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USLHC | USA

Broadcast your data

Ken Bloom
Saturday, January 28th, 2012

Are you addicted to YouTube? No, I wouldn’t say that about myself, but gosh, it’s rather amazing what you can find on there. At home with the kids lately, we’ve been looking at classic bits of The Electric Company, the 1970′s Children’s Television Workshop educational show which spans the period of late Tom Lehrer to early Morgan Freeman. Part of what makes YouTube great is that it’s so easy to use. You put a phrase into the search window, and some computer somewhere (don’t ask me where) quickly finds the data that you are looking for. Then you just click a button and the videos come streaming onto your computer, without a whole lot of effort from you. You don’t have to know what computer disk the file resides on, or the directory structure of that computer. For all you know, the video might be coming from several different computers at once, with the source being adjusted in real time to give the best streaming performance.

Now, compare that to how we go about getting our data in particle physics experiments. Back in the day, you definitely had to know the exact directory and exact file names of the dataset that you wanted to analyze, and then carefully type that into your computer programs. A single typo could destroy hours or days of computing effort. We’ve largely gotten past that — we have better technology for file catalogues, such that you can just specify the name of a dataset, and all the file names will be looked up for you. But we are still largely constrained by “data locality,” the requirement that your analysis program must be running on a computer in the same room as the computer that has the disk with your data on it. This constraint leads to a variety of optimization problems. What if a dataset gets popular all of a sudden — are there enough processing resources in the right place to handle the demand? Can you get more copies out to the bigger processing centers quickly? Are you then under-using other centers and letting CPU cycles go idle? If you want to run on a given dataset, you might know which computing sites have that data, but how do you know which has the most available resources right now? And finally, what if data at a site gets corrupted? Will all the jobs running in that computer room start failing? Needless to say this doesn’t sound like YouTube at all.

I and some colleagues are working on a project that tries to change this. We’ve called it “Any Data, Anytime, Anywhere,” as our goal is to make it as easy to access LHC data as it is to access a YouTube video. At the heart of the system is a “redirector,” a system that serves as a giant index of files that reside at computing sites all over the country. A computer program asks the redirector for a file, the redirector finds an optimal source for the file, and the program then reads the file from that source, without the user having to know where the file actually is. That means that the source could be thousands of miles away, and the only way for the remote reading to be efficient is for it to be nearly as fast as reading from a computer in the same room, so some effort has gone into making that happen. Once you have removed the data locality requirement, all sorts of things are possible. If a file is corrupt at one site, it could introduce a fallback mechanism so that a read failure results in an attempt to get the same file through the redirector instead. If a particular site gets overloaded with jobs, we could start to migrate them to a less busy site, even if that site doesn’t actually have the data that the jobs want; they can be obtained through the redirector instead. That could lead to a better global balancing of supply and demand for resources. While we imagine that it’s computers at CMS institutions that will be reading the data, there’s nothing to stop any computer anywhere from reading the data, even if it is not part of CMS. That could really fulfill the promise of grid computing — if we can borrow a computer for a few hours, we can use it to analyze CMS data even if that computer starts out knowing nothing about CMS. It also gives us a straightforward way to use cloud-computing resources, if that were to turn out to be cost effective.

And on top of all that, what stops this from being limited to the LHC? Many disciplines have large datasets that need to be analyzed by distributed teams of scientists. In principle, they could use the same infrastructure. We’re hoping that this technology could eventually be used across the sciences and even into emerging fields like digital humanities. If that were to happen, then researchers from all sorts of disciplines could consider themselves Easy Readers, at least as far as their data is concerned.

Anatomy of an aurora

Aidan Randle-Conde
Thursday, January 26th, 2012

This week the Earth has seen some increased magnetic activity in the upper atmosphere, and that means we got to see aurore! Across Northern Europe and the Northern USA people looked to the skies to see the northern lights. An aurora is one of the most beautiful sights in the natural world, and a phenomenon that actually tells us a lot about the Earth and how it interacts with its environment.

Those who followed me on Twitter (@aidanatcern) may have already seen some of the wonderful images of aurorae. There are dedicated webcams that capture the night sky, and you can see some sample images at the Aurora Webcam archive.

Aurora over Alaska (wikimedia)

Aurora over Alaska (wikimedia)

When charged particles accelerate or decelerate, they emit electromagnetic radiation, and it is this radiation that we see in the aurora. The color of the light depends on the wavelength of the radiation, and the intensity of the light depends on how much radiation is emitted. That means that there is always an aurora above us, but if the energy of the radiation is too low, or the intensity is too weak, we won’t see anything. Once we know how to interpret the light we can learn something about the radiation that is emitted. Usually we see a variety of colors in an aurora and each color corresponds to a different wavelength, so if we can see a region of the sky that is all one color, we know that the wavelength (and hence the energy, ignoring the effects of aberration) must be the same. That means we can “map” the sky and find contours of wavelength.

Since the particles are accelerating, there must be something that causes the acceleration. The Earth’s core is made of (among other materials) molten iron. The rotation of the Earth means that this core is also rotating, and a rotating fluid magnetic medium creates a magnetic dipole, giving the Earth magnetic North and South poles. These poles are aligned near the geographic North and South poles of the Earth, but not exactly. (In fact, magnetic North and South keep moving and from time to time they even swap places. The exact mechanism behind this is not yet fully understood, but geological records show it happens every few hundred thousand years. Simulations suggest that the rotating magnetic fluid is a chaotic system, so the reversals occur at stochastic, or random, intervals of time.)

