RELATIONS BETWEEN ACID ATMOSPHERIC DEPOSITION AND THE SURFACE PH OF SOME OMBROTROPHIC BOGS IN BRITAIN

Citation
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
Citations number
33
Categorie Soggetti
Ecology
Journal title
ISSN journal
00220477
Volume
86
Issue
2
Year of publication
1998
Pages
329 - 340
Database
ISI
SICI code
0022-0477(1998)86:2<329:RBAADA>2.0.ZU;2-U
Abstract
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.