Time for a New Article on Time

New Calculations on Blackbody Energy Set the Stage for Clocks With Unprecedented Accuracy

Even a completely isolated atom senses the temperature of its environment. Just as heat swells the air in a hot-air balloon, so-called “blackbody radiation” (BBR) enlarges the size of the electron clouds within the atom, though to a much lesser degree — by one part in a hundred trillion, a size that poses a severe challenge to precision measurement.

Um, not quite. This analogy is drawing a Bohr-atom-esque analogy between orbit size and energy and implying that this due to some ideal gas behavior (hey, things expand when they’re hot!). The effect here is called the AC Stark shift, aka the light-shift. When you interact with a system, the interaction shifts the location of the energy levels in the system. This is a big problem in any precision experiment where the effect in question depends on the energy difference between the states, and the second is defined in those terms — 9192631770 Hz is the defined difference between the two hyperfine ground states, in complete theoretical isolation, and this holds true for any transition one might use, including the “you can call me Al+” device in the article. Any interaction with the atoms shifts those energy levels, so you have to know what the interaction is in order to allow you to measure that shift. That includes static magnetic and electric fields (the Zeeman and DC Stark shifts); oscillating fields in the form of EM radiation are also a problem. This is why atomic clocks which use lasers have to turn those lasers off when the atoms are “ticking” — the perturbation is huge. Simply accounting for it is not an option, because it depends on the intensity, so the shift would depend on how well you could servo the intensity of the laser light, and the answer is not “nearly well enough to do a part in 10^18 measurement” by many orders of magnitude.

As the articles mentions, blackbody radiation from, well, everything, is present, too. The walls emit radiation, you emit radiation; room-temperature-ish thing radiate most strongly near about 10 microns but the peak of the distribution depends on the temperature, which is exploited in thermal imaging. There were a few talks on the BBR effects at the Frequency/Timing conference I recently attended in San Francisco, including this one, though this result is quoted from its presentation at a different conference. The Blackbody radiation shift is one of the larger errors in any frequency standard; while one can measure the temperature of the vacuum system pretty well, what radiation profile the atoms actually see is not something that is known quite as well. Nothing is a true blackbody, and even though you’ve shut lasers off, windows in your system can let in thermal radiation from the outside. And then there’s the theory, which probably needs to include several orders of effects involving multiple energy states in order to be useful at this level. This was the nail sticking up in the error budgets of the frequency standards, so it’s not surprising that it is the one getting hammered down in recent theoretical and experimental work.

The problem I have with the imagery is twofold. First, the generic “atom gets bigger” picture runs counter to the deBroglie wavelength argument. That atom really isn’t hotter, since it’s not in thermal equilibrium with the radiation (a single atom can’t have a temperature, anyway), but an atom in a cold ensemble is bigger, because it has a smaller momentum, and hotter atoms get smaller in that regard. Second, the AC Stark shift is a tad more complicated than is described here. In an interaction with a two-state system (1 and 2, with 2 having a higher energy) it will indeed lower |1> and raise |2>, if you are shining radiation that is near that resonance. But |2> is a nominally unoccupied state. Even in the Bohr picture, that state isn’t what you think of when you look at the size of an orbit. The ground state, which is being pushed down to a lower energy, is what we naively use. In real atoms, with multiple states, the picture is much more complicated (and why the theory is as well). The direction of the shift on a state depends on the frequency of the light relative to the transition. If you consider a three-level system, the shift in the |2> state can be in the opposite direction of the shift in |3>, which happens if you tune the laser to a higher frequency than the 1—>2 transition. (There is a class of frequency standards using optical lattices where you choose the light frequency to exactly match the size of the shifts, so that frequency difference of the 1—>2 transition is unaffected.) Saying that BBR makes electron clouds bigger is just wrong.

I have another nit, related to the usual “this is a frequency standard, not a clock” disclaimer:

This quantum-logic clock, based on atomic energy levels in the aluminum ion, Al+, has an uncertainty of 1 second per 3.7 billion years, translating to 1 part in 8.6 x 10-18, due to a number of small effects that shift the actual tick rate of the clock.

This is backwards. The thing you can measure is the short-term stability, i.e. the frequency stability at short times (e.g. at one second, or at some later time when the measurement stops integrating down due to the systematic errors) is the value that can be determined by your experiment, and the time stability is extrapolated, Disco-Stu style (if these trends continue…). The reality that this experiment probably ran for a few hours at best. When it was shut off, the stability of the timing system reverted to whatever the stability of the other clocks was.

See Sack

Not sure why the Chip-Scale Atomic Clock (CSAC) is making news again; this seems to be a rehash of news from January, but it’s an opportunity to make a few comments.

One of the sessions I attended at the recent timing conference discussed some of the pros and cons of the new competitors to the traditional quartz oscillator, one being the CSAC and the other being microelectromechanical systems (MEMS). CSACs have a niche because of the desire to optimize on several variables such as cost, power, stability, and startup requirements. A good quartz oscillator, for example, needs a relatively long warmup time, and the ones with good stability are expensive and tend to drift a bit. So there’s room to beat it on some variables, depending on what the user needs vs. what s/he doesn’t care about, e.g. power and size are variables that matter for a portable system but not for a server rack.