The sun produces a stream of charged particles, known as the solar wind, and they create their own electromagnetic field. The two fields, from the Earth and the sun, interact and they force the charged particles along curved paths. As they particles move along these paths they accelerate and decelerate, and that is what produces the aurorae. The most recent increase in magnetic activity can be traced back to a huge coronal mass ejection that arrived from the sun. This video shows the arrival of the flare:

The effect looks impressive, but don’t be scared, solar winds like this are perfectly harmless. Far bigger winds have hit the Earth in the past few billions years and life has continued to flourish in spite of them. Life has adapted to the Earth’s magnetic field and this field protects us from the high energy particles.

It turns out that while looking up at the night sky is a beautiful and moving experience in itself, it is also important to particle physicists. Some of the most important discoveries in the last century came from a different phenomena, cosmic rays. Cosmic rays are very high energy particles (usually protons) that travel huge interstellar distances and rain down on the Earth in much the same way that the solar wind does. They interact with the upper atmosphere to create cascades of particles, and usually the muons are the only detectable particles that reach sea level. Interactions of these cosmic rays gave rise to the discovery of the muon (“Who ordered that?!”), the pion and the kaon, the lightest forms of mesonic matter. It was around this time that large scale accelerators were developed, and we found hundreds of new mesons and baryons. Cosmic rays gave us a very small glimpse into a rich “zoo” of particles that has occupied physicists ever since.

Eventually, when we have exhausted our ability to accelerate particles to higher energies we might need to rely on cosmic rays again. There are proposals to develop ground based detectors to study the interactions of extremely high energy particles from outer space. Those particles have the potential to reach energy regimes we can only dream of at the moment. (Incidentally, this is one of the ways that we know for sure that the LHC cannot destroy the world. The universe creates much more energetic particles than we could ever hope to create in our accelerators, and since the universe seems to be in one piece we can conclude that the LHC is safe on Earth!)

An aurora from above (Expedition 28 on board the International Space Station)

An aurora from above (Expedition 28 on board the International Space Station)

If you’re fortunate enough to see an aurora then take a few moments to think about the huge forces at work, the vast distances involved, and how the colors tell us so much about how the Earth and solar wind behave. It really is one of the most beautiful phenomena in the universe.

Getting layed

Aidan Randle-Conde
Friday, January 20th, 2012

On a past blog post I came across the most wonderful comment from Kelly, one of our readers:

Lay people are far smarter than it is supposed, they are also fickle and quick to get bored or offended if talked down to

This got me thinking about the last time I spoke to an expert in another field about their research, about the last time I got “layed”, if you’ll excuse the awful pun. I also hope you’ll excuse an excursion into biochemistry for one post.

Alex and Kia, relaxing in the sun

Alex and Kia, relaxing in the sun

I was in Manchester for the weekend, spending the evening with Alex and Kia, a couple of friends from undergraduate and we had a lot of catching up to do! They’re both biochemistry graduate students and they work in the same lab, although in different areas. We stayed up all night over tea and biscuits (how British), discussing our research, using analogies, looking at diagrams, and coming up with all sorts of thought experiments to try to understand what was happening. They had a lot of questions about how the detector works, how we reconstruct particles (including the Higgs!) and why it takes so long to find it.

Having a discussion about something technical with an expert is not only lots of fun, but it also tells you a lot about your own skills when it comes to explaining concepts. As Kelly mentioned in her comment, there’s a temptation to talk down to people, but I find it’s more rewarding for all involved if we match our discussion to the intelligence of the audience. I’d like to think that most people who read Quantum Diaries and US LHC Blogs are here because they’re intelligent, they’re not scared of nuance, they want to read more than what a press release will tell them, and they may even be a scientist too. Once we find the right level of discussion for a given audience things get much more rewarding!

From the outside biochemistry is such a wonderful field of research. Their work is instantly relevant to the fight against disease and cancer, the field is expanding so rapidly that what students learn one year may be out of date a couple of years later, and there’s no end to the range of different topics you can research. It’s about as fast paced as you can get! It must have its frustrations, like any area of research, but being a layperson I got a chance to appreciate the concepts without the hard work, and that made it sound amazing.

The watered down version of what they told me went something like this:

HIV and T cells

What HIV looks like (Telegraph)

What HIV looks like (Telegraph)

The HIV virus is extremely dangerous for one reason- it infects the white blood cells (T cells) that fight disease in the body. This in itself isn’t a huge problem, but when a person with HIV have some infection then things become very serious. It’s not so much that the white blood cells don’t function anymore, it’s more that they use so many of their resources building more copies of the virus. The virus attaches itself via a protein, and a small percentage of the population have a different form of the protein, which has a different shape. In principle, if a person could get a complete blood transfusion then they could be given the white blood cells with the other protein and may become immune to HIV. An easier way to do this would be to have a bone marrow transplant from another person, as the bone marrow creates the white blood cells. Naturally there are dangers associated with any procedure like this, so it’s not something to be taken lightly. Still, in the course of an hour or so my friends gave me a wonderful insight into how HIV works and some of the discoveries in the fight against the disease.

