Soil Water Infiltration Rate
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 7 benchmarks together — the OptimalRange form drives the primary score, while 6 guard(s) constrain the result.
Evidence & Context
A rate of less than 10 mm/hr is identified as a lower critical threshold, signifying a tipping point into a stable, degraded state characterized by high runoff, soil erosion, and a loss of productive capacity.
Lower critical threshold for Soil Water Infiltration Rate below which ecosystem function is impaired.
This benchmark defines the lower critical infiltration rate threshold below which soil function degrades, leading to increased runoff, erosion, and loss of productivity in the Arid Karstic Woodlands & Shrublands biome under livestock grazing.
Based on multiple studies showing infiltration rates in degraded patches and bare soils around or below 10 mm/hr, indicating a regime shift to degradation.
Sources (1)
Using a landscape functional approach to soil health
View SourceSupporting Sources (5)
Additional references from the underlying research that informed this benchmark.
Healthy soils and water infiltration in the paddock - Local Land Services - NSW Government
View SourceInfiltration rates and soil moisture in a groved mulga community near Alice Springs, arid central Australia: Evidence for complex internal rainwater redistribution in a runoff-runon landscape | Request PDF - ResearchGate
View SourceInfiltration rates and soil moisture in a groved mulga community near Alice Springs, arid central Australia: Evidence for complex internal rainwater redistribution in a runoff-runon landscape | Request PDF - ResearchGate
View SourceRangeland Soil Quality: Infiltration - Natural Resources Conservation Service
View SourceThresholds in Ecological and Social-Ecological Systems: A Developing Database
View Source