Sulphide sediments are fine-grained deposits formed on the Baltic sea bed after the last ice age. The soils are often black in colour due to sulphide minerals. In many areas, land uplift has caused these former sea beds to become land.

Stable below the water table

As long as the sulphide sediments are below the groundwater table, they are stable and have no impact on the surrounding environment. If, however, sulphide soils are exposed to oxygen in the air, the sulphide minerals oxidise. The soil's pH value then decreases sharply and some of its metals become readily mobile. The soil thus formed is called acid sulphate soil. This soil is among the most environmentally harmful soils in the world.

Foton på svart sulfidjord och grå, rostig, sur sulfatjord.Sulphide sediments (left) are often completely black or have black bands and are characterised by a neutral pH. In contact with air, the colour of the soils lightens quickly and their pH decreases. Acid sulphate soils (right) are formed after oxidation of sulphide soil and can often be recognised by the naked eye. They are characterised by vertical cracks covered by a layer of rust. Photo: Gustav  Sohlenius.

Exposed through human activities

Even though the sulphide sediments were formed without human influence, it is often human activities, such as trenching and other excavation, which results in the exposure of these soils to oxygen and thus an adverse effect on the environment. The sulphide sediments are often nutrient-rich and suitable as agricultural land. Therefore, to make cultivation possible, the water table has in many places been lowered by ditches, with the result instead being the formation of acid sulphate soils. Excavation, e.g. due to road construction, can also lead to the exposure of sulphide sediments to oxygen. In order to avoid activities that contribute to the oxidisation of the sulphide mineral and the resultant release of metals and acid, it is therefore important to be aware of where the sulphide sediments occur.

Finland also has large areas of acid sulphate soils where metal and acid leakage has periodically caused major problems with fish death in coastal waters. In these areas, it has been possible to demonstrate that the release of certain metals from acid sulphate soils is greater than that of Finnish industry as a whole. Although the area with acid sulphate soils is less in Sweden than in Finland, it is clear that these soils in some areas have an adverse effect on the environment and that they contribute to a major release of metals.

Sulphide sediments are most commonly occurring along the coast of Norrland

Broadly speaking, we know where in Sweden acid sulphate soils are found. They mainly occur along the coast of Norrland, but also further south, for example around Lake Mälaren. SGU has compiled results from documented occurrences of sulphide sediments and acid sulphate soils along the coast of Norrland. The results show that these soils mainly occur on farmlands in areas with silt and clay soils, where the groundwater surface has been lowered by ditches. Acid sulphate soils are especially abundant close to the coastline in areas which have risen from the sea through isostatic uplift during the last millennia. Acid sulphate soils are most often underlain by sulphide sediments, thus, it is important to avoid land use that will expose these deposits to the atmosphere. The total areal of acid sulphate soils in Västerbotten and Norrbotten is estimated to at least 600 km2

The work has been reported in the publication below.

Sulfidjordar och sura sulfatjordar i Västerbotten och Norrbotten (pdf in Swedish, new window)