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CONTEXT: Sulphur is one of the most abundant elements in the Universe. Surprisingly, sulphuretted molecules are not as abundant as expected in the interstellar medium and the identity of the main sulphur reservoir is still an open question. AIMS: Our goal is to investigate the H2S chemistry in dark clouds, as this stable molecule is a potential sulphur reservoir. METHODS: Using millimeter observations of CS, SO, H2S, and their isotopologues, we determine the physical conditions and H2S abundances along the cores TMC 1-C, TMC 1-CP, and Barnard 1b. The gas-grain model Nautilus is used to model the sulphur chemistry and explore the impact of photo-desorption and chemical desorption on the H2S abundance. RESULTS: Our modeling shows that chemical desorption is the main source of gas-phase H2S in dark cores. The measured H2S abundance can only be fitted if we assume that the chemical desorption rate decreases by more than a factor of 10 when n H > 2 × 104. This change in the desorption rate is consistent with the formation of thick H2O and CO ice mantles on grain surfaces. The observed SO and H2S abundances are in good agreement with our predictions adopting an undepleted value of the sulphur abundance. However, the CS abundance is overestimated by a factor of 5 - 10. Along the three cores, atomic S is predicted to be the main sulphur reservoir. CONCLUSIONS: The gaseous H2S abundance is well reproduced, assuming undepleted sulphur abundance and chemical desorption as the main source of H2S. The behavior of the observed H2S abundance suggests a changing desorption efficiency, which would probe the snowline in these cold cores. Our model, however, highly overestimates the observed gas-phase CS abundance. Given the uncertainty in the sulphur chemistry, we can only conclude that our data are consistent with a cosmic elemental S abundance with an uncertainty of a factor of 10.
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GEMS is an IRAM 30m Large Program whose aim is determining the elemental depletions and the ionization fraction in a set of prototypical star-forming regions. This paper presents the first results from the prototypical dark cloud TMC 1. Extensive millimeter observations have been carried out with the IRAM 30m telescope (3 mm and 2 mm) and the 40m Yebes telescope (1.3 cm and 7 mm) to determine the fractional abundances of CO, HCO+, HCN, CS, SO, HCS+, and N2H+ in three cuts which intersect the dense filament at the well-known positions TMC 1-CP, TMC 1-NH3, and TMC 1-C, covering a visual extinction range from A V ~ 3 to ~20 mag. Two phases with differentiated chemistry can be distinguished: i) the translucent envelope with molecular hydrogen densities of 1-5×103 cm-3; and ii) the dense phase, located at A V > 10 mag, with molecular hydrogen densities >104 cm-3. Observations and modeling show that the gas phase abundances of C and O progressively decrease along the C+/C/CO transition zone (A V ~ 3 mag) where C/H ~ 8×10-5 and C/O~0.8-1, until the beginning of the dense phase at A V ~ 10 mag. This is consistent with the grain temperatures being below the CO evaporation temperature in this region. In the case of sulfur, a strong depletion should occur before the translucent phase where we estimate a S/H ~ (0.4 - 2.2) ×10-6, an abundance ~7-40 times lower than the solar value. A second strong depletion must be present during the formation of the thick icy mantles to achieve the values of S/H measured in the dense cold cores (S/H ~8×10-8). Based on our chemical modeling, we constrain the value of ζ H2 to ~ (0.5 - 1.8) ×10-16 s-1 in the translucent cloud.
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OBJECTIVE: In view of the fact that Paget's disease of bone (PD) tends to appear in so-called 'foci', a case-control study was undertaken with the dual aim of: 1) identifying areas having a higher likelihood of constituting PD 'foci'; and 2) detecting the geographic origin of 'PD-carrier' families. METHODS: Two data sets were analysed, one covering the place of birth of 231 cases and 436 controls, and the other covering the place of birth of cases, controls and their parents. Analysis was restricted to six Autonomous Regions accounting for 60% of Spain's towns and cities. To identify geographical areas of high prevalence we used the scan statistic. RESULTS: In the first analysis, 6 possible clusters were detected, corresponding to the districts of Avila (Avila), Lozoya-Somosierra (Madrid), Tierra de Campos(Palencia), the Guadalajara Range, South-west Madrid and Cuenca Hills. The second analysis confirmed the 6 groupings identified by the above procedure and, in addition, detected a further 8 possible clusters. Geographical proximity suggests that in some cases, rather than individual groupings, these may instead constitute larger foci. CONCLUSION: The results point to the possible existence of different PD foci, some coinciding with clusters that have already been reported, and others indicating familial origin in areas that had never previously received PD-specific attention.
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Osteíte Deformante/epidemiologia , Análise por Conglomerados , Métodos Epidemiológicos , Humanos , Pessoa de Meia-Idade , Prevalência , Espanha/epidemiologiaRESUMO
Este artículo pretende mostrar diversos protocolos de actuación ante un paciente que se presenta en nuestra consulta con dolor articular de inicio reciente, insistiendo en la detección de aquellos signos de alarma ante los cuales un diagnóstico precoz determina una disminución de la morbimortalidad (AU)