Janoo, V., R. L. Berg, E. Simonsen, and A. Harrison. 1994. Seasonal
Changes in Moisture Content in Airport and Highway Pavements. Proceedings
of the Symposium on Time Domain Reflectometry in Environmental,
Infrastructure, and Mining Applications, Evanston, Illinois, Sept 7-9, U.S.
Bureau of Mines, Special Publication SP 19-94, NTIS PB95-105789, pp. 357-363
With the introduction of the Strategic Highway Research Program Long-Term
Pavement Performance Study, there has been an increased effort to determine
the influence of environmental factors such as temperature and moisture on
pavement performance. The Federal Aviation Administration (FAA) continues
to sponsor research to improve its pavement design and evaluation
procedures; the effect of environmental factors is one of its
considerations. The new Denver airport was instrumented for this study.
The Corps of Engineers (COE) has instrumented other smaller airports to
study the effect of freeze-thaw on pavement performance. The COE is also
involved in the study of highway pavement performance subjected to
freeze-thaw cycling in Vermont, Maine, New Hampshire, and Minnesota. The
moisture content in the pavement structure is measured with the time domain
reflectometry (TDR) method. We observed the seasonal changes not only in
the soil but also in portland cement concrete pavements. Preliminary
results show a few significant problems with this method in some types of
soil and at high degrees of saturation. The paper presents some early
results and discusses the problems observed at some of the test sites.
Stein, J. and D. L. Kane. 1983. Monitoring the Unfrozen Water Content of
Soil and Snow Using Time Domain Reflectometry. Water Resources Research,
Vol. 19, No. 6, Dec., pp. 1573-1584.
Time domain reflectometry is a technique that can be used to directly
measure the insitu moisture content of soil. The principal objectives of
this field investigation were, apply the TDR technique to monitor the
unfrozen water content in the soil, utilize this technique to determine
snowmelt infiltration into seasonally frozen soils, and explore the
feasibility of using the TDR technique to monitor snowmelt percolation in
the snowpack. An additional goal of this paper was to explain in a
straightforward manner how to use the TDR technique to obtain the liquid
water profile in a soil. Various configurations of parallel transmission
lines were installed horizontally at various depths in the soil and also in
the snowpack. This technique gave good delineation of the unfrozen water
content with depth in frozen soils. Results looked promising in snow if
insitu snow density measurements were taken along with the TDR measurements.
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