More cards in this set

Card 6

Front

The process by which an unstable atomic nucleus loses energy by radiation and transform into stable isotopes, e.g. 14C -> 14N

Back

Preview of the front of card 6

Card 7

Front

The exponential rate at which radioactive decay occurs as displayed on a graph

Back

Preview of the front of card 7

Card 8

Front

The number of protons and neutrons in the nucleus of a carbon atom

Back

Preview of the front of card 8

Card 9

Front

14C forms in the upper atmosphere when 14N is bombarded by...

Back

Preview of the front of card 9

Card 10

Front

A method of measurement: the counting of beta particle emissions over a standard length of time

Back

Preview of the front of card 10

Card 11

Front

A method of measurement: an accelerated mass spectrometer is used to count the number of 14C atoms present, instead relying on emission of their daughter products. Can process smaller samples, e.g. insect remains, individual seeds, etc.

Back

Preview of the front of card 11

Card 12

Front

Rate of 14C production in the atmosphere is constant. 14C uptake by organisms is in equilibrium with their environment. No new 14C enter an organism after death, so the concentration is entirely a function of time since death. No "old" carbon is recycled

Back

Preview of the front of card 12

Card 13

Front

Who won the Nobel prize for developing this technique in the 1940s?

Back

Preview of the front of card 13

Card 14

Front

Calculates an age in years for geologic materials by measuring the presence of a short-life radioactive element, e.g. 14C. A type of this dating method is radiocarbon (14C) dating.

Back

Preview of the front of card 14

Card 15

Front

This technique allows the construction of year-by-year annual chronologies which can be temporally fixed (linked to the present day) or floating, e.g. dendrochronology

Back

Preview of the front of card 15