Soil Water Infiltration Rate
Benchmark Value
Scoring Curve
This curve shows how a field measurement for this indicator would score across all available benchmark forms in this context.
Evidence & Context
Reference values for other key soil types found within the floodplain system include: Sandy Loams (e.g., Red-Brown Earths/Chromosols): Typically found on levees and higher ground, these soils have intrinsically higher infiltration rates. A healthy range is given as 30–120 mm/day.
Soil Water Infiltration Rate as the final infiltration rate for healthy sandy-loam to light clay loam soils (Chromosols).
This benchmark represents the final infiltration rate for healthy sandy-loam to light clay loam soils in the Arid Inland Floodplains & Ephemeral River Systems biome under production forestry land use.
Represents healthy sandy-loam to light clay loam soils found on levees and higher ground.
Sources (1)
Appendix H - Water Infiltration Modelling - NTEPA
View SourceSupporting Sources (30)
Additional references from the underlying research that informed this benchmark.
Managing soils - Department of Primary Industries and Regional Development, accessed July 8, 2025,
View SourceReview of fertiliser use in Australian forestry - Forest & Wood Products Australia
View SourceAn Event-Based Approach to the Hydrology of Arid Zone Rivers in the Channel Country of Australia | Request PDF - ResearchGate
View SourceArid Swamps | WetlandInfo
View SourceAustralia's State of the Forests Report
View SourceChange in Organic Carbon in Forest Plantation Soils in Eastern ..., accessed July 20, 2025,
View SourceExtensive Management Promotes Plant and Microbial Nitrogen Retention in Temperate Grassland | PLOS One - Research journals
View SourceLandscape Function Analysis: A System for Monitoring Rangeland ...
View SourceLearning More About Ephemeral Creeks | Flow-MER
View SourceComparing infiltration rates in soils managed with conventional and alternative farming methods: A meta-analysis
View SourceDescription of Ecological Communities: Arid Eucalypt Woodlands - DCCEEW
View SourceDISPERSIVE SOIL MANUAL - Grains Research and Development Corporation (GRDC)
View SourceHydraulic Failure Defines the Recovery and Point of Death in Water-Stressed Conifers | Plant Physiology | Oxford Academic
View SourceEcosystem wicks: Woodland trees enhance water infiltration in a fragmented agricultural landscape in eastern Australia, accessed May 15, 2025,
View Sourcerisks and impacts of plant industries on soil condition - Department of Agriculture and Fisheries
View SourceInvestigating Plant Responses to Water Stress via Plant Hydraulics Pathway - EGUsphere
View SourceInnovative Forestry and Forest Industries Research in Australia
View SourceProtection of Lake Eyre Basin rivers and floodplains - Queensland Environment Department
View SourceQuantifying water requirements of riparian river red gum (Eucalyptus camaldulensis) in the Murray-Darling Basin, Australia: Implications for the management of environmental flows - USGS Publications Warehouse
View SourceRIvER RED guMs AND wooDLAND FoREsts - Natural Resources Commission
View SourceRiver red gum – more than just a tree - CSIROpedia
View SourceSoil condition | NSW State of the Environment
View SourceRiverine soils: a guide to the soils of the Lower Murrumbidgee Floodplain
View SourceMicrobial impact on initial soil formation in arid and semiarid environments under simulated climate change - Frontiers, accessed July 28, 2025
View SourceAnalysing water sensitive urban design options - Australian Water Association
View SourceThe-Potential-Use-for-Groundwater-Use-by-Vegetation-in-the-Aust.-Arid-Zone.pdf - Northern Territory Government
View SourceThe floodplain inundation history of the Murray-Darling Basin through two-monthly maximum water depth maps - PMC
View SourceGrey Box (Eucalyptus microcarpa) Grassy Woodlands and Derived ...
View SourceRegenerative agriculture in Australia: the changing face of farming - Frontiers, accessed July 16, 2025,
View SourceRestoration of degraded grazing country in the semi-arid areas of NSW
View Source