534 THE COLLIERY GUARDIAN. March 15, 1918. revolutions could be obtained over a period of from one to two minutes. Figs. 4 and 5 show the arrange- ment fitted to a Simplex indicator. The apparatus consists of a steel tube that can be . easily.fixed to the indicator by a clamp ; it carries at its extreme end a pulley running on ball-bearings driven at a constant speed by gearing and a governed clockwork through a flexible shaft. The ordinary reciprocating drum on the indicator is replaced by a pulley running on ball bearings, and a belt of paper 6 ft. long runs on the two pulleys. Variable gearing is provided, and there is a considerable range of speed in the clockwork, the proper speed being adjustable between 2 ft. and 10 ft. per minute. A governor is provided, so that any predetermined speed is constant. The pencil of the indicator marks the paper as it passes over the drum, and an auxiliary or signalling pencil also marks the paper by means of a small magnet controlled by a push-button in the hand of the operator, so that the instant of starting, stopping, end of stroke of the piston, etc., can be given relatively to the indicator record. Signals can also be given autom itically from a contact-maker on the shaft of the engine. It will be seen that the paper moves under the pencil continuously, and does not reciprocate as in the ordinary indicator, and that the movement of the paper is pro- portional to time and not to the volume swept by the piston. The pencil line, therefore, does not return on itself, but gives a series of waves or cycles, the lengths of which, are inversely proportional to the speed at which the crankshaft is revolving. The mean pressure can be readily calculated, but the card has to be specially divided so as to give readings representing constant differences of volumes swept by the cylinder. A very large number of diagrams have been taken and compared with those taken by an ordinary indicator, and a'though the indicator used is a small one, very consistent lesults have been obtained. The signalling pencil gives a continuous line along the top of the record, which is useful for obtaining the atmospheric line. In indicating a winding engine, the paper is set to travel its whole length in a few seconds longer than the winding cycle, and the indicator and signal pencils are set against the paper. The operator watches the piston rod and presses the button twice on the engine starting, at the same time starting a stop watch. He. also presses the button at the end of every stroke, and this is recorded on the paper. This is important, as although the earlier strokes can be easily deciphered while steam is on, the period of running free and braking with the steam does not give a definite indication on the diagram of the end of the stroke. The signal marks the end of each stroke, and shows where steam is against the engine. At the end of the run, a signal is marked on the paper, the stop watch hand is stopped, and the time taken is recorded. In working out the diagram, it is cut in two, giving a paper 6 ft. long, and pinned to a wooden straight-edge. The length of the paper between the signals “start” and “stop” is measured, and when divided by the number of seconds of the run this gives the length of a division of paper repi esenting one second. The length is stepped out on the paper, and the time taken by each stroke can be obtained, as also the space of time from the start to the beginning of each stroke. After the mean pressures are calculated, they are plotted out, and compared with the relative times, as shown in fig. 6. The revolutions per minute are also plotted in the same way. From these curves the indicated horse-power at any moment, the velocity of the cage and accelerations, both positive and negative, can be calculated (fig. 7). The weight of steam used can also be calculated in the usual way from the diagrams, but this is, of course, only an approximation, as the “ missing quantity,” or the difference between the weight of steam shown on the diagram and that actually used, has to be esti- mated. By taking this “ missing quantity ” to be a fourth of the total amount, or a third of that shown on the diagram, a conservative estimate of the steam used can be obtained, the maximum rate of flow being par- ticularly interesting. It does not take a draughtsman very long to obtain the curves shown on figs. 6 and 7, but in order to get the steam consumption, diagrams have to be taken from the four cylinder ends and about sixty cards worked out, entailing at least two days’ work. This gear can a’so be used for finding the maximum load and variations of speed of continuously-running engines (fig. 8). It is readily digged up, and can be attached to a winding-engine and a complete card taken in a. quarter of an hour. This apparatus is not claimed to be a novelty, as the Mathot in-lira* or gives a somewhat similar diagram. Similar results are given of some German tests in Messrs. McCulloch and Filters’ book on Winding Engines and Winding Appliances* but the apparatus is not described. The apparatus described in this paper has been in regular use since-1903. Inking* Chronograph. This instrument records short intervals of time, and is very useful for taking the speed cycles of winding engines, rolling mills, and lifts, and other apparatus having variable