The migration of D and H was measured by using a steady-state method. It was found that both isotopes moved towards the cooler end. The heat of transport was appreciably smaller for H than for D. The addition of Cr or Ti increased the heat of transport, whereas Fe or Mo did not greatly affect it (table 184).
H.Nakajima, M.Yoshioka, M.Koiwa: Transactions of the Japan Institute of Metals, 1987, 28[12], 949-56
Table 184
Heat of Thermomigration of 1at%D or H
in V, V-Cr, V-Fe, V-Mo and V-Ti
Material | Temperature (C) | Isotope | E (kJ/mol) |
V | 360-420 | H | 4.8 |
V | 360-430 | D | 12.9 |
V-4.0at%Cr | 350-420 | H | 8.6 |
V-4.0at%Cr | 350-420 | D | 17.4 |
V-4.0at%Fe | 350-420 | H | 6.9 |
V-4.0at%Fe | 350-420 | D | 12.2 |
V-4.27at%Mo | 350-420 | H | 8.0 |
V-4.27at%Mo | 360-430 | D | 10.9 |
V-4.02at%Ti | 370-430 | H | 18.3 |
V-4.02at%Ti | 350-430 | D | 24.3 |