
© 2005 Delta-T Devices Ltd Page 7
a0a1
Mineral 1.6 8.4
Organic 1.3 7.7
Example
Take a reading with the SM200 V= 0.294 volts
either
Convert the reading to √ε using the polynomial or
linearisation table below. √ε = 3.62
Then convert √ε to soil moisture, θ, using the soil
calibration values (a0, a1). θ= 24.0%
or (for mineral soil)
Convert directly for mineral or organic soils θ= 24.0%
5 Convert SM200 voltages to soil moisture readings
Note: The SM200 output is automatically converted to soil moisture when using an
HH2 meter or Delta-T data loggers.
Conversion to √ε
Polynomial (use for SM200 readings from 0 to 1.1 Volts)
5432 536.13032.46881.60725.38103.160.1 VVVVV +−+−+=
ε
where Vis the SM200 output in volts
Linearisation table (use for SM200 readings from 0 to 1.2 Volts)
V√ε V√ε V√ε V√ε V√ε
0.000 1.011 0.120 2.461 0.260 3.442 0.820 5.936 1.150 7.661
0.030 1.447 0.150 2.718 0.310 3.700 0.960 6.586 1.200 8.039
0.060 1.832 0.180 2.946 0.400 4.105 1.040 6.991 1.220 8.264
0.090 2.168 0.220 3.211 0.600 4.953 1.100 7.333 1.800 9.000
Conversion from √ε to Soil Moisture
Soil moisture
10 aa−=
εθ
Use these generalised soil calibration values for
mineral and organic soil types, or carry out a soil-
specific calibration to derive your own values – see SM200 User Manual.
Multiply x100 to convert soil moisture from m3.m-3 to % volumetric.
Direct conversion for Mineral and Organic soils
5432
mineral 611.148.5248.761.4917.1071.0 VVVV +−+−+−=
θ
5432
organic 758.1978.5907.7029.5091.2039.0 VVVVV +−+−+−=
θ