Search results
• Alpha particles carry a positive charge, beta particles carry a negative charge, and gamma rays are neutral. • An alpha particle is made up of two protons and two neutrons bound together. • Beta particles are high energy electrons or positrons.
People also ask
What is the difference between beta decay and gamma decay?
What is alpha decay?
What happens when a nucleus ejects a beta particle?
What is the difference between a gamma ray and a beta particle?
Gamma rays are simply high energy photons, electromagnetic radiation. When a nucleus still has too much energy, but is done releasing alpha and beta decay particles, it will release the energy by swapping the spin of a neutron or proton and releasing a high energy photon in the process.
- simply speaking, the electrons in your finger are pushing the electrons of the object. Think of trillions of magnets in your finger with North faci...
- Yes! That has huge practical consequences e.g. for the choice of materials for the reactor vessels of nuclear power plants. You have to make sure t...
- "elektron" is the greek word for amber. It was the first material which was shown to have "strange" properties when rubbed (eg it attracted things)...
- Neutrons do *not* consist of a proton and an electron! Neutrons are made of three quarks: two "down" (short: d) quarks and an "up" (u) quark. A "d"...
- n --> p + e + neutrino In the decay process a certain (fixed) amout of energy is released and shows up in the kinetic energy of the three product p...
- You're right Michael, the positron (+ charge) would be attracted to, and annihilate with an electron (- charge) to produce energy equal to the comb...
- "instable" means that it is a state with excess energy which can undergo some process to reach a state of lesser energy. "Decay" of some sort provi...
- Yes, there are three types of nuclear decay. Alpha decay - an alpha particle emitted (alpha particle = nucleus of He atom --> 2 protons and 2 neutr...
- He-4 is a very stable nucleus configuration. It has an extremely high binding energy relative to the number of nucleons and is much more likely to...
Jan 3, 2024 · Radioactive decay, a spontaneous process, involves the transformation of an unstable atomic nucleus into a more stable one. On the MCAT, you’ll be expected to memorize and understand three different kinds of radioactive decay: Alpha, Beta, and Gamma. As Easy As Learning Your A, B, G’s.
Feb 12, 2021 · (Note: This guide is part of our MCAT Physics series.) Table of Contents Part 1: Introduction to atomic and nuclear physics Part 2: Atomic structure. a) Nuclear structure. b) Components of the nucleus. Part 3: Radioactive decay. a) Alpha decay. b) Beta decay. c) Gamma decay. d) Half-life and exponential decay. Part 4: High-yield terms and equations
- How can scientists tell when something is releasing radiation?
- How do you read a decay graph?
- What is a half-life?
- Consider the following… carbon dating
We know that radiation is more than just the spooky, silent threat that we see in movies. Healthcare providers can actually harness the unique properties of radiation to look inside the human body and diagnose diseases in new ways. We also know that all radiation occurs when an unstable nucleus releases energy to become more stable. This happens when the nucleus changes into a different nucleus This happens in three different ways:
1.Alpha decay: The nucleus splits into two chunks, a little chunk called an “alpha particle” (which is just two protons and two neutrons) and a daughter nucleus with a lower atomic number than the initial nucleus. The “radiation” here is the small chunk, which generally moves away from the nucleus at a pretty high speed.
2.Beta decay: There are two types of beta decay: In beta-minus decay, a neutron in an atom changes into a proton, an electron, and an antineutrino, creating and releasing an electron along the way (since the total charge has to stay the same!). The radiation here is the super fast-moving electron released. In beta-positive decay, a proton turns into a neutron, causing the nucleus to shoot out an exotic positive particle called a “positron” or “anti-electron.”
3.Gamma decay: The number of protons, neutrons, and electrons stays the same, but they rearrange themselves within the atom, giving off energy in the form of high-energy photons (gamma radiation), in order to have lower overall energy.
For all of these cases, the total amount of the radioactive element decreases over time. So if a scientist takes a chunk of carbon-10 (which undergoes beta decay), counts the number of carbon-10 atoms inside it, goes to make coffee, and then comes back to count the number of atoms again, she’ll find that the total number of atoms of carbon-10 is now smaller! In their place she’ll find the beta decay product of carbon-10, which is the element boron.
