30
Weak links in communication contribute to harmful algal blooms in Lake Erie Laura Johnson, Rem Confesor, Dave Baker, Ken Krieger

Weak Links in Communication Contribute to Harmful Algal Blooms in Lake Erie - johnson

Embed Size (px)

Citation preview

Weak links in communication contribute to harmful algal

blooms in Lake Erie

Laura Johnson, Rem Confesor, Dave Baker, Ken Krieger

Algal blooms in Lake Erie have been increasing

May 2013 issue of National Geographic

2011 harmful algal bloom

6 largest algal blooms since mid-1990s have occurred over the past 7 years

Primarily Microcystis aeruginosa

Ohio P Taskforce 1

Toxins from the 2014 bloom shut down Toledo’s (pop 400,000) drinking water

2015 Seasonal HAB forecast

Current 2015 bloom on July 24

Photo: Darren Bade

Why are algal blooms returning to Lake Erie?

Heidelberg Tributary Loading Program

• Samples collected 3x a day• Analyzed for all major nutrients and

suspended sediments

Colorimetry for TP, DRP, TKN, NH4, Si

Ion chromatography for NO3, NO2, Cl, Fl, SO4

Suspended Sediments

Long-term trends in discharge and phosphorus

Annual discharge

• 5 year running average shows a marked increase since 2000

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

Dis

char

ge (

km3)

0

2

4

6

8

10

Maumee River

1975 1980 1985 1990 1995 2000 2005 20100.0

0.5

1.0

1.5

2.0

2.5

Sandusky River

1975 1980 1985 1990 1995 2000 2005 20100.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

Cuyahoga River

1975 1980 1985 1990 1995 2000 2005 20100.0

0.2

0.4

0.6

0.8

1975 1980 1985 1990 1995 2000 2005 2010

An

nual

FW

MC

(m

g/L)

0.0

0.2

0.4

0.6

0.8

1975 1980 1985 1990 1995 2000 2005 20100.0

0.2

0.4

0.6

0.8

1975 1980 1985 1990 1995 2000 2005 20100

200

400

600

800

1000

Sandusky River

r2 = 0.02P = 0.40

r2 = 0.04P = 0.29

r2 = 0.02P = 0.37

Annual total particulate P

1975 1980 1985 1990 1995 2000 2005 2010

An

nual

Loa

d (m

etric

to

ns)

0

1000

2000

3000

4000

Maumee River

r2 = 0.25P = 0.002

r2 = 0.20P = 0.01

1975 1980 1985 1990 1995 2000 2005 20100

100

200

300

400

500

600Cuyahoga River

5 yr running mean

LOAD CONCENTRATION

Suspended Sediments

• Sediments suspended in the water has decreased!

• Patterns are more apparent when corrected for weather variability

1975 1980 1985 1990 1995 2000 2005 2010TS

S lo

ad (

1000

met

ric to

ns)

0

500

1000

1500

2000

2500

1975 1980 1985 1990 1995 2000 2005 2010

TS

S F

WM

C (

mg/

L)

0

100

200

300

400

500

1975 1980 1985 1990 1995 2000 2005 2010D

isch

arge

(km

3)

0

2

4

6

8

10

1975 1980 1985 1990 1995 2000 2005 2010TS

S lo

ad (

1000

met

ric to

ns)

0

100

200

300

400

500

600

700

1975 1980 1985 1990 1995 2000 2005 2010

TS

S F

WM

C (

mg/

L)

0

100

200

300

400

500

600

1975 1980 1985 1990 1995 2000 2005 2010

Dis

char

ge (

km3)

0.0

0.5

1.0

1.5

2.0

2.5

r2=0.11, p=0.04

r2=0.24, p=0.003Maumee

Sandusky

CONCENTRATION

Richards et al., 2009 JSWC

1975 1980 1985 1990 1995 2000 2005 20100

50

100

150

200

250

Sandusky River

r2=0.45P<0.001

1975 1980 1985 1990 1995 2000 2005 20100.00

0.02

0.04

0.06

0.08

0.10

0.12

0.14

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

Lo

ad (

me

tric

ton

s)

0

200

400

600

800

1000

Maumee River

r2=0.35P<0.001

1975 1980 1985 1990 1995 2000 2005 2010A

nnu

al F

WM

C (

mg/

L)

0.00

0.02

0.04

0.06

0.08

0.10

0.12

0.14

1975 1980 1985 1990 1995 2000 2005 20100

20

40

60

80

100

120

Cuyahoga River

1975 1980 1985 1990 1995 2000 2005 20100.00

0.02

0.04

0.06

0.08

0.10

0.12

0.14

Annual dissolved P

LOAD CONCENTRATION

Why did dissolved phosphorus increase?

