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
Therefore, a value of >100 mm/hr is selected as the benchmark representing a state of high ecological function.
Soil Water Infiltration Rate (SWIR) is the rate at which water enters the soil surface, measured in millimeters per hour.
The benchmark represents the minimum soil water infiltration rate indicative of high ecological function in well-structured soils under best-practice regenerative grazing.
Derived from analogous tropical mainland grazing systems and fundamental soil physics principles, reflecting a state of high biomass and soil organic matter.
Sources (2)
CSIRO (2016)
View SourceThe effect of soil and pasture attributes on rangeland infiltration rates in northern Australia
View SourceSupporting Sources (2)
Additional references from the underlying research that informed this benchmark.
Ludwig, J.A., Bastin, G.N., Chewings, V.H., Eager, R.W., and Liedloff, A.C. (2005). Clearing savannas for use as rangelands in Queensland: Altered landscapes and water-erosion processes. Rangeland Journal, 27(2), 135-149.
View SourceClimate-Affected Australian Tropical Montane Cloud Forest Plants: Metabolomic Profiles, Isolated Phytochemicals, and Bioactivities - PubMed Central
View Source