Title: Lake Ecology
1Lake Ecology
- Unit 1 Modules 2/3 Part 6 ManagementJanuary
2004
2Modules 2/3 overview
- Goal Provide a practical introduction to
limnology - Time required Two weeks of lecture (6 lectures)
and 2 laboratories - Extensions Additional material could be used to
expand to 3 weeks. We realize that there are far
more slides than can possibly be used in two
weeks and some topics are covered in more depth
than others. Teachers are expected to view them
all and use what best suits their purposes.
3Modules 2/3 outline
- Introduction
- Major groups of organisms metabolism
- Basins and morphometry
- Spatial and temporal variability basic physical
and chemical patchiness (habitats) - Major ions and nutrients
- Management eutrophication and water quality
46. Management topics
- Trophic status
- Eutrophication
- Water quality
5Nutrients most limiting to algal growth
- Phosphorus
- Essential for growth
- PO4-3 is primary dissolved form
- PO4-3 sticks to soil and sediment particles
- Usually key nutrient for triggering excess plant
growth - Must be reduced to control eutrophication
- 1 lb (kg) P can yield 500 lbs (kg) fresh algae
- Nitrogen
- Essential for growth
- NO3-, NH4, and N2 are primary biological forms
- NO3- soluble in water
- May limit algal growth in some circumstances
- More difficult to remove from wastewater than P
- Some forms are toxic or disease-causing to fish
and mammals (including humans)
6Limiting nutrients demand versus supply
- Nitrogen and phosphorus are typically in
extremely short supply in water relative to plant
demand - The Redfield ratio is the average composition
of elements in phytoplankton - Ratio 100DW40C7N1P
7The concept of limiting nutrients
- Liebigs Law of the Minimum (1840)
- An organisms total biomass yield is proportional
to the lowest concentration of nutrient relative
to the requirements of that organism
(paraphrased). - Lake managers are interested in limiting
nutrients because - An increase might change water quality or food
webs. - Restoration often requires a strategy for
reducing nutrient loading and predictions of the
consequences of specific actions.
8Limiting nutrients a conceptual example
- The following set of slides were developed to
illustrate more specifically what is meant by
limiting nutrients in the context of
eutrophication studies - This may be appropriate for a lab exercise in
which different combinations of N and P are added
to lake water - Lake Superior was used as an example because we
can see it out our window and because it is the
biggest lake in the world and the cleanest of the
Laurentian Great Lakes, so it is important to
understand
9Example loosely based on Lake Superior
10Conceptual nutrient limitation bioassay 1
- This example is loosely based on Lake Superior
- 1. Algal composition is approximately
- 500 g wet weight 100 g dry weight 40 g C 7
g N 1 g P
Remember that the ratio of CNP is called the
Redfield ratio and approximates the composition
of algae! 4071 by weight 100161 by atoms
11Conceptual nutrient limitation bioassay 2
- 2. Mid-summer bioavailable water chemistry
- Dissolved inorganic carbon (DIC)
- 10,000 µg C/L (as carbon dioxide and
bicarbonate) - Dissolved inorganic nitrogen (DIN)
- 300 µg N/L (95 as nitrate, with very low
ammonium) - Dissoved inorganic phosphorus (ortho-P, DIP)
0.5 µg P/L
12Conceptual nutrient limitation bioassay 3
- 3. Assume
- Algal biomass B0 200 µg C/L (particulate)
- Algal maximum growth rate 20 per day
13Conceptual nutrient limitation bioassay 4
- 4. Run a nutrient enrichment experiment to
estimate the limiting nutrient by doubling each
nutrient - Set up 4 liter bottles of lake water in
triplicate -
- Incubate for 1 day and re-measure algal biomass
(Bf)
14Conceptual nutrient limitation bioassay 5
- 5. What happens?
- After 1 day algae grow 20 X 200 µg C/L 40
µg C/L - Apply the Redfield Ratio to estimate nutrient
needs
- Is there sufficient DIC to support this much
growth? - Is there sufficient DIN to support this much
growth? - Is there sufficient DIP to support this much
growth?
15Conceptual nutrient limitation bioassay 6
- 6. What happened?