Average soil test P (Mehlich 3 P)

• Over 1500 farms sampled throughout the Sandusky River Basin

• Most farms within the maintenance range

• Only 10% of the farms were above 71ppm

• P has accumulated on the surface

Evidence of macropore tile drain flow

Photos: Kevin King, USDA-ARS Edge of Field Research

Evidence of macropore tile drain flowData from Doug Smith, USDA-ARS

St. Joseph River watershed

14 May 2011

• Tile drain flow peaked with surface flow at in a May 2011 storm • Data from Kevin King, USDA-ARS around the basin shows 50-80% of the dissolved P

loading is from tile drains

Smith et al. 2014, JEQ

Intense precipitation (2”+) is increasing

8 Events in 16 Years!

20 Events in 16 Years

Data from Kevin King, USDA-ARS

Common misconceptions

Found in Media• Tile drains do not deliver

phosphorus– Article in Journal Sentinel

• Filter strips help with dissolved phosphorus– Former Ohio Representative Chris

Redfern

– Pennsylvania NPR

• Combined sewage overflows contribute a majority of the phosphorus– Toledo Blade

• Farmers are carelessly over applying fertilizer, applications rates have increased

Weak links in communication contribute to harmful algal

blooms in Lake Erie

• Concern over the link between increasing dissolved P exports and HABs in Lake Erie have been discussed since 2007

• Studies in the 1970s showed P loss in tile drains• A report in 1980 warned of the potential tradeoffs in

the Lake Erie watershed of switching to conservation no till

• Yet misconceptions on P runoff are still prevalent• How can we expect a solution?

How can we expedite knowledge transfer?Can we make progress without a disaster?

• WLEB 4R retailer certification program– 16 certified nutrient service providers that cover ~1000 farmers,

50 applications, nearly 10% of the basin covered already

• Ohio fertilizer application training– Required for all who apply nutrients to over 50 acres

– 6586 people have attended training sessions since last fall

• WLEB tri-state RCPP– $17.5 million to the WLEB for incentives

• County SWCDs and NRCS• Webpages

– LakeErieAlgae.com just launched

• Field days, lab tours, media interviews

Questions?

For more information visit: http://www.heidelberg.edu/NCWQR

Or contact me at [email protected]

http://www.facebook.com/NCWQR

Maumee River spring 2015

Annual nitrate-NNitrate-N

Annual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

FW

MC

(m

g/L

)

0

2

4

6

8

10

Total Kjeldahl NitrogenAnnual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

FW

MC

(m

g/L

)

0

1

2

3

Annual Nitrate-N Load

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ua

l Lo

ad (

met

ric t

ons)

0

20000

40000

60000

Ann

ual D

ischarge

(10

6 m3)

0

2000

4000

6000

8000

10000

12000

LoadDischarge

Annual Total Kjeldahl Nitrogen Load

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

An

nu

al L

oad

(m

etric

ton

s)

0

5000

10000

15000

20000 Ann

ual D

ischarge

(10

6 m3)

0

2000

4000

6000

8000

10000

12000

LoadDischarge

5y running average

Nitrate-NAnnual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

FW

MC

(m

g/L

)

0

2

4

6

8

10

12

Total Kjeldahl NitrogenAnnual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

FW

MC

(m

g/L

)

0.0

0.5

1.0

1.5

2.0

2.5

Annual Nitrate-N Load

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

Lo

ad (

met

ric t

ons)

0

2000

4000

6000

8000

10000 Ann

ual D

ischarge

(10

6 m3)

0

500

1000

1500

2000

2500

Annual Total Kjeldahl Nitrogen Load

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

Lo

ad (

met

ric t

ons)

0

500

1000

1500

2000

2500

3000

3500 Ann

ual D

ischarge

(10

6 m3)

0

500

1000

1500

2000

2500

LOAD CONCENTRATION

MA

UM

EE

SA

ND

US

KY

Nitrate-NAnnual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

FW

MC

(m

g/L

)

0

2

4

6

8

10

Total Kjeldahl NitrogenAnnual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

FW

MC

(m

g/L

)

0

1

2

3

Annual Nitrate-N Load

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ua

l Lo

ad (

met

ric t

ons)

0

20000

40000

60000

Ann

ual D

ischarge

(10

6 m3)

0

2000

4000

6000

8000

10000

12000

LoadDischarge

Annual Total Kjeldahl Nitrogen Load

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

An

nu

al L

oad

(m

etric

ton

s)

0

5000

10000

15000

20000 Ann

ual D

ischarge

(10

6 m3)

0

2000

4000

6000

8000

10000

12000

LoadDischarge

Nitrate-NAnnual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

FW

MC

(m

g/L

)

