1270 THE COLLIERY GUARDIAN. June 18, 1915. experiments, which were suspended for the present, started again as soon as possible. Mr. J. Drummond Paton (Manchester) thought that a solution of the varying effects which resulted in the explosions would be found by a study of the trans- mission of heat in the form of radiant energy. If one considered the emissivity of the gas in the zone of pro- duction, and also the absorption capacity of the various shales based on radiant energy conditions, he was sure that interesting information would be obtained. If the nature of the gases were analysed on the basis of a radiant energy, transmission, he thought the investiga- tions would reveal certain information. Mr. J. T. Winmill (Doncaster) expressed his agree- ment with Dr. Haldane as to the necessity for further experiment with English coal dust, because the results given in the paper showed very definitely that there was a, considerable discrepancy between the results obtained on American coal dust and English coal dust, although the point upon which they disagreed was not very easy of determination. Dr. Haldane had suggested that the reason might be the difference between natural gas and the pit gas obtained in this country, which was almost pure methane. He did not think that that was a very reasonable explanation, because in the 1 per cent, of gas used in the ignition test there would only be a very minute proportion of methane. . The figures quoted in the paper showed that the relative explosibility of the natural gas they were using to pure methane was about 50 to 55—5 per cent, of the natural gas as against 54 per cent, of methane. Therefore, he did not think that that explanation could possibly cover the difference in the results. There was either a very striking difference in the coals, or there was one other possibility, viz., that there might be a big difference in the shale dust. He could not find any analyses in the paper of the shale dust used, but it would almost seem that it contained very little water, because the water in the coal was estimated, but not the water in the shale dust. As to the shale dust used in the Eskmeals experiments, all the experiments he had had contained up to 10 per cent, of water, and that water was given off extremely easily from the dust as soon as it was warmed in the slightest degree. Probably the large volume of water given oft when the dust was raised in suspension and slightly warmed rendered the coal dust far less inflammable than if the stone dust were absolutely dry, and that might account for the difference between the American and Eskmeals results; but that was merely a conjecture, since no data of the analysis of the shale dust were given. Sir Arthur Markham (London), referring to Mr. Winmill’s remarks, said that the tests made at Tredegar gave exactly the result which Dr. Haldane had men- tioned. In the Senghenydd explosion certain tests were made to ascertain, with natural gas and with methane, at what percentage an ignition could be obtained at different voltages. If those experiments were based, as he believed they must be, on the use of natural gas, then the paper was valueless from the practical stand- point of mining. The industry in this country was now being asked, or would shortly be asked, by legislation, to have compulsory stone dusting in all mines. If the writer of the paper were correct, it would be wholly wrong for Parliament to enact that there should be a given percentage of stone dust in all roads, because if, when any gas was present, it had the effect which the author stated, the whole of the benefit of the stone dust was lost. In regarJ to Pittsburg dust, it was said that the mixture would not ignite when the percentage of shale was 60 per cent. With 3 per cent, of gas, the mixture would not' ignite under 80 per cent. Those tests, as Dr. Haldane had said, were absolutely con- tradicted by every single test that had been made at Eskmeals for years past; and if the author could state whether natural gas was used in those experiments or not, he would relieve a great many engineers of a good deal of anxiety, occasioned by reading the paper, as to whether what was now proposed in this country, was not based on an incorrect test. He did not for a moment suggest that the Bureau of Mines in America, who had done excellent work in scientific research, were wrong; but if they were right in the test which they had made, and all our tests in this country were wrong, we ought not to proceed , by legislation to do certain acts till we knew where we stood. Sir William Garforth, referring to the last report of the Eskmeals Committee, in which it was stated that Dr. Haldane was going to make certain experiments with respect to shale dust and flue dust, asked whether Dr. Haldane was at liberty to say anything pn that point. . . , . Dr. Haldane replied that his report on that subject was printed some, months ago. He supposed it had not yet been made public. He could not say any more about it;, he,.did not know what had become of it. Sir William Garforth said that, with regard to the academic question, he had learned far more from the exploration work in connection with the Altofts explo- sion in 1886 than from the gallery experiments. Although in the latter they had the advantage of know- ing the velocity of the flame and the pressure, and the constitution of several of the gases evolved, still the other was a practical test, and it was to that that he would like to refer, in answer to Prof. Louis’s question. In that case, the ignition of the coal dust took