Der deutsche Militarismus in seiner Bedeutung für die menschliche Kultur

Georg Bonne

Natural and anthropogenic methane fluxes in Eurasia: a mesoscale quantification by generalized atmospheric inversion

Eight surface observation sites providing quasi-continuous measurements of atmospheric methane mixingratios have been operated since the mid-2000’s in Siberia. For the first time in a single work, we assimilate 1 year of these in situ observations in an atmospheric inversion. Our objective is to quantify methane surface fluxes from anthropogenic and wetland sources at the mesoscale in the Siberian lowlands for the year 2010. To do so, we first inquire about the way the inversion uses the observations and the way the fluxes are constrained by the observation sites. As atmospheric inver- sions at the mesoscale suffer from mis-quantified sources of uncertainties, we follow recent innovations in inversion techniques and use a new inversion approach which quantifies the uncertainties more objectively than the previous inversion systems. We find that, due to errors in the representation of the atmospheric transport and redundant pieces of information, only one observation every few days is found valuable by the inversion. The remaining high-resolution quasi-continuous signal is representative of very local emission patterns difficult to analyse with a mesoscale system. An analysis of the use of information by the inversion also reveals that the observation sites constrain methane emissions within a radius of 500 km. More observation sites than the ones currently in operation are then necessary to constrain the whole Siberian lowlands. Still, the fluxes within the constrained areas are quantified with objectified uncertainties. Finally, the tolerance intervals for posterior methane fluxes are of roughly 20 % (resp. 50 %) of the fluxes for anthropogenic (resp. wetland) sources. About 50–70 % of Siberian lowlands emissions are constrained by the inversion on average on an annual basis. Extrapolating the figures on the constrained areas to the whole Siberian lowlands, we find a regional methane budget of 5–28 TgCH4 for the year 2010, i.e. 1–5 % of the global methane emissions. As very few in situ observations are available in the region of interest, observations of methane total columns from the Greenhouse Gas Observing SATellite (GOSAT) are tentatively used for the evaluation of the inversion results, but they exhibit only a marginal signal from the fluxes within the region of interest.

La duchesse d'Enville à Genève, une aristocrate chez les Républicains

Admiratrice de Tronchin, la duchesse d'Enville se rend plusieurs fois à Genève pour de longs séjours. Elle y fréquente toute la bonne société. Et manifestement, elle y apprend à s'intéresser à la politique, à cause des troubles de la cité, qu'elle observe en personne en 1765-1766 et, par l'intermédiaire de ses amis genevois, au début des années 1780. Cette expérience lui a-t-elle servi au début de la révolution française, à l'époque où son salon sert de lieu de rivalité aux Jacobins ?

Zum Projekt der Industriebank

Alfred Bonne

Die Wirtschaftslage in Palästina seit 1933

Alfred Bonne

[Rezension]

Alfred Bonne

Manejo de suelo mediante coberturas vegetales establecidas

El objetivo de esta investigación fue determinar los efectos de las coberturas vegetales en el microclima de la planta de vid. Se compararon cinco coberturas de diferente ciclo vegetativo con respecto al manejo de suelo sin labranza mediante aplicación de herbicidas. El estudio se desarrolló en un viñedo cv. Malbec conducido en espaldera alta, situado en Agrelo, Luján de Cuyo, Mendoza, Argentina. Se determinaron parámetros microclimáticos, temperatura, humedad relativa y radiación a nivel de racimos, temperatura del suelo, cantidad y calidad de la radiación reflejada por la cobertura. También se midió la expresión vegetativa y de uvas y el potencial enológico. Se verificó una significativa disminución de la radiación fotosintéticamente activa (RFA) reflejada por las coberturas con una menor relación “Rojo/Rojo lejano" comparada con el suelo descubierto. Sin embargo, el efecto no se percibió dentro de la canopia debido a que las coberturas permanentes de trébol rojo (Trifolium pratensis) y agropiro alargado (Agropyron elongatum) restringieron el vigor de las cepas, disminuyendo el crecimiento de brotes y el tamaño de hojas, lo cual se tradujo en una mayor recepción directa de la RFA a nivel de racimos. No hubo una significativa variación en cuanto a temperatura máxima, mínima y amplitud térmica a nivel de racimos. No obstante ello, los tratamientos con mayor cobertura de suelo tendieron a reducir levemente la temperatura mínima a nivel de racimos. La humedad relativa en la canopia no fue significativamente afectada. El trébol rojo, el agropiro alargado, la mezcla centeno-cebadilla (Secale cereale-Bromus catharticus) y el sorgo del Sudán (Sorghum sudanensis) redujeron notablemente la amplitud térmica del suelo. El efecto fue determinado principalmente por la disminución de la temperatura máxima. Las coberturas vegetales con alguna dificultad para desarrollarse durante su ciclo vegetativo tuvieron un comportamiento intermedio o uno muy similar al de un suelo descubierto. La introducción de una cobertura permanente con buena invasión del sitio interfilar permitió modificar indirectamente las características microclimáticas de la canopia, a través del control del crecimiento vegetativo y de los rendimientos de la planta de vid, modificando el equilibrio vigor / producción del viñedo, y por lo tanto la composición de las uvas y del vino elaborado.

