1 Water chemistry and nutrient cycling in tributaries of Lake Superior Amy Marcarelli Department of Biological Sciences 17 March 2014 Photos by A. Marcarelli or C. Huckins unless otherwise noted
Dec 16, 2015
1
Water chemistry and nutrient cycling in tributaries of Lake
Superior
Amy MarcarelliDepartment of Biological Sciences
17 March 2014
Photos by A. Marcarelli or C. Huckins unless otherwise noted
2
Coble et al. in review, J Geophy Res - Biogeosci
3
Stream Ecosystem Ecology @ Michigan Tech
Stream – GREAT Lake interactions
Year-round stream biogeochemistry – what
happens under all that snow?
A. Coble A. Coble
http://marcarelli-lab.bio.mtu.edu/
Monitoring Ecosystem Functions• Nutrient cycling• Material retention• Metabolism
Nutrient spiraling
Uptake Length (Sw)
Uptake Velocity (Vf)
Areal Uptake Rate (U)
𝑈=V f ×𝐶
6
Calumet and Wallace Lake – long term monitoring
http://www.nwss.mtu.edu/sites.html
For information on long-term data:
Dr. Robert [email protected]
7
Over the last 25 years at the Wallace watershed on Isle Royale, snowmelt has occurred more rapidly earlier in the growing season, resulting in less infiltration and higher runoff (A), concomitant with higher DOC concentrations in stream water (B).
For information on long-term data:
Dr. Robert Stottlemyer, [email protected]
8
Year-round measurements of nutrient uptake in a snowmelt-driven stream
A. A. Coble, A. M. Marcarelli, E. S. Kane
Discharge
Disch
arg
e (L
s-1
)
0
100
200
300
400
NH4
NH
4 V
f (mm
min
-1)
0
2
4
6
8
10
12
SRP
SR
P (m
m m
in-1
)
0
2
4
6
8
10
12
Detectable Vf Undetectable Vf
DOC
Ma
r M
ay
Se
p
No
v
Ma
r M
ay
Se
p
No
v
Ma
r M
ay
Se
p
No
v
Ma
r M
ay
Se
p
No
v
Jan
Jul
Jan
Jul
Jan
Jul
Jan
Jul
Jan
DO
C V
f (mm
min
-1)
0
2
4
6
8
10
12
2013 201420122011
Discharge
Disch
arg
e (L
s-1
)
0
100
200
300
400
NH4
NH
4 V
f (mm
min
-1)
0
2
4
6
8
10
12
SRP
SR
P (m
m m
in-1
)
0
2
4
6
8
10
12
Detectable Vf Undetectable Vf
DOC
Ma
r M
ay
Se
p
No
v
Ma
r M
ay
Se
p
No
v
Ma
r M
ay
Se
p
No
v
Ma
r M
ay
Se
p
No
v
Jan
Jul
Jan
Jul
Jan
Jul
Jan
Jul
Jan
DO
C V
f (mm
min
-1)
0
2
4
6
8
10
12
2013 201420122011
Sum
mer
Sum
mer
Sum
mer
Sum
mer
Win
ter
Win
ter
Win
ter
Does in-stream processing of N occur in winter? Discharge
Disch
arg
e (L
s-1
)
0
100
200
300
400
NH4
NH
4 V
f (mm
min
-1)
0
2
4
6
8
10
12
SRP
SR
P (m
m m
in-1
)
0
2
4
6
8
10
12
Detectable Vf Undetectable Vf
DOC
Ma
r M
ay
Se
p
No
v
Ma
r M
ay
Se
p
No
v
Ma
r M
ay
Se
p
No
v
Ma
r M
ay
Se
p
No
v
Jan
Jul
Jan
Jul
Jan
Jul
Jan
Jul
Jan
DO
C V
f (mm
min
-1)
0
2
4
6
8
10
12
2013 201420122011
Yes, Uptake Occurs in Winter Beneath Ice & Snow
Coble et al. in prep, Ecology
10
Restoration of the Salmon Trout River, and mechanistic linkages between in-stream fine
sediment and fluvial fishCasey Huckins, Amy MarcarelliPhD Students: Ashley Coble, Tony Matthys
around 1900:
~ over 100 coaster populations (Newman et al. 1999).
