Análisis de la carga interna en los entrenamientos de fútbol sala femenino de 1ª división nacional

El objetivo de este estudio es analizar la frecuencia cardiaca (FC) y la percepción subjetiva del esfuerzo (RPE) en los entrenamientos de fútbol sala en jugadoras (25.42±4.42 años, 166.57±7.14 cm, 56.50±4.95 kg y 22.23±0.97 IMC) de un equipo de primera división de la liga nacional española. Se registraron, mediante monitores de ritmo cardiaco y la escala de Foster, ocho sesiones de entrenamiento de tipo técnico-táctico, físico y partidos modificados, distribuidas durante la mitad de la temporada. Los resultados de la FC máxima y media obtenida son 174.03±4.15 y 128.29±0.81 ppm en sesiones técnico-tácticas, 179.75±2.05 y 132±2.12 ppm en sesiones físicas, 180.99±1.06 y 133.63±5.52 ppm en partidos modificados, respectivamente. Habiendo diferencias significativas en los resultados de la FC máxima entre las sesiones técnico-tácticas y los partidos modificados (p=0.03) y entre la sesiones físicas y las técnico-tácticas (p=0.04). En cuanto a los resultados de la carga de entrenamiento y la RPE en las sesiones técnico-tácticas son 381.22±16.42 y 6.21±0.12 rpe, en las sesiones físicas 533.25±5.59 y 7.90±0.0 rpe, y en los partidos modificados 531.18±4.21 y 7.97±0.22 rpe, respectivamente. Encontrando diferencias significativas entre los resultados de la RPE y la magnitud de la carga de entrenamiento de las sesiones técnico-tácticas y los partidos modificados (p=0.00) y entre la sesiones físicas y las técnico-tácticas (p=0.00). Estos resultados muestran que la sesión de partido modificado obtiene unos valores de frecuencia cardiaca y de percepción subjetiva del esfuerzo mayor que las sesiones técnico-tácticas y las de trabajo físico.

(Table 1) Age and depth of reflectors of the 3.5-kHz and airgun seismic record and their corresponding depth of ash layers, carbonate peaks, and transition zones from DSDP Hole 83-504B

DSDP cores from areas of low (Site 505) and high heat flow (Site 504 B) near the Costa Rica Rift, together with seismic profiles from the Panama Basin, have been studied to determine the relationship between: (1) carbonate content and physical and acoustic properties; and (2) carbonate content, carbonate diagenesis and acoustic stratigraphy. Except for ash and chert layers, bulk density correlates strongly and linearly with carbonate content. Velocity is uniform downcore and only small variations at a small scale are measured. Thus an abrupt change in carbonate content will cause abrupt changes in acoustic impedance and should cause reflectors that can be detected acoustically. A comparison of seismic profiler reflection records with physical properties, carbonate content and reflection coefficients indicates that the main reflectors can be identified with ash layers, diagenetic boundaries, and carbonate content variations. Diagenesis of carbonate sediments is present at Site 504B in a 260 m-thick ooze-chalk-limestone/chert sequence. These diagenetic sequences occur in areas of higher heat flow (200 mW/m**2). Seismic profiler records can be used to map the extent and depth of these diagenetic boundaries.

(Table 1) Paleomagnetic properties of specimens from DSDP Holes 69-504B and 70-504B

Paleomagnetic and rock magnetic measurements of basalt specimens from DSDP Hole 504B, associated with the Costa Rica Rift, have a mean natural remanence intensity (Jn) between 5 and 10 x 10**-3 gauss, consistent with the presence of a magnetized layer that is 0.5 to 1 km thick, which produces the observed magnetic anomalies. A mean Koenigsberger ratio (Qn) greater than 10 indicates that the remanence dominates the magnetic signal of the drilled section. The susceptibility (x) increases with depth, and the median demagnetizing field (MDF) decreases with increasing depth in Hole 504B, congruent with the downhole increase in the relative abundance of massive flow units. Hole 504B is composed of at least 12 units with distinct stable average inclinations (Is), which probably represent extrusion at times of different geomagnetic field directions and possibly also the effects of faulting. The thickness of basalt associated with these inclination units varies from less than 9 meters to possibly as much as 160 meters. Two relatively thick magnetic units (40 m and 45 m, separated by 100 m) have anomalously high Is values of -53° and -63°, in contrast with the near zero inclinations expected for the equatorial latitude of Site 504. For this reason and because the average inclination of all the magnetic units is skewed to a negative value, it might be that the entire section at Hole 504B was tilted by approximately 30°.

Geochemistry at DSDP Sites 69-505, 69-504 and 70-504

Deep basement penetration during Legs 69 and 70 at Hole 504B in the Panama Basin allowed the recovery of a 561.5-meter sequence of basaltic pillows, thin flows, and breccias interspersed with thick massive flows. The lavas, which are aphyric to moderately plagioclase-olivine-clinopyroxene phyric, are petrologically indistinguishable from typical mid-ocean-ridge basalts (MORB). Some units are distinctive in that they carry accessory chrome-spinel microphenocrysts or emerald green clinopyroxene phenocrysts. Major and trace element analyses were carried out on 67 samples using X-ray fluorescence techniques. The basalts resemble normal MORB in terms of major elements. However, the trace element analyses show that most of the basalts are characterized by very strong depletion in the more incompatible elements compared with, for instance, normal (N type) MORB from the Atlantic at 22°N. Interdigitated with these units are one or two units that have distinctly higher incompatible element concentrations similar to those in basalts of the transitional (T) type from the Reykjanes Ridge (63°N in the Mid-Atlantic Ridge). All the basalts appear to have undergone some high-level crystal fractionation, although this has not proceeded to the extent of yielding ferrobasalts as it has at the adjacent Galapagos Spreading Center or along the East Pacific Rise. The magnetic anomalies are of lower amplitude than in the latter two regions, which suggests that the absence of ferrobasalts may be a general feature of the ocean crust generated at the Costa Rica Rift. The presence of two distinct magma types, one strongly depleted and the other moderately enriched in incompatible elements, suggests that magma chambers at the spreading center are discontinuous rather than continuous and that there is some chemical heterogeneity in the underlying mantle source. Observed variations in incompatible element ratios of basalts from the more depleted group could, however, reflect mixing between these two magma types. In general it would appear that the mantle feeding the Costa Rica Rift is significantly more depleted in incompatible trace elements than that feeding the Mid-Atlantic Ridge.