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Canada reprints

Canniff, W. 1869 The Settlement of Upper Canada (reprinted 1971). Belleville, Mika Silk Screening, Ltd. [Pg.20]

Traill, C.P. 1836 The Backwoods of Canada (reprinted 1966). Toronto, McClelland and Stewart. [Pg.22]

Figure 3.8 Comparison of theory and experiments (water-air horizontal flow at 25°C and 1 atm pressure with diameter of 2.5 cm). Solid lines theory. (From Dukler, 1978. Copyright 1978 by National Council of Canada. Reprinted with permission.) Fuzzy lines experimental data. (From Mand-hane et al., 1974. Copyright 1974 by Elsevier Science Ltd., Kidlington, UK. Reprinted with permission.)... Figure 3.8 Comparison of theory and experiments (water-air horizontal flow at 25°C and 1 atm pressure with diameter of 2.5 cm). Solid lines theory. (From Dukler, 1978. Copyright 1978 by National Council of Canada. Reprinted with permission.) Fuzzy lines experimental data. (From Mand-hane et al., 1974. Copyright 1974 by Elsevier Science Ltd., Kidlington, UK. Reprinted with permission.)...
Geoscience Canada Reprint Series, pp. 259-296. Facies Models, 2nd ed.,... [Pg.429]

Summary of the various evaporitic textures indicative of particuiar physicai environments. Source-. From Kendaii, A. C. (1984). Facies Modeis, 2nd ed., Geoscience Canada Reprint Series, Walter, R. G., ed. pp. 259-296. [Pg.430]

Figure 11.28 Re-Os isochron for black shales and sulfide deposits of Yukon Territory (Canada). Reprinted from M. F. Horan et ah, Geochimica et Cosmochimica Acta, 58, 257-265, copyright 1994, with kind permission from Elsevier Science Ltd., The Boulevard, Langford Lane, Kidlington 0X5 1GB, UK. Figure 11.28 Re-Os isochron for black shales and sulfide deposits of Yukon Territory (Canada). Reprinted from M. F. Horan et ah, Geochimica et Cosmochimica Acta, 58, 257-265, copyright 1994, with kind permission from Elsevier Science Ltd., The Boulevard, Langford Lane, Kidlington 0X5 1GB, UK.
Fig. 5.11 Emergency and military tourniquet (Delfi Medical Innovations, Inc., Vancouver, Canada, reprinted with permission)... Fig. 5.11 Emergency and military tourniquet (Delfi Medical Innovations, Inc., Vancouver, Canada, reprinted with permission)...
Bull. 101 Copyright 1977 by Fisheries Enviro. Canada. Reprinted by permission of the Minister of Supply and Services Canada, 1996. [Pg.302]

Dominion Bureau of Statistics, Sources of Official Statistical Information Relative to Canada reprinted from Canada Year Book... [Pg.460]

Warner, B. G. (ed.), 1990. Methods in Quaternary Ecology. Geoscience Canada Reprint Series 5, St. John s, NF., 170pp. [Pg.5]

James, N. P. P. W. Choquette, 1990. Limestones — The Sea Floor Diagenetic Environment. Geoscience Canada Reprint Series 4. Geological Association of Canada, SL Johns, Newfoundland 13-34. [Pg.214]

Frey, R. W. Pemberton, S. G. (1984) Trace fossil facies models. In Walker, R.G. (Ed). Facies models. Geoscience Canada Reprints, Serie, /, 189-207. [Pg.189]

Underlined minerals occur in economic quantities in the zones indicated. Table published in the Geology of Industrial Minerals in Canada. Reprinted with permission of the Canadian Institute of Mining, Metallurgy and Petroleum. [Pg.72]

Hesse, R.. Origin of Chert Diagenesis of Biogenic Siliceous Sediments. In Diagenesis . Mcllreath, I.A. Morrow, D.W., Eds. Geological Association of Canada, Geoscience Canada Reprint Series 4,1990 pp 227-251. [Pg.244]

A. P. James, "Chemistry of Peroxygen Bleaching," paper presented at 83rdAmerican Oil Chemists Society Toronto, Canada, May 1992, Interox America Reprints, Houston, Tex., 1992. [Pg.540]

Figure 3.49 Comparison of experimental and calculated data. (From Deev et al., 1978. Copyright 1978 by National Research Council of Canada, Ottawa, Ont. Reprinted with permission.)... Figure 3.49 Comparison of experimental and calculated data. (From Deev et al., 1978. Copyright 1978 by National Research Council of Canada, Ottawa, Ont. Reprinted with permission.)...
Mcllraith, S. J. (1990), Diagenesis, Canada Geoscience Reprint Series, Toronto. McKeever, S. W. (1988), Thermoluminescence of Solids, Cambridge Univ. Press, Cambridge, UK. [Pg.597]

