Isolated AU (p < 0.001), isolated keratitis (p = 0.001), and intraocular pressure elevation (p = 0.013) were more likely to be concomitant to HZO active skin disease, while keratouveitis occurred more likely more than 1 month after HZO eruption (p < 0.001).
In the current study, isolated AU and isolated keratitis were more likely to be concomitant to HZO eruption (p < 0.001 and p = 0.001, respectively); however, keratouveitis is more likely to occur at least 1 month after HZO (p < 0.001).
Canine eruption led to more loss of appetite than incisor (p = 0.033) or molars eruption (p = 0.014).
Low serum selenium concentration was significantly associated with primary skin disease of HIV/AIDS, such as pruritic papular eruption of AIDS (P = 0.003), xeroderma (P = 0.030), fluffy hair (P = 0.021), blue-black nail hyperpigmentation (P = 0.033) and secondary skin disease, such as oral candidiasis (P = 0.002).
Serum levels of HGF were inversely proportional to grades of both acneiform eruption (grade 0/1 3, P = 0.012) and paronychia (grade 0/1 3, P = 0.005; grades 0 1/2 3, P = 0.039).
Serum levels of AREG tended to be inversely proportional to grades of acneiform eruption (grades 1 2/2 3, P = 0.039; grades 0 2/3, P = 0.026).
Using a simplified formalism the probability of eruption is given by P ( eruption ) = P ( unrest ) × P ( magma — unrest ) × P ( eruption — magma, unrest ) (1) Figure 1 Schematic representation of the BET_EF model's settings (Marzocchi et al.2008).2008
There was a significant difference in distribution of the grade of skin toxicities between acneiform eruption and paronychia (P = 0.021), as shown in Table S2.
For a given eruption scenario, the probability P M at coordinates x,y is calculated based on the number of times a given threshold of accumulation is reached and divided by the total number of runs N R : P_{M} x,y) = frac{sum_{i=1}^{N_{R}}n_{i}}{N_{R}} n_{i} = left{ begin{array}{l l} 1 & quad text{if (M_{i} x,y) geq) threshold (mid) eruption} 0 & quad text{otherwise.} end{array} right.
Between VEI or eruption magnitude categories of I p and I q (I p < I q ), the mean ratio of the global eruption frequency to the Japanese eruption frequency, r g, is: {r}_g = frac{1}{I_q-{I}_p}{displaystyle underset{I_p}{overset{I_q}{int }}}frac{10^{a_g-{b}_gI}}{10^{a_j-{b}_jI}}dI (20).
The difference between body temperature on the days before (36.54 ± 0.40 °C) and after eruption (36.53 ± 0.39 °C) was not significant (p = 0.601).
