Geographic information systems - GIS, a view from the water resource

This research paper presents an overview of the state of the art Geographic Information Systems - GIS, which has been defined and characterized important aspects about these systems and their contribution to the analysis of water bodies from various use and development, which allows the achievement of the Platform for water Resources Network of the Colombian Caribbea

Geographic information systems - GIS, a view from the water resource

This research paper presents an overview of the state of the art Geographic Information Systems - GIS, which has been defined and characterized important aspects about these systems and their contribution to the analysis of water bodies from various use and development, which allows the achievement of the Platform for water Resources Network of the Colombian Caribbea

Tectonic evolution, geomorphology and influence of bottom currents along a large submarine canyon system: The São Vicente Canyon (SW Iberian margin)

A multi-scale dataset consisting of multi-beam echo-sounder, 2D multi-channel seismic and sidescan sonar (TOBI) data allows us to identify a large variety of morphologies originating from sedimentary and tectonic processes along the São Vicente Canyon (SVC), which is the largest submarine canyon developed in the external part of the Gulf of Cadiz. The SVC is located in one of the most seismogenic areas of Western Europe. The convergence between the Eurasian and African plates has controlled the formation and evolution of the canyon. The SVC is tectonically controlled by three main thrust faults: the Marquês de Pombal Fault, the São Vicente Fault and the Horseshoe Fault. No major rivers feed sediment to the canyon head, but the main sediment source is related to the dismantling of canyon flanks and the MOW (Mediterranean Overflow Water). This current contributes sediments by two different processes: a) conturites deposition at the head and flanks of the SVC that periodically fail into the canyon; and b) the coarser-grained and denser sediment of the MOW might be trapped at the head of the canyon and could develops into hyperpycnal flows. The SVC is characterized by retrogressive erosion being submarine landslide deposits and scars the main seafloor morphologies. The tectonic and stratigraphic interpretation of seismic profiles indicate that the SVC is a clear example of a diachronous and segmented canyon developed since the Late Miocene in an area of present-day active plate tectonics. This study investigates the interaction between active tectonics, the dynamics of submarine canyons and the resulting geomorphologies

Human papillomavirus vaccine administration behaviors and influences among Arizona pharmacists and pharmacy interns

This study assessed 27 Arizona community pharmacists’ and pharmacy interns’ human papillomavirus (HPV) vaccine administration behaviors and influences. We recruited community pharmacists and pharmacy interns from a statewide pharmacy conference to complete a 40-item cross-sectional survey. Informed by the Theory of Planned Behavior, the survey assessed pharmacists’ HPV vaccine-related behaviors, intentions, attitudes, subjective norms, and perceived behavioral control to vaccinate against HPV. We analyzed all data using descriptive statistics and correlations. Overall, most pharmacists held positive attitudes about the HPV vaccine. However, the majority rarely administered the HPV vaccine. Intentions to vaccinate and subjective norms positively correlated with vaccine administration behavior. Pharmacists’ positive attitudes about the vaccine, subjective norm to vaccinate, and behavioral control or self-efficacy to recommend the vaccine impacted their intentions to vaccinate against HPV. Most surveyed pharmacists believed that the most substantial HPV vaccine administration barriers include parental consent and parental stigma against the vaccine. The most common pharmacy-related barrier was the lack of a tracking and reminder system to encourage patients to return for additional HPV vaccine doses. This work highlights the need to increase public awareness that pharmacists can administer vaccines to adolescents. Study authors recommend offering communication training to increase pharmacists’ perceived behavioral control to recommend the HPV vaccine

(Table 1) Grain size results, statistical parameters and magnetic susceptibility values of disturbed sediments from ODP holes 204-1249C and 204-1245B

Soupy and mousse-like fabrics are disturbance sedimentary features that result from the dissociation of gas hydrate, a process that releases water. During the core retrieval process, soupy and mousse-like fabrics are produced in the gas hydrate-bearing sediments due to changes in pressure and temperature conditions. Therefore, the identification of soupy and mousse-like fabrics can be used as a proxy for the presence of gas hydrate in addition to other evidence, such as pore water freshening or anomalously cool temperature. We present here grain-size results, mineralogical composition and magnetic susceptibility data of soupy and mousse-like samples from the southern Hydrate Ridge (Cascadia accretionary complex) acquired during Leg 204 of the Ocean Drilling Program. In order to study the relationship between sedimentary texture and the presence of gas hydrates, we have compared these results with the main textural and compositional data available from the same area. Most of the disturbed analyzed samples from the summit and the western flank of southern Hydrate Ridge show a mean grain size coarser than the average mean grain size of the hemipelagic samples from the same area. The depositional features of the sediments are not recognised due to disturbance. However, their granulometric statistical parameters and distribution curves, and magnetic susceptibility logs indicate that they correspond to a turbidite facies. These results suggest that gas hydrates in the southern Hydrate Ridge could form preferentially in coarser grain-size layers that could act as conduits feeding gas from below the BSR. Two samples from the uppermost metres near the seafloor at the summit of the southern Hydrate Ridge show a finer mean grain-size value than the average of hemipelagic samples. They were located where the highest amount of gas hydrates was detected, suggesting that in this area the availability of methane gas was high enough to generate gas hydrates, even within low-permeability layers. The mineralogical composition of the soupy and mousse-like sediments does not show any specific characteristic with respect to the other samples from the southern Hydrate Ridge

Grain-size and bulk and clay mineralogy of ODP Leg 204 sediments

We present grain size, granulometric statistical parameters, and calcium carbonate content of sediment samples from the summit and east and west flanks of southern Hydrate Ridge (Sites 1244-1250). These data are compared with magnetic susceptibility measurements from the same intervals. Bulk and clay mineralogy from Sites 1244 (east flank), 1247 (west flank), and 1250 (summit) are also presented. The integration of these data allows us to characterize the main sedimentary facies and composition of the Quaternary age sediments from southern Hydrate Ridge