From stellar to planetary composition: Galactic chemical evolution of Mg/Si mineralogical ratio

Aims. The main goal of this work is to study element ratios that are important for the formation of planets of different masses. Methods. We study potential correlations between the existence of planetary companions and the relative elemental abundances of their host stars. We use a large sample of FGK-type dwarf stars for which precise Mg, Si, and Fe abundances have been derived using HARPS high-resolution and high-quality data. Results. A first analysis of the data suggests that low-mass planet host stars show higher [Mg/Si] ratios, while giant planet hosts present [Mg/Si] that is lower than field stars. However, we found that the [Mg/Si] ratio significantly depends on metallicity through Galactic chemical evolution. After removing the Galactic evolution trend only the difference in the [Mg/Si] elemental ratio between low-mass planet hosts and non-hosts was present in a significant way. These results suggest that low-mass planets are more prevalent around stars with high [Mg/Si]. Conclusions. Our results demonstrate the importance of Galactic chemical evolution and indicate that it may play an important role in the planetary internal structure and composition. The results also show that abundance ratios may be a very relevant issue for our understanding of planet formation and evolution.

Si fecisti, nega

-l.

Leḳsiḳon fun der yidisher liṭeraṭur, prese un filologie

Zalmen Reyzen

Affetti musici : ne quali si contengono motetti a una, 2, 3, 4, & sei voci ; co'l modo per concertarli nel basso per l'organo

7 Stb.: Canto, Alto, Tenore, Basso, Quinto, Sesta parte, Organo

"Si vous abuzez de ma patience!"

Signatur des Originals: S 36/G10567

Marcel Junca als Mossoul, Rollenbild, in: Adolphe Adam: Si jé̀tais Roi

Signatur des Originals: S 36/G01261

Ṿos ṿill "Agudat Yiśraʾel"? : referaṭ ershṭaṭṭeṭ oyf der ḳonferents tsu Ḳatovits am 12. Siṿan (28ten May) 5672

fon Yaʿaḳov Rozenhaym, Franḳfurṭ a. M.

Validating the dietary intake questions from the Tu Salud, ¡Si Cuenta! questionnaire

Background. Poor nutrition is an important factor in the onset of obesity which is a growing problem in the United States that disproportionately affects Mexican-Americans. In order to form recommendations and effectively target nutrition in interventions it is necessary to have valid epidemiological tools to better understand dietary trends. Purpose. The purpose of this study is to evaluate the validity of the nutritional intake questions from the Tu Salud, ¡Sí Cuenta! Questionnaire in an adult Mexican-American population. Methods. Fifty participants in the Cameron County Hispanic Cohort were recruited into the validity study, which consisted of completing the Tu Salud, ¡Sí Cuenta! questionnaire and the 24-hour recall with a 2 hour time period between administrations. Responses were analyzed to determine the percent agreement, kappa statistic and Spearman rank order correlation. Results: Five items had good validity (>0.6), three items had fair validity (>0.4), and three items had poor validity (<0.4). In general, items that had low validity were those that were reported in low frequencies by study subjects. Overall, the Tu Salud, ¡Sí Cuenta! questionnaire showed good validity, making this questionnaire a valuable tool to assess the dietary intake patterns of this Mexican-American adult population. ^

(Table 1) Water column biogenic silica concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa

Southern Ocean biogeochemical processes have an impact on global marine primary production and global elemental cycling, e.g. by likely controlling glacial-interglacial pCO2 variation. In this context, the natural silicon isotopic composition (d30Si) of sedimentary biogenic silica has been used to reconstruct past Si-consumption:supply ratios in the surface waters. We present a new dataset in the Southern Ocean from a IPY-GEOTRACES transect (Bonus-GoodHope) which includes for the first time summer d30Si signatures of suspended biogenic silica (i) for the whole water column at three stations and (ii) in the mixed layer at seven stations from the subtropical zone up to the Weddell Gyre. In general, the isotopic composition of biogenic opal exported to depth was comparable to the opal leaving the mixed layer and did not seem to be affected by any diagenetic processes during settling, even if an effect of biogenic silica dissolution cannot be ruled out in the northern part of the Weddell Gyre. We develop a mechanistic understanding of the processes involved in the modern Si-isotopic balance, by implementing a mixed layer model. We observe that the accumulated biogenic silica (sensu Rayleigh distillation) should satisfactorily describe the d30Si composition of biogenic silica exported out of the mixed layer, within the limit of the current analytical precision on the d30Si. The failures of previous models (Rayleigh and steady state) become apparent especially at the end of the productive period in the mixed layer, when biogenic silica production and export are low. This results from (1) a higher biogenic silica dissolution:production ratio imposing a lower net fractionation factor and (2) a higher Si-supply:Si-uptake ratio supplying light Si-isotopes into the mixed layer. The latter effect is especially expressed when the summer mixed layer becomes strongly Si-depleted, together with a large vertical silicic acid gradient, e.g. in the Polar Front Zone and at the Polar Front.

