Soil Water Infiltration Rate
Benchmark Value
Scoring Curve
The scoring engine could not generate a curve for this benchmark context. The primary form is CompositeFramework, 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
Considering these points, a SWIR consistently below 15-25 mm/hr is proposed as a lower critical threshold for maintaining essential ecological functions and long-term productivity in Australian Temperate Dry Woodlands & Native Grasslands under production forestry.
Soil Water Infiltration Rate (SWIR) is the rate at which water enters the soil profile, typically expressed in millimeters per hour (mm/hr).
This benchmark sets a minimum soil water infiltration rate of 15 mm/hr below which soil function and productivity are critically impaired in Australian Temperate Dry Woodlands under production forestry.
This threshold represents a point where the system shifts from effectively absorbing and utilizing water to predominantly shedding it, with attendant degradation, based on ecological function impairment and long-term productivity loss.
Sources (2)
General Soil Water Infiltration Rate Classification
View Sourcewww.waikatoregion.govt.nz, accessed May 15, 2025,
View SourceSupporting Sources (1)
Additional references from the underlying research that informed this benchmark.
Ecosystem wicks: Woodland trees enhance water infiltration in a fragmented agricultural landscape in eastern Australia, accessed May 15, 2025,
View Source