000
| 02424cam 2200433zi 4500 |
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001 | 9.868978 |
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003 | CaOODSP |
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005 | 20221107162732 |
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006 | m o d f |
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007 | cr ||||||||||| |
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008 | 190227e198707##oncd ob f000 0 eng d |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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041 | |aeng|bfre |
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043 | |an-cn-ns |
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086 | 1 |aEn13-5/87-108E-PDF |
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100 | 1 |aThompson, Mary E., |eauthor. |
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245 | 14|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. |
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264 | 1|aBurlington, Ontario, Canada : |bNational Water Research Institute, Canada Centre for Inland Waters, River Research Branch, LRTAP Project, |cJuly 1987. |
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300 | |a1 online resource (6 pages, 3 unnumbered pages) : |bgraphs. |
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336 | |atext|btxt|2rdacontent |
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337 | |acomputer|bc|2rdamedia |
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338 | |aonline resource|bcr|2rdacarrier |
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490 | 1 |aNWRI contribution ; |v87-108 |
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500 | |aTitle from cover. |
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500 | |a"RRB-87-33"--Cover. |
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500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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504 | |aIncludes bibliographical references. |
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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. |
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546 | |aIncludes a management perspective and an abstract in English and French. |
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692 | 07|2gccst|aWater management |
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692 | 07|2gccst|aModelling |
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692 | 07|2gccst|aRivers |
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710 | 1 |aCanada. |bEnvironment Canada. |
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710 | 2 |aNational Water Research Institute (Canada). |bRivers Research Branch. |
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710 | 2 |aCanada Centre for Inland Waters. |
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710 | 1 |aCanada. |bLRTAP Program Office. |
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830 | #0|aNWRI contribution ;|v87-108.|w(CaOODSP)9.844121 |
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856 | 40|qPDF|s645 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-87-108-eng.pdf |
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