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The contribution of fluid entrapment to the SIFs is investigated through an extensive parametric analysis.
Investigation of intracrustal faults is important not only to understand their relationships with intracrustal earthquakes (e.g., Yadav et al. 2013) but also the contribution of fluid interactions between the mantle and crust in generating earthquakes (e.g., Sano et al. 2014).
Specifically, we consider (1) the contribution of fluid flow in response to coseismic pressure changes in the lithosphere to the postseismic deformation and (2) the role of fluids rising from the subducting slab in the volcanic arc of NE Japan in producing localized weakening of the lower crust.
The contribution of fluid management and diastolic dysfunction to elevation of BNP was also evaluated.
Beside these possible causes, we wanted to assess the contribution of fluid used for irrigation in the SMILE procedure.
Differences in the contribution of fluid types to TFI were observed between the two age groups, which have been reported by others [ 10, 18].
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When we also considered a contribution of fluids derived from MH dissociation, we obtained the following contribution ratios in the seepage fluid ('Freshwater derived from CMD' section): about 4% fluid derived from CMD, about 5% fluid derived from MH dissociation, 20%to50%0% SPF of the accretionary prism, and more than 40% SW (Figure 6; Source B).
Phase angle reflects the relative contributions of fluid (resistance) and cellular membranes (capacitance) of the human body.
Phase angle reflects the relative contributions of fluid (resistance) and cellular membranes (reactance) of the human body.
Phase angle reflects the relative contributions of fluid (R) and cellular membranes (Xc) and is positively associated with capacitance and negatively with resistance [ 11].
Likewise, the presence of a nominal amount of gastroduodenal proteins in pancreatic fluid is to be expected, but the contribution of this fluid is minimized by fluid aspiration in the duodenum before ePFT.
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