The soil properties most likely to influence species composition in lo
wland order of importance: P availability, Al toxicity, drainage, wate
r-holding capacity, and availability of K, Ca, and Mg. A total of 18 s
tudies were located in which species occurrence was studied in relatio
n to such soil properties. Several of these report clear trends with s
oil physical properties, mainly drainage as affected by topographic po
sition. Only three offer evidence for correlations with soil chemical
properties. In all three, the study area spanned soils of very widely
differing age and thus soil fertility. Failure to find correlations wi
th chemical properties may be due to: lack of range in soil fertility
across the sites studied. failure of soil test methods to measure avai
lability of nutrients to plants, or temporal and spatial variability i
n soil properties.Existing soil classification systems do not provide
enough information on any particular soil to help establish relations
between its chemical properties and plant distribution. Nonetheless, s
oils at ecological study sites must be classified if their nature and
properties are to be made clear to others working worldwide. Tradition
al, largely subjective, soil-mapping ;; techniques may reduce sampling
needs by allowing stratification of soil and plant sampling by broad
soil types. The mapping must be done, however, at a scale similar to t
he patchiness of the plant community (usually finer than 1:5000), some
thing done in only 3 of the 18 studies located. Correlative studies; a
re ?only, the ;first step in understanding causal relations between so
il properties and plant species distribution. Next, nutritional, drain
age, and water requirements must be established for individual species
. Then field experiments must be set up to establish cause and effect.