An increase of surface loading from rain and snow may trigger pore fluid diffusion that increases pressure in fluid-filled cracks and consequently reduces seismic velocity (Mordret et al. 2016).
Even a small rise in pressure may trigger the fluid particles near the wall to stop and turn back to form a recirculating flow region, which is the characteristic of the separated flows.
Various geophysical and geochemical studies suggest that within the mantle wedge and crust in subduction zones, fluid fluxes may trigger seismicity and magmatism throughout the system (e.g., Iwamori 2007; Hasegawa et al. 2008).
Fluid overload may trigger a vicious cycle leading to further kidney and venous congestion (especially in patients with sepsis and capillary leak with secondary IAH) as shown in (Fig. 8) and should be avoided [87].
Obviously, the risk at this phase is to be too aggressive with fluid removal and to induce hypovolemia, which may trigger a "fourth hit" for hemodynamic deterioration and hypoperfusion (Fig. 5).
These fluid pressure oscillations may provide nutrition and may trigger the cartilage cells to initiate tissue repair (re-differentiation of the diseased chondrocytes).
It is also well established that renal and cardiac function are closely related to fluid control and maladjustment in one of the organs may trigger an alteration in the other [ 46].
These questions may trigger further research into the role of lactate and lactate-based intravenous fluids in resuscitation of the critically ill.
Carbon nanotube catalyst residues may trigger similar metal-mediated toxicity, but only if the metal is bioavailable and not fully encapsulated within fluid-protective carbon shells.
Lack of employment opportunities may trigger violence and juvenile delinquency.
