F
|
Ø
A (30) potometer (蒸騰計) can be used to
measure the
rate of transpiration of a
plant.
n
Bubble potometer (氣泡蒸騰計) measures the rate of (31) water absorption / uptake of a leaf shoot
n Assumption for valid measurement:
Rate of transpiration = Rate of (32) water absorption
= Volume of water absorbed / time (ml min-1)
n
(33) Weight potometer can
measures volume of water absorbed by and the volume of water loss from the
plant
Component
|
Used
to measure
|
Burette
|
(34) rate of water
uptake
|
Balance
|
(35) rate of water loss
|
l Assumption for valid result:
² the loss of water over a short period of
time is only due to transpiration
² gain or loss of weight due to photosynthesis
and/or respiration is insignificant不明顯
|
l
Rate of
water absorption
= volume change in burette /
time
l
Rate of
water loss = weight change / time
l Rate of transpiration
= Rate of (36) water loss
=
Weight loss
/ time
(mg min-1)
l Volume of water absorbed should be (37) larger
than / smaller
than / equal to the volume of water loss
because some water is consumed by the plants for
maintaining the process of life
such as (38)
photosynthesis,
growth and cellular
metabolism.
Ø
Effect of different environmental factors on the rate of transpiration:
Factor
|
Effect on rate of
transpiration
|
Reason
|
Light intensity
|
The rate (39) increases /
|
n
As light intensity increases, the stomata open (40) wider.
The cross-sectional area
for the diffusion of water vapour (41) increases.
Water vapour diffuses out more rapidly.
n
In darkness, the stomata
are closed. Only a small amount of water vapour diffuses out.
|
Temperature
|
The rate (42) increases with an
increase in temperature.
|
n
As temperature increases, the rate of (43) evaporation of water from
the surfaces of mesophyll cells increases.
Water vapour diffuses out more rapidly.
|
Air movement
|
The rate (44) increases in windy
conditions.
|
n
Without air movement,
water vapour diffused out accumulates around the stomata.
n
Wind blows away water vapour around the stomata.
This helps maintain a (45) steeper concentration gradient of
water vapour between the air space and the
surrounding
air, thus (46) increasing the rate of diffusion.
|
Relative
humidity
|
The rate (47) decreases with an
increase in the relative humidity
of the surrounding air.
|
n
A higher relative humidity of the surrounding
air decreases the (48) concentration
gradient of water vapour between
the air space and the surrounding air.
(49) Less water vapour
diffuses out.
|
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