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K<sub>d</sub>, the ratio of the concentrations of a radionuclide in two heterogenous phases (in this case, water and sediment) in equilibrium with each other.
([[ICRP Publication 114]], 2009)
'''Return to [[ICRP Glossary|Glossary]]'''
K<sub>d</sub>, the ratio of the concentrations of a radionuclide in two heterogenous phases (in this case, water and sediment) in equilibrium with each other.
([[ICRP Publication 114]], 2009)
'''Return to [[ICRP Glossary|Glossary]]'''