Mcf. Proctor et E. Maltby, RELATIONS BETWEEN ACID ATMOSPHERIC DEPOSITION AND THE SURFACE PH OF SOME OMBROTROPHIC BOGS IN BRITAIN, Journal of Ecology, 86(2), 1998, pp. 329-340
1 Analyses are presented of major ion concentrations in surface water
samples, and exchangeable cations in peats, collected in November-Dece
mber 1992 from 16 ombrotrophic bogs in England and Wales and one in Sc
otland, spanning most of the range from the lowest (Dartmoor, west Wal
es, west Highlands) to the highest (south Pennines, north Yorkshire) o
f the mean 1986-88 rainwater concentrations of hydrogen ions and non-m
arine sulphate (NMS). 2 There was a strong positive correlation (r = 0.89) between surface water pH and mean rainwater pH, and a less close
correlation (r = +0.71) between surface water pH and total hydrogen i
on deposition. 3 The correlation between surface water pH and mean con
centration of rainwater NMS (which may be taken as a surrogate measure
of acid deposition) was r = -0.85, and that between surface water pH
and total deposition of NMS was r = -0.65. 4 The intercept of the regr
ession of surface water pH on NMS is at pH 4.40 (95% confidence limits
4.22-4.58), suggesting this as the winter pH of an ombrotrophic bog s
urface in the absence of acid atmospheric pollution. 5 Total sulphur c
ontent of intact surface peats from 11 sites correlated well (r = +0.9
0) with mean rainwater total sulphate concentration. 6 The H+ ion conc
entration in wet deposition, plus the net H+ input resulting from meta
bolism of deposited NO3- and NH4+, is insufficient to account for the
difference between the inferred pH of an unpolluted bog surface and pH
values (up to 0.8 pH units lower) measured in the field in polluted s
ites. Analogy with deposition of NMS suggests that this discrepancy is
accounted for quantitatively by seeder-feeder enhancement, cloudwater
deposition, and dry deposition of acidity. 7 Ombrotrophic bog surface
waters are buffered by the cation-exchange properties of the peat. Th
ey are likely to be less sensitive to moderate acid deposition than we
akly bicarbonate-buffered near-neutral peats, soils and fresh waters.