València (regne). Mapas generales

Escala en el ángulo superior derecho expresada en varias unidades

València (regne). Mapas generales

Escala en el ángulo superior derecho expresada en varias unidades

Direito de retenção e seus limites

Diante da necessidade de atualização do estudo relativo ao direito de retenção, uma vez que as grandes obras doutrinárias estrangeiras e nacionais acerca do tema datam do final do século XIX e do início do século XX, abordaram-se as principais controvérsias relativas ao jus retentionis à luz da atual codificação a fim de concluir-se se o instituto ainda encontra justificativa em nosso ordenamento, bem como se seria admitido tal qual concebido em suas origens. Para tanto, procurou-se definir o que entendemos por direito de retenção, delimitando seu campo de atuação, suas características, seus elementos e sua natureza jurídica. Ao longo do estudo, analisou-se essa figura à luz do Código Civil de 2002 e do atual estágio da jurisprudência, concluindo que a previsão legislativa do instituto ainda se justifica, porém merece reforma. Ademais, conclui-se que os limites rígidos em que concebido o direito de retenção devem ser flexibilizados em atenção aos princípios da função social da posse e da boa-fé objetiva para admitir-se a utilização do bem retido em alguns casos.

Valoración energética de subproductos de palmera datilera

Este trabajo se integra en el marco de un estudio de valoración energética de subproductos obtenidos de la palmera datilera, disponibles en grandes cantidades y que actualmente no se valorizan. El objetivo principal de este trabajo consiste en evaluar los subproductos de la palmera datilera, y en concreto, estudiar el poder calorífico superior de las principales especies presentes en los oasis, y en obtener, mediante pirolisis de estos subproductos, carbón activo, y de esta al forma valorar residuos, obtener un aprovechamiento económico secundario, al mismo tiempo que estamos valorando estos residuos. El estudio se realiza sobre siete especies arbóreas, entre ellas cinco variedades de palmera datiliera, y en concreto sobre un único subproducto. Los resultados de estas pruebas permitieron poner de manifiesto que el Poder Calorífico de las especies que habitan los oasis es más importante que el de las otras especies arbóreas. El residuo sólido se obtiene de la madera de la parte inferior del árbol que se llama (Kornaf), activada a una temperatura de 700 °C utilizando el vapor de agua como agente de activación. Se estudió la calidad del carbón activo obtenido, mediante el cálculo de su superficie específica, y resultó de buena calidad (1050m2/g).

