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 14 benchmarks together — the OptimalRange form drives the primary score, while 13 guard(s) constrain the result.
Evidence & Context
Based on this evidence, a lower critical threshold (i.e., an upper limit for acceptable penetrometer resistance) of >2000 kPa is proposed for agricultural crop production in the alpine and subalpine context.
Soil penetrometer resistance measured as the force required to push a standardized cone through the soil profile, expressed in kilopascals (kPa).
This benchmark defines the maximum penetrometer resistance threshold beyond which soil functions and crop productivity are significantly impaired in agricultural crop production within the Australian alpine and subalpine biome.
Based on consistent findings across agricultural studies indicating significant root impediment and functional decline at penetrometer resistances exceeding 2000-2500 kPa.
Sources (3)
Ripping Mallee soils, what are the production benefits? - Agronomy Australia Proceedings
View SourceDiagnosing Soil Compaction Using a Penetrometer - Sherman
View SourceSoil Compaction in Annual Crop Production: Causes, Impacts, and Solutions - WSU Research Exchange
View SourceSupporting Sources (3)
Additional references from the underlying research that informed this benchmark.
Identify Soil Compaction to Boost Crop Yields - Innoquest Inc
View SourceCritical Limits for Soybean and Black Bean Root Growth, Based on ...
View SourceUnderstanding Soil Compaction: How It Affects Crop Yield in Agriculture
View Source