Viscous Flow and Fluid Dynamics

Exam questions and solutions for a third year maths course. Diagrams for the questions are all together in the support.zip file, as .eps files

Comparación de la anestesia espinal con anestesia general endovenosa para legrado uterino obstétrico

Introducción: La elección de la técnica anestésica para cualquier procedimiento quirúrgico debe estar basada en su seguridad, la rapidez para su aplicación, la recuperación óptima para el paciente y minimización de los efectos secundarios, la anestesia raquídea es una técnica anestésica que puede ser utilizada con buenos resultados clínicos y minimas complicaciones . Materiales y métodos: Se realizó un estudio observacional con recolección prospectiva en mujeres clasificadas como ASA I - II y que posteriormente fueron llevadas a la realización de legrado uterino obstétrico por embarazo no viable durante las primeras 12 semanas de gestación, las técnicas anestésicas fueron anestesia espinal o anestesia general endovenosa dependiendo de la elección hecha por el anestesiólogo previo al procedimiento. Se midieron variables hemodinámicas, control del dolor postoperatorio, tiempo de recuperación y complicaciones perioperatorias con el fin de determinar si se presentaban diferencias significativas entre estas dos técnicas anestésicas. Resultados: Se incluyeron un total de 110 pacientes, 63.6% (n=70) con anestesia general y 36.4% (n40) con anestesia espinal. Ambas poblaciones fueron comparables. Se presentaron menos efectos secundarios con la técnica espinal, hay una diferencia estadísticamente significativa en cuanto al dolor a favor de la anestesia espinal (p0,000) Discusión: La anestesia raquídea es una opción viable, sencilla , fácil y eficaz para la realización de legrados obstétricos, se puede realizar con monitorización básica y las complicaciones son mínimas. Se requieren estudios más amplios para determinar el papel de cual es la mejor técnica. Palabras claves: legrado uterino instrumentado, anestesia espinal, anestesia general endovenosa

Interpreting students??? perceptions in fluid mechanics learning outcomes

Resumen basado en el de la publicaci??n

Estudi citològic i bioquímic del fluid epididimari de "Sus domesticus"

En aquest estudi s'ha determinat que al augmentar el ritme d'extraccions de semen es produeixen canvis en el patró d'absorció i secreció del fluid epididimari, que provoquen alteracions en la maduració epididimaria dels espermatozoides i un desenvolupament anòmal de la motilitat espermàtica. La concentració de glutamat i carnitina al fluid epididimari augmenten al llarg del conducte epididimari, alhora que la concentració de myo-inositol disminueix. El contingut de myo-inositol a l'interior dels espermatozoides disminueix, mentre que el contingut de glutamat augmenta a partir del caput distal i el contingut de carnitina no varia al llarg del conducte. S'ha determinat la presència de la ruta del poliol a l'epidídim de porcí. Els resultats obtinguts indiquen que la glucosa difon de la sang cap al fluid epididimari, és convertida a sorbitol per l'aldosa reductasa, i aquest sorbitol s'acumula al fluid luminal i és convertit a fructosa per l'acció de la sorbitol deshidrogenasa.

Velocity discrimination of angular motion at different frequencies in individuals with normal vestibular function

The purpose of this study was to evaluate discrimination of angular velocity in individuals with normal vestibular function using a newly developed adaptive psychophysical measure. Vestibular psychophysical testing may complement existing clinical measures in diagnosing and treating patients with imbalance.

General relationships between pressure, weight, and mass of a hydrostatic fluid

In curved geometries the hydrostatic pressure in a fluid does not equal the weight per unit area of the fluid above it. General weight–pressure and mass–pressure relationships for hydrostatic fluids in any geometry are derived. As an example of the mass–pressure relationship, we find a geometric reduction in surface pressure as large as 5 mbar on Earth and 39 mbar on Titan. We also present a thermodynamic interpretation of the geometric correction which, as a corollary, provides an independent proof of the hydrostatic relationship for general geometries.

