Water Electrical Conductivity (EC)
Benchmark Value
Scoring Curve
The scoring engine could not generate a curve for this benchmark context. The primary form is Point, 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
Peak ECs are significantly higher than the 30uS/cm of undisturbed bogs and may potentially retard bog flora vigour.
Shallow groundwater electrical conductivity within alpine peatlands, measured weekly using a network of piezometers.
Reference baseline electrical conductivity for pristine alpine peat bog groundwater.
This field study provides direct, local measurements of pristine groundwater chemistry in unimpacted, endangered alpine bog ecosystems within Kosciuszko National Park.
Sources (1)
Hocking, R., Greene, R., Hughes, C., Johnston, S., & Grover, S. (2011). The impact of de-icing salts on alpine bogs in Kosciuszko National Park.
View SourceSupporting Sources (6)
Additional references from the underlying research that informed this benchmark.
1.5.2.1 Surface water - Bioregional Assessments |
View SourceNorthern Territory Government (2020) Darwin Harbour Region Water Quality Objectives, Report Card Section 3.0.
View SourceThe Effects of Road De-icing Salts on Water Quality and Macroinvertebrates in Australian Alpine Streams
View SourceNew South Wales Government. (2000). Water Quality Guidelines for the Border Rivers Catchment.
View SourceFeral horses (Equus caballus) increase suspended sediment in subalpine streams
View SourceShenton, M. D., Nichols, S. J., Bray, J. P., Moulding, B. J. G., & Kefford, B. J. (2022). The Effects of Road De-icing Salts on Water Quality and Macroinvertebrates in Australian Alpine Areas.
View Source