Author： Wollschläger Ute Roth Kurt
Publisher： Springer Publishing Company
ISSN： 1566-0184
Source： Subsurface Sensing Technologies and Applications, Vol.6, Iss.2, 2005-04, pp. : 207-218
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Abstract
Time series of ground-penetrating rader traces are used to monitor temporal changes of soil water content down to about 1.5 m. The results are compared with high-resolution time series of time-domain reflectometry measurements at a few locations in the soil profile. We find a reasonable agreement between the two approaches and discuss the differences in terms of their respective limitations.
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