Repuesta al tratamiento súper ovulatorio, con folltropin V (Análogo sintético de la FSH), en hembras bovinas donantes, de las razas Pardo Suizo y Holsteins de la finca las mercedes de la Universidad Nacional Agraria, Managua

El presente trabajo investigativo se llevo a cabo en la finca Las Mercedes, propiedad de la Universidad Nacional Agraria ubicada en el Departamento de Managua, Nicaragua, en el Km 12.5 Carretera Norte. El objetivo del estudio fue determinar si hay influencia del factor raza en la repuesta súper ovulatoria en las hembras bovinas donantes de la> razas Holsteins y Pardo Suizo sometidas al tratamiento hormonal mediante la aplicación del Folltropin V (Análogo Sintético de la Hormona Foliculoestimulante FSH).El tamallo requerido de la muestra fue d 1 O hembras donantes para cada raza en estudio ;las cuales fueron previamente seleccionados según la calidad genética de cada hembra , la edad comprendida para la selección fue de entre 3 y 5 años además se realizaron exámenes clínicos y ginecológicos para determinar si cumplían con los requisitos o parámetros de salud para realizar esta técnica de mejoramiento productivo, los datos se obtuvieron mediante el conteo de cuerpos lúteos y folículos atravez de la palpación rectal de los ovarios ;el mismo dla en que realizo la recolecta de los embriones; los cuales fueron llevados al laboratorio para ser clasificados según su estado de desarrollo y calidad posteriormente fueron transferidos y congelados . Los resultados obtenidos atravez del análisis de la respuesta súper ovulatoria, indican que hay diferencia signicativa en cuanto al numero de cuerpos híteos en la raza Pardo Suizo ya que obtuvo un promedio de 9.2 cuerpo lúteos y la raza Holsteins obtuvo un promedio de 6.9 cuerpos lúteos . Por otra parte no hubo diferencia significativa en lo que respecta al número de embriones que tuvo un promedio de 3.8 cultivados en comparación con los 3. 7 embriones de la Raza Holsteins.

解不可压缩流体力学问题的降阶法——Ⅱ.空间V~h的基函数和误差估计

本文对于一大类数值求解二维Navier-Stokes方程边值问题的有限元格式给出了零散度空间V~h的一组简单基函数,讨论了速度的数值误差对压力的数值解的影响,并提出一个改进算法。

倒V电子沉降通量能谱的理论计算

沿极光区磁力线大约在2000公里到8000公里的高度范围内,存在着一个等离子体湍流和大尺度平行电场的加速区。沿磁力线运动的等离子体片中的电子通过此加速区时,受到等离子体湍流和平行电场的共同作用,形成电子沉降的倒V结构。从一维准线性的动力学方程出发,导出了沉降电子通量的能谱方程,得出了电子通量能谱的理论公式。对等离子体湍流和平行电场对沉降电子能谱的影响作了分析和讨论。本文所提出的理论可以解释目前观测到的某些基本现象。

Vortex dynamics in the studies of looping in tropical cyclone tracks

This paper proposes criteria for predicting the tendency of looping in tropical cyclone tracks using the approach of vortex dynamics. We model the asymmetric structure of a cyclone by a system of vortex patches. The evolution of such system of vortices is simulated by the method of contour dynamics. A new set of exact analytic formulas for contour dynamics calculations is derived, which is shown to be more computationally effective. Based on point-vortex models, we derive analytic formulas for the criteria of looping in a cyclone track. From numerical experiments, the simulated trajectories obtained from the point-vortex system and vortex patch system agree quite well. Hence, the looping criteria obtained from the point-vortex system can be applied by forecasters to stay alert for tendency of looping in a cyclone track. To demonstrate the applicability of the proposed criteria, the trajectory of Typhoon Yancy (9012), whose field data are available from ''TCM-90'', is simulated. The case study shows that the asymmetric structure similar to the pattern of a beta gyre is responsible for its recurvature when Yancy landed Fujian Province, China on 20 August 1990.

Periodic vortex breakdown in wide spherical gaps

The flow field with vortex breakdown in wide spherical gaps was studied numerically by a finite difference method under the axisymmetric condition. The result shows that the flow bifurcates to periodic motion as the Reynolds number or the eccentricity of the spheres increases. (C) 1997 American Institute of Physics.

Singular behaviour near the tip of a sharp V-notch in a power law hardening material

This paper presents an asymptotic analysis of the near-tip stress and strain fields of a sharp V-notch in a power law hardening material. First, the asymptotic solutions of the HRR type are obtained for the plane stress problem under symmetric loading. It is found that the angular distribution function of the radial stress sigma(r) presents rapid variation with the polar angle if the notch angle beta is smaller than a critical notch angle; otherwise, there is no such phenomena. Secondly, the asymptotic solutions are developed for antisymmetric loading in the cases of plane strain and plane stress. The accurate calculation results and the detailed comparisons are given as well. All results show that the singular exponent s is changeable for various combinations of loading condition and plane problem.

Two-time scales inner solutions and motion of a geostrophic vortex

Based on the authors' previous work, in this paper the systematical analyses on the motion and the inner solutions of a geostrophic vortex have been presented by means of thematched asymptotic expansion method with multiple time scales (S/gh001/2 and α S/gh001/2) and space scales. It has been shown that the leading inner solutions to the core structure in two-time scales analyses are identified with the results in normal one-time scale analyses. The time averages of the first-order solutions on short time variable τ are the same as the first-order solutions obtained in one normal time scale analyses. The geostrophic vortex induces an oscillatory motion in addition to moving with the background flow. The period, amplitude andthe deviation from the mean trajectory depend on the core structure and the initial conditions. The velocity of the motion of vortex center varies periodically and the time average of the velocity on short time variable τ is equal to the value of the local mean velocity.

The motion and the core structure of a geostrophic vortex - one-time scale inner solution and the motion of the vortex

By means of the matched asymptotic expansion method with one-time scale analysis we have shown that the inviscid geostrophic vortex solution represents our leading solution away from the vortex. Near the vortex there is a viscous core structure, with the length scale O(a). In the core the viscous stresses (or turbulent stresses) are important, the variations of the velocity and the equivalent height are finite and dependent of time. It also has been shown that the leading inner solutions of the core structure are the same for two different time scales of S/(ghoo)1/2 and S/a (ghoo)1/2. Within the accuracy of O(a) the velocity of a geostrophic vortex center is equal to the velocity of the local background flow, where the vortex is located, in the absence of the vortex. Some numerical examples demonstrate the contributions of these results.