| 000 | 00000nam 2200000za 4500 |
| 001 | 9.865246 |
| 003 | CaOODSP |
| 005 | 20241203113644 |
| 007 | cr ||||||||||| |
| 008 | 181127s1986 oncd|||fo||| f000 0 eng d |
| 040 | |aCaOODSP|beng |
| 041 | |aeng|bfre |
| 043 | |an-cn--- |
| 086 | 1 |aEn13-5/86-43E-PDF |
| 100 | 1 |aStewart, Kenneth, |d1936- |
| 245 | 10|aTwo hypersaline lakes in the Canadian High Arctic and consideration of their development |h[electronic resource] / |cK.M. Stewart and R.F. Platford. |
| 260 | |aBurlington, Ont. : |bEnvironmental Contaminants Division, National Water Research Institute, Canada Centre for Inland Waters, |c[1986]. |
| 300 | |a30, [6] p. : |bgraphs. |
| 490 | 1 |aNWRI contribution ; |vno. 86-43 |
| 500 | |a"Division Control No. ECD-125B". |
| 500 | |a"This manuscript has been submitted to Journal of Fish. and Aquatic Sci. and the contents are subject to change". |
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
| 504 | |aIncludes bibliographical references. |
| 520 | 0 |a"The Polaris lead-zinc mine at latitude 75N is the world's most northerly mine. This mine discharges its tailings into Garrow Lake on Little Cornwallis Island. High concentrations of heavy metal sulfides accumulate in the stable bottom layer of the lake, although they appear to pose no problems for the life in the upper layer of the lake. Garrow Lake, and Sopha Lake on an adjoining island are interesting examples of two meromicic lakes, which we believe have developed their strong salinity gradients through differential freezing each year"--Management perspective. |
| 546 | |aIncludes abstract in French. |
| 692 | 07|2gccst|aPollutants |
| 692 | 07|2gccst|aMining industry |
| 692 | 07|2gccst|aWater quality |
| 700 | 1 |aPlatford, R. F. |
| 710 | 1 |aCanada. |bEnvironment Canada. |
| 710 | 2 |aNational Water Research Institute (Canada) |
| 830 | #0|aNWRI contribution ;|vno. 86-43|w(CaOODSP)9.844121 |
| 856 | 40|qPDF|s2.46 MB|uhttps://publications.gc.ca/collections/collection_2018/eccc/En13-5-86-43-eng.pdf |