Levelogger Series User Guide - Software Version 4
Page 11
1.2.3 Temperature
Leveloggers record temperature compensated water levels. Groundwater and
surface water temperature measurements are particularly important in situations
where temperatures may fluctuate significantly, and when temperature is used
in determining liquid level, viscosity and hydraulic conductivity. Temperature
monitoring is vital in the calculation of certain temperature dependent contaminant
reaction rates. A Platinum Resistance Temperature Detector is used to accurately
compensate for temperature changes within the range of 0 to +50ºC for the
Levelogger Edge, -10ºC to +50ºC for the Barologger Edge, 0 to +40ºC for the
Levelogger Junior Edge, and 10 to +40 for the LTC Levelogger Junior. The
Levelogger will record temperature in its thermal range of -20 to +80ºC, but
outside the range, compensation will be less accurate.
1.2.4 Conductivity
The LTC Levelogger Junior provides the added feature of electrical conductivity
measurement. It measures the actual conductivity at the current temperature.
Conductivity measurement is particularly useful in monitoring saltwater intrusion,
surface water infiltration and mixing, as well as the monitoring of certain pollutants
and contaminant parameters. Conductivity is measured via a platinum 4-electrode
sensor, which produces highly stable and consistent readings. Conductivity
calibration is performed by using a liquid solution with a known conductivity
value and the Calibration Wizard in the Levelogger Windows Software. The Data
Compensation Wizard allows you to convert conductivity readings to Specific
Conductance (at 25ºC), or Salinity expressed in Practical Salinity Units (PSU).
A Practical Salinity Unit (PSU) is a dimensionless descriptor for the Practical
Salinity Scale (PSS). The PSS defines salinity as the ratio of a water sample's
conductivity to that of a standard KCL solution. The Data Compensation
Wizard uses the equation given in the UNESCO Technical Paper "Algorithms
for computation of fundamental properties of seawater", to convert Conductivity
readings to Salinity. For more information, see: Fofonoff, N. P. and R.C. Millard,
Jr. Algorithms for computation of fundamental properties of seawater, UNESCO,
Tech. Pap. Mar. Sci.,44.
1.2.4.1 Calibration of the Conductivity Sensor
The conductivity sensor of the LTC Levelogger Junior is a highly sensitive device
requiring regular calibration by the user. The conductivity calibration frequency
is dependent on the water quality of the Levelogger’s monitoring environment.
To determine whether an LTC Levelogger Junior should be re-calibrated, test
the unit in a solution with a known electrical conductivity value at a reference
temperature. In Real Time View, observe current readings by using the Read
Now function. If this reading varies from the known Specific Conductance of the
solution by greater than 2% of the Full Scale of Conductivity measurement, the
unit should be re-calibrated using the Conductivity Calibration Wizard procedure
outlined in Section 6. As a minimum, calibrate your LTC Levelogger Junior at
least twice a year. Ensure that a conductivity calibration is performed when the
LTC Levelogger Junior is being set up for its initial use and after long periods of
dry storage.
1.2.5 Total Rainfall
The Solinst Rainlogger is designed to record the tip times of an external tipping-
bucket rain gauge, and output the amount of rainfall per tip.
NOTE
For every degree change in
temperature, there is approximately
a 2% change in conductivity.
To convert raw conductivity
measurements to Specific
Conductance measurements, you
can use the following equation:
Specific Conductance =
Conductivity / (1 + 0.02 *
(temp(C) - 25))
You can also perform this
calculation automatically using the
Data Compensation Wizard.