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 12 benchmarks together — the OptimalRange form drives the primary score, while 11 guard(s) constrain the result.
Evidence & Context
The measured infiltration capacity is very high for both the burnt and unburnt sites, in the range 400-1300 mm h-1.
Infiltration capacity (maximum rate of water intake) measured via ring infiltrometers.
This benchmark defines the optimal soil water infiltration rate range for alpine and subalpine forest soils, indicating the soil's capacity to absorb intense mountain rainstorms without causing runoff.
Represents the natural high-functioning state of alpine forest soils.
Sources (1)
Variation in hillslope-scale erosion processes following a severe fire in Victoria
View SourceSupporting Sources (11)
Additional references from the underlying research that informed this benchmark.
Victoria's State of the Forests Report 2013, accessed March 28, 2026,
View SourceCENTRAL HIGHLANDS COMPREHENSIVE REGIONAL ASSESSMENT REPORT
View SourceInfiltration rates in subalpine forested catchments
View SourceInfluence of Vegetation Cover and Soil Properties on Water Infiltration: A Study in High-Andean Ecosystems of Peru - MDPI
View SourceInfiltration Characteristics of Soils Under Forestry and Agriculture in ...
View SourceManaging soil disturbance - EPA Victoria
View SourceCostin, A. B. 1954. A Study of the Ecosystems of the Monaro Region of New South Wales.
View SourceSaturated hydraulic conductivity in wet Eucalyptus forest
View SourceNew South Wales Vegetation classification and Assessment: Part 3 Plant communities of the NSW Brigalow Belt South, Nandewar an - Botanic Gardens of Sydney, accessed March 28, 2026,
View SourceGeotechnical testing requirements for infiltration systems
View SourceAustralian Alps Rehabilitation Manual
View Source