Carbon dioxide is a sneaky molecule. It reacts with water to form carbonic acid,
which is a pretty weak acid in the scheme of things, but an acid
nonetheless. It is only stable in an
acidic solution. In seawater, which is
basic (i.e. not acidic), it breaks down to bicarbonate and carbonate. This means several things. For my purposes, it means if I want to
measure the total amount of inorganic carbon in seawater, then I’ve got my work
cut out for me. Carbon could be hiding
as any of four different molecules counting dissolved carbon dioxide (and
that’s just the inorganic stuff… don’t get me started on how messy things get
when biology gets involved). Luckily, we
chemists are molecular bullies, and we have lots of tools at our disposal to
flush the carbon out of hiding:
Step 1: Kill all the
things! We don’t want to risk biology
doing any more damage than it already has to our pristine seawater chemistry,
so the first thing we do after collecting water is poison it. Weird, I used to feel bad for all of the
bacteria and other plankton in my 300 milliliter samples...
Step 2: Set aside a known amount of seawater. This is what the vast majority of the doodads
in the lab with me are for. There are
plastic and glass tubes, twisting all about, venting air, seawater, and acid in
a confusing tangle. Why is this a
challenge? Well, we have two
problems. First, we can’t lose any
carbon while we’re setting the seawater aside, which means we have to keep the
water isolated from air as much as possible.
Also, we’re on a rocking boat, which means we can’t use a scale to weigh
how much water we have. So, we do it by
rinsing and filling a pipette (think a glass bulb, open on both ends) with known
volume. We keep the pipette at a
specific temperature so we know the density of the seawater, and so the pipette
doesn’t expand or contract too much and change its volume. This means a lot of temperature control. The AC says 70 °F, but that ice-furnace―blasting
directly on my workstation―is fighting a Hawaiian summer and exhaust from all
of the machines in here, so I’m estimating my subjective temperature is
somewhere between “I’ll probably survive” and “at least if I die, my body will
be well-preserved.”
Step 3: Next we put our known amount of seawater into the
“stripper.” This is where we’re really
chemical bullies… we acidify the heck out of the seawater with phosphoric acid. MUAHAHAHA.
All that carbon that was hiding as bicarbonate and carbonate is abruptly
forced into carbonic acid, which is constantly exchanging with dissolved carbon
dioxide. We’re also pumping large
amounts of nitrogen gas through this acidified solution, so the carbon dioxide
gets swept up into the bubbles of nitrogen and carried away (this is called
sparging). Within a couple minutes, all
of the carbon has been removed from our beleaguered seawater.
Step 4: We then pass our dissolved gas on to an ethanolamine
mixture in a fancy piece of tech called a coulometer. The solution sucks up the carbon dioxide,
letting the nitrogen gas go. It changes
color as it does, so our instrument knows there’s carbon dioxide and starts
electrocuting the solution to break it down.
As the carbon breaks down, the solution goes back to the original
color. The coulometer keeps track of how
much electricity it dumped into the solution, and that tells us how much carbon
was in our known amount of seawater.
Step X: I’m just noting here that there are a bunch of cleaning,
checking, and calibration steps I won’t bore you with. They’re boring and tedious, and I kinda love
them. Check out Zen and the Art of
Motorcycle Maintenance if that last sentence made no sense.
So, this poor carbon was poisoned, acidified, sparged,
reacted with ethanolamine, and electrocuted.
As I said, chemists are bullies… but in the end, we have the information
we want… the amount of inorganic carbon, in all of its various forms, in a
known volume of seawater. Bingo!
By
Brendan Carter