Fig. 14 Plot of logk, — logaH,o against X for the hydrolysis of acetylimidazole in aqueous sulfuric acid at 25°C. Data from refs 251 and 252. Reprinted with permission from ref. 254, 1997 NRC Canada. Fig. 14 Plot of logk, — logaH,o against X for the hydrolysis of acetylimidazole in aqueous sulfuric acid at 25°C. Data from refs 251 and 252. Reprinted with permission from ref. 254, 1997 NRC Canada.
Fig.34 Interlayer species in shigaite, [Mn6Al3(0H)i8][(S04)2 Na(0H2)6 (H20)6], projected down (001) Na(OH2)6 octahedra are cross-shaded, SO4 tetrahedra are random-dot shaded, oxygen atoms of water are shown as black circles, hydrogen atoms of water molecules as small open circles and dotted lines indicate hydrogen bonds. Reprinted with permission from [259]. Copyright Mineralogical Association of Canada... Fig.34 Interlayer species in shigaite, [Mn6Al3(0H)i8][(S04)2 Na(0H2)6 (H20)6], projected down (001) Na(OH2)6 octahedra are cross-shaded, SO4 tetrahedra are random-dot shaded, oxygen atoms of water are shown as black circles, hydrogen atoms of water molecules as small open circles and dotted lines indicate hydrogen bonds. Reprinted with permission from [259]. Copyright Mineralogical Association of Canada...
S. A. Ramsden P. Savic, "A Radiation Model for the Development of Laser-Induced Spark in Air , Nature 203, 1217-19(1964) (Reprint of National Research Council of Canada, Ottawa, Ontario) (In the course of recent work on the spark produced in air... [Pg.437]

Fig. 11.6. Reprinted with permission of the Department of Fisheries and Oceans and the Minister of Supply and Services, Canada, 1991, from Chisholm S, et al. (1986). The individual cell in phytoplankton ecology. Can. Bull. Fish. Aquat. Sci. 214 343-369. Fig. 11.6. Reprinted with permission of the Department of Fisheries and Oceans and the Minister of Supply and Services, Canada, 1991, from Chisholm S, et al. (1986). The individual cell in phytoplankton ecology. Can. Bull. Fish. Aquat. Sci. 214 343-369.
Figure 3.20 Schematic of the interfacial polymerization process. The microporous film is first impregnated with an aqueous amine solution. The film is then treated with a multivalent crosslinking agent dissolved in a water-immiscible organic fluid, such as hexane or Freon-113. An extremely thin polymer film forms at the interface of the two solutions [47]. Reprinted from L.T. Rozelle, J.E. Cadotte, K.E. Cobian, and C.V. Knopp, Jr, Nonpolysaccharide Membranes for Reverse Osmosis NS-100 Membranes, in Reverse Osmosis and Synthetic Membranes, S. Sourirajan (ed.), National Research Council Canada, Ottawa, Canada (1977) by permission from NRC Research Press... Figure 3.20 Schematic of the interfacial polymerization process. The microporous film is first impregnated with an aqueous amine solution. The film is then treated with a multivalent crosslinking agent dissolved in a water-immiscible organic fluid, such as hexane or Freon-113. An extremely thin polymer film forms at the interface of the two solutions [47]. Reprinted from L.T. Rozelle, J.E. Cadotte, K.E. Cobian, and C.V. Knopp, Jr, Nonpolysaccharide Membranes for Reverse Osmosis NS-100 Membranes, in Reverse Osmosis and Synthetic Membranes, S. Sourirajan (ed.), National Research Council Canada, Ottawa, Canada (1977) by permission from NRC Research Press...
Figure 6.10. Accumulation of C in non-steady-state soils of a mature black spruce/moss forest in central Manitoba, Canada. Data shown are (A) for sphagnum moss that has accumulated since the site last burned (-100 yr before sampling), and (B) for the humus and charred layer below the regrowing moss and including the A horizon. The soil is developed on the sediments of a lake that dried up -7000 years ago. The parameters 7 = plant input (kgCuf2yr ) and k = decomposition constant (yr-1). Reprinted from Trumbore and Harden (1997), with permission from the American Geophysical Union. Figure 6.10. Accumulation of C in non-steady-state soils of a mature black spruce/moss forest in central Manitoba, Canada. Data shown are (A) for sphagnum moss that has accumulated since the site last burned (-100 yr before sampling), and (B) for the humus and charred layer below the regrowing moss and including the A horizon. The soil is developed on the sediments of a lake that dried up -7000 years ago. The parameters 7 = plant input (kgCuf2yr ) and k = decomposition constant (yr-1). Reprinted from Trumbore and Harden (1997), with permission from the American Geophysical Union.
Figure 15.9. 13C CPMAS NMR spectrum of humin extracted from a brown chernozem soil from Western Canada. The characteristic doublet in the unsubstituted aliphatic region is characteristic of methylene carbon (28-34 ppm) and shows the presence of both amorphous (soft) domains at 29 ppm and crystalline (rigid) domains at 33 ppm in soil humin. Reprinted from Simpson, M. I, and Johnson, R C. E. (2006). Identification of mobile aliphatic sorptive domains in soil humin by solid-state 13C nuclear magnetic resonance. Environ. Toxi. Chem. 25, 52-57, with permission from the Society of Environmental Toxicology and Chemistry. Figure 15.9. 13C CPMAS NMR spectrum of humin extracted from a brown chernozem soil from Western Canada. The characteristic doublet in the unsubstituted aliphatic region is characteristic of methylene carbon (28-34 ppm) and shows the presence of both amorphous (soft) domains at 29 ppm and crystalline (rigid) domains at 33 ppm in soil humin. Reprinted from Simpson, M. I, and Johnson, R C. E. (2006). Identification of mobile aliphatic sorptive domains in soil humin by solid-state 13C nuclear magnetic resonance. Environ. Toxi. Chem. 25, 52-57, with permission from the Society of Environmental Toxicology and Chemistry.
Present address Paprican, 570 St. Jean Blvd., Pointe Claire, Quebec, H9R 3JR, Canada. Author to whom all correspondence and reprint requests should be addressed. [Pg.1115]

