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.
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, the rate at which water enters the soil surface, measured in mm/hr.
Critical lower threshold below which soil infiltration is insufficient to prevent runoff and erosion.
Represents the point at which the soil can no longer absorb rainfall at a sufficient rate, causing runoff and erosion.
Sources (1)
Effects of Grazing on Water Erosion, Compaction and Infiltration on Grasslands - MDPI
View SourceSupporting Sources (2)
Additional references from the underlying research that informed this benchmark.
Nutrient surpluses in Australian grazing systems: management practices, policy approaches, and difficult choices to improve water quality - ResearchGate
View SourceHealthy soils and water infiltration in the paddock - Local Land ...
View Source