Double electron capture is a decay mode of atomic
nucleus
. For a nuclide (A, Z) with number of nucleons A and
atomic number
Z, double
electron
capture has to occur when the mass of the nuclide of (A, Z-2) is lower. |
In this mode of decay, two of the orbital
electrons
are captured by two
protons
in the
nucleus
, forming two
neutrons
. Two
neutrinos
are emitted in the process. Since the
protons
are changed to
neutrons
, the number of
neutrons
increases by 2, the number of
protons
Z decreases by 2, and the
atomic mass
A remains unchanged. By changing the number of
protons
, double
electron
capture transforms the nuclide into a new
element
. |
Example: |
|
There exist 35 naturally occurring
isotopes
that can undergo double
electron
capture. However, there are no confirmed observations of this process. The one reason is that the probability of double electron capture is enormously small (the theoretical predictions of
half-lives
for this mode lies well above 1020 years). The second reason is that the only detectable particles created in this process are
X-rays
and Auger electrons that are emitted by the excited atomic shell. In the range of their energies (~1 to 10
keV
), the background is usually high. Thus, the experimental detection of double
electron
capture is more difficult than that for double beta decay. |
If the mass difference between the mother and daughter atoms is more than two masses of
electron
(1.022
MeV
), the energy released in the process is enough to allow another mode of decay:
electron
capture with
positron
emission. It occurs simultaneously with double electron capture, their branching ratio depending on nuclear properties. When the mass difference is more than four electron masses (2.044
MeV
), the third mode - double
positron
decay - is allowed. Only 6 naturally occurring nuclides can decay via these three modes simultaneously. |