Particle analysis of surgical lung biopsies from deployed and non-deployed US service members during the Global War on Terrorism.

The role that inhaled particulate matter plays in the development of post-deployment lung disease among US service members deployed to Southwest Asia during the Global War on Terrorism has been difficult to define. There is a persistent gap in data addressing the relationship between relatively short-term (months to a few years) exposures to high levels of particulate matter during deployment and the subsequent development of adverse pulmonary outcomes. Surgical lung biopsies from deployed service members and veterans (DSMs) and non-deployed service members and veterans (NDSMs) who develop lung diseases can be analyzed to potentially identify residual deployment-specific particles and develop associations with pulmonary pathological diagnoses.

Grain boundary mobility of carbon in Earth's mantle: a possible carbon flux from the core.

The importance of carbon in Earth's mantle greatly exceeds its modest abundance of approximately 1,000-4,000 ppm. Carbon is a constituent of key terrestrial volatiles (CO, CO(2), CH(4)), it forms diamonds, and it may also contribute to the bulk electrical properties of the silicate Earth. In contrast to that of the mantle, the carbon content of Earth's metallic core may be quite high ( approximately 5 wt %), raising the possibility that the core has supplied carbon to the mantle over geologic time.

A diffusion mechanism for core-mantle interaction.

Understanding the geochemical behaviour of the siderophile elements--those tending to form alloys with iron in natural environments--is important in the search for a deep-mantle chemical 'fingerprint' in upper mantle rocks, and also in the evaluation of models of large-scale differentiation of the Earth and terrestrial planets. These elements are highly concentrated in the core relative to the silicate mantle, but their concentrations in upper mantle rocks are higher than predicted by most core-formation models. It has been suggested that mixing of outer-core material back into the mantle following core formation may be responsible for the siderophile element ratios observed in upper mantle rocks.

A uranyl sulfate cluster in Na10[(UO2)(SO4)4](SO4)2.3H2O.

Decasodium uranyl hexasulfate trihydrate, Na(10)[(UO(2))(SO(4))(4)](SO(4))(2).3H(2)O, contains an unusual uranyl sulfate cluster with the composition [(UO(2))(SO(4))(4)](6-). The cluster is composed of a uranyl pentagonal bipyramid and four sulfate tetrahedra.

Alterations in cellular retinol metabolism contribute to differential retinoid responsiveness in normal human mammary epithelial cells versus breast cancer cells.

The present study was undertaken to compare ROH growth responsiveness between normal human mammary epithelial cells (HMECs), estrogen receptor positive (MCF-7) and negative (MDA-MB-231) breast cancer cells, and assess whether this responsiveness is correlated with differences in ROH metabolism, particularly RA synthesis. HMECs were markedly more growth sensitive to a physiological dose of ROH than breast cancer cells, exhibiting a significant decrease in cell number by 48h and >70% decrease by 144h. In comparison, numbers of MCF-7s were only decreased 32% by 144h.