- 40 µg C/L of new growth would require
- 40 µg DIC/L 7 µg DIN/L 1 µg DIP/L
- 0 control treatment
- 10,000 µg DIC/L is much more than enough
- 300 µg DIN/L is more than enough (293 excess)
- 0.5 µg DIP/L is half of what is needed
- Therefore growth is 50 of maximum
- 20 µg C/L
16Conceptual nutrient limitation bioassay 6
- 6. What happened?
- 40 µg C/L of new growth would require
- 40 µg DIC/L 7 µg DIN/L 1 µg DIP/L
- N treatment
- 10,000 µg DIC/L is much more than enough
- 600 µg DIN/L is more than enough (593 excess)
- 0.5 µg DIP/L is half of what is needed
- Therefore growth is 50 of maximum
- 20 µg C/L
17Conceptual nutrient limitation bioassay 6
- 6. What happened?
- 40 µg C/L of new growth would require
- 40 µg DIC/L 7 µg DIN/L 1 µg DIP/L
- C treatment
- 20,000 µg DIC/L is much more than enough
- 300 µg DIN/L is more than enough (293 excess)
- 0.5 µg DIP/L is half of what is needed
- Therefore growth is 50 of maximum
- 20 µg C/L
18Conceptual nutrient limitation bioassay 6
- 6. What happened?
- 40 µg C/L of new growth would require
- 40 µg DIC/L 7 µg DIN/L 1 µg DIP/L
- P treatment
- 10,000 µg DIC/L is much more than enough
- 300 µg DIN/L is more than enough (293 excess)
- 1.0 µg DIP/L is just what is needed
- Therefore growth is 100 of maximum
- 40 µg C/L
19Nutrient bioassay summary and plot
- An enrichment of only 0.5 µg P/L doubled algal
growth - It would take a depletion of 43 µg P/L to deplete
the 300ug DIN/L, based on the 71 ratio - The DIC is virtually inexhaustible in all lakes.
- It may briefly limit algal growth in
hypereutrophic sewage oxidation ponds - The data suggest strong P-limitation for Lake
Superior
20Nutrient limitation bioassay responses
21Halsteds Bay late summer mixing events
- What might this mean for phosphorus levels in the
water column? - Why?
22Medicine Lake Algal blooms mixing events - 1
- Background
- Medicine Lake is extremely productive because of
historically high nutrient enrichment from its
watershed - (go to http//lakeaccess.org/lakedata/lawnfertiliz
er/mainlawn.htm) - Major blooms of algae can be detected in the
RUSS data set as - supersaturated O2 (why ?)
- increased pH (why ?)
- increased chlorophyll-a or turbidity (why ?)
23Medicine Lake Algal blooms mixing events-2
Color O2 Line pH
STRATIFY
RE- STRATIFY
MIX
MIX
24Halsteds Bay Algal blooms mixing events- 3
Why did the phosphorus in the bottom water drop
so dramatically in August 1999 in Halsteds Bay ?
P levels drop
25Halsteds Bay Algal blooms mixing events- 4
- First, focus on the ice-free season water quality
- relatively high epilimnion (surface)TP 75-150
ugP/L - chlor-a (algae ) builds up steadily to levels gt
50 ug/L
26Halsteds Bay Algal blooms mixing events- 5
See how secchi drops as chlorophyll increases ?
