989 resultados para 820[71]-1


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The title compound, C21H33N3O3, is a tri-substituted cyclo­hex­yloxy triazine. In the crystal, the triazine rings form (C3i-PU) Piedfort units. The inter-centroid distance of the [pi]-[pi] inter­action involving the triazine rings is 3.3914 (10) Å. In the crystal, mol­ecules are linked by C-H...O hydrogen bonds, forming ribbons propagating along [1-10]. There are also weak C-H...N and C-H...O contacts present, linking inversion-related ribbons, forming a three-dimensional structure.

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Welsch (Projektbearbeiter): Aufruf von 14 Urwählern des Berliner 71. Bezirks, nur solche Wahlmänner zu wählen, die den Staatsstreich des 9. November 1848 (Verlegung der Nationalversammlung nach Brandenburg) wieder rückgängig machen und eine Verfassung schaffen, welche im Unterschied zu der vom 5. Dezember 1848 kein Gnadengeschenk darstellt

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BACKGROUND The purpose of this clinical study was to assess the prevalence of acidic oral mucosal lesions and periodontal conditions in patients suffering from erosive esophageal reflux disease (ERD) compared with non erosive esophageal reflux disease (NERD) patients, both treated with long term proton pump inhibitors (PPI). METHODS Seventy-one patients with diagnosed GERD were studied: i.e. 29 ERD and 42 NERD patients. Thorough visual examination of the oral mucosa and a periodontal evaluation was performed. The primary outcome was defined as a statistically significant difference, between the two groups, in the presence of acidic lesions of the oral mucosa and specific periodontal parameters. RESULTS This study failed to demonstrate statistically significant differences between ERD and NERD patients with respect to the prevalence of oral mucosal lesions. However, significantly more ERD patients suffered from severe periodontitis (CAL ≥ 5 mm) as compared to NERD patients. Accordingly, it may be assumed that PPI-use had no adverse effects on the prevalence of acidic oral mucosal lesions and on periodontal destruction. CONCLUSIONS Within the limitations of this study it may be concluded that ERD and NERD patients need separate evaluation with respect to periodontal destruction. Moreover, long term PPI medication had no adverse clinical impact on acidic oral mucosal lesions and periodontal destruction. Further studies are necessary to elucidate the role of reflux in the periodontal destruction of ERD individuals.

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BACKGROUND HIV-1 RNA viral load (VL) testing is recommended to monitor antiretroviral therapy (ART) but not available in many resource-limited settings. We developed and validated CD4-based risk charts to guide targeted VL testing. METHODS We modeled the probability of virologic failure up to 5 years of ART based on current and baseline CD4 counts, developed decision rules for targeted VL testing of 10%, 20%, or 40% of patients in 7 cohorts of patients starting ART in South Africa, and plotted cutoffs for VL testing on colour-coded risk charts. We assessed the accuracy of risk chart-guided VL testing to detect virologic failure in validation cohorts from South Africa, Zambia, and the Asia-Pacific. RESULTS In total, 31,450 adult patients were included in the derivation and 25,294 patients in the validation cohorts. Positive predictive values increased with the percentage of patients tested: from 79% (10% tested) to 98% (40% tested) in the South African cohort, from 64% to 93% in the Zambian cohort, and from 73% to 96% in the Asia-Pacific cohort. Corresponding increases in sensitivity were from 35% to 68% in South Africa, from 55% to 82% in Zambia, and from 37% to 71% in Asia-Pacific. The area under the receiver operating curve increased from 0.75 to 0.91 in South Africa, from 0.76 to 0.91 in Zambia, and from 0.77 to 0.92 in Asia-Pacific. CONCLUSIONS CD4-based risk charts with optimal cutoffs for targeted VL testing maybe useful to monitor ART in settings where VL capacity is limited.

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2 Briefe zwischen Marga Wadsack und Max Horkheimer, 24.08.1937, 29.08.1937; 1 Brief von Gloria H. Wagner an Max Horkheimer, 27.12.1948; 1 Brief von Herta Wagner an Leo Löwenthal, 05.06.1936; 3 Brief und 1 Beilage zwischen Herta Wagner, 12.03.1936, 1936; 8 Brief zwischen Katja Walch-Lux und Max Horkheimer, 1934-1938; 2 Brief zwischen K. Walcher und Max Horkheimer, 07.08.1936, 04.09.1936 sowie Bemerkungen zum Brief von Max Horkheimer; 2 Briefe zwischen Morris Waldman und Max Horkheimer, 17.04.1940, 11.05.1940; 6 Briefe zwischen Sidney Wallach und Max Horkheimer, 1940; 2 Briefe von Max Horkheimer an Waldman; 2 Briefe von Max Horkheimer an Landau; 1 Brief Max Horkheimer an Warburg; 1 Brief von Hans Wallenberg an Leo Löwenthal, 06.05.1940; 1 Brief von Willard W. Waller an Franz Neumann, 28.04.1941; 2 Briefe und 1 Beilage zwischen Hans Waloschek und Max Horkheimer, 04.08.1938, 31.08.1938; 4 Briefe und 2 Beilagen zwischen Emil J. Walter und Max Horkheimer, 1937, 1938; 5 Briefe und 1 Beilage zwischen Hilde Walter und Max Horkheimer, 1937, 1945; 1 Brief von Rose Walter an Max Horkheimer, 16.11.1938; 2 Briefe zwischen Yu-Chuan Wang und Max Horkheimer, 12.10.1936, 09.12.1936; 1 Brief von Rike Wankmüller-Freyh an Max Horkheimer, 06.07.1949; 1 Brief von Ilse Bach an Heinz Wartenberg, 11.11.1940; 1 Brief von Heinz Wartenberg an Richard Bach, 07.02.1941; 1 Brief von Max Horkheimer an Heinz Wartenberg, 11.03.1941; 1 Brief von Richard Bach an Max Horkheimer; 1 Brief von Franz und Hilde Wasem an Max Horkheimer, 16.02.1949; 5 Briefe zwischen Goodwin Watson und Franz Neumann, 1941; 11 Briefe und Notizen zwischen Julien Wavrinek und Max Horkheimer, 1938-1940; 1 Brief von Max Horkheimer an M. Bruhat; 2 Briefe von Max Horkheimer an Walter Benjamin, 03.05.1940;

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veröffentlicht in: Schopenhauer, Arthur : Arthur Schopenhauers sämtliche Werke - München : Piper - Bd. 15 : Der Briefwechsel Arthur Schopenhauers ; 2 (1849 - 1860), Nr. 747

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veröffentlicht in: Schopenhauer, Arthur : Arthur Schopenhauers sämtliche Werke - München : Piper - Bd. 15 : Der Briefwechsel Arthur Schopenhauers ; 2 (1849 - 1860), Nr. 732

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Bottom morphology of the Jan Mayen transform fracture zone and rock chemistry data show that petrological and chemical specific features of igneous rocks can result from higher permeability of the transform fracture zone and deeper penetration of ocean water into the lithosphere in comparison with rift zones of the Kolbeinsey and Mohn's mid-ocean ridges. Age of alkaline magmatism of the Jan Mayen fracture zone is similar to that of rift zones due to palingenesis of metamorphosed and hydrated mantle and crustal rocks.

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A comparison of 50 basalts recovered at Sites 706, 707, 713, and 715 along the Reunion hotspot trace during Ocean Drilling Program Leg 115 in the Indian Ocean shows that seafloor alteration had little effect on noble metal concentrations (Au, Pd, Pt, Rh, Ru, and Ir), determined by inductively coupled plasma-mass spectrometry (ICP-MS), which generally tend to decrease with magma evolution. Their compatible-element behavior may be related to the precipitation of Ir-Os-based alloys, chromite, sulfides, and/or olivine and clinopyroxene in some combination. The simplest explanation indicates silicate control of concentrations during differentiation. Basalts from the different sites show varying degrees of alkalinity. Noble metal abundances tend to increase with decreasing basalt alkalinity (i.e., with increasing percentages of mantle melting), indicating that the metals behave as compatible elements during mantle melting. The retention of low-melting-point Au, Pd, and Rh in mantle sulfides, which mostly dissolve before significant proportions of Ir-Os-based alloys melt, explains increasing Pd/Ir ratios with decreasing alkalinity (increasing melting percentages) in oceanic basalts. High noble metal concentrations in Indian Ocean basalts (weighted averages of Au, Pd, Rh, Pt, Ru, and Ir in Leg 115 basalts are 3.2, 8.1, 0.31, 7.3, 0.22, and 0.11 ppb, respectively), compared with basalts from some other ocean basins, may reflect fundamental primary variations in upper- mantle noble metal abundances