Water-meadow

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A water-meadow (also water meadow or watermeadow) is an area of grassland subject to controlled irrigation to increase agricultural productivity. Water-meadows were mainly used in Europe from the 16th to the early 20th centuries. Working water-meadows have now largely disappeared, but the field patterns and water channels of derelict water-meadows remain common in areas where they were used, such as parts of Northern Italy, Switzerland and England. Derelict water-meadows are often of importance as wetland wildlife habitats.

Water-meadows should not be confused with flood-meadows, which are naturally covered in shallow water by seasonal flooding from a river. "Water-meadow" is sometimes used more loosely to mean any level grassland beside a river.

Types of water-meadow[edit]

Two main types of water-meadow were used.

Catchwork water-meadow[edit]

These were used for fields on slopes, and relatively little engineering skill was required to construct them. Water from a stream or spring was fed to the top of a sloping field, and gentle sloping terraces were formed along which the water could trickle in a zig-zag fashion down the field. The water could be used again for fields lower down the slope.

Bedwork water-meadow[edit]

Flooded derelict bedwork water-meadow at Fordingbridge, Hampshire, England. Winter flooding has filled an old carrier channel along the crest of a ridge (running from right foreground to middle distance), and has also flooded the drainage channels (on left and into distance, where they join the river). In use, water would have seeped from the carrier channel on the right, through the grass in the foreground into the drainage channel on the left, which would have been almost empty.

Bedwork or floated water-meadows were built on almost-level fields along broad river valleys, and required careful construction to ensure correct operation.

A leat, called a main, carrier or top carrier, was used to divert water from the river and carry it down the valley at a gentler slope than the river, producing a hydrostatic head between the two. Mains were often along the edge of the valley, each main supplying up to about 1 km (0.6 mi) of the valley. The water from the main was used to supply many smaller carriers, on the crests of ridges built across the fields. The channel on the crest of each ridge would overflow slowly down the sides (the panes) of the ridge, the channel eventually tapering to an end at the tip of the ridge. The seeping water would then be collected between the ridges, in drains or drawns, these joining to form a bottom carrier or tail drain which returned the water to the river. The ridges and the drains made an interlocking grid (like interlaced fingers), but the ridge-top channels and the drains did not connect directly. A by-carrier took any water not needed for irrigation straight from the main back to the river. The ridges varied in height depending on the available head – usually from around 10 to 50 cm (4 to 20 in). The pattern of carriers and drains was generally regular, but it was adapted to fit the natural topography of the ground and the locations of suitable places for the offtake and return of water.

The water flow was controlled by a system of hatches (sluice gates) and stops (small earth or wooden-board dams). Irrigation could be provided separately for each section of water-meadow. Sometimes aqueducts took carriers over drains, and causeways and culverts provided access for wagons. The working or floating (irrigation) and maintenance of the water-meadow was done by a highly skilled craftsman called a drowner or waterman, who was often employed by several adjacent farmers.

The terminology used for watermeadows varied considerably with locality and dialect.[citation needed]

Uses of water-meadows[edit]

Water-meadow irrigation did not aim to flood the ground, but to keep it continuously damp – there is no standing water in a working water-meadow. Irrigation in early spring kept frosts off the ground and so allowed grass to grow several weeks earlier than otherwise, and in dry summer weather irrigation kept the grass growing. It also allowed the ground to absorb any plant nutrients or silt carried by the river water – this fertilised the grassland, and incidentally also reduced eutrophication of the river water by nutrient pollution. The grass was used both for making hay and for grazing by livestock (usually cattle or sheep).

Derelict water-meadows[edit]

Former water-meadows are found along many river valleys, where the sluice gates, channels and field ridges may still be visible (however the ridges should not be confused with ridge and furrow topography, which is found on drier ground and has a very different origin in arable farming). The drains in a derelict water-meadow are generally clogged and wet, and most of the carrier channels are dry, with the smaller ones on the ridge-tops often invisible. If any main carrier channels still flow, they usually connect permanently to the by-carriers. The larger sluices may be concealed under the roots of trees (such as crack willows), which have grown up from seedlings established in the brickwork. The complex mixture of wet and drier ground often gives derelict water-meadows particularly high wetland biodiversity.

Further reading[edit]

  • Hadrian Cook and Tom Williamson (eds.), Water Management in the English Landscape: Field, Marsh and Meadow. Edinburgh: Edinburgh University Press, 1999.

External links[edit]