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(Aside: my policy
on scientific explanations.)
Calorimetry
is the science of heat. It is not about how many calories are in a Big Mac, but
about how a given material responds to temperature changes on both the atomic
and macroscopic level. This varies widely from substance to substance, and
reveals important information about the arrangement and interaction of the
atoms.
Microcalorimetry is the calorimetry of small
samples, specifically microgram samples (or thereabouts). These are much more
challenging to study than big chunks of material because (1) the time scale for
changing the temperature is much faster and (2) the probes you attach to the
sample to measure it suck away a greater proportion of the heat involved (see
the comments on the pages below about "addenda".)
Both chemists and physicists perform
microcalorimetry experiments. Since I am a physicist, my emphasis will be on
the way we think about this subject. Don't be surprised if you talk to a
chemist who does calorimetry and it sounds like a different language! (Language
barriers between scientists are actually quite a big problem). What my old
group at UCSD works on is the measurement of heat capacity.
If I apply heat to a mass of rock, its
temperature rises a bit. If I apply the same heat to the same mass of copper,
its temperature will rise more. The heat capacity describes this effect: it is
the proportionality between heat applied and subsequent temperature rise.
Heat capacity=(change in heat)/(change in
temperature)
Copper has a lower heat capacity than rock
because it has a larger change in temperature for the same change in heat. The
heat capacity is different at different temperatures; in general it is flat
above room temperature and drops toward zero at lower temperatures because the
material's ability to absorb and transmit heat changes with temperature.
This is interesting (trust me, it is). The
way the material deals with heat involves the electrons, the ionic cores, and
the interaction between the two. What really distinguishes materials (like copper
and rocks) from each other is where electrons are and how they
interact with the ions and the other electrons. Heat capacity alone cannot
tell you everything, of course, but it's an important piece of the whole
picture.
You might suspect that the way to measure
heat capacity is to make two measurements: the added heat and the temperature
rise. Then you just divide them and get the heat capacity. Certainly this
works, but it is not always possible. Think about how you would make the
measurement. To determine the temperature, you need a thermometer. When you add
the heat, you warm up both the thermometer and the sample. That's one
source of error. Also, to add the heat, you must have something connected to
the sample, like heater leads. As you add the heat, some of it leaks back down
the leads-- more error. Another consideration is the time scale of the heating
(how long will it take the whole sample to heat up?) and the temperature
measurement (how quickly does my thermometer respond?). Such concerns are
easily accomodated when measuring large samples like rocks, but what if you can
only make a few thousandths of a gram of the material of interest? What if you
can only make a thin film, which has a mass of a few millionths of a
gram? Many materials studied today indeed come in such small packages. Suddenly
the heater leads, the substrate that the film is grown upon, and the
thermometer contribute extra heat capacity that is the same size (or even
larger) than what you're trying to measure (jargon: this extra heat capacity is
called "addenda"). And time considerations require the use of fast
electronics to measure the temperature changes.
People have developed a variety of methods
for measuring heat capacity, appropriate for various masses and types of
sample. I can't go into all of them, so I'll just describe the one I used,
which is called the relaxation method (that's what the links below will
lead you to). If you want to dig deeper and learn more on your own, I have
provided a reference list.
Since my samples were only about 10
micrograms (10 millionths of a gram), I probed them with a microcalorimeter. I
have measured thin films of pure C60 and K3C60,
C82, C84, and two "endohedral" fullerenes (materials
where there are atoms inside the fullerene cage).
(Note: I have published two papers about
these results-- please look them up to learn more:
Specific
heat of endohedral and higher fullerene thin films, Journal of Chemical
Physics, volume 11, number 12, p. 5291 (1999)
and
Specific
heat of C60 and K3C60 thin films for T=6-400K, Physical Review B, volume 60,
number 16, p. 11,765 (1999).)
Next pages:
Return to the Main Microcalorimetry Page
Copyright © 1997-present Kim Allen
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Email: kimall (at symbol) mindspring.com