27Halsteds Bay Algal blooms mixing events- 6
Now see how much TP is in the hypolimnion
28Halsteds Bay Algal blooms mixing events- 7
Summary slide without animation
29Medicine Lake Storm mixing events
- This sequence runs from 1-5 from Aug 29-30, 1999
30Trophic status classification
- This topic will be developed further in Module
22 (Regulations and Compliance Monitoring - Lake
Biocriteria) - Managers need to classify lakes to set water
quality standards and prioritize monitoring,
research, and restoration . - Lake productivity, as indicated by its
production of algal biomass, is a useful
classification in regard to water quality issues
as well as fisheries management - Trophic status indices usually assume that
nutrient levels (e.g. total-P) control algal
biomass (measured by chlorophyll-a) which in turn
regulates lake clarity (Secchi disk transparency)
31Trophic Status
- Carlson trophic state index (TSI)- most widely
used - based on log transformation of Secchi disk
values as a measure of algal biomass on a scale
from 0 110 - 10 units doubling of algal biomass
- TSIs also developed for chlor-a and total-P
based on their relationships to secchi for a set
of midwestern lakes - TSI useful for comparing lakes within a region
and for assessing changes in trophic status over
time - Time period usually summer often set at June
15 Sep 15 but it is rarely a good idea to
restrict data acquisition without a good reason
especially Volunteer secchi data
32Carlson TSI equations
- TSI-S 60 - 14.41 ln Secchi disk, m
- TSI-C 9.81 ln Chlor-a, µg/L 30.6
- TSI-P 14.42 ln TP, µg/L 4.15
- Average TSI TSI-P TSI-C TSI-S / 3
- If the 3 TSI values are not similar to each
other, it is likely that - algae may be light- or nitrogen-limited instead
of P-limited, or - secchi is affected by erosional silt rather than
by algae, or something else. One should look
deeper into the data! - Note that Dr. Carlson recommended not averaging
the 3 values to avoid obscuring important
differences
33Carlson TSI vs water quality
lt40 Oligotrophic clear water high hypolimnetic O2 year-round but possible anoxia in the deeper hypolimnion part of year
40-50 Mesotrophic moderately clear water possible hypolimnetic anoxia in summer and/or under ice. Fully supportive of all swimmable /aesthetic uses possible cold-water fishery
50-60 Mildly eutrophic decreased secchi anoxic hypolimnion possible macrophyte problems warm-water fishery supportive of all swimmable /aesthetic uses but threatened
60-70 blue-green algal dominance with scums possible extensive macrophyte problems not supportive of all beneficial uses
gt70 Heavy blooms and scums in summer likely dense weed beds hypereutrophic possible fish kills fewer plant beds due to high algae not supportive of many beneficial uses
34TSI (Carlson) - graphical
35What are Ecoregions ?
- Areas with similar
- Climate
- Landuse
- Soils
- Topography
- Potential natural vegetation
- Minnesota has seven major ecoregions
- Four ecoregions contain most of the lakes
- Water quality varies greatly from south to north
36Minnesotas Ecoregions
371.6-3.3 ft
38Comparison of trophic indicators in Minnesota
TP (ug/L) TP (ug/L) TP (ug/L) Chlor-a (ug/L) Chlor-a (ug/L) Chlor-a (ug/L) Secchi (m) Secchi (m) Secchi (m) TSI (Carlson) TSI (Carlson) TSI (Carlson)
Trophic Status O M E O M E O M E O M E
Standard Criteria lt11 11- 24 gt24 lt3 3- 7 gt7 gt4.0 4.0- 2.2 lt2.2 lt35 40-55 gt55
NLF 14 - 27 14 - 27 14 - 27 lt 10 lt 10 lt 10 2.4 - 4.6 2.4 - 4.6 2.4 - 4.6 41 - 52 41 - 52 41 - 52
NCHF 23-50 23-50 23-50 5 - 22 5 - 22 5 - 22 1.5 3.2 1.5 3.2 1.5 3.2 49 - 66 49 - 66 49 - 66
WCB 65 - 150 65 - 150 65 - 150 30 - 80 30 - 80 30 - 80 0.5 1.0 0.5 1.0 0.5 1.0 67 - 77 67 - 77 67 - 77
NGP 130 - 250 130 - 250 130 - 250 30 - 55 30 - 55 30 - 55 0.3 1.0 0.3 1.0 0.3 1.0 67 - 73 67 - 73 67 - 73
O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994. O oligotrophic M mesotrophic E eutrophic see slide notes and accompanying slide for Minnesota Ecoregions map and code names General values from Axler et al. 1994.
39TSI Trends in Minneapolis, MN area WOW Lakes
Note importance of flagging which TSI is plotted
and leaving space for missing years
Solid barsTSI average for TP, chlor and secchi
striped secchi only
How would you determine how well the TSI- secchi
alone (stripes) predicts average TSI or TSI-
chlor ?
40Chlor-a - TP and Secchi TP relationships in MN
Notice that lake clarity is much more
sensitive to increased phosphorus at the low end
of the scale. Why ?
