Nuclear Chemistry .2 Chemistry Midland High School Mrs. Daniels 2007 Back to the Beginning Recall the particles that make up an atom: Proton (+1 charge) Neutron (no charge) Electron (-1 charge) If you write out the symbol for an element and include the atomic number and the atomic mass, it should look like this: 23 Na 11 For sodium: the symbol is Na the atomic mass is 23 and the atomic # is 11 What information can you take from the following? 238 How many e-? P+? n0? e-=92 p+=92 n0=146 U 92 Isotopes What if I change the # of protons? It would be a different element What if I change the # of electrons It would be an ion What if I change the # of neutrons It would be the same element, but a different ISOTOPE of that element Hydrogen Let’s look at a couple of isotopes of hydrogen 1 H 1 2 H 1 The one on the left is referred to as “light” hydrogen and the one on the right is “heavy” Which one is the “normal” hydrogen that we usually see Variety of Isotopes Even though there are ~110 different elements listed on the periodic table, there are nearly 1500 different known isotopes of these elements Some are stable and some “decay” or break apart over time Nuclear Decay All nuclear decay is accompanied by the emission of radiation Spontaneous emission of radiation from an atom is called radioactivity All elements have isotopes that are unstable and underdo decay to become other element Nuclear Decay Radioactive isotopes can emit three types of radiation: Alpha particles: a helium nucleus (2 protons, 2 neutrons, with a charge of +2) Not very fast; can be blocked by something as thin as a piece of paper Beta particles: fast moving electrons created from the splitting of a neutron (into a proton and an electron) Requires aluminum foil 3mm thick to Nuclear Decay Gamma rays: radiation that is NOT particles at all, but are invisible rays of energy with no mass or electrical charge Very penetrating; need several cm of lead or several meters of concrete to stop Emitting alpha or beta particles changes the element into a new element This is called nuclear transformation Detection How do we know that radiation is being released or emitted? There are several types of “counters” used to detect radiation: Geiger counter- uses Argon to transfer the radiation into a temporary electric pulse Scintillation counter - uses sodium iodide to produce flashes of light when in contact with radiation Half - Life We can also go larger scale and look at the half life of various isotopes Half life is defined as the time it takes for HALF of the sample of element to decay For example, the half life of carbon-14 is 5,730 years Half - Life Calculate how many years it would take to decay 100g of carbon-14 into 12.5g. Think on this: how many times was 100 cut in half to get to 12.5? 100 --> 50 50 --> 25 25 --> 12.5 So… 3 half lives If each half life takes 5,730 years and we cut our sample in half three times, how long did it take? 5,730 x 3 = 17,190 years Roughly how much of a 100.0g sample would be left after 1 year? Well, 50g will take 5,730 years to decay A good estimate would be that .0087g would decay each year So… 100.0-.0087 = 99.99g We’d actually have to graph it to determine this more accurately Radioactive Dating Carbon-14, potassium-40, and others are isotopes can be used for dating objects from the past We need to make the following assumptions for carbon dating: All living organisms contain the same ratio of carbon-14 atoms and decay begins upon death Remains of organisms or items created from once living organisms contain the remaining amount of carbon-14, which can be measured Radioactive Dating If we know the half life of carbon-14 is 5,730 years and we make the above assumptions, then we can compare the amount of carbon-14 in the sample with the amount of carbon-14 in a living organism Then, we simply calculate how many half-lives the material underwent and multiply by 5,730 years per half life Ta Daa! Now, we know how old it is…roughly Fission and Fusion With all the discussion of nuclear power…we HAVE to talk about fission and fusion. Nuclear fusion: combining (FUSING together) two lighter nuclei to form a heavier nucleus Nuclear fission: splitting a heavy nucleus into two smaller nuclei with smaller mass numbers Nuclear Fission Bombarding various isotopes with neutrons can cause an isotope to split into two lighter elements The splitting is not always equal, so two different elements may be produced Also, excess neutrons fly off during the splitting process and hit other atoms of the isotope This begins several other fission reactions in the CHAIN of events Fission Continued A huge amount of energy can be released from nuclear fission reactions For example, splitting one mole of uranium-235 is 26 million times the energy released from the combustion of one mole of methane Chain Reaction Fission Continued If no neutrons go flying off and cause the chain reaction to keep going, then the reaction stops If more than one neutron causes a new “chain” in the reaction, a build up of heat and an explosion can happen The “critical mass” of fissionable material is needed to maintain a productive and constant fission reaction Nuclear Fusion Produces even more energy than nuclear fission; however, initiating the fusion reaction is much more difficult Protons don’t want to come together because they repel each other Temperatures of ~40 million K are estimated to be necessary to overcome the repulsion forces Figure out a way to do it at more manageable temps (ie cold fusion) and you’ll be very rich and famous Don’t forget to thank your high school chemistry teacher if this happens