Effect of combined care nursing on patient satisfaction, staff satisfaction, and quality of care /

This research evaluates the effect of combined care nursing on three outcomes: i) patient satisfaction; ii) staff satisfaction; and iii) quality of care. Oakville-Trafalgar Memorial Hospital was in the early planning stages of changing to combined care nursing from the traditional method of providing separate postpartum and nursery care to mothers and babies. The opportunity existed to evaluate formally the change to combined care. There were three hypotheses to be investigated. Data were collected from four sources: patient surveys, staff surveys, informal interviews, and internal hospital documents. Both quantitative and qualitative data were analyzed. The surveys were administered on three different occasions to patients and staff. Other sources of data included informal interviews with patients and staff who responded to the surveys, and chart audits.The study findings revealed that the majority of respondents had increased levels of satisfaction and perceptions of increased quality of care following implementation of combined care. These findings, related to combined care and the role of change in its implementation and evaluation, indicate that there are no right or easy answers about how to make new ideas become reality in a smooth, pleasant way.

Genesis and distribution of Mississippi Valley-type ore assemblages in Middle Silurian strata, Niagara Peninsula, Ontario /

Presently non-commercial occurrences of Mississippi Valley-type ore assemblages in the Middle Silurian strata of the Niagara Peninsula have been studied. Based on this detailed study, a new poly-stage genetic model is proposed which relates ore mineralization in carbonate environments to the evolution of the sedimentary basin. Sulphide ore mineralization occurred during two episodes: 1. During the late diagenesis stage, which is characterized by compaction-maturation of the sediments, the initial mineralization took place by upward and outward movement of connate waters. Metals were probably supplied from all the sediments regardless of their specific lithologies. However, clay minerals were possibly the main contributors. The possible source of sulphur was from petroleum-type hydrocarbons presently mixed with the sediments at the site of ore deposition. Evidence for this is the fact that the greatest abundance of ore minerals is in petroliferous carbonates. The hydrocarbons probably represent liquids remaining after upward migration to the overlying Guelph-Salina reservoirs. The majority of sphalerite and galena formed during this period, as well as accessory pyrite, marcasite, chalcopyrite, chalcocite, arsenopyrite, and pyrrhotite; and secondary dolomite, calcite, celestite, and gypsum. 2. During the presently ongoing surface erosion and weathering phase, which is marked by the downward movement of groundwater, preexisting sulphides were probably remobilized, and trace amounts of lead and zinc were leached from the host material, by groundwaters. Metal sulphides precipitated at, or below, the water table, or where atmospheric oxygen could raise the Eh of groundwaters to the point where soluble metal complexes are unstable and native sulphur co-precipitates with sphalerite and galena. This process, which can be observed today, also results in the transport and deposition of the host rock material. Breakdown of pre-existing sulphide and sulphate, as well as hydrocarbon present in the host rock, provided sulphur necessary for sulphide precipitation. The galena and sphalerite are accompanied by dolomite, calcite, gypsum, anglesite, native sulphur and possibly zincite.

Consumo voluntario de alimento y comportamiento productivo de cerdas lactantes de acuerdo al nivel de alimentación durante la gestación

Tesis (Maestría en Ciencias en Producción Animal) UANL

Oscilaciones electromecánicas en sistemas de potencia

Tesis (Maestría en Ciencias en Ingeniería Eléctrica con Especialidad en Potencia) UANL

Evsebii Pamphili episcopi Caesariensis Opera, in duos diuisa tomos,omnia, que hactenus inueniri potuerunt, nuc denuo ex uetustiss. Grecisexemplaribus, aucta & correcta in ordinemq redacta. In hac editione accessit Panegyricus de laudibus Constantini Magni, Imp. Augusti, continens multa quae apud alios historicos uix inueniuntur

UANL

Aprecio y estima de la divina gracia que nos merecio el hijo de Dios con su preciosa sangre, y passion repartido en cinco libros

UANL

Tesoros de Cornelio a. Lapide : extracto de los comentarios de este célebre autor sobre la Sagrada Escritura

UANL

Comentaria in scripturam sacram

UANL

María : praedicatoris necnon confessarii aurifodina

UANL

Catenam auream complectens, ex fententiis sanctorum patrum, miro artificio connexam, quorum catalogum & chronologiam, veria pagina ostendit

UANL

Dynamique végétale récente du complexe tourbeux des Tourbières-de-Lanoraie (Québec).

Les milieux humides sont parmi les écosystèmes les plus menacés de la planète que ce soit par le drainage, l’exploitation des ressources naturelles ou les changements climatiques. Dans une optique de conservation, il est primordial de comprendre la part des facteurs autogènes et allogènes dans la dynamique temporelle de ces écosystèmes. Dans ce contexte, les objectifs de cette étude étaient de : 1) reconstituer la dynamique des communautés végétales de deux secteurs ombrotrophes du complexe de milieux humides des Tourbières-de-Lanoraie au cours des trois derniers millénaires et 2) déterminer l’impact des activités humaines depuis les 500 dernières années sur cette dynamique. Pour ce faire, une approche paléoécologique pluridisciplinaire a été utilisée. La dynamique végétale a été semblable dans les deux secteurs étudiés. Elle a d’abord été caractérisée par une ombrotrophication des systèmes tourbeux puis par une transformation graduelle d’une tourbière ombrotrophe ouverte, dominées par les sphaignes et les éricacées, vers des tourbières ombrotrophes forestières. L’ombrotrophication se serait amorcée peu avant le Petit-Âge glaciaire (1570-1850 AD), période associée à des conditions plus fraiches et plus sèches. Le développement de la phase forestière serait beaucoup plus récent (début 1900) et semble être associé à une période d’intensification de l’empreinte anthropique dans le paysage, notamment du drainage. Ce travail montre que les perturbations anthropiques constituent depuis le début du XXème siècle le moteur principal de la dynamique de la végétation des deux secteurs étudiés.

Inversion comique ou critique satirique ? La vue du Capitole de Hieronymus Cock (1562)

Hieronymus Cock's view of the Capitoline Hill, published in 1562 series on Roman ruins, has long been considered a useful document by historians of art and architecture for the key historical and topographical information it contains on one of Rome's most celebrated sites during the Renaissance. Beyond its documentary nature, which, as will appear, was essentially rhetorical, the view also offers much information as to how a mid sixteenth-century Flemish artist might perceive Rome's illustrious topography and celebrated ancient statuary. In other words, Cock's engraving enables us to put into practice what may be called an "archaeology of the gaze". Through previously unnoticed details, Cock invents a comical - verging on the satirical - vision of the antique sculptures proudly displayed on the famous piazza. Such an ironical reversal of Italian classical dignity is typical of the attitude of some contemporary Flemish artists, such as Pieter Brueghel, who was then close to Cock, and exposes the ambivalent position of some Northern European artists towards the classical tradition and Italian art theory. Finally, the analysis of other engravings of ruins by Hieronymus Cock where two emblematic characters - the draftsman and the 'kakker' (the one who defecates) - appear side by side, sheds light on the origin and possible significance of these comical and subversive details.