OGG (1964a,b) has recently reviewed the importance of irrigation in H agricultural and horticultural practice in this country. The usual method of irrigating is to apply the water either through oscillating spraylines or through rotary sprinklers. In both methods the water reaches the ground in the form of drops falling freely under gravity, and therefore the effect is similar to that of natural rain except that the rate of precipitation with irrigation-1 in. of water in from 4 to 8 hr-is normally greater. Also, irrigation is likely to be needed in hot, sunny weather when rain does not usually occur. Commercial growers often ask whether the irrigation water may have an adverse effect on growth by suddenly cