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
A Critical Failure Threshold can be defined at < 10 mm/hr.
Soil water infiltration rate below which the soil is effectively sealed, promoting massive runoff and erosion.
This benchmark defines the critical failure threshold for soil water infiltration rate below which the soil is effectively sealed, leading to severe runoff and erosion in tropical and subtropical rainforest soils under conservation management in Australia.
Research on agricultural soils shows that infiltration rates below this level generate significant runoff and erosion, indicating severe degradation.
Sources (2)
Chapter 5 Soil crusting and sealing - Food and Agriculture Organization of the United Nations
View SourceSoils with low infiltration capacity - Minnesota Stormwater Manual
View SourceSupporting Sources (6)
Additional references from the underlying research that informed this benchmark.
Early Response of Soil Properties and Function to Riparian Rainforest Restoration | PLOS One - Research journals
View SourceEastern NSW Plant Community Type Percentage Cleared Calculation Technical Notes - Environment and Heritage
View SourceEarly response of soil properties and function to riparian rainforest restoration - UQ eSpace
View SourceEarly response of soil properties and function to riparian rainforest restoration - PubMed
View SourceEarly Response of Soil Properties and Function to Riparian Rainforest Restoration - PMC
View SourceSoil erosion as a resilience drain in disturbed tropical forests
View Source