Gamma Spectroscopy – How to identify radioactive isotopes!

Welcome back my fellow radiation nerds. Today we are diving deep into the world of gamma spectroscopy and how can we use it to identify different radioactive isotopes.

So what is gamma spectroscopy?

Gamma spectroscopy is a technique used to identify and analyse different radioactive isotopes based on their characteristic gamma energies that they emit.

Although this technique has been around since the early 20th century, it was after World War II that the technology began to improve, particularly with the development of scintillation detectors, which allowed scientists to perform more detailed analyses of gamma-ray spectra.

By the 1970s, advances in semiconductor technology led to the creation of detectors like HPGe (High-Purity Germanium), which resolutions far surpassing what can be achieved with traditional scintillation crystals.

For much of its history, gamma spectroscopy has been an expensive tool available only to professionals but in recent years, companies like Gamma Spectacular have made it more accessible and affordable to hobbyists and amateurs alike.

Today, devices like the RAYSID fit can easily in a jeans pocket and still deliver excellent-quality gamma spectra, making gamma spectroscopy easier than ever. Long story short, we are currently in a golden age of gamma spectroscopy.

Scintillation Crystals

There are several methods for detecting and creating gamma spectra, but the most common is by using scintillation crystals. Each crystal type has its advantages and drawbacks and the choice which one to use really depends on the use case. Here are some of the most common ones

NaI(Tl) – Sodium Iodide Thalium Doped crystals are probably the most commonly used scintillation crystals and they are known for producing high-quality gamma spectra and being very sensitive to gamma radiation. However, they are hygroscopic (absorb moisture) and temperature-sensitive, making them better suited for controlled environments rather than in field use.

CsI(Tl) – Cesium Iodide, Thalium doped crystal outperform NaI(Tl) in pretty much every way. They are more durable, dont suffer from moisture absorption and produce better resolution. Their only shortcomings are that they are a bit more expensive and have slower light decay time. They are often used in small, portable scintillation devices like my RAYSID, which uses a 5 cm³ crystal that has a resolution of 6.5% at 662 keV.

BGO – Bismuth Germanate scintillation crystals are known for their density and excellent high energy gamma-ray efficiency. At 662 keV, they typically offer an energy resolution of around 10-12%, making them less suitable for gamma spectroscopy applications compared to other crystals..

LaBr3 – Lanthanum Bromide crystal are relatively new to the market but they quickly gained popularity due to their exceptionally high resolution of below 3.5% at 662keV. Unfortunately due to more difficult production process, they are significantly more expensive compared to more common options such as NaI(Tl or CsI(Tl). Since these crystals use Lanthanum, which by itself is a naturally radioactive due to the isotope La138, they self generate a Lanthanum 138 Gamma spectrum which has to be accounted for when conducting a spectroscopy of low activity samples.

Plastic Scintillators are also common and are made from organic polymers but they produce very low quality spectrum which is generally unsuitable for gamma spectroscopy. Their low price however makes them a great fit for detectors meant only for radiation detection.

HPGe – High purity germanium detectors are a bit different. Instead of scintillation crystal, they use semiconductors which results in extremely good resolution allowing to distinguish peaks that are very close in energy range. While they are the gold standard for resolution, they are less suited for casual use due to their size, high cost and difficult maintenance, as they require liquid nitrogen to keep them at their working temperature which is below 110 kelvin.

Crystal size plays a key role when it comes to gamma ray detection. Depending on what will be measured, it is important to take the size of the crystal into the consideration. For detecting low energy gamma rays and X-rays, it is better to use a thin crystal while for detecting higher energy gammas, a thicker crystal would be a preferred choice. For most cases a crystal size between 1-2″ will be perfectly fine

Photomultiplier tubes (PMT)

Photomultiplier tubes are essential as they convert small flashes of light produced during the interaction of the gamma rays with the scintillation crystal, into electric current which is directly proportional to the gamma energies detected. Their quality and performance will impact the final resolution of the gamma spectrum.

