Soil Water Infiltration Rate

AUS-TMI-FOR-SWI General Moderate confidence

Benchmark Value

1421 mm/hr
Direction: Higher is desirable ↑
Form: Point

Scoring Curve

Scoring curve unavailable

The scoring engine could not generate a curve for this benchmark context. The primary form is Point, but the benchmark data may be missing required fields (e.g., optimal range bounds for an OptimalRange benchmark). This is typically a data quality issue in the benchmark pipeline.

Evidence & Context

The mean infiltration rate measured in the remnant riparian rainforest was 1421 mm/hr, with a standard deviation of 995 mm/hr, based on measurements from two sites.

Metric Definition:

Soil water infiltration rate is defined as the process of water entering the soil from the surface, measured as the rate at which water infiltrates the soil.

Benchmark Definition:

This benchmark represents the rate at which water enters Ferrosol soils in remnant riparian rainforest, reflecting high soil hydrological function and ecological health in the Tropical & Subtropical Maritime Islands biome under production forestry.

Justification:

This value is selected as the 'best-on-offer' benchmark for high-functioning Ferrosols. The remnant rainforest represents the highest state of ecological health and soil structural integrity achievable on this soil type, making it the ideal aspirational target for a best-practice forestry system.

Sources (2)

Preview of Gageler, R., et al. (2014). Restoring soil carbon, nitrogen and functionality in an Australian tropical catchment: a chronosequence approach. PLOS ONE, 9(8), e104198.
Gageler, R., et al. (2014). Restoring soil carbon, nitrogen and functionality in an Australian tropical catchment: a chronosequence approach. PLOS ONE, 9(8), e104198. Journal

Early Response of Soil Properties and Function to Riparian Rainforest Restoration - PMC

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Preview of USDA Natural Resources Conservation Service. (n.d.). Soil Quality Indicators: Infiltration.
USDA Natural Resources Conservation Service. (n.d.). Soil Quality Indicators: Infiltration. Journal

Natural Resources Conservation Service (USDA NRCS)

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Supporting Sources (3)

Additional references from the underlying research that informed this benchmark.

Preview of Early response of soil properties and function to riparian rainforest restoration - Lake Baroon Catchment Care Group, accessed July 18, 2025,
Early response of soil properties and function to riparian rainforest restoration - Lake Baroon Catchment Care Group, accessed July 18, 2025,
Direct Evidence GreyLiterature

Ecology of Nitrogen Fixing, Nitrifying, and Denitrifying ...

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Preview of Gregory, J. H., et al. (2006). Effect of urban soil compaction on infiltration rate. Journal of Soil and Water Conservation, 61(3), 117-124.
Gregory, J. H., et al. (2006). Effect of urban soil compaction on infiltration rate. Journal of Soil and Water Conservation, 61(3), 117-124.
Direct Evidence Journal

Gregory, J. H., et al. (2006). Effect of urban soil compaction on infiltration rate. Journal of Soil and Water Conservation, 61(3), 117-124.

View Source
Preview of NSW Local Land Services. (2021). Healthy soils and water infiltration in the paddock.
NSW Local Land Services. (2021). Healthy soils and water infiltration in the paddock.
Direct Evidence

NSW Local Land Services. (2021). Healthy soils and water infiltration in the paddock.

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Context

  • Region Australia
  • Biome Tropical & Subtropical Maritime Islands
  • Land Use Production Forestry
  • Assessment Pristine Reference
  • Vegetation Forest
  • Evidence Type ReferenceCondition

Lifecycle

  • Status Active
  • Version 1
  • Effective From 5 Jun 2026

Notes

Lower Critical Threshold: 30 mm/hr. No upper detrimental threshold — higher values are always better up to natural saturation. High infiltration may increase nutrient leaching risk, which is a management consideration.