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| 02061cam 2200397zi 4500 |
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| 001 | 9.867687 |
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| 003 | CaOODSP |
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| 005 | 20221107162358 |
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| 006 | m o d f |
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| 007 | cr nn||||||||| |
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| 008 | 190129s1986 onc 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-on |
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| 045 | |ax7x8 |
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| 086 | 1 |aEn13-5/86-206E-PDF |
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| 100 | 1 |aThompson, Mary E., |eauthor. |
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| 245 | 14|aThe cation denudation rate model applied to data for Harp Lake watershed no. 4, 1977-1982 / |cby Mary E. Thompson. |
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| 264 | 1|aBurlington, Ontario : |bAquatic Physics & Systems Division, National Water Research Institute, Canada Centre for Inland Waters, |c1986. |
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| 300 | |a1 online resource (7 pages, 1 unnumbered page). |
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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 ; |v86-206 |
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| 500 | |aCover title. |
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| 500 | |a"Control no. AP260." |
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| 500 | |a"November 1986." |
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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"Validation of the CDR (cation denudation rate) model in as many different kinds of waters and areas of Canada is desirable because of the uses to which the model has been put - first, in deciding upon a target load of sulfate deposition, and, second, in predicting that stream water quality will improve readily, once sulfate deposition is decreased. This report shows that the CDR model works well, using six years of data for Harp Lake Watershed No. 4, near Huntsville, Ontario"--Management perspective. |
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| 546 | |aIncludes management perspective and abstract in French. |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 2 |aNational Water Research Institute (Canada) |
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| 830 | #0|aNWRI contribution ;|v86-206.|w(CaOODSP)9.844121 |
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| 856 | 40|qPDF|s635 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/En13-5-86-206-eng.pdf |
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