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 6 benchmarks together — the OptimalRange form drives the primary score, while 5 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 critical hydrological failure occurs.
This benchmark defines the critical soil water infiltration rate below which the soil is effectively sealed, causing severe runoff, erosion, and risk of irreversible land degradation in tropical and subtropical rainforest conservation areas.
Supported by research on agricultural soils showing severe runoff and erosion at this infiltration rate.
Sources (2)
Early Response of Soil Properties and Function to Riparian Rainforest Restoration - PMC
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 SourceTASVEG VCA Manual: A manual for assessing vegetation condition in Tasmania, Version 2.0. Natural and Cultural Heritage, Department of
View SourceChapter 5 Soil crusting and sealing - Food and Agriculture Organization of the United Nations
View SourceEarly Response of Soil Properties and Function to Riparian Rainforest Restoration - PMC, accessed August 2, 2025
View SourceEarly response of soil properties and function to riparian rainforest restoration - PubMed, accessed August 2, 2025
View SourceRunoff generation in tropical forests (Chapter 14) - Forests, Water and People in the Humid Tropics - Cambridge University Press
View Source