specific conductivity in streams and rivers of the

20
Specific conductivity in streams and rivers of the Delaware River Basin 17 May 2020 Online MWS and sensor station owner Workshop Presenter: Diana Oviedo-Vargas, PhD Assistant Research Scientist

Upload: others

Post on 26-Jul-2022

1 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Specific conductivity in streams and rivers of the

Specific conductivity in streams and rivers of the

Delaware River Basin

17 May 2020

Online MWS and sensor station owner Workshop

Presenter:

Diana Oviedo-Vargas, PhD

Assistant Research Scientist

Page 2: Specific conductivity in streams and rivers of the

Electric conductivity (conductance)

• Measurement of the capacity of water to conduct an electric current as a result of the movement of ions through the solution. It depends on:

• Temperature

• Amount of dissolved ions

• What your sensor measures is Specific conductivity, already corrected for temperature (25 ºC)

• Units are (micro- mili-) Siemens per centimeter (S/cm)

• https://pubs.usgs.gov/tm/09/a6.3/tm9-a6_3.pdf

Page 3: Specific conductivity in streams and rivers of the

Electric conductivity (conductance)

• Regularly measured during laboratory and field experiments by aquatic scientists as a rapid indicator of water chemistry and water quality.

• Often measured continually at USGS stream gauges

• https://waterdata.usgs.gov/nwis/rt

Page 4: Specific conductivity in streams and rivers of the

Specific conductivity (SC)

• Depends on the amount of dissolved ions in the water

• Concentration: mass of solute per unit of volume (e.g., mg/L)

• Ions: atoms or molecules with a charge (positive, negative), salts.

• NaCl, sodium chloride

Page 5: Specific conductivity in streams and rivers of the

Specific conductivity (SC)

• Many more ions besides Na and Cl in natural waters:

Major Cations Formula

Calcium Ca2+

Magnesium Mg2+

Potassium K+

Sodium Na+

Major Anions Formula

Bicarbonate/carbonate HCO3-/CO3

2-

Sulfate SO42-

Chloride Cl-

Silicate HSiO3-

Page 6: Specific conductivity in streams and rivers of the

Natural Specific Conductivity in the US

Olson, J.R. and Cormier , S.M., 2019. Modeling Spatial and Temporal Variation in Natural Background Specific Conductivity. ES&T, 53.

Page 7: Specific conductivity in streams and rivers of the

Natural Specific Conductivity in the DRB

Olson, J.R. and Cormier , S.M., 2019. Modeling Spatial and Temporal Variation in Natural BackgroundSpecific Conductivity. ES&T, 53.

Page 8: Specific conductivity in streams and rivers of the

DRWI study sites land-use

0%

10%

20%

30%

40%

50%

60%

70%

80%

90%

100%

1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 37 39 41 43 45 47 49

Other natural

Developed

Agriculture

Forested

Land use data from the National Land Cover Database 2011 (NLCD2011)

Page 9: Specific conductivity in streams and rivers of the

Specific conductivity (µS/cm)

• All available data in 2017-2018

Rocky Run at Marriott

Hurricane Run at Woodland Road

Page 10: Specific conductivity in streams and rivers of the

Specific conductivity (µS/cm)

• All available data in 2017-2018

Rocky Run at Marriott

Hurricane Run at Woodland Road

Page 11: Specific conductivity in streams and rivers of the

Specific conductivity and land use

• % developed land in the WS was the best land-use predictor of mean SC across the study period

• For sites with highest mean SC, it was best explained by % highly developed land-use

0

200

400

600

800

1000

1200

1400

1600

0 20 40 60 80 100

Me

an

SC

S/c

m)

% Developed land

0

200

400

600

800

1000

1200

1400

1600

0 5 10 15

Me

an

SC

(uS

/cm

)

% Highly developed

r = 0.76, p<0.01 r = 0.81, p<0.01

Page 12: Specific conductivity in streams and rivers of the

Seasonal trends: forested streams

• 80% Forested

• Highest in summer – drier, no groundwater dilution with low-conductivity surface water

• Frequent low extremes, no high extremes

Aquashicola Creek, Monroe Co, PA 17 km2

100

150

200

250

Fall Spring Summer WinterSeason

SC

(u

S/c

m)

