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| 02181cam 2200421zi 4500 |
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| 001 | 9.870443 |
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| 003 | CaOODSP |
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| 005 | 20221107163122 |
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| 006 | m o d f |
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| 007 | cr ||||||||||| |
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| 008 | 190322e198706##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 |aEn13-5/87-144E-PDF |
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| 100 | 1 |aThompson, Mary E., |eauthor. |
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| 245 | 10|aComparison of cation denudation rates, excess sulfate yields, and wet deposition of excess sulfate for the Mersey River below Mill Falls, Kejimkujik National Park, Nova Scotia, 1980-1985 / |cby Mary E. Thompson. |
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| 264 | 1|aBurlington, Ontario, Canada : |bNational Water Research Institute, Rivers Research Branch, Canada Centre for Inland Waters, |cJune 1987. |
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| 300 | |a1 online resource (9 pages, 8 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 ; |v87-144 |
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| 500 | |a"RRB-87-21." |
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| 500 | |aTitle from 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 | 3 |a"Cation denudation rates and excess sulfate yields of the Mersey River below Mill Falls for the years 1980-1985 have been calculated and compared with wet deposition of excess sulfate at Kejimkujik National Park, and show little relation to each other, although the excess sulfate yields and wet deposition of excess sulfate are of the same order of magnitude"--Abstract. |
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| 546 | |aIncludes a management perspective and abstract in English and French. |
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| 692 | 07|2gccst|aRivers |
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| 692 | 07|2gccst|aWater quality |
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| 692 | 07|2gccst|aSedimentology |
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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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| 830 | #0|aNWRI contribution ;|v87-144.|w(CaOODSP)9.844121 |
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| 856 | 40|qPDF|s1.01 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-87-144-eng.pdf |
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