Genetic diseases

While on the topic of diseases with risky treatments we also discussed a family of genetic diseases (known as mucopolysaccharide diseases, a name I could not remember) which cause premature aging or degradation of the body. The diseases are associated with the failure of the body to break down certain sugars, so the cells get clogged up, do not function as well and then part of the body ages. The exact type of disease manifests in different ways, and sometimes they can only be identified once the disease has progressed. So I asked why children aren’t just screened for this at birth, as they are for many other diseases. It turns out that the cost of the test isn’t low enough and rate of incidence of the disease isn’t high enough for that to become a realistic option yet. Putting groundbreaking, life saving research in that kind of context is rather chilling. I’m glad physicists don’t have to deal with those kinds of choices!

Kia was kind enough to link to one of the charities, so I could find out more about the disease and how it affects us: The MPS Society.

The immune system

But we weren’t done yet! We also talked about the immune system and cancer. Having heard so much about T cells, I was curious about where they came from and why they only attacked foreign objects in the body. It turns out that T cells spend much of their time in the thymus where they are trained to learn what cells in the body look like. When the T cells are produced there is some shuffling of genes and each T cell ends up a little different. If a T cell latches onto part of the thymus it gets destroyed and isn’t allowed into the rest of the body. Otherwise the T cell is let out into the bloodstream. If it finds a cell it “thinks” is attractive, it latches on and releases chemicals into the blood stream. Other T cells respond to the chemical gradient and they too latch on. After a short while the foreign body is overwhelmed and dies.

A red blood cell, a platelet and a T-cell, side by side (Wikipedia)

A red blood cell, a platelet and a T-cell, side by side (Wikipedia)

Well that’s how it works in principle, and there are many ways in which it can go wrong. Some viruses are adept at mutating so that their appearance changes. (On the subject of mutations, my friends also treated me to a discussion of “frame shifts” and how you can get two proteins from one gene!) If one of these viruses gets identified and overwhelmed, one copy may mutate into another form, and the T cells are back to square one again. Another “nightmare scenario” is when a cancerous growth releases a different kind of chemical which essentially says “All fine over here! Carry on!” to the T cells. If that happens then things can go quite seriously wrong quite quickly. If all that wasn’t complicated enough, T cells can also get “confused” and latch on cells from their host body, giving rise to auto immune diseases. The immune system is so amazingly intricate that you could easily spend a whole evening just scratching the surface of the subject. At the same time it also seems immensely fragile and wonderfully robust. Although the apparatus for making an immune system is inherited, the good work it does fighting disease isn’t. If those ideas doesn’t blow your mind then I don’t know what will!

The PhD problem

To round off the evening we also discussed how our PhDs had progressed. Biochemistry seems less forgiving than physics, and they told me that between them and two other mutual friends, two of them had to find new topics, new funding and new institutions. Sometimes, when a research idea doesn’t work out and the funding disappears, even if it’s through no fault of the student, the student has no choice but to start again. I faced a similar situation with my own PhD, as funding for the experiment was cut short and I suddenly found myself with 18 months left, no research topic and no service task. My colleagues rallied round, asked questions, contacted people and helped me find a new topic and a new service task on the same experiment. I finished about 9 months later than expected (but still within four years!) with a decent thesis and some glowing letters of recommendation. Once again, I was glad to be in the cozy realm of physics! It’s differences like these that aren’t at all obvious, and make us realize just how much we have to learn from each other. (My friends were also amazed to find I had about a hundred papers with my name on!)

PhDs are elastic... (PhD Comics)

PhDs are elastic... (PhD Comics)

When did you last get layed?

So for a few hours I was a layperson with two experts at my disposal, and it was one of the most entertaining evenings I’ve had in a long time. So to the lay people reading this blog, if you don’t find the term “layperson” pejorative, it would be great to hear about your experiences. What discussions particularly excited you? How you deal with being patronized or, perhaps worse, overwhelmed with ideas? Or for that matter, if you’re an expert in another area, what are your experiences telling other people about your work? In short, tell us happened last time you got “layed”.

Location, Location, Location

Seth Zenz
Thursday, January 19th, 2012

If I had to pick one thing that’s definitely better on my old experiment, ATLAS, than on my new experiment, CMS — and especially if I had to pick something I could write publicly without getting into trouble — it would be this: the ATLAS detector is across the street from the rest of CERN. I’m not sure how that was decided, but once you know that, you know where CMS has to be: on the other side of the ring, 5 or 6 miles away. That’s because the detectors have the same goals and need the same beam conditions; two opposite points on the LHC are where a duplicate performance is easiest. The pre-existing caverns from the LEP collider, whose tunnel the LHC now uses, probably also helped determine where the detectors are.

In any case, it used to be that when I wanted to work on my detector, I had only to go across the street. Now I have to drive out of Switzerland and several miles into France. Except, I don’t like driving. So I’ve been working on alternate means of transportation. A few months ago I walked. Last night I had to go to downtown Geneva, so I took the bus. It’s actually pretty good, although the bus stop is a mile away from CMS. There’s also the shift shuttle, which runs from the main CERN site to CMS every 8 hours via a rather roundabout route. And I can bike, once the weather gets better and I get myself a little more road-worthy. To be honest, every option for getting here is much slower than driving, but I enjoy figuring out ways to get places enough that I’m going to keep trying for a while.

I have plenty of chances to try, because I’ll be here in the CMS control room a lot of the time over the next few weeks. Right now, I’m learning and helping with the pixel detector calibration effort. (We’re changing the operating temperature, so all the settings have to be checked.) Soon I’ll be learning to take on-call shifts. So the more I stay here, the more I learn. I got here this morning, and I won’t leave tonight until about 11 pm. I could take the shift shuttle back — or maybe I’ll just get a ride.

