Dj. Reuter et al., AN APPRAISAL OF SOIL-PHOSPHORUS TESTING DATA FOR CROPS AND PASTURES IN SOUTH AUSTRALIA, Australian journal of experimental agriculture, 35(7), 1995, pp. 979-995
Data from more than 580 field experiments conducted in South Australia
over the past 30 years have been re-examined to estimate extractable
soil phosphorus (P) levels related to 90% maximum yield (C-90) for 7 c
rop species (wheat, barley, oilseed rape, sunflower, field peas, faba
beans, potato) and 3 types of legume-based pasture (subterranean clove
r, strawberry clover, annual medics). Data from both single-year and l
onger term experiments were evaluated. The C-90 value for each species
was derived from the relationship between proportional yield responsi
veness to applied P fertiliser rates (determined as grain yield in cro
ps and herbage yield in ungrazed pastures) and extractable P concentra
tions in surface soils sampled before sowing. Most data assessments in
volved the Colwell soil P test and soils sampled in autumn to 10 cm de
pth. When all data for a species were considered together, the relatio
nship between proportional yield response to applied P and soil P stat
us was typically variable, particularly where Colwell soil P concentra
tion was around C-90. When data could be grouped according to common s
oil types, soil surface texture, or P sorption indices (selected sites
), better relationships were discerned. From such segregated data sets
, different C-90 estimates were derived for either different soil type
s or soil properties. We recommend that site descriptors associated wi
th the supply of soil P to plant roots be determined as a matter of co
urse in future P fertiliser experiments in South Australia. Given the
above, we also contend that the Colwell soil P test is reasonably robu
st for estimating P fertiliser requirements for the diverse range of s
oils in the agricultural regions of the State. In medium- and longer t
erm experiments, changes in Colwell soil P concentration were measured
in the absence or presence of newly applied P fertiliser. The rate of
change (mg soil P/kg per kg applied P/ha) appeared to vary with soil
type (or soil properties) and, perhaps, cropping frequency. Relatively
minor changes in soil P status were observed due to different tillage
practices. In developing P fertiliser budgets, we conclude that a maj
or knowledge gap exists for estimating the residual effectiveness of P
fertiliser applied to diverse soil types under a wide range of South
Australian farming systems.