place at a point about half-way along the roadway; the explosive blast did very little damage for the first 200 yds. on the one side, and about 150 yds. on the other, and then the damage commenced. When it had travelled 500 yds. the tubs were all broken to pieces, and there was one boy whose funeral took place on two occasions, and then for 1,700 yds. there were broken tubs, in many cases lying under a chain, as if the chain had been put into a state of oscillation, and then settled down on the tubs. The evidence was very conflicting; sometimes great destruction was found, and then for a distance very little destruction; but he thought the evidence obtained from actual experience must be taken to be more reliable than that obtained from an experimental mine. Although one knew there were those academic questions which should be solved in order to be able to make our theories coincide as nearly as possible with the actual facts, still, he did not think, he could give Prof. Louis any better information than that which he had given, which had come from actual observation. The details of the distances and the destruction which had taken place were all given in the appendix to the Report of the Royal Commission on Coal Dust in Mines, which was published in 1891. Had Col. Blackett been present, no doubt he would have said a good deal about retonation waves. He might have attempted to do something more, had the question been put some three or four years ago, when he was more familiar with the experi- mental work done at Altofts. As to the actual method, they were now trying to experiment for coal dust explo- sions in what might be called the commonest possible way, that was to say, in the same way as, if one had a fall of roof, one would send a man to re-timber, and if one had water accumulating on the dip side of the roadway, one would put a pump down and get it out. In the same way with stone dust. They had now some 13 miles of haulage roads on which it was-necessary to keep stone dust. More than 20 miles had been dusted, but 13 miles were kept in an efficient state. The early dusting had been carried out in 1912 at a cost of about <£180 a year. The second year, 1913, it only cost £150; and last year it had cost, so far, about £90 per annum. That included grinding the dust and other things, the details” of which he would be very glad to give if required. They had always an opportunity of seeing whether the stone dust was in proper proportion, by putting up a couple of sheets of cloth, causing an increased velocity in the roadway, -and then letting a man stand about 500 or 1,000 yds. away from the point. The men always grumbled if they had to do repairs, and contract the roadway. Several gentlemen present had had an opportunity of seeing the roadways and some of the seams, and they would bear him out in saying that they were leaving the shaft pillar, which was, of course, already covered with stone dust; they knew the coal existed, but until one got to the coal base one could not see a black road—they were all grey. It was an easy matter, after they had had several dustings of coal dust and shale dust, to brush part of it away. One found no angle of repose on which the coal dust could lodge, and it showed the grey surface underneath. It was such a trifling matter with regard to explosions, that they were going on just as they should do in the other matters connected with the colliery. Prof. L. T. O’Shea said, with regard to the point raised by Prof. Louis, Sir 'William Garforth had said that something might be learned by referring to practical instances of explosions, and he might refer to the explo- sion which took place at Wharncliffe Silkstone Colliery not so long ago. It seemed there was evidence there of the phenomena to which the author had called atten- tion, viz., the development of some force in the opposite direction to which the explosion was travelling, at some distance from the point of ignition. He understood that the explosion originated by an ignition of gas in the face, and was not an explosion to begin with; it was simply an ignition which eventually, in travelling towards the dip, developed into an explosion. The explosion then travelled down the level at right angles to the coal face, and in that level there was evidence of the tubs being blown in two directions, some of them being blown inbye and some outbye. He had had a very long discussion on the subject with the manager of the pit, because it had been suggested that the explosion had been in some other direction altogether, and there certainly seemed to be evidence of such phenomena taking place some way from the seat of ignition. Prof. Cadman said that Prof. O’Shea had made a very nice point between ignition and explosion. Would he define a little more what he meant by ignition? Prof. O’Shea said that the question was a thorny one, and he would rather not enter into it. He had differen- tiated between the two, because the report stated where the ignition was, and in the direction of the rise there was no evidence of any violence at all;- there was con- siderable evidence of burning,, however, and that burning passed down the gates and cross cuts into what was known as the slant; whereas in the opposite direc- tion, going down to the dip, there was evidence of considerable violence which one generally associated with the development of an explosion. There was abso- lutely no mechanical damage done in the opposite direction. Prof. Cadman thought there was little or no difference between ignition and explosion. If violence were going to be