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Out-of-Body Exploration Methods
Radiometric dating - Wikipedia
Begin by placing a full length mirror in the room you have selected for out-of-body exploration. The mirror should be placed in a location which allows you to easily see your entire reflection without any physical movements. As you look into the mirror, begin to study and memorize your image. Become as objective as possible and view your reflection as an object you are about to paint in your mind. Pay close attention to the small details of your body and clothes.
Measurement of N, the number of 14 C atoms currently in the sample, allows the calculation of t, the age of the sample, using the equation above. The above calculations make several assumptions, such as that the level of 14 C in the atmosphere has remained constant over time. The calculations involve several steps and include an intermediate value called the "radiocarbon age", which is the age in "radiocarbon years" of the sample: Radiocarbon ages are still calculated using this half-life, and are known as "Conventional Radiocarbon Age".
Radioactive decay[ edit ] Example of a radioactive decay chain from lead Pb to lead Pb. The final decay product, lead Pb , is stable and can no longer undergo spontaneous radioactive decay. All ordinary matter is made up of combinations of chemical elements , each with its own atomic number , indicating the number of protons in the atomic nucleus. Additionally, elements may exist in different isotopes , with each isotope of an element differing in the number of neutrons in the nucleus. A particular isotope of a particular element is called a nuclide.