lake mixing: density. thermal stratification epilimnion hypolimnion

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Lake Mixing: Density D ensity ofW ater Tem perature ( o C) 0 5 10 15 20 25 30 D ensity (g/cm 3 ) 0.995 0.996 0.997 0.998 0.999 1.000 1.001 Maximum

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Page 1: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Lake Mixing: Density

Density of Water

Temperature (oC)

0 5 10 15 20 25 30

Den

sity

(g/

cm3 )

0.995

0.996

0.997

0.998

0.999

1.000

1.001

Maximum

Page 2: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Thermal Stratification

0

5

10

15

20

0 10 20 30

Temperature (°C)

Dep

th (

m)

Epilimnion

Hypolimnion

Page 3: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Seasonal Stratification

Page 4: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Thin ice?

Page 5: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Field Trip Results

0

2

4

6

8

10

12

14

16

0 5 10 15 20

Temp. (oC)

Dep

th (

m)

Dollar Bay

Portage

Page 6: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Chemistry-Physics-Biology Linkage

0

2

4

6

8

10

12

14

16

0 2 4 6 8

Dissolved Oxygen (mg/L)

Dep

th (

m)

Dollar Bay

Portage

Page 7: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Significance of Stratification

Unstratified,Single CSTR (CMFR) Stratified

2 CSTRs withfeedback

Page 8: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Upwelling

Page 9: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Nutrient LimitationNutrient Limitation

The growth of algae and higher aquatic plants in lakes is regulated by conditions of light and temperature and the availability of those inorganic nutrients required to support growth. The element most often in limiting supply is phosphorus, P.

C

CC

O O

OO

P PP P

P P

C C

C C

C

C

C C C

O O O O

O O O O

O O O O

C

CC

O O

OO

P P+

O

O

O

O

C

C

C

Page 10: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Eutrophication

P

Page 11: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Effects of Eutrophication

Oligotrophic1. Low biomass2. High diversity3. Complex food web4. Oxic waters5. Cold-water fish present6. High aesthetic quality7. No taste or odor problems

Eutrophic1. High biomass2. Low diversity3. Simple food chain4. Anoxic bottom waters5. Cold-water fish absent6. Low aesthetic quality7. Taste and odor problems8. Rough fish abundant9. Toxic algae present

Page 12: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Oxygen supply

Surface mass transport

Vertical mass transport

Hypolimneticoxygen demand0

2

4

6

8

10

12

14

Dis

solv

ed O

xyg

en (

mg

/L)

Page 13: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Onondaga Lake: “most polluted lake in U.S.A.”

Page 14: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Biogeochemistry: study of the interactions of biology, geology,

chemistry, physics

Page 15: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Water Reservoirs

Page 16: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Hydrologic Cycle

Page 17: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion
Page 18: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Biogeochemical Cycles

Page 19: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Carbon Cycle

Page 20: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Another view of the carbon cycle

CO2 Organic C

CH4

Respiration

Photosynthesis

MethanogenesisMethaneoxidation

Page 21: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Nitrogen Cycle

N 2

NH 3/N H 4+ NO 3-

O rgan ic-N

DENITRIFICATIO NFIXATIO N

NITRIFICATIO N

DISSIM ILATO RYREDUCTIO N

ASSIM ILATIO NASSIM ILATIO N

Page 22: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Human perturbations to N Cycle

Page 23: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

L. Superior

Mississippi R.

Page 24: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

N2O Emissions:310 x greenhouse effect of CO2

U.S. Emissions increased 1.1% in 1990s30% of anthropogenic emissions occur in “coastal” areasNo reliable estimates of emissions from Great Lakes

Page 25: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

93.5 92.5 91.5 90.5 89.5

Longitude (deg.)

28.5

29.0

29.5

30.0

Lat

itu

de

(deg

.)

July 23-28, 1999, Shelfwide Oxygen Survey

Bottom Dissolved Oxygen Less than 2.0 mg/L

Atchafalaya R.

Mississippi R.

