An Evaluation of the Second Generation Consolidation Monitoring Device, HR-1013, 1984

The objective was to evaluate the usefulness, accuracy, precision, and reproducibility of the second generation CMD for PC concrete under production conditions.

Efficient transduction of dendritic cells and induction of a T-cell response by third-generation lentivectors.

In order to induce a therapeutic T lymphocyte response, recombinant viral vaccines are designed to target professional antigen-presenting cells (APC) such as dendritic cells (DC). A key requirement for their use in humans is safe and efficient gene delivery. The present study assesses third-generation lentivectors with respect to their ability to transduce human and mouse DC and to induce antigen-specific CD8+ T-cell responses. We demonstrate that third-generation lentivectors transduce DC with a superior efficiency compared to adenovectors. The transfer of DC transduced with a recombinant lentivector encoding an antigenic epitope resulted in a strong specific CD8+ T-cell response in mice. The occurrence of lower proportions of nonspecifically activated CD8+ cells suggests a lower antivector immunity of lentivector compared to adenovector. Thus, lentivectors, in addition to their promise for gene therapy of brain disorders might also be suitable for immunotherapy.

Code des assurances sur la vie : manuel pratique de l'assureur et de l'assuré,... / par Édouard Fey,...

Collection : Petite encyclopédie juridique ; 30

A reassessment of models for hydrocarbon generation in the Khibiny nepheline syenite complex, Kola Peninsula, Russia

Although hydrocarbon-bearing fluids have been known from the alkaline igneous rocks of the Khibiny intrusion for many years, their origin remains enigmatic. A recently proposed model of post-magmatic hydrocarbon (HC) generation through Fischer-Tropsch (FT) type reactions suggests the hydration of Fe-bearing phases and release of H-2 which reacts with magmatically derived CO2 to form CH4 and higher HCs. However, new petrographic, microthermometric, laser Raman, bulk gas and isotope data are presented and discussed in the context of previously published work in order to reassess models of HC generation. The gas phase is dominated by CH4 with only minor proportions of higher hydrocarbons. No remnants of the proposed primary CO2-rich fluid are found in the complex. The majority of the fluid inclusions are of secondary nature and trapped in healed microfractures. This indicates a high fluid flux after magma crystallisation. Entrapment conditions for fluid inclusions are 450-550 degrees C at 2.8-4.5 kbar. These temperatures are too high for hydrocarbon gas generation through the FT reaction. Chemical analyses of rims of Fe-rich phases suggest that they are not the result of alteration but instead represent changes in magma composition during crystallisation. Furthermore, there is no clear relationship between the presence of Fe-rich minerals and the abundance of fluid inclusion planes (FIPs) as reported elsewhere. delta C-13 values for methane range from -22.4% to -5.4%, confirming a largely abiogenic origin for the gas. The presence of primary CH4-dominated fluid inclusions and melt inclusions, which contain a methane-rich gas phase, indicates a magmatic origin of the HCs. An increase in methane content, together with a decrease in delta C-13 isotope values towards the intrusion margin suggests that magmatically derived abiogenic hydrocarbons may have mixed with biogenic hydrocarbons derived from the surrounding country rocks. (C) 2006 Elsevier BV. All rights reserved.