Lake Nipigon
Lake Superior
Nipigon Area
Salmon Trout River
Tobin HarborSiskiwit Bay
Currant RiverPancake River
Now:
scattered remnant populations (Hansen 1994), with small numbers (Huckins, et al. 2008)
Calumet0.003 m3 s-1
Little Huron 0.047 m3 s-1
Big Pup0.078 m3 s-1
Salmon Trout 0.786 m3 s-1
E. Br. Huron 0.180 m3 s-1
Little Garlic 0.098 m3 s-1
Fish Abundance(2004-2012)
2D Graph 2
Sampling Sites
Fis
h A
bund
ance
(in
div
iduals
*m-2)
0.0
0.1
0.2
0.3
0.4
0.5
Brook Trout Rainbow TroutCoho Salmon
Neighboring Rivers Salmon Trout River
Huckins et al. in prep
14
Salmon Trout River water quality monitoring, 2010-2014
2012
Te
mpe
rature (C
)
0
5
10
15
20
25
Dissolve
d Oxyg
en (%
Sa
turation
)
60
70
80
90
100
110
120
2013
Con
duc
tivity
(m
S /
cm
)
0.04
0.06
0.08
0.10
0.12
0.14
0.16
0.18
Marcarelli & Huckins unpublished
Nitrogen Uptake
Calumet
Little Huron
Big PupLittle Garlic
E. Branch Huron
Salmon Trout
NH
4 V
f (mm
min
-1)
0
2
4
6
8
10
12
20122013
ns 2012ns 2013 ns 2013
Coble et al. in prep – Limnol. Oceanogr.
[NH4] ug L-1
0 5 10 15 20 25
NH
4 Vf (m
m m
in-1
)
0
2
4
6
8 Salmon trout
2012
2013
16
Monitoring stream ecosystem function responses to stamp sand stabilization in Hills Creek
Collaborators: Casey Huckins, Gina Nicholas (Houghton-Keewenaw Conservation District), Rob Aho (USDA-NRCS)
Students: Ashley Coble, James Olson, Tony Matthys
Functions to be monitored:• Nutrient uptake• Particulate and dissolved retention• Nutrient uptake• Organic matter transfer to fishes
17
Map of the study streams; underlying imagery from July 2013. Note the large deposits of red-brown sand along Hills Creek and absence of similar deposition from Black Creek and the Gratiot River. Inset show the location of the study area relative to Lake Superior.
Gratiot RiverHills Creek
Black Creek
18
Organic matter transfer to fishes
Coarse particulate organic matter retention
Retention of dissolved materials in transient
storage
Nutrient uptake via nutrient spiraling
techniques
19
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
1.8
Black Creek Hills Creek -Reference
Hills Creek -Restoration
Hills Creek -Stamp Sand
Gratiot
NH4Uptake velocity (m
m / m
in)
notdetected
Ammonium uptake velocity measured using nutrient injections in study streams. The only reach with undetectable nutrient uptake in August 2013 was one dominated by stamp sands on Hills Creek.
Marcarelli, Huckins et al. unpublished
20
http://marcarelli-lab.bio.mtu.edu/
Photos by A. Marcarelli or C. Huckins unless otherwise noted
21
Name of Academic Institution
Person Presenting
Type of Monitoring Data (e.g., water quality, sediment sampling, species census, etc.)
Location(s) Where Data Collected
Time PeriodData Collected
Data Available Online? (provide web address)
Michigan Tech
Amy Marcarelli,
Water chemistry and nutrient cycling in tributaries of Lake Superior
Various streams in Houghton, Keweenaw, Marquette counties
One historic dataset for 1980 - current; others 2011-2014
Not currently