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Hydraulic effects are frequently the result of inflows and outflows of water.
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Although operating at such high rates to mimic cell swimming velocities may result in the cantilevers being subject to hydraulic dampening, we maintained consistent experimental conditions (including solution viscosity) throughout the experiments, thus any potential hydraulic dampening effects are consistent across the three surfaces investigated here.
While k values may change spatially with river hydraulic conditions, these effects are currently not included in the model.
Smooth and realistic hydraulic profiles along drains are obtained while backwater effects are clearly represented.
The effect of the hydraulic force is illustrated in a physical model (Fig. 1 and Supplemental Video S1), and the hydraulic force magnitude was found to be an important component of the total force responsible for left ventricular filling.
These effects are not similar for all numbers of hydraulic fractures and all fracture lengths and heights.
These hydrodynamic effects are important issues and should be addressed during the design of hydraulic machines.
This result was also found in the field-based modeling results, but the radius of hydraulic and thermal effects was larger.
For the purposes of understanding the effects of hydraulic forces upon LV diastolic filling, only the longitudinal component of the hydraulic force is relevant (FAL and FVL in Fig. 4).
The hydraulic fracturing effect is most sensitive to horizontal principal stress difference, followed by the angle between perforated well casing and laminae.
After directional hydraulic fracturing was put into effect, no dynamic effects were encountered, which indicated that directional hydraulic fracturing of the main roof can reduce the local stress and greatly diminish dynamic load.
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