Some seasonal time-course water relation and gas exchange parameters w
ere monitored under natural conditions in three groups of 80-year-old
Quercus robur L. trees growing along an urbanization gradient, in orde
r to explain the positive correlation observed between the degree of d
ie-back and urbanization exhibited by these trees. All three groups of
trees exhibited the same general pattern of seasonal variation in pre
dawn (psi(pd)) and midday (psi(md)) leaf water potential, net photosyn
thesis (A), transpiration (E) and stomatal conductance (g), i.e. a dec
rease as the season progressed (from spring to winter), The extent of
these decreases were, however, more pronounced in the trees growing at
the edge of town (group b) and the urban trees (group c). Unlike the
rural trees (group a), which were able to maintain their A/E ratios wi
thin 50% of that during spring and were typified by both lower A/g and
E/g ratios, the trees of groups b and c were unable to maintain their
seasonal A/E ratios and had higher A/g and E/g ratios. The trees of g
roup a maintained higher A rates (accompanied by higher E) and could i
ntercept, more radiation. We propose that the trees of groups b and c
were dying back because of a reduced water supply, resulting in the co
st to gain carbon (because of smaller leaf area, reduced light interce
ption, insect herbivory, stromatal and non-stomatal inhibition) to exc
eed the cost in terms of available water.