(Rabalais, Turner & Wiseman)

50 km

TerrebonneBay

Sabine L.L. Calcasieu

Gulf of Mexico Hypoxic Zone

Page 26: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Eutrophication

Eutrophication: the process of becoming or being made eutrophic

Eutrophic: the state of being enriched in nutrients or food sources

In aquatic ecosystems, eutrophication is caused by excessive inputs of nutrients, both N & P. Generally, freshwaters are P-limited and coastal estuarine waters are N-limited. The nutrients enhance algal growth, and this, in turn, may have a cascade of effects on the ecosystem. These effects may include: algal blooms, growth of undesirable algal species, oxygen depletion or anoxia in bottom waters, loss of cold-water fish species, abundance of “rough fish”, fish kills, unpleasant tastes and odors.

Page 27: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Sources of nutrients

• Point sources– Sewage treatment plant discharges– Storm sewer discharges– Industrial discharges

• Non-point sources– Atmospheric deposition– Agricultural runoff (fertilizer, soil erosion)– Septic systems

Page 28: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Solution: Reduce nutrient inputs

• Agriculture– Reduce animal density, restrict timing of manure spreading,

buffer strips by streams, reduced tillage, underground fertilizer application, wetland preservation and construction

• Watershed management– Buffer zones, wetland filters

• Storm runoff– Eliminate combined sewer systems (CSO’s)– Stormwater treatment required (holding ponds, alum)– Education on yard fertilization

• Erosion from construction, forestry– Erosion barriers, soil cover, road and bridge stabilization

• Septic systems– Distance from lake, adequate drainfields

Page 29: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Mitigation strategies

Often there is pressure for quick actions that will reduce the severity of the symptoms. Numerous options exist. To understand these options and choose among them, one should understand the nutrient cycle within the aquatic system (lake).

Page 30: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

P Cycle

InorganicP

OrganicP

SedimentHypolimnion

Epilimnion

InorganicP

InorganicP

OrganicP

OrganicP

Burial

Settlin

gS

ettlingD

isp

ersi

on

Uptake

Mineralization

Mineralization

Burial

The P cycle may be manipulated in several ways to reduce the regeneration of inorganic P and its transport to the epilimnion or to reduce the algal uptake of P.

Page 31: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Within-lake actions

• Reduce algal growth– Apply algicide

– Biomanipulation

• Reduce mineralization– Remove organic P before it is mineralized

• Dredging

• Macrophyte harvesting

• Reduce transport of inorg. P to epilimnion– Hypolimnetic water withdrawal

Page 32: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Macrophyte harvesting

Page 33: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Lake Phosphorus CycleLoading, W

O utflowQCl

SettlingBuria l

VdC

dtW QC v CAs

VdC

dtm m rxnin out

Page 34: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Vollenweider Model

Steady State Solution:

CW

Q v A

CW

Q v A

A

A

WA

QA

v

J

q v

s

ss

s

log( ) log log( )J C q vs

0.1

1

10

100

1 10 100 1000

Hydraulic Loading rate, q, (m3/m2-yr)

P l

oa

din

g r

ate

, J

,

(g

P/m

2y

r)

Page 35: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Terms to know:EpilimnionHypolimnionThermoclineMetalimnionOligotrophicEutrophicMesotrophic

Oxygen sag curveCritical pointOxygen deficitSaturationReaerationDeoxygenation

DenitrificationNitrificationAcid rainMineralizationLimiting nutrientLiebig’s LawSulfate reductionNitrogen fixationHydrologic cycleEvapotranspirationBiogeochemical cycleMicronutrientMacronutrient

Page 36: Lake Mixing: Density. Thermal Stratification Epilimnion Hypolimnion

Review of previous terms:BioticAbioticAtmosphereHydrosphereLithosphereBiosphereEcosphereEcologySpeciesPopulationCommunity

Organism groups:virusesbacteriaalgaefungiprotozoarotifersmicrocrustaceansmacrophytesmacroinvertebratesfish

PhotosynthesisChlorophyllRespirationRedoxReductionOxidationElectron donorElectron acceptorAerobesObligate vs. facultativeAnaerobic respirationAerobic respirationanoxic

AnaerobicFermentationAutotrophHeterotrophBiomassProductivityPrimary productionSecondary productionLithotrophsPhotoautotrophsPhotoheterotrophsChemoheterotrophsChemoautotrophsProducers Consumers

Herbivores CarnivoresOmnivores Trophic levelFood chain Food webMicrobial loop Decomposers