A system of containment to prevent oil spills from sunken tankers.

Worldwide tank spills represent 10% of the average annual input of oil in the sea. When such spills arise from wrecks at depth, neutralisation of environmental impacts is difficult to achieve. Extracting oil from sunken tankers is expensive, and, unfortunately, all of the oil cannot be extracted, as the Prestige case demonstrates. We propose an environmentally appropriate, cost-effective and proactive method to stop the long-term problem of leaks from sunken tankers similar to the Prestige. This method confines the wreck with a "sediment" capping of sepiolite mineral that emulates a natural sediment. A set of experiments and simulations shows that sepiolite has the characteristics necessary to accomplish the confinement of any current or future sunken tanker with minimal environmental perturbation.

Inmunidad humoral a tétanos, sarampión y rubéola en niños con leucemia linfoblástica aguda luego del tratamiento quimioterápico / Humoral immunity to tetanus, measles and rubella in children with acute lymphoblastic leukemia after chemotherapy

Los regímenes de quimioterapia y los avances en el soporte clínico han mejorado la supervivencia de los niños con leucemia linfoblástica aguda. Son temas de preocupación las secuelas del tratamiento, entre ellas, el daño inmunológico inducido por la terapia inmunosupresora, que se refleja en la pérdida de niveles protectores de anticuerpos provistos por inmunizaciones previas. Nuestro objetivo fue evaluar la presencia de títulos protectores de anticuerpos para sarampión, rubéola y tétanos en pacientes con leucemia linfoblástica aguda luego de haber finalizado el tratamiento quimioterápico. Se incluyeron 61 niños con leucemia linfoblástica aguda asistidos en el Hospital Garrahan, que habían finalizado el tratamiento, como mínimo, 6 meses antes y con vacunación completa previa al diagnóstico. Las tasas de anticuerpos protectores fueron sarampión: 46% (IC 32-59); tétanos: 53% (IC 40-67); rubéola: 60% (IC 47-63). Estos resultados refuerzan la necesidad de reconsiderar la revacunación en este grupo de pacientes.

Chemotherapy regimens and clinical support advances have improved survival in children with acute lymphoblastic leukemia. The after-effects of treatment are a reason for concern, including damage to the immune system induced by immunosuppressive therapy which is reflected in the loss of antibody protection provided by prior immunizations. Our goal was to assess the presence of measles, rubella, and tetanus protective antibody titers among patients with acute lymphoblastic leukemia after completing chemotherapy. Sixty-one children with acute lymphoblastic leukemia seen at the Hospital Garrahan were included; patients had finished their chemotherapy at least 6 months earlier and had a complete immunization schedule before diagnosis. The rates of protective antibodies were 46% (CI: 32-59) for measles, 53% (CI 40-67) for tetanus, and 60% (CI 47-63) for rubella. These results strengthen the need to reconsider revaccination in this group of patients.

Humoral immunity to tetanus, measles and rubella in children with acute lymphoblastic leukemia after chemotherapy. / Inmunidad humoral a tétanos, sarampión y rubéola en niños con leucemia linfoblástica aguda luego del tratamiento quimioterápico.

Chemotherapy regimens and clinical support advances have improved survival in children with acute lymphoblastic leukemia. The after-effects of treatment are a reason for concern, including damage to the immune system induced by immunosuppressive therapy which is reflected in the loss of antibody protection provided by prior immunizations. Our goal was to assess the presence of measles, rubella, and tetanus protective antibody titers among patients with acute lymphoblastic leukemia after completing chemotherapy. Sixty-one children with acute lymphoblastic leukemia seen at the Hospital Garrahan were included; patients had finished their chemotherapy at least 6 months earlier and had a complete immunization schedule before diagnosis. The rates of protective antibodies were 46% (CI: 32-59) for measles, 53% (CI 40-67) for tetanus, and 60% (CI 47-63) for rubella. These results strengthen the need to reconsider revaccination in this group of patients.

