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 12 benchmarks together — the OptimalRange form drives the primary score, while 11 guard(s) constrain the result.
Evidence & Context
Therefore, for many TMS soils, particularly those that are not inherently heavy, impermeable clays, SWIR values falling consistently < 5 mm/hr would almost certainly represent a critically low threshold, indicative of severe degradation such as heavy compaction, advanced sodicity, or the formation of a persistent surface crust.
Critically low Soil Water Infiltration Rate threshold indicating severe degradation such as compaction or sodicity.
This benchmark represents a critically low soil water infiltration rate threshold indicating severe soil degradation such as compaction or sodicity in Australian Tropical Monsoonal Savannas production forestry.
Based on general soil infiltration classification systems and USDA guidelines.
Sources (1)
Inherent Factors Affecting Soil Infiltration Infiltration ... - USDA
View SourceSupporting Sources (2)
Additional references from the underlying research that informed this benchmark.
The role of active fractions of soil organic matter in physical and chemical fertility of Ferrosols
View SourceThe effect of three fire regimes on stream water quality, water yield ...
View Source