Baro-acoustic decrepitation only detects fluid inclusions
It does not detect sample events cause by crystallographic changes
Although the technique is often referred to merely as "acoustic
decrepitation", the prefix "baro-" is used to emphasize the fact that
the instruments actually detect a pressure change emanating from the
sample when it decrepitates. Although sound can be transmitted as
either a pressure wave (P) or a shear wave (S), the instrument
configuration detects only the P wave and not S waves. Consequently it
is technically incorrect to think that the instrument detects sound in
general when it really only detects pressure impulses. This distinction
is important as it means that the counts observed are only generated by
the decrepitation of fluid inclusions in the sample and do not
originate from any crystallographic changes in the sample as it is
heated, despite incorrect claims to the contrary in some published
papers.
The key to this important distinction is understanding the construction
of the sample tube assembly of the instrument. The sample tube, which
is a 15 cm. long quartz tube, is shown in this picture. The sample is
placed at the tip (right) of the tube, which will be heated when placed
into the furnace, while there is a pressure sensor (microphone) placed
at the far end (left) of the tube.
The acoustic connection between the sample and the pressure sensor is
through 15 cm of air within the tube. This allows the detection of P
waves, but S waves cannot travel through fluids, in this case air, and
so cannot be detected.
Pressure waves are generated when a fluid inclusion bursts open because
its internal pressure at the present temperature exceeds the strength
of the mineral grain that it is within. This typically requires an
internal pressure of approximately 500 bars. For an aqueous inclusion,
such pressures can only be attained after the fluid homogenizes to a
liquid phase at elevated temperature. Upon bursting, the sudden
depressurisation of this superheated water leads to a steam explosion
which generates a pressure pulse which is transmitted through the air
to the pressure sensor and counted. Gas rich inclusions typically have
high internal pressures at room temperature and pressure increases
further in accordance with the gas law (see detailed explanation)
when heated. When these inclusions burst, the release of high pressure
gas and superheated water both contribute to the generation of a
pressure pulse.
However, when crystallographic changes, such as twinning rearrangements
or the alpha to beta phase transition in quartz, occur they cause only
small volume changes which then cause only minute pressure
changes in the air in the sample tube. These pressure changes are so
small that they are well below the instrument threshold and are not
counted. Crystallographic changes do generate significant S waves, but
these cannot travel through the air and are not detected by the
pressure sensor at all. To detect these S waves you need to use a
completely different type of microphone and to have a transmission path
through a solid all the way from the sample to the detector. The
deliberate use of an air path in the instrument completely eliminates
interference from crystallographic changes as the sample is heated.
The immunity from crystallographic transition interference is clearly
shown when quartz samples are heated through the alpha to beta phase
transition at 573 C. At this transition quartz changes its structure
and the beta phase has a slightly larger unit cell volume. This phase
transition is rapid and cannot be "frozen in" as a metastable phase
when the quartz is cooled back below the transition temperature. When
"sterilized" quartz is heated through the transition temperature, no
decrepitation counts are detected, confirming that crystal phase
transitions do not generate detectable decrepitation counts in the
instrument. Note that all known decrepitation instruments since about
1975 use an airpath and pressure sensor detection and are immune to
crystallographic change interference. Only a few early Russian
decrepitometers used a solid transmission path which allowed the
detection of S waves and almost no data from these instruments is
available. It seems their use was quickly discontinued, perhaps because
of this interference problem.
I use the term "sterilized" quartz to refer to quartz which has already
been heated well beyond the transition temperature and cooled back to
room temperature. This procedure eliminates any fluid inclusions from
the quartz which might generate counts as they decrepitate. This is
necessary because any fluid inclusions present at the transition
temperature can burst because the quartz strength decreases dramatically
during the phase transition, encouraging the decrepitation of even low
pressure inclusions. (Detailed explanation here).