The leaching and migration of radionuc1ides from shallow land burial sites is controlled by the amount, composition and mobility of soil water. The measurement of soil water together with the prediction and monitoring of its behavior in soil is critical to the proper design and operation of a burial site. The amount of water present may be measured and expressed as cubic meters of water per cubic meter of soil, or the soil water pressure may be measured and expressed as bars. The amount of water is called the water content and the pressure is referred to as the water potential. Low-level waste management has two major tasks that require the ability to measure soil water potential. There are the soil hydraulic characterization studies performed during selection of a burial site, and the monitoring of soil water during site operation and post-closure. Soil hydraulic characterization requires the determination of two basic relationships, the relationship between soil water content and soil water potential, known as the soil water characteristic, and the relationship between hydraulic conductivity ~nd soil water potential. Monitoring activities include the long term measurement of soil water potential at active as well as retired burial sites.There are four basic types of sensors used to measure soil water potential. These are: 1) tensiometers; 2) soil psychrometers; 3) electrical resistance blocks; and 4) heat dissipation probes. Tensiometers are designed to measure the soil water potential directly by measuring the soil water pressure. This is done by linking a pressure gage or manometer to a porous ceramic cup buried in the soil. The tensiometer has high precision (millibar), but a limited range (0 to -0.8 bars). Tensiometers perform best in loamy soils, and are difficult to use in sandy soils. They also have depth limitations and require regular maintenance. Soil psychrometers are sensors that infer water potential from a direct measurement of the relative humidity of the soil air. These sensors rarely achieve a precision of greater than 0.5 bars, and this is only in soils drier than -1 bar. The lower limit to soil psychrometry ranges from -70 to -90 bars depending on the soil temperature. Psychrometers are very sensitive to temperature gradients present in the so;l and also seem to ; ; i '.