EFFECTS OF SOIL COMPACTION ON PLANT-GROWTH, PHOSPHORUS UPTAKE AND MORPHOLOGICAL-CHARACTERISTICS OF VESICULAR-ARBUSCULAR MYCORRHIZAL COLONIZATION OF TRIFOLIUM-SUBTERRANEUM
H. Nadian et al., EFFECTS OF SOIL COMPACTION ON PLANT-GROWTH, PHOSPHORUS UPTAKE AND MORPHOLOGICAL-CHARACTERISTICS OF VESICULAR-ARBUSCULAR MYCORRHIZAL COLONIZATION OF TRIFOLIUM-SUBTERRANEUM, New phytologist, 135(2), 1997, pp. 303-311
We investigated the effect of soil compaction and phosphorus (P) appli
cation on morphological characteristics of mycorrhizal colonization an
d growth responses, to determine the reasons for reduced responses obs
erved in our previous work with compacted soil. Growth, phosphorus (P)
uptake and intensity of vesicular-arbuscular (VA) mycorrhizal coloniz
ation were studied in clover plants (Trifolium subterraneum L.) with a
nd without VA mycorrhizal colonization at two P applications and three
levels of soil compaction. Phosphorus was supplied either at constant
mass concentration (mg P kg(-1) soil) or at constant volume concentra
tion (mg P dm(-3) soil). Increasing bulk density of the soil from 1.1
to 1.6 Mg m(-3) significantly decreased root length and shoot d. wt, b
ut increased the diameter of both main axes and first order lateral ro
ots regardless of P application. Total P uptake and shoot d. wt of clo
ver plants colonized by Glomus intraradices (Schenck & Smith) were sig
nificantly greater than those of non-mycorrhizal plants at all levels
of soil compaction and both P applications. However, soil compaction t
o a bulk density of 1.6 Mg m(-3) (penetrometer resistance = 3.5 MPa at
a matric potential of -33 kPa) significantly decreased mycorrhizal gr
owth response. There was no evidence that the increased volume concent
ration of P at high bulk densities was responsible for the reduced res
ponses. Soil compaction had no significant effect on the fraction of r
oot length containing arbuscules and vesicles, but total root length c
olonized by arbuscules, vesicles or by any combination of arbuscules,
vesicles and intra-radical hyphae significantly decreased as soil comp
action was increased. The air-filled porosity of highly compacted soil
, which varied from 0.07 to 0.11 over the range of matric potentials e
ncountered (-33 and -100 kPa), had no significant effect on the intens
ity of internal colonization.