Visiting LHCb!

Anna Phan
Thursday, January 19th, 2012

Warning for those on slow internet connections: this post contains quite a few large images
which may take a long time to load. Just be patient, I promise they’ll be worth the wait!

I’ve been blogging about LHCb for about eight months now, telling you all about the detector and the physics. If you’ve been following my posts from the start, you might recall that as well as being new to Quantum Diaries, I was also new to LHCb.

Why do I bring that fact up now? Combined with the timetable of the LHC (which operated between March and November last year), this has meant that while I could read about the detector, monitor the data taking and start analysing the recorded data, I had never actually been underground and seen the detector.

So when I found out that Kathryn Grim, of USLHC Communications, was taking a pair of videographers and photographers down, I asked to be part of the visit. Luckily, there was space for me and I had already passed all the necessary training and had all the required access privileges.

I was pretty excited about the visit, in addition to getting to see the detector I work with, the last LHC detector I saw was ATLAS, back in 2009 before any serious data taking had begun. And before that, I visited ATLAS and CMS during construction way back in 2007.

Why is this history important? Well, visiting LHCb is a history lesson of sorts. Unlike ATLAS and CMS, which are located in caverns especially built for the experiments, as seen the schematic map below, LHCb and ALICE reside in caverns which previously contained LEP detectors, DELPHI and L3.

As I’ve mentioned before, ALICE took advantage of that fact by incorporating the L3 magnet in its detector. LHCb took a different approach, simply disconnecting the DELPHI detector and moving it away from the beam line into an exhibition area behind concrete shielding. I didn’t have much time in the DELPHI part of the cavern as the videographers and photographers wanted to get straight to LHCb, but I was able to grab a couple of shots of the detector, one of which I include below…

So you may be wondering about the videographers and photographers Kathryn and I were accompanying underground (along with a couple of other LHCb colleagues). It was kind of confusing actually, there were two separate crews, each of which contained one videographer and one photographer. However, the focus of one team was the videographer and the focus of the other was the photographer.

Here on the left, I have a photo of the videographer, Steve Elkins, who was filming for a documentary. He had a accompanying crew member to assist with the filming and to take photos of the process for promotion. You can find out more about the upcoming documentary at his website.

In his words, “The film will be about questions, and the diverse routes to ask them. It will be about the struggles to lift the seemingly impenetrable veils of mystery from the intangible and transcendent, whether through bodies, machines, brains, or stars… It will involve the largest astronomy project in human history, Tuvan throat singers, a neuroscientist’s quest to actually photograph memories being formed in the brain, and the Kalacakra sand mandala ceremony overseen by the Dalai Lama in India, all told through the true story of a man running alone across Death Valley in average temperatures of 130 degrees fahrenheit.”

It sounds really intriguing and I look forward to seeing it.

Here on the right, I have a photo of the photographer, Enrico Sacchetti. You may be wondering why a photographer requires a videographer. It has to do with the camera he was using, a Phase One 645DF. From what I gathered, the company lent him the camera, on the condition that he film himself using it for promotional purposes.

You can find some of his previous photos of the LHC experiments on his website, which are quite nice. From what I saw on the preview screen on the camera though, the new ones will be spectacular.

That’s enough about the people on the visit; onto photos of the detector! I won’t bombard you with images of the whole detector, since they all look fairly similar, but instead, below, I’ll show you a few different unique views of certain components.

The top photo shows the view between the hadronic calorimeter and the muon system from below the detector, looking up towards the ceiling. You can see the beam pipe on the right of the photo. The left photo shows people working in the tracking system. The experiments use the LHC downtime to maintain their detectors. You can see that two of the tracking stations have been retracted, while one remains in position (the two left stations are the retracted ones). The right photo shows the dipole from the front, with a lot of safety tape and plastic covering the beam pipe. These are placed there during the maintenance period to protect the equipment. They will be removed before the start of data taking so they won’t interfere with the physics.

 

Pretty cool huh? I really enjoyed my visit and the unique opportunity to witness physics and art in action. I’ll leave you all now with the obligatory photo of me and the detector.

New State Discovered by the ATLAS Collaboration!

Brian Dorney
Tuesday, January 10th, 2012

Over the Christmas Holiday the ATLAS Collaboration submitted an article to Physical Review Letters, a peer-review journal.  The article titled, “Observation of a New χb State in Radiative Transitions to Υ(1S) and Υ(2S) at ATLAS,” can be found on arXiv.

The processes under study in this paper are the following:

χb(nP)→ Υ(1S) γ → μ+μ- γ

χb(nP)→ Υ(2S) γ → μ+μ- γ

Where n = 1,2 or 3.

The focus of this paper was on finding a meson known as the χb(nP). Mesons are a class of particles formed by a bound state of a quark and an anti-quark; the χb(nP) happens to be a bound state of a b-quark (termed b, for beauty) and an anti-b-quark (termed b).  The (nP) part means that quark/anti-quark are bound together in a P-orbital of energy level n. As a consequence of the relativistic energy-momentum relation, different energy levels correspond to bound states with different rest masses.  So basically for each value of n you have a unique particle! The n = 3 particle has only ever been theoretically predicted, so in this paper a new particle was discovered!

