Ck. Yoder et Rs. Nowak, Soil moisture extraction by evergreen and drought-deciduous shrubs in the Mojave Desert during wet and dry years, J ARID ENV, 42(2), 1999, pp. 81-96
Annual and seasonal evapo-transpiration (ET) were compared among Mojave Des
ert shrubs with different leaf phenologies over a 3-year period during whic
h annual precipitation varied from well below average to more than twice av
erage. During the wet year, soil wetting fronts reached maximum depths of 0
.75 m to >1.95 m, depending on soil texture at the study sites. The evergre
en shrubs Larrea tridentata and Ephedra nevadensis, and the drought-deciduo
us shrub Ambrosia dumosa, were able to extract soil water in a uniform mann
er to depths >1 m. For stands of the deciduous shrub Lycium pallidum, a soi
l texture change at c. 0.75 m impeded percolation of water below that depth
. There were no significant differences (p < 0.05) in annual ET between the
evergreen shrubs Larrea and Ephedra relative to the drought-deciduous shru
bs Ambrosia and Lycium during the 3 years of the study. Early in the growin
g season, extraction of soil water from beneath plant canopies was slightly
greater than from shrub interspaces for Ambrosia, Ephedra, and Lycium, but
not for Larrea. For all species, annual soil water extraction from beneath
plant canopies was not significantly different than that from shrub inters
paces. The lower limit of soil water extraction (L-e) for the study sites v
aried from 4 to 10 volumetric per cent, depending on soil texture, and did
not differ significantly among species. For all species, L-e was reached wi
thin 6 to 12 months following twice average precipitation during the period
of November 1994 to March 1995. We conclude that ET in the Mojave Desert i
s dependent largely on winter precipitation and the amount of soil water av
ailable during the growing season rather than on species composition. (C) 1
999 Academic Press.