# Radioactive dating methods beyond 60000 years

### Dating Methods Using Radioactive Isotopes

This breakdown age is about 60, years old. .. For all manner of reasons beyond radiometric dating, such as thick sequences of sediments. This method is sometimes called C or carbon dating. radiocarbon dating cannot be used for samples older than around 60, years, or ten half-lives. Non-Radiogenic Dating Methods for the Past , Years Radiometric dating techniques indicate that the Earth is thousands of times older Tree rings do not provide continuous chronologies beyond 11, years ago because a . Ages of 60, years may be off by up to 10%, and the uncertainty rises to 20% for.

These different forms of an element—called isotopes—are inherently stable or unstable. The latter are called radioactive isotopes, and over time they will decay, giving off particles neutrons or protons and energy radiation and therefore turn into another isotope or element. They do this at a constant rate called an isotope's "half-life". Most carbon comes in the stable forms of carbon six protons, six neutrons or carbon, but a very small amount about 0. Living plants and animals take up carbon along with the other carbon isotopes, but when they die and their metabolic functions cease, they stop absorbing carbon.

Over time, the carbon decays into nitrogen; half will do so after about 5, years this is the isotope's half-life.

After about 60, years, all of the carbon will be gone. Anything that was once part of a living object—such as charcoal, wood, bone, pollen or the coprolites found in Oregon—can be sent to a lab where scientists measure how much carbon is left.

## Radiometric dating

Because they know how much there would have been in the atmosphere and, therefore, how much someone would have absorbed when alive, they can calculate how long it has been since death or deposition. The coprolites averaged about 14, years old and are some of the oldest human remains in the Americas.

Hominid skulls, Herto, Ethiopia Age: How old were they? The organic remains were too old for carbon dating, so the team turned to another method. Radiocarbon dating works well for some archaeological finds, but it has limitations: However, there are other radioactive isotopes that can be used to date non-organic materials such as rocks and older materials up to billions of years old. One of these radioisotopes is potassium, which is found in volcanic rock. After the volcanic rock cools off, its potassium decays into argon with a 1.

It is possible to measure the ratio of potassium to argon and estimate a rock's age, but this method is imprecise. However, scientists discovered in the s that they could irradiate a rock sample with neutrons and thereby convert the potassium to argon, an isotope not normally found in nature and easier to measure. Though more intricate, this process yields more precise dates.

Alternatively, if several different minerals can be dated from the same sample and are assumed to be formed by the same event and were in equilibrium with the reservoir when they formed, they should form an isochron.

This can reduce the problem of contamination.

In uranium—lead datingthe concordia diagram is used which also decreases the problem of nuclide loss. Finally, correlation between different isotopic dating methods may be required to confirm the age of a sample. For example, the age of the Amitsoq gneisses from western Greenland was determined to be 3.

The procedures used to isolate and analyze the parent and daughter nuclides must be precise and accurate. This normally involves isotope-ratio mass spectrometry. For instance, carbon has a half-life of 5, years.

After an organism has been dead for 60, years, so little carbon is left that accurate dating cannot be established. On the other hand, the concentration of carbon falls off so steeply that the age of relatively young remains can be determined precisely to within a few decades. Closure temperature If a material that selectively rejects the daughter nuclide is heated, any daughter nuclides that have been accumulated over time will be lost through diffusionsetting the isotopic "clock" to zero.

The temperature at which this happens is known as the closure temperature or blocking temperature and is specific to a particular material and isotopic system.

These temperatures are experimentally determined in the lab by artificially resetting sample minerals using a high-temperature furnace. As the mineral cools, the crystal structure begins to form and diffusion of isotopes is less easy.

### Radiometric dating - Wikipedia

At a certain temperature, the crystal structure has formed sufficiently to prevent diffusion of isotopes. This temperature is what is known as closure temperature and represents the temperature below which the mineral is a closed system to isotopes. Thus an igneous or metamorphic rock or melt, which is slowly cooling, does not begin to exhibit measurable radioactive decay until it cools below the closure temperature.

The age that can be calculated by radiometric dating is thus the time at which the rock or mineral cooled to closure temperature. This field is known as thermochronology or thermochronometry. The age is calculated from the slope of the isochron line and the original composition from the intercept of the isochron with the y-axis. The equation is most conveniently expressed in terms of the measured quantity N t rather than the constant initial value No.

The above equation makes use of information on the composition of parent and daughter isotopes at the time the material being tested cooled below its closure temperature. This is well-established for most isotopic systems. Plotting an isochron is used to solve the age equation graphically and calculate the age of the sample and the original composition.

Modern dating methods[ edit ] Radiometric dating has been carried out since when it was invented by Ernest Rutherford as a method by which one might determine the age of the Earth. In the century since then the techniques have been greatly improved and expanded. The mass spectrometer was invented in the s and began to be used in radiometric dating in the s.

It operates by generating a beam of ionized atoms from the sample under test. The ions then travel through a magnetic field, which diverts them into different sampling sensors, known as " Faraday cups ", depending on their mass and level of ionization. On impact in the cups, the ions set up a very weak current that can be measured to determine the rate of impacts and the relative concentrations of different atoms in the beams.

Uranium—lead dating method[ edit ] Main article: Uranium—lead dating A concordia diagram as used in uranium—lead datingwith data from the Pfunze BeltZimbabwe. This scheme has been refined to the point that the error margin in dates of rocks can be as low as less than two million years in two-and-a-half billion years.

Zircon has a very high closure temperature, is resistant to mechanical weathering and is very chemically inert. Zircon also forms multiple crystal layers during metamorphic events, which each may record an isotopic age of the event.

This can be seen in the concordia diagram, where the samples plot along an errorchron straight line which intersects the concordia curve at the age of the sample. Samarium—neodymium dating method[ edit ] Main article: Samarium—neodymium dating This involves the alpha decay of Sm to Nd with a half-life of 1.

Accuracy levels of within twenty million years in ages of two-and-a-half billion years are achievable. Potassium—argon dating This involves electron capture or positron decay of potassium to argon Potassium has a half-life of 1.

Rubidium—strontium dating method[ edit ] Main article: Rubidium—strontium dating This is based on the beta decay of rubidium to strontiumwith a half-life of 50 billion years. This scheme is used to date old igneous and metamorphic rocksand has also been used to date lunar samples. Closure temperatures are so high that they are not a concern.

Rubidium-strontium dating is not as precise as the uranium-lead method, with errors of 30 to 50 million years for a 3-billion-year-old sample.

Uranium—thorium dating method[ edit ] Main article: Uranium—thorium dating A relatively short-range dating technique is based on the decay of uranium into thorium, a substance with a half-life of about 80, years.

It is accompanied by a sister process, in which uranium decays into protactinium, which has a half-life of 32, years.

### measurements - Radioactive Dating Accuracy After 60, years - Physics Stack Exchange

While uranium is water-soluble, thorium and protactinium are not, and so they are selectively precipitated into ocean-floor sedimentsfrom which their ratios are measured. The scheme has a range of several hundred thousand years. A related method is ionium—thorium datingwhich measures the ratio of ionium thorium to thorium in ocean sediment. Radiocarbon dating method[ edit ] Main article: Carbon is a radioactive isotope of carbon, with a half-life of 5, years, [25] [26] which is very short compared with the above isotopes and decays into nitrogen.