speeds. It consists of a good centre- seconds watch, having at the end of the seconds hand a little cup full of ink. On pressing a knob, a spot of ink is left on the dial, and a large number of consecutive readings can be recorded at short intervals. It is par- ticularly useful for plotting the acceleration curves of electrical winding engines. It is a rare instrument, and is used for astronomical work. That used by the writer was made in 1877. The Measurement of Compressed Air. Although the electrical plant at a colliery is strictly controlled by Home Office Regulations, and it is a general practice to have ammeters, voltmeters, leakage indicators and recorders, and circuit breakers to give * 1912, page 245. power measurements and to control the circuits, very few compressed-air plants are fitted with anything more than a pressure gauge, which is frequently of a type that is liable to give inaccurate readings. This is all the more remarkable as compressed air is probably of greater importance to most collieries than electricity. This statement holds good, particularly in South York- shire, as regards inbye haulage, there being a wide- spread feeling among mining engineers that electricity should only be used underground under the shaft pillar and in main intake airways. It is probable that the amount of steam used for compressing air largely exceeds that used for generating electricity at the average colliery, even when the surface plant and main haulages are electrically driven. Great strides have been made in the last few years in the simplification of means of measuring and recording the flow of compressed air, and remarkable improve- ments have been made in the accuracy of these instruments. In fact, air-flow indicators and recorders that will give accurate readings at full load within 1 per cent, of the mean can be obtained at a reasonable cost. Venturi and Orifice Measurements. The Venturi meter is, perhaps,the most refined method of making air and water measurements, the readings being extremely accurate and the fall of pressure over the instrument very low. The thin-edged orifice is also a s’mple and accurate means of measurement, but has the disadvantage that it requires a larger drop of pressure than the Venturi tube, so that the loss of pressure may be as great as 1 per cent, at full load. It is not, therefore, so suitable for leaving in the pipe- circuit for taking daily readings. It is, however, very easily made, and the calculations for its construction Fig. 8.—Mean Pressure Curve of Ordinary Steam Engine. An — M E AN PRESSURE 40 30 2.0 to □ to SCCOXOt ZO JQ 4oa< Rate of- Flow per 8-imch Meter-valve 0 +. f.TeO ft * <0 £ m Too Cu8‘ /yffiT ' l/x? 7 2ooa Fig. 9.—Results of Calibration Tests on Sentinel Meter Valves. and use are quite within the mathematical attainments of the mining engineer. The flow of air is proportional to the square roots of the fall of pressure across the orifice, the absolute pressure of the air measured, and the reciprocal of the absolute temperature. As to take all these data into consideration would involve a complication, it is quite possible for practical purposes to read only the fall of pressure over the orifice, a constant being used to include a standard pressure and temperature. The scale of the instrument can then be calibrated to give the weight of air or the volume (either at working pressure or atmospheric pressure) passing in unit time, the usual unit being the number of cubic feet of free air compressed per minute. Meter Valve. The writer has fortunately been able to arrange with Messrs. Beiliss and Morcom Limited, for the testing of two meter valves, the readings being taken by com- parison with standard instruments on their test plate. These valves were made by Messrs. Alley, MacLellan and Company Limited, and consist of well-made full- bore valves, fitted with an accurate scale to show the travel of the valve disc. A manometer is fitted, which indicates against a fixed mark when there is a pre- arranged fall of pressure across the valve. The valve is closed until this float shows that this fall of pressure is obtained, and the reading on the scale when compared with a* chart gives the flow of air, corrected for both pressure and temperature. The test readings of the two 8-in. valves are shown in fig. 9, the result showing a quite remarkable accuracy. It is certain that the general use of some form of air meter is of the greatest importance, both for proving the condition and efficiency of the air compressors and the leakage in the mains. All these instruments are affected by pulsations in the air supply, and should be placed in the outlet side of ample receivers. The intention of this paper is to call attention to various means of maintaining the efficiency and safety of colliery power plants, particularly with a view to the reduction of coal and power consumption. MAGNESITE AND MAGNESITE BRICKS. A paper on this subject was read by Mr. W. Donald (Glasgow) at the ordinary monthly meeting of the Ceramic Society, on March 9, at Stoke-on-Trent. The supplies of magnesite are at present obtained from Greece and India. Other available supplies are to be found in South Africa, Australia, Canada and California, while in Europe deposits occur in Russia, Norway, Sweden and Lapland, apart from the well- known deposits in Austria