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A metallurgical model for particle coarsening below the dissolution temperature is considered.
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The dissolution temperature was varied in the range of 30 50 °C, while all other parameters were kept constant.
Seeded growth occurred at a maximum rate of 2.1 mm/day when the dissolution zone temperature was 535 °C and the growth zone temperature was 495 °C.
The results indicated that interaction time plays a more important role in promoting the dissolution of CRM whereas the interaction temperature is more responsible for the breaking of backbone of the main chain of rubber.
The caves were formed by the dissolution of limestone by water, a continuing process; their natural temperature is 54 °F (12 °C), with a relative humidity of a high 87 percent.
In practice, the temperature is kept at 5~10 °C to slow down the barrier layer dissolution.
Increasing NaOCl's temperature is accepted as an activation technique that increases the solution's dissolution effect, and increased anti-microbial activity and faster tissue dissolution have been reported by increasing the temperature of the NaOCl [ 11].
What's more, the formation and dissolution temperatures could be independently controlled by controlling the ratios of disordered and ordered segments in the biomaterial.
Due to the relatively minor differences observed in the rate and extent of dissolution at 140 °C, the temperature was reduced to 70 °C to determine if there were any significant differences observed in swelling and dissolution between the WT and LLHPL2.
In random ethylene propylene copolymers (EP), the incorporation of ethylene into the polypropylene chain reduces the crystallinity and therefore causes both the crystallization and the dissolution temperatures to be lower than the one in the PP homopolymer.
Changes in mineral dissolution as a function of temperature are accounted for by β i and ns,iin the y-intercept and in α i in the slope in addition to the saturation terms (Ω, KT,eq) and T in equation 19.
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