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Gray, Daniel

Paulille s Gray Dynamite. Consisted of 20—25% NG mixed with Na nitrate, resin and charcoal Ref Daniel (1902), 362... [Pg.537]

DANIEL G. NOCERA, ANDREW W. MAVERICK, JAY R. WINKLER, CHI-MING CHE, and HARRY B. GRAY... [Pg.23]

Daniel Gray perfected a stable bath from which indium can be plated simultaneously with other elements (90). Alloyed with precious metals, indium has been made into jewelry, alloyed with silver, it is sometimes used to plate silverware with a suiface resistant to tarnish in the form of an amalgam, it can be used for dental fillings (88, 89, 93) The portraits of Reich and Richter and much of the information about indium have been obtained through the kind assistance of Professor L. W. McCay of Princeton University and Professor O. Brunck, Rectoi of the Freiberg Academy. [Pg.648]

Figure 64 Comparison of the carbon isotopic composition of diamonds containing inclusions ascribed to transition zone and sublithospheric depths (TZ-UM clear) to diamonds with inclusions derived from lower mantle depths (LM gray). The number of specimens is given for each group (n = 132). Note that the —4 to —6 bar for lower mantle diamonds is off-scale at a number of 68. Transition zone and upper mantle diamonds are from these kimberlites Jagersfontein (6), Juina (1), KanKan (5), Orapa (1), Premier (1), and Sao Luiz (10). Lower mantle diamonds (and the number analyzed from each) are from these kimberlites Dokolwayo (1), DO-27 (5), Juina (30), KanKan (36), Koffiefontein (3), Letseng-la-Terai (1), and Sao Luiz (33) (sources Daniels and Gurney, 1999 Davies et al, 1999 Deines etal, 1989,1991a, 1993 Hutchison eta/., 1999 Kaminsky etal, 2001 McDade and Harris, 1999 ... Figure 64 Comparison of the carbon isotopic composition of diamonds containing inclusions ascribed to transition zone and sublithospheric depths (TZ-UM clear) to diamonds with inclusions derived from lower mantle depths (LM gray). The number of specimens is given for each group (n = 132). Note that the —4 to —6 bar for lower mantle diamonds is off-scale at a number of 68. Transition zone and upper mantle diamonds are from these kimberlites Jagersfontein (6), Juina (1), KanKan (5), Orapa (1), Premier (1), and Sao Luiz (10). Lower mantle diamonds (and the number analyzed from each) are from these kimberlites Dokolwayo (1), DO-27 (5), Juina (30), KanKan (36), Koffiefontein (3), Letseng-la-Terai (1), and Sao Luiz (33) (sources Daniels and Gurney, 1999 Davies et al, 1999 Deines etal, 1989,1991a, 1993 Hutchison eta/., 1999 Kaminsky etal, 2001 McDade and Harris, 1999 ...
One of the most important applications of thermoluminescence (Sect. 3.3) is in the field of radiation dosimetry [12,13]. Here a material is exposed for a specific time to a radiation field. The absorbed doses ranging from iO -mGy to ICPOy (iGy (I gray) = 100 id (rad) I rad is equivalent to an absorbed energy of 0.01 J/kg) are measured by monitoring the thermoluminescence after the exposure lime. Many materials display an intensity of thermoluminescence which is proportional to the amount of radiation absorbed. This led Daniels and colleagues in the early 1950 to use thermoluminescence as a means of radiation dosimetry. [Pg.176]

Nitrate reductase P increases in cytosol, B and R soluble and particulate forms Cheniae and Evans (1959) Lowe and Evans (1964) Daniel and Appleby (1972) Kennedy et al. (1975) Daniel and Gray (1976) Pagan et al. (1977) Broughton et al. (1978)... [Pg.85]

AWWA Publications Manager Gay Porter De Nileon Senior Technical Editor Melissa Valentine Technical Editor/Project Manager Martha Ripley Gray Production Editor Cheryl Armstrong Cover Art Daniel Feldman... [Pg.162]

Tatsuya Okuzumi, Dorothea Fiedler, Chao Zhang, Daniel C Gray, Brian Aizenstein, Randy Hoffman Kevan M Shokat see also p 448... [Pg.5]

The AtoZ of Marxism by David Walker and Daniel Gray, 2009. [Pg.266]


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See also in sourсe #XX -- [ Pg.648 ]




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