I like to horrify current and recent students by telling them that I spent a month of my PhD figuring out what sort of film to use for best capturing the colors produced by the cathodoluminescence centres in carbonado diamond. Of course, by the time it came to submit my thesis, I then had to spend days scanning all those slides. Although, I still have a poster somewhere that is made from big glossy 8x10 prints, all glued to cardboard backing.
Now if you'll excuse me, I need to chase some kids off my psilphytopsid lawn...
I'm a geochemist. My main interest is in-situ mass spectrometry, but I have a soft spot in my heart for thermodynamics, poetry, drillers, trees, bicycles, and cosmochemistry.
Saturday, October 26, 2013
Wednesday, October 23, 2013
Argon-Argon Dating: The Simple Version
Sciency Thoughts has a post up on recent high-precision 39Ar/40Ar
dating of the Toba supervolcano in Indonesia . Unfortunately he seems a bit confused about
the technique.
Argon has three naturally occurring isotopes: 36Ar,
38Ar, and 40Ar. Potassium also has three isotopes, 39K,
40K, and 41K. One of these isotopes, 40K, is radioactive, with a half life of about 1248 million years, and one of its
stable decay products is 40Ar.
In the universe, and
in Jupiter and the Sun locally, 36Ar is the most abundant argon
isotope, followed by 38Ar. In
the cosmic scheme of things, 40Ar is so rare that we don’t even know
what its overall abundance is.
However, Earth is a rocky planet. It was not able to hold onto much gas during
its formation, so there is very little 36Ar and 38Ar
here. Earth has lots of potassium
though, so almost all the Ar in the atmosphere is 40Ar, which is the
decay product of 40K.
In a potassium-bearing mineral, the 40K decays
into 40Ar, so you can measure the ratio of these two isotopes to
figure out how old the mineral is.
The problem is that it is technically very difficult to
measure a potassium argon ration accurately, because one is a reactive solid,
and the other is an inert gas. They
require different sorts of ion sources, different mass spectrometers, and there
are all sorts of chemical effects that complicate the measurement.
If you want an accurate ratio, it is much easier to measure
isotopes of the same element.
So for 39Ar-40Ar dating, what happens
is that the mineral of interest is put into a nuclear reactor and bombarded by
neutrons. Some of the 39K
(the most abundant stable potassium isotope) absorbs a neutron, ejects a
proton, and transmutes into radioactive 39Ar. 39Ar has a half-life of a few
hundred years, and is virtually non-existent in nature. So as
long as you know your nuclear 39K to 39Ar conversion
ration well, this method allows you to use the 39Ar as a proxy for 39K. The handy thing is that because it is argon,
not potassium, it behaves chemically just like the other naturally occurring
argon isotopes, so you can measure it in a gas source mass spectrometer much
more accurately than you can measure the chemically different 39K
and 40Ar.
The initial 39K-40K ratio doesn’t very
much in nature, and is taken as constant (I think- I’ve never actually done
Ar-Ar). But the take-home point is that 39Ar-40Ar dating
is not its own decay system. It is the 40K-40Ar
decay system, but using a nuclear reactor to change some of the potassium into
an unstable argon isotope to make the nuts and bolts of measuring it easier.
A few brief words on sexual harassment in academia
It appears to be sexual harassment revelations week here in
the science blogosphere, so I figured I’d share a brief story.
In the year 2000, when I was a PhD student, I talked to the
student counseling unit about making a formal complaint about sexual harassment
by a senior member of staff.
They made it clear to me that taking this course
of action would result in revocation of my student visa and deportation from Australia .
I chickened out and kept my mouth shut.
I was fortunate enough to be in a position where I was able
to put my head down, write up, and finish my degree by making this choice. Since that time, I have learned of other
international students at other universities who did the right thing, and were
deported for reporting.
I tell myself that had I gone through with reporting, I
would have been disappeared long before having the opportunity to make an
official statement (way back before blogs, shipping someone halfway around the world was an effective way of shutting them up). And I thought that the incidents which I wished to report
were not severe or well documented enough to bring to the police. But while this is true, here I am, 13 years
later, still awake at one in the morning second-guessing myself.
