Soil Structure & Compaction
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 13 benchmarks together — the OptimalRange form drives the primary score, while 12 guard(s) constrain the result.
Evidence & Context
Values >3000−3500 kPa indicating conditions where root growth virtually ceases.
Penetrometer resistance level at which root growth virtually ceases.
Critical upper threshold for penetrometer resistance beyond which root growth stops.
Severe compaction at this level leads to profound loss of soil function.
Sources (1)
high soil strength - fact sheet - Grains Research and Development Corporation (GRDC)
View SourceSupporting Sources (9)
Additional references from the underlying research that informed this benchmark.
(PDF) Management of compaction during harvest of Pinus plantations in Queensland: I. Policy considerations for controlling machine activity. 1 - ResearchGate
View SourceState forests around Bombala - Forestry Corporation, accessed August 17, 2025,
View SourceDistribution, nature and threats to soils of the Australian Alps: A ...
View SourceImpacts of Logging-Associated Compaction on Forest Soils: A Meta-Analysis - Frontiers
View SourceNew South Wales Regional Forest Agreements - DAFF
View SourceShort-term effects in canopy gap area on the recovery of compacted soil caused by forest harvesting in old-growth Oriental beech (Fagus orientalis Lipsky) stands - iForest - Biogeosciences and Forestry
View SourceSoil Compaction and Productivity Evolution in a Harvested and Grazed Mediterranean Scots Pine (Pinus sylvestris L.) Forest - MDPI
View SourceSoil Compaction and Productivity Evolution in a Harvested and Grazed Mediterranean Scots Pine (Pinus sylvestris L.) Forest - ResearchGate
View SourceSoil Conservation Guidebook - Gov.bc.ca
View Source