CONSOLIDATION TEST
ASTM D2435, BS EN ISO 17892

1. Scope*
1.1 These test methods cover procedures for determining
the magnitude and rate of consolidation of soil when it is
restrained laterally and drained axially while subjected to
incrementally applied controlled-stress loading. Two alternative
procedures are provided as follows:
1.1.1 Test Method A—This test method is performed with
constant load increment duration of 24 h, or multiples thereof.
Time-deformation readings are required on a minimum of two
load increments. This test method provides only the compression
curve of the specimen and the results combine both
primary consolidation and secondary compression deformations.
1.1.2 Test Method B—Time-deformation readings are required
on all load increments. Successive load increments are
applied after 100 % primary consolidation is reached, or at
constant time increments as described in Test Method A. This
test method provides the compression curve with explicit data
to account for secondary compression, the coefficient of
consolidation for saturated materials, and the rate of secondary
compression.
NOTE 1—The determination of the rate and magnitude of consolidation
of soil when it is subjected to controlled-strain loading is covered by Test
Method D4186.
1.2 These test methods are most commonly performed on
saturated intact samples of fine grained soils naturally sedimented
in water, however, the basic test procedure is
applicable, as well, to specimens of compacted soils and intact
samples of soils formed by other processes such as weathering
or chemical alteration. Evaluation techniques specified in these 
test methods assume the pore space is fully saturated and are
generally applicable to soils naturally sedimented in water.
Tests performed on other unsaturated materials such as compacted
and residual (weathered or chemically altered) soils
may require special evaluation techniques. In particular, the
rate of consolidation (interpretation of the time curves) is only
applicable to fully saturated specimens. 

1.3 It shall be the responsibility of the agency requesting
this test to specify the magnitude and sequence of each load
increment, including the location of a rebound cycle, if
required, and, for Test Method A, the load increments for
which time-deformation readings are desired. The required
maximum stress level depends on the purpose of the test and
must be agreed on with the requesting agency. In the absence
of specific instructions, Section 11 provides the default load
increment and load duration schedule for a standard test.

1.4 These test methods do not address the use of a back
pressure to saturate the specimen. Equipment is available to
perform consolidation tests using back pressure saturation. The
addition of back pressure saturation does not constitute nonconformance
to these test methods.

4. Summary of Test Methods
4.1 In these test methods a soil specimen is restrained
laterally and loaded axially with total stress increments. Each
stress increment is maintained until excess pore water pressures
are essentially dissipated. Pore pressure is assumed to be
dissipated based on interpretation of the time deformation
under constant total stress. This interpretation is founded on the
assumption that the soil is 100% saturated. Measurements are
made of change in the specimen height and these data are used
to determine the relationship between the effective axial stress
and void ratio or strain. When time deformation readings are
taken throughout an increment, the rate of consolidation is
evaluated with the coefficient of consolidation.
5. Significance and Use
5.1 The data from the consolidation test are used to estimate
the magnitude and rate of both differential and total settlement
of a structure or earthfill. Estimates of this type are of key
importance in the design of engineered structures and the
evaluation of their performance.
5.2 The test results can be greatly affected by sample
disturbance. Careful selection and preparation of test specimens
is required to reduce the potential of disturbance effects.