Leaf responses to soil water deficits in controlled environments may b
e mediated by nonhydraulic root signals (RS). The aim of this study wa
s to evaluate in the field the effects of RS and leaf water potential
(psi(l)) on leaf expansion rate (LER) of sunflower (Helianthus annuus
L.). Two experiments were performed on a deep sandy-loam soil (Typic X
erofluvent) in a Mediterranean environment under spring (Exp. 1) and s
ummer conditions (Exp. 2). WET and DRY treatments were established at
the 16th-leaf stage in both experiments. WET plots were irrigated dail
y with an amount of water equal to the reference evapotranspiration of
the previous day. DRY plots received no water during the treatment pe
riod which was maintained until LER declined to about 30% of the WET c
ontrols. A split-root (SR) treatment with the root zone divided in dry
and wet sections was included in Exp. 2. Soil water content (theta(a)
), LER and psi(l) were measured. Responses of LER to soil drying were
better described by psi(l) than by plant available water (PAW); i.e.,
the response of LER to PAW depended on evaporative demand, whereas a s
ingle regression of psi(l) on LER fitted all the data (P < 0.001). Lea
f expansion rate and psi(l) of DRY plants began to decline with respec
t to that Of WET plants at similar PAW thresholds. The soil water cont
ent in the dry soil zone of the SR plots WaS Similar to that in the DR
Y plots during the first week of treatment whereas theta(a) in the wet
zone allowed SR plants to maintain a water status similar to that Of
WET controls. Split-rooted plants did not behave as DRY controls, as e
xpected in the case of a significant root signal effect, but maintaine
d LER similar to the WET plants. It is concluded that, under the condi
tions of the present experiments, hydraulic effects were probably of m
ore importance than nonhydraulic root signals in the regulation of sun
flower leaf expansion.