Some small portable devices such as my RAYSID use solid-state Silicone Photo Multipliers (SiPM) instead of the PMT found on bigger detectors. This is mainly because SiPM are more compact and don’t require high voltage to operate making better suited for small detectors.

Sometimes PMT don’t come with voltage dividers, which are crucial to supply adequate power to different pins of the tube. Generally the schematics are easily available online but if soldering is not your strong side, it might be better to get a pre-made kit or just buy a probe that is already assembled and ready to use.

My Scintillation probe

I got my Scintillator probe from my good friend GigaBecquerel (https://gigabecquerel.wordpress.com) who was kind enough to send me one of his spare ones and he also helped me with writing and fact checking this post. If you want to learn more about cool nuclear science projects, then I definitely recommend checking out his blog.

The probe itself is a Bicron 2M2/2 and it uses a 2×2″ NaI(Tl) Crystal which should give a resolution of 6.8% at 662keV. Thanks to the large crystal, the probe is very sensitive and it produces around 130CPS just from the background activity alone. Inside my lead castle, the activity drops to just 12 CPS.

Here is a detailed spec sheet of the detector: https://luxiumsolutions.com/sites/default/files/2021-09/s600-8468.pdf

A probes offered by Gamma Spectacular (affiliated):

1.5×1.5″ NaI(Tl) Detector: https://www.gammaspectacular.com/blue/gs-1515-nai?tracking=6758d3c492392

2×2″ NaI(Tl) Detector: https://www.gammaspectacular.com/blue/GS-2020-NAI?tracking=6758d3c492392

1.5×1.5″ CsI(Tl): https://www.gammaspectacular.com/blue/gs-1515-csi?tracking=6758d3c492392

2×2″ CsI(Tl): https://www.gammaspectacular.com/blue/gs-2020-csi?tracking=6758d3c492392

Spectrometers and the Gamma Spectacular GS-PRO-V5

A scintillator probe is however not enough to start making gamma spectrums. In order to connect the probe to the computer, we need a soundcard Multi-Channel-Analyser (MCA) Spectrometer which will power and convert gamma energies detected by the probe into a usable audio signal.

I’d like to thank Steven from Gamma Spectacular for supporting the channel and sending me one of the GS-PRO-V5 which has inspired this video in the first place.

The unit feels nice and solid and the initial setup was pretty simple and straight forward. It can be used with both single and dual cable probes and its voltage can be easily adjusted from 300 to 2000V making it compatible with a wide range of different detectors. The only change I would make is to move the USB C connector to the back of the device but I guess that is just a matter of personal preference.

There are several different softwares that can be used with Gamma Spectacular but since I personally prefer working on Mac computers, I will be using the IMPUSLE software which has some great features such as a simple and quick, multi-point calibration, and the “energy to bin” switch which makes it much easier to see small peaks from the high energy gamma rays like in the case of Thallium 208 found in the Thorium 232 decay chain.

Get your own Gamma Spectacular (affiliated link): https://www.gammaspectacular.com/blue/gs-pro-v5?tracking=6758d3c492392

Lead castle and minimising background radiation

One last thing before we get started with creating gamma spectra.

Radioactivity is all around us and it is often referred to as background radiation. It can negatively affect the quality of the gamma spectrum and make it harder to see individual peaks especially when the activity o the sample is low. This is why it is why it is important to try to minimise it. For this purpose it is best to use lead shielding as it’s extremely dense making it very effective at cutting background out.

At the moment, I have two lead castles. The first one I made about three years ago to use with my RAYSID. It’s basically a paint can that has another, smaller can inside and the space between them is filled with lead which creates lead walls that are about 2cm thick from all sides.

While lead is great for shielding radiation, it can fluoresce and this results in a X-Ray peak at around 70-80keV. In order to reduce it, I added 2mm thick copper shielding on the inside of the castle.

