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 2 benchmarks together — the OptimalRange form drives the primary score, while 1 guard(s) constrain the result.
Contributing Benchmarks
Evidence & Context
For fine-textured clay soils, where the best-case scenario is already low, a rate below 1 mm/hr would signify a critical state of degradation.
Soil water infiltration rate below which ecosystem function is critically impaired for fine-textured clay soils.
Lower critical threshold for infiltration rate indicating severe degradation in fine-textured clay soils.
This threshold is supported by evidence showing that sodic soils can see rates drop to less than 0.2 mm/hr.
Sources (1)
A framework relating soil surface condition to infiltration and sediment and nutrient mobilization in grazed rangelands of northeastern Queensland, Australia | Request PDF - ResearchGate
View SourceSupporting Sources (3)
Additional references from the underlying research that informed this benchmark.
Landscape rehydration and regenerative agriculture improves soil health, accessed July 23, 2025
View SourceNutrient surpluses in Australian grazing systems: management practices, policy approaches, and difficult choices to improve water quality - ResearchGate
View SourceUnderstanding soil tests for pastures | Soil | Farm management ..., accessed July 18, 2025,
View Source