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Draft DEWCP and EPA guidance on managing acid sulfate soils1 Overview of acid sulfate soils in Western Australia1.1 The purpose of this guidanceThis guidance has been prepared to assist agencies, including local government authorities, to manage development in areas where acid sulfate soils may potentially exist. The advice will also assist individuals and organisations that carry out works that may disturb acid sulfate soils.The purpose of the document is to provide:
A summary of the management advice is the flow-chart in Appendix 1. The information in this guidance should be read in conjunction with the Western Australian Planning Commission's Planning Bulletin No. X: Acid Sulfate Soils.
1.2 Introduction - What are acid sulfate soils?Acid sulfate soil is the common name for soil containing iron sulfides or their oxidation products.When acid sulfate soils are exposed to air, the iron sulfides (commonly iron pyrite) oxidise and produce sulphuric acid, iron precipitates, and concentrations of dissolved metals such as aluminium, iron and arsenic. This leachate has been responsible for environmental damage, damage to infrastructure and buildings, and human health problems. While the eastern coastline of Australia has had to deal with acid sulfate soils problems for some time, Western Australia has, until recently, only infrequently encountered the issue. While, it is thought that acid sulfate soils problems in Western Australia are on a more localised and less severe scale, there is still much to be learnt about the issue. For the purposes of this guidance, acid sulfate soils include both actual acid sulfate soils and potential acid sulfate soils. Actual acid sulfate soils are soils or sediments that contain iron sulfides and/or other sulfidic material that have been exposed to the air and have oxidised, producing highly acidic soil horizons or layers. Queensland and New South Wales guidelines recognise a pH criterion of 4 or less for actual acid sulfate soils. Upon exposure of acid sulfate soils to air, acidity problems may persist for a long time. In some areas of Australia, acid sulfate soils drained 100 years ago are still releasing acid (Sammut 2000). Potential acid sulfate soils (PASS) are soils or sediments which contain iron sulfides and/or other sulfidic material that have not oxidised by exposure to air. Based on criteria in the Queensland and New South Wales guidelines for PASS, the field pH of these soils in their undisturbed state is pH 4 or more and may be neutral or slightly alkaline. These soils or sediments are invariably saturated with water in their natural state. This waterlogged layer may be peat, clay, loam or sand and is usually dark grey and soft. PASS are not associated with environmental problems unless they are exposed to air. While the natural exposure of these soils or sediments to air (eg during severe droughts), is associated with the generation of acid, the acidity tends to occur in low frequency, low magnitude, short duration events after drought breaking rains (NHT 2001). 1.3 Where are acid sulfate soils found?In Western Australia, acid sulfate soils are known to have formed in the following general locations:
Particular areas of concern in Western Australia include (though are not limited to):
In the Perth area, specific examples of disturbances of acid sulfate soils include sediments disturbed during bridge construction at the Garrett Road and Guildford bridges on the Swan River; disturbances in Stirling, Bassendean, Guildford and Bayswater; and exposure of acid sulfate soils in wetlands eg Lake Gnangara. The identification of areas in Western Australia where there may be a risk of disturbing acid sulfate soils is further addressed in Section 2.3 and Appendix 2. 1.4 What types of development may cause acid sulfate soil problems?Developments that involve excavation works or the lowering of the water table in acid sulfate soil risk areas may result in soil, groundwater and/or surface water acidity and the release of metals and precipitates.Examples include:
1.5 What are the potential impacts from disturbing acid sulfate soils?When acid sulfate soils oxidise there may be considerable generation of acid and iron precipitates, and the release of metals such as aluminium, manganese, arsenic and cadmium. Problems from this leachate may persist over a long time, or peak seasonally after dry periods with the first drought breaking rains. Environmental, economic and social impacts may be short term and long term.The potential environmental, social and economic impacts that may be experienced in Western Australia include:
In the Perth region, acid sulfate soils problem have been triggered by the disturbance of wetlands, peat and the lower parts of waterways. The main concerns identified to date in the Perth region are as follows:
1.6 National Strategy for the Management of Coastal Acid Sulfate SoilsIn recognition that a nation-wide co-ordinated approach to managing the acid sulfate soil issue was needed, the National Working Party on Acid Sulfate Soils was set up. The Working Party has developed a National Strategy for the Management of Coastal Acid Sulfate Soils (NWPASS 2000).The National Strategy identifies four principle objectives:
1.7 Statutory controls, and agencies that may provide adviceThe legislation processes and agencies most relevant to acid sulfate soils issues in Western Australia are outlined in this section.The land use planning process is arguably best positioned to ensure that new developments in areas prone to acid sulfate soils are appropriately managed to meet the community's planning objectives. The WAPC has prepared Planing Bulletin No. X: Acid Sulfate Soils to provide advice and guidance on matters that should be taken into account in the rezoning, subdivision and development of land that contains acid sulfate soils. Proposed developments that may disturb acid sulfate soils may also be subject to the provisions of the Environmental Protection Act 1986 - the licensing provisions, the environmental impact assessment process, and/or the provisions of various environmental protection policies. Where pollution arising from the disturbance of acid sulfate soils has occurred, the general pollution prevention provisions of the Act may, depending on the circumstances, be applicable. Groundwater extraction and dewatering in declared public drinking water source areas including underground water pollution control areas, water reserves and public water supply catchment areas declared under the Metropolitan Water Supply, Sewerage and Drainage Act 1909 and the Country Areas Water Supply Act 1947 are subject to licensing by DEWCP. Development within and abutting the Swan River Trust management area generally requires the approval of the Swan River Trust. Similarly, other catchment management authorities eg the authorities for the Peel Inlet, Leschenault Inlet, Wilson Inlet and Albany Harbour areas determine some approvals in their area of jurisdiction. At this stage, the Western Australian government department leading action on the issue is DEWCP. Advice on technical aspects of acid sulfate soils issues is available from DEWCP's Land and Water Quality Branch. Other agencies that may be able to provide advice in relation to specific categories of developments include:
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