I’m sure everyone of you got livid with the return value of the
atan2 functions. Here is a fix.
This is Java code, but easy to adapt for other languages. And since you are here, a little hint: Multiply the result with
180 / Math.PI to receive the angle in degrees.
I just installed Icinga, it was the right decision!
First of all respect to the Icinga guys, the compatibility to Nagios is great! Moving from Nagios to Icinga is mainly copy and paste. Syntax is the same, management structure also equals, you can even use all your previous installed Nagios plugins and the nagios-checker add on. Well done! Except for the web interface (looks much more professional) every feels like Nagios. So I can’t see any reason to stay with Nagios.
Here are some things I had to do:
- First of all I changed the credentials for the web interface:
- This new user needs also authorizations, so you need to edit
- The rights in
www-datawasn’t able to access the directory. So I wasn’t able to schedule manual checks via web. When I changed the permissions everything was fine:
- I added the following into the
/etc/icinga/apache2.conf, to force me to use SSL encryption:
- I shortened the mail subject of the notifications. By default the subject looks like:
But I’m just interested in the important parts, so I changed the following in
the the notifications now come with a subject like this:
All in all I’m glad that I gave Icinga this chance and recommend to test it if you are still using Nagios. Maybe I’ll test some further Icinga features and maybe we’ll migrate at the university..
The developers around you might know that there are some mechanism hooked when creating an object. Lets have a look at the order of these processes.
Even beginners should know about constructors. They are called if you create an object of a class, but there are some things running before. Here is an example class:
The output is:
As you can see, first of all the static initializer is called. It’s also called exactly once, when the class is loaded. It’s clear that the class has to get loaded before the
main () inside can be executed.
main () then prints a string to indicate the start of that routine and afterwards it creates the first object of the type
Initializing . This calls the instance initializer before the constructor is executed. Also the creation of the second object calls first the instance initializer and then the constructor.
That’s the workaround. At the first time a certain class is used the static initializer is executed, and each time an object of that class is created first the instance initializer is called and then the constructor.
Btw. all of these routines are able to access members that are private, but notice that the static initializer can only access static fields.
Today I had to install a new server for some biologists, they want to do some NGS. It took a whole day and all in all we’ll send it back…
These biologists ordered the server without asking us, I think the salesmen noticed that they don’t have expertise. The money is provided by the university, so no need to design for efficiency. And that is how it came that they send the hardware (2 Xeon-DP 5500, 72 GB mem) in a desktop case with a Blu-ray writer, a DVD-writer, a GPU with 2.72 TeraFLOPS (afaik they don’t want to OpenCL) and: NO CHASSIS FANS!! Ouch..
It’s as clear as daylight that this cannot work. Did they thought the hot air around the mem (18 slots, each 4GB) leaves the chassis by diffusion?? The processor cooling construction for my Athlon X2 is twice as big as all their fans together…
After setting up a Linux and installing
lm-sensors the CPU’s are running at >75°C, fighting for air. Of course we immediately turned off the hardware! After half an hour we were able to start it again and took a look at the BIOS sensors for the memory. No time to get bored while the temperatures raised up to 80°C and more in less than 5 min, see figure 2… Of course time to turn it off again! Don’t want to hazard a nuclear meltdown..
They also enclosed a raid controller. I’ve googled that. Less than 100$.. wtf… The controller came with a CD to create a driver disk. But when you boot into the small Linux on the CD it hangs with the message “Searching for CD…”. And there is no driver for us, you are only able to use this controller when you are running Win 2003/XP/Vista or a RHEL or a Suse Enterprise. Other systems are not supported.. Proprietary crap..
What should I say, I’m pissed off. A whole business day is gone for nothing… Just because of some less-than-commodity handycrafts… I strongly recommend to ask Micha before plugging such bullshit!
After getting started to work with the new Synapt G2 HDMS from Waters a few questions about the working principle of this machine came up. Here I’ll try to explain where the drift time detector is located and how the software can distinguish between fragments produced in the trap and transfer cell, respectively.
As far as I know Waters is the first manufacturer who joined the IMS- and QTOF-technologies to combine all well known benefits from the QTOF instruments plus the advantages of separating ions by their shape and size.
But lets start at the beginning. As any other MS instrument the Synapt carries an ion source. Here are also some attractive innovations located, but nothing remarkable for now, so I won’t explain anything of it. The interesting magic part starts when the ions pass the quadrupole. To give you a visual feedback of my explanations I created an image of the hierarchical ion path:
Assume only one big black ion has entered the machine and found its way to the quadrupole. This ion will now follow the ion path and arrive at the Triwave cell, consisting of a trap cell, the new IMS cell and a transfer cell. Trap and transfer cell are able to fragment the ions, so you can produce fragments before and/or after separation by ion mobility. Producing fragments is nothing new, most of the MS instruments out there are able to do so.
