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(b) P0, initial (explosion) pressure; P a, atmospheric pressure; m s, mass of solid material; m g, mass of gas; ρ a, the density of ambient air; ρ s, the density of solid material at source and r, the distance that solid material has reached, are used in the Fagents and Wilson (1993) model.
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Source/sink term (Kg/m3 s), mass source term (Kg/m3 s).
After recording swollen mass (M s), the gels were lyophilized and the dry masses were measured (M d) (n = 6).
Where q e (mg g− 1) is the adsorption capacity, C e (mM) is the equilibrium concentration in the aqueous phase, Ci (mM) is the initial aqueous phase concentration, V (L) is the volume of solution and M s (g) is the mass of solid adsorbent.
where M s is a generalized mass matrix and h s is a generalized force vector.
Hiroyasu and Kadota [39] developed a simple soot model to predict the production rate of soot mass ( dot; m s Open image in new window) using a single-step competition between the soot mass formation rate dot; m sf Open image in new window and the soot mass oxidation rate dot; m so Open image in new window according to dot; m s = dot; m sf − dot; m so Open image in new window.
The generalized mass matrix M s and the generalized force vector h s are given as.
All these cryogel sections used for determination of porosity were in triplicates and percent porosity was calculated as (2) % Porosity = M s − M d M s − M sub × 100, where M s is wet mass of the cryogel saturated with deionized water, M d is the dry mass of the cryogel, and Msub is the submerged mass of the cryogel.
The equilibrium swelling ratio was calculated from (1) Q = (M s − M d ) M d, where Q is equilibrium swelling ratio M s and M d are mass in swollen and dried states, respectively.
E_{text{s}} = left( {frac{{m_{text{o}} times C_{text{s}} }}{{m_{text{s}} }}} right) times 100% (2 where m s is the mass of extraction agent feed into HCE, m o and C s are the mass and extraction agent mass content of the light phase (Table 1).
We find no evidence for an exomoon around the planet and exclude moons of mass M S > 0.
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