Shear wave (SW) imaging is an ultrasound elastogrpahy technique for estimating the elastic properties of biological tissues. Increasing the frequency would improve both the confinement of the radiation force generating the shear wave, and the imaging spatial resolution. The objectives of the study were to realize a simple high frequency (HF) system for the generation and detection of SW propagation and to implement this system to develop and characterize tissue-mimicking gelatin phantoms (TMGP) for HF SWI with elastic properties in the range of those encountered in biological tissue. A 5 MHz and 10 MHz focused transducer were used to induced SW’s in TMGP ranging from 4% to 12% gelatin with 3% silica for scattering and a 25 MHz single-element focused transducer recorded pulse-echo signals in order to capture the SW. The shear wave speeds in the TMGP were found to range linearly from 1.59-4.59 m/s in the 4% to 12% gelatin samples.

The characteristics of crystallized fats depend on their solid fraction (SF) and fractal structures, which are affected by shear during crystallization. Binary mixtures of trilaurin (LLL) and trimyristin (MMM) diluted in triolein were used as samples. Pure diluted LLL and MMM were also studied. Samples were examined at different crystallization temperatures either statically or at shear rates of 800, 80, and 8 1/s. The sample cell combined a rheometer with a nuclear magnetic resonance (NMR) device to measure SF value and apparent viscosity. The measurements were compared to equations that describe the dependency of viscosity on solid volume fraction, to understand the effect of crystallites orientation at higher shear rates. Phase transitions during crystallization were observed by time-resolved synchrotron X-ray diffraction under similar conditions. Shear induced a strong reduction in phase onset and transition time and variations in phase distributions and the crystal size.

In this thesis we will investigate the role of diapycnal mixing on the ocean general circulation. This thesis is divided into three main parts. In the first part we show that there exists an almost infinite number of pathways to turbulence in oceanic energetic shear zones at high Reynolds number. Such a large number of accessible routes to truly chaotic motion is not typical of most of the existing body of laboratory and numerical experiments of shear-induced diapycnal mixing, but is shown to be of relevance to diapycnal mixing in geophysical flows. A key finding is that the use of generally accepted empirical relations based on laboratory experiments for the quantification of diapycnal mixing leads to large inaccuracies. In the second part we perform high resolution numerical experiments of diapycnal mixing in the oceanographically relevant high Reynolds number parameter range. Through detailed analysis of the flow energetics and mixing properties of these flows, we show that the net buoyancy flux facilitated by turbulence, the efficiency of diapycnal mixing, and the resultant effective diffusivity, all depend in non-trivial ways on the specific route to turbulence for each individual mixing event. This has important implications for practical methods of estimating an effective diapycnal mixing diffusivity from observations as well as for parametrization of mixing in ocean general circulation models. We show quantitatively that such methods can be inaccurate to the extent that they will need to be completely revised or replaced. In the third and final part of the thesis we investigate the sensitivity of the meridional overturning circulation of the abyssal ocean to the intensity and spatial variations of diapycnal mixing. We show that changes in intensity of mixing by factors well within the errors associated with practical estimates (as discussed above) lead to significant changes in ocean circulation. We show that enhanced abyssal mixing, surface winds, and meso-scale eddies play leading roles in driving the abyssal ocean circulation and in setting the stratification. As an example of the application of our analysis we show that proper parametrization of enhanced abyssal mixing leads to realization of the important role of the (often neglected) geothermal heat flux in driving the Antarctic Bottom Water circulation.

No description available.

The vascular endothelium is a single layer of cells that lines the interior surface of our blood vessels. The endothelium plays a key role in vasoprotection and vasoregulation and its proper function is therefore essential to the maintenance of vascular health. The endothelial cells respond to the frictional force (shear stress (SS)) that occurs with an increase in blood flow. As a response, vasoactive substances are released, causing the artery to dilate, this is termed flow-mediated dilation (FMD). Endothelial cell function can be assessed by measuring the vasodilatory response to an increase in SS. Currently however, our ability to interpret the results of FMD assessment in order to make accurate judgements regarding arterial health is hindered by an incomplete understanding of the “dose-response” relationship between SS and FMD. The dose-response relationship is characterized by 1) the SS stimulus required to elicit an FMD response (threshold), 2) the magnitude of dilation for a given increase in SS (the slope of the SS-FMD relationship), and 3) the point at which further increases in SS no longer elicit dilation (the ceiling). The primary purpose of the current study was to characterize the magnitude and day-to-day variability of the parameters described above. N=20 males (mean 22-years). Brachial artery diameter (BAD) and blood velocity (BV) were assessed with echo and Doppler ultrasound. SS was estimated as shear rate (SR=BV/BAD). Subjects performed 2 incremental handgrip exercise trials on two separate visits (V1 and V2). CV=co-efficient of variation. The SS-FMD relationship was characterized by a shallow slope followed by an inflection point (threshold (T1)) and a steeper slope (pre vs. post T1 slope p=0.002). There was no difference between V1 vs. V2 in the SR-FMD slope or threshold (p>0.05), but there was considerable within-subject variability in the SR-FMD parameters: pre-T1 slope CV = 47.0 ± 33.1%; post-T1 slope CV = 55.3 ± 40.7%; T1 CV = 25.6 ± 6.3%. In conclusion, %FMD did not plateau with increasing SR, therefore no ceiling was identified. The inflection in slope may indicate the involvement of different or additional vasodilator mechanisms post-threshold. / Thesis (Master, Kinesiology & Health Studies) -- Queen's University, 2011-09-15 20:17:11.582