Now the χb(nP) particles are very short lived and usually can’t be observed directly.  So to find them the ATLAS Collaboration has to infer their presence by summing up the energy of their decay products.  In the above two equations, the χb(nP) is decaying into another meson known as the Upsilon, Υ(kS), and in the process a photon is also emitted (hence the “radiative transition” in the title). Now the Upsilon is also made up by a bb pair.  The (kS) part means that the quark/anti-quark pair are bound together in an S-Orbital of energy level k = 1 or 2.

The Υ(kS) is also a very short lived particle (mean lifetime of approximately 10-20 seconds).  To identify the Upsilons needed for this study the ATLAS Collaboration had to look for two oppositely charged muons, called a di-muon or μ+μ- pair, having a summed rest mass (termed “invariant mass”) near the published mass values for the Υ(kS).  A plot of the di-muon invariant mass can be see at right [1].  From left to right the peaks in the graph represents di-muons originating from decays of the Υ(1S),  Υ(2S), and the Υ(3S), respectively. The muons in the shaded regions from the Υ(1S) and Υ(2S) decays were used in the search for the χb(nP) particles.

Then to find the χb(nP) particles, ATLAS researchers looked for a point in the detector from which a di-muon and a photon originated from.  This point is known as a vertex.

Charged particles, such as muons, leave tracks in the ATLAS Detector’s inner tracking detector (which consists of a silicon pixel detector, a silicon microstrip detector, and a transition radiation tracker).  The inner tracking detector is like a giant CCD camera, and is based on the same technology.

However, neutral particles, like photons, do not leave a track in the tracker.  Photons are detected by energy depositions in the ATLAS Detector’s electro-magnetic calorimeter.  To see if an energy deposition marked as a photon comes from this di-muon vertex, you take every di-muon vertex, and you try and match it with one of your photon energy depositions.  If the match is “good enough” you call this di-muon plus photon a χb(nP) candidate.

Before we show you these χb(nP) candidates I want to talk about the di-muon invariant mass plot one more time.  Notice how the peaks in this plot have some width to them.  This has to do with the resolution of the ATLAS Detector.  The narrower the peaks are the better the resolution.  However, there is a limit to how thin these peaks can be.  For example, the Υ(1S) has its own natural width of  about 54 keV or 0.000054 GeV.  So suppose you had the perfect particle detector and made the measurement shown in the di-muon invariant mass plot.  Even using your perfect detector your Υ(1S) peak would still have a width of exactly 0.000054 GeV.  As you can see the peaks are no where near this, and as I said this is due to the finite resolution of the ATLAS Detector.  To account for this resolution, researchers at ATLAS worked with a variable defined as:

Δm = m(μ+μ-γ) - m(μ+μ-)

This takes the invariant mass (e.g. rest mass) of the di-muon and the photon, the χb(nP) candidates, and subtracts the di-muon mass.  Then the ATLAS researchers add the world average values of the Upsilon masses back to Δm.

m k = Δm + mΥ(kS) = m(μ+μ-γ) - m(μ+μ-) + mΥ(kS)

Note, for your perfect detector measuring the Υ(1S) this quantity: m(μ+μ-) – mΥ(1S) is approximately zero, but has a maximum value of 0.000027 GeV, e.g. this would be half the width of the Υ(1S)!  This is how the use of Δm and the world average value of the Upsilon minimizes the affect of the ATLAS detector’s resolution.

A little side note about world average values in particle physics.  They are a single value for some experimental observation, produced by the Particle Data Group [2], and take into account every experimental result that has ever been published.

A plot of mk is shown at left [1] for the χb(nP) candidates in which the photon was measured directly (as opposed to an indirect measurement from the photon splitting into an e+e- pair).  The first two peaks are the previously observed χb(1P) and χb(2P) particles.  The third peak is the first ever observation of the χb(3P)!

In case you all remember the golden rule of particle physics, the ATLAS Collaboration reports that:

“the significance of the χb(3P) signal is found to be in excess of six standard deviations in each of the unconverted and converted photon selections independently” [1]

Or put plainly, the probability that this third peak could have happened by coincidence is about 2 in one billion.  You literally have a higher probability of winning the lottery at 1 in approximately 16 million [3] or being struck by lightning this year at 1 in 775,000 [4].

 

So how about that? Not everyday a new particle is discovered!

 

 

Until Next Time,

-Brian

 

References

[1] The ATLAS Collaboration, “Observation of a New State in Radiative Transitions to and at ATLAS,” arXiv:1112.5154v1 [hep-ex].

[2] K. Nakamura et al. (Particle Data Group), J. Phys. G 37, 075021 (2010). Note this may be found online here: http://pdg.lbl.gov/2011/tables/contents_tables.html

[3] wikiHow, “How to Calculate Lotto Odds,” http://www.wikihow.com/Calculate-Lotto-Odds, Jan 10th 2012.

[4] NOAA, “Medical Aspects of Lightning,” http://www.lightningsafety.noaa.gov/medical.htm, Jan 10th 2012.

A new year, a new outlook

Aidan Randle-Conde
Saturday, December 31st, 2011

2011 has been a year of change and excitement. We’ve had plenty of good news and bad news to deal with. The new year doesn’t mean just another calendar on the wall, it means a new way of looking at physics. There’s no better way to bring in the new year than watching the fireworks in central London, surrounded by friends. There’s usually a fantastic display, because London is not only one of the most important cities in the world, but it’s also home of universal time. With the Greenwich Meridian running through the capital, we’re reminded of the role that timekeeping has played in the development our history and our science. But this year was even more special, since London is literally inviting the world to its streets this year for the Olympics. So I got caught up in the excitement of it all my thoughts turned to what we’ve seen in the world of physics, and where we’re going next.

