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Mobility Issues in the Developing WorldGakenheimer, Ralph 11 July 2002 (has links)
No description available.
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Career mobility patterns of Oklahoma school superintendents /McGinn, Mary. January 1989 (has links)
Thesis (Ph.D.)--University of Tulsa, 1989.
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Taibei shi Wanhua Diqu ju min zhi ye liu dong zhi yan jiuSu, Qingchao. January 1900 (has links)
Thesis (M.A.)--Guo li Taiwan da xue, 1977. / Reproduced from typescript; on double leaves. Bibliography: p. 150-156.
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Taibei shi Wanhua Diqu ju min zhi ye liu dong zhi yan jiuSu, Qingchao. January 1900 (has links)
Thesis (M.A.)--Guo li Taiwan da xue, 1977. / Reproduced from typescript; on double leaves. Bibliography: p. 150-156.
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Adverse Effects of Mobility Aids on Postural StabilizationBateni, Hamid 05 1900 (has links)
Note:
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Labour mobility : its measurement and causesRobinson, H. W. January 1939 (has links)
No description available.
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Transport properties of lithium and sodium ions in gasesAkridge, Garth Russell 12 1900 (has links)
No description available.
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Transport properties and reaction rates of hydrogen and deuterium ions in hydrogen and deuterium gasesGraham, Edward 05 1900 (has links)
No description available.
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Mobility of elements from cesium formate residue emplaced on pegmatite tailings, Bernic Lake, Manitoba, CanadaSolylo, Patrick 20 September 2012 (has links)
A Cesium Products Facility (CPF) at Bernic Lake, Manitoba, manufactures a Cs-formate drilling mud from pollucite (CsAlSi2O6•H2O) ore. The waste residue is dry-stacked over pegmatite tailings. This thesis studied the mineralogy of the residue and tailings, and the mobility of residue related elements: Ca, Cs, Rb, S and Sr.
Major minerals in the residue include gypsum, quartz, barite, spodumene, feldspar, pollucite, and Cs-sulphate, and in the tailings, quartz, feldspar, spodumene, pollucite and micas. The residue contains an order of magnitude more Cs (<2 wt. %) than the tailings (<0.3 wt. %), with 47 % being mobile from Cs-sulphate and Cs-carbonate. Cs in the residue is immobile in microcline, pollucite, Cs-formate, and Cs in Fe-oxy-hydroxides. Elements from the residue are mobilized by water from several sources: meteoric water and surface runoff from the residue pile, precipitation leaching through the residue pile into the tailings, and direct contact of residue with groundwater.
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Mobility of elements from cesium formate residue emplaced on pegmatite tailings, Bernic Lake, Manitoba, CanadaSolylo, Patrick 20 September 2012 (has links)
A Cesium Products Facility (CPF) at Bernic Lake, Manitoba, manufactures a Cs-formate drilling mud from pollucite (CsAlSi2O6•H2O) ore. The waste residue is dry-stacked over pegmatite tailings. This thesis studied the mineralogy of the residue and tailings, and the mobility of residue related elements: Ca, Cs, Rb, S and Sr.
Major minerals in the residue include gypsum, quartz, barite, spodumene, feldspar, pollucite, and Cs-sulphate, and in the tailings, quartz, feldspar, spodumene, pollucite and micas. The residue contains an order of magnitude more Cs (<2 wt. %) than the tailings (<0.3 wt. %), with 47 % being mobile from Cs-sulphate and Cs-carbonate. Cs in the residue is immobile in microcline, pollucite, Cs-formate, and Cs in Fe-oxy-hydroxides. Elements from the residue are mobilized by water from several sources: meteoric water and surface runoff from the residue pile, precipitation leaching through the residue pile into the tailings, and direct contact of residue with groundwater.
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