Therfield Rectory

Water levels have been recorded at Therfield Rectory in Hertfordshire since 1883, and it is one of the few sites with continuous monitoring prior to 1900.

Our enquiries service can help you to access groundwater level data for this well.

Hydrograph


hydrograph

Show data from :-
1883 to 1949 1950 to 2013 1970s 1980s 1990s 2000s 2010s


Information about the well

Therfield Rectory
Wellmaster ID TL33/4
NGR 5335 2369
Datum 154.81  m AOD
Monitoring details
Type Groundwater Level
Aquifer Chalk
Confinement Confined
Depth 83.23 m
Record
Monitored by EA Thames
Records commence 1883
Records end Active

Map of Washpit Farm showing geology and water level contours.

Hydrogeological setting

This well penetrated the Lewes Nodular Chalk Formation and Seaford Chalk Formation (undifferentiated). The Chalk aquifer is overlain, and confined, by 3 metres of low permeability Lowestoft Formation till.

Well or borehole construction

The well consists of an 83.23 m deep, 1.52 m diameter well brick lined to 4.57 m.

The well was originally only 81.1 m deep, it was deepened to 84.1 m deep prior to measurements commencing in 1883. When plumbed in 1992, it was found to be only 83.2 m deep, presumably due to silting.

Hydrograph response

The well hydrograph has an annual sinusoidal appearance, except when it goes dry. As the average thickness of the unsaturated zone is between 75 and 80 metres below ground level, there is normally a two to three month time lag between the start of winter recharge and when the water level starts rising. The time lag has been known to reach 5 months.

Data issues

The method used to measure the water level in the earliest measurements was presumably a line with some kind of float on the end. These lines underwent considerable amounts of stretching and shrinking over time. Between the start of records in 1883 and August 1885 the line was found to have stretched 3.5 metres, between September 1885 and December 1895 it had stretched a further 4.0 m. The line used between July 1903 and February 1923 stretched 6.9 m over this period. Whereas the line used from May 1921 to December 1937 shrank 2.2 m, and a further 4.2 m by May 1949. Measurements were corrected assuming that the stretching and shrinkage had occurred uniformly, which may not have been the case.

There are no records for the period June 1952 and June 1956 and there is a note on the file that the EA consider the levels for the period between 1914 and 1920 as very dubious.

In 1999 a dedicated observation well was constructed at Hay Farm (TL33/67) and this has replaced Therfield Rectory as an Index Well.

References

Ó Dochartaigh, B. 1999. Long groundwater records: Processing and presentation of the Therfield Rectory Hydrograpgh. BGS Report WD/99/11.

Contact

Contact Andrew McKenzie for further information