Frost
can affect your crop at all stages of
development reducing yield and quality. Here
Dr. Ben Biddulph Research officer with
DAFWA explains how a frost occurs and
the contributing environmental factors
that will determine the severity. When we
have a wet canopy we get a lot more
frost damage than if the canopy was dry
and there's two main reasons because
of this. One is because of the wetness the
actual water. The other because of the
ice nucleators which happening. So
frost is not just freezing damage.
there's three main processes which
happen with frost. The first two are
cold and desiccation and most of
our frost event that's what we get.
So the cold is basically that
temperature response to the diagonal
stress of actually going from quite a
warm daytime temperature to a low
overnight minimum and then back up
to a warm temperature following a frost
event. So that cold effect essentially
the plants have to change their
membrane fluidity and their energy
balance and the process around that just
to cope with that cold stress. So frost
has initially has that effect of
cold the next effect is desiccation so
when we get a frost event we get ice
the dew forms on the canopy and then that
dew freezes after that it then starts
to suck water out of the air and so it
will freeze water from out of the air
but then it will also start to freeze
water out of the plant mesophyll
cells and out through the stomata itself
so it'll actually start to desiccate the
plant tissue and the flag leaf tissue
often after a frost event you can go out
the morning and when you see the flag
leaves defrost you'll see them wilt as
well and that's because they've lost all
that water from inside the tissue to
the outside so the desiccation effect.
So there's these first two processes and we get
that for most frost events. The other
effect we get is ice formation
and freezing damage. Now plants of
wheat will normally supercool to about
minus 10 degrees out in the paddock but when
we add ice nucleators they will start to
freeze at warmer temperatures. Now
ice nucleators are just like you know when
you leave your beer in the freezer and you
forget to take it out. You know when you
first take it out if you don't bang it
hard or you don't open the beer won't freeze
but soon as you open it and break that
seal it will freeze straight away and
that's because you basically had an ice nucleator
come in there.
Same thing happens with your wheat out in
the paddock. Essentially
when it's at minus 10 degree or minus 4 or 5
degrees it will super cool down to those
temperatures and the plant tissue won't
freeze. So you only get the cold and
desiccation effects. What happens with
ice nucleators they will actually make your
canopy freeze at warmer temperatures.
So normally in the paddock, we do
have ice nucleators in the form of
dust and different bacterial spores on
the canopy and these normally raise
the freezing point of those canopies to
around minus 5 degrees but when we have
a rainfall event which goes through and
actually wets the canopy those rain
droplets also bring in with
them ice nucleators and so a lot of
those ice nucleators which come with that
rainfall event raise the
freezing point to around minus 2C. So when we
have a wet canopy with a lot of these
ice nucleators which have been
introduced by the rainfall and the rain
itself we end up with a lot more
freezing damage because the plant
tissue will freeze at minus 2C doing and won't
super cool anywhere near as much so
compared to a dry frost, a frost when
you've got a wet canopy always a lot
more damage.
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