One of the observation is that CSACs could soon find their way into computers tied into ultra-high speed networks, because the clock performance becomes a limiting factor in data transfer — you can send data at a higher frequency and you spend less time re-synchronizing the clocks.

Another observation was a reminder that DARPA is currently funding another program to drive the size and power down even further.

This Movie is One Egg Long

If it’s a three-minute egg

How an hourglass is made

Director Philip Andelman traveled to Basel, Switzerland, to document the designer’s modern take of the classic hourglass inside the Glaskeller factory. Each hand made hourglass comprises highly durable borosilicate glass and millions of stainless steel nanoballs, and is available in a 10 or 60 minute timer.

I like glassblowing/fashioning. I went to the Corning Glassworks several times when I was a kid and never got tired of the tour, especially the part where the guy would make the little glass animals.

via Kottke

Of Course There's an App for That

“Einstein’s Pedometer” App Measures How Special Relativity Affects Your Daily Activity

The iPod app, designed by a Japanese developer, uses the iPhone’s GPS capabilities and Lorentz transformation equations to calculate [time dilation]. The Lorentz transformation is a set of equations that relate one observer’s space and time coordinates to those of another observer.

via @JenLucPiquant

No Problem for Frogs, but a Problem for Time

The One-second War (What Time Will You Die?)

Leap seconds make sure the sun is due south at noon by adjusting noon to happen when the sun is due south at the reference location. This very important job is handled by the IERS (International Earth Rotation Service).

Leap seconds are not a viable long-term solution because the earth’s rotation is not constant: tides and internal friction cause the planet to lose momentum and slow down the rotation, leading to a quadratic difference between earth rotation and atomic time. In the next century we will need a leap second every year, often twice every year; and 2,500 years from now we will need a leap second every month.

On the other hand, if we stop plugging leap seconds into our time scale, noon on the clock will be midnight in the sky some 3,000 years from now, unless we fix that by adjusting our time zones.

Good summary of the problem, but falls short in explaining why we have leap seconds. The common explanation is that the earth is slowing down, but that’s not quite right. You have leap seconds because the earth has slowed down. Even if tidal friction were to magically stop, you would still need to insert leap seconds. The earth, as a clock, is running slow compared to atomic time, so it lags farther and farther behind the longer you wait — which means adding leap seconds to get them to approximately agree. The fact that tidal friction will still be with us means this discrepancy is accelerating — that’s why leap seconds will have to be added at shorter and shorter intervals, should we decide to continue to make the adjustments.

Getting Robbed by the Man

Here in the US we lose an hour to daylight saving time tomorrow. A reminder of its existence, and also a reminder that “the man” is the DoT. Timekeepers use universal coordinated time (UTC), which doesn’t change.

Daylight Saving Time: How to Cope With the Loss of an Hour

For most people, the shift is a nuisance. But for some, it provokes weeks of sleep deprivation that take a heavy toll on mood and productivity, according to Dr. Phil Gehrman, clinical director of the University of Pennsylvania’s Behavioral Sleep Medicine program.

I’m one of them, at least in recent years. I suppose it doesn’t help that I generally get up before sunrise to beat the traffic for my commute, so exposing myself to sunlight (and only sunlight) immediately isn’t an option.

via @BoraZ

A Bar Walks Into a Physicist

… oops, wrong reference frame.

I mentioned Brian Malow, the science comedian, in one of my Science Online 2011 summary posts. Here he is discussing (bad) science in Star Wars. Yes, you probably know the scene, and it has nothing to do with who shot first.

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and some X walks into a bar jokes, some of which you already know

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She Sells CSACS Down by the Seashore

And they are only about $1500. Chip-scale atomic clock approaches performance of modules

Which applications need a CSAC, with GPS-based clocks so available and prevalent? First, there are applications where the GPS-based timing may not be accurate enough. But there are also many applications where GPS is unavailable, such as underwater exploration, underground drilling, geophysical research, and EMI shielded rooms. There are also in-the-field military situations where GPS and all EM waves are deliberately jammed by patrols, to prevent remote triggering of improvised explosive devices (IEDs), yet there is a need for precise communication-equipment synchronization among combat teams.

Knowing, with some precision, what time it is also helps in acquiring a GPS signal, too. The advantage of a soldier not having to stand out in a field for a minute or so while a GPS receiver acquires a signal and gives coordinates is left as an exercise for the student.

I’ve seen some, up close and personal; they’re pretty cool. In fact, we had a prototype and I took a picture of it with my novelty dime (3″ diameter) to make it look really small.

Buckets of Watch

Quartz of them, at least.

Back from vacation, delayed a little by Snowpocalypse 2010 II: The Wrath of James Caan (It’s NOT Snowpocalypse 2010; that was the storm in February). I didn’t know how much snow the DC area would get and it seemed foolish to drive in during the storm or just as the cleanup were to begin. (And the part of abandoning my mom with whatever snowfall was there. That would have been bad). Turns out that DC got almost nothing — it had all melted by Wednesday evening — and Niskayuna got around 6″ (an amount easily handled), though you didn’t have to travel too far to find pockets which had gotten a foot or more, especially up in the hills. Further south and east got dumped upon. My route back, which was inland (Rt 88 to 81 to 15 to the beltway), was all clear.

So here’s a video about how a quartz watch works, which I found via fine structure

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