Table 1 shows the relative difference in drain current values in terms of the average root mean square (RMS) errors (absolute and normalized) between the simulated and measured data when the glucose is varied from 2 to 50 mM.
Before SiN passivation, there was a significant difference in drain current between quiescent points (V gs, V ds) of (0, 0) and (−3, 0), and the difference was further increased when the quiescent point (V gs, V ds) was set to (0, 10) and (−3, 10), respectively.
A 25percentnt difference in drain volume between treated and untreated wounds was considered clinically important.
An a priori sample size calculation with a difference in drain output of 300 (SD 350) mL between knees being considered to be a clinically relevant difference revealed that 22 knees in each group would be needed to show significance.
The difference in the drain current (i.e., on/off current ratio) can be measured in the range of memory window after programming and erasing processes [31 34].
The BioFET signal is defined as the difference in the drain current between a surface with hybridization and a surface without hybridization.
But our study showed no differences between the 3 groups in terms of estimated blood loss and drain output in the first 24 hours after surgery, a finding which is comparable to a study by Ezequiel et al. [ 16] which also found no significant difference in postoperative drain output between their placebo and ketorolac groups.
Although sediment delivery and hydrologic response from MTM operations remain highly variable and poorly resolved, the inherent close coupling between hillslopes and headwater channels is expected to result in geomorphic differences in stream channels draining MTM landscapes relative to unmined landscapes.
No statistically significant differences were found in drained volumes, nor in Na and Ca losses through drainage, between both treatments in each of the three growing seasons (Gossypium hirsutum L. in 2003 and 2005; Beta vulgaris L. in 2003 2004).
This variation may be caused by differences in the terrestrial systems they drain (for example, varying forest age or composition, hydrology, soil organic matter content, and so on) and/or by differences between the streams themselves (for example, contrasting geomorphology, biotic nitrogen [N] demand, rates of instream nitrogen transformations).