Here is a spectrum of Cs137 before and after adding additional copper shielding. Pay attention to the Xray peak at 75keV in the spectrum in which copper shielding is missing

While this castle works great and I get inside only 1.2 CPS with my RAYSID compared to ~35CPS outside, it doesn’t work too well with my new, bigger setup. This lead me to building a second castle for my new setup that will work better with a larger detector.

I made it out of lead bricks that I’ve casted myself and while the castle isn’t yet finish by any means and I still need to make a few changes to it, I can already tell that I’m very happy with the fact that I can keep the detector inside at all time without the need to remove it to access the sample.

In the future I’m hoping to get some proffesional Chevron lead bricks which design eliminates any gaps between them allowing for even better background activity inside the castle.

Lead is toxic, so it’s best to avoid touching it with bare hands. I’ve painted my lead bricks to add a layer of protection which works well as it’s very easy to see when the paint starts to chip off and bricks need a repaint.

How does the set-up perform?

After connecting everything and configuring all the settings, I managed to get a nice 6.96% FWMH at 662keV. Maybe with some extra tweaking I can get the resolution to go even lower but I’m definitely happy with my current results.

While I do get slightly better resolution with my RAYSID with 6.5% at 662keV, this new setup is far more sensitive thanks to the much larger crystal.

Now let’s run some gamma spectrums. Each spectrum has been set to a total count of 100k.

Uranium Ore

Gamma Energies: 144, 186, 242, 295, 352, 609 keV


Radium 226 (Radium painted hand watch)

Gamma Energies: 186, 242, 295, 352, 609 keV


Thorium 232 (Gas Mantle)

Gamma Energies: 129, 239, 338, 583, 911, 969, 1588, 2615 keV


Lutetium 176 (LYSO Crystal)

Gamma Energies: 88, 202, 307 keV


Cesium 137 (Spark Gap Tube)

Gamma Energies: 31, 662 keV


Potassium 40 (Potassium Chloride Powder)

Gamma energies: 1461keV


Americium 241 (Smoke Detector)

Gamma Energies: 59.5 keV


Krypton 85 (Robotron Smoke Detector)

Gamma Energies: 514 keV


Conclusion

Since the day I started learning about radioactivity, I always wanted to be able not only to detect but also identify different radioactive isotopes. I love both of my gamma spectrometers and testing anything I can get my hands on and I can’t wait to do more experiments and tests with them!

My new setup with Gamma Spectacular is now permanently stationed by my desk, connected to my computer and ready to start a new spectrum at a moment’s notice, while my RAYSID travels with me as my daily carry radiation detector, always within reach. Both are excellent tools designed for different purposes and use cases, with the RAYSID offering convenience on the go, while the Gamma Spectacular delivering much higher sensitivity, better versitility and better efficiency.

I want to thank Steven from Gamma Spectacular once again for sending me the GS-PRO-V5 and supporting the channel. If you’d like to purchase a Gamma Spectacular for yourself, make sure to use one of my affiliated links, it doesn’t cost any extra and I get a little commission to fund future videos! Until March 31st, 2025, you can also use my code ALLRAD which will give you 5% off from your order. This code is however limited to the first 10 customers so make sure to use it while it last!

Get your own Gamma Spectacular kit (affiliated link): https://www.gammaspectacular.com/blue/GSB-1515-NAI?tracking=6758d3c492392

Also make sure to check out GigaBecquerell’s blog and YouTube channel as he has some great content there!

I want to hear from you, do you have a gamma spectroscopy set-up and what devices do you use? Let me know in the comments below!


Thank you so much for reading this post, I hope you enjoyed it and learned something new! If yes, please make sure to subscribe to the email list so that you get notified when new posts are added. Also feel free to check out my Ko-Fi page where you can donate a nice cup of radioactive coffee and support my work financially.

and remember, stay active!

Exploring What Happened in Bayo Canyon?

Welcome back fellow radiation nerds! Today we dive deep into what really happened in the Bayo Canyon!

Bayo Canyon is located east of Los Alamos, New Mexico and it is a place of striking natural beauty. With its breathtaking landscapes, towering cliffs, and vibrant wildlife, one might assume this area has been a peaceful retreat for ever, but in the 1940s, a series of powerful explosions shocked this place, leaving behind a legacy that endures to this day.

