Abstract
Few quantitative studies have been done on the hydrology of fens, bogs, and mires. Consequently predicting the cumulative impacts of disturbances on their hydrologic functions is extremely difficult. For example, few data are available on the role of bogs and fens with respect to flood desynchronization and shoreline anchoring. However, recent studies suggest that very small amounts of groundwater discharge are sufficient to radically modify mire surface-water chemistry, and consequently, vegetation communities and their associated surface-water hydrology. Bogs and fens are, in a sense, hydrobiologic systems, and any evaluation of cumulative impacts will have to (1) consider the complicated and little understood interactions among wetland hydrology, water chemistry, and biota, and (2) place the effect of individual wetland impacts within the context of the cumulative impacts contributed to the watershed from other geomorphic areas and land uses.
It is difficult to evaluate the potential cumulative impacts on wetland hydrology because geologic settings of wetlands are often complex and the methods used to measure wetland streamflow, groundwater flow, and evapotranspiration are inexact (Winter 1988). This is especially so for bogs, fens, and mires underlain by thick organic soils. These wetlands, found in the circumboreal areas of North America, Europe, and Asia, are major physiographic features in eastern North America, northern Europe, and Siberia (Kivenen and Pakarinen 1981, Gore 1983, Glaser and Janssens 1986). Their very scale makes it difficult to quantify the hydrologic function accurately. The hydrology of small bogs and fens found elsewhere is just as poorly understood because of conflicting conceptual models of pertinent hydrologic processes.
This article (1) reviews our current understanding of the hydrologic function of bogs, fens, and mires at different scales and in different physiographic settings and (2) presents hypotheses on potential cumulative impacts on the hydrologic function that might occur with multiple disturbances.
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Literature cited
Adamus, P. R. 1983. A method for wetland functional assessment, vol. II FHWA assessment method. U.S. Federal Highway Administration Report FHWA-IP-82-24. National Technical Information Service, Springfield, Virginia, 134 pp.
Bay, R. R. 1967. Groundwater and vegetation in two peat bogs in northern Minnesota.Ecology 48:308–310.
Boelter, D. H. 1965. Hydraulic conductivity of peats.Soil Science, 100:227–231.
Boelter, D. H. 1969. Physical properties of peats related to degree of decomposition.Proceedings of the Soil Science Society of America, 33:606–609.
Boelter, D. H., and E. S. Verry. 1977. Peatland and water in the northern lake states. U.S. Department Forest Service General Technical Report NC-31, U.S. Forest Service, Washington, D.C.
Boldt, D. R. 1986. Computer simulations of groundwater flow in a raised bog system, Glacial Lake Agassiz Peatlands, northern Minnesota. Thesis, Syracuse University, Syracuse, New York, 52 pp.
Brooks, K. N. 1988. Model of surface hydrology.In: H. E. Wright, Jr. (ed.), The patterned peatlands of northern Minnesota. University of Minnesota Press, Minneapolis, Minnesota, in press.
Chason, D. B., and D. I. Siegel. 1986. Hydraulic conductivity and related properties of peat, Lost River Peatland, northern Minnesota.Soil Science 142:91–99.
Clymo, R. S. 1973. The growth ofSphagnum. Some effects of measurement.Journal of Ecology 61:849–869.
Cowartin, L. M., V. Carter, F. C. Golet, and E. T. LaRoe. 1979. Classification of wetlands and deepwater habitats of the United States. FWS/OBS-79/31, U.S. Fish and Wildlife Service, Washington, D.C., 103 pp.
Dilley, A. C., and I. Helmond. 1973. The estimation of net radiation and potential evapotranspiration using atmometer measurements.Agricultural Meteorology 12:1–11.
Glaser, P. H., and J. A. Janssens. 1986. Raised bog in eastern North America: transitions in landforms and gross stratigraphy.Canadian Journal of Botany 64:395–415.
Glaser, P. H., D. I. Siegel, and J. A. Janssens. 1986. The detection of groundwater discharge in extensive peatlands by remote sensing. Abstract Proceedings of the IVth International Congress of Ecology, Syracuse, New York, August 1986, pp. 159–160.
Glaser, P. H., G. A. Wheeler, E. Gorham, and H. E. Wright, Jr. 1981. The patterned mires of the Red Lake Peatland, northern Minnesota.Journal of Ecology 69:575–599.
Gore, A. J. P. (ed.). 1983. Mires-swamp, bog, fen, and moor: general studies, vol. 4A, Elsevier, Amsterdam, The Netherlands. 440 p.
Gorham, E. 1957. The development of peatlands.Quarterly Review of Biology 32:145–166.
Guertin, D. P., and K. N. Brooks. 1985. Modeling streamflow response from Minnesota Peatlands. Pages 123–131 in Proceedings of the Symposium on Watershed Management, American Society Civil Engineering, Denver, Colorado, April 1985.
Heinselman, M. L. 1963. Forest sites, bog processes, and peatland types in the Glacial Lake Agassiz region, Minnesota.Ecological Monographs 33:327–372.
Heinselman, M. L. 1970. Landscape evolution, peatland types, and the environment in the Lake Agassiz Peatland Natural Area, Minnesota.Ecological Monographs 40:235–261.
