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All FAQs
(1762 total: showing 281-300)
Can the CS616 or CS625 be measured with a 21X or CR7 datalogger?
Can the CS616 be used with CR200- or CR200X-series dataloggers?
When the soil becomes completely saturated, does the CS616/CS625 still provide accurate readings, or does it display “NAN”?
How can the relative dielectric permittivity value be calculated from the available output of the CS616 or the CS625?
What might cause a CS616 or CS625 signal to keep reading -6999?
What might cause a “NAN” readout for a CS616 or CS625?
With the CS616 or CS625, what is the method for correcting for temperature fluctuations?
If a CS616 or CS625 is removed from one site and placed at another site, is there any resetting or recalibration that needs to be done?
If the rods on the CS616 or CS625 get bent, can they be bent back to parallel again without negatively affecting future measurements?
Is it possible to cut the rods of the CS616 or the CS625?
Is there any temperature dependence in CS616 or CS625 measurements?
How many CS616 probes can be connected to a CR1000?
Can the CS616 or CS625 be connected to a multiplexer?
Can measurements from a CS616 be read by a non-Campbell Scientific datalogger?
Can measurements from a CS625 be read by a non-Campbell Scientific datalogger?
Can the CS625 be measured with a CR1000 datalogger?
What soil moisture range can be measured with the CS616 or CS625?
Do the CS616 and CS625 work correctly in soil that has a lot of fine roots?
Can a CS616 or CS625 be used to measure the moisture content within a tree?
Are the CS616 and CS625 waterproof? For example, can they withstand being covered with water, sand, and soil?
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