Although the decay of individual nuclei happens randomly, it turns out that large numbers of nuclei can be modelled by a mathematical function that predicts the amount of radioactive nuclei remaining at a given time:
If a scientist comes across a funky new radioactive rock while exploring an excavation site, she can identify what radioactive isotope is present in it by measuring the the decay constant of the isotopes inside the rock.
An exponential decay graph like the one shown above can be generated by taking a sample of an unknown radioactive isotope and repeatedly measuring the total mass of radioactive material within it. At the start of the experiment, a piece of the sample is run through a mass spectrometer or similar device that can identify the relative mass of various isotopes currently present. Then, at several later times, the procedure is repeated and the new fraction of various isotopes is recorded.
The fraction of radioactive isotopes observed in the spectrometer will decrease exponentially in time, while the mass of decay products (like boron for carbon-10) will gradually increase. The scientist can use this information to draw an exponential decay plot like the one above and estimate the decay constant. She can then look her value up in a glossary of known radioactive decay constants to figure out which isotope is in her sample.
Another type of graph that scientists like to use to show nuclear decay data is a semilog plot (shown below)
Semilog plots are pretty tricky because the vertical axis has funny spacing. In the plot above, 100 appears to come halfway between 10 and 1000. This is because when we take logarithms of these numbers we get log(1000)=6.9, log(100)=4.6, log(10)=2.3, which are evenly spaced. So when we read the slope on a semilog plot, we need to remember to always take the logarithm of whatever values we read off the vertical axis. The slope of the line on the semilog plot corresponds to the same decay constant k, that we can identify in a normal exponential decay plot.
But, when decay data is plotted as it is in our exponential decay graph, the decay constant is much harder to figure out because it’s not that easy to compare the “sharpness” of different exponential decay curves. Finding the slope of straight lines, however, is generally much easier. By plotting data on semi-log plots, the scientist can better compare and identify different isotopes.
Half-life is defined as the amount of time it takes for half of an isotope to change into another isotope.
Like the decay constant, the half-life tells us everything we need to know to guess what kind of isotope we might have. It even turns out that the two numbers are equivalent if you correctly solve the radioactive decay equation. This means that, like the decay constant, the half-life gives an estimate of the stability of a particular radioactive substance, and it can thus be used to identify unknown isotopes. The primary reason that scientists use half-lives instead of decay constants is because half-lives have a more intuitive immediate meaning: if a scientist collects 20 kg of a radioactive isotope with a half-life of 30 min, and she leaves her lab to meet with a grad student for 30 minutes, when she comes back she will have 10 kg of the isotope remaining. If she then goes to check on another experiment for 30 minutes, when she gets back she will have 5 kg remaining… in other words, for every 30 minutes that passes, she’ll lose half of her sample!
Most living things contain carbon-14, an unstable isotope of carbon that has a half-life of around 5,000 years. That means that when scientists dig up fossil bones, they can figure out how old they are by measuring the amount of carbon-14 remaining in the bones. For example, if a fossil bone has half as many of carbon-14 nuclei as a new, non-fossilized bone, then scientists can guess that the fossil is roughly 5,000 years old. This technique of carbon dating has been used to estimate the ages of fossils from many different periods in Earth’s history, and at its core it simply relies on scientists drawing decay graphs and counting the number of half-lives that have passed. Carbon dating was recently used to study one of the oldest human-like fossils ever found, and it determined that it was nearly 100,000 years old!
[Licensing]
Beta decay is when the nucleus ejects a beta particle (electron). Alpha decay is when the nucleus ejects an alpha particle (helium nucleus). Electron capture is when the nucleus caputres an electron from the inner most shell.
The passage tells us that we have a couple kinds of radiation that are occurring. We have gamma emissions or emitting light, we’re doing gamma decay. And we’re also doing beta minus decay. Gamma Decay. In gamma decay, just the nucleus reorganizes slightly, and it becomes more stable.
