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Sulphur: the trigger of gunpowder 
Geoff Smith
Journal of the Ordnance Society, Vol.28, 2021
Much has been written about the sources and properties of saltpetre and charcoal but the third component of gunpowder, sulphur, has received scant attention. Although the ‘modern’ spelling of saltpeter and sulfur 
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 are becoming more widely used, saltpetre and sulphur are almost universal in contemporary literature. The sulphur spelling is still used by the city of Sulphur, Louisiana, US technical manuals, EU legislation, major producers and many place names. As this paper deals primarily with literature pre-twenty-first century, the original spelling is used throughout. Although gunpowder can be made without sulphur, it has been considered an essential component from the earliest times. Of the theories propounded for the invention of gunpowder, none address the question of why the three ingredients were present in proportions that could result in a credible explosion. A previous paper 
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 has posited the development of gunpowder as an evolutionary process following a logical progression involving no unique inventive step. This, incidentally, explains the difficulty in assigning a specific date to the invention of gunpowder.Briefly, the sequence of development could credibly have been ...Charcoal – A fire weapon (fire pot)Charcoal + Sulphur – A chemical weapon (stink pot)Charcoal + Sulphur + Saltpetre - An enhanced flame weapon (flame thrower)By increasing the saltpetre content as an obvious means of enhancing the flame effect, theexplosive properties became evident and were exploited.
Properties
Sulphur is an element, number16 in the periodic table, and is widely distributed in nature, mostly in combination with other minerals such as calcium sulphate (gypsum) and as metal ores of copper, iron, nickel etc. It is also found in association with natural oil and gas deposits. In its uncombined state, it is commonly associated with volcanic activity. Some isproduced by a range of bacteria.It combines readily with oxygen to form sulphur dioxide and trioxide and has long been an essential raw material for the manufacture of sulphuric acid (oil of vitriol in antiquity) and many other chemicals.Sulphur forms two main crystalline states.
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When heated, sulphur exhibits unusual behaviour. At 114.5
o
C it melts to a clear free flowing liquid but at about 230
o
C it thickens and cannot be poured. On further heating it becomes more fluid again until it boils at 448
o
C. On cooling, the sequence reverses. The significance of this to the overall function is unknown but, since it occurs within the ignition temperature range of gunpowder, it may be worthy of further investigation.
Function
It is well recognised that the function of sulphur in the gunpowder mix is to lower the ignition temperature. The mechanism of the reaction is less well understood and depends, to some extent on a variety of factors. For instance, the reactions taking place at initial ignition may differ from those when the pressure has built up at a later stage and these may again change during cooling.The reaction products of burned gunpowder have been investigated in depth since the beginning of the eighteenth century by many of the great chemists of that era. Names like Bunsen, Gay-Lussac, Nobel, Berthollet, Abel, Dewar et al., the list goes on, and their findings have not been challenged by modern investigations. The significance of volatile organic chemicals trapped within the cellular structure of charcoal has been discussed elsewhere
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 and it is the reaction of these at relatively low temperature that accounts for the ready ignition of gunpowder.Considering the sensitivity of gunpowder to ignition by a spark, it is interesting to note that by raising the temperature slowly it is possible to sublime off the sulphur without igniting the powder.
Sources
Sulphur was known to the ancients, often under the name of brimstone (burning stone). Itsbright yellow colour is impossible to miss and its basic properties were well understood. In volcanic regions, significant quantities of sulphur can be found exposed on the surface. Deposits are found in Mexico, Japan, New Zealand, Caucasian and Abu Dhabi
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. In Europe, Sicily was the dominant supplier and for Nordic countries, Iceland. Britain has a minor source at Cae Coch (N. Wales). It has been exploited by the local chemical industry but there is no record of association with gunpowder. This is a significant factor in determining the geographic origin of gunpowder since it could only be developed where the ingredients were available. Sulphur is still collected by hand from the Ijen volcano in Eastern Java.(2021)
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Fig 2 a Ijen Volcanic sulphur deposits.Fig 2 b Hand transport in Java
 
 A lesser known source was Jebel Dhanna in Abu Dhabi which appears to have supplied the needs of the Levant and doubtless other minor deposits served some local demands.
Spain
From the fifteenth to the early nineteenth century Spain controlled a vast empire centred on the Americas. To support and expand its possessions required a considerable supply of gunpowder. It is not surprising, although rarely reported, that Spain should seek to be self-supporting in the supply of sulphur,
azufre
. Spain had its own sulphur mines from the first century BC to the twentieth century and appears to have been entirely self-sufficient
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.The mine at Hellín in the province of Albacete, was known simply as Las Minas. Early production under private ownership was partly traded, mostly among the North African states until it became a crown monopoly from 1589 when it was purchased by Philip II and became a “
coto minero real 
”, a mining restricted area, in order to monopolize the sulphur as a major strategic resource. As such, it is unlikely that any sulphur from this source was traded outside Spain until after 1870 when it returned to private ownership. Mining was carried out by
los de abajio
, 'those of below', living in cave houses on site, supplemented during the Civil War by political prisoners.With such a widespread area to administer and the hazards of trans-Atlantic trade, there was obvious advantage to be gained from local sources within New Spain. The active volcano Popocatépetl in Mexico
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 was mined in the period 1820 - 1920 in spite of eruptions during that period,
Sicily
.In Europe, Sicily was the major supplier of sulphur,
zolfo
, and its production was the main source of employment for much of the population. The technique of extraction was unique and brutally simple. Raw sulphur was stacked in a simple open top furnace leaving verticalair spaces. Sulphur was ignited at the bottom and as the impure sulphur slowly burned, near pure product flowed from the bottom into moulds. The production of sulphur dioxide gas had a devastating effect both on the workers who tended the process and on the surrounding environment killing all vegetation over a considerable area.Fig 3 Sicilian sulphur extraction

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