Talc | Picrolite | ||||||||||
(m) | (%) | (cm2 g-1) | (m) | (%) | (cm2 g-1) | ||||||
300 K | 200 K | 100 K | 10 K | 300/10 K | 10 K | 300 K | 200 K | 100 K | 10 K | 300/10 K | 10 K |
- | - | 26.5 | 26.5 | - | 1000 (400) | 25.6 | 25.5 | 25.4 | 25.5 | 0.4 | 1700 (600) |
28.9 | 28.9 | 28.8 | 28.8 | 0.3 | 450 (340) | 26.8 | 26.8 | 26.8 | 26.7 | 0.4 | 1300 (800) |
32.0 | 32.0 | 31.9 | 31.9 | 0.3 | 110 (60) | 31.4 | 31.4 | 31.4 | 31.3 | 0.3 | 190 (140) |
- | 34.2 | 34.0 | 34.0 | - | 62 (30) | 32.7 | 32.7 | 32.6 | 32.6 | 0.3 | 2300 |
38.7 | 38.4 | 38.4 | 38.3 | 1.1 | 140 (110) | 42.9 | 42.6 | 42.5 | 42.4 | 1.2 | 530 |
43.2 | 43.2 | 43.0 | 42.9 | 0.7 | 51 (30) | 49.3 | 49.3 | 49.2 | 49.1 | 0.4 | 34 (25) |
56.5 | 56.5 | 56.0 | 56.0 | 0.9 | 130 (60) | 77.0 | 76.5 | 76.0 | 76.0 | 1.3 | 130 |
59.5 | 59.5 | 59.0 | 59.0 | 0.8 | 150 (90) | ||||||
98.51 | 98.0 | 97.0 | 95.5 | 3.1 | 45 (20) | ||||||
Montmorillonite | Chamosite | ||||||||||
(m) | (%) | (cm2 g-1) | (m) | (%) | (cm2 g-1) | ||||||
300 K | 200 K | 100 K | 10 K | 300/10 K | 10 K | 300 K | 200 K | 100 K | 10 K | 300/10 K | 10 K |
26.8 | 27.0 | 27.1 | 27.2 | -1.5 | 470 (100) | 29.4 | 29.4 | 29.2 | 29.1 | 1.0 | 1400 (550) |
29.0 | 29.0 | 29.0 | 29.0 | - | 760 (440) | 35.2 | 35.2 | 35.0 | 34.6 | 1.7 | 940 (430) |
33.0 | 32.9 | 32.9 | 32.8 | 0.6 | 280 (45) | 41.0 | 40.5 | 40.0 | 40.0 | 2.5 | 440 (60) |
49.7 | 49.7 | 49.6 | 49.5 | 0.4 | 190 (55) | - | 42.5 | 42.5 | 42.5 | - | 400 (80) |
60.0 | 60.0 | 60.0 | 60.0 | - | 134 (8) | 49.5 | 49.5 | 49.0 | 49.0 | 1.0 | 310 (80) |
- | - | 66.0 | 66.0 | - | 129 (3) | 72.5 | 72.0 | 72.0 | 71.5 | 1.4 | 220 (90) |
- | 72 | 72 | 72 | - | 134 (15) | 77.0 | 76.5 | 76.5 | 76.5 | 0.6 | 190 (80) |
86 | 84 | 82 | 80 | 7.0 | 129 (15) | 91.5 | 90.5 | 89.0 | 89.0 | 2.8 | 220 (120) |
105 | 104 | 103 | 103 | 1.9 | 110 (25) | - | - | 108 | 108 | - | 65 (10) |
277 | 274 | 273 | 272 | 0.7 | 31 (19) |