Water-Plant Relations (Exam 2) Flashcards

(49 cards)

1
Q

water is the

A

universal solvent

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2
Q

why is water the universal solvent?

& therefore (2)

A

bc water is polar
& therefore has partial charges (no net charges) (solvent for other polar molecules & ions)
& allows for hydrogen bonding (approx 4 kJ/mol) (tensile strength)

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3
Q

what explains water movement through X?

A

tensile strength

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4
Q

what leads to tensile strength

A

cohesion

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5
Q

cohesion =

A

water liking itself

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6
Q

adhesion =

A

water liking others

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7
Q

water moves from

A

a higher potential energy to a lower potential energy

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8
Q

water moves… (2)

A
  • downhill w/ gravity
    (U = mgh)
  • “up” from bodies of water
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9
Q

water potential aka

A

“U”

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10
Q

water movement depends on

A

overall water potential (U) energy

U in water > U in air

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11
Q

water potential energy (U) is usually measured in

A

units of pressure

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12
Q

units of pressure we saw

A
  • Bars (1 bar = 14.5 psi)

- MPa (megapascals) (1 MPa = 10 bar)

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13
Q

plant cell pressure is measured in

A

MPa (megapascals)

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14
Q

components for liquid water (4)

A
  1. ) H = Hydrostatic Pressure (P)
  2. ) Π = Osmotic Pressure (solutes)
  3. ) ρ(of w)gh = Pressure due to gravity
  4. ) Matric pressure (H2O interactions with surfaces)
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15
Q

Π (Osmotic Pressure) eqtn

A
Π = RT(Ec)
E = sigma
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16
Q

as solute conc increases (2)

A
  • Π (Osmotic Pressure) increases

- U (water potential energy) decreases

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17
Q

in trees, P =

A

(-)

this is why trees don’t bleed

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18
Q

clay soil…

small particles

A

“holds” H2O best

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19
Q

sandy soil…

big particles

A

“drains” H2O best

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20
Q

Ψsoil vs Ψroot

A

Ψsoil > Ψroot (for root to take up H20)

21
Q

Water potential energy (U) equation

A

Ψ = P - Π + ρ(of w)gh + Matric Pressure

22
Q

P increases with

23
Q

how does water move up the plant?

A

plants let physics do the dirty work

24
Q

from leaves, water…

25
why does water evaporate from the leaf?
humidity in the leaf almost = 100% | air is rarely over 50%
26
stomata on leaves open for | therefore
CO2 uptake, | therefore water loss in inevitable
27
in the xylem, water exists as
a column
28
tensile strength (due to cohesion) of water allows...
...water to be "pulled" up the plant through the X
29
what happens when transpiration > supply?
= cavitation
30
soil consists of
particles & open spaces (pores)
31
soil pores are typically occupied by | which has
air & water, | which has dissolved inorganic nutrients
32
availability of water in soil depends on
the interactions of water with the soil
33
(availability of water) sand...
...dries quickly, but when wet, most of the water is available to the plant
34
(availability of water) clay...
...holds water longer, but less of the water is available to the plant
35
what determines the water potential in soil? | unless...
hydrostatic pressure & interactions with the surfaces (matrix pressure) determine water potential (Ψ/U) more than solutes (unless soil has very high concentrations of salts)
36
soil water =
hygroscopic (solid particles)
37
roots take up
capillary water
38
field capacity =
max amount of water held by soil
39
roots take up most of their water through | &...
root hairs | & mycorrhizae can take up water too
40
can leaves take up water?
yes, through fog
41
water is not
actively absorbed | which means no energy is expended
42
water moves into the plant if...
Ψsoil > Ψroot
43
when Ψsoil < Ψroot
water can actually flow out of the plant | usually changes in the root prevent this
44
how do roots prevent water form flowing out of it
casparian strip kill cortex lignify epidermis
45
water in the X is
"pulled"
46
water that evaporates is
replaced on cell walls
47
what allows water to be pulled?
the cohesive properties of water | tension
48
tension =
(-) hydrostatic pressure
49
the theory of water movement in plants =
evaporation-cohesion-tension theory