CS655 12 cm Soil Water Content Reflectometer

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1. Can the cable for the CS650 or CS655 be shortened?

   Modifications to the CS650 or CS655, including shortening the cable, will void the warranty. However, shortening the cable will not affect the sensor’s performance. If a decision is made to shorten the cable, care should be taken to avoid damaging the cable jacket and exposing bare wire except at the ends that connect to the data logger or multiplexer terminals.

2. Can the CS650 and the CS655 be repaired?

   Damage to the CS650 or the CS655 electronics or rods cannot be repaired because these components are potted in epoxy. Cable damage, on the other hand, may possibly be repaired. For more information, refer to the Repair and Calibration page.

3. Can the CS650 and the CS655 measure water content in concrete?

   Some customers have successfully used water content reflectometers, such as the CS650 and the CS655, to measure water content of wet concrete mix to ensure consistency between different batches of concrete. However, after concrete begins the curing process, salts are formed that make the electrical conductivity too high for the CS650 and the CS655 to operate. Thus, these sensors cannot be embedded in wet concrete to measure the water content of the concrete as it cures and dries.  

4. Can the CS650 and the CS655 measure water content in gravel?

   Yes. Keeping the sensor rods parallel during installation is especially difficult in gravel, but it can be done. Gravel has large pore spaces that drain quickly, so the water content readings will likely show rapid changes between saturation and very dry. If small changes of water content at the dry end are of interest, a soil-specific calibration may need to be performed to convert period average directly to volumetric water content.

5. Using a CS650 or a CS655, when should a soil-specific calibration be performed?

   To get accurate water content readings, a soil-specific calibration is probably required if any of the following are true:

   • The soil has more than 5% organic matter content.
   • The soil has more than 20% clay content.
   • The soil is derived from volcanic parent material.
   • The soil has porosity greater than 0.5.

   For details on performing a soil-specific calibration, refer to “The Water Content Reflectometer Method for Measuring Volumetric Water Content” section in the CS650/CS655 manual.

6. With regard to the CS650 and the CS655, is there a generic calibration equation for artificial soil?

   No. The equation used to determine volumetric water content in the firmware for the CS650 and the CS655 is the Topp et al. (1980) equation, which works for a wide range of mineral soils but not necessarily for artificial soils that typically have high organic matter content and high clay content. In this type of soil, the standard equations in the firmware will overestimate water content.

   When using a CS650 or a CS655 in artificial soil, it is best to perform a soil-specific calibration. For details on performing a soil-specific calibration, refer to “The Water Content Reflectometer Method for Measuring Volumetric Water Content” section in the CS650/CS655 manual. A linear or quadratic equation that relates period average to volumetric water content will work well.

7. How can it be determined if the NAN values are caused by soil conditions or a faulty CS650 or CS655 sensor?

   Three of the values returned by the M3! command are never changed to NAN by logical tests. If non-zero readings for soil temperature, period average, and voltage ratio are displayed, the sensor is working.

   A simple test in air and water will also show whether the CS650 or CS655 is functioning. When performing this test, look at the permittivity value and not the water content value. In air, the sensor will read a permittivity value of 1. In room-temperature water, the value should be close to 80. The water container should have a diameter of at least 20 cm (8 in.) and a depth of 33 cm (13 in.). A smaller container will result in a lower permittivity value because the sensor will be measuring some of the air outside the container as well as the water. Tap water is acceptable for this test.

8. With the CS650 and the CS655, where is the soil temperature measurement made?

   A thermistor is encased in the epoxy head of the sensor next to one of the stainless-steel rods. This provides an accurate point measurement of temperature at the depth where that portion of the sensor head is in contact with the soil. This is why a horizontal placement is the recommended orientation of the CS650 or CS655. The temperature measurement is not averaged over the length of the sensor rods.

9. Can the CS650 and the CS655 measure water content in greenhouse pots?

   Yes, but the pots would have to be large. The CS650 and CS655 can detect water as far away as 10 cm (4 in.) from the rods. If the pot has a diameter smaller than 20 cm (8 in.), the sensor could potentially detect the air around the pot, which would underestimate the water content. In addition, potting soil is typically high in organic matter and clay, causing the probable need for a soil-specific calibration. 

10. Can the CS650 and the CS655 measure water content in compost?

    Campbell Scientific does not recommend using the CS650 or the CS655 to measure water content in compost. A compost pile is a very hostile environment for making dielectric measurements with soil water content sensors. All of the following combine to make it very difficult to determine a calibration function: high temperature, high and varying electrical conductivity, high organic matter content, heterogeneity of the material in the pile, changing particle size, and changing bulk density. The temperature and electrical conductivity values reported by the CS650 or CS655 may give some useful information about processes occurring in the compost pile, but these sensors will not be able to give useful readings for water content.