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When the hydrophobic character increases, a more significant dehydration of OEGMA side chains leads to a strengthening of polymer chain interactions, resulting in the formation of nanosized and phase-segregated particles.
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It is noted that these fault rocks contain more abundant clays than the intact and/or weakly deformed basalts, and the amount/rate of dehydration described above will be more significant along the faults.
Patient-related risks include, but are not limited to, age, hormonal therapy, dehydration, active cancer, obesity, one or more significant medical comorbidities, varicose veins, superficial VTE, and known thrombophilias [ 20, 21].
Moderate diarrhoea was defined as more than 4 unformed stools and severe diarrhoea as more than 6 unformed stools in a 24 hour period or evidence of significant dehydration.
More significant.
There are more significant challenges.
Of 113 patients, 10.6% had significant dehydration.
A weight change of ≥5% was considered clinically significant dehydration.
The ultrasound-measured IVC/Ao ratio is a modest predictor of significant dehydration in children.
Significant dehydration was defined as moderate (5 to 10%) and severe (>10%) dehydration combined as previously described in the literature [5],[5]],[5]],[5]].
It is the cold subduction that leads to the insignificant dehydration at the shallow depths but the significant dehydration and anatexis at the subarc depths >80 km.
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