The recent round of revelations has focused heavily on the
perpetrators of sexual harassment. Which is good. But reporting wrongdoing is much more difficult than it should be, due to the institutional
coercion that universities use to protect their reputations at the expense of
their students.
Sunday, October 20, 2013
Not much going on here
I realize that for the last few years, this blog has been sputtering along with a low level of volume and quality. I can offer neither explanation nor remediation at this stage. But I have listed a few of my old favorites below, for anyone looking for straightforward explanations of how geology explains, among other things, sex, drugs, and Rock and Roll.
Phase Equilibria of Pie Crust
Thermodynamics of Hot Chicks
Cetacean Liposuction
Relativistic Obesity
Geologic Lifespan of Jon Bon Jovi
Stars get Lonely Too
Testing the Earthquake-Modesty Connection
Dear Hypothesis
Phase Equilibria of Pie Crust
Thermodynamics of Hot Chicks
Cetacean Liposuction
Relativistic Obesity
Geologic Lifespan of Jon Bon Jovi
Stars get Lonely Too
Testing the Earthquake-Modesty Connection
Dear Hypothesis
Harry Connolly new series Kickstarter
In "The best book you've never read", I mentioned that Author Harry Connolly, fantastic Urban fantasy "Circle of Enemies", which was an amazing novel that hardly anyone has managed to get a hold of. It turns out that the Author is launching his next series on Kickstarter. The appeal finishes tomorrow, but anyone interested in getting in on this can still do so, if you read this blog post in the next 12 hours.
Friday, October 11, 2013
Jailbait zircons
As the company SHRIMP driver, I do a fair bit of
demonstration analyses for potential customers.
One thing that has become increasingly common over the past two years is
demonstration of the ability to successfully date jailbait zircons. For those of you unfamiliar with the term, a jailbait
zircon is a zircon so young that dating it while making all the usual
assumptions will get you into all sorts of trouble.
The chief problem is that for deep geologic time, we assume
that the 238U to 206Pb decay is a simple process. In
actuality, there are eight alpha decays and more beta decays than I can
remember in this process, but most of the intermediate daughter products are
short-lived relative to the age of the analyst, much less the Earth.
However, if you are dating a phase that is much, much
younger than the Earth, then these intermediate decay products can become
important. Corrections need to be made
relating to whether or not now-extinct intermediate species were incorporated
into the target mineral more or less efficiently than uranium.
For minerals which are a few hundred thousand years old, or
younger, you can abandon the uranium-lead system entirely, and use
uranium-thorium dating instead. This
simply looks at how close to secular equilibrium 230Th and 234U
have grown after their initial incorporation into the target mineral in a
unequilibrated ratio. The linked
wikipedia explanation is good (at least qualitatively). Check it out.
Of course, even for targets old enough for uranium-lead
dating, in addition to the theoretical problems above, there is the practical
problem of measuring a statistically significant amount of very low levels of
radiogenic lead, while somehow keeping common Pb contamination to an absurdly
low level. Because one of the nasty
things about the disequilibrium species is that they disrupt many of the
assumptions that are needed to accurately and precisely correct for common
lead. Which means that if you can’t keep
the blank down, you’re screwed.
Thursday, October 10, 2013
Who actually shuts down in a shutdown
So the government has been shut down for over a week now. What does this mean? NASA is shut down. If you want to learn about the International Space Station, you'll need to learn Russian. The USGS is mostly shut down, except for hazards programs that are on skeleton staffs. On the other hand, the spy agencies are operating as normal. Taxes are still being collected. And you can still register as a congressional lobbyist. So all the unpleasant aspects of government are still business as usual. I guess that's what essential means. The main people suffering are those off work, and small business owners and employees and their suppliers. See the Riprarian Rap to see how non-federal employees get screwed because contracts and grants get delayed or cancelled.
Sunday, October 06, 2013
How the shutdown plays in SE Asia
I have been flying home from Korea via SE asia the last couple of days, and reading a few local newspapers. What is happening here is that while the US Government remains shut down, the premier and PM of China have been engaging on a major goodwill tour, offering things like a billion dollars towards a new monorail project in Indonesia, or 40 billion dollars in increased trade with Malaysia over the next four years. In contrast, the US has cancelled the Presidents trip, sending John Kerry in his place.
