14,468 research outputs found
Der grösste Gewünn eines frommen Christen : nach Anleitung der Worten des Apostels I. Tim. VI. V
No full textin einer erbaulichen, den 15. Christm. 1695 zu Genf in St. Peters Kirch von Hr. Alphonso Turretin, D. am W.G., gehaltner Predig vorgestellet ; jezund aber zu mehrerer Erbauung in das Teutsche übersezet von H.G. K. u. Sch.D.Dedikation von Joh. Wilhelm Simler an David Hess, Caspar Hess, Heinrich Hess, Ursula Hirzel-Hess, Ludwig Hirzel, Dorothea Escher-Hess und Joh. Jacob Escher auf S. 2Titelvignett
Communication circuits : analyaio and design. By Kenneth K? Clarke and Donald T. Hess.
No full textClarke (Kenneth K)& G-US 656 Hess (Donald T) . K.S.1
Corrections to the capacitance between two electrodes due to the presence of quantum confined system
No full textWe have studied the capacitance between two parallel plates enclosing a quantum confined system and its dependence on the applied voltage. The concepts of capacitance and differential capacitance are discussed together with their applicability to systems characterized by single-electron tunneling. We determine the tunneling thresholds by means of a formalism based on the minimization of the system free energy and we retrieve, as a special case, Luryi's quantum capacitance formula. We apply our method to the study of an idealized system made up of a number of quantum dots with random size distributed according to a gaussian, Results are shown for different choices of the position of the dots between the plates and of the voltage span applied to perform the measurement of the differential capacitance
Numerical simulation of capacitance spectroscopy for multiple vertically stacked quantum dots
No full text
Flora Louise Hess Property
No full textEntry created by John H. Herrick January 7, 1974.John H. Herrick Archives: Documenting Structures at The Ohio State UniversityThe University Archives has determined that this item is of continuing value to OSU's history.The Flora Louise Hess Property was located at 2637 and 2703 Olentangy River Road. This property was never officially named by Board of Trustees action. It was purchased from Flora Louise and Elizabeth H. Hess. The author has never heard it referred to as anything, but the "Flora Louise Hess" property
Viscosities of granitic (sensu lato) melts: influence of the anorthite component
No full textThe viscosities of a series of granitic (sensu lato) melts have been determined in the range of 103 to 1012 Pa·s. The anhydrous melt compositions are based on the addition of 10, 20, 50, and 75 wt% of the anorthite component (CaAl2Si2O8) to a haplogranitic melt (HPG8) whose composition lies near
the 2 kbar water-saturated minimum melt composition in the system NaAlSi3O8-KAlSi3O8-SiO2. Melts with 10 and 20 wt% normative anorthite were subjected to high-pressure hydration syntheses using a piston-cylinder apparatus to generate water contents up to 2 wt%. Viscosities were determined for the anhydrous melts using the concentric cylinder method in the viscosity range of 102 to
105 Pa·s, and for both anhydrous and hydrated melts in the range of 109 to 1012 Pa·s. The results for the temperature dependence of viscosity in the anhydrous system indicate that the
influence on melt viscosity, caused by the addition of normative anorthite to the haplogranitic melt
composition, is strongly temperature-dependent. Viscosity-temperature relationships of the melts
become much more non-Arrhenian with addition of normative anorthite. The addition of water to
melts with 10 and 20 wt% normative anorthite results in strong nonlinear decreases in viscosity. In the high viscosity range, the results for hydrous melts with 10% normative anorthite are adequately reproduced using the calcalkaline melt viscosity model of Hess and Dingwell (1996), whereas those
for hydrous melts with 20 wt% normative anorthite are higher than the model predictions by amounts
that depend on the water content. It appears that, at the higher temperatures anticipated for intermediate
granitic magmatism, the calcalkaline model can adequately deal with up to 15 wt% normative anorthite in the melt composition in the range of temperatures relevant for intermediate magmas in nature
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