The water relations of arbuscular mycorrhizal plants have been compared oft
en, but virtually nothing is known about the comparative water relations of
mycorrhizal and nonmycorrhizal soils. Mycorrhizal symbiosis typically affe
cts soil structure, and soil structure affects water retention properties;
therefore, it seems likely that mycorrhizal symbiosis may affect soil water
relations. We examined the water retention properties of a Sequatchie fine
sandy loam subjected to three treatments: seven months of root growth by (
1) nonmycorrhizal Vigna unguiculata given low phosphorus fertilization, (2)
nonmycorrhizal Vigna unguiculata given high phosphorus fertilization, (3)
Vigna unguiculata colonized by Glomus intraradices and given low phosphorus
fertilization. Mycorrhization of soil had a slight but significant effect
on the soil moisture characteristic curve. Once soil matric potential (Psi
(m)) began to decline, changes in Psi (m) per unit change in soil water con
tent were smaller in mycorrhizal than in the two nonmycorrhizal soils. With
in the range of about -1 to -5 MPa, the mycorrhizal soil had to dry more th
an the nonmycorrhizal soils to reach the same Psi m. Soil characteristic cu
rves of nonmycorrhizal soils were similar, whether they contained roots of
plants fed high or low phosphorus. The mycorrhizal soil had significantly m
ore water stable aggregates and substantially higher extraradical hyphal de
nsities than the nonmycorrhizal soils. Importantly, we were able to factor
out the possibly confounding influence of differential root growth among my
corrhizal and nonmycorrhizal soils. Mycorrhizal symbiosis affected the soil
moisture characteristic and soil structure, even though root mass, root le
ngth, root surface area and root volume densities were similar in mycorrhiz
al and nonmycorrhizal soils.