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040 |aCaOODSP|beng|erda|cCaOODSP
041 |aeng|bfre
043 |an-cn-ns
0861 |aEn13-5/87-108E-PDF
1001 |aThompson, Mary E., |eauthor.
24514|aThe CDR model applied to data for Rogers Brook, a small tributary to the Mersey River, Kejimkujik National Park, Nova Scotia, 1985 / |cby Mary E. Thompson.
264 1|aBurlington, Ontario, Canada : |bNational Water Research Institute, Canada Centre for Inland Waters, River Research Branch, LRTAP Project, |cJuly 1987.
300 |a1 online resource (6 pages, 3 unnumbered pages) : |bgraphs.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aNWRI contribution ; |v87-108
500 |aTitle from cover.
500 |a"RRB-87-33"--Cover.
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
504 |aIncludes bibliographical references.
520 |a"The CDR model is applied to data for Rogers Brook, a small highly organic tributary to the Mersey River above Kejimkujik Lake, Kejimkujik National Park, Nova Scotia. The organic anion A- calculated by the method of Oliver et al. 1983, is always higher than SRA-, the difference between MTB and IC sulfate. Testing whether the higher A- is due to partial complexing with Fe and Al, using mean monthly data, leads to the conclusion that the organic matter in Rogers Brook is more reactive per gram C during the plant growth period of summer and fall than it is during the winter and spring"--Abstract.
546 |aIncludes a management perspective and an abstract in English and French.
69207|2gccst|aWater management
69207|2gccst|aModelling
69207|2gccst|aRivers
7101 |aCanada. |bEnvironment Canada.
7102 |aNational Water Research Institute (Canada). |bRivers Research Branch.
7102 |aCanada Centre for Inland Waters.
7101 |aCanada. |bLRTAP Program Office.
830#0|aNWRI contribution ;|v87-108.|w(CaOODSP)9.844121
85640|qPDF|s645 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-87-108-eng.pdf