934 resultados para ADDITIONS
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بسم الله الرحمن الرحيم اللهم انا نحمدك على ما علمت في البيان والهمت في البيان كما نحمدك على ما مبعت في الغطا... :Incipit
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Title from inside cover in a later handscript.
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A biographical dictionary of sufis.
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Local paper. Beginning and end folios in brittle and poor condition, several folios repaired, many folios water-stained.
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This article systematically scrutinizes the intergovernmental and administrative aspects of Franco- German relations with the 1963 Elysée Treaty at their core. This treaty, together with its various additions and extensions, has defined the basic processes of bilateral interaction between the French and German states. Recurrent tension in Franco-German relations notwithstanding, many observers and participants have viewed France and Germany to be connected particularly closely since the 1960s. This article explores key elements of what it is that links France and Germany. Thereby it clarifies the concept of regularized intergovernmentalism, suggests viewing this specific set of international practices from a social-structural perspective, and evaluates the effects and limits of such regularized procedures. Its findings suggest that bilateral structures have complemented and undergirded a broadly multilateral post-World War II world and are likely to continue to do.
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kdens produces univariate kernel density estimates and graphs the result. kdens supplements official Stata's kdensity. Important additions are: adaptive (i.e. variable bandwidth) kernel density estimation, several automatic bandwidth selectors including the Sheather-Jones plug-in estimator, pointwise variability bands and confidence intervals, boundary correction for variables with bounded domain, fast binned approximation estimation. Note that the moremata package, also available from SSC, is required.
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The speciation of strongly chelated iron during the 22-day course of an iron enrichment experiment in the Atlantic sector of the Southern Ocean deviates strongly from ambient natural waters. Three iron additions (ferrous sulfate solution) were conducted, resulting in elevated dissolved iron concentrations (Nishioka, J., Takeda, S., de Baar, H.J.W., Croot, P.L., Boye, M., Laan, P., Timmermans, K.R., 2005, Changes in the concentration of iron in different size fractions during an iron enrichment experiment in the open Southern Ocean. Marine Chemistry, doi:10.1016/j.marchem.2004.06.040) and significant Fe(II) levels (Croot, P.L., Laan, P., Nishioka, J., Strass, V., Cisewski, B., Boye, M., Timmermans, K.R., Bellerby, R.G., Goldson, L., Nightingale, P., de Baar, H.J.W., 2005, Spatial and Temporal distribution of Fe(II) and H2O2 during EisenEx, an open ocean mescoscale iron enrichment. Marine Chemistry, doi:10.1016/j.marchem.2004.06.041). Repeated vertical profiles for dissolved (filtrate < 0.2 µm) Fe(III)-binding ligands indicated a production of chelators in the upper water column induced by iron fertilizations. Abiotic processes (chemical reactions) and an inductive biologically mediated mechanism were the likely sources of the dissolved ligands which existed either as inorganic amorphous phases and/or as strong organic chelators. Discrete analysis on ultra-filtered samples (< 200 kDa) suggested that the produced ligands would be principally colloidal in size (> 200 kDa-< 0.2 µm), as opposed to the soluble fraction (< 200 kDa) which dominated prior to the iron infusions. Yet these colloidal ligands would exist in a more transient nature than soluble ligands which may have a longer residence time. The production of dissolved Fe-chelators was generally smaller than the overall increase in dissolved iron in the surface infused mixed layer, leaving a fraction (about 13-40%) of dissolved Fe not bound by these dissolved Fe-chelators. It is suggested that this fraction would be inorganic colloids. The unexpected persistence of such high inorganic colloids concentrations above inorganic Fe-solubility limits illustrates the peculiar features of the chemical iron cycling in these waters. Obviously, the artificial about hundred-fold increase of overall Fe levels by addition of dissolved inorganic Fe(II) ions yields a major disruption of the natural physical-chemical abundances and reactivity of Fe in seawater. Hence the ensuing responses of the plankton ecosystem, while in itself significant, are not necessarily representative for a natural enrichment, for example by dry or wet deposition of aeolian dust. Ultimately, the temporal changes of the Fe(III)-binding ligand and iron concentrations were dominated by the mixing events that occurred during EISENEX, with storms leading to more than an order of magnitude dilution of the dissolved ligands and iron concentrations. This had strongest impact on the colloidal size class (> 200 kDa-< 0.2 µm) where a dramatic decrease of both the colloidal ligand and the colloidal iron levels (Nishioka, J., Takeda, S., de Baar, H.J.W., Croot, P.L., Boye, M., Laan, P., Timmermans, K.R., 2005, Changes in the concentration of iron in different size fractions during an iron enrichment experiment in the open Southern Ocean. Marine Chemistry, doi:10.1016/j.marchem.2004.06.040) was observed.
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When this image was taken this building was a hospital. Built 1840. Professors' Houses (East Residence) 1840-1868. University Hospital 1868-1891. Additions in 1877 and after in the form of two parallel wings built out from back of house and several additions onto them. Dental College 1891-1908. Building removed 1908. Replaced by new Chemistry Building 1910
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Built 1840. Professors' Houses (East Residence) 1840-1868. University Hospital 1868-1891. Additions in 1877 and after in the form of two parallel wings built out from back of house and several additions onto them. Dental College 1891-1908. Building removed 1908. Replaced by new Chemistry Building 1910On verso in two hands: (1) Looking at 2 prof. houses at this time both converted into a) Univ. Hosp. & b) Homeo. [Homeopathic] School (2) R.C. Smith.
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When this image was taken this building was a hospital. Built 1840. Professors' Houses (East Residence) 1840-1868. University Hospital 1868-1891. Additions in 1877 and after in the form of two parallel wings built out from back of house and several additions onto them. Dental College 1891-1908. Building removed 1908. Replaced by new Chemistry Building 1910
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View from the east. Built 1840. Professors' Houses (East Residence) 1840-1868. University Hospital 1868-1891. Additions in 1877 and after in the form of two parallel wings built out from back of house and several additions onto them. Dental College 1891-1908. Building removed 1908. Replaced by new Chemistry Building 1910
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Built 1840. Professors' Houses (East Residence) 1840-1868. University Hospital 1868-1891. Additions in 1877 and after in the form of two parallel wings built out from back of house and several additions onto them. Dental College 1891-1908. Building removed 1908. Replaced by new Chemistry Building 1910. On verso: Photographed in 1887 by A.L. Colton of '89
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Built 1840. Professors' Houses (East Residence) 1840-1868. University Hospital 1868-1891. Additions in 1877 and after in the form of two parallel wings built out from back of house and several additions onto them. Dental College 1891-1908. Building removed 1908. Replaced by new Chemistry Building 1910. On verso: Photographed in 1887 by A.L. Colton of '89
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Built 1840. Professors' Houses (East Residence) 1840-1868. University Hospital 1868-1891. Additions in 1877 and after in the form of two parallel wings built out from back of house and several additions onto them. Dental College 1891-1908. Building removed 1908. Replaced by new Chemistry Building 1910
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Built 1840. Professors' Houses (East Residence) 1840-1868. University Hospital 1868-1891. Additions in 1877 and after in the form of twoparallel wings built out from back of house and several additions onto them. Dental College 1891-1908. Building removed 1908. Replaced by new Chemistry Building 1910. On verso: Randall '76. 220 Woodward Avenue. Detroit, Mich.