Hemmond, H. F., and J. C. Goldman. 1985. On non-Darcian water flow in peat.Journal of Ecology 73:579–584.
Ingram, H. A. P. 1967. Problems of hydrology and plant distribution in mires.Journal of Ecology 55:711–724.
Ingram, H. A. P. 1982. Size and shape in raised mire ecosystems: a geophysical model.Nature 297:300–303.
Ingram, H. A. P. 1983. Hydrology. Pages 67–158in A. J. P. Gore (ed.), Mires-swamp, bog, fen, and moor: general studies, vol. 4A, Elsevier, Amsterdam, The Netherlands.
Ivanov, K. E. 1981. Water movement in mires. Academic Press, London.
Jones, J. A. A. 1981. The nature of soil piping: a review of research. British Geomorphological Research Group Research Monograph Series 3, Geo Books, Norwich, England.
Kivenen, E., and P. Pakarinen. 1981. Geographical distribution of peat resources and major peatland complex types in the world.Annales Academici Scientice Fennici, Series A3 132:5–28.
Newson, M. D. and Harrison, J. G. 1978. Channel studies in the Plynlimon experimental catchments. Institute Hydrology Wallingford Report No. 47: 61 p.
Novitzki, R. P. 1978. Hydrologic characteristics of Wisconsin wetlands and their influence on floods. Pages 377–388in P. Greson, J. R. Clark, and J. E. Clark (eds.), Wetland functions and values: the state of our understanding. American Water Resources Association, Minneapolis, Minnesota.
Penman, H. L. 1963. Vegetation and hydrology. Commonwealth Agricultural Bureau, Farnham Royal, Essex, 124 pp.
Romanov, V. V. 1968. Hydrophysics of bogs. Israel Program of Scientific Translations, Jerusalem, 299 pp.
Rycroft, D. W., D. J. A. Williams, and H. A. P. Ingram. 1975. The transmission of water through peat. I. Review.Journal of Ecology 63:535–556.
Sander, J. E. 1976. An electric analog approach to bog hydrology.Groundwater 14:30–35.
Sokolov, A. A., and T. G. Chapman (eds.). 1974. Methods for water balance calculations, UNESCO Press, Paris, 127 pp.
Siegel, D. I. 1981. Hydrogeologic setting of the Glacial Lake Agassiz Peatlands, northern Minnesota. U.S. Geological Survey Water Resources Investigations 81-24, U.S. Geological Survey, Washington, D.C.
Siegel, D. I. 1983. Groundwater and the evolution of patterned mires, Glacial Lake Agassiz Peatlands, northern Minnesota.Journal of Ecology 71:913–921.
Siegel, D. I. 1987. A review of the recharge-discharge function of wetlands. Pages 59–66 in D. D. Hook, W. H. McKee, Jr., H. K. Smith, J. Gregory, V. G. Burrell, Jr., M. R. DeVoe, R. E. Sojka, S. Gilbert, R. Banks, L. H. Stolzy, C. Brooks, T. D. Mathews, and T. H. Shear (eds.), The ecology and management of wetlands, vol. 1: Ecology of wetlands, Croom Helm, London, England.
Siegel, D. I. 1988a. The recharge-discharge function of wetlands near Juneau, Alaska: Part I. Hydrologic studies.Journal of Groundwater, 26;427–434.
Siegel, D. I. 1988b. The recharge-discharge function of wetlands near Juneau, Alaska: Part II. Geochemical studies:Journal of Groundwater, in press.
Siegel, D. I. 1988c. A model for groundwater flow.In H. E. Wright (ed.), The patterned peatlands of northern Minnesota. University of Minnesota Press, Minneapolis, Minnesota, in press.
Siegel, D. I., and P. H. Glaser. 1987. Groundwater flow in a bog/fen complex, Lost River Peatland, northern Minnesota.Journal of Ecology, 75:743–754.
Sjörs, H. 1963. Bogs and fens on Attawapiskat River, northern Ontario.Contributions in Botany of the National Museum of Canada Bulletin 186:45–133.
Tallis, J. H. 1973. Studies on southern Pennine peats. V. Direct observations of peat erosion and peat hydrology at Featherbed Moss, Derbyshire.Journal of Ecology 61:1–22.
Thornthwaite, C. W. 1948. An approach toward a rational classification of climate.Geographic Review 33:55–94.
Verry, E. S. 1975. Streamflow chemistry and nutrient yields from upland peatlands in Minnesota.Ecology 56:1149–1157.
Wilcox, D. A., R. J. Shedlock, and W. H. Hendrickson. 1986. Hydrology, water chemistry, and ecological relations in the raised mound of Cowles Bog.Journal of Ecology, 74:1103–1117.
Winter, T. C. 1988, A conceptual framework for assessing cumulative impacts on the hydrology of nontidal wetlands.Environmental Management 12(5):605–620.
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Siegel, D.I. Evaluating cumulative effects of disturbance on the hydrologic function of bogs, fens, and mires. Environmental Management 12, 621–626 (1988). https://doi.org/10.1007/BF01867540
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DOI: https://doi.org/10.1007/BF01867540