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A sough (pronounced /saʊ/ or /sʌf/) is an underground channel for draining water.
Out of a mine: ideally the bottom of the mine would be higher than the outlet, but where the mine sump is lower, water must be pumped up to the sough.
Out of sloping farmland: these are to be found (at least) around the Pennine areas of East Lancashire to carry water from higher up, down through the clay based fields to reduce flooding and soft ground.
Derbyshire lead mining
The term is closely associated with the lead mining areas of Derbyshire (see Derbyshire lead mining history). Early Derbyshire lead mines were fairly shallow, since methods to remove water were inefficient and miners had to stop when they reached the water table. By digging soughs, miners found they could lower the water table and allow mines to be worked deeper.
Soughs were typically dug from their open end near a stream or river back into the hillside beneath the mine to be drained. One sough would often drain more than one mine, since these were often very close, working the same vein of lead. This also helped spread the cost of digging the sough. Some soughs include branches to facilitate further drainage.
Many soughs were dug throughout the 17th and 18th centuries. The falling price of lead brought the decline of the Derbyshire lead mining industry towards the end of the 19th century.
Some soughs were very extensive. Meerbrook sough is over four miles in length. Digging such long tunnels took a long time. Vermuyden sough, named after the Dutch engineer, Cornelius Vermuyden, who planned it, took 20 years to dig. The Cromford sough, which Sir Richard Arkwright subsequently used to power his mill at Cromford, took 30 years to dig. It was still being extended a century after construction began.
Some soughs are still in use. According to the British Geological Survey, the Meerbrook sough, started in 1772, still provides 3.75 million litres (990,000 US gal) a day for the public water supply.
The Sough drains of East Lancs
The date of the construction of these ancient field drains is currently unknown, they are the forerunner to the modern plastic perforated land drain pipe and were built by hand. First by digging a deep trench anywhere from 30 to 90cms deep where the water was naturally gathering and/or where it was to be diverted. Sometimes the larger drains had flat stone bottoms, the smaller poor quality ones did not. Sides were then formed in the same way as a dry stone wall by stacking interlocking stones. These were then capped off by large flatter stones (to form a tunnel) and rubble (both stones, broken pottery and glass) thrown around the outside and on top before the clay and soil were put back and the grass left to grow. Not only do they divert water from higher ground under the fields to a lower open watercourse, they also take it from the fields themselves as it percolates through into them.
Many drains are now suffering blockages from clay or iron ochre leaching in and collapse. The latter caused naturally, but also from the weight of modern heavy farm machinery driving over them.
Elsewhere
The coal mining industry depended on using soughs until the mines became too deep to be drained by this means. With the advent of the steam engine, which could pump out water, soughs became less necessary for de-watering mines.
See also
References
- ^ Water Wars: Meerbrook Sough, British Geological Survey, accessed 30 October 2012
- J. Hatcher, History of the British Coal Industry: Before 1700: Towards the Age of Coal (Oxford 1993)
External links
- Water Wars: Meerbrook Sough, British Geological Survey
Further reading
- Rieuwerts, J. H. History and gazetteer of the lead mine soughs of Derbyshire. Author, 1987