Radioactive Dating

An ingenious application of half-life studies established a new science of determining ages of materials by half-life calculations. For geological dating, the decay of U -238 can be used. The half-life of U-238 is 4.5×109 years. The end product of the decay of U-238 is Pb-206. After one half-life, a 1.00 gram sample of uranium will have decayed to 0.50 grams of U-238 and 0.43 grams of Pb-206. By comparing the amount of U-238 to the amount of Pb-206 in a sample of uranium mineral, the age of the mineral can be estimated. Present day estimates for the age of the Earth's crust from this method is at 4 billion years.

Organic material (material made from things that were once living, such as paper and fabric) is radioactively dated using the long-lived nuclide of carbon, carbon-14. This method of determining the age of organic material (or once living materials) was given the name radiocarbon dating. The carbon dioxide consumed by living systems contains a certain concentration of ¹⁴CO₂ . When an organism dies, the acquisition of carbon-14 stops but the decay of the C-14 in the body continues. As time goes by, the ratio of C-14 to C-12 decreases at a rate determined by the half-life of C-14. Using half-life equations, the time since the organism died can be calculated. These procedures have been used to determine the age of organic artifacts and determine, for instance, whether art works are real or fake.

مواضيع ذات صلة

الخواص الطيفية للاحماض الامينية Spectroscopic of Amino Acids

الاحماض الامينية غير البروتينية Non-protein Amino Acids

الاحماض الامينية النادرة في البروتينات

تصنيف الاحماض الامينية

امتصاص النيوترونات Absorption of Neutrons

طرائق امتصاص الدقائق المشحونة الثقيلة

طرائق امتصاص الدقائق المشحونة الخفيفة

التفاعلات النووية الضوئية Photonuclear Reactions

الاستطارة المترابطة Coherent Scattering

ظاهرة انتاج مزدوج الكترون-بوزترون

تأثير كومبتون Compton Effect

التأثير الكهروضوئي Photoelectric Effect