History

During the Manhattan Project, a team of scientists led by high explosive expert, George Kistiakowsky, was tasked with studying the behaviour of radioactive materials under extreme conditions. Their work was critical to the development of the plutonium implosion-type bomb just like the bomb Fat-Man which was later used over Nagasaki.

A total of 242 tests were conducted in Bayo Canyon, with each test using several hundred curies of radioactive materials, primarily radioactive Lanthanum-140 often referred to as “RaLa”, which has a half-life of just 40 hours , however, Lanthanum was not the only radioactive element used .

These tests continued until 1961 and in 1976, the government initiated a cleanup of the area, burying radioactive contaminants deep underground. Yet, to this day, debris can be easily found around the location of the test site with some pieces still exhibiting traces of radioactivity.

Today the Bayo Canyon has slightly elevated activity, though I’m not sure if it’s contamination from the test or is it from natural sources, as I’ve recorded the same increased activity pretty much through out my entire hike to the location of the test site.

Analysis of the samples collected

During my exploration of the canyon, I discovered around two dozen pieces, including metal shrapnel and cable wiring. When inspected closely, you can see how the intense force of the explosions tore the metal apart with ease.

From all the pieces I found, one appears to be radioactivity and clocks around 2000 CPM on my Ludlum Model 3 with a 44-9 probe at 1cm distance. This discovery was particularly intriguing, given that all radioactive Lanthanum-140 should have decayed by now. Curious to uncover its source, I conducted a gamma spectrum analysis of the sample using my RAYSID gamma spectrometer.

The analysis reveals peaks at 63, 93, and 186 keV, which are characteristic for Uranium. Given the small size of the peak at 186 keV, it’s likely that the sample contains depleted uranium instead of regular one as U-235 was in high demand for the production of the uranium bomb, Little Boy, which was later used over Hiroshima.

Conclusion

If you find yourself in Los Alamos with some time to spare, I highly recommend hiking through Bayo Canyon. Whether you’re a nuclear physics enthusiast or a casual tourist, the canyon offers stunning natural beauty, diverse wildlife, and a unique glimpse into the history of atomic bomb development. The hike is about 1.5 hours one way, so be sure to bring plenty of water and prepare accordingly!

Thank you so much for reading this post, I hope you enjoyed it and learned something new! If yes, please make sure to subscribe to the email list so that you get notified when new posts are added. Also feel free to check out my Ko-Fi page where you can donate a nice cup of radioactive coffee and support my work financially.

and remember, stay active!

Radioactive Lanthanum 138

Today we will take a closer look at another naturally occurring radioactive element, Lanthanum!

Lanthanum is a rare earth element and it’s the first element in the lanthanide series. It has an atomic number of 57 and was first discovered by a Swedish chemist, Carl Gustaf Mosander in 1839 but pure Lanthanum wasn’t obtained until 1923. Today, Lanthanum is most commonly used in the production of Tungsten electrodes, scintillators and in the past, it was added to some vintage lenses.

Lanthanum Metal

LaBr3(Ce) Scintilation crystals

Lanthanum Bromide scintillation crystals are well known for their incredible resolution which measures as low as 2.2% at 662 keV and since they have a relatively low price compared to other hi resolution detectors, they are a viable option for amateur gamma spectroscopy setups. These crystals however are not perfect, due to the Lanthanum content, they are slightly radioactive themselves which causes them to self generate a characteristic background spectrum that must be removed if measuring low activity samples.

Radioactivity and gamma spectroscopy

In nature, there are two isotopes of Lanthanum, La-139 (99.91% abundance) and La-138 which has an abundance of 0.09% and it is also radioactive.

Lanthanum 138 has a very long half-life of 1.02E+11 years and its activity cannot be easily detected with a conventional Geiger counter. To do that a large scintillator must be used since it is much more sensitive.

