The CS725 measures snow-water equivalent (SWE) by passively detecting the change in naturally occurring electromagnetic energy from the ground after it passes through snow cover. It is mounted above the ground and has no contact with the snow. As the snow pack increases, the sensor detects the attenuation of the electromagnetic energy from the ground, and SWE can be calculated. The measurement area of the CS725 is 50 to 100 square meters (540 to 1,075 square feet), making it an excellent replacement sensor for the traditional snow pillow and snow scale.
Common applications for the CS725:
The CS725 uses an innovative, non-contact method of measuring snow water equivalent (SWE). It passively detects the change in naturally occurring electromagnetic energy (mainly from the decay of 40K) from the ground after it passes through snow cover.
As SWE changes, the amount of energy that penetrates the snow pack changes—regardless of the state of the water (that is, liquid or frozen). A sensor installed above the ground prior to the first snowfall will have a base-line measurement of the electromagnetic energy coming from the ground. As snow accumulates and energy is attenuated, the SWE value will increase. The CS725 has an internal processor that determines the SWE and sends this information to a datalogger or communication device via RS-232.
Measurement Range | 600 mm maximum water equivalent |
Accuracy |
|
Resolution | 1 mm |
Coverage Angle | 60° |
Operating Temperature Range | -40° to +40°C |
Power Requirements | 11 to 15 Vdc |
Power Consumption | 180 mA |
Output Options | RS-232 (1200 to 115200 bps) |
Cable Type | Four conductor, two-twisted pair, 22 AWG, Santoprene jacket |
Warranty | 2 years |
Maximum Cable Length | 30 m (98.43 ft) |
Diameter | 12.7 cm (5 in.) |
Length | 62 cm (24.4 in.) |
Main Body Weight | 9 kg (20 lb) |
Collimator Weight | 25 kg (55 lb) |
Total Weight | 34 kg (75 lb) |
Please note: The following shows notable compatibility information. It is not a comprehensive list of all compatible products.
Other sources of electromagnetic radiation (40K) such as trees, vegetation, and buildings that are not covered by the same amount of snow as the ground can affect the readings. To filter these signals, the optional heavy steel collar (collimator assembly, pn 29390) is installed on the bottom of the CS725.
The following chart outlines when a collimator should be used:
Site Characteristics | Maximum SWE 300 mm | Maximum SWE 300 to 400 mm | Maximum SWE > 400 mm |
Very open site with no proximity to trees, buildings, or tall vegetation within a 48 m (160 ft) radius |
Optional |
Optional |
Optional |
No trees, buildings, or tall vegetation within a 24 m (80 ft) radius |
Optional |
Optional |
Required |
No trees, buildings, or tall vegetation within a 12 m (40 ft) radius |
Optional |
Required |
Required |
Site with minimum clearance radius of 6 m (20 ft) radius |
Required |
Required |
Required |
Note: Always confirm that your sensor has the “Collimator Installed” parameter set properly. The SWE calculations are different for a sensor with and without a collimator.
Number of FAQs related to CS725: 5
Expand AllCollapse All
The sensor takes the measurement and outputs data in RS-232 format. If your data logger can receive RS-232 signals, it should work with the CS725. It’s also best that the data logger can measure volumetric soil moisture.
Yes, however the data would have to be back-calculated at the end of the season once all snow has melted, you would not have real-time SWE measurements.
No, it only measures naturally emitted gamma radiation coming from the ground. The strongest signal of gamma comes from potassium-40 (40K).
No, at this time the sensor does not output in SDI-12 format; however, it may be added in the future.
We've updated our privacy policy. Learn More
Update your cookie preferences. Update Cookie Preferences