Los regímenes de quimioterapia y los avances en el soporte clínico han mejorado la supervivencia de los niños con leucemia linfoblástica aguda. Son temas de preocupación las secuelas del tratamiento, entre ellas, el daño inmunológico inducido por la terapia inmunosupresora, que se refleja en la pérdida de niveles protectores de anticuerpos provistos por inmunizaciones previas. Nuestro objetivo fue evaluar la presencia de títulos protectores de anticuerpos para sarampión, rubéola y tétanos en pacientes con leucemia linfoblástica aguda luego de haber finalizado el tratamiento quimioterápico. Se incluyeron 61 niños con leucemia linfoblástica aguda asistidos en el Hospital Garrahan, que habían finalizado el tratamiento, como mínimo, 6 meses antes y con vacunación completa previa al diagnóstico. Las tasas de anticuerpos protectores fueron sarampión: 46% (IC 32-59); tétanos: 53% (IC 40-67); rubéola: 60% (IC 47-63). Estos resultados refuerzan la necesidad de reconsiderar la revacunación en este grupo de pacientes.

Long-term geochemical evolution of the near field repository: insights from reactive transport modelling and experimental evidences.

The KBS-3 underground nuclear waste repository concept designed by the Swedish Nuclear Fuel and Waste Management Co. (SKB) includes a bentonite buffer barrier surrounding the copper canisters and the iron insert where spent nuclear fuel will be placed. Bentonite is also part of the backfill material used to seal the access and deposition tunnels of the repository. The bentonite barrier has three main safety functions: to ensure the physical stability of the canister, to retard the intrusion of groundwater to the canisters, and in case of canister failure, to retard the migration of radionuclides to the geosphere. Laboratory experiments (< 10 years long) have provided evidence of the control exerted by accessory minerals and clay surfaces on the pore water chemistry. The evolution of the pore water chemistry will be a primordial factor on the long-term stability of the bentonite barrier, which is a key issue in the safety assessments of the KBS-3 concept. In this work we aim to study the long-term geochemical evolution of bentonite and its pore water in the evolving geochemical environment due to climate change. In order to do this, reactive transport simulations are used to predict the interaction between groundwater and bentonite which is simulated following two different pathways: (1) groundwater flow through the backfill in the deposition tunnels, eventually reaching the top of the deposition hole, and (2) direct connection between groundwater and bentonite rings through fractures in the granite crosscutting the deposition hole. The influence of changes in climate has been tested using three different waters interacting with the bentonite: present-day groundwater, water derived from ice melting, and deep-seated brine. Two commercial bentonites have been considered as buffer material, MX-80 and Deponit CA-N, and one natural clay (Friedland type) for the backfill. They show differences in the composition of the exchangeable cations and in the accessory mineral content. Results from the simulations indicate that pore water chemistry is controlled by the equilibrium with the accessory minerals, especially carbonates. pH is buffered by precipitation/dissolution of calcite and dolomite, when present. The equilibrium of these minerals is deeply influenced by gypsum dissolution and cation exchange reactions in the smectite interlayer. If carbonate minerals are initially absent in bentonite, pH is then controlled by surface acidity reactions in the hydroxyl groups at the edge sites of the clay fraction, although its buffering capacity is not as strong as the equilibrium with carbonate minerals. The redox capacity of the bentonite pore water system is mainly controlled by Fe(II)-bearing minerals (pyrite and siderite). Changes in the groundwater composition lead to variations in the cation exchange occupancy, and dissolution-precipitation of carbonate minerals and gypsum. The most significant changes in the evolution of the system are predicted when ice-melting water, which is highly diluted and alkaline, enters into the system. In this case, the dissolution of carbonate minerals is enhanced, increasing pH in the bentonite pore water. Moreover, a rapid change in the population of exchange sites in the smectite is expected due to the replacement of Na for Ca.