Gc. Topp et Wd. Reynolds, TIME-DOMAIN REFLECTOMETRY - A SEMINAL TECHNIQUE FOR MEASURING MASS AND ENERGY IN SOIL, Soil & tillage research, 47(1-2), 1998, pp. 125-132
Soil water exerts a strong influence on the transfer and storage of so
lutes, heat, air, and even water itself, within the soil profile. Soil
water also dominates the mass and energy balance of the soil-atmosphe
re interface. Over the last decade or so, the development and continui
ng refinement of the time-domain reflectometry (TDR) technique for in
situ, nondestructive measurement of water, ionic solutes and air has r
evolutionized the study and management of the transfer and storage of
mass and energy within the soil profile. TDR-measured water content ha
s been applied successfully to water balance studies ranging from the
km scales of small watersheds to the mm scale of the root-soil interfa
ce. TDR-measured ionic solute status, which applies to the same sample
volume as the water content measurement, has been used successfully o
n soil column, held plot and whole field scales for in situ determinat
ion of solute transport parameters, such as pore water velocity and di
spersivity. TDR-measurement of air-filled porosity in space and time h
as given new insights into the mechanisms controlling aeration and gas
eous exchange in the crop root zone. The combined water content - solu
te mass measurement capability of TDR has made this technique a very p
owerful tool for characterizing solute leaching characteristics, as we
ll as for evaluating solute transport theories and solute transport mo
dels. The portability of TDR instrumentation coupled with the simplici
ty and flexibility of TDR soil probes has allowed the separation of wa
ter and solute content measurement error from soil variability, result
ing in the capability for determining the mechanisms behind the spatia
l and temporal variability in held-based soil water content distributi
ons and solute leaching patterns. The usefulness and power of the TDR
technique for characterizing mass and energy in soil is increasing rap
idly through continuing improvements in operating range, probe design,
multiplexing and automated data collection. (C) 1998 Elsevier Science
B,V. All rights reserved.