Soil pH
Benchmark Value
Scoring Curve
This curve shows how a field measurement for this indicator would score across all available benchmark forms in this context. The scoring engine uses 3 benchmarks together — the OptimalRange form drives the primary score, while 2 guard(s) constrain the result.
Contributing Benchmarks
Evidence & Context
A pH value greater than 8.5 (H₂O) serves as a robust indicator of a shift from a healthy, calcium-dominated alkaline system to a degraded, sodium-dominated one.
Soil pH measured in a 1:5 soil:water suspension, representing the acidity or alkalinity of the soil.
This benchmark marks the upper soil pH limit of 8.5, beyond which soil degradation due to sodicity is indicated in the Arid Karstic Woodlands & Shrublands.
This threshold is based on scientific literature distinguishing natural alkalinity from detrimental sodicity conditions causing soil structure degradation and reduced ecosystem function.
Sources (1)
SOIL pH—SOUTH AUSTRALIA
View SourceSupporting Sources (6)
Additional references from the underlying research that informed this benchmark.
Caritat, P. de, & Cooper, M. (2011). The pH of Australian soils: Field results from a national survey. Soil Research, 49, 172-182.
View SourceArsenic and other elements in saltbush (Atriplex vesicaria) and soils from the goldfields of Western Australia
View SourceA Case for Below-Ground Dispersal? Insights into the Biology, Ecology and Conservation of Blind Cave Spiders in the Genus Troglodiplura (Mygalomorphae: Anamidae) - PubMed Central, accessed July 23, 2025
View SourceUPTAKE OF ARSENIC BY NATIVE PLANTS GROWING ON GOLD TAILINGS IN WESTERN AUSTRALIAN RANGELANDS1
View SourceSoil Groups of Western Australia - SoilsWest
View SourceSoil pH Explained - Soil Quality Knowledge Base
View Source