Unfortunately, my sample of Lanthanum is pretty small and my set-up isn’t sensitive enough to detect it so I reached out to my friend Gigabecquerell who has provided a gamma spectrum of his Lanthanum sample.

Lanthanum 138 decays through electron capture or by beta emission and in both cases, it also releases a gamma-ray at 789 keV and 1436 keV.

A gamma spectroscopy reviels two peaks at 789 keV and 1436 keV which are both caused by the decay of Lanthanum 138 through electron capture or by beta emission and in both cases a gamma ray is also released.

Lanthanum 138 gamma spectrum

Radioactive Cobalt 60

Cobalt 60 is a radioactive isotope of Cobalt and it is produced by neutron activation of stable Cobalt 59 in nuclear reactors. Since it has a short half-life of only 5.3 years, it does not occur in nature and all samples that exist are synthetic. A single gram of Co-60 has an activity of 44TBq and it undergoes a beta decay into an excited state of Nickel 60 which emits two gamma rays at 1173 and 1332 keV before becoming stable.

Gamma spectroscopy of Cobalt 60

One of the main uses of Cobalt 60 is in radiotherapy where cancer cells are exposed to a beam of high energy gamma radiation, effectively killing them. Its gamma rays are also used in the sterilisation of food and medical equipment and they can even be used in levelling devices and thickness gauges to detect structural errors.

Bomac 1B63A Waveguide Tube

For decades tubes have been a key component of electrical devices such as radios, amplifiers and many more. Some of these tubes contained radioactive elements which improved the ionisation process and also made them radioactive.

My sample of Co-60 is in an old Bomac 1B63A tube which was originally used in radars and it contained <1uCi of Co-60. These tubes have been manufactured in the late XX century and sadly there is no detectable activity left since almost all of Co-60 has decayed.

Dirty nukes

Unfortunately, Cobalt 60 can also be used in weapons of mass destruction. Dirty nukes or salty nukes are nuclear weapons that contain Cobalt 59 but during nuclear fission, it turns into Cobalt 60 which contaminates the surrounding area for decades. Officially, there are no countries in possession of such weapons and let’s hope that even if there are, they will never use them.

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Radioactive Lutetium (176 & 177)

Uranium and Thorium along with Potassium are the most common, naturally occurring radioactive isotopes but there are also many other, lesser-known ones. One of them is Lutetium, which will be today’s main topic.

Lutetium is the last element in the Lanthanide series and it has been discovered in 1907 by French scientist Georges Urbain. Today Lutetium has very little commercial use due to its difficult production and high price but one of the uses is in the production of scintillation crystals which are used in positron emission tomography.

LYSO crystal

In nature, there are two isotopes of lutetium, 175Lu and 176Lu. Lutetium 176 is radioactive and it decays by a Beta emission into Hafnium 176 with a half-life of 37.8 billion (3.78×1010) years. Since Lutetium has a very long half-life, it is used in Lutetium-Hafnium dating of meteorites.

Lutetium has small, but detectible activity. My sample, which an LYSO crystal, measures 16 CPS above background on my RAYSID which has a [5cm3 (CsI(Tl) crystal]. Such activity is more than enough for gamma spectroscopy but it is not for measuring with a Geiger counter.

Lutetium has a very interesting gamma spectrum, it emits two gamma rays (202 keV and 307 keV) but since they are emitted at the exact same time, they sum up and form a peak at 509 keV.

176Lu gamma spectrum

Another use of lutecium is in the treatment of prostate cancer where a synthetic isotope of lutetium, 177Lu, is injected into patient’s body where it irradiates and kills cancer cells. Lutetium 177 emits two gamma rays at 113 keV and 208 keV.

177Lu gamma spectrum

Radioactive tubes and electronics!

Introduction

Small amounts of radioactive isotopes are often used in common household items. A good example of that would be 241Am in smoke alarms or 226Ra in watches but today, I want to focus on tubes (valves) and other less common electrical components containing radioactive isotopes!

