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The volume percentage of silicate component in Iapetus is substantially below 60%.
b Evolution of NBO/T of the silicate component in the fluid as a function of temperature.
These two methods provide indirect evidence that the silicate component is mainly incorporated in the PS rather than PIB domains.
In our modeling, we will have six parameters: Asi, αsi, ab,si for the silicate component, and Ac, αc, ab,c for the graphite component.
Dynamic mechanical analyses (DMA) of these hybrid materials suggest that the silicate component preferentially incorporates within the sulfonated polystyrene (PS) domains.
If we do not fix the total silicate (Vtot,si) and graphite volume (Vtot,c), instead, we allow the quantity of the silicate component to vary with respect to that of graphite: by taking the silicate-to-graphite mass ratio to be mgra/msil = 0.4, 0.5, and 0.6, our model results show that AVtoward the GC is in the range of ~ 35 45 mag.
Similar(52)
Silicate components and their species exist in coexisting silicate melts and C O H N fluid.
Where Si4+ is a proxy for silicate components and Si(OH 3+ a proxy for hydroxylated silicate.
Their results reveal that the crystalline silicate components of cold dust in the outer regions of protoplanetary disks and debris disks are hidden in the amorphous silicate components.
These complex relations likely reflect several effects on the solubility of H2O of individual silicate components.
Silicate components dissolved into the fluids were ignored in the present calculations for estimating fluid densities.
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