Due to the small
timeframe for sampling
in the tree nursery in Schinznach a well structured sampling design and time
management plan is of great importance. On site plant specific Transpiration
can be measured by a weighing experiment and the output of this measurement
will be used to calculate crop specific Evapotranspiration by the help of a
temperature based calculation model which will be explained below.
Weighing
Experiment
· The largest crops in the tree
nursery will be class divided by their size on one hand and whether they are
coniferous or broadleaved woody plants on the other hand.
-
The
crops will be divided by size in two classes (>0.5 meter, <0,5 meter).
-
Thuja occidentalis and Taxus baccata could be well fitting representatives for the
coniferous plants, Prunus laurocerasus
for the broadleaved woody plants.
· Five plants of every class are going
to be labelled and weighed individually in the morning and in the evening. In
the meantime, they`re going to be put back in the cultivating area to make sure
they have the same conditions like the whole cultivation area.
· Exclusion criterias are covered
cultivation areas, Plants weighing more than 20kg including the pot (due to the
limit of the scale) and Plants growing on non drained areas
material:
-
Scales,
small and big (up to 20kg)
-
Adhesive
tape and waterproof marker for the labelling (different colours)
-
Hand
truck for transporting big plants
-
Cable
reel
Evapotranspiration
calculation:
· The measured values for
crop-specific Evapotranspiration are going to be used to adjust the reference
crop coefficients. If there are for any reasons crops who can’t be measured,
values from literature have to be used.
· Due to the insufficient or missing
radiation data of the tree nursery, the evapotranspiration will be calculated
by using a temperature based model such as the “Blaney – Criddle” model will be
used. The required data for the calculation will be provided by the measuring
station “Campus Grüental”. Only the temperature data (Tmean ) will be taken from the
measuring station of the tree nursery.
· The evaporation of the pond will be
calculated by using literature-values for water bodies, as there are not big
differences in different water bodies.
Blaney –
Criddle equation
ETo = p
·(0.457·Tmean + 8.128)
Where:
-
ETo is the reference evapotranspiration [mm day−1]
(monthly)
-
Tmean is the mean daily temperature [°C] given as Tmean =
(Tmax + Tmin )/ 2
-
p is the mean daily percentage of annual daytime hours.
Hi Mattias
AntwortenLöschenI agree with most of what you wrote in a clear way. I think your plan is realistic, but do you also have a plan B? In Addition, it would be nice to know, which equation you will use to estimate the evaporation from the pond in order to know which parameters you have to measure in the field (e.g. water temperature). Katharina mentions a suitable method for evaporation from a free water surface in her second blog.
Best Luzi