TG-36 Spark Gap Tube

Isotope: 137Cs

Activity originally: <1 uCi

TG-36 is a spark gap tube most probably produced in the late 1960s or early 1970s and it originally contained around 1 uCi (37 kBq) of 137Cs. Even though some 137Cs has decayed, it is still active enough so that it can be used as a calibration source for gamma spectroscopy as well as a check source for Geiger counters. When placed right against my RAYSID gamma spectrometer with a CsI(Tl) 5cm3 crystal, the activity increased by 218 CPS.

Bomac 1B63A Waveguide Tube

Isotope: 60Co

Activity (originally): <1 uCi

1B63A tube contains a small amount of 60Co which was used to better ionise the gas inside of the tube. Originally these tubes contained 1 uCi of Cobalt-60, however, Cobalt-60 has a rather short half-life of only 5.3 years, which means that there is less than 0.013 uCi left which means that there is no detectable activity. A gamma spectrum of Cobalt-60 should show two characteristic peaks at 1173 keV and 1332 keV.

DV3A Voltage Regulator Tube

Isotope: 63Ni

Activity: not detectable

Victoreen’s DV3A is a voltage regulator tube containing a microscopic amount of 63Ni. These tubes can be found in some old US survey meters from the cold war. I found mine in my Eberline 120 survey meter that I have bought some time ago without even knowing the tube contained any radioactive isotopes! Unfortunately, 63Ni emits only weak beta radiation which is not able to go through the glass tube and even if it would, the amount of 63Ni is too small to be detected.

2x2a Rectifier Tube

Isotope: None

Activity: None

While this tube does not contain any radioactive isotopes it can generate x-rays if hooked to a high voltage. Sadly, I don’t own a power supply capable of generating high voltage so I won’t be able to demonstrate it. Maybe one day…

AZS Switch

Isotope: 226Ra

Activity: 17.1k CPM (STS-5)

AZS switches were often used in different vehicles such as tanks and military planes produced in the Warsaw pact. The tip of the switch has radium 226 paint on it in order to make it glow in the dark but it also causes it to be very radioactive and emit huge amounts of radon since most of these switches are not sealed as a result of their age. It is worth mentioning that newer AZS have a non-radioactive, glow in the dark paint. An easy way to check if the switch contains 226Ra is simply to check if it glows in the dark. If NOT, then it is most probably radium.

BH-45M

Isotope: 226Ra

Activity: 200k CPM (LND 7311)

BH-45M is very similar to the above mentioned AZS with the main difference being a slightly smaller activity.

Wait, there is more!

If you know of any interesting tubes, switches and other electrical components containing radioactive isotopes, let me know in the comments section and I’ll do my best to get them and add them to the post!

This is NOT Uranium Glass!

Items generating “Negative Ions” are no strangers to this channel. In fact, my first proper video was on one of them! Today we take a closer look at another pendant but this one is pretty special!

Unlike the old pendant, this one is made out of green glass which also glows under black light and is radioactive so my first assumption was that it must be uranium glass.

Uranium glass (aka vaseline glass) was produced mainly during the age of atomic madness however because of the nuclear weapons, people got scared of radiation and as a result, they stopped buying products containing uranium. Today, Uranium glass can be mainly found in antique shops but also in the Czech Republic because it is one of the very few countries producing Uranium glass!

Uranium glass under the black light

Anyhow, back to the pendant. My first guess was that it was made out of Uranium glass but just to be sure, I did gamma spectroscopy of it. To my surprise, gamma spectroscopy revealed that the pendant did not contain uranium but Thorium meaning that this Thorium glass! When compared to Uranium glass, Thorium glass looks a little bit darker and it doesn’t glow so brightly under black light. It is also much more radioactive (U-Glass X CPM, Th-Glass 3 000 CPM)

Mysterious Green Glass Pendant Gamma Spectrum.

After making a video on my first negatrive ion pendant, many people pointed out to me that the authenticity card is also radioactive but sadly I could not detect anything. Who knows, maybe they are running out of Thorium?

If you got any suggestions for future post, feel free to post them in the comments section below!

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