brought into the question, if ignition were some- thing more than gas burning, and if explosion were something that made a noise, it seemed to him that the question wanted very careful consideration. Sir William- Garforth said that Mr. Fryar had carried out a great deal of practical work in connection with stone dusting, and had given very valuable infor- mation at last year’s meeting. His experience with •stone dusting in the last 12 months would be interesting. Mr. J. W. Fryar (Eastwood, Notts),, speaking of the stone dusting work carried out at Bentley Colliery, said he had not anything to say on the subject in reference to the last 12 months which was in any way different from the experience stated at the last meeting. They had gone on in the same way, and had kept their places stone dusted, and so far had had no trouble. He might once again call attention to the Nottinghamshire coalfield, and to the fact that that coalfield had an average of about 43 per cent, of stone dust naturally in the dust’in the mines, and point out that the circumstance that that coalfield had not had a dust explosion in its history was a very good basis to work upon in legislation for the safety of English coalfields. One could hardly get any better illustration than practically the whole life of one coal- field. Mr. J. D. Morgan, in a written communication, expressed his appreciation of Mr. Rice’s paper. He (Mr. Morgan) had recently designed an electrostatic flame indicator, which had been found very useful in laboratory experiments on gas and dust explosions, and it occurred to him to suggest that a similar indicator would be more reliable than those employed by the author. A full account of that instrument was given in Engineering of January 8, 1915. He was interested to observe the author’s remarks on super-dusting. The diminishing effect of excess on the explosibility of coal dust was the subject of a communication by him (Mr. Morgan) to the Institution in March last, and in the discussion Mr. Henshaw had cited a case in his mining experience in which excess of dust appeared to have a retarding effect on an explosion. The author stated that retardation had been observed by him when the excess had been placed close to the firing cannon, and that under no other condition had super-dusting proved to have a noticeable retarding effect. That was a some- what puzzling statement; it was hardly conceivable that the explosibility of a given dust depended on the posi- tion in which it was placed relatively to the igniting medium. Perhaps what * the author desired them to understand was that at a position in the gallery remote from the cannon there was insufficient atmospheric dis- turbance to raise an excess of dust, and that it was for that reason that no retardation was experienced. The curves at fig. 6 were extremely interesting, but unfor-. tunately they were not very fully explained in the text. It was noticed that as abscissae the values plotted were the ratio of volatile combustible to the total combustible in the dust, and for ordinates was taken the quantity of inert matter necessary to prevent explosion. At first sight there did not appear to be any rational connection between the quantities chosen. The crucial question was : Why the ratio of volatile to total combustible? There was an opinion in this country that the relation between the volatile and the total combustible consti- tuents of coal had no definable connection with explosibility. That was certainly his own opinion at present, and he believed it was also that of others. As against that opinion, there was the remarkable regu- larity of the author’s curves, and it would be very surprising to find that the regularity was accidental. He would also ask the author if he had observed whether the roughness of the walls of his gallery had any increasing effect upon the violence of a coal dust explosion. Atten- tion had been drawn to the possibility of that pheno- menon in his (Mr. Morgan’s) paper to the institution to which he had referred. There seemed no doubt that the surface of the gallery had a modifying effect upon an explosion, but direct proof by investigation on a large scale appeared to be wanting. The author had had experience of a smooth gallery, and one made to imitate a mine roadway; he would doubtless be able to say, therefore, whether any effect had been noticed which was attributable to the character of the surface of the gallery. Mr. H. W. G. Halbaum (Cardiff) wrote that, in his opinion, Mr. Rice’s paper was a most valuable record. It demonstrated the practical utility of the principle that the air current itself was the best selector of dust, and the success of the plant proved conclusively that it was sufficient to break up the mass by a purely hammer- like action, leaving the air current itself to select the fine dust required. That principle of the automatic selec- tion of dust by the air current was evidently capable of extension to the case of stone dust, as well as to the case of coal dust. He would like .to ask Mr. Rice to state precisely what was meant by, say, a “ 240-mesh ” screen. The first paragraph of the section entitled “ Point of Ignition ” would greatly surprise some authorities in this country, if one might judge by the hostile reception they accorded not so long ago to a suggestion that an excess of coal dust might ’ have an influence analogous to that exerted in other cases of combustion where one of the agents was much in excess of the other. Personally, he had never been able to agree that chemical laws acted differently in different