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TRANSCRIPT
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Physics and Ionic Content ofWater
2 September 2004
1. How does waters unusual temperature-density relationship
influence life in lakes?
2. What are the major substances dissolved in water?
3. How does the ratio of inertial forces to viscous forces
affect both water flow and how organisms experience their
environment?
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Water has several unique propertiesthat make life in lakes possible
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Water molecules are dipoles:
d+
H H
O
d-
104.5
These hydrogen bonds form and break at a rate determined by
the temperature
And hydrogen bonding occurs:
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Forms a tetrahedron when frozen
Kalff2002 Wetzel 2001
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Density relationships
Density of ice is 0.9168 g/cm3at 0C, but water is 0.9999 g/cm3
As water is warmed from 0C, it increases in density until a
maximum of 1.000 is reached at ~4C (actually 3.94C).
Density of water is affected by pressure
Many lakes are too shallow for this to matter
Density of water is affected by salinity
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An important consequence of hydrogen
bonding and the density relationships:
Ice floats
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Other unique properties of water:
Water naturally occurs as a liquid, solid and gas
Water has a high specific heatthe amount of heat
in calories required to raise the temperature of 1 g
of water 1C
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Water has a high surfacetensionmeasures the
strength of the surface film
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Higher for any other liquidexcept mercury
Barrier to diffusion
Decreases with increasing
temperature
Can be disrupted byorganic compounds
Organisms live in and on
the surface film
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Ionic content of water:Water is a solvent for many ionic compounds
Salinitythe concentration of eight major ions (next slide)
Seawater = 32 g/L = ppt =
Freshwater < 3 g/L
Saline lakes = 18330 g/L
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Principle dissolved substances (in order of abundance)
Cations Anions
Ca++ (Calcium) CO32- (carbonate)
Mg++ (Magnesium) HCO3- (bicarbonate)
Na++ (Sodium) SO42- (sulfate)
K+ (Potassium) Cl- (chloride)
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Other substances are also present in fresh water at low
concentrations and have a negligible effect on salinity.
Some rare compounds are of great biological significance.
They are often referred to as Nutrients
PO43- (Phosphate)
NO3- (Nitrate)
SiO4- (Silicate)
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Mechanisms controlling salinity:
1.Rock dominance
2. Atmospheric precipitation
3. Evaporation - precipitation balance
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Saline Lakes formed in a closed basin when
evaporation exceeds inflow, yet that inflow issufficient to sustain a standing body of water.
Dominated by Na and Cl
Hard waters contain
large concentrations of
Ca and Mg salts
Soft waters water of
low salinity (dont have
many of the ions)
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Water also dissolves gases
O2
CO2
N2
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Explain the reasons for the shape of the
relationship between temperature and
density for water.
Why is the solid form of water (ice) lessdense than the liquid form?
What are 3 other properties of water that
are important to understand for limnology?
Why?
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Dynamic Viscosityresistance of a liquid to motion
How to measure:
How much force is needed to move the plates?
Higher force, higher viscosity
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Viscosity of water varies with temperature, warm water isless viscous than cold water
Viscosity at 0C = 1.792 x 10-3 kg/m/sViscosity at 30C = 0.801 x 10 -3 kg/m/s
The frictional resistance encountered by a swimming fish is
about 100 times greater than for organisms living in air
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Forces acting on an organism in water:
1. viscosity
2. gravity
3. pressure4. motility
The relative impact of viscosity on the momentum of an
organism depends on:
the size of the organism
the speed of the organism
These determine relative contribution of viscous and inertial
forces
INERTIAL FORCES
VISCOUS FORCES
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Inertial forces keep things going, viscous forces make things
stop
Gravity keeps pulling you downward
Pressure, in this case, is equal in all directions
Motility keeps you going
Viscosity determines how far you go
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To determine relative importance of inertial forces to,
viscous forces use the ratio:
Inertial forces/Viscous Forces = Reynolds Number= Re
Re= ( U L) /
= density of the fluidU = Velocity of the organism (or current)
L = Length of the organism (or thickness of the water layer)
= viscosity
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Small Re means that viscous forces dominate
A large Re means that inertial forces dominate
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BrownianRe < 0.1
Depending on Re, organisms occupy one
of three realms
StokesianRe 0.1 low 100
ArchemedianRe > 500
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BrownianRe < 0.1
Very small organism (e.g. phytoplankton) and
molecules
Viscous forces dominate
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StokesianRe 0.1 low 100s
Stokes Law applies The terminal velocity of a
particle is proportional to 1/viscosity of water
Viscous forces still dominateif stop propelling,
stop moving
This influences the moving and feeding ofzooplankton
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ArchemedianRe > 500
Inertial forces dominate
These organisms live in a turbulent environment
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1 m 0.1 mm 1 cm 1 m 100 m
Re
0.000001
0.0001
0.01
1
100
10,000
1,000,000
Realms
Archimedean
Stokesian
Brownian
Hutchinson 1971
Phytoplankton
Zooplankton
Fish
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Laminar flow is smooth and orderly,dominated by viscous forces (Re < 500)
Reynolds number also defines whether the
flow of water is laminarorturbulent
Turbulent flow contains a swirling of water and
chaotic eddies (Re > 2000)
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Laminar flow is smooth and orderly,dominated by viscous forces (Re < 500)
Reynolds number also defines whether the
flow of water is laminarorturbulent
Turbulent flow contains a swirling of water and
chaotic eddies (Re > 2000)
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Turbulent flow, not laminar flow,
is what mixes heat, gases,
nutrients etc. in the water
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Terms to Know
hydrogen bonding
specific heat
surface tension
salinitynutrients
hard water
soft water
saline lakeviscosity
viscous force
inertial force
Reynolds number
Brownian RealmStokesian Realm
Archimedian Realm
laminar flow
turbulent flow