930 resultados para 200-1224F
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本文采用氢感应法,测定低温水热条件下Pt 的H2 渗透常数k ,并可根据H2 渗透来计算实验体系的氧逸 度。这种方法无需依赖H2 在氧缓冲体系与实验体系间平衡状态的到达, 但要求有精确的氢渗透常数。本研 究在200 ℃, NNO 及HM氧缓冲的实验条件下,通过测定氢感应体系中淬火溶液Cl - 浓度的变化, 计算求得Pt 的H2 渗透常数k 为10 - 13~10 - 14数量级。并讨论了在实验及数据处理过程中对H2 渗透常数k 可能带来的误 差及影响因素。
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8 fotografías a color.
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Actualmente la influencia que tiene la tecnología en la Educación Matemática como medio facilitador tanto en el proceso de aprendizaje como en el de enseñanza de algunas temáticas de las matemáticas escolares, ha generado su inclusión en las instituciones educativas como es el caso, de las calculadoras graficadoras. No obstante, en general son varios los profesores de matemáticas que aunque cuentan con este tipo de recursos para desarrollar sus clases, se abstienen de utilizarlos porque no saben cómo ni en qué momento hacerlo. Por tanto, se presenta algunas actividades sobre ciertas temáticas de la matemática escolar en donde sea factible el uso de herramientas básicas de la calculadora.
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En este artículo se analiza la posición que ocupa Laplace en el desarrollo de la teoría clásica de la probabilidad. Se hace en el marco de los 200 años de la publicación del "Essai philosophique sur les probabilités". El artículo se divide en las siguientes secciones: en la primera se introducen algunas de las características de las matemáticas del periodo. En la segunda, se presentan algunos de los desarrollos fundamentales en la teoría de la probabilidad alcanzados durante los siglos XVII y XVIII. Finalmente, presentamos algunas de las principales contribuciones de Laplace. En general, se considera que con Laplace la teoría clásica de la probabilidad adquiere su forma definitiva.
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The census and similar sources of data have been published for two centuries so the information that they contain should provide an unparalleled insight into the changing population of Britain over this time period. To date, however, the seemingly trivial problem of changes in boundaries has seriously hampered the use of these sources as they make it impossible to create long run time series of spatially detailed data. The paper reviews methodologies that attempt to resolve this problem by using geographical information systems and areal inter-polation to allow the reallocation of data from one set of administrative units onto another. This makes it possible to examine change over time for a standard geography and thus it becomes possible to unlock the spatial detail and the temporal depth that are held in the census and in related sources.
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Urban areas are pivotal to global adaptation and mitigation efforts. But how do cities actually perform in terms of climate change response? This study sheds light on the state of urban climate change adaptation and mitigation planning across Europe. Europe is an excellent test case given its advanced environmental policies and high urbanization. We performed a detailed analysis of 200 large and medium-sized cities across 11 European countries and analysed the cities' climate change adaptation and mitigation plans. We investigate the regional distribution of plans, adaptation and mitigation foci and the extent to which planned greenhouse gas (GHG) reductions contribute to national and international climate objectives. To our knowledge, it is the first study of its kind as it does not rely on self-assessment (questionnaires or social surveys). Our results show that 35 % of European cities studied have no dedicated mitigation plan and 72 % have no adaptation plan. No city has an adaptation plan without a mitigation plan. One quarter of the cities have both an adaptation and a mitigation plan and set quantitative GHG reduction targets, but those vary extensively in scope and ambition. Furthermore, we show that if the planned actions within cities are nationally representative the 11 countries investigated would achieve a 37 % reduction in GHG emissions by 2050, translating into a 27 % reduction in GHG emissions for the EU as a whole. However, the actions would often be insufficient to reach national targets and fall short of the 80 % reduction in GHG emissions recommended to avoid global mean temperature rising by 2 °C above pre-industrial levels. © 2013 Springer Science+Business Media Dordrecht.