654 THE COLLIERY GUARDIAN. September 27, 1918. CARBONISATION REACTIONS.* Founded in 1911, the first William Young Memorial . Lecture was delivered by Dr. Harold G-. Colman in 1912, the second by Dr. W. B. Davidson in 1913, and the third by Dr. R. Lessing in 1914. After a lapse of four years, the long interVai being mainly attribu- table to war conditions, the fourth lecture was delivered by Prof. J. W. Cobb, Livesey Professor of Coal Gas and Fuel Industries in the University of Leeds, who took for his subject “ Carbonisation Reactions.” Prof. Cobb said that in taking up a complex study such as that of the reactions occurring during the carbonisation of coal, there seemed to be two main roads to follow. One might take the original substance in all its com- plexity, carbonise it under various conditions, and, by the careful consideration of exactly recorded results, attempt to arrive at general conclusions, the validity of which could be determined by further observation, or by modifying practice in the direction indicated. This method was followed more or less by every good gas engineer, and was what one understood by intelligent and progressive works practice. Alternatively, one might try to arrive at a better understanding of the highly complex by a preliminary study of the simple, determining, for instance, the mode of formation and decomposition of some one constituent of coal gas under a variety of conditions, including, of course, as of primary importance, those conditions to which it would be subjected in carbonising practice. This was par- ticularly a method for the laboratory. When one considered the number of substances involved in a survey of carbonisation on such a plan, it was plainthat the amount of work waiting to be done was enormous, and left plenty of room for judicious discrimination between the more and the less important. In connection with the first method of investigation, there might be some temptation to believe at first sight that so much coal had been carbonised under so many conditions in the past that data must be to hand already for the solution of all the principal elementary problems. This was not so. In order to trace exactly what happens in the process, coal should be heated slowly, and the decomposition at each temperature should be completed, or practically completed, before the temperature was further raised. This could not be done in ordinary practice, for commercial and other reasons. It w. s possible, however, to slow down the operation of car- bonisation to any desired extent—raising the tempera- ture with extreme slowness, and collecting the products. This had been done in the laboratory by a number of workers, and the results obtained were useful and interesting, but incomplete, as the quantity of coal which could be handled was not sufficient to allow of a thorough quantitative examination of the products, For the solution of this particular problem, a larger scale of apparatus was necessary—something in the pature of a small gas plant, designed primarily to allow of the most effective control of temperature and every other determining condition. A Study of Benzene, The second method of investigation—the study of the decomposition of single constituents—was one which he (Prof. Cobb) had applied recently, in collaboration with Dr. S. F Dufton, to two constituents of coal gas which had assumed dominating importance—benzene and toluene. In developing a process for the production of the latter from other constituents of coal tar, they set to wrork (starting with benzene) to find out where and how these substances decomposed under the action of heat, but bearing in mind the special conditions attaching to the carbonisation process. For this purpose they passed benzene vapour through a silica tube which contained a 5 in. column of red-hot coke maintained at the desired temperature, and the rate at which the benzene passed was so adjusted that its time of contact with the red-hot coke was of the same order as would occur in carbonising practice— some 10 to 15 seconds. The benzene was not simply boiled through the tube, but was first vaporised in a “ carburetting ” flask by bubbling gps through it, The gas used was nitrogen when they wished it to be inactive, but a potentially active gas—usually hydrogen —^was employed when they wished to determine its influence on the reaction. By raising the temperature of the carburetter, the richness of the gas stream in the benzene could be varied at will. Thus, saturating at air temperature (15 degs. Cent.), the percentage of benzene present by volume would be 8, while at 50 degs. Cent, the percentage would be 36. The stream of gas, after passing through the coke, came away to a flask which was simply air-cooled or immersed in ice and salt, and there easily condensible products were deposited. It then passed through a second condenser cooled by solid CO2 or liquid air to complete condensation, and the remaining gas was collected, measured and analysed. They first determined that, in a stream of nitrogen rich in benzene, decomposition had just started at a temperature of 550 degs. Cent. The benzene then passing the tube deposited a small quantity of a solid resembling naphthalene in appearance. It was identified as diphenyl, and was produced in greater quantities, along with hydrogen gas, as the temperature rose. The decomposition indicated was a molecular condensa- tion of the one-ring compound benzene to a two-ring compound diphenyl. Eliminating hydrogen, and in the material deposited at higher temperatures, they found a three-ring compound, diphenyl benzene, the molecular condensation having evidently gone a step further. At 750 degs. Cent, (a red heat) 32 grammes of these solid highly condensed compounds accompanied 115 grammes of unchanged benzene. This decomposition of benzene to produce diphenyl by passing through a red-hot tube has been known since the time of Berthelot, and is a recognised method of preparing diphenyl. On the other hand, although benzene is found in some quantity in coal gas and tar, diphenyl is only present * William Young Memorial Lecture, delivered by Prof. J. W. Cobb before the North British Association of Gas Managers at Glasgow on September 6. in minute quantities which