Water Electrical Conductivity (EC)
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 7 benchmarks together — the OptimalRange form drives the primary score, while 6 guard(s) constrain the result.
Evidence & Context
It explicitly defines that any spring system where the water is consistently at or above 5,000 μS/cm is considered too saline to be classified as part of the protected ecological community.
Upper detrimental threshold for Water Electrical Conductivity (EC) indicating the salinity level beyond which the karstic groundwater-dependent ecosystem is considered too saline to maintain its ecological integrity.
This benchmark marks the upper salinity limit beyond which the karstic groundwater-dependent ecosystem is considered degraded and no longer part of the protected ecological community in the Arid Karstic Woodlands & Shrublands biome.
This threshold is based on official conservation advice for a threatened ecological community in a semi-arid South Australian karst system, marking a fundamental change in ecosystem state.
Sources (1)
Conservation Advice for the Karst springs and associated alkaline fens of the Naracoorte Coastal Plain Bioregion
View SourceSupporting Sources (18)
Additional references from the underlying research that informed this benchmark.
How to Calculate Electrical Conductivity From TDS? - Rika Sensor, accessed July 27, 2025,
View SourceGeological Control upon Groundwater Flow and Major Ion Chemistry with Influence on Basin Management in a Coastal Aquifer, South Australia - Scientific Research Publishing, accessed July 27, 2025,
View SourceCONSULTATION INFORMATION PACK Establishing baseline data for the conservation of Koonalda Cave, accessed July 27, 2025,
View SourceDEPARTMENT OF MINES AND ENERGY SOUTH AUSTRALIA REPORT BOOK 96/10 MUSGRAVE PROCLAIMED WELLS AREA GROUNDWATER ASSESSMENT by A J L - NET
View SourceEyre Peninsula Groundwater Dependent Ecosystem Scoping Study - Department for Environment and Water, accessed July 27, 2025,
View SourceGSA Today - The evolution of end-member continental waters: The origin of acidity in southern Western Australia, accessed July 27, 2025,
View SourceThe Nullarbor deserves better protection - La Trobe University, accessed July 27, 2025,
View SourceInvestigation on the groundwater resources of the South Eyre Peninsula, South Australia, determined from laterally constrained inversion of tempest data - ResearchGate, accessed July 27, 2025,
View SourceKarst and agriculture in Australia - Digital Commons @ USF, accessed July 27, 2025,
View SourceNullarbor Plain - Wikipedia, accessed July 24, 2025
View SourcePalaeovalley Groundwater Resources in Arid and Semi-Arid Australia, accessed July 27, 2025,
View SourceStygofaunal community trends along varied rainfall conditions: Deciphering ecological niche dynamics of a shallow calcrete in We - Archimer, accessed July 27, 2025,
View SourceTDS and EC Conversion - Snowate, accessed July 27, 2025,
View SourceKarst and agriculture in Australia - Digital Commons @ USF, accessed July 23, 2025
View SourceTotal dissolved solids | Australian Drinking Water Guidelines - NHMRC, accessed July 13, 2025
View SourceWater Data SA 62 Available Data - WaterConnect, accessed August 1, 2025
View SourceFalls in groundwater for southern Eyre Peninsula in South Australia force 2024 decision for plant to desalinate seawater | Adelaide AZ, accessed July 27, 2025,
View SourceInterim Management Guidelines For The Nullarbor Caves And Selected Karst Features - ACKMA 1973 - 2011, accessed July 27, 2025,
View Source