Laternenlied: Mit Feuer: 1. Sie ler-nen nichts, sie ler-nen nichts die Herrn Hochwohl-ge-bo-ren! Ver-geb-lich schmettert des Ge-richts Po-sau-ne ih-ren Oh-ren ...

Welsch (Projektbearbeiter): Abdruck eines Revolutionsliedes (nach dem Vorbild des französischen 'Ça ira' von 1789): "Weil denn die Herrn vom bes-sern Blut die neu-e Zeit nicht ler-nen: drum hängt die Herren kurz und gut ... hoch, hoch an die La-ter-nen!" Vgl. dazu Dunder, W. G.: Denkschrift über die Wiener October-Revolution; Wien 1849 S. 36: "Dieses Gedicht erschien abgedruckt im politischen Studenten-Courier vom 4. October [1848], Nr. 91, redigirt von Adolf Buchheim und Oscar Falke [recte Georg Peter] ..."

Der Tempel des heiligen Grals : Oh! Heilige Wonne! Wie hell grüßt und heute der Herr!

Signatur des Originals: S 36/F07076

Margaret OH̀ea, Brustbild

Signatur des Originals: S 36/F09444

Der Tempel des heiligen Grals : Oh! Heilige Wonne! Wie hell grüßt und heute der Herr!

Signatur des Originals: S 36/F12378

Elizabeth Bannister als Patty, George Mattocks als Lord Aimworth, Szenenfoto, Doppelbildnis, in: Samuel Arnold: The Maid of the Mill, II. Akt, 3. Szene : Patty: "Cease, oh cease, to overwhelm me"

Signatur des Originals: S 36/G00065

La Sonnambula. Act I. Scene XI. : Elvino: Al nuovo amante, sconoseente t'abbandono. Amina: Oh crudo istante! Deh mudite io rea von sono. ; Elvino: I abandon thee ungrateful, to thy new lover. Amina: Oh, cruel moment! I am not guilty.

Signatur des Originals: S 36/G03300

Third-generation synchrotron x-ray diffraction of 6-μm crystal of raite, ≈Na3Mn3Ti0.25Si8O20(OH)2⋅10H2O, opens up new chemistry and physics of low-temperature minerals

The crystal structure of raite was solved and refined from data collected at Beamline Insertion Device 13 at the European Synchrotron Radiation Facility, using a 3 × 3 × 65 μm single crystal. The refined lattice constants of the monoclinic unit cell are a = 15.1(1) Å; b = 17.6(1) Å; c = 5.290(4) Å; β = 100.5(2)°; space group C2/m. The structure, including all reflections, refined to a final R = 0.07. Raite occurs in hyperalkaline rocks from the Kola peninsula, Russia. The structure consists of alternating layers of a hexagonal chicken-wire pattern of 6-membered SiO4 rings. Tetrahedral apices of a chain of Si six-rings, parallel to the c-axis, alternate in pointing up and down. Two six-ring Si layers are connected by edge-sharing octahedral bands of Na+ and Mn3+ also parallel to c. The band consists of the alternation of finite Mn–Mn and Na–Mn–Na chains. As a consequence of the misfit between octahedral and tetrahedral elements, regions of the Si–O layers are arched and form one-dimensional channels bounded by 12 Si tetrahedra and 2 Na octahedra. The channels along the short c-axis in raite are filled by isolated Na(OH,H2O)6 octahedra. The distorted octahedrally coordinated Ti4+ also resides in the channel and provides the weak linkage of these isolated Na octahedra and the mixed octahedral tetrahedral framework. Raite is structurally related to intersilite, palygorskite, sepiolite, and amphibole.