can hardly be separated. They were here faced with one of those so-called differences between theory and practice, or between laboratory and large-scale results, which indicated that important factors in the operation had not been taken into account. In this case the reason was suggested in the results of experiments made by Mr. Hol lings and the lecturer, and published in the Transactions of the Institution of Gas Engineers in 1914. It was there noted that benzene was not decomposed at 800 degs. Cent, under conditions similar to those described above, excepting that the benzene was present in a state of high dilution with hydrogen and methane, to repr» sent, approximately the condition of carbonising piacti e. Dr. Dufton and he, therefore, repeated their experi- ments—in the first place using benzene highly diluted with nitrogen. Decomposition was lessened, and ti e yield of such solid condensates as diphenyl lowered. They then tried substituting hydrogen for the nitrogen. Since the decomposition of benzene to diphenyl liberated hydrogen, the presence of this gas in quantity from the beginnir g should tend to counter- balance the reaction, and so limit the decomposition. They found it to do so. By gradually diluting further and further with hydrogen, the amount of molecular condensates—such as diphenyl—produced at 750 degs. Cent, gradually diminished, until when hydrogen was simply bubbled through benzene, and the latter, there- fore, became only about 8 per cent, by volume of the gas mixture, only traces of diphenyl were produced, the benzene being practically undecomposed by the treat- ment. What this indicated was that the condensation of benzene with the elimination of hydrogen might well be reversible; and an experiment was therefore made in which diphenyl was placed in the carburetter and hydrogen was bubbh-d through it—being saturated at 90 degs. Cent. A small quantity of liquid was found in the condensing train at the end of the experiment and identified as benzene. The condensation of benzene to diphenyl was so proved to be reversible. The reason was now clearly established for the stability of benzene in carbonisation, at such tempera- tures as 800 degs. Cent., and the almost complete absence of diphenyl, although the latter is so easily produced from benzene in an ordinary laboratory experiment at the same temperature. The solid condensates which had been obtained from the benzene—nitrogen mixture as 750 degs. Cent, con- tained no naphthalene and no unsaturated compounds, such as consumed sulphuric acid in their treatment; nor did they yield any pitch on distillation. Moreover, very little carbon was deposited in the hot silica tube. So far their experiments had been limited to 750 or 800 degs. Cent—a medium carbonis’ng tempera- ture. At the higher temperature of 900 degs. Cent,, even in hiyh dilution with hydrogen, benzene was found to be freely decomposed, with the deposition of grey methane carbon in the hot-coke layer, the particles being cemented together by it, and the separation of softer black sooty carbon at the cooler end of the tube and in the issuing gas stream. The process of decomposition had become more drastic Mr, Rollings and he had previously found that benzene, even when highly diluted with methane and hydrogen to imitate carbonising conditions, disappeared com- pletely at 1,100 degs. Cent, Experiments on Toluene. The next experiments were made on toluene (C7 H8), which may be regarded as a benzene ring with an attached — CH3 group. The first decomposition of this compound when vaporised and carried through the coke by a stream of nitrogen was noted at 550 degs. Cent, (a dull red heat), and at 600 degs. Cent, sufficient of the new solid compound was produced to admit of its examination. It was found to be stilbene (C1%H12 or C6H5CH=CH— C6H5), which ivsembles the diphenyl formed from benzene in containing two benzene rings, but differs from it in being an unsaturated compound. At the same time an oily substance was formed. Thus the first decomposition of toluene, like that of benzene, was found to be one of condensation from a single-ring to a double-ring compound. But, as is readily com- prehensible on chemical grounds, it differed in taking place in more than one direction, as indicated by the presence of the oil, and in forming an unsaturated compound, such as would take up sulphuric acid in a washing process. At higher temperatures increasing decomposition was noted, and at 750 degs. Cent, it was quite extensive. The solid products of decomposition or molecular condensation, on examination, yielded both naphthalene (double-ring compound) and anthracene, and consisted partially of unsaturated substances, as was plainly shown by their high consumption of sulphuric acid on washing—resulting in a black, viscous liquid. The plainest distinction from the behaviour of benzene was, however, yet to come. On substituting hydrogen for nitrogen as the carrier gas, it was found that decomposition of the toluene was very much accelerated, with the production of large quantities of oenzene and smaller amounts of solid condensates. The gas collected at the end of the train contained considerable quantities (such as 50 per cent.) of methane. There was no difficulty in interpreting these results. The formation of molecular condensates, such as stilbene, takes place with the liberation of hydrogen. If, then, a large quantity of hydrogen is present initially, the action is checked, as explained in connec- tion with the formation of diphenyl from benzene. The hydrogen atmosphere can, however, act directly on thi toluene, reducing it to benzene by combining with the CH3 group to form methane. This reaction, too, is reversible. On passing a mixture of methane and benzene through red hot coke at 750 degs. Cent., and examining the products, they were found to consist mainly of undecomposed benzene with some diphenyl, but to contain also a small quantity of toluene. The formation of toluene from benzene is, therefore, possible in this way, but is effected only very slowly and under special conditions. The main difference between the decomposition of the two substances, benzene and toluene, lies, therefore, in the action of hydrogen. The decomposition of benzene