Abstract

Scientific chemical production on a commercial scale was evident in Britain in the early nineteenth century. One of the first palaeotechnic chemical industries was the manufacture of synthetic alkali. By 1823 a well-defined pattern of soda production had emerged. An understanding of this initial distribution is important as those areas associated with the early growth of the synthetic alkali industry showed a remarkable continuity of inorganic chemical production for the remainder of the century. The paper attempts to consider those factors which contributed to this selective regional response, and in doing so, a number of interesting factors of location are revealed