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.
Evidence & Context
Given this evidence, a benchmark reference value range of 100 - 1080 mm/hr is proposed for Soil Water Infiltration Rate in Alpine Humus Soils within Australian alpine and subalpine protected natural areas.
Soil Water Infiltration Rate (SWIR) is a critical soil physical property that governs the partitioning of precipitation into surface runoff, soil water storage, and groundwater recharge.
This benchmark defines the typical range of soil water infiltration rates in Alpine Humus Soils of Australian alpine and subalpine protected areas, indicating healthy soil function for water absorption and movement.
The benchmark is based on direct, field-based measurements of saturated hydraulic conductivity (Ksat) values for Alpine Humus Soils in the Snowy Mountains, representing a range from functional to optimal health.
Sources (1)
Rainfall infiltration and soil hydrological characteristics below ancient forest, planted forest and grassland in a temperate northern climate
View SourceSupporting Sources (28)
Additional references from the underlying research that informed this benchmark.
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