Soil Water Infiltration Rate
Benchmark Value
Scoring Curve
The scoring engine could not generate a curve for this benchmark context. The primary form is Point, but the benchmark data may be missing required fields (e.g., optimal range bounds for an OptimalRange benchmark). This is typically a data quality issue in the benchmark pipeline.
Evidence & Context
Based on the measured average steady-state flow rate (20.2 mm/hr) at the managed (ponded) Mt Riddock site, which has a Sandy Clay Loam soil.
Soil water infiltration rate measured as steady-state infiltration in mm/hr.
This benchmark represents the rate at which water infiltrates into sandy clay loam soils under best-practice regenerative cropping in the Australian Arid Mountain Ranges & Uplands biome.
This value is anchored to real-world data from the Mt Riddock site, representing a conservative, field-verified proxy for hydrological function achievable through management in the target biome.
Sources (2)
Comparing infiltration rates in soils managed with conventional and alternative farming methods: A meta-analysis
View SourceChapter 7 Nutrient Leaching - SIPS Soil & Crop Sciences Section
View SourceSupporting Sources (2)
Additional references from the underlying research that informed this benchmark.
Rainfall infiltration and runoff from an Alfisol in semi-arid tropical India. I. No-till systems1
View SourceInfiltration.pdf - Natural Resources Conservation Service
View Source