Few studies have compared cortisol responses to psychological and physical stress tasks with or without social evaluation. Flow-mediated dilation (FMD) with reactive hyperemia is impaired following acute stress though less is known regarding the impact of stress and cortisol on FMD with exercise induced increases in shear stress (EX-FMD). The purpose of this study was 1) to compare cortisol responses between the Trier Social Stress Test (TSST) and 5min cold pressor test with and without social evaluation (CPT, CPT+SE) and 2) to examine the impact of these stressors and cortisol elevation on EX-FMD. 59 healthy male subjects were randomly assigned to one of three conditions: TSST, CPT, or CPT+SE. Brachial artery EX-FMD was assessed before, 15 and 35min post-stress with Echo and Doppler ultrasound. Results are mean ± SD. Baseline parameters did not differ between conditions (p>.05) and stress responses were similar between the three conditions for peak cortisol: TSST 11.34±5.53nmol/L; CPT 10.08±4.48nmol/L; CPT+SE 8.51±3.60nmol/L; condition effect p=.292; cortisol responders only (increase >2nmol/L) TSST 12.48±5.24nmol/L; CPT 12.13±5.31nmol/L; CPT+SE 10.70±2.86nmol/L; condition effect p=.560; peak MAP: 131.99 ±18.56mmHg, condition effect p=.664; peak TPR: 25.84 ± 9.78mmHg/L/min, condition effect p=0.841; peak stress rating out of 10: 5.11 ± 2.12, condition effect p= 0.292; with the exception of HR (TSST: 95.06 ± 15.29bpm; CPT: 79.00 ± 11.85bpm; CPT+SE: 77.98 ± 7.66bpm; condition effect p= 0.003) and pain ratings out of 10 (TSST: 1.21 ± 1.72; CPT: 6.66 ± 1.42; CPT+SE: 6.38 ± 1.73; condition effect p<.001). Shear stress was lower in the 15min post-stress vs. pre stress and 35min post-stress trials (72.34 ± 4.46; 15min post-stress: 70.79 ± 5.39; 35min post-stress: 70.60 ± 6.10; condition effect p= 0.592; trial effect: p= 0.018). EX-FMD increased from pre- stress to 15min post-stress in all conditions (pre-stress 6.22 ± 2.75%; 15min-post stress: 7.91 ± 3.24%; 35min post-stress: 6.60 ± 2.93%; trial effect p<.001). No correlation between change in EX-FMD and change in cortisol was detected (r2= 0.0125; p=.404). In conclusion, the TSST, CPT and CPT+SE elicited similar stress responses and stress transiently enhanced EX-FMD. Cortisol responses did not explain the enhanced EX-FMD post stress. / Thesis (Master, Kinesiology & Health Studies) -- Queen's University, 2012-09-14 15:41:33.325

No description available.

No description available.

No description available.

Timber beams with end splits were investigated in this study to determine their shear strength. Two conditions were considered: a) Group 1 had supports located near the ends with the portion of the beam extending beyond the support, and b) Group 2 had supports located right at the end of the beam subjected to a horizontal split at approximately mid height. In Group 1, seventeen beams were tested under static loading and four were tested in fatigue. In Group 2, nineteen beams were tested under static loading and four under fatigue. In Group 1, eight beams under static loading failed in shear. In Group 2, all beams under static loading failed in shear. Group 1 and Group 2 beams under static load produced average shear strength values of 4.93 MPa and 4.49 MPa, respectively. During fatigue tests, Group 1 sustained more cycles than beams in Group 2.