Data from Minnesota Pollution Control Agency Year
2000 Lake Assessment report (www.pca.state.mn.us)
41Ex Halsteds Bay late summer mixing events
- Run the color mapper from April 1999 through 2002
focusing on storm events in mid August 1999 and
2000 - START with MAP TEMP and plot DO to show
variable stratification - Then switch to MAP DO and PLOT TEMP to show
anoxic events and discuss the release of P from
sediments that swamps annual P-inflow from the
watershed
42Hypolimnion responses to increasing productivity
Trophic Status O2 PO4-3 NH4 H2S Fe2 (ferrous)
Oligotrophic High (mostly) Low Low Absent Absent
Mesotrophic Low partly anoxic Low High if anoxic Moderate High if anoxic Absent Present where anoxic
Eutrophic Anoxic High High High High
43Hypolimnion responses to anoxia
- As the hypolimnion becomes O2 depleted
- NH4 accumulates
- increased organic matter is decomposing
- cannot be converted to NO3- without 2
(bacterial nitrification) - not much algal uptake (its dark and anoxic)
- Insoluble oxidized Fe3 (ferric) at sediment
surface is reduced to Fe 2 (ferrous) that is
soluble the phosphate adsorbing layer dissolves - PO4-3 diffusion from the sediments increases
dramatically - Increasing decomposition leads to strong
reducing conditions that favor bacterial
reduction of sulfate to sulfide - producing
rotten egg gas (H2S) - Mixing adds lots of available N P to the
sunlit zone ALGAE !!
44Eutrophication and water quality
45Trophic (feeding metabolism) terminology
Oligotrophic low nutrients and productivity
usually high clarity
Mesotrophic moderate nutrients, productivity
and clarity
Eutrophic high nutrients and productivity
low clarity
46Eutrophication Excess fertility leading to
excessive plant growth
47Water Quality Impacts- Eutrophication (some of
them)
- excess algae scums, noxious blue-greens,
taste/odor/smell
- O2 depletion loss of fish habitat
- loss of clarity (secchi depth) aesthetic loss
- excess macrophyte (weed) growth- loss of open
water favors exotic species (EWM) sediment
destabilization
48Water Quality Impacts- Eutrophication (and some
more)
- loss of native macrophytes from algal shading
loss of fish waterfowl habitat and food
reduced shoreline bottom stabilization,
increased erosion
- lower bottom O2 increased sediment nutrient
release loss of fish habitat
- excess organic matter smothers eggs and bugs
49Eutrophication natural vs cultural
- Natural filling by mineral and organic sediment
leads to lower V and larger AwA0 and A0V - Lake to wetland conversion
- Time scale gt 103 years (if at all)
- Irreversible
- Human-caused from excess nutrient inputs and poor
land-use management - Water quality degraded loss of beneficial uses
- Time scale lt decades
- Reversible loading
50Eutrophication the sad Lake Tahoe story
Data courtesy of C.R. goldman and J.E. Reuter,
Tahoe Reesrach Group, U. of California-Davis,
http//www.news.ucdavis.edu/tahoetv/
51Other regulators of lake productivity - Grazing
- Top-down Model
- High rates of nutrient driven algal growth is
removed by intense zooplankton grazing pressure
(usually cladoceran Daphnids) - Fishless lakes with low zooplankton predation
- Lakes where planktivorous fish are regulated by
predatory fish (game fish) usually by intensive
control - In these cases, algae are not nutrient limited
- management tool biomanipulation
- Bottom-up Model
- Nutrient inputs drive algal growth
- Classic Pyramid
52Potential Top-down effects on food chains
Low Predators
HIGH Predators
HIGH Planktivores
Low Planktivores
HIGH Zoops
Low Zoops
Smaller Zoops less grazing
Larger Zoops more grazing
HIGH Algae
Low Secchi O2 stress high pH ??
Low Algae
Higher Secchi less O2 stress lower pH ??
