Tc. Sheahan et Pj. Watters, USING AN AUTOMATED ROWE CELL FOR CONSTANT RATE OF STRAIN CONSOLIDATION TESTING, ASTM geotechnical testing journal, 19(4), 1996, pp. 354-363
The paper describes the automation and calibration of a hydraulic Rowe
consolidation cell that tests 151-mm-diameter by 60-mm-high specimens
. The associated measurement instrumentation for the cell and specimen
preparation procedures are also described. The cell was used to perfo
rm a set of one-dimensional constant rate of strain (CRS) tests at two
vertical strain rates, 0.1 and 1%/h. The nonlinear CRS theory of Wiss
a et al. (1971) is presented, including methods for interpreting test
results at higher strain rates. The results from the Rowe cell tests c
onducted on resedimented Boston Blue Clay am compared to those from mo
re conventional incremental loading (IL) oedometer tests (63.5-mm-diam
eter by 23-mm-high specimens). For both the 0.1%/h tests (in which neg
ligible excess pore pressure was generated at the undrained specimen b
ase) and the 1%/h tests, the compression curves compare well with the
baseline IL oedometer test curves. Values of preconsolidation pressure
, sigma(p), averaged 94.0 kPa in the Rowe tests and 94.5 kPa in the IL
oedometer tests. The compression ratios, CR = Delta epsilon(v)/Delta
log sigma'(v), in the virgin compression range were slightly lower in
the Rowe cell tests (average 0.156 versus an average CR = 0.173 in the
IL oedometer tests), which may be due to different testing conditions
(e.g., back pressure in the Rowe cell) or the larger Rowe cell specim
en. The coefficient of consolidation and hydraulic conductivity values
computed from the Rowe cell tests are essentially identical with rega
rd to stress level to the IL oedometer tests. The automated Rowe cell
data indicate that the device offers a reliable and potentially rapid
method for determining consolidation parameters, including hydraulic c
onductivity.