000 02247cam  2200385zi 4500
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003CaOODSP
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008190315t19711971oncad   obt  f000 0 eng d
040 |aCaOODSP|beng|erda|cCaOODSP
041 |aeng|bfre
043 |an-cn---
0861 |aM38-1/240-1971E-PDF|zM38-1/240
1001 |aReeve, D. A., |eauthor.
24514|aThe dissolution of fused quartz in ferrous silicate slags / |cD.A. Reeve, Metals Reduction and Energy Centre.
264 1|aOttawa : |bDepartment of Energy, Mines and Resources, Mines Branch, |cJuly 1971.
264 4|c©1971
300 |a1 online resource (ii, 15 pages) : |billustrations, charts.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aResearch report ; |vR 240
500 |aCover title.
500 |aDigitized edition from print [produced by Natural Resources Canada].
500 |a"July 1971."
504 |aIncludes bibliographical references (page 9).
5203 |a"The dissolution of fused quartz in ferrous silicate slags was studied at 1250 and 1350 °C by measuring the decrease in diameter of lengths of fused quartz rod rotated in the slags. The dissolution rate was thought to be controlled by mass transfer of the dissolving species through a liquid boundary layer on the surface of the rotating specimen. Devitrification occurred on the outer surface of the specimen and the amount of devitrification was probably governed by the degree of penetration of the slag into the crystallizing layer. The dissolution rate of fused quartz in ferrous silicate slags, with silica contents varying from close to wüstite saturation to close to silica saturation, decreased with increasing silica content of the slag"--Abstract, page i.
546 |aIncludes abstract in French.
693 4|aQuartz
7101 |aCanada. |bDepartment of Energy, Mines and Resources.
7101 |aCanada. |bMines Branch.
830#0|aResearch report (Canada. Mines Branch)|vR 240.|w(CaOODSP)9.855660
85640|qPDF|s2.14 MB|uhttps://publications.gc.ca/collections/collection_2019/rncan-nrcan/m38-1/M38-1-240-1971-eng.pdf