238.2T-14 Concrete Thixotropy

Fresh concrete can exhibit different rheological behavior when at rest than when flowing. This difference is due to thixotropy, which can have important consequences for formwork pressure, multi-lift casting, slip-form paving, pumping, and segregation resistance. This TechNote defines thixotropy and distinguishes it from other changes in rheological properties; discusses the origins of, test methods for measuring, and factors affecting thixotropy; and concludes with its applications.

14C as a tool to trace terrestrial carbon in a complex lake system: implications for foodweb structure and carbon cycling

Carbon and nitrogen stable isotope analysis (SIA) has identified the terrestrial subsidy of freshwater food-webs but relies on different 13C fractionation in aquatic and terrestrial primary producers. However dissolved inorganic carbon (DIC) is partly comprised of 13C depleted respiration of terrestrial C and ‘old’ C derived from weathering of catchment geology. SIA thus fails to differentiate between the contribution of old and recently fixed terrestrial C. DIC in alkaline lakes is partially derived from weathering of 14C-free carbonaceous bedrock This
yields an artificial age offset leading samples to appear significantly older than their actual age. As such, 14C can be used as a biomarker to identify the proportion of autochthonous C in the food-web. With terrestrial C inputs likely to increase, the origin and utilisation of ‘old’ or ‘recent’ allochthonous C in the food-web can also be determined. Stable isotopes and 14C were measured for biota, particulate organic matter (POM), DIC and dissolved organic carbon (DOC) from Lough Erne, Northern Ireland, a humic but alkaline lake. High winter δ15N values in calanoid zooplankton (δ15N =24‰) relative to phytoplankton and POM (δ15N =6‰ and 12‰ respectively) may reflect several microbial trophic levels between terrestrial C and calanoids. Furthermore winter calanoid 14C ages are consistent with DOC from inflowing rivers (87 and 75 years BP respectively) but not phytoplankton (355 years BP). Summer calanoid δ13N, δ15N and 14C (312 years BP) indicate greater reliance on phytoplankton. There is also temporal and spatial variation in DIC, DOC and POM C isotopes.

Evidence for the reliability and validity, but not the practical utility of the two-factor Consideration of Future Consequences Scale-14

Researchers have proposed 1-factor, 2-factor, and bifactor solutions to the 12-item Consideration of Future Consequences Scale (CFCS-12). In order to overcome some measurement problems and to create a robust and conceptually useful two-factor scale the CFCS-12 was recently modified to include two new items and to become the CFCS-14. Using a University sample, we tested four competing models for the CFCS-14: (a) a 12-item unidimensional model, (b) a model fitted for two uncorrelated factors (CFC-Immediate and CFC-Future), (c) a model fitted for two correlated factors (CFC-I and CFC-F), and (d) a bifactor model. Results suggested that the addition of the two new items has strengthened the viability of a two factor solution of the CFCS-14. Results of linear regression models suggest that the CFC-F factor is redundant. Further studies using alcohol and mental health indicators are required to test this redundancy.

Mundo Shuar 14: Organizarse o sucumbir

En la búsqueda de un modelo de desarrollo para FED-Q, presentamos a la Federación de Centro Shuar como un caso de desarrollo positivo, como un modelo de movimiento indígena que hasta el presente se muestra como liberador. Como aporte al modelo de desarrollo, la Federación de Centro Shuar tiene, ante todo , su Organización.

14º Encontro Internacional de Arte e Tecnologia: #14.ART: arte e desenvolvimento humano

#14ART: Arte e Desenvolvimento Humano propõe-se discutir novos territórios para uma maior sustentabilidade, assim como debater futuras evoluções criativas. O evento procurará entrepor-se em zonas de contato entre domínios tradicionalmente separadas - a arte e a ciência, pesquisa acadêmica e práticas criativas independentes, politicas sustentáveis e engajamento social, para o século XXI. Pretende-se que a discussão se centre, sobretudo, sobre como explorar o potencial transformativo da arte na pós-média. Hoje, de acordo com vários pensadores - Rosalind Krauss, a Lev Manovich, Peter Weibel – estamos numa fase pós- média; não existe um só meio, nos nossos dias, que domine o discurso da pratica artística contemporânea no campo dos média, bem pelo contrário os média encontram-se, hoje, engajados no pensamento critico do discurso da contemporaneidade. Através dos eventos anteriores deste Encontro Internacional, ficou claro que a arte hoje - com as condições proporcionadas pelo discurso do pós-média - oferece um potencial muito mais inteligente e interessante elocução para as artes. No entanto, as qualidade simbólicas e estéticas, bem como o pensamento critico e os aspectos investigativos e de confronto teórico da “pré-média arte”, também se apresentam ser tão importantes para a “pós-media arte”, obrigando o discurso artístico a manter um fio condutor entre o físico (a obra) e o mental (conceito) - realidades e utopias.

Repply to: Brito, A.C., Brotas, V., Caetano, M., Coutinho, T.P., Bordalo, A.A., Icely, J., Neto, J.M., Serôdio, J., Moita, T. (2012) "Defining phytoplankton class boundaries in Portuguese transitional waters: an evaluation of the ecological quality status according to the Water Framework Directive" [Ecological Indicators 19, 5-14]

We write to comment on the recently published paper “Defining phytoplankton class boundaries in Portuguese transitional waters: an evaluation of the ecological quality status according to the Water Framework Directive” (Brito et al., 2012). This paper presents an integrated methodology to analyse the ecological quality status of several Portuguese transitional waters, using phytoplanktonrelated metrics. One of the systems analysed, the Guadiana estuary in southern Portugal, is considered the most problematic estuary, with its upstream water bodies classified as Poor in terms of ecological status. We strongly disagree with this conclusion and we would like to raise awareness to some methodological constraints that, in our opinion, are the basis of such deceptive conclusions and should therefore not be neglected when using phytoplankton to assess the ecological status of natural waters.