Mover para melhor nascer: liberdade de movimentos e posições verticais no primeiro estádio do trabalho de parto

A Organização Mundial de Saúde destaca a deambulação e a adoção de posições verticais pela parturiente, como práticas demonstradamente benéficas, devendo ser estimuladas pela enfermeira obstetra na condução do trabalho de parto e parto normal, em situações de baixo risco obstétrico. O projeto preconizou a promoção da deambulação e o incentivo à adoção de posições verticais na fase ativa do trabalho de parto. As intervenções de enfermagem na promoção destas práticas foram avaliadas na equipa de enfermeiros obstetras do Serviço de Urgência Obstétrica e Ginecológica do Centro Hospitalar Barreiro-Montijo, Entidade Pública Empresarial e num grupo de parturientes, através da aplicação de questionários. As necessidades dos enfermeiros obstetras e das parturientes determinaram a realização de ações formativas e educacionais e a elaboração de materiais informativos de suporte à prática assistencial. A avaliação do projeto demonstrou que ainda existem práticas a serem melhoradas, sendo a sua continuidade vantajosa para profissionais e parturientes; ABSTRACT: TITLE: Move to Better Birth - Freedom of Movement and Upright Positions in First Stage of Labor. The World Health Organization highlights ambulation and adoption of vertical position by the woman, as demonstrated beneficial practices and should be encouraged by obstetric nurses in the conduct of obstetric labor and normal delivery, in low risk situations. The project advocated for the promotion of ambulation and encouragement for the adoption of vertical positions in the active phase of labor. Nursing interventions to promote these practices were evaluated in the obstetric nurses team of Obstetric and Gynecological Emergency Department from Hospital Center Barreiro-Montijo, Business Public Entity, and in a group of women in labor, through the use of questionnaires. The needs of obstetric nurses and women in labor determined the realization of training and educacional activities and the development of information materials to support the care practice. The project evaluation demonstrates that there are still practices to be improved, and its continuity being advantageous for professionals and women in labor.

Improving magnetic coupling for battery charging through 3D magnetic flux

The spatial distribution of the magnetic field and the coupling between the coils in the Wireless Power Transfer (WPT) systems is an important aspect to consider in the system design and efficiency optimization. The presented study in this paper is based on tests performed on a physical model. The transmitting (primary) equipment, is an electrical three-phase system, capable to be connected in star or delta (both electrically and geometrically). The measured results allow to describe graphically the magnetic field distribution in three dimensions. The analytical formulas aim to help to understand and to quantify the physical phenomena but they cannot be considered a universal approach and the measurement results help to understand better the observable facts. In the WPT, the key issues that will influence the efficiency, are the alignment of the coils, the spatial orientation of the magnetic field, the detachment and the tilt between the windings, all they changing the magnetic coupling between the transmitter and the receiver of energy. This research is directed not only to the magnetic field distribution but finally, to optimize the energy transfer efficiency.

Extensional orogenic collapse captured by strike-slip tectonics:

The late Paleozoic collision between Gondwana and Laurussia resulted in the polyphase deformation and magmatism that characterizes the Iberian Massif of the Variscan orogen. In the Central Iberian Zone, initial con- tinental thickening (D1; folding and thrusting) was followed by extensional orogenic collapse (D2) responsible for the exhumation of high-grade rocks coeval to the emplacement of granitoids. This study presents a tectonometamorphic analysis of the Trancoso-Pinhel region (Central Iberian Zone) to ex- plain the processes in place during the transition froman extension-dominated state (D2) to a compression-dom- inated one (D3).Wereveal the existence of low-dipping D2 extensional structures later affected by several pulses of subhorizontal shortening, each of them typified by upright folds and strike-slip shearing (D3, D4 and D5, as identified by superimposition of structures). The D2 Pinhel extensional shear zone separates a low-grade domain from an underlying high-grade domain, and it contributed to the thermal reequilibration of the orogen by facil- itating heat advection from lower parts of the crust, crustal thinning, decompression melting, and magma intru- sion. Progressive lessening of the gravitational disequilibrium carried out by this D2 shear zone led to a switch from subhorizontal extension to compression and the eventual cessation and capture of the Pinhel shear zone by strike-slip tectonics during renewed crustal shortening. High-grade domains of the Pinhel shear zone were folded together with low-grade domains to define the current upright folded structure of the Trancoso-Pinhel re- gion, the D3 Tamames-Marofa-Sátão synform. Newdating of syn-orogenic granitoids (SHRIMP U\\Pb zircon dat- ing) intruding the Pinhel shear zone, together with the already published ages of early extensional fabrics constrain the functioning of this shear zone to ca. 331–311 Ma, with maximum tectonomagmatic activity at ca. 321–317 Ma. The capture and apparent cessation of movement of the Pinhel shear zone occurred at ca. 317– 311 Ma.