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008190114s2002    onc    #ot   f|0| 0 eng d
040 |aCaOODSP|beng
043 |an-cn-on
0861 |aEn13-5/01-216E-PDF
1001 |aVan Stempvoort, Dale,|d1957-
24510|aTOC fluctuations in a wetland under restoration, Wainfleet Bog, Ontario, Canada |h[electronic resource] / |cDale R. Van Stempvoort and Allan S. Crowe.
260 |aBurlington, Ont. :|bEnvironment Canada, |c2002.
300 |a[15] p.
4901 |aNWRI contribution ; |vno. 01-216
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
500 |aReprinted from Wetlands and Remediation II: Proceedings of the Second International Conference on Wetlands & Remediation, edited by Karl W. Nehring and Susan E. Brauning.
504 |aIncludes bibliographic references.
520 |a"Wainfleet Bog is the largest remaining bog in southern Ontario, Canada. Through the construction of drainage ditches. much of the former bog has been convened to agricultural lands and peat has been extracted. The drainage ditches have caused extensive changes to the hydrology and ecology of the bog, including the loss of Sphagnum moss and invasion by birch and aspen. Human activities have potentially contaminated the bog. The large pool of organic matter in Wainfleet Bog can bind/sorb hydrophobic contaminants. Measured as TOC, there are high levels (up to 200 mg/L) of aquatic organic matter (dissolved plus suspended) in the drainage water at Wainfleet Bog. This mobile organic matter may play an important role in flushing contaminants from the bog. Large seasonal fluctuations in TOC are related to climatic and hydrological changes"--Abstract.
69207|2gccst|aWater management
69207|2gccst|aWetlands
7001 |aCrowe, Allan, |d1952-
7101 |aCanada. |bEnvironment Canada.
7102 |aNational Water Research Institute (Canada)
830#0|aNWRI contribution ;|vno. 01-216.|w(CaOODSP)9.844121
85640|qPDF|s1.25 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/En13-5-01-216-eng.pdf