al., 2018, Journal AWWA• Hohner et al., 2016, Water Research• Hohner et al., 2017, ESWRT• WRF 4590 Report, 2018• Writer et al., 2014, Journal AWWA• Contact: Amanda Hohner, Washington State University, [email protected]