and Hungary. The refractoriness of magnesite bricks has relations with the density, porosity, tensile strength, resistance under load conditions at high temperatures, and chemical composition. For the control of these factors it is necessary to acquire full knowledge of the raw magnesite both as regards mineral impurities and the varied effects of different degrees of heat acting for different periods and in oxidising or reducing atmo- spheres, followed by slow or rapid coolb g. The effects of eliminating certain impurities, and adding certain others should also be known, and the effects of furnace heats on the products. Of great importance, too, is the detailed microscopic examination, which furnishes information not otherwise obtainable, particularly as to the course taken by alterations, the causes of which can often be traced in this way. After describing at some length the mode of occurrence of the Austrian magnesite deposits, and the chief characteristics of the materials and the bricks made from them, the author proceeded to deal similarly with Greek magnesite, which (like the magnesites from India, Canada, etc.), has a finely crystalline structure as contrasted with the massive crystalline structure of the Austrian magnesite. The average analysis of calcined Greek magnesite shows 90*67 per cent, mag- nesia, 3*02 lime, 0*71 ferric oxide, 0*69 alumina, and 4*20 silica, but much of the rock is pure enough to give up to 95 per cent, magnesia on calcination. Chemically the Greek magnesite is purer than the Austrian material, but the iron compound which constitutes the bulk of the impurity in the latter is very evenly distributed throughout the mass, whereas the corresponding con- stituent in Greek magnesite is very irregularly dis- tributed, as are also the alumina and silica, though lime runs uniformly through most of the raw magnesite. Irregularity of distribution of impurities is even greater in Canadian magnesite. In sections of Greek magnesite bricks fired at 1,750 degs. Cent, and 1,850 degs. Cent, it was evident that the face next the heat was quite fused, and half an inch from that face the brick showed alterations of crystals from the small to the large crystal, but no bad effect of the heat was visible where the large crystals had been formed. Sections of Austrian magnesite bricks fired at the same temperatures showed no sign of being fired at a high temperature. In Austrian magnesite bricks the magma has inter- penetrated each particle, and is distributed through the whole mass of the brick. In Greek magnesite bricks no such interpenetration of the particles by the magma has occurred, but as the brick with each presentation of a new face after spalling is converted bit by bit into the larger crystal formation, the impurities present in the magma often cause a frothing with great porosity. The silicates of magnesia are bulky and highly viscous, and having a melting point at 1,550 degs. Cent, they must be still almost immovable as a molten liquid at 1,650 degs. Cent. Hence it seems necessary to introduce ferrous iron. Dr. A. Scott has shown that whilst magnesia com- pounds and lime compounds have melting points ranging between 1,500 degs. Cent, and 1,550 degs. Cent., com- pounds, including both the magnesia and the lime, melt at at least 150 degs. Cent, lower. Hence lime should be eliminated in every way possible, or its equal distri- bution should be facilitated by giving the necessary consistency to the magma. On the whole, the result of using Greek magnesite bricks of British make in basic open-hearth furnaces, pig iron mixers, Talbot furnaces, and electric furnaces, is satisfactory from the steelmaker’s point of view. But difficulties are still experienced with regard to spalling, and inability to withstand the corrosive action of the basic slag, and the great strain that arises in the roofs of electric furnaces. Generally speaking, two types of magnesite brick are made in Great Britain. One is made from finer material, and the bricks weigh about 72-76 cwt. (sometimes to 80 cwt.) per thousand, the other being made from less finely ground material, and the bricks weighing 82-86 cwt. (sometimes to 88 cwt.) per thousand. In sections, the lighter bricks show finer particles and on the whole a more complex colour scheme, whilst in the heavier bricks there is greater light and shade between particle and magma and between some particles and others. Comparison with sections of calcined.magnesite shows that a considerable percentage of the particles in British-made bricks remains in the state of calcined magnesite, and that the impurities surround rather than interpenetrate them. Indian and Greek magnesite calcined at 1,250 degs. Cent., showed minute granular forms; Indian magnesite, calcined at 1,750 degs. Cent, in an electric furnace, showed alteration, which seemed greatest where impurity was present. In Greek magnesite, fired to about 1,900 degs. Cent., the particles around the impurity were completely altered, and the alteration spread in all directions from such centres. Greek magnesite, after prolonged calcination at a lower temperature in a modern shaft kiln, showed the change in the mineral particles practically throughout the mass. The mineral crystals in these magnesites resembled those seen in microscopic sections of Austrian magnesite bricks, and