Coasts, Mediterranean Sea Region, 1763 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Carte de la mer Méditerranée : appuyée sur les observations astronomiques, combinées avec les itinéraires anciens et modernes, par M. Bonne, Mtre. de Mathemat., Membre de la Société litéraire militaire, Ingénieur-Géographe. It was published by Chez Lattré in 1763. Scale [ca. 1:6,000,000]. Covers Mediterranean Sea region, part of the Black Sea, and coasts of Europe, North Africa, and the Middle East. Map in French.The image inside the map neatline is georeferenced to the surface of the earth and fit to the World Miller Cylindrical projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, shoreline features, and more.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Western Hemisphere, 1740 (Image 1 of 2) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Carte nouvelle de la mer du Sud : dressée par ordre des principaux directeurs & tirée des memoires les plus recents et des relations des navigateurs les plus modernes, tant de France, que d'Espagne l'on ÿa joint, diverses remarques curieuses par raport aux decouvertes des graduations des manierres du pais que de la navigation. It was published by Donné au public, par And. & Henry de Leth ... sur le Pont de la Bourse au Pescheur ca. 1740. Scale [ca. 1:30,000,000]. Covers the Pacific and Atlantic oceans, and the Americas, with parts of Asia, Australia, Europe, and Africa. This layer is image 1 of 2 total images of the two sheet source map representing the western portion of the map. Text in French, Dutch, and Latin. The image inside the map neatline is georeferenced to the surface of the earth and fit to the 'Mercator' projection. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. Note: The central meridian of this map is not the same as the Prime Meridian and may wrap the International Date Line or overlap itself when displayed in GIS software. This map shows features such as drainage, cities and other human settlements, territorial boundaries, shoreline features, and more. Relief is shown pictorially. Includes historical and cultural notes, view of "Fort au Cap de Bonne Esperance," and other ill. Insets: Vera-cruz -- Baye de Rio Janeiro -- La Havane ... -- Le Detroit de Gibaltar -- La ville de Mexico -- Istme de Panama ou de Darien -- Baye de Porto Bello. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection and the Harvard University Library as part of the Open Collections Program at Harvard University project: Organizing Our World: Sponsored Exploration and Scientific Discovery in the Modern Age. Maps selected for the project correspond to various expeditions and represent a range of regions, originators, ground condition dates, scales, and purposes.

Western Hemisphere, 1740 (Image 2 of 2) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Carte nouvelle de la mer du Sud : dressée par ordre des principaux directeurs & tirée des memoires les plus recents et des relations des navigateurs les plus modernes, tant de France, que d'Espagne l'on ÿa joint, diverses remarques curieuses par raport aux decouvertes des graduations des manierres du pais que de la navigation. It was published by Donné au public, par And. & Henry de Leth ... sur le Pont de la Bourse au Pescheur ca. 1740. Scale [ca. 1:30,000,000]. Covers the Pacific and Atlantic oceans, and the Americas, with parts of Asia, Australia, Europe, and Africa. This layer is image 2 of 2 total images of the two sheet source map representing the eastern portion of the map. Text in French, Dutch, and Latin. The image inside the map neatline is georeferenced to the surface of the earth and fit to a non-standard 'Mercator' projection with the central meridian at 172.66600 degrees west. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. Note: The central meridian of this map is not the same as the Prime Meridian and may wrap the International Date Line or overlap itself when displayed in GIS software. This map shows features such as drainage, cities and other human settlements, territorial boundaries, shoreline features, and more. Relief is shown pictorially. Includes historical and cultural notes, view of "Fort au Cap de Bonne Esperance," and other ill. Insets: Vera-cruz -- Baye de Rio Janeiro -- La Havane ... -- Le Detroit de Gibaltar -- La ville de Mexico -- Istme de Panama ou de Darien -- Baye de Porto Bello. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection and the Harvard University Library as part of the Open Collections Program at Harvard University project: Organizing Our World: Sponsored Exploration and Scientific Discovery in the Modern Age. Maps selected for the project correspond to various expeditions and represent a range of regions, originators, ground condition dates, scales, and purposes.

Cape Town, South Africa, 1770 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Plan de la ville du Cap de Bonne Esperance et environs, par M.B.C.T. en Décembre 1770 ; Croisey sc. It was published in 1770. Scale [ca. 1:24,360]. Covers Cape Town, South Africa. Map in French. The image inside the map neatline is georeferenced to the surface of the earth and fit to the 'WGS 1984 UTM 34S' coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, built-up areas and selected buildings, fortification, ground cover, and more. Relief shown by hachures. Depths shown by soundings. Includes index. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.