«Si el hombre careciera de oído…», según Bernardo Silvestre

Durante la primera mitad del siglo XII cobró vigencia en Chartres una escuela de pensamiento filosófico-teológico caracterizada, en buena medida, por el afán de explicación del Génesis mediante el Comentario de Calcidio al Timeo de Platón. La Cosmografía de Bernardo Silvestre, dedicada a Teodorico de Chartres, permanece en las proximidades del interés cientificista y argumentativo propio de esta escuela, pero está formulada en términos literarios, en parte en prosa y en parte en verso. Dividida en dos grandes secciones: ‘Macrocosmos’ y ‘Microcosmos’, se cierra con la descripción de la naturaleza humana y su funcionamiento operativo en los procesos vitales y gnoseológicos. Los sentidos de que goza el hombre, asentados en la cabeza, son considerados instrumentos al servicio del intelecto que juzga. Ellos provienen de una única fuente pero desarrollan de diversas maneras sus operaciones. Si faltaran, no habría ni enseñanza de las letras ni sabiduría.

(Appendix 1) Age, Ge/Si ratio, aluminium and opal contents in ODP Sites 175-1081 and 175-1084

As a result of both culture and sediment core studies, the ratio of germanium (Ge) to silicon (Si) in diatom shells has been proposed as a proxy for monitoring whole-ocean changes in seawater Ge/Si, a ratio affected by changes in continental weathering. However, because of the difficulties of extracting and cleaning diatom frustules from deep-sea sediments, only samples from highly pure diatom oozes in the Antarctic region have been previously analyzed. Here we present data on diatom Ge/Si ratios, (Ge/Si)opal, for the time interval between 3.1 and 1.9 Ma from a mid-latitude, coastal upwelling area where significant terrigenous sediment input complicated the sample processing and analyses. In general, our (Ge/Si)opal values show the same decreasing trend after 2.6 Ma than previously measured in Antarctic sediments (Shemesh et al., 1989. Paleoceanography 4, 221-231), but with a noisier background that may reflect the local imprint of proximal continental input superimposed upon global changes in the ocean reservoir. The time of initiation of large-scale North Hemisphere glaciation at ~2.6 Ma is characterized by a declining pattern of diatom Ge/Si ratios, which could have resulted from a global increase in the input of riverine Si due to enhanced silica weathering and/or equatorward (northward) intrusions of subantarctic waters enriched in silica. High (Ge/Si)opal ratios are associated with high opal contents from the same sediment samples and with warm climate as indicated by depleted benthic foraminiferal d18O values from the North and Equatorial Atlantic. Cold periods signified by enriched benthic d18O values, on the contrary, are associated with lower (Ge/Si)opal ratios. We interpret diatom Ge/Si values to reflect the prevailing weathering state on the continents, with greater chemical weathering during warm and wet periods of the Pliocene and less during cooler and drier intervals.

Química y medio ambiente : "¿Y si nos ponemos las pilas?" Una propuesta de taller para llevar al aula

En este trabajo se presenta una propuesta didáctica implementada, en el marco de la Semana de la Ciencia y la Tecnología, a través de la modalidad de taller para alumnos de escuelas secundarias referido a pilas y baterías y su impacto en el medio ambiente. Dicha propuesta tiene base en el enfoque Ciencia, Tecnología, Sociedad y Ambiente (CTSA), la cual tiende a favorecer la integración de las dimensiones cognitivas y actitudinales de los estudiantes así como también propender un trabajo interdisciplinario. El creciente consumo de pilas y baterías induce a reflexionar sobre su destino cuando quedan en desuso y el impacto ambiental que su acumulación origina. En este sentido, puede resultar de interés la implementación de esta propuesta de trabajo referida a aspectos generales y efectos en el medio ambiente de pilas y baterías así como también el análisis de las posibles vías de deposición. La escasez de información clara sobre el destino que se le debe dar a las pilas y el desconocimiento generalizado respecto al manejo de residuos peligrosos nos lleva a pensar en la necesidad de promover este tipo de reflexiones en el aula