Page 13: Specific conductivity in streams and rivers of the

Seasonal trends: urban streams

• 71% Urban

• Much higher SC relative to forested and agricultural

• Extreme SC in the winter but also in the fall and spring

0

3000

6000

9000

Fall Spring Summer WinterSeason

SC

(u

S/c

m)

Naylors Run, Delaware Co, PA, 7 km2

Page 14: Specific conductivity in streams and rivers of the

0

100

200

300

0

500

1000

1500

Jul 2018 Oct 2018 Jan 2019 Apr 2019Date

SC

(u

S/c

m) D

ep

th (m

m)

Depth (mm)

SC (uS/cm)

0

3000

6000

9000

12000

0

10000

20000

30000

40000

Jul 2018 Oct 2018 Jan 2019 Apr 2019Date

SC

(u

S/c

m) D

ep

th (m

m)

Depth (mm)

SC (uS/cm)

Aquashicola Creek (Forested)

Page 15: Specific conductivity in streams and rivers of the

0

3000

6000

9000

12000

0

500

1000

1500

2000

Jul 2018 Oct 2018 Jan 2019 Apr 2019Date

SC

(u

S/c

m) D

ep

th (m

m)

Depth (mm)

SC (uS/cm)

0

100

200

300

0

500

1000

1500

Jul 2018 Oct 2018 Jan 2019 Apr 2019Date

SC

(u

S/c

m) D

ep

th (m

m)

Depth (mm)

SC (uS/cm)

0

3000

6000

9000

12000

0

10000

20000

30000

40000

Jul 2018 Oct 2018 Jan 2019 Apr 2019Date

SC

(u

S/c

m) D

ep

th (m

m)

Depth (mm)

SC (uS/cm)

Naylors Run (Urban)

Aquashicola Creek (Forested)

Page 16: Specific conductivity in streams and rivers of the

Salinization of freshwater

Brandywine Town Center, winter 2018 Road salt pile

• Sources of ions to freshwaters:

• Natural: soils and geology

• Anthropogenic:

• GW extraction->Salt water intrusion

• Irrigation and fertilizer application

• Mining

• Demineralization of concrete

• Road salt application

• Sewage and industrial waste discharge

REF: Kaushal, S.S., Likens, G.E., et al. 2018. Freshwater salinization syndrome on a continental scale. PNAS, 115

Page 17: Specific conductivity in streams and rivers of the

Salinization of freshwater

• Environmental implications of are still poorly understood.

• Symptoms can include changes in biodiversity due to osmotic stress and desiccation.

• Emerging threat to freshwater biodiversity

Source: https://www.haikudeck.com/streams--rivers-science-and-technology-presentation-V85aFFyFRe#slide5

• Kaushal, S.S., Likens, G.E., et al. 2018. Freshwater salinization syndrome on a continental scale. PNAS, 115 • Reid, A.J., Carlson, A.K., et al. 2019. Emerging threats and persistent conservation challenges for freshwater biodiversity. Biol Revs, 94

Page 18: Specific conductivity in streams and rivers of the

Potential effects on stream health

• Linear model that predicts SC at which 5% of benthic invertebrate genera will be extirpated (XCD05)

• 95% will be protected

• Based on background SC

Cormier, S.M., Zheng, L. and Flaherty, C.M., 2018. A field-based model of the relationship between extirpation of salt-intolerant benthic invertebrates and background conductivity. Science of The Total Environment, 633

• Background SC ~ 300 uS/cm

• XCD05 ~ 500 uS/cm

Olson, J.R. and Cormier , S.M., 2019. Modeling Spatial and Temporal Variation in Natural Background Specific Conductivity. ES&T, 53.

Page 19: Specific conductivity in streams and rivers of the

In summary:

• Some tributaries of the DRB are experiencing increased salinity likely affecting stream biota.

• Related to land use, urbanization • Winter extremes likely

related to road salt application

• Increased SC year-around in agricultural and urban streams

Page 20: Specific conductivity in streams and rivers of the

Acknowledgments

• Collaborators: • Marc Peipoch

• John Jackson

• David Bressler

• David Arscott

• Charlie Dow