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| 02219nam 2200397zi 4500 |
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001 | 9.871682 |
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003 | CaOODSP |
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005 | 20221107163444 |
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006 | m o d f |
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007 | cr ||||||||||| |
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008 | 190416s1999 oncd #ot f000 0 eng d |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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043 | |an-cn-on |
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086 | 1 |aEn13-5/99-203E-PDF |
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100 | 1 |aZanini, L. |q(Lavinia)|eauthor. |
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245 | 10|aInvestigation of radial diffusion in dolostone core samples from the Lockport formation, Smithville, Ontario : |bphase II / |cby: Lavinia Zanini, Kent Novakowski and Greg Bickerton. |
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246 | 14|aInvestigation of radial diffusion in dolostone core samples from the Lockport formation, Smythville, Ontario :|bphase II |
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264 | 1|aBurlington, Ontario : |bNational Water Research Institute, Environment Canada, |c1999. |
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300 | |a1 online resource (iv, 37 pages) : |bfigures. |
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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 ; |v99-203 |
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500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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500 | |a"January, 1999." |
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504 | |aIncludes bibliographical references. |
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520 | |a"Dolostone samples from the geological units which comprise the Lockport Formation, were collected from core samples obtained from boreholes drilled near Smithville, Ontario. These samples were used in forward and reverse diffusion tracer experiment to estimate the effective porosity of the dolostone units and determine the effective diffusion coefficients, and thus a geometric factor, for specific chemical tracers. The experiments were conducted using radial diffusion cells of various dimensions"--Abstract. |
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692 | 07|2gccst|aGroundwater |
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692 | 07|2gccst|aWater pollution |
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700 | 1 |aNovakowski, Kent S., |eauthor. |
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700 | 1 |aBickerton, Gregory S., |eauthor. |
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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 ;|v99-203.|w(CaOODSP)9.844121 |
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856 | 40|qPDF|s1.77 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-99-203-eng.pdf |
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