Drain/replace acidic water
Overall effectiveness category Unknown effectiveness (limited evidence)
Number of studies: 2
Background information and definitions
Peatlands can hold onto acidic water, especially in thick carpets of moss. This is a natural process in the development of peatlands from fens to bogs (Rydin & Jeglum 2013). However, where the desired plant community is a fen, intervention may be needed to reduce acidity. Fen plants prefer weakly acidic, neutral or even alkaline peat (approximately pH 6–8, similar to saliva, tap water or sea water). Ditches can be dug to drain excess surface water (especially during periods of heavy rain). This may be replaced by less acidic water naturally, or with further intervention.
Caution: Peatland vegetation is very sensitive to water quantity and quality (Rydin & Jeglum 2013). If acidic water is drained, it will probably have to be replaced to prevent the peatland drying out. The chemistry of this water should be carefully monitored or controlled to avoid changing the chemical conditions of the peatland. This intervention is generally not applicable to bogs, which are naturally acidic.
Rydin H. & Jeglum J.K. (2013) The Biology of Peatlands, Second Edition. Oxford University Press, Oxford.
Supporting evidence from individual studies
A controlled study in 1989–1993 in a degraded floating fen in the Netherlands (Beltman et al. 1996) reported that draining acidic surface water increased herb cover, but only when moss was also removed. These results were not tested for statistical significance. Drainage alone had no effect on vegetation cover. After four years, a drained and undrained plot had similar vegetation cover (total moss: 93%; Sphagnum: 62%; herbs: 3%). However, drainage in combination with moss removal favoured herbs. A plot drained and cleared of moss developed 76% herb cover with 0% moss cover. In contrast, a plot cleared of moss but not drained regained high moss cover (total moss: 96%; Sphagnum: 53%; herbs: <1%). In 1989, a ditch was built to drain surface water from two 16 m2 plots in an acidified, nutrient-enriched fen. Two other plots were not drained. In 1991, the moss carpet was also cleared from one drained and one undrained plot. In 1995, vegetation cover was recorded in six 1 m2 quadrats/plot.Study and other actions tested
A controlled, before-and-after study in 1991–1996 in a degraded floating fen in the Netherlands (Bootsma et al. 2002) reported that draining acidic surface water (and replacing it with less acidic water) increased plant species richness and Sphagnum moss cover, but had no effect on sedge or common reed abundance. These results were not tested for statistical significance. Before intervention, plots contained approximately 16 species. After five years, drained plots contained 22–43 plant species, compared to 14–16 species in undrained plots. Drained plots had 41–100% Sphagnum cover, compared to 21–40% in undrained plots. Drain and undrained plots had similar cover of sedge Carex nigra (0–20%) and abundance of common reed Phragmites australis (in 81–100% of quadrats). Effects of drainage on cottongrass Eriophorum angustifolium abundance were more complicated and depended on whether moss was also removed (see original paper). In January 1992, ditches were built to drain surface water from one plot in an acidified, nutrient-enriched fen. An inflow of less acidic water was also created. Water was not manipulated in a neighbouring plot. Within each plot, surface moss was cleared from three subplots but not three others. Between 1991 and 1996, vegetation was estimated in quadrats covering 6–8 m2 of each subplot.Study and other actions tested