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Published byKerry Barnaby Booth Modified over 9 years ago
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WATER Plants' most important chemical most often limits productivity
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WATER Plants' most important chemical most often limits productivity Often >90% of a plant cell’s weight
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WATER Plants' most important chemical most often limits productivity Often >90% of a plant cell’s weight Gives cells shape
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WATER Plants' most important chemical most often limits productivity Often >90% of a plant cell’s weight Gives cells shape Dissolves many chem
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WATER Dissolves many chem most biochem occurs in water Source of e - for PS
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WATER most biochem occurs in water Source of e - for PS Constantly lose water due to PS (1000 H 2 O/CO 2 )
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WATER most biochem occurs in water Source of e - for PS Constantly lose water due to PS Water transport is crucial!
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WATER Water transport is crucial! SPAC= Soil Plant Air Continuum moves from soil->plant->air
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Plant Water Uptake Water is drawn through plants along the SPAC, using its special properties to draw it from the soil into the air
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WATER Formula = H 2 O Formula weight = 18 daltons Structure = tetrahedron, bond angle 104.5˚
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WATER Structure = tetrahedron, bond angle 104.5˚ polar :O is more attractive to electrons than H + on H - on O
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Water Polarity is reason for water’s properties water forms H-bonds with polar molecules
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Water Polarity is reason for water’s properties water forms H-bonds with polar molecules Hydrophilic = polar molecules Hydrophobic = non-polar molecules
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Properties of water 1)Cohesion = water H-bonded to water -> reason for surface tension
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Properties of water 1)Cohesion = water H-bonded to water -> reason for surface tension -> why water can be drawn from roots to leaves
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else Cohesion and adhesion are crucial for water movement in plants!
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else Cohesion and adhesion are crucial for water movement in plants! Surface tension & adhesion in mesophyll creates force that draws water through the plant!
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat absorb heat when break H-bonds: cools leaves
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat absorb heat when break H-bonds Release heat when form H-bonds
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats 5) Universal solvent
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats 5) Universal solvent Take up & transport nutrients dissolved in water
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Properties of water 5) “Universal” solvent Take up & transport nutrients dissolved in water Transport organics dissolved in water
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats 5) Universal solvent 6) Hydrophobic bonds
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Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats 5) Universal solvent 6) Hydrophobic bonds 7) Water ionizes
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pH [H + ] = acidity of a solution pH = convenient way to measure acidity pH = - log 10 [H + ] pH 7 is neutral: [H+] = [OH-] -> at pH 7 [H+] = 10 -7 moles/l
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pH Plants vary pH to control many processes!
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Water movement Diffusion: movement of single molecules down ∆[ ] due to random motion until [ ] is even Driving force?
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Water movement Diffusion: movement of single molecules down ∆[ ] due to random motion until [ ] is even Driving force: lowers free energy ∆G = ∆H- T∆S
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Water movement Diffusion: movement of single molecules down ∆[ ] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient
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Water movement Diffusion: movement of single molecules down ∆[ ] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆ [ ] !
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Water movement Diffusion: movement of single molecules down ∆[] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆[ ] ! How water moves through xylem
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Water movement Diffusion: movement of single molecules down [] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆ [ ] ! How water moves through xylem How water moves through soil and apoplast
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Water movement Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆ [ ] ! How water moves through xylem Main way water moves through soil and apoplast Very sensitive to radius of vessel: increases as r 4
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Water movement Diffusion: movement of single molecules down ∆[] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆[ ] ! How water moves through xylem Main way water moves through soil and apoplast Very sensitive to radius of vessel: increases as r 4 Osmosis: depends on bulk flow and diffusion!
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Water movement Osmosis: depends on bulk flow and diffusion! water crosses membranes but other solutes do not water tries to even its [ ] on each side
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Water movement Osmosis: depends on bulk flow and diffusion! water crosses membranes but other solutes do not water tries to even its [ ] on each side other solutes can’t: result is net influx of water
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Water movement Osmosis: depends on bulk flow and diffusion! Moves through aquaporins, so rate depends on pressure and [ ] gradients!
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Water movement Osmosis: depends on bulk flow and diffusion! Moves through aquaporins, so rate depends on pressure and [ ] gradients! Driving force = water's free energy (J/m 3 = MPa)
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Water potential Driving force = water's free energy = water potential w Important for many aspects of plant physiology
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Water potential Driving force = water's free energy = water potential w Water moves to lower its potential
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Water potential Driving force = water's free energy = water potential w Water moves to lower its potential
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Water potential Driving force = water's free energy = water potential w Water moves to lower its potential Depends on: 1.[H 2 O]: s (osmotic potential)
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Water potential Water moves to lower its potential Depends on: 1.[H 2 O]: s (osmotic potential) 2.Pressure : p Turgor pressure inside cells
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Water potential Water moves to lower its potential Depends on: 1.[H 2 O]: s (osmotic potential) 2.Pressure : p Turgor pressure inside cells Negative pressure in xylem!
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Water potential Water moves to lower its potential Depends on: 1.[H 2 O]: s (osmotic potential) 2.Pressure p 3.Gravity g w = s + p + g
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Water potential Water moves to lower its potential Depends on: 1.[H 2 O]: s (osmotic potential) 2.Pressure p 3.Gravity g w = s + p + g w of pure water at sea level & 1 atm = 0 MPA
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Water potential w = s + p + g w of pure water at sea level & 1 atm = 0 MPA s (osmotic potential) is always negative
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Water potential w = s + p + g w of pure water at sea level & 1 atm = 0 MPA s (osmotic potential) is always negative If increase [solutes] water will move in
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Water potential w = s + p + g w of pure water at sea level & 1 atm = 0 MPA s (osmotic potential) is always negative If increase [solutes] water will move in p (pressure potential) can be positive or negative
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Water potential w = s + p + g w of pure water at sea level & 1 atm = 0 MPA s (osmotic potential) is always negative If increase [solutes] water will move in p (pressure potential) can be positive or negative Usually positive in cells to counteract s
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Water potential p (pressure potential) can be positive or negative Usually positive in cells to counteract s Helps plants stay same size despite daily fluctuations in w
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Water potential w = s + p + g p (pressure potential) can be positive or negative Usually positive in cells to counteract s Helps plants stay same size despite daily fluctuations in w p in xylem is negative, draws water upwards
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Water potential w = s + p + g p (pressure potential) can be positive or negative Usually positive in cells to counteract s Helps plants stay same size despite daily fluctuations in w p in xylem is negative, draws water upwards g can usually be ignored, but important for tall trees
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Water potential Measuring water potential
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Water potential Measuring water potential s (osmotic potential) is “easy” Measure concentration of solution in equilibrium with cells
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Water potential Measuring water potential s (osmotic potential) is “easy” Measure concentration of solution in equilibrium with cells g (gravity potential) is easy: height above ground -0.01 Mpa/m
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Water potential Measuring water potential s (osmotic potential) is “easy” Measure concentration of solution in equilibrium with cells g (gravity potential) is easy: height above ground P (pressure potential) is hard! Pressure bomb = most common technique
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Water potential Measuring water potential s (osmotic potential) is “easy” Measure concentration of solution in equilibrium with cells g (gravity potential) is easy: height above ground P (pressure potential) is hard! Pressure bomb = most common technique Others include pressure transducers, xylem probes
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Measuring water potential P (pressure potential) is hard! Pressure bomb = most common technique Others include pressure transducers, xylem probes Therefore disagree about H 2 O transport in xylem
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