Fig. 11.22 Steady state fiber orientation with respect to shear planes for GF-filled PP. [Reprinted by permission from A. T. Mutel, Ph.D. Thesis, Department of Chemical Engineering, McGill University, Montreal, Canada (1989).]... Fig. 11.22 Steady state fiber orientation with respect to shear planes for GF-filled PP. [Reprinted by permission from A. T. Mutel, Ph.D. Thesis, Department of Chemical Engineering, McGill University, Montreal, Canada (1989).]...
Fig. 13.13 Shrinkage distributions of injection molded amorphous PS (a) at two injection rates longitudinal direction, (b) solid curves, longitudinal direction broken curve, transverse direction. [Reprinted with permission from G. Menges and G. Wiibken, Influence of Processing Conditions on Molecular Orientation in Injection Molds, Soc. Plastics Eng., 31st Annual Technical Conference, Montreal, Canada, 1973.]... Fig. 13.13 Shrinkage distributions of injection molded amorphous PS (a) at two injection rates longitudinal direction, (b) solid curves, longitudinal direction broken curve, transverse direction. [Reprinted with permission from G. Menges and G. Wiibken, Influence of Processing Conditions on Molecular Orientation in Injection Molds, Soc. Plastics Eng., 31st Annual Technical Conference, Montreal, Canada, 1973.]...
We thank the Natural Sciences and Engineering Research Council of Canada and the FCAR, programme d 6tablissement de nouveaux chercheurs of the Quebec Government for their financial support. J.W.C. would also like to thank UQAM for a post-doctoral fellowship. We also thank Prof. J. Wang for providing a reprint of the Ref. 16 prior to its publication. [Pg.35]

Bradshaw, P. M. D., Clews, D. R., and Walker, J. L. (1972). Exploration geochemistry A series of seven articles. Reprinted from Mining in Canada and Canadian Mining Journal. Barringer Research Ltd., Toronto, Ontario, 49 p. [Pg.11]

Source Reprinted from Health Canada, Health Protection Branch consultative document on draft proposals-sub-jects (1) fortification of flour and pasta with folic acid, (2) harmonization of flour enrichment with the United States of America, (3) optional enrichment of flour. [Pg.355]

Moshe Peer, regarding Bergen-Belsen, in K. Seidman, Surviving the horror , The Gazette (Montreal, Canada), August 5, 1993. Facsimile reprint in JHR, 13(6) (1993), p. 24. [Pg.128]

After Yamaguchi et al. Reprinted with permission from Cart. J. Chem., 69, 759 (1991a). Copyright 1991, National Research Council of Canada. [Pg.596]

