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HANDBOOK ON THE PHYSICS AND CHEMISTRY OF RARE EARTHS VOLUME 37... [Pg.514]

Handbook on the Physics and Chemistry of Rare Earths, Volume 41 ISSN 0168-1273, DOI 10.1016/S0168-1273(ll)41002-3... [Pg.95]

Figure 1.2 Radial distribution functions of 4f, 5s, 5p, 5d, 6s, and 6p electrons for cerium [2]. (Courtesy of Z.B. Goldschmitd, Atomicproperties (free atom), in K.A. Gschneidner andL. Eyring (eds.). Handbook on the Physics and Chemistry of Rare Earths, volume I, 2nd edition. North Holland Publishing Company, Amsterdam. 1978.)... Figure 1.2 Radial distribution functions of 4f, 5s, 5p, 5d, 6s, and 6p electrons for cerium [2]. (Courtesy of Z.B. Goldschmitd, Atomicproperties (free atom), in K.A. Gschneidner andL. Eyring (eds.). Handbook on the Physics and Chemistry of Rare Earths, volume I, 2nd edition. North Holland Publishing Company, Amsterdam. 1978.)...
Figure 6.8 Crystal structure of La3( X3,r -mmp)2(iJL2,h -ininp)3(nimp)4 [25]. (Reproduced from Z.P. Zheng, Cluster compounds of the f-elements, in K.A. Gschneidner, Jr., J.C.G Btinzh, and V.K. Pecharsky (eds.), Hmdbook on the Physics and Chemistry of Rare Earths, volume 40, 2010, with permission from Elsevier.)... Figure 6.8 Crystal structure of La3( X3,r -mmp)2(iJL2,h -ininp)3(nimp)4 [25]. (Reproduced from Z.P. Zheng, Cluster compounds of the f-elements, in K.A. Gschneidner, Jr., J.C.G Btinzh, and V.K. Pecharsky (eds.), Hmdbook on the Physics and Chemistry of Rare Earths, volume 40, 2010, with permission from Elsevier.)...
Teleseismic travel time tomographic images are determined from the inversion of relative travel time residuals so as to minimize bias resulting from errors in the earthquake location and origin time and the effects of 3D structures outside the Earth volume of interest. A second reason for using relative arrival times is that they can be determined more precisely than absolute arrival times in the presence of noise. The relative travel time is given by... [Pg.58]

Handbook on the Physics and Chemistry of Rare Earths, volume 29... [Pg.420]

The soil porosity is the total volume of pores in the soil mass expressed as a percentage of the total intact earth volume. The pores in the soil have different shapes and sizes and they are filled either with water or with air. The determination of the total porosity P is calculated from the ratio of the specific (S) and reduced bulk weight, using formula... [Pg.689]

You would get 20 1.27 X 10 ° molecules, which is about 10 Earth volumes. The same calculation for a pentapeptide gives more comprehensible results. [Pg.764]

We anticipated the need for other volumes to follow the first four, both to cover topics already mature but not included and others whose time had not yet come. We underestimated both aspects of this need. There is a time for a review of past work when the review itself promotes understanding and stimulates new lines of research. In response to this the publisher will continue the series to assure an evolving authoritative and comprehensive Handbook on the Physics and Chemistry of Rare Earths. Volume 5 contains new topics concerning thin films of alloys and compounds, transport properties of intermetallic compounds, catalytic behavior of metallic and non-metallic surfaces, defects and transformations in oxides, physical and chemical properties of fluorides, and spectroscopic properties of lanthanide ions in a variety of ionic hosts. [Pg.704]


See other pages where Earth volume is mentioned: [Pg.450]    [Pg.458]    [Pg.460]    [Pg.262]    [Pg.58]   
See also in sourсe #XX -- [ Pg.74 ]




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