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@INPROCEEDINGS{vanDusschoten:1020588,
author = {van Dusschoten, Dagmar and Pflugfelder, Daniel and Kochs,
Johannes},
title = {{R}oot water uptake in relation to plant transpiration},
reportid = {FZJ-2024-00283},
year = {2023},
abstract = {Typically, root water uptake (RWU or Utot) is said to be
driven by transpiration (Tr). It is however more accurate to
state that transpiration causes a reduction in leaf water
content that reduces the leaf water potential such that a
water potential gradient builds up between leafs and soil
water, such that water can be extracted from the soil. For
herbaceous plants, the amount of water that is hereby lost
is typically assumed to be negligible so the plant can be
treated as a resistive system. In how far this is true is
open to discussion as quantifying shoot water changes is not
easily feasible, especially when the soil-root system is
drying out. A balance cannot observe water moving between
the soil and the shoot and shoots have empty spaces such
that 3D cameras provide an incomplete picture. Shoot weight
determination requires that the amount of soil water is
independently assessed to discriminate between the two pools
of water. This can be achieved when a balance is combined
with a Soil Water Profiler (SWaP) on the same soil-plant
system. The precision of the SWaP is comparable to that of
an expensive balance (<10mg for a 6kg system). Here we
performed experiments with the SWaP – balance combination
under modulated light with progressive soil dehydration for
sunflower and faba beans (N=4). Our data shows that
transpiration precedes Utot by about 5 to 10 mins under wet
conditions (pF<2.5) and Utot can exceed Tr by up to $20\%.$
Gradually, with decreasing soil water content we find that
Utot becomes smaller than Tr and at the same time the delay
between Tr and Utot increases. For pF>3 most of the
transpired water stems from the shoot, not from root water
uptake, indicating that Tr is a poor proxy for RWU for pot
experiments where soil is drying at a rate of $~5\%$ per day
at well watered conditions. This is very important for
calculations of root conductance during drying scenarios. We
found significant differences between sunflower sensitivity
to soil drying as compared to faba beans that are somewhat
more sensitive. We also present data that shows that the
delay between Tr and local water uptake is rather dependent
on depth and not so much dependent on local pF, which is
typically lower for shallow sections of the pot. This may
potentially be explained by loss of root water when Tr
increases with light, analogous to shoot water losses, as
the soil dries.},
month = {Apr},
date = {2023-04-24},
organization = {EGU General Assembly 2023, Vienna
(Austria), 24 Apr 2023 - 29 Apr 2023},
subtyp = {After Call},
cin = {IBG-2},
cid = {I:(DE-Juel1)IBG-2-20101118},
pnm = {2171 - Biological and environmental resources for
sustainable use (POF4-217)},
pid = {G:(DE-HGF)POF4-2171},
typ = {PUB:(DE-HGF)6},
doi = {10.5194/egusphere-egu23-12018},
url = {https://juser.fz-juelich.de/record/1020588},
}