Table 1. Results of regression analyses--test soils from Mn/ROAD.
A. Frozen condition.
Std
lb/in.2)*
r2
Material
Equation (Mr in
error
n
Clay subgrade sample 1206 (565)
Mr = 1, 087 f (wu )-5.259
207
0.99
0.319
Frozen
Mr = 1, 049 f (wu-g )-2.344
207
0.99
0.275
Frozen
Mr = 1, 052 f (wu- v )-2.929
207
0.99
0.262
Frozen
Clay subgrade sample 1232 (566)
Mr = 905 f (wu )-4.821
244
0.98
0.378
Frozen
Mr = 846 f (wu- g )-2.16
244
0.98
0.423
Frozen
Mr = 848 f (wu- v )-2.633
244
0.98
0.394
Frozen
Class 3 "stockpile"
Mr = 5, 824 f (wu )-2.026
186
0.97
0.491
Frozen
Mr = 5, 488 f (wu- g )-1.076
210
0.97
0.507
Frozen
Mr = 5, 542 f (wu- v )-1.249
186
0.97
0.467
Frozen
Class 4 (taxiway A subbase)
Mr = 2, 826 f (wu )-5.220
69
0.92
0.835
Frozen
Mr = 1, 813 f (wu- g )-1.733
85
0.93
0.885
Frozen
Mr = 1, 652 f (wu- v )-2.813
69
0.91
0.916
Frozen
Class 5 (dense graded stone)
Mr = 11, 320 f (wu )-2.036
28
0.97
0.404
Frozen
-1.2814
Mr = 8, 695 f (wu-g )
28
0.95
0.511
Frozen
Mr = 9, 245 f (wu- v )-1.489
28
0.97
0.432
Frozen
Class 6 "stockpile"
Mr = 19, 924 f (wu )-1.243
260
0.98
0.372
Frozen
Mr = 19, 427 f (wu-g )-0.795
260
0.98
0.338
Frozen
Mr = 19, 505 f (wu- v )-0.897
260
0.98
0.341
Frozen
(lb/in.2 )
(kPa)
layers resulting from calculations, and 3)
5
5
10
7 x 10
stress conditions for all points specified.
For this study, the points specified were
located 0.01 in. above the bottom of the
asphalt or PCC and 0.01 in. below the top
of the subgrade. In the program, a 4090-kg
(9,000-lb) load was applied to a 15-cm
(5.91-in.) radius, which approximates the
area of a standard set of dual wheels or a
falling weight deflectometer ( FWD) test-
σ3 (lb/in.2 )
1
ing plate.
2
w = 16.1%
4
γ d = 105 lb/ft3
7
CUMDAM
7 x 10 4
104
20 (lb/in.2 )
The program CUMDAM calculates
0
10
cumulative damage to the pavement struc-
0
70
140 (kPa)
Deviator Stress
ture, and was developed at CRREL. In
Figure 8. Stress dependence of resilient modulus in station
general form, the procedure used for
1206 clay subgrade material (from Bigl and Berg 1996a).
CUMDAM's calculations is the linear
6