The local take on this, from the Persian Gulf to Japan and everywhere in between, is that it makes America look weak and unreliable, and that it is a serious blow to the new "Asian Pivot" strategy. China's rivals are worried that this inability of America to project soft power will tip the regional balance too far in China's favor. Whether the bickering factions in Washington are too myopic to see or too shortsighted to care is not entirely clear.
The local take on this, from the Persian Gulf to Japan and everywhere in between, is that it makes America look weak and unreliable, and that it is a serious blow to the new "Asian Pivot" strategy. China's rivals are worried that this inability of America to project soft power will tip the regional balance too far in China's favor. Whether the bickering factions in Washington are too myopic to see or too shortsighted to care is not entirely clear.
Saturday, October 05, 2013
The wood between the worlds
I’m typing this blog post on the airport wifi, while sitting
in a lounge chair with full AC power. Behind
me, the waterfalls of the koi pond water gently tinkles, while to my left, the
butterfly garden gently sleeps in the pre-dawn darkness. I’m in Singapore airport, the long-haul
air travel version of Narnia’s wood between the worlds.
Friday, October 04, 2013
Never complain about your stove again
Geologist have it pretty easy, in terms of lab safety. Compared to chemists and biologists, we have
to deal with a relatively low number of lethal chemicals, and our habits
confirm this. It is not coincidence the
people call us rock-lickers. But there
are still some reagents which are genuinely dangerous, and command respect.
For most rock knockers, the chief among these is
hydrofluoric acid, or HF. HF is a
volatile (evaporates easily) acid which is notorious for being a contact
poison. You don’t have to drink it for
you to kill you, as it will diffuse through skin, and attack muscle tissue and
bone inside your body. If the muscle it
attacks is your heart, then you die. As
a result, geologists are taught from a young age to observe strict safety
protocols with HF: gloves, face shields, aprons, appropriate supervision and
fume cupboards are all part of the drill.
But not all fluorine health effects are as dramatic. excess fluorine consumption can often cause
dental fluorinosis, a condition in which excess fluorine is deposited in the
teeth, discoloring them. In more severe
cases, fluorine deposition in the bones can lead to osteofluorosis, which can
cause disfigurement, deformity, and chronic pain.
One area in which osteofluorosis is distressingly common is Guizhou , China . Over the past decade, this disease here was
linked to the combustion of high Fluorine coal.
Studies showed tha the clay that was intermixed wit hthe coal was high
in F, and a steady stream of recommendations has come along describing how this
must be getting aerosolized in smoke ,and adhering to food, particularly corn
and chilies hung up in houses to dry.
But something didn’t add up.
People were educated to wash their vegetables, to not breathe coal
smoke, and still the disease persisted.
Finally, recent studies showed that the F was not adhering to the food
products. TOF SIMS showed that it appeared inside uncut chilies, and
sometimes was associated with silica- particulate matter which should not be
able to penetrate food and is biologically inactive.
This was the key to a renewed investigation into the
coal. Which, as it turns out, was not
just rich in fluorine, but also rich in pyrite- fools gold. And all of a sudden, everything fell into
place.
When burned, pyrite reacts exothermically with oxygen and
water to form iron oxide and sulfuric acid:
2FeS2 + 8.5O2 + 4H2O ->
Fe2O3 + 4H2SO4.
Sulfuric acid is not great to breathe, but it doesn’t cause
fluorine poisoning. It will, however,
react with fluorite (the most common fluorine mineral like this:
H2SO4 + CaF2 -> CaSO4
+ 2 HF
And there is the chemical that terrifies geochemists even in
controlled lab spaces, HF, being generated in the household stove. It, in turn reacts with coal ash to form the toxic gas SiF4, which permeates plant and animal tissues and deposits silicon inside of vegetables. In short, domestic cooking stoves are generating incredibly toxic F-bearing gases inside the home. Not even your brother-in-law’s cooking is as
hazardous as this. This was the coolest
talk from the session I was fortunate enough to chair this afternoon; there is
a paper here.