82,195 research outputs found
C. W. Schmidt family
No full textC. W. Schmidt family; top row, l. to r., unknown, William, George; bottom row, l. to r., unknown, Minna, Bernard, Frieda, ca. 1910https://mavmatrix.uta.edu/specialcollections_schmidtfamily/1027/thumbnail.jp
Demokratische Skizzen vom Jahre 1848 : mit dem Stahlstich: G. A. Wislicenus / herausgegeben von Gustav Rawald
No full textDie Illustration ist ein gestochenes Frontispiz von Naumburg's Kunstanstalt.Die Rückseite des Titelblatts ist unbedrucktVorlageform der Veröffentlichungsangabe: "Halle, 1849. Verlag des Verfassers und in Commission bei H. W. Schmidt." . - Kolophon: "Halle, Druck von H. W. Schmidt."1 Illustration (Stahlstich
Hortus Halensis Tam Vivus Quam Siccus Iconibus Et Descriptionibus Illustratus / A D. F. L. De Schlechtendal, Horti Directore
No full textErscheinungsbeginn: 1841Vorlage des Erscheinungsvermerks Fasc. I und II: Halis Saxonum Apud C. A. Schwetschke Et Filium. Impensis Auctoris Editum. - Vorlage des Erscheinungsvermerks Fasc. III: Halis Saxonum Apud H. W. Schmidt. Typis Expressum Schmidtii.Erschienen: Fasciculus I [1841] - Fasciculus III [1853] ; wahrsch. noch Fasciculus IV und V erschienen12 Ill (Kupferst., teilw. kolor.
Orthogonal least squares methods and their application to non-linear system identification
No full textIdentification algorithms based on the well-known linear least squares methods ofgaussian elimination, Cholesky decomposition, classical Gram-Schmidt, modifiedGram-Schmidt, Householder transformation, Givens method, and singular valuedecomposition are reviewed. The classical Gram-Schmidt, modified Gram-Schmidt,and Householder transformation algorithms are then extended to combinestructure determination, or which terms to include in the model, and parameterestimation in a very simple and efficient manner for a class of multivariablediscrete-time non-linear stochastic systems which are linear in the parameters
Trechus tilitshoensis Schmidt 1994
No full textTrechus tilitshoensis Schmidt, 1994 (Figs. 30, 42) Catalogue: Trechus tilitshoensis Schmidt, 1994: 130. Locus typicus: Central Nepal, Manang Distr., Plateau above Tilitshó Lake at N-slope of Annapurna Massif, altitude approximately 5000 m. Type material: Holotype male, with label data “NEPAL-HIMALAYA, Annapurna-N-Abfall, W-Manang, 6- 8.10.92”, “Plateau über dem Tilitschok-Lake 5000 m, lg. Schmidt”, “ HOLOTYPUS Trechus tilitshoensis des. J. Schmidt 1993” (SMTD). Paratypes: 8 males, 3 females, with same label data as holotype (CSCHM, SMTD); 10 males, 7 females, Annapurna Mts., Tilitshó Lake W Manang, 4950–5200 m, 4.VI.1993, leg. Schmidt (CSCHM); 2 males, Annapurna Mts., Thorong Pass N Manang, E slope, 4900–5200 m, 8.VI.1993, leg. Schmidt (CSCHM). Additional material: NEPAL: 8 males, 3 females, Annapurna Mts., Manang Distr., E slope Kang La Pass, 5000 m, 3.VI.1994, leg. J. Schmidt (CSCHM); 3 males, 1 female, Annapurna Mts., Yakkharka N Manang, 4500 m, 28.V.1996, leg. J. Schmidt (CSCHM); 10 males, 2 females, N Annapurna Mts., Gungdang N-slope, W Thorung Phedi, 4600–4900 m, 30.V.1996, leg. J. Schmidt (CSCHM); 24 males, 12 females, Dhaulagiri, upp. Yakkharka [place above Marpha north of Tukuche Peak], 4500–4600 m, 12.7.1998, leg. C. Berndt & J. Schmidt (CSCHM). Identification: See key above. Relationships: This species and the Western Nepalese species T. aedeagalis sp. n., T. eremita sp. n., T. franzianus Mateu & Deuve, 1979, T. muguensis sp. n., and T. sculptipennis sp. n., together forming a group of closely related species which, in external morphology, differ very slightly from each other or, in some cases are almost identical, but which evolved remarkable differences in genital morphology. Currently, based on these characters it seems impossible to determine sister species relationships. Distribution: Fig. 98. Tibetan Himalaya of Manang and Mustang Districts, Central Nepal. The species is known from several localities north of Annapurna Massif as well from the Northeast slope of Dhaulagiri Himal. Habitat: Edaphic species of the higher alpine zone; vertical distribution approximately 4900–5200 m. The specimens were found on humid, gently inclined slopes and along small depressions, often close to snow fields and melting water.Published as part of Schmidt, Joachim, 2009, Taxonomic and biogeographical review of the genus Trechus Clairville, 1806, from the Tibetan Himalaya and the southern central Tibetan Plateau (Coleoptera: Carabidae: Trechini) 2178, pp. 1-72 in Zootaxa 2178 (1) on pages 25-26, DOI: 10.11646/zootaxa.2178.1.1, http://zenodo.org/record/531227
Charles W. Schmidt
No full textCharles “Chuck” W. Schmidt was born in New York City on March 18, 1928. He earned his undergraduate degree in Chemistry from Williams College before moving on to do his graduate work at Carnegie Technical institute and the Advanced Management Program at Harvard University.
Schmidt’s professional career in the paper industry began when he joined S. D. Warren Co. as an apprentice salesperson in 1948. Two years later, he became District Manager in Rochester, N.Y., a position he held until 1952. From this position, he moved to the West Coast, then Philadelphia territories before going to Boston as Assistant Sales Manager. Schmidt was promoted to Vice President of Sales before advancing to the position of President in 1972, after S. D. Warren became a division of Scott Paper Company.