53Biomanipulation fish management
- Fish control
- Intensive netting
- Rotenone (poison)
- Stock increased s of piscivorous fish
- Selective catch or catch restrictions
- Control conditions for fish and zoop growth and
survival
54Biomanipulation- Summary
- Summary
- Considered experimental
- Requires complex knowledge of food web processes
(shallow lakes are particularly poorly
understood) - Herbivores may not consume certain blue-greens
- May be more successful in lakes without
large-bodied zooplankton - May require external loading to also be
controlled - Currently considered only a management tool- not
a restoration technique
55Lake Mendota Biomanipulation Project
- Lake Mendota large, urban, limnologically
famous lake in Madison, WI - Eutrophic with blooms of blue-green algae
- Sewage effluents diverted out of basin entirely
by 1971 - Continued nonpoint pollution from agricultural
and urban runoff - 1987 attempt to control blooms by a massive
stocking of walleye to reduce planktivorous fish
- 1988 hot summer causes summerkill of Ciscos,
the major planktivore - zoops increase and algae decrease for few years
- Ciscos recover, anglers hammer the walleye,
zoops decrease and algae are back
56Other lake productivity regulators light shading
- Nutrients arent always the whole story
- Shallow lake research
- Aquatic plants vs algae
- Over a wide range of nutrients there are
alternative stable states of dominance - Plants shade phytoplankton creating clearwater
- Phytoplankton turbidity shades plants and
restricts growth to nearshore - Periphyton mats and mucky sediments hinder plant
rooting - High densities of grazers regulate periphyton on
leaves
57Water transparency clear vs turbid state
Water transparency clear vs turbid state
58Water transparency clear vs turbid state -2
Water transparency clear vs turbid state -2
59Shallow lakes vs deeper lakes - switches
- Usually more productive higher AwAo ratio
- Plants vs algae
- Natural predominance of macrophytes over algae.
Human impacts can switch them from
clearwater-plants to turbid water-algae state
maintained by - Poor fish management (carp, exotics, )
- Inadequate shoreline protection of emergent veg
- Boat damage
- Pesticide and nutrient runoff (fish, grazers,
plants) - Susceptible to very obnoxious algal blooms
- Difficult to reestablish clearwater-macrophyte
state
60Photosynthesis (PPr) respiration (Rn) effects
on routine water quality parameters examples
Temperature no effect generally. High rates of
respiration can increase the temperature in
bottom waters over long periods of time
(gtdecades) but this is unusual and associated
with meromixis DO High rates of photosynthesis
( primary productivity PPr) produce O2 and can
lead to supersaturation (gt100) EC25 EC
increases in the hypolimnion during stratified
periods due to mostly to the accumulation of
bicarbonate ions (HCO3- ) from respired CO2 that
dissolves in the water at moderate pH (6-9). The
pH is usually lowered as well. pH High rates of
PPr increase pH due to the removal of CO2 and
HCO3- from the water (essentially removing
carbonic acid) repiration does the opposite as
noted above for EC25.
61PPr Rn effects in relation to density layering
- The line plots are dissolved-O2
62More about Onondaga in 2003
Heres DO
- DO gt 150 from 0-3m and then lt10 down to the
bottom ! - pH drops gt1 unit from 3 down to 5 m
- EC jumps up and down by 400 uS/cm !
63Lake Washington tidbits Apr- Oct 2002
Apr high chlor Is it real ?
Sep low chlorophyll low metalimnion DO - Is
it real ?
Oct high chlorophyll - Is it real ?
64Water Quality What is it ?
- Water quality is actually a subjective term that
is used to describe the condition of a water body
in relation to - the needs of humans (beneficial uses in
regulatory parlance), - or the needs of aquatic organisms
- Water quality is not an absolute since different
user groups may have different expectations and
values - Water quality protection involves both human
health and environmental health risk assessments
and management - Water quality regulatory standards alone may be
met yet the patient may die. For this reason
biocriteria have become an important new aspect
of water resource protection
65Water Quality Whats a high value ?
- Protection environmental health vs human health
- Beneficial use fishable swimmable vs drinkable
- Lake-P 100 ppb hyper-eutrophic
- Cola-P 1000's ppb tasty
- Drinking water-P no limit (Duluth adds 1000 ppb
to control lead leaching from old pipes) - Lake-N gt500 ppb high
- Drinking water OK if lt 10,000 ppb Nitrate-N
- Lake Hg lt 3 ppt vs DW lt 2,000,000 ppt
- Lake fish PCBslt 50 ppb vs Baby food lt 2000 ppb
66Water quality depends on many factors
- Characteristics of the ecoregion
- Type and size of the watershed
- Precipitation patterns and surface water
hydrology - Groundwater influences
- Lake size, shape, and retention time
- Number of people and land uses in the watershed
67Minnesota Ecoregions
681.6-3.3 ft
69Other important factors affecting the health and
economic sustainability of lake resources
- Non-water quality impacts
- shoreline attached algae aquatic plants
- shoreline woody debris aquatic habitat
- exotic species (invasive plants animals)
- noise pollution
- light pollution
- sight pollution
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