Soil Structure & Compaction

AUS-AMR-FOR-SSC General Moderate confidence

Benchmark Value

No specific value — see range
Range: 500 to 2000 kPa
Optimal Range: 500 to 2000
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 13 benchmarks together — the OptimalRange form drives the primary score, while 12 guard(s) constrain the result.

Evidence & Context

Optimal Range: 500 – 2000 kPa (measured at or near field capacity). This range defines a healthy state for arid upland forest soils.

Metric Definition:

Penetrometer resistance (PR) measured at or near field capacity, indicating soil mechanical strength affecting root growth.

Benchmark Definition:

Penetrometer resistance range indicating optimal soil compaction balancing root growth and water retention in arid mountain upland forest soils.

Justification:

Based on evidence that moderate compaction improves water retention without significantly impeding root growth in arid upland forests.

Sources (1)

Preview of The Influence of Compaction and Soil Strength on the Establishment of Four Australian Landscape Trees | Arboriculture & Urban Forestry
The Influence of Compaction and Soil Strength on the Establishment of Four Australian Landscape Trees | Arboriculture & Urban Forestry Journal

Australia's State of the Forests Report, accessed May 15, 2025

View Source

Supporting Sources (1)

Additional references from the underlying research that informed this benchmark.

Preview of RELATIONSHIPS BETWEEN CONE PENETRATION RESISTANCE, BULK DENSITY, AND MOISTURE CONTENT IN UNCULTIVATED, REPACKED, AND CULTIVATED, accessed July 30, 2025,
RELATIONSHIPS BETWEEN CONE PENETRATION RESISTANCE, BULK DENSITY, AND MOISTURE CONTENT IN UNCULTIVATED, REPACKED, AND CULTIVATED, accessed July 30, 2025,
Direct Evidence Journal

Relationships between cone penetration resistance, bulk density, and moisture content in uncultivated, repacked, and cultivated hardsetting and non-hardsetting soils from the coastal lowlands of south-east Queensland, Australia

View Source

Context

  • Region Australia
  • Biome Arid Mountain Ranges & Uplands
  • Land Use Production Forestry
  • Assessment Pristine Reference
  • Evidence Type ReferenceCondition

Lifecycle

  • Status Active
  • Version 1
  • Effective From 21 Mar 2026

Notes

The optimal range avoids inefficiency of overly loose soils and stays below the 2500 kPa threshold where root growth is severely restricted.