Orogenic Exploration Pty Ltd

Australian Potash Brine


As part of the exploration consulting practice by Orogenic Exploration, an extensive database has been compiled on Australian potash brine deposits.


Over the last 15 years, exploration for brines containing potash has escalated in Australia. Nitrogens (N), phosphates (P) and potash (K) are the three major fertiliser types widely used. Potash is water-soluble, and certain natural brines depending on their chemistry can be used to create Sulphate of Potash (SOP), also called Potassium Sulphate (K2SO4). SOP is a low chloride, premium fertiliser applied primarily on high value crops and is the second most common potash type (after the chloride containing MOP).

Orogenic Exploration has captured and collated available brine water analyses across Australia. This is not just published reserves but all available individual water samples defining a deposit have been captured in detail. This has incorporated the standardisation of the samples geographical and analytical units. While the brine analyses have been completed by different laboratories (e.g. Bureau Veritas, ALS, NTEL, Genalysis) and differing methods (but mainly ICP based) it is apparent that natural fluctuations in saline chemistry due to rainfall and other weather variations are often more significant than variations in analytical procedures.

The data has been captured from ASX company public releases and from open-file company reports from the various Mines Departments. All individual samples have full geographical, sampling and analytical details together with company, exploration licence and reference information. Western Australia has the most prospective known brine lake systems therefore the majority of data is from that state.

Red dots are individual brine water analyses across Australia and the size of the underlying grey circle represents the SOP concentrations (in g/L).

As Sulphate of Potash (SOP) is the primary objective this has been calculated for each brine analysis as a method of ranking individual local surface waters and aquifers. Percival Lakes in northern Western Australia has the highest calculated near surface SOP concentration in Australia. These samples were collected at depths less than a metre below the dry lake surface (Johnston, 2015). The table below lists selected lake systems sorted by decreasing averaged SOP concentrations (in g/L which is the same as kg/m3).

Australian Potash Brine Table - March 2020

Having this detailed data allows for plotting and examination of relationships and trends. The two graphs below show brine potassium (K) concentration verses Sulphur (S) and Sodium (Na) concentrations. Samples from selected lake systems are highlighted and clear trends are evident. Separate grouping of samples from one geographical lake system would indicate separated water bodies, probably related to depth of sample (captured if provided). Often water samples at or very near surface are disconnected from deeper palaeochannel water samples by impervious clay layers associated with the lake sediments.

The data can provide information on the ratios of the different salts. To create SOP from brines you require potassium but sufficient sulphide is also required. Brines having a higher excess of common salt (NaCl) will require extra processing.

K-S plot with Percival-Lake Wells-Kallium Lakes - October 2019 K-Na plot with Percival-Lake Wells-Kallium Lakes - October 2019

Brine water has filled the abandoned Williamson Gold Mine large opencut pit located within (normally dry) Lake Wells near Wiluna in central Western Australia. This single body of water has an average of 25.3 g/L SOP from a number of water samples from different depths and locations across the pit (Salt Lake Potash, ASX release 12/3/2018). The Lake Way pit samples plot close together in the plots above as expected given the very similar salt concentrations from the single body of water.


There appears to be little potential for lithium brines in Australia based on available data. While individual brine analyses are not often released, brines in Argentina can reach at least 1000mg/L in Li concentration (Galan Lithium ASX Release 6/10/19). This compares with the best known lake brine in Australian containing only 3mg/L Li from a lake near Wudinna on the Eyre Peninsula (Belperio & Godsmark, 2017). Unfortunately Lithium is not listed as an analysed element in many brine water samples so there may be better values not reported from Australia. Other than near Wudinna, all available Australian brine analyses are below 1mg/L Li.

While the Geoscience Australia Record 2013/39 (Mernagh (ed), 2013) mentions lithium brine exploration around Lake Dumbleyung in Western Australia and Lakes Torrens and Frome in South Australia both these exploration programs was not successful and quickly abandoned.


Some of the Argentina brines contain up to approximately 600mg/L boron (Candelas area, Galan Lithium Ltd). In Australia the near surface brine with the highest known boron concentration is Lake Auld in Western Australia. River Rock Energy Ltd sample 15WS077 contained 46mg/L and sample 15WS073 contained 42mg/L boron (Johnston, 2015) from this lake. The data on boron is limited, like lithium, with only 15% of available Australian brine available analyses including this element.


While potash brine concentration is a very important parameter in economic assessment, there are many other issues that need to be considered. Thus the data presented here should not and cannot be used in making investing decisions without further external advice. All data is sourced from open-file Mines Department reports or ASX public releases. Orogenic Exploration has taken all due care in the data compilation but takes no responsibility for any errors including errors in the source documentation.

If you are interested in further details on brine in Australia please contact us. If you are aware of any public data omissions, misrepresentation or factual errors please also contact Orogenic Exploration.