Abstract
In-situ X-ray computed tomography (CT) was used to observe microstructure formations during freeze-drying of a dextrin solution. A specially designed freeze-drying stage was equipped at the X-ray CT stage. Frozen and dried microstructures were successfully observed. The CT images of the frozen solution clarified the ice crystal size increase and obvious boundary formation between the ice and freeze-concentrated phases upon performing post-freezing annealing at −5°C. These structural modifications emerged owing to Ostwald ripening and glassy phase relaxation. During the freeze-drying, pore microstructures formed as a consequence of water removal. The pores were replicas of the original ice microstructures; some pore microstructures newly formed by the removal of water. The latter mechanism was more obvious in the non-annealed sample than in the annealed sample. The glassy phase in the non-annealed solution was not perfectly freeze-concentrated; water was rapidly removed from this phase, losing its original microstructure. At this moment, the freeze-concentrated region piled up to new pore walls, which consequently thickened the pore walls. An image analysis estimated that the mean pore wall thicknesses for the non-annealed and annealed samples were 13.5 and 8.6 μm, respectively. It was suggested that the advantages of annealing are not only to reduce drying time owing to the modification of ice crystal morphologies but also to avoid quality loss related to the structural deformation of the glassy matters.
Highlights
Freeze-drying is known as one of the best drying methods in terms of preservation of product qualities
When an aqueous solution is subjected to freezing, an ice crystal phase coincidently forms with the freeze-concentrated phase
The freeze-drying performance of the employed system was evaluated by sublimating pure ice before loading on the X-ray computed tomography (CT) stage
Summary
Freeze-drying is known as one of the best drying methods in terms of preservation of product qualities. The glass transition temperature of the maximally freezeconcentrated glassy phase is commonly denoted as T’g. This temperature is crucial in the operation of a freeze-drying run. Annealing over Tg reduces the fraction of amorphous phase, achieving completion of the freeze-concentration and leading to a reduction in the water content This phenomenon is known as glassy state relaxation, where the state behavior is governed by the mobility of the matrix plasticized by water. Ice crystals coexisting with the glassy phase can recrystallize above T’g to minimize the interphase surface area, leading to ripening of ice crystals This phenomenon is referred to as Ostwald ripening (Kurz and Fisher, 1986; Ratke and Voorhees, 2013), which modifies ice microstructures in terms of size and uniformity (Searles et al, 2001)
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