Fig. 8 The apodized H, emission spectrum from the southern auroral zone of Jupiter recorded by Maillard et a/. using the Canada-France-Hawaii telescope Fourier-transform spectrometer. The spectral lines match well with the laboratory spectrum at T = 1000 K given in Fig. 3. Reprinted with permission from The Astrophysical Journal (1990). Fig. 8 The apodized H, emission spectrum from the southern auroral zone of Jupiter recorded by Maillard et a/. using the Canada-France-Hawaii telescope Fourier-transform spectrometer. The spectral lines match well with the laboratory spectrum at T = 1000 K given in Fig. 3. Reprinted with permission from The Astrophysical Journal (1990).
Figs 1,2 and 3 are reprinted from Sep. Sci. and Tech, with permission of M. Dekker Inc. Figs. 4, 5, 11, 12, 16 and 17 are reprinted from J. Chem. Phys. with permission of the American Institute of Physics Fig. 6 is reprinted from J. Stat. Phys. with permission of Plenum Publishing Figs. 7 and 8 are reprinted from Mol. Phys. with permission of Taylor and Francis Figs. 9 and 10 are reprinted from Proc. IV th Int. Conf. on Fundamentals of Adsorption with permission of Kodansha Publishers Fig. 13 is reprinted from Can. J. Chem. with permission of the National Research Coimcil of Canada Figs. 14 and 15 are reprinted from Langmuir with permission of the American Chemical Society and Fig. 18 is reprinted from Phys. Rev. E with permission of the American Physical Society. [Pg.619]

Figure 7.5 Schematic process flow diagram for DuPont-Canada (now Nova) solution process for production of polyethylene. (Reprinted with permission of John Wiley Sons, Inc., Kirk-Othmer Encyclopedia of Chemical Technology, John Wiley and Sons, Inc., 6" edition, 2006). Figure 7.5 Schematic process flow diagram for DuPont-Canada (now Nova) solution process for production of polyethylene. (Reprinted with permission of John Wiley Sons, Inc., Kirk-Othmer Encyclopedia of Chemical Technology, John Wiley and Sons, Inc., 6" edition, 2006).
Figure 2.20 Cross-section showing the theoretical distribution of hydraulic head and gravity-induced groundwater flow pattern in a homogeneous and isotropic drainage basin with complex ground surface geometry (modified after T6th, 1970. Reprinted by permission of the National Research Council of Canada). Figure 2.20 Cross-section showing the theoretical distribution of hydraulic head and gravity-induced groundwater flow pattern in a homogeneous and isotropic drainage basin with complex ground surface geometry (modified after T6th, 1970. Reprinted by permission of the National Research Council of Canada).
Figure 2.27 Schematic model of the relation between cross-formational gravity-induced groundwater flow and changes in temperature and heat flow with depth in Alberta, Canada (after M orowicz et al., 1985. Reprinted with permission from Journal of Geodynamics 4, Fig. 10, p. 280 Copyright, 1985, Pergamon Press Ltd.). Figure 2.27 Schematic model of the relation between cross-formational gravity-induced groundwater flow and changes in temperature and heat flow with depth in Alberta, Canada (after M orowicz et al., 1985. Reprinted with permission from Journal of Geodynamics 4, Fig. 10, p. 280 Copyright, 1985, Pergamon Press Ltd.).
Fig. 2. Human thyroid biopsies. 1D >H MR spectra (8.5 T, 37°C) residual water suppressed by selective gated irradiation, sweep width 3957 Hz, using 8192 data points, 128 accumulations, and acquisition time of 1.14 s and relaxation delay of 2 s. (a) Normal thyroid tissue, (b) Known follicular carcinoma, (c) Thyroid follicular neoplasm predicted by MRS to be normal—confirmed by histopathology. (d) Thyroid follicular neoplasm predicted by MRS to be cancer and confirmed by histopathology—the presence of capsular invasion. Reprinted with permission from the National Research Council, Canada. Fig. 2. Human thyroid biopsies. 1D >H MR spectra (8.5 T, 37°C) residual water suppressed by selective gated irradiation, sweep width 3957 Hz, using 8192 data points, 128 accumulations, and acquisition time of 1.14 s and relaxation delay of 2 s. (a) Normal thyroid tissue, (b) Known follicular carcinoma, (c) Thyroid follicular neoplasm predicted by MRS to be normal—confirmed by histopathology. (d) Thyroid follicular neoplasm predicted by MRS to be cancer and confirmed by histopathology—the presence of capsular invasion. Reprinted with permission from the National Research Council, Canada.

See other pages where Canada reprints is mentioned: [Pg.235]    [Pg.185]    [Pg.235]    [Pg.185]    [Pg.233]    [Pg.234]    [Pg.80]    [Pg.105]    [Pg.361]    [Pg.495]   
See also in sourсe #XX -- [ Pg.175 ]




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