Lynham, T. J., Wickware, G. M. and Mason, J. A. 1998. Soil chemical changes and plant succession following experimental burning in immature jack pine. Can. J. Soil Sci. 78: 93-104. In 1975 and 1976, an experimental burning program was conducted in an immature stand of boreal jack pine (Pinus banksiana Lamb.) growing on level, granitic outwash sands in northern Ontario. Nine 0.4-ha plots were burned under a range of fire weather conditions and sampling was conducted to examine the effect of fire on soil chemical changes and revegetation. Results indicated that depth of burn (DOB) affected both soil chemical changes and plant succession on these pine sites. Vaccinium angustifolium Ait., Oryzopsis spp,. Waldsteinia fragarioides (Michx.) Tratt, Salix spp. and Viola adunca Sm. increased in cover at two levels of DOB but the increase was greatest at the lower DOB and decreased to pre-burn levels after 10 yr. Comptonia peregrina (L.) Coult., Epilobium angustifolium L., Polytrichum commune Hedw. and Amelanchier sanguinea (Pursh) DC. were not found in the pre-burn surveys but appeared after burning. Vegetation cover for these species was always higher at the deeper DOB but decreased almost to zero after 10 yr. Other species such as Pleurozium schreberi (Brid.) Mitt., Linnaea borealis L., Corylus cornuta Marsh., Cladina rangiferina (L.) Nyl. and Aralia nudicaulis L. were eliminated from the site and did not recover even after 10 yr. Soil pH increased 0.3 to 1.0 pH units in the organic and mineral soil layers. The rate of increase in pH was always steeper at the higher DOB and pH returned to pre-burn levels in the mineral soil layers after 10 yr. Immediately after burning, exchangeable Ca in the mineral soil layers doubled but 10 yr later, Ca returned to preburn levels. Phosphorus and K increased in the mineral soil, leveled off and were still elevated after 10 yr. Total Kjeldahl N was reduced by 50% in the organic soil while N in all mineral soils increased, and was still increasing after 10 yr. Except for immediate post-fire increases in pH, Ca and N, soil chemical changes were small or they rebounded to pre-burn levels 10 yr after burning. Therefore it is unlikely that these changes were the cause of the plant cover changes that persisted to 10 yr. ) établi sur des sables de délavage granitiques dans le nord de l'Ontario. Neuf placettes de 0,4 ha étaient brûlées dans diverses conditions météorologiques propices aux feux de forêt, après quoi des prélèvements étaient faits pour examiner l'effet du feu sur les modifications chimiques du sol et sur la reprise de la végétation. La profondeur de brûlage (PDB) influait à la fois sur les modifications chimiques du sol et sur les successions floristiques. La couverture du sol fournie par Vaccinium angustifolium Ait., Oryzopsis spp. Waldsteinia fragarioides (Michx.) Tratt, Salix spp. et Viola adunca Sm augmentait aux 2 profondeurs de brûlage, surtout à la profondeur inférieure puis revenait au niveau d'avant le brûlage au bout de 10 ans. Certaines espèces nouvelles comme Comptoni...
On the basis of vegetational physiognomy, 47 sites within 1 to 43 km of the southern James Bay coast were classified in the field into four fen types: graminoid, low shrub, graminoid-rich treed, and sphagnum-rich treed. The four types are directly related to differences in vegetational cover and in soil and water parameters, specifically depth to water level, peat thickness, selected groundwater nutrients, and distance from the coast. Detrended correspondence analysis was used to ordinate the vegetational cover of the fen sites. No one or two of the 16 soil and water parameters obtained in this study could be used to discriminate conclusively among fen types. Linear discriminant function (LDF) analysis, however, indicated that the better discriminators were pH, peat thickness, SO4−, K+, and depth to water level. When all water and soil parameters were used, regrouping by LDF analysis into the four a priori groups was achieved with 78% accuracy. Canonical analysis also showed separations when soil and water parameters for sites were plotted in two dimensions. Because of isostatic rebound, distance from the coast represents a temporal as well as a spatial gradient. Peat depth in the fens increases with distance from the coast, at a mean rate of 4.7 cm for each kilometre inland. Na+ plus Cl− in the groundwater of the fens decreases asymptotically with increasing distance from the coast.
Peatland waters of the Moose River basin, as well as surficial sediments and vascular plants of the estuary were sampled in 1982. Elevated levels of PCBs were found at all five peatland sites; concentrations ranged from 28 to 65 ng/L. Of the seventeen organochlorine pesticides investigated, the hexachlorocyclohexane isomers (a-and y-BHC) were the most prominent with total BHC concentrations ranging from 1.5 to 13.7 ng/L. The presence of these contaminants in ombrotrophic bogs indicated that there was atmospheric deposition of organochlorine contaminants in the basin. Analyses of surficial sediments, collected from tidal flats and coastal marshes, showed that PCBs and organochlorine pesticides were not present. Samples of Triglochin maritima L. seed heads and Typha latifolia L. roots were also free of PCBs.
Two beach ridge soils are described from the area west of Winisk, Ontario, in the Hudson Bay Lowland. These soils, although frozen, are podzolic and incipient-podzolic. The occurrence of frozen podzols in the Lowland indicates vegetational and pedological changes related to regional paludification.
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