So consider this big black ion is decayed in the trap cell into three smaller ions, a blue, a red and a green one:
As the figure indicates all fragments have different shape sizes and actually share the same velocity. They now enter the magic IMS cell and an IMS cycle starts. This cell is a combination of two chambers. One small chamber at the front of this cell is flooded with helium and operates as a gate. During an IMS cycle it is impossible that further ions can pass this gate. The main chamber of the IMS cell is filled with nitrogen. The pressures of helium and nitrogen are sensible tuned, such that nitrogen doesn’t form an counterflow for incoming ions. Here is a smart graphic of both chambers:
These nitrogen molecules represent a barrier, so the passing ions are slowed done while they have to find their way through this chamber. Here is the awesome trick located! The bigger the ion shape the bigger the braking force and the slower the ion. A heavy but compact ion might be faster than a lightweight but space consuming ion. So the drift time through the IMS cell is independent of m/z values, it separates the ions by their shape size. Back to the example the blue ion is much smaller so it is much faster, in contrast the fat green ion is inhibited a lot by this nitrogen gas:
Thence the blue fragment arrives first at the transfer cell. Here it is again fragmented in smaller components:
Each of the smaller blue ions then reaches the TOF analyzer. Here they have to fly a specific way, the required time is tracked at the TOF-detector. Heavier ions are slower, so the resulting m/z values are measured here:
The first acquired spectrum is recorded. All blue ions have the same drift time (they were all present when the pusher pushed), but are distinguished by their mass:
At the same time the red ion was able to reach the transfer cell and got also decayed again. Passing the transfer cell they reach the pusher and the next push will make them fly through the flight tube:
All red fragments also have the same drift time, but this time differs from the drift time of the blue ions. Nothing was said about their mass, the m/z isn’t determined before their flight through the TOF analyzer! So it might (and will) happen, that they are lighter than the blue ions. At this point the spectrum will look like this:
The same will happen with the green ions. Entering transfer cell, getting decayed, flying with the next push:
At the end the spectrum produced by the big black ion might look like this:
You see, the drift time is measured without any additional IMS detector! A common MS instrument is just able to record the left m/z spectrum, so if it produces the same seven fragments you are only able to identify five peaks. Since the dark blue and the light red ions have the same mass (they are called isobars) the produced peak is a merge of both ions. Same issue with the dark red and the light green ion. The new IMS technology now enables you to split this peak by the required drift time. Nice, isn’t it?
Ok, so far, back to reality! First of all I have to say the images are not true to scale, I’ve warped the elements for a better representation. The size of the IMS cell is not comparable with the size of the TOF! Fortunately the IMS cell was broken so I was able to look into the machine (figure 1). While the TOF is about 1m the IMS cell is a bit longer than half of a keyboard length, see figure 2. By the way the ions don’t fly a linear way through the TOF analyzer. The Synapt operates with reflectrons and knows two modes: V-TOF (ions are reflected once) and W-TOF (ions are reflected three times).
The energy beam transporting the ions through the IMS cell can be understood as a wave. You can define the wave height and the velocity to effectively separate your present ions. Don’t ask me why the call it height and velocity, and not amplitude and frequency, but what ever ;-) These two parameter are nevertheless very sensitive. So if they are not chosen very well, an ion might need longer then one IMS cycle to pass the cell, so it enters the transfer cell when the next cycle is still started. I don’t have any empirical knowledge yet, but it seems to be hard to find a well setting.
The complexity of this system of curse increases crucial if there isn’t only one big black ion in your machine! So analyzing is not that trivial as my images might induce. You are also able to separately enable or disable fragmentation in trap and transfer cell. So your awareness of this process is essential to understand the resulting data.
In reality one IMS cycle takes the time of 200 pushes, but the pusher isn’t synchronized with the IMS gate. What did he say? Time to get confused! If an IMS cycle takes exactly the time of 200 pushes, ions that arrive between two pushes (one push of course takes some time) should be lost every time, because they should arrive with the next IMS cycle, exactly +200 pushes, again between two pushes. This scenario would mean your sensitivity is crap. Theoretically correct, but fortunately we can’t count on our hardware. Even if you tell the pusher to push every 44 μs, the consumed time will fluctuate in the real world. So he’ll need 45 μs for one push and 43.4 μs for the following. Instead an IMS cycle will always take 44*200=8800 μs, independent of the real time the pusher needs for 200 pushes. So if an IMS cycle starts exactly with a push the next cycle will probably start within two pushes and ions that weren’t able to catch a push last time might now get pushed.
All in all you have to agree that this is an absolutely great invention. If you are interested in further information Waters provides some videos to visualize the IMS technology, and here you can find some smart pictures of the Triwave system in a Synapt.