
CS725 Snow Water Equivalent Sensor
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2. Cautionary Statements
•If you are unable to determine that your structure or mounting method is
suitable for the CS725 sensor, please contact Campbell Scientific for
assistance in determining the structural mounting requirements.
•We recommend installing this CS725 before there is snow on the ground
to establish a baseline SWE.
•Always ensure that when using a collimator, it is secured to the structure
with the safety cable provided. Due to its weight, the collimator should be
handled with caution.
•Do not disassemble the CS725 without consulting the factory. The CS725
contains a fine bead-like insulation material - Aerogel Nanogel (Cabot
Corporation). Proper MSDS sheets and instructions should be obtained
prior to opening the CS725.
•Never force the connector on to the CS725. If the connector does not
easily fit into place, it is likely misaligned.
3. Initial Inspection
•Upon receipt of the CS725, inspect the packaging and contents for
damage. File any damage claims with the shipping company. Immediately
check package contents against the shipping documentation. Contact
Campbell Scientific about any discrepancies.
•The model number and cable length are printed on a label at the
connection end of the cable. Check this information against the shipping
documents to ensure the expected product and cable length are received.
•The CS725 is shipped with a DB9F-TERM for communication, and a
safety cable.
4. Overview
The CS725 sensor is a gamma radiation spectrometer that has been specifically
designed to measure SWE. The CS725 utilizes a Thallium-doped Sodium
Iodide crystal NaI(Tl) to detect gamma radiation.
Naturally-occuring terrestrial gamma radiation is produced by traces of
radioactive elements in the earth. The most abundant of those elements are
Potassium_40 (40K) and Thallium_208 (208Tl). 40K emits gammas at 1.460
megaelectronvolts (MeV), and 208Tl at 2.613 MeV. Gamma rays have a well
defined “probability of interaction”, based on the energy of the gamma and the
nature of the material it is travelling through.
The net effect of gamma rays travelling through the snow pack, is that a
fraction of the rays interact with the snow, while another fraction is either
degraded in energy, or attenuated. Quantifying the attenuated gamma rays
provides necessary information to calculate the SWE within the CS725. As
such, the CS725 should be installed prior to snowfall to acquire a baseline