. 1999. An assessment of potato sap flow as affected by soil water status, solar radiation and vapour pressure deficit. Can. J. Soil Sci. 79: 245-253. Water-use of three field-grown potato cultivars (Atlantic, Monona and Norchip) was examined using a commercially available sap flow monitoring system over three consecutive growing seasons. The objectives of the investigation were to utilize the sap flow system to assess the water use of three fieldgrown potato cultivars. This included an assessment of the relationship between environmental conditions, water status and measured sap flow including the plant-to-plant variation in sap flow and an evaluation of relative transpiration in relation to the soil water status.Each cultivar maintained daily sap flow close to the atmospheric potential transpiration until approximately 70% of the available water was depleted. Under conditions where the soil was drier (> 70% depleted), Monona potato plants exhibited a more rapid decline in transpiration than Norchip and Atlantic.Hourly sap flow rates were closely related to solar irradiance, especially under well-watered conditions, with no apparent light saturation point. Vapour pressure deficit effects on sap flow were less pronounced, although maximum vapour pressure deficits encountered were only 2 kPa. The lack of drought tolerance of the potato (Solanum tuberosum L.) crop has been well documented (van Loon 1981). Specific physiological factors such as leaf expansion, cell enlargement, the conversion of intercepted radiation into dry matter and enzymatic activities have all been shown to be affected by soil water MacKerron 1987, 1989). Even under well-watered conditions midday stress response has been observed ( Van der Zaag and Burton 1978). A need exists for accurate irrigation scheduling strategies through assessments of the water relations of potatoes to improve their yield potential, even in regions with abundant rainfall.It is recognized that both photosynthesis (P) and transpiration (T) of well-fertilized crops are proportional to intercepted solar radiation below saturation thresholds when soil water (θ) is non-limiting (Monteith 1966). At low levels of θ, both P and T can be reduced due to an increase in stomatal resistance (r s ) (Campbell et al. 1976). For example, the major factor reducing P during periods of water stress is a decreased availability of CO 2 imposed through an increase in r s . Zelitch (1971) points out that the resistance to water vapour transfer imposed by the stomata, is less than the simultaneous resistance of CO 2 into the mesophyll cells. Thus an increase in r s may conceivably result in a greater relative reduction in T than P. Therefore measurements of T may be a more sensitive indicator of the onset of water stress than measurements of P.In considering the relationship between T and P, Bierhuizen and Slatyer (1965)