0

2

4

6

8

10

12

Total Kjeldahl NitrogenAnnual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

FW

MC

(m

g/L

)

0.0

0.5

1.0

1.5

2.0

2.5

Annual Nitrate-N Load

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

Lo

ad (

met

ric t

ons)

0

2000

4000

6000

8000

10000 Ann

ual D

ischarge

(10

6 m3)

0

500

1000

1500

2000

2500

Annual Total Kjeldahl Nitrogen Load

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

Ann

ual

Lo

ad (

met

ric t

ons)

0

500

1000

1500

2000

2500

3000

3500 Ann

ual D

ischarge

(10

6 m3)

0

500

1000

1500

2000

2500

Nitrate-NAnnual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

An

nu

al F

WM

C (

mg/

L)

0

2

4

6

8

10

r2=0.387,P=0.004,m=-0.16

Nitrate-NAnnual Flow-Weighted Mean Concentration

Water Year

1975 1980 1985 1990 1995 2000 2005 2010

An

nu

al F

WM

C (

mg/

L)

0

2

4

6

8

10

12

r2=0.391,P=0.004,m=-0.18

Annual nitrate-NLOAD CONCENTRATION

MA

UM

EE

SA

ND

US

KY

Toledo drinking water crisis• Over 400,000 people had no drinking water for 3 days (Aug 4-6)• Microcystin toxin was above World Health Organization’s limit of 1 mg/L

31 July 2014 3 Aug 2014

• Journal Sentinel http://www.jsonline.com/news/wisconsin/toxic-algae-cocktail-brews-in-lake-erie-b99344890z1-274542731.html

Journal Sentinel Thorbahn says the pipe he's laying actually alleviates the phosphorus problem because it allows water that hits the crops to first be filtered through the soil. He says water coming straight off the surface of the fields, instead of flowing down to the tiles, is more likely to be contaminated with excess fertilizer

"It's surface runoff," he says, referring to how agriculture contributes to the phosphorus problem in the lake. "It's not the tile system."

http://www.alleghenyfront.org/story/ohio-farmers-point-algae-law-loopholeThe Allegheny Front, Radio show

Bouncing along the edge of head-high corn fields in an electric golf cart, 65-year-old, fourth-generation Ohio farmer Roger Wise is showing off grass-covered filter strips that wind for miles along Wolf Creek, a small tributary of the Sandusky River less than 10 miles from Lake Erie.

"We have a buffer between the corn and the crick over there," says Wise. "There's a lot of wildlife back here. It's primarily wildlife and water retention and conservation.

Filter strips, paid for by federal conservation programs, are just one way to help curb phosphorous runoff.

http://www.toledonewsnow.com/story/26263076/sewage-overflow-during-monday-storms-can-intensify-algae-problemWTOL August 2014

A gentle rain would have been great, because it has been very dry, but the downpour like we had creates sewage overflows," explained Lake Erie Waterkeeper Sandy Bihn.

http://www.npr.org/sections/thesalt/2014/08/08/338936920/lake-eries-toxic-bloom-has-ohio-famers-on-the-defensive

Harmful algal blooms (HABs) in the western Lake Erie basin (WLEB) garnered national attention in August 2014 when microcystin toxins exceeded World Health Organization limits in Toledo’s drinking water resulting in a 3-day ban on drinking tap water. Yet the recurrence of HABs in the WLEB have been an on-going problem for many years– the first Ohio Lake Erie Phosphorus Task Force was formed in 2007. Increases in HAB intensity and extent over the past decade correspond closely to increasing dissolved phosphorus (DP) loads to Lake Erie from the agricultural Maumee River. The uptick in DP exports followed a period of intense land management change in the 1980s aimed at reducing soil erosion through conservation tillage and reserves. While this program succeeded in decreasing both suspended sediment and particulate P concentrations in the Maumee River, it encouraged use of broadcast P fertilizer and enhanced soil P stratification. Thus, increased DP runoff is the product of these unintended consequences in combination with intensified subsurface drainage installation, increased soil compaction, and increasing extreme spring weather events. Although other sources (wastewater inputs, residential fertilizer use, failing septic tanks) are acknowledged as minor contributors of P, producers are largely blamed for the events in Toledo. Based on the media coverage following Toledo’s drinking water incident, there appears to be a knowledge gap among producers regarding how and what form of P is entering Lake Erie, which influences how producers reduce P loss. Thus the current state of the lake is partly due to weak or slow communication among researchers/educators and the agricultural community. Our biggest challenge is to better disseminate accurate information to the agricultural community that results in implementation of practices focused on DP runoff and to foster flexibility in adopting new practices as our understanding improves or the pollutant of concern evolves.