The practice of chemistry has always been a dirty endeavor. Looking through the old alchemical paintings just outside my office, nearly all of them have one thing in common: smoke. Smokestacks feature prominently in paintings and book covers celebrating the chemical enterprise from the last two centuries. Not that the smoke was always seen as a good thing. Concerns about air pollution and health entered the public debate in Britain not coincidentally about the same time that the alkali factories got up and running. But the smoke and the smokestacks still presented an image of progress. It wasn’t so much about the smoke, as how much smoke.
Purity and impurity: what makes the difference? Well, it depends. It depends upon what you’re trying to do. If you’re fabricating semiconductors, then your water better be as close to pure as you can possible get it. But there’s the rub: how do we know when pure is pure, or impure, or pure enough?
We’ve come a long way from the days when Michael Faraday could offer his card to Father Thames, or when rivers in the United States might catch fire (like the Cuyahoga in Ohio did several times in the 20th century). The divide between pure and impure is no longer something simply visible, or obvious.

The ability to monitor chemicals grew up alongside the more industrial side of chemistry as a way of keeping tabs of what went where.
While in earlier days a public health official might have used a Ringlemann smoke chart as a way of qualifying the dirtiness of the smoke being emitted, today we rely on more sophisticated equipment to help give quality (and quantity) to those elements of the air, water, and soil that we can’t see.
But our ability to see more, to find a trace of a chemical in ever smaller amounts, has had the reciprocal effect of challenging our notions of presence, dose and the purity/impurity divide.
When James Lovelock first introduced his electron capture detector as a new tool for environmental monitoring, scientists gained a new perspective on the world. Traces of pesticides could be found in streams and lakes hundreds of miles from where they were applied. CFCs could be found in the air at sea and in the upper reaches of the ozone layer. Were these molecules not there previously? Of course they were. But now, with the ability to see them, our very ideas about the chemical constitution of the world, and our effect on it, were changing. How much is too much? It depends – how much can you see?
In Making Modernity we’ve tried to show the people, the places, and the tools that made this transformation possible in a way that helps to make visible this ongoing story. It’s been a fascinating task for me. Objects do not speak on their own. An electron capture detector cannot convey the stories that link it to some of the most famous scientific battles of the late-20th century. From the debates about the hole in the ozone layer to Silent Spring, the ECD played a pivotal role. Helping the visitor to see those connections is a little like building an ecological system for the museum. Each piece depends upon its positioning, its place, and its connections for the story to unfold in precisely the right way. And, with luck, the story will keep evolving.
Jody Roberts is program manager for environmental history and policy in the Center for Contemporary History and Policy at CHF