New year fireworks in London (New York Times)

New year fireworks in London (New York Times)

2011 got off to a start with ATLAS announcing a startling asymmetry in the jet momenta in heavy ion collisions. However, the joy was tainted by a leaked abstract from an internal document. That document never made it through internal review and should never have been made public. We were faced with several issues of confidentiality, ethics and biases, and how having several thousand people, all armed with the internet and with friends on competing experiments makes the work tough for all of us. In the end we followed the right course, subjected all the analyses to the rigors of internal and external review, and presented some wonderful papers.

There was more gossip over the CDF dijet anomaly presented at Blois. CDF saw a bump, and D0 didn’t. Before jumping to any conclusions it’s important to remember why we have two experiments at Tevatron in the first place! These kinds of double checks are exactly what we need and they represent the high standard of scientific research that we expect and demand. The big news for Tevatron was, of course, the end of running. We’re all sad that the shutdown had to happen and grateful for such a long, productive run, but lets look to the future in the intensity frontier.

Meanwhile both ATLAS and CMS closed in on the Higgs boson, excluding the vast majority of the allowed regions. The combinations and results just got better and better, until eventually on December 13th we saw the result of 5fb-1 from each experiment. The world watched as the presentations were made and quite a few people were left feeling a little deflated. But that’s not the message we should take away. If the Higgs boson is there (and it probably is) then we’ll see by the end of the year. There’s no more of saying “Probably within a year, if we’re lucky”, or “Let’s not get ahead of ourselves”. This time we can be confident that this time next year we’ll have uncovered every reasonable stone. The strategies will change and we narrow the search. We may have new energies to explore, and we’ll tweak our analyses to get more discriminating power from the data. Now is the time to get excited! The game has changed and the end is definitely in sight.

Raise a glass as we say farewell to a great year of physics, and welcome another

Raise a glass as we say farewell to a great year of physics, and welcome another

It’s been a good year for heavy flavor physics as well. LHCb has gone from strength to strength, probing deeper and deeper into the data. We’ve seen the first new particle at the LHC, a state of bottomonium. Precision measurements of heavy flavor physics give some of the most sensitive tests of new physics models, and it’s easy to forget the vital role they play in discover.

ALICE has been busy exploring different questions about our origins, and they’ve studied the quark gluon plasma in great detail. The findings have told us that the plasma acts like a fluid, while showing unexpected suppression of excited bottomonium states. With even more data from 2011 being crunched we can expect even more from ALICE in 2012.

The result that came completely out of left field was the faster than light neutrinos from OPERA. After seeing neutrinos break the cosmic speed limit, OPERA repeated the measurements with finer proton bursts and got the same result. Something interesting is definitely happening with that result. Either it’s a subtle mistake that has eluded all the OPERA physicists and their colleagues across the world, or our worldview is about to be overturned. I don’t think we’ll get the answers in the immediate future, so let’s keep an eye out for results from MINOS and OPERA.

Finally it’s been an incredible year for public involvement. It’s been a pleasure to have such a responsive audience and to see how many people all across the world have been watching CERN and the LHC. A couple of years ago I would not have thought that the LHC and Higgs boson would get so much attention, and it’s been a of huge benefit to everyone. The discoveries we share with the world are not only captivating us all, they’re also inspiring the next generation of physicists. We need a constant supply of fresh ideas and new students to keep the cutting edge research going. If we can reach out to teenagers in schools and inspire some of them to choose careers in science then we’ll continue to answer the most fascinating, far reaching and beautiful questions about our origins.

So when you a raise a glass to the new year, don’t forget that we’ve had an incredible 2011 for physics, and that 2012 is going to deliver even more. We don’t even know what’s out there, but it’s going to be amazing. To physics!

Does the world want it to be like that?

Ken Bloom
Tuesday, December 27th, 2011

Lincoln, Nebraska, where I live, is on the western end of the Central time zone, and as a result, the sun goes down pretty late on the clock here. Even at this time of year, sundown isn’t until 5 PM, and it’s not really dark until at least six. We usually get home with the kids around five, and then we do dinner and playtime inside until bed. That means that the children, who are five and three, are rarely outside when it is really dark out, and they don’t get to see the stars, beyond the bright planets, very often.

The past weekend was an exception; it was Chanukah and there were many evening celebrations, as you are supposed to light the candles at sundown, so we were out past bedtime. On Friday night, as we went out to our car to drive home, my daughter, the older kid, looked up at the cloudless sky and marveled at the number of stars that she could see. I looked up too, and took the opportunity to point out one of the few constellations that I can identify, Orion. (Whenever I think about Orion, I think about John Guare’s “The House of Blue Leaves” — sorry.) “See, it looks like a person, with a top part and a bottom part, and those three stars are a belt,” I explained. My daughter looked at this a little more, and then asked, “Does the world want it to be like that?”

Interesting question — what she meant was whether the stars were intentionally arranged in the shape of a person, or whether it was just something that people made up when they looked at the stars. The answer is the latter, of course, although perhaps the ancients thought differently. Our conversation for the evening went on to other topics in astronomy (“Planets are round,” she said, “so it’s very hard to stand on them.”), but I kept thinking about what she had asked me.

