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Dispersion of Particle‐Reactive Elements Caused by the Phase Transitions in Scavenging
Author(s) -
Maderich V.,
Kim K. O.,
Brovchenko I.,
Jung K. T.,
Kivva S.,
Kovalets K.
Publication year - 2022
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1029/2022jc019108
Subject(s) - scavenging , thermal diffusivity , diffusion , thermodynamics , sorption , particulates , desorption , dispersion (optics) , particle (ecology) , chemistry , phase (matter) , analytical chemistry (journal) , atomic physics , physics , quantum mechanics , chromatography , geology , biochemistry , oceanography , organic chemistry , adsorption , antioxidant
A generalized model of scavenging of the reactive radionuclide 239,240 Pu was developed, in which the sorption‐desorption processes of oxidized and reduced forms on multifraction suspended particulate matter are described by first‐order kinetics. One‐dimensional transport‐diffusion‐reaction equations were solved analytically and numerically. In the idealized case of instantaneous release of 239,240 Pu on the ocean surface, the profile of concentrations asymptotically tends to the symmetric spreading bulge in the form of a Gaussian moving downward with constant velocity. The corresponding diffusion coefficient is the sum of the physical diffusivity and the apparent diffusivity caused by the reversible phase transitions between the dissolved and particulate states. Using the method of moments, we analytically obtained formulas for both the velocity of the center mass and apparent diffusivity. It was found that in ocean waters that have oxygen present at great depths, we can consider in the first approximation a simplified problem for a mixture of forms with a single effective distribution coefficient, as opposed to considering the complete problem. This conclusion was confirmed by the modeling results for the well‐ventilated Eastern Mediterranean. In agreement with the measurements, the calculations demonstrate the presence of a maximum that is slowly descending for all forms of concentration. The ratio of the reduced form to the oxidized form was approximately 0.22–0.24. At the same time, 239,240 Pu scavenging calculations for the anoxic Black Sea deep water reproduced the transition from the oxidized to reduced form of 239,240 Pu with depth in accordance with the measurement data.