Data fields: groundwater level
Groundwater level observations made manually with a dipping tape are available. The frequency of observations varies from monthly to once every six months, with significant missing periods across different drillholes depending on the monitoring requirements.
There are three different datums in which groundwater level data is available. This figure shows how they inter-relate:
Automated groundwater level measurements are available for some monitoring wells on the Aquarius Web Portal at Water Data SA. These measurements are not available through Groundwater Data.
Depth to Water (DTW)
This is the depth to water level in metres measured below a reference point. Increasing numbers indicate an increasing depth to water. Negative numbers indicate flowing artesian conditions. The reference point’s true elevation above ground surface can change i.e. if a casing standpipe is installed, removed, or modified, so although this number is the “raw measurement” it should generally not be used for analysis.
Warning
Do not use Depth to Water for analysis.
Standing Water Level (SWL)
This is the Depth to Water, automatically corrected such that it represents a depth below ground level. Increasing numbers indicate an increasing depth to water. Negative numbers indicate flowing artesian conditions. The SWL and DTW values are only different when well elevation data is available and the two elevation values (of the reference point, and the ground) are different - the difference is used to calculate the SWL. If they are the same (e.g. maybe the elevation was derived from a digital elevation model), or no elevation data is available, then the SWL will be present but it will be identical to the DTW.
Note
Use Standing Water Level for all trend or status analysis of data from individual wells.
Reduced Standing Water Level (RSWL)
This value has been corrected to represent the groundwater level measured above Australian Height Datum (AHD). Increasing numbers indicate a decreasing depth to water. RSWL values are only present when we have an elevation survey for that well. This is obviously the correct value to use for most purposes, if it is available.
Note
Use Reduced Standing Water Level for all analysis of data between wells i.e. groundwater flow analysis.
Fields and field names are listed below for: the CSV file obtainable from Groundwater Data; the JSON returned
by GetWaterLevelDetails; and the pandas DataFrame returned by sa_gwdata.water_levels()
. A dash
indicates the field is missing.
Property |
Description |
CSV |
DataFrame |
JSON |
---|---|---|---|---|
Alternative unique well ID |
DHNO |
dh_no |
||
Observation well network |
Not all wells are part of a network - most are not, in fact. |
network |
network |
|
Unit number (integer format) |
Alternative unique well ID |
Unit_Number |
unit_long |
|
Aquifer monitored |
Aquifer interval(s) opposite the production zone |
Aquifer |
aquifer |
|
UTM easting |
Easting |
easting |
||
UTM northing |
Northing |
northing |
||
UTM zone |
Zone |
zone |
||
Unit number (hyphenated) |
Alternative unique well ID |
Unit_No |
unit_hyphen |
|
Obswell number |
Alternative unique well ID - not assigned for all wells |
Obs_No |
obs_no |
|
Water level observation date |
obs_date |
obs_date |
OBS_DATE |
|
The actual measurement recorded in most cases |
dtw |
dtw |
||
Automatically derived from DTW |
swl |
swl |
STANDING_WATER_LEVEL |
|
Automatically derived from RSWL |
rswl |
rswl |
REDUCED_STANDING_WATER_LEVEL |
|
Pressure |
pressure |
pressure |
||
Temperature |
temperature |
temperature |
||
Dry indicator |
dry_ind |
dry_ind |
||
Anomalous indicator |
Y/N indicating anomalous data |
anom_ind |
anomalous_ind |
ANOMALOUS_IND |
Pumping indicator |
Y/N indicating that pumping was observed locally at the time of measurement |
pump_ind |
pump_ind |
PUMPING_IND |
Measured during |
measured_during |
measured_during |
MEASURED_DURING |
|
Data source |
data_source |
data_source |
DATA_SOURCE_CODE |
|
Comments |
Comments |
comments |