archiving of SOWACS
proudly sponsored by

this could be your logo - >

[Date Prev][Date Next][Thread Prev][Thread Next][Date Index][Thread Index]

Re: Tensiometers: data variability vs TDR



NOTE:  To get off this list, send email to majordomo@aqua.ccwr.ac.za
with the body of the message containing the line:
unsubscribe sowacs

I conducted an experiment seven years ago to measure volumetric water
content for potting soil from 0 - 0.50 m3/m3 moisture range.

I found that TDR can be used to accurately measure volumetric water content
in potting soil. I prefer to express the time delay as T/Tair, the ratio of
propagating time in medium to that in air with the same travel distance
science the relationship between T/Tair vs. volumetric water content is
linear. The experimental results show:

1. Volumetric water content = (T/Tair - Ts/Tair)/[sqrt(dielectric constant
of water)-1]

2. The slope of the regression line (T/Tair vs. volumetric water content)
for potting soil is almost the same as  that for fine sand (0.1256 vs 0.1263
with R2 = 0.995).

3. The X intercept (Ts/Tair, the ratio of propagating time in dry soil to
that in air with the same travel distance) needs to be adjusted. For loamy
soil Ts/Tair value is approximately 1.55 and for potting soil it should be
adjusted to approximately 1.14. This adjustment is required because the
dielectric constant of dry loamy soil is different to that of dry potting
soil, not related to so-called "isolated water".
4. Part of the results has been published in Soil Science of American
Journal volume 60, 1996. More details can be found in my Ph.D thesis.

Z. J. Sun Ph.D
Research Scientist
ESI Environmental Sensors Inc.
100-4243 Glanford Avenue
Victoria, BC, Canada
V8Z 4B9
Tel: 250-479-6588
Fax: 250-479-1412
e-mail: jason@esica.com