Characteristics of Langmuir Turbulence in the Ocean Mixed Layer

This study uses large-eddy simulation (LES) to investigate the characteristics of Langmuir turbulence through the turbulent kinetic energy (TKE) budget. Based on an analysis of the TKE budget a velocity scale for Langmuir turbulence is proposed. The velocity scale depends on both the friction velocity and the surface Stokes drift associated with the wave field. The scaling leads to unique profiles of nondimensional dissipation rate and velocity component variances when the Stokes drift of the wave field is sufficiently large compared to the surface friction velocity. The existence of such a scaling shows that Langmuir turbulence can be considered as a turbulence regime in its own right, rather than a modification of shear-driven turbulence. Comparisons are made between the LES results and observations, but the lack of information concerning the wave field means these are mainly restricted to comparing profile shapes. The shapes of the LES profiles are consistent with observed profiles. The dissipation length scale for Langmuir turbulence is found to be similar to the dissipation length scale in the shear-driven boundary layer. Beyond this it is not possible to test the proposed scaling directly using available data. Entrainment at the base of the mixed layer is shown to be significantly enhanced over that due to normal shear turbulence.

Diagnostic analysis of atmospheric moisture and clear-sky radiative feedback in the Hadley Centre and Geophysical Fluid Dynamics Laboratory (GFDL) climate models

The interannual variability of the hydrological cycle is diagnosed from the Hadley Centre and Geophysical Fluid Dynamics Laboratory (GFDL) climate models, both of which are forced by observed sea surface temperatures. The models produce a similar sensitivity of clear-sky outgoing longwave radiation to surface temperature of ∼2 W m−2 K−1, indicating a consistent and positive clear-sky radiative feedback. However, differences between changes in the temperature lapse-rate and the height dependence of moisture fluctuations suggest that contrasting mechanisms bring about this result. The GFDL model appears to give a weaker water vapor feedback (i.e., changes in specific humidity). This is counteracted by a smaller upper tropospheric temperature response to surface warming, which implies a compensating positive lapse-rate feedback.

Velocities of compressional and shear waves in limestones

Carbonate rocks are important hydrocarbon reservoir rocks with complex textures and petrophysical properties (porosity and permeability) mainly resulting from various diagenetic processes (compaction, dissolution, precipitation, cementation, etc.). These complexities make prediction of reservoir characteristics (e.g. porosity and permeability) from their seismic properties very difficult. To explore the relationship between the seismic, petrophysical and geological properties, ultrasonic compressional- and shear-wave velocity measurements were made under a simulated in situ condition of pressure (50 MPa hydrostatic effective pressure) at frequencies of approximately 0.85 MHz and 0.7 MHz, respectively, using a pulse-echo method. The measurements were made both in vacuum-dry and fully saturated conditions in oolitic limestones of the Great Oolite Formation of southern England. Some of the rocks were fully saturated with oil. The acoustic measurements were supplemented by porosity and permeability measurements, petrological and pore geometry studies of resin-impregnated polished thin sections, X-ray diffraction analyses and scanning electron microscope studies to investigate submicroscopic textures and micropores. It is shown that the compressional- and shear-wave velocities (V-p and V-s, respectively) decrease with increasing porosity and that V-p decreases approximately twice as fast as V-s. The systematic differences in pore structures (e.g. the aspect ratio) of the limestones produce large residuals in the velocity versus porosity relationship. It is demonstrated that the velocity versus porosity relationship can be improved by removing the pore-structure-dependent variations from the residuals. The introduction of water into the pore space decreases the shear moduli of the rocks by about 2 GPa, suggesting that there exists a fluid/matrix interaction at grain contacts, which reduces the rigidity. The predicted Biot-Gassmann velocity values are greater than the measured velocity values due to the rock-fluid interaction. This is not accounted for in the Biot-Gassmann velocity models and velocity dispersion due to a local flow mechanism. The velocities predicted by the Raymer and time-average relationships overestimated the measured velocities even more than the Biot model.