Soil Moisture
Benchmark Value
Scoring Curve
The scoring engine could not generate a curve for this benchmark context. The primary form is CompositeFramework, 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
Numerically, drawing from the global ranges of θcrit 13, this threshold could vary from approximately 12% VWC (for coarser textured soils in the drier parts of the biome) to 20% VWC (for finer textured soils in more mesic areas within the biome), below which significant plant water stress and impairment of ecosystem functions occur.
Lower critical threshold for soil moisture where significant plant water stress begins and primary productivity markedly declines.
The lower critical threshold is the soil moisture content below which ecosystem function is impaired due to water stress in temperate dry woodlands and native grasslands under livestock grazing.
This threshold is based on global ranges of critical soil moisture thresholds (θcrit) and varies with soil texture and local conditions.
Sources (1)
Global critical soil moisture thresholds of plant water stress - ResearchGate
View SourceSupporting Sources (2)
Additional references from the underlying research that informed this benchmark.
Pasture yield and soil physical property responses to soil compaction from treading and grazing — a review - ANU Open Research
View SourceSoil | Australia state of the environment 2021
View Source