Understanding Carbon 14 Half Life
Carbon 14 is a radioactive isotope of carbon. It forms in the upper atmosphere. Living plants and animals take it in. They keep exchanging carbon while alive. After death, exchange stops. The carbon 14 atoms then decay at a steady rate.
Why Half Life Matters
A half life is the time needed for half of a radioactive sample to decay. Carbon 14 is commonly modeled with a half life of 5,730 years. This makes it useful for dating once living material. It is best for archaeological, geological, and forensic samples within useful age ranges.
What This Calculator Does
This tool handles several common chemistry cases. It can find remaining carbon 14 after a known time. It can estimate age from fraction modern, percent modern, activity ratio, or counting data. It also reports decay constant values, remaining percent, decay percent, atom estimates, and activity estimates when mass is supplied.
Using Measured Activity
Activity measures decays per second. A fresh standard has higher activity than an old sample. The ratio between measured activity and original activity gives the remaining fraction. The calculator can also subtract background counts from both sample and standard. That step helps remove detector noise and natural background radiation.
Interpreting Results
Radiocarbon results are estimates. Contamination can add new carbon or old carbon. Reservoir effects can shift apparent age. Instrument calibration can also change calendar age. This page gives the mathematical radiocarbon age. It does not replace laboratory calibration curves or expert sample preparation.
Good Practice
Use clean data. Enter units carefully. Keep half life values consistent. Use the physical half life for basic decay work. Use the Libby value when matching conventional radiocarbon age rules. Always record assumptions beside the result. The CSV and PDF options help keep a clear record.
Useful Output Notes
The decay constant shows the yearly decay rate. The mean life shows the average lifetime of one atom. Remaining mass helps when the initial carbon 14 mass is known. Remaining percent is easier for quick checks. Age output is shown in years before present. In radiocarbon work, present means 1950. Use the uncertainty range as a rough mathematical spread only. It is not a full calibration or contamination model.