Rj. Ryel et al., TEMPORAL DYNAMICS OF SOIL SPATIAL HETEROGENEITY IN SAGEBRUSH-WHEATGRASS STEPPE DURING A GROWING-SEASON, Plant and soil, 184(2), 1996, pp. 299-309
Variability in five soil resources essential for plant growth (NH4+, N
O3-, P, K and soil moisture) was quantified using univariate, multivar
iate and geostatistical techniques in a sagebrush-grass steppe ecosyst
em at three times (early April, June and August) during the 1994 growi
ng season. Samples were collected every meter in a 10 x 10-m 'macrogri
d', every 20 cm within nested 1 x 1-m 'minigrids', and every 3 cm with
in additionally nested 15 x 15-cm 'microgrids'. Strong autocorrelation
for all variables in the three sample periods was only found over dis
tances less than 2 m, indicating that patches of high internal uniform
ity in this soil were smaller than 2 m during the growing season. Diff
erences in semivariograms between sample periods were most pronounced
for NO3-, NH4+ and soil moisture, variables that we consider to primar
ily limit plant growth in this system. The distance over which sample
points were autocorrelated for NO3-, NH4+ and soil moisture increased
from April to June. In contrast P and K, which are relatively more abu
ndant at the study site, exhibited relatively constant semivariance pa
tterns over the three sample periods. Weak correlation was found betwe
en samples collected in the three sample periods for N and soil moistu
re indicating that the spatial pattern of these limiting resources cha
nged between sample periods. However, P and K had highly significant c
orrelations (p < 0.00001) among sample periods, indicating that the di
stributional patterns of these relatively more abundant resources rema
ined rather constant. There were strong negative correlations between
P and K and distance from the base of shrubs for all sample times (p <
0.001), indicating an increase in P and K close to shrubs. Similar st
rong negative correlations were not found between distance from the sh
rubs and levels of NH4+, NO3-, or soil moisture, nor for any soil vari
able and distance from perennial tussock grasses. Changes in patterns
of nutrient and soil moisture variability within a growing season sugg
est that not only must plants acquire soil resources that vary in time
and space, but that they may also have to adjust to different scales
of resource patchiness during the season.