Tracking Carbon and Nitrogen Pollution from Headwaters to ... › ... · Tracking Carbon and...

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Tracking Carbon and Nitrogen

Pollution from Headwaters to Coasts

Sujay Kaushal1, Shahan Haq1, Shuiwang Duan1,

Jake Beaulieu2, Rose Smith1, Guangming

Zheng3, Michael Ondrusek3, Marilyn Murphy3,

Paul DiGiacomo3

1University of Maryland, Department of Geology &

Earth System Science Interdisciplinary Center

2U.S. Environmental Protection Agency

3National Oceanic and Atmospheric Administration,

NESDIS, STAR

How does land use impact the coastal carbon cycle?

• Urban development replaces natural drainage with infrastructure

– Storm drain systems

– Leaky sewers

– Impervious surfaces

• Major impacts on carbon cycle over space and time

Kaushal and Belt (2012)

Urban Watershed Continuum: Research Questions

• How does human-accelerated weathering

impact the coastal carbon cycle?

• Is the urban river continuum a transporter or

transformer of carbon?

• What are implications for the coastal carbon

cycle?

Evolving Weathering in

Urbanized Watersheds

Over Time

Kaushal and Belt (2012)

Kaushal et al. (2014, 2015)

Cities create a distinct urban geology

Weathering of “urban karst”

1. Urban weathering

impacts coastal carbon?

Increasing alkalinity in 66% of sites:

Watershed Size

Elevation

Lithology

Land UseKaushal et al. (2013), ES&T

0

5

10

15

20

25

30

35

0

10

20

30

40

50

60

70

80

Oct-54 Jun-68 Feb-82 Oct-95 Jul-09

Calc

ium

Concentr

ation (

mg/L

)

Calc

ium

Con

centr

ation (

mg/L

)

Patuxent River, Maryland, USASaddle River, New Jersey, USABaltimore Drinking Water, Maryland, USA

Kaushal et al.

(2013, 2014)

Human-Accelerated Weathering in Watersheds

Map Created by Noah Bowman - Kaushal et al. (2017)

Kaushal et al. (2017)

Ca2+ Mg2+ DIC SO42- pH

K+ Si

Impervious Surfaces?

Na+ Ca2+ Mg2+ K+ Cl-

SO42-

Road Salts?

Si DIC SO42- NO3

-

K+

Sewage?Kaushal et al. (2017)

Coastal Alkalinization?

Kaushal et al. (2017)

2. The Urban Watershed Continuum:

Transporter or Transformer?

Discharge Controls Carbon Transport

BBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBB

0

4

8

12

16

0.1 1.0 10.0

DO

C m

g L

1

Site

NERP r2=0.38

NWHV r2=0.11

PBCP r2=0.35

SLIGO r2=0.16

Dissolved Organic Carbon

CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC

5

10

15

20

25

0.1 1.0 10.0

Discharge m3s

1

DIC

mg

L1

Site

NERP r2=0.45

NWHV r2=0.22

PBCP r2=0.25

SLIGO r2=0.32

Dissolved Inorganic Carbon

DDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOMaquatic DOM

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0.5

0.6

0.7

0.8

0.9

1.0

0.1 1.0 10.0B

IX

Site

NERP r2=0.44

NWHV r2=0.21

PBCP r2=0.14

SLIGO r2=0.19

Recent Autochthonous Inputs (BIX)

Smith and Kaushal (2015)

Light Controls Carbon Metabolism

0.0

0.5

1.0

1.5

2.0

2.5

10 11 12 13 14 15Day length (hr)

GP

P g

C m

2 d

ay

Site

NERP

PBCP

SLIGO

Smith and Kaushal (2015)

Streams as Tranporters vs. Transformers?

-50

0

50

100

0.1 1.0 10.0

% D

IC I

nput

Fro

m S

tream

N

et

Resp

iratio

n (

ER

-GP

P)

Site

SLIGO

PBCP

NERP

a.

0

50

100

150

0.1 1.0 10.0

Q (m3s

1)

% D

IC I

nput

from

Wate

rshed

(Soil

Resp

iratio

n +

Weath

ering)

b.

Smith and Kaushal (2015)

3. Implications for the Coastal Carbon Cycle?

Courtesy of ICPRB

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Year

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mg/L

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0 Potomac River − Washington, DC

Year

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/L)

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Chattahoochee River − Whitesburg, GA

Year

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alin

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/L)

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Alabama River − Claiborne, AL

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/L)

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Tombigbee River − Coffeeville, AL

Year

Alk

alin

ity (

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/L)

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1960 1970 1980 1990 20000

50

10

01

50

Peace River − Arcadia, FL

n

n

Year

Alk

alin

ity (

mg/L

)

Kaushal et al. (2013), ES&T

Increased Inorganic Carbon in Rivers

Land Use Change Increases

Carbon to Coastal Zones

Kaushal et al. (2014)

Links with Remote Sensing?

Evolution of sediment plumes in the Chesapeake Bay (2015)

Guangming Zheng, Paul M. DiGiacomo, Sujay S. Kaushal, Marilyn A. Yuen-Murphy, Shuiwang Duan

CONCLUSIONS

• Transport and transformation along an urban

watershed continuum (space and time)

• Long-term changes in coastal carbon cycle –

human-accelerated weathering and metabolism

• Links between remote sensing and coastal

biogeochemistry…exploring w/ NOAA

AcknowledgementsField Assistance

• Steve Hohman

• Jon Coplin

• Sofia D’Ambrosio

• Eric Stengle

Laboratory Assistance

• Metthea Yepsen

• Michael Evans

• Rebecca Plummer

• UMD Stable Isotope Laboratory

Funding Sources: NOAA, CICS, NSF, EPA