Seasonal Patterns in the Relative Importance of Organic Acids and Sulfate in Episodic Acidification...

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Seasonal Patterns in the Relative Importance of Organic Acids and Sulfate in Episodic Acidification of

Downeast Salmon Rivers

By Mark Whiting, Maine DEP & William Otto, U of Maine at

Machias

Cove BrNarraguagus R

Pleasant R

Machias R

E Machias RDennys R

Pleasant R Data Sonde at Columbia Falls

0

0.5

1

1.5

2

2.5

3

3.5

4

4.5

J J J J F F F M M M M A A A A M M M J J J J J J J J A A A A S S S O O O O N

Date

Ra

in i

n I

nc

he

s

3

3.5

4

4.5

5

5.5

6

6.5

7

7.5

8

pH

RainpH

Summary of GMC Hypothesis

• These river are naturally acidic• The important acidity is natural organic

acidity (Dissolved Organic Carbon, or DOC), this drives day to day pH and our episodic acidification events

• Salmon recovery may be hindered by low pH, but since it is natural, the original salmon decline must be from other causes

How do you tell which acids are the important ones?

Review available data

• 700 total samples from all rivers, from 1999 – 2002

• Water samples were taken by volunteers from salmon river watershed councils

• Analysis done by George Mitchell Center

• Samples ranged from N = 19 (Tunk Stream) to N = 142 (Sheepscot R.)

Episodic acidification occurs in all downeast salmon rivers

• Low pH is driven by rain events and especially runoff and snowmelt

• Low pH events occur October - May

• pH will respond to either changes in the concentration of acids or bases, this report concentrates on the sources of acidity

Pleasant R sonde at Columbia Falls, August 10-12, 2005

6.3

6.4

6.5

6.6

6.7

6.8

6.9

7

7.1

7.2

7.3

Date - Time

Fiel

d pH

The role of CO2

• Carbon dioxide concentrations vary diurnally, with a low at night and a high in the afternoon, following the relative amounts of photosynthesis and respiration

• pH varies ± 0.2 pH unit around the daily mean in the peak of the summer season due to CO2

PH

SO

4D

OC

PH

NO

3

SO4 DOC NO3

correlations for Pleasant R, estuary sites removed

Pleasant River, All Samples

Narraguagus, Stormwater Only

PH

SO

4

PH

DO

C

SO4 DOC

Narraguagus, DEP data, Stormwater only

Seasonal scale pH variation

• Regressions are variable, different acids are important at different times and places

• Two acids, DOC often important overall and in some stormwater data sets

• Sulfate is sometimes more important than DOC in specific stormwater data sets (i.e., depending on the river, specific storms, during acidic episodes, etc)

Analysis of low pH events

• Plot pH by month for each river, include plots of the acidic anions by month, which acid source accounts for pH minima?

• One ueq/l of an acid is needed to neutralize one ueq/l of a base, so the dominant anion is the one with the most ueq’s above baseflow values

10 2 3 4 5 6 7 8 9MONTHS

4

5

6

7

PH

10 2 3 4 5 6 7 8 9MONTHS

0

10

20

30

40

50

60

70

80

DO

C

10 2 3 4 5 6 7 8 9MONTHS

40

50

60

70

80

90

100

SO

4

10 2 3 4 5 6 7 8 9MONTHS

0

5

10

15

20

NO

3

Tunk Stream, All Sites by Month, in UEQ

10.0002.000

3.0004.000

6.0007.000

8.0009.000

MONTHS

4

5

6

7

8

PH

10.0002.000

3.0004.000

6.0007.000

8.0009.000

MONTHS

0

50

100

150

200

DO

C

10.0002.000

3.0004.000

6.0007.000

8.0009.000

MONTHS

10

20

30

40

50

60

70

80

SO

4

10.0002.000

3.0004.000

6.0007.000

8.0009.000

MONTHS

0

5

10

15

NO

3

Pleasant R, all sites and flows, in UEQ

10.0002.000

3.0004.000

6.0007.000

8.0009.000

MONTHS

5

6

7

8

PH

10.0002.000

3.0004.000

6.0007.000

8.0009.000

MONTHS

0

10

20

30

40

50

60

70

80

90

100

DO

C

10.0002.000

3.0004.000

6.0007.000

8.0009.000

MONTHS

0

50

100

150

SO

4

10.0002.000

3.0004.000

6.0007.000

8.0009.000

MONTHS

0

10

20

30

40

50

NO

3

Narraguagus R, All Data, in UEQ

10.0003.000

4.0006.000

7.0008.000

9.000

MONTHS

4

5

6

7

8

PH

10.0003.000

4.0006.000

7.0008.000

9.000

MONTHS

10

20

30

40

50

60

70

80

90

DO

C

10.0003.000

4.0006.000

7.0008.000

9.000

MONTHS

10

20

30

40

50

60

70

80

90

100

110

SO

4

10.0003.000

4.0006.000

7.0008.000

9.000

MONTHS

0

1

2

3

4

NO

3

Machias R, All Data, in UEQ

10.0002.000

3.0006.000

7.0008.000

9.000

MONTHS

4

5

6

7

8

PH

10.0002.000

3.0006.000

7.0008.000

9.000

MONTHS

10

20

30

40

50

60

70

80

90

100

110

DO

C

10.0002.000

3.0006.000

7.0008.000

9.000

MONTHS

10

20

30

40

50

60

70

80

90

100

110

SO

4

10.0002.000

3.0006.000

7.0008.000

9.000

MONTHS

0

5

10

15

NO

3

E Machias, All Sites, All Flows, in UEQ

10.000

11.000

6.0007.000

8.0009.000

MONTHS

5.5

6.0

6.5

7.0

7.5

PH

10.000

11.000

6.0007.000

8.0009.000

MONTHS

0

50

100

150

DO

C

10.000

11.000

6.0007.000

8.0009.000

MONTHS

0

50

100

150

200

SO

4

10.000

11.000

6.0007.000

8.0009.000

MONTHS

0

1

2

3

NO

3

Dennys R, All Sites and Flows, in UEQ

Summary

• Overall Sulfate and DOC are about equal when measured in ueq/L

• Sulfate, DOC and combinations of the two are apparently the acids responsible for low pH events

• In this data set, during low pH events Sulfate dominates in Tunk, the Narraguagus, and Pleasant Rivers

Summary (continued)

• Sulfate and DOC both play a role in acidic episodes on the Machias, E Machias and Dennys

• Only in the Dennys is DOC more abundant during low pH events than Sulfate

• Nitrate often peaks in high flow periods, but the concentration are still very low

Conclusions

• Acid rain is our oldest, best known, and most studied problem affecting salmon survival downeast

• Our low pH events are classic episodic acidification with acid rain components, esp. sulfate the primary driver

• DOC is important in baseflow, and sometimes in stormwater acidity

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