The Province operates a network of observation wells to provide data on ground water level fluctuations and ground water quality information on developed aquifers in British Columbia. Observation well water levels are monitored using one of four methods: 1) manually with a wetted tape, 2) continuously using Steven's chart recorders, 3) electronically with data loggers or 4) remote monitoring using cellphone technology.
Water level data from observation wells are collected on a monthly basis by field observers and forwarded to Regional Offices. Data are then checked for errors and ommissions and forwarded to the Water and Air Monitoring and Reporting Section for final checking and storage. Water level data are referenced from ground level and the month end water level reading are entered and stored in Excel to produce a month-end hydrograph. The method of measurement and accuracy of each method are given below:
|Method of measurement||Accuracy|
|Wetted Tape Method||+/- 1 mm|
|Steven's Chart Recorder||+/- 1 mm|
|Data Logger||+/- 0.1 %|
Hydrograph Analysis- Observation Well No.127
The hydrograph above shows the change in ground water level in the observation well (meters below ground level) over time. The well water level was monitored by a Steven's recorder, which monitors the ground water level fluctuations in the observation well. In 1996, the observation well was abandoned at the request of the property owner.
Observation well No.127
is completed to a depth of 71.6 m in an undelineated, bedrock aquifer. Between
1972 and 1996, the ground water level in the well ranged from a high of 0.1
m below ground level in March 1989, to a low of 2.3 m below ground level in
October 1973. The difference between maximum and minimum ground water levels
in any single year ranges from approximately 1.0 (in 1990) to 1.7 (in 1989)
meters. The hydrograph shows that ground water levels in this observation
well follow a regular seasonal pattern. Maximum ground water levels occur
in March and April and minimum ground water levels occur in the months of
October, November and December. Ground water levels for this observation well
have generally remained at a dynamic equilibrium for the period of record.