28
For maximum accuracy, you
may choose to perform a
soil-specific calibration
rather than use either of the internal (Standard or High
Clay) soil calibrations coded into the TDR 300’s firm-
ware. In these cases, an independent soil moisture content
measurement is required. A relation can then be devel-
oped that relates the meter’s period reading (see MODE
button, p. 8) to actual volumetric water content (VWC).
This is most easily accomplished by doing a regression of
one set of data against another.
VWC data can be obtained with a device such as a neutron
probe, by measuring the weight of a saturated soil column
of known volume as it is gradually dried, or by gradually
wetting a known volume soil with the addition of known
increments of water. In most cases, however, the calibra-
tion will be done with gravimetric sampling. This proce-
dure is briefly described below.
In the field, establish a number of sites to sample. Each
site should be wetted to a different soil moisture content
by adding varying amounts of water. At each site a Field
Scout TDR reading is taken followed by the extraction of
a known volume of soil. Ideally, this would be an undis-
turbed soil core. The wet weight of this soil must be de-
termined. If the soil cannot be weighed immediately, it
should be stored in a plastic bag to reduce evaporation.
The soil is then oven-dried (105
o
C for 48 hours is a com-
mon requirement) and weighed again. The volumetric
water content is calculated as follows:
Appendix 2
Soil-Specific
Calibration
Period = 0950 uS
N015