is prevented by hydrogen, because it counterbalances the tendency to form diphenyl, which would require the elimination of hydrogen. It facilitate^ the decomposition of toluene by combining with its CH3 group, and so reducing the original compound, toluene, consisting of a ring and an attached group to benzene—a simple ring, forming methane at the same time. These considerutions are probably of wide application in the complex process of carbonisation. The hydrocarbon next to toluene in the same chemical series is xylene, or rather the three xylenes ortho-, meta-, and para-, boiling from 143 degs. to 138 de^S? Cent. The decomposition of a sample boiling at 138 degs. to 140 degs. Cent, was very similar to that of toluene, yielding in an atmosphere of hydrogen at 750 degs. Cent, toluene and benzene by reduction, and a limited quantity of solid condensates. These three substances, benzene, toluene, and xylene, boiling respectively at 80 degs. Cent., 110 degs. Cent., and 140 degs. Cent, (average), constitute the most important ingredients of the light oil fraction in the tar from medium temperature carbonisation (800 degs. Cent). Cresol, the characteristic constituent of the “cresol” fraction in tar distillation, is also reduced extensively at 750 degs. Cent, in a stream of hydrogen to toluene, and necessarily to benzene also. A Study of Carbonisation. There is clearly indicated a tendency for hydrogen ^always present in quantity in the products of carbonisa- tion) to reduce the single-ring benzene compounds to benzene, and at the same time to preserve benzene itself. A similar action of hydrogen may be inferr- d as in every way probable on the attached groups of more complicated ring compounds, resulting in the formation of naphthalene and anthracene. Hence it is not surprising that William Young and Thomas Glover pointed out in 1897 that carbonising at high temperatures made for the predominance of benzol and naphthalene in the products and scantiness of the higher benzols, phenols, and paraffins. The s'udy of the decompositions undergone by benzene and toluene may not only be regarded as useful in itself, because of the great importance of these substances at the present time, but may be of service in other ways. We see clearly why the process of carbonisation can never be regarded as a simple effect of heat independent of the gaseous atmosphere in which it is conducted, and the way in which we may hope to modify the results of carbonisation in various directions by the deliberate control of that atmosphere. The experiments on benzene and toluene lead to a quite definite conception as to how hydrogen may exert its influence in preventing or minimising those decompositicns which are of the nature of molecular condens itions—such as the passage of a one-ring into a two-ring or three-ring molecule— and, on the ether band, how hydrogen may promote decompositions tending to simplification of molecular structure by combining with attached groups and pro- moting their detachment. Both effects will tend to set and keep a course for the reactions in carbonisat on which will lead to the minimum production of heavy molecules, such as may be taken to constitute the bulk of the heaviest tar fractions and solids. An a'tempt had been made to treat coal under con- ditions which-may be taken as the extreme logical application of this effect of hydrogen in determining the nature of the products. Bergius has described a process in which coal is heated with hydrogen or hydrogen mixtures under high pressure (preferably above 100 atmospheres), and he claims that the hydrogen reacts readily, giving liquid products or easily melting solids. The process has been descril ed as “ the liquefaction of coal.” Bergius claims, also, the application of the same process to such products of carbonisation as tar and pitch, stating (as exemplifying the results obtainable) that 1 kilog. of tar heated with hydrogen to 400 degs. Gent, at 100 atmospheres pressure for four hours, and afterwards distilled to 250 degs. Cent., gave about 60 per cent, of distillate resembling petroleum oil. The general reaction relied upon is no doubt the same as the conversion of solid diphenyl into liquid benzene by hydrogen, previously descril ed, the effect being intensify d by pressure. This method of treating coal had just reached the stage of works trial in Germany when the war broke out. The treatment was rather heroic, and one would be interested to know what are the various costs of installation, operation and depreciation. Turning to more normal practice, very considerable experimental work bad been done by gas engineers during the last few years in which this principle of the importance of atmosphere had been applied, but it was on y the advent of the vertical retort which had made it possible to subject the descending charge during carbo- nisation to the really effective contact, penetration, and action of an ascending stream of gas: Hydrogen in quantity, although not unmixed, could be readily brought into the retort, either as coal-gas stripped of its by-products or as water gas, while it could also be supplied indirectly by blowing in sham and depending on the water-gas reaction which necessarily occurs when this steam impinges on red-hot coke at the bottom of the retort. The action of a gas in the retort might be regarded in two ways. Even an inert gas, such as nitrogen, would not be without effect, because it would wash the volatile products of decomposition out of the pores of the coke, assist their volatilisation by lowering their concentration in the vapour phase, and hurry them away from the region of decomposition. A gas like hydrogen, being so light, had greater diffusive power, its molecules travel their zigzag paths at a higher speed, and it is, therefore, even better able to penetrate the pores and perform these duties. But the all-important action of hydrogen is chemical, as has been already sufficiently emphasised; and other gases cannot be expected to exercise the same chemical influence. Their physical action is no doubt similar, but rendered less effective by their higher density and lower diffusive power. The general effect of the ascending gas stream to be anticipated is that of lowering the average mole-