As scientists, we collect data from the world around us, and try to make patterns out of it that we can understand. These patterns are theories, really, and as more data come in, we re-evaluate the theories to see if they are still consistent with the data. Do all the stars make shapes that look like familiar things? Are all of the measurements from the LHC consistent with a Higgs boson at 125 GeV? Are we humans just imposing an anthropic view onto the world? Measurements throughout particle physics, not just at the LHC, seem to support the idea of the Higgs mechanism. Is that consistency just a pattern that we have invented? Or does the world actually want it to be like that?

A year from now, we hope to have an answer to this question. As we head into 2012, a potentially decisive year for particle physics, I hope that all of our Quantum Diaries readers have the opportunity to ask, and answer, their own questions about what the world wants it to be like.

Numerical Family Connections

Seth Zenz
Wednesday, December 21st, 2011

Just a brief random thought at the start of the first winter break in my life where I’m not visiting or living with my parents… Whenever I need the number π — that is, the ratio between a circle’s circumference and its diameter — in computer analysis code I’m writing, I always write it out like this:

3.141592654

That’s not exactly π, but it’s quite close. What I really should do is look up where it’s already defined in the math library I’m using, but this is more than accurate enough for any reasonable purpose. It’s too many digits, in fact, although I know a few more. So why do I always write out exactly that many places? Well, after thinking about it for a minute a little while ago, I remembered the answer: it’s the number of digits of π my dad taught me when I was a kid.

On the edge of the icepack

John Huth
Tuesday, December 20th, 2011

Now that we might (maybe, possibly, could be, it could go away, let’s be careful about what we say here lest we put a jinx on it…) be seeing hints of a Higgs, it’s time of some cautionary tales that a ‘discovery’ is not the end of the story, it’s only the beginning.

When I was a young graduate student, Martinus Veltman gave a talk at a summer school. He had yet to share the Nobel Prize in physics with Gerard t’Hooft for work on the Standard Model. This was 1980. Veltman said, “Right now, theorists are in the driver’s seat. In fact, for the next 30 years, with the exception of the details of the masses of some particles, we know what’s going to happen. But in 30 years, we absolutely are going to need experimental guidance to make any progress in particle physics whatsoever.”

In point of fact, I don’t think anyone recorded Veltman’s words for posterity, but it made a deep impression on me in a number of ways. First and foremost to a rookie experimentalist was the realization that I had to toil in the vineyards for thirty years until something truly of note would arrive. The second thought was “What on earth is he talking about?” We were handed the Higgs boson as an article of faith.

In the current publicity about the Higgs boson, I often worry that we simplify the goals of what we’re doing to the point of trivializing it. Veltman was right: What we call the “Higgs boson” or the “God particle” is really a surrogate for a strange mechanism that bestows mass on all particles through an interaction. We have the most precise theory of anything and, yet, this absolutely crucial piece is missing. We’ve gotten to that point, 30 years later, at which we’ve found almost all of the particles theorists predicted as part of the Standard Model and are now heading into uncharted territory in higher energy ranges.

What we don’t often talk about are the odd properties that this mysterious particle is thought to have. Often times, theorists, like Veltman, feel that the current model is horribly inelegant and must therefore be completely wrong and only a pale approximation of what nature really does to bestow mass, the most elemental of properties a particle can possess.

What makes it so inelegant? In the first place, if it is as described in our simplest model, it would be the only elementary particle we know of that doesn’t possess an intrinsic property of ‘spin’, which seems to be key in the workings of our theory of fundamental forces. For more on the inherently quantum mechanical property of particles known as spin, see this post by Flip Tanedo.

Beyond its spin 0, the Higgs has a very odd property: It gives energy to the vacuum of space. We don’t really know what this means and often just ignore it. Yet, a kind of vacuum energy has been invoked to describe cosmology on very different energy scales from the energies we’re exploring at the LHC. Astrophysicists often talk about something called the “flatness problem”.

If you took a pot of boiling water just off the stove, and dumped ice into it, eventually you would see the ice and the hot water come to some equilibrium temperature. But, in order for this to happen, the ice and hot water have to physically come in contact with each other. When we look around the universe, the temperature of everything is the same to a remarkable degree, as if it was all sitting in the same pot and came to the same temperature. That would all be well and good, but one patch of the universe cannot possibly have been in contact with another part, because they’re separated by such a large distance that light itself cannot connect the two. How could the entire universe be at the same temperature?

The answer is largely thought to lie in a period called ‘inflation’. Initially the very early universe was so dense and compact that temperatures from one part could communicate to another part: everything was sitting in the same ‘pot’. Then, a mysterious vacuum energy appeared that pushed parts of the universe out of contact, but preserved the uniformity of temperature. This happened within a very early phase of the universe when temperatures and energy densities were far hotter than the conditions we’re producing at the LHC. This vacuum energy is about a trillion times larger than what we associate with the Higgs.

Astrophysicists have also invoked a vacuum energy at another, much weaker scale. You may have heard of ‘dark energy’. Our best guess is that, like the vacuum energy of the early universe, this mysterious force that seems to be pushing the universe apart also seems to be a kind of vacuum energy. Yet, in this case the energy of the vacuum is exceedingly weaker than the energies we’re exploring at the LHC. So, there’s a vacuum energy invoked to explain both the very early universe and the very late universe. At the same time, there’s a vacuum energy associated with the Higgs, but it just sits there like an orphan, of no consequence.

To deal with some of these strange properties, theorists have come up with other ideas for how the Higgs might manifest itself:

1.) Supersymmetric Higgs – The energy scale where the three main forces other than gravity, the strong, weak and electromagnetic- join together is close to the scale associated with the cosmic inflation. This is often called the ‘Grand Unification scale.’ The fact that we see two of the fundamental forces – weak and electromagnetic – joining together at the LHC energies presents a conundrum. It is very difficult to reconcile the Grand Unification scale with the LHC scale in a natural way without having some other kinds of matter arise. The constants of the theory would have to line up just perfectly, fine-tuned to a level of precision that is equivalent to balancing a pencil on its point. With Supersymmetry, a number of Higgs-like particles arise.

2.) Composite Higgs – Rather than deal with an inelegant particle with no spin, theorists have speculated that it’s actually made of multiple objects, possible pair of top quarks, tightly bound together. The opposite spins of the objects bound together in a composite Higgs would cancel out to give it zero spin.

3.) No Higgs –According to some models, the Higgs is not a particle at all, but the result of interactions that create mass. These models are sometimes called ‘technicolor’. Although they aren’t particularly favored by theorists because they’re difficult to calculate, we cannot rule them out.

Experimentalists are checking the data for all of these possibilities.

But, what if something like our vanilla-Higgs shows up with a high degree of certainty? Are we done? Hardly! Given all the possibilities and the somewhat inelegant nature of the vanilla-Higgs model, the work has just begun. We have to ask questions like: Is there only one? What is its spin? How does it interact with all the other particles? Are there any variations in its interactions from what we expect, and if so, how does that relate to other measurements we do. These are the tough questions, the one Veltman was alluding to and my betting odds are that we’ll find deviations from our vanilla-Higgs, but it won’t be easy. It may take a decade or more of data taking at the highest beam intensities and energies before we begin to understand what’s really going on.

Science may begin with blinders and theories may run aground, but eventually we do manage to figure out what’s going on.

Here’s a cautionary tale from the 19th century. It illustrates how people can be steered in the direction of one theory, but ultimately can end up with a far more powerful idea.

A German geographer named August Petermann championed a theory of a warm Polar sea. Some expeditions to the high Arctic reported seeing vast stretches of ice-free water extending off toward the horizon. An oceanographer named Silas Bent speculated the that warmth of the Gulf Stream waters flowing north, combined with the waters of a similar ocean current, called the Kurosiwa (black current) flowing off of the coast of Japan would be sufficient to warm the Polar Ocean to the point that an expedition, if it could make it through some part of the ice pack, could sail directly to the Pole. Petermann was one of the main champions of the idea.

James Gordon Bennett Jr. was the publisher of the New York Herald and tried to boost publication by underwriting adventurous expeditions. He financed Henry Morton’s Stanley’s search for David Livingston, garnering a boost in the circulation of the Herald. Hearing of Petermann’s theory of the warm polar sea, Bennett set about to finance an expedition and purchased a British gunboat, the HMS Pandora, and refitted it. He enlisted the US Navy to find a crew. Rechristened the USS Jeanette, it was captained by Lieutenant Commander George DeLong. Hoping to repeat the publicity of the famous Stanley-Livingston meeting, Bennett sent the Jeanette north through the Bering Strait in hopes of reaching the famed open Polar Sea. The Jeanette left San Francisco in July 1879, and was last heard from in late August of that year.

After crossing the Bering Strait, the Jeanette was soon frozen fast in the icepack. Trapped there for nearly two years, it slowly drifted northwest from the coast of Siberia and was ultimately crushed by the icepack. DeLong ordered his crew to abandon ship and began a trek over the frozen icepack, hauling three lifeboats in hopes of eventually reaching settlements along the delta of the Lena River in Siberia. DeLong didn’t make it out alive, perishing in the maze of channels. Some survivors did make it to settlements and eventually made it back home.

Three years later, the wreckage of the Jeanette washed up on the coast of Greenland, some three thousand miles away. This prompted many to wonder how the wreckage could travel so far across the frozen icecap. Theories about ocean current proliferated. One adventurer, Fridtjof Nansen, constructed a polar exploration vessel, the Fram. Fram had a rounded hull that allowed it to be frozen into the icepack without being crushed. Nansen and crew sailed to roughly the point where the Jeanette had been frozen in and commenced a drift across the Polar Sea. At this point, the theory of the Open Polar Sea was completely abandoned in the face of the overwhelming data to the contrary.

Although Nansen never reached the North Pole, during the Fram’s expedition, the remaining crew made detailed observations of wind patterns, drift, the ocean depths and temperatures. On its return to Norway, the Fram had a wealth of data that took years to sift through. Vagn Ekman was a student in physics at the University of Uppsala, Sweden. He was studying fluid dynamics and heard of the data from the Fram. After exploring the mathematics of the interactions of air and water flow on the surface of the rotating earth, he developed the modern theory of surface ocean currents, which bears his name: Ekman transport.

Ekman’s work remains one of the fundamental underpinnings of oceanography.

What I’m trying to point out is this: We are on a voyage of discovery. As Veltman said, experimentalists are really now the ones in the drivers seat. The vanilla-Higgs is an easy target to fire at, as there are quite specific predictions for how it will be manifested, but there are good reasons to be suspicious that the Higgs is precisely as it is described in the simplest version of the Standard Model. Like the long, meandering progression from the theory of the Open Polar Sea to the modern theory of Ocean Currents, I suspect that we’ll have many changes and false leads. As it stands now, with the performance of the LHC, we are just beginning to penetrate the icepack, and we don’t really know what to expect.

A rendering of the long retreat to the Lena River Delta by the DeLong Expedition