By Sydney Marks
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Additional info for A textbook of inorganic chemistry vol.VI part III Vanadium, Niobium, and Tantalum
The second technique has an additional difficulty for these samples. The saturation of the E' signal inflintresults in a sharply curved growth curve, as shown in Figure 1. Thus the interpolation of the natural signal onto the regenerated curve has more uncertainty than is reported when this technique is used in TL. The reported values of D in Table I are derived from extrapolation of the reduced growth curves. 98. ch004 e Table I. 1 — — c Age a Ufl, Thfl, and Kfl refer to isotope concentrations within the sample.
ESR spectrum of Floridaflint,taken at 77K, showing Al signal. Note that the intensity (I) of the signal is measured from the peak of the high-g line to the trough of the low-g line. ; ACS Symposium Series; American Chemical Society: Washington, DC, 1996. 46 ARCHAEOLOGICAL CHEMISTRY rely on the presence of this signal, but in fact it is found in most flints. This signal must be measured at 77 Κ in order to localize the unpaired electron. It appears to be annealed more readily than the E' signal.
2 As Sn ppm ppm Sb ppm £780 £670 £790 1500 £780 £600 £540 £730 £670 £540 £500 £650 £680 £170 £160 470 £170 £180 £160 £170 £180 £190 200 220 £90 £150 £170 £160 £180 £170 £190 £170 £180 £180 £190 £110 £100 £100 £140 Table IV. ; ACS Symposium Series; American Chemical Society: Washington, DC, 1996. ch003 3. HANCOCK ET AL. 29 Turquoise Blue Glass Trade Beads Table V. ; ACS Symposium Series; American Chemical Society: Washington, DC, 1996. ch003 Table VI. 7 mm m:50;Al:51 =1750-1950 =1700-1800+ * Based on shape, size and colour.
A textbook of inorganic chemistry vol.VI part III Vanadium, Niobium, and Tantalum by Sydney Marks