Report of the treasurer of the Committee of Relief for the Sufferers by the Fall of the Pemberton Mill, in Lawrence, Mass, on the 10th of January, 1860

Signed, p. 19: Charles S. Storrow.

Managerialism at the bottom of the pyramid: a case study in Brazil

Nas últimas décadas, a Base da Pirâmide tem sido cada vez mais debatida entre líderes ocidentais como a nova terra das oportunidades. Com o advento do neoliberalismo no campo do desenvolvimento na década de 1990, o papel da sociedade civil e, em particular, o de Organizações Não-Governamentais, passou a ser enfatizado como sendo central nas estratégias ocidentais no "Sul" do mundo. Os atores do desenvolvimento, no entanto, muitas vezes abordaram essas questões utilizando perspectivas tradicionais, que estavam geralmente fora de contexto. A tese foca na controvérsia em torno do uso de técnicas de gestão em cenários que diferem daqueles nos quais estas ferramentas têm sido desenvolvidas. Em particular, ela procura compreender em que medida o gerencialismo - a ideologia da gestão - está a influenciando as atividades de uma Organização Não-Governamental brasileira, a Galpão Aplauso. O estudo, usando uma estrutura teórica, analisa o relacionamento entre a ONG e seus parceiros, sublinhando os resultados de conflitos ideológicos. No geral, descobriu-se como o encontro das perspectivas do Norte e do Sul originou alguns debates que levaram, em parte, à aceitação de ideias gerencialistas, tais como a replicabilidade e sistematização de processos, enquanto que em alguns casos, eles intensificaram a resistência da ONG sobre conceitos como sustentabilidade financeira e transformação em um negócio social.

Heat flow and heat conductivity coefficient measured in bottom sediments collected in Cruise 13 of R/V Akademik Sergey Vavilov in the Pechora Sea

In Cruise 13 of R/V Akademik Sergey Vavilov in the Pechora Sea, six heat flow varied from 50 to 75 mW/m**2. Deep heat flow in the Pechora Sea was calculated equal to 45 mW/m**2, which is confirmed by results of geological and geophysical studies and corresponds to Middle Baikal age of the basement. A model of structure of the lithosphere in the Pechora Sea is suggested. Total thickness of the lithosphere in the basin (190 km) determined from geothermal data agrees well with that in transition zones from the continent to the ocean. According to estimates of deep heat flow in the region obtained, thickness of the mantle (160 km), of the basaltic (15 km), and of the granitic (15 km) layers of the lithosphere were also evaluated. Temperature values at boundaries of the sedimentary layers were calculated over a geological and geophysical profile crossing the Pechora Sea basin. Temperatures obtained agree with the temperature interval of hydrocarbon generation and correspond to Permian-Triassic sedimentary sequences, which are the most productive ones in the Pechora Sea region from the point of view of oil and gas potential.

Heavy metal contents in Fe-Mn nodules and crusts from R/V Vityaz polygons and stations in the East Indian Ocean

Regional variations in abundance, morphology, and chemical composition of Fe-Mn nodules have a zonal character. Due to circumcontinental zonality of terrigenous sedimentation the main mass of the nodules occurs in the pelagic part of the ocean, in areas of minimal sedimentation rates. In spatial variations in morphology and chemical composition of the nodules the latitudinal zonality is very clear and associated with latitudinal changes in facial conditions of sedimentation. Elevated contents of Mn, Ni, and Cu and of Mn/Fe ratio occur in nodules from the radiolarian belt. Changes of chemical composition of the nodules with depth (vertical zonality of mineralization) are confirmed. Local variations in abundance, morphology and chemical composition of the nodules are caused by ruggedness of relief and depth variations, variations in sedimentation rate, age of ore formation, intensity of diagenetic redistribution of metals.