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
The recommended benchmarks, differentiated by soil texture to reflect varying inherent potential, are: 30 - 70 mm/hr for general Loamy to Sandy-Loam soils within mature, stable vegetation groves.
Soil water infiltration rate measured as steady-state infiltration capacity in mm/hr within high-functioning vegetated groves in arid mountain ranges and uplands.
This benchmark represents the steady-state soil water infiltration rate range measured in millimeters per hour within mature, stable vegetated groves in arid mountain ranges and uplands, indicating high ecological function.
These values represent the infiltration capacity measured within mature, stable, and highly functional mulga grove ecosystems (resource sinks) at Fowlers Gap and Menindee, reflecting a high state of natural ecological function.
Sources (1)
Infiltration rates and soil moisture in a groved mulga community near Alice Springs, arid central Australia: Evidence for complex internal rainwater redistribution in a runoff-runon landscape | Request PDF - ResearchGate
View SourceSupporting Sources (3)
Additional references from the underlying research that informed this benchmark.
Effects of Grazing on Water Erosion, Compaction and Infiltration on Grasslands - MDPI
View SourceMonitor Soil Degradation or Triage for Soil Security? An Australian Challenge - MDPI, accessed July 8, 2025,
View SourceWater Infiltration Rates into Unponded and Ponded Soils in Central Australia - Department of Agriculture and Fisheries
View Source