With any method for measuring soil water content it is useful to know the spatial sensitivity of the measurement, i.e., what volume of soil is measured and what the distribution of sensitivity is within that volume. We determined this information for the method of time-domain reflectometry (TDR), using a laboratory procedure in which the distribution of water surrounding the waveguides was controlled to give different spatial arrangements of water around the waveguides. The sensitivity is largely confined to a region with a cross-sectional area of approximately 1000 mm2surrounding the waveguides, although a limited sensitivity extends much farther, enclosing 3500 to 4000 mm2. The width of the region of sensitivity normal to the plane containing the wave-guides is approximately 30 mm, indicating that the method should allow excellent depth resolution when the waveguides are installed horizontally, and that it should be possible to place such waveguides within 20 mm of the surface. Finally, there was no discernible variation in sensitivity longitudinally (along the length of the wave-guides).