Radioactive decay is random; we can not predict when a particular nucleus in a sample will decay or which one will decay. Each nucleus within a sample has the same chance of decaying per unit time.
Radioactive decay is spontaneous because the decay of nuclei is not affected by the presence of other nuclei in the sample and external factors such as pressure.
The half-life of an isotope is the average time it takes for half the number of active nuclei in the sample to decay.
The activity A of a source is the rate at which nuclei decay or disintegrate.
Activity = Decay constant x number of nuclei in the sample.
The decay constant has SI unit of s^-1; it is defined as the probability of decay of an individual nucleus per unit time.