Journal . id eonies into contact. Tin column is tubularin form and provided with flanges, which are secured tothe preceding and tollowing sections, as the column is builtup of successive super-imposed sections (Fig. 1). 1{ arcrectangular nozzles opening oatwaids and into the interiorof the section. These nozzles are located opposite to eachother and in the same horizontal plane. C are the Hue-sheets which receive tlie Hue-pipes I). K and E are thecovers pro\ idcd with partition walls b b upon E and rf uponE, which walls statu! at right angles to the inner faces ofthe covers, and when i)]uccd i
Journal . id eonies into contact. Tin column is tubularin form and provided with flanges, which are secured tothe preceding and tollowing sections, as the column is builtup of successive super-imposed sections (Fig. 1). 1{ arcrectangular nozzles opening oatwaids and into the interiorof the section. These nozzles are located opposite to eachother and in the same horizontal plane. C are the Hue-sheets which receive tlie Hue-pipes I). K and E are thecovers pro\ idcd with partition walls b b upon E and rf uponE, which walls statu! at right angles to the inner faces ofthe covers, and when i)]uccd in position form the chambers1, 2, 3, •), and .> ( Fig. 2). F and F are the couplings forthe water pipes. The water enters the chamber 1, i>assesthence transversely through the flues into 4, thence into 2,thence across into 5, and lastly into 3, whence it passes outthrough F. Fig. 3 shows a column in which .several sectionsare coupled together, all taking the water from a singlestand-pipe m.— Feb. 29,1888.] THE JOURNAL OF THE SOCIETY OF CHEMICAL DJDUSTRY. Ill GAS. AND LIGHT. Servian Coal. S. M. Losanitscti. l!ir. 20,-fi-STlS-CoAi. is verv widely distributed in , and occurs inInrpe quantilies in many localities, but at the present timeonly a few mines are constantly at vork. Tlic strata varyin ae from that of the carboniferous to that of the tertiary formations. The author has examined all speci-mens of importance, and his results are given in thefollowiuK table. The percentage of volatile matter anrlcoke was estimated by igniting the sample in a coveredcrucible, corrections bein? madi! for the hygroscopic waterand ash it contained ; the calorimetric results were obtainedhv ciilculation. Source. 100 Farts of Coal contain O(andN). BjO. Ash. VolatileC?onsti-tucnts. Coke. Calorics, 1. Stol. 92-50 0-46 2.—COAI. FKOM CaUBOSIFEROUS FORMATIOX Mustapie MiJljenovac Osipaonica Kladuroro
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Keywords: ., bookcentury1800, bookdecade1880, booksubjectchemist, bookyear1882
