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 7 benchmarks together — the OptimalRange form drives the primary score, while 6 guard(s) constrain the result.
Contributing Benchmarks
Evidence & Context
Synthesizing these independent lines of evidence, a steady-state soil water infiltration rate that falls consistently within the range of 5–15 mm/hr can be considered a critical lower threshold for this biome.
Steady-state soil water infiltration rate in mm/hr below which ecosystem function is impaired and degradation occurs.
This benchmark defines the critical lower threshold soil water infiltration rate range in millimeters per hour below which the ecosystem shifts to a dysfunctional, erosion-prone state in arid mountain ranges and uplands.
This threshold is supported by multiple independent studies including degraded sites with infiltration rates as low as 5 mm/hr and hydrological modelling indicating 10 mm/hr as a limiting case for bare, degraded soils.
Sources (3)
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 SourceSupporting Sources (1)
Additional references from the underlying research that informed this benchmark.
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 Source