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
soil saturated hydraulic conductivity (Ksat) remained very high (100-1000 mm h -1)
Field saturated hydraulic conductivity ().
This benchmark defines the range of saturated hydraulic conductivity for high-health wet sclerophyll forests.
Established range for high-health wet sclerophyll forests.
Sources (1)
Saturated hydraulic conductivity in wet Eucalyptus forest
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 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 SourceVariation in hillslope-scale erosion processes following a severe fire in Victoria
View Source