After 33 years with S. D. Warren and Scott Paper, in 1983 Schmidt departed to become President and Chief Executive Officer of SCA Services, Inc. At the time the third largest but scandal-ridden, U.S.-based waste management company. Under attack by corporate takeover bids, Schmidt arranged a $423.2 million dollar sale of the company in a 60/40 split between Waste Management Inc. and Genstar Corporation, a financial services, building supplies, and real estate company.
Following the sale of SCA Services, Inc., Schmidt went on to become the first Executive-in-Residence of Babson College in January 1985. He was also named a full professor, lecturing on the mission of business management. The college presented him with an Honorary doctorate. The following June, Schmidt was elected Senior Vice President and Group Executive of Raytheon, Co. of Lexington, Massachusetts. He retired from Raytheon at the end of 1990.
Schmidt’s association with the UMaine Pulp and Paper Foundation began in 1973 when he was elected as a director. In 1975 he served as Vice President and between 1979 and 1981, as President. Schmidt established the William C. Schmidt & William C. Schmidt, Jr. Named Scholarship Fund in honor of his father and elder brother, Ensign W. C. Schmidt, Jr. who was killed in the Pacific Theater of World War II on Nov. 24, 1943.
Chuck Schmidt died at his home in West Tisbury, Massachusetts on September 25, 2018.https://digitalcommons.library.umaine.edu/ppf_images/1020/thumbnail.jp
Schmidt, Fred W. (Birth, 1884-04-15)
No full textAddress: 26 Woodward St.1956/Pg 194/1884/M W/Mrs C. Beekel,Mid.Original record filed in drawer labeled 'SCHMERR-SCHMIDT'
Synthesis and characterization of derivatives of a chelating aluminum dichloride complex containing a 3,5-di-tert-butylpyrazolato unit
No full textThe chelating aluminum complex [{3,5-N-tBu(2)pz-N'-CH = C(SiMe3)}AIR(1)R(2)] [R-1 = R-2 = Me (2); R-1 = R-2 = H (3); R-1 = R-2 = 1 (4)] was prepared in modest yield from an organoaluminum dichloride precursor [{3,5-N-tBu(2)pz-N'-CH = C(SiMe3))AlCl2] (1). Compounds 2 and 3 were obtained from the reaction of 1 with MeLi in Et2O or with LiAlH4 in THF, respectively. Reaction of 2 or 3 with I-2 in toluene gave 4. In addition, the reaction of 1 with two equivalents of water yielded the hydrolyzed product H[3,5-N-tBu(2)pz-N'-CH = C(SiMe3)] (5). All compounds were characterized by elemental analysis, NMR spectroscopy, and mass spectrometry. The X-ray structure analysis shows that complex 2 exhibits one fused five-membered AlC2N2 ring and one pyrazolate ring system
Experimental subsolidus studies on epidote minerals
No full textDespite the fact that epidote group minerals are very typical for metamorphism at very low pressure, e.g., in geothermal fields (Bird and Spieler 2004), the first successful synthesis of zoisite and epidotess was reported by Coes (1955) in a paper in the Journal of American Ceramic Society entitled “High pressure minerals.” Synthesis conditions were 1 GPa at 800°C; zoisite was obtained from a mixture of kaolin, SiO2, CaO, and CaCl2, whereas epidote was formed by adding FeCl2·H2O to the previous mixture. Once experimental facilities enabled pressures exceeding a few hundred MPa, zoisite and epidote minerals were easily obtained from a variety of starting materials, made of oxides, gels and glasses.
Historically, early experimental studies on epidote focused on the formation at low pressure conditions, and then ventured into the simple system CaO-Al2O3-SiO2-H2O at conditions attainable by piston cylinder equipment (Newton and Kennedy 1963; Boettcher 1970) in which zoisite was found to have an extremely large temperature stability. Then, the role of Fe3+ was investigated systematically at pressures typical for the middle and lower continental crust (Holdaway 1972; Liou 1973). Epidote minerals in bulk compositions directly applicable to natural rocks were not investigated experimentally until the early 70’s (Liou et al. 1974; Apted and Liou 1983). Subsequent studies in the context of the very popular hydrous phase stabilities at subduction conditions in the 90’s extended the experimentally determined stability of epidotess in natural compositions to 3.5 GPa. With the relatively easy access to multi-anvil machines, the pressure stability of zoisite was defined (Poli and Schmidt 1998).
The increasing number of experimental studies on epidote minerals reveals that the members of this group of ubiquitous rock forming minerals have huge stability fields, which extend to 7 GPa in pressure and to more than 1200°C in temperature. However, most of the experimental studies were performed at subsolidus conditions, thus melting relations are still partially unknown.
In this chapter we focus on experimental studies in the subsolidus performed both on simplified model systems and on natural (or close to natural) rock compositions where epidotess is described by the components (clino)zoisite and epidote. Experimental investigations clarifying the role of epidote in magmatic systems are discussed in Schmidt and Poli (2004). Experimental studies on Mn bearing epidote minerals are presented by Bonazzi and Menchetti (2004), those on REE bearing allanite by Gieré and Sorensen (2004).
Unless differently stated the term epidotess employed in this chapter is intended to describe epidote mineral compositions along the pseudobinary join (clino)zoisite-epidote
Schmidt, Carl C. (Birth, 1907-07-18)
No full textAddress: 536 Dandridge St.3877/Pg. 140/1907/M W/Cinti, Ohio/Cinti, Ohio/Dr. C. C. FiheOriginal record filed in drawer labeled 'SCHMERR-SCHMIDT'
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