LEAF
RELATIVE WATER CONTENT (RWC)
Relative
water content (RWC) is probably the most appropriate measure of plant water
status in terms of the physiological consequence of cellular water deficit.
Water potential as an estimate of the energy status of plant water is useful in
dealing with water transport in the soil-plant-atmosphere continuum. However,
it does not account for osmotic adjustment (OA). OA is a powerful mechanism of
conserving cellular hydration under drought stress and RWC expresses also the
effect of OA in this respect. For the same leaf water potential two different
cultivars can have different leaf RWC, indicating a corresponding difference in
leaf hydration, leaf water deficit and physiological water status. Hence RWC is
an appropriate estimate of plant water status in terms of cellular hydration
under the possible effect of both leaf water potential and OA.
The
method has long been in use, even before its re-examination (Barrs and Weatherley, 1962), when
it was termed ‘relative turgidity’. It gained increasing appreciation with time
and experience. Some exemplary uses and discussions of RWC in physiological as
well breeding research can be found on this web site ‘Reference
Database’ ID numbers 1903, 2181, 3418, 3813, 3883, 3940 and 4793. Searching
for keyword RWC will provide many more recent studies where this measurement
has been used.
The
method is simple and this is one more advantage. It estimates the current water
content of the sampled leaf tissue relative the maximal water content it can
hold at full turgidity. Normal values of RWC range between 98% in fully turgid
transpiring leaves to about 30-40% in severely desiccated and dying leaves,
depending on plant species. In most crop species the typical leaf RWC at around
initial wilting is about 60% to 70%, with exceptions.
The
protocol
All
components of leaf water relations change during the day as irradiance and
temperatures change. For no more than two hours at and after solar
Usually,
between 4 to 6 samples (replications) are taken from a single treatment or
genotype. Each sample represents a different plant, if possible. Top-most fully
expanded leaves are sampled, unless the interest is in profiling leaves on the
plant. In large broad-leaves (sunflower, cotton, etc)
leaf discs are cut from the leaves, to obtain a total of about 5-10 cm2/sample.
Sample size does not have to be the same for all samples. Avoid large veins.
Leaf discs should be large enough (around 1.5 cm in diameter) so as to reduce
the area of cut leaf surface/sample. Various leaf disc cutters were designed by
laboratories and might be available commercially. Alternatively a sharp cork borer may be used, cutting the leaf over a piece of
dense rubber or a large rubber stopper. It is important that sampling will
proceed quickly. In smaller composite leaves (groundnuts, alfalfa, clover,
chickpeas) several leaflets make up a fast and convenient sample. In cereals, a
sample may constitute of a mid-leaf section of about 5-10 cm2 cut
with scissors. With larger leaves such as maize or sorghum a section measuring,
say, about 1x7 cm can be cut with scissors from the area between the mid-vein
and the edge.
Each
sample is placed in a pre-weighed airtight (possibly also oven proof) vial.
Cereal leaf sample should be placed in a vial slightly longer than the sample,
with its basal part to the bottom. Vials should be immediately placed in a
picnic cooler (around 100C-150C) but not frozen on ice. .
Samples should reach the lab as soon as possible. This is why leaf sampling
should be done quickly and it is important to enlist as much help as possible
for the job.
In
the Lab vials are weighed to obtain leaf sample weight (W), after which the
sample is immediately hydrated to full turgidity for 3-4h under normal room
light and temperature. Some prefer to hydrate samples on the lower shelf of a
lab refrigerator (about 100C). Leaf discs and small leaflets are
hydrated by floating on de-ionized water in a closes petri dish. Cereal leaf
samples receive water into the vial to a level of 1-2 cm after which the vial
is capped.
After
hydration the samples are taken out of water and are well dried of any surface
moisture quickly and lightly with filter/tissue paper and immediately weighed
to obtain fully turgid weight (TW). Samples are then oven dried at 800C
for 24h and weighed (after being cooled down in a desiccator) to determine dry
weight (DW). All weighing is done to the nearest mg. Calculation:
RWC
(%) = [(W-DW) / (TW-DW)] x 100,
Where,
W –
Sample fresh weight
TW
– Sample turgid weight
DW
– Sample dry weight.
With
good and careful work the method should normally result in about 2% to 3% of
RWC being a statistically significant difference between treatments.
Barr, H.D. and Weatherley,
P.E. 1962. A re-examination of the relative turgidity technique for estimating
water deficit in leaves. Aust. J. Biol. Sci. 15:413-428.