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 11 benchmarks together — the OptimalRange form drives the primary score, while 10 guard(s) constrain the result.
Evidence & Context
The formation of a surface crust on bare, untilled soil limited the steady-state infiltration rate to approximately 10 mm/hr. Below this rate, runoff becomes a direct function of rainfall intensity.
Steady-state soil water infiltration rate below which hydrological function fails.
This benchmark represents the lower critical threshold for soil water infiltration rate indicating system failure in the Australian Arid Mountain Ranges & Uplands biome.
This threshold is supported by multiple studies and baseline measurements at degraded sites, indicating severe ecological and agronomic consequences below this rate.
Sources (2)
Chapter 7 Nutrient Leaching - SIPS Soil & Crop Sciences Section
View SourceRainfall infiltration and runoff from an Alfisol in semi-arid tropical India. I. No-till systems1
View SourceSupporting Sources (2)
Additional references from the underlying research that informed this benchmark.
Comparing infiltration rates in soils managed with conventional and alternative farming methods: A meta-analysis
View SourceInfiltration.pdf - Natural Resources Conservation Service
View Source