Soil Water Infiltration Rate

AUS-TDG-LVG-SWI General Moderate confidence

Benchmark Value

No specific value — see range
Range: 25 to 75 mm/hr
Optimal Range: 25 to 75
Direction: Higher is desirable ↑
Form: OptimalRange

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.

Evidence & Context

While specific values will vary with soil type, a reasonable expectation for steady-state SWIR under best-practice management on moderately textured soils (loams, clay loams) in this biome would likely be in the range of 25 - 75 mm/hr.

Metric Definition:

Soil Water Infiltration Rate (SWIR) quantifies the rate at which water enters the soil profile at the surface.

Benchmark Definition:

This benchmark represents the expected steady-state soil water infiltration rate under best-practice grazing management on moderately textured soils in the Temperate Dry Woodlands & Native Grasslands biome of Australia. It indicates the rate at which water enters the soil surface, reflecting healthy soil hydrological function.

Justification:

The benchmark is grounded in well-established principles of soil physics and hydrology and supported by multiple studies demonstrating the positive impact of best-practice grazing on factors controlling infiltration. Evidence also clearly indicates critical low thresholds associated with degradation. However, confidence is moderated by the lack of direct, replicated field measurements of SWIR specifically from sites confirmed as representing the 'best available condition' under regenerative grazing across the diverse Australian Temperate Dry Woodlands & Native Grasslands biome. The proposed range is therefore derived through synthesis and interpretation of related data and principles, acknowledging inherent site-specific variability.

Sources (2)

Preview of Adaptive multi-paddock grazing improves water infiltration in Canadian grassland soils | Request PDF - ResearchGate
Adaptive multi-paddock grazing improves water infiltration in Canadian grassland soils | Request PDF - ResearchGate Journal

Adaptive multi-paddock grazing improves water infiltration in Canadian grassland soils | Request PDF - ResearchGate, accessed May 12, 2025

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Preview of Soil structure, soil hydraulic properties and the soil water balance - ResearchGate
Soil structure, soil hydraulic properties and the soil water balance - ResearchGate
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Supporting Sources (6)

Additional references from the underlying research that informed this benchmark.

Preview of (PDF) Final report Scoping Study of Soil Management in Livestock ..., accessed May 12, 2025
(PDF) Final report Scoping Study of Soil Management in Livestock ..., accessed May 12, 2025
Contextual Support GreyLiterature

(PDF) Final report Scoping Study of Soil Management in Livestock ..., accessed May 12, 2025

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Preview of (PDF) Response of Grazing Land Soil Health to Management Strategies: A Summary Review - ResearchGate, accessed May 12, 2025
(PDF) Response of Grazing Land Soil Health to Management Strategies: A Summary Review - ResearchGate, accessed May 12, 2025
Contextual Support Journal

Soil compaction controls the abundance, biomass and distribution of earthworms in a single dairy farm in south-eastern Australia - ResearchGate, accessed May 12, 2025

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Preview of Do regenerative grazing management practices improve vegetation and soil health in grazed rangelands? Preliminary insights from a space-for-time study in the Great Barrier Reef catchments, Australia - CSIRO Publishing, accessed August 5, 2025,
Do regenerative grazing management practices improve vegetation and soil health in grazed rangelands? Preliminary insights from a space-for-time study in the Great Barrier Reef catchments, Australia - CSIRO Publishing, accessed August 5, 2025,
Contextual Support

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.

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Preview of Removing Grazing Pressure from a Native Pasture Decreases Soil Organic Carbon in Southern New South Wales, Australia - ResearchGate
Removing Grazing Pressure from a Native Pasture Decreases Soil Organic Carbon in Southern New South Wales, Australia - ResearchGate
Contextual Support

Removing Grazing Pressure from a Native Pasture Decreases Soil Organic Carbon in Southern New South Wales, Australia - ResearchGate

View Source
Preview of Significance of terms used to predict the effect of rainfall and herbage mass on runoff, accessed May 12, 2025
Significance of terms used to predict the effect of rainfall and herbage mass on runoff, accessed May 12, 2025
Contextual Support Journal

Significance of terms used to predict the effect of rainfall and herbage mass on runoff, accessed May 12, 2025

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Preview of SNOWY MOUNTAIN FORESTED HILLSLOPE SOIL CHARACTERISATION, SOIL HYDROLOGICAL PROPERTIES AND SOIL GEOCHEMISTRY PROGRAM (Data derived from research linked to Save our Snow Gum (SOSG) project and Australian Mountain Research Facility (AMRF))
SNOWY MOUNTAIN FORESTED HILLSLOPE SOIL CHARACTERISATION, SOIL HYDROLOGICAL PROPERTIES AND SOIL GEOCHEMISTRY PROGRAM (Data derived from research linked to Save our Snow Gum (SOSG) project and Australian Mountain Research Facility (AMRF))
Direct Evidence Journal

Dynamics of Sudanian Savanna-Woodland Ecosystem in Response to Disturbances - - Administrative page for SLU library, accessed May 12, 2025

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Context

  • Region Australia
  • Biome Temperate Dry Woodlands & Native Grasslands
  • Land Use Livestock Grazing & Pasture
  • Assessment Pristine Reference
  • Evidence Type TargetCondition

Lifecycle

  • Status Active
  • Version 1
  • Effective From 24 Mar 2026

Notes

No upper detrimental threshold — higher values are always better up to natural saturation. Benchmark represents a functional state achieved under best-practice regenerative grazing, characterized by SWIR significantly above degradation thresholds. Represents expected steady-state rates on moderate-textured soils; initial rates may be higher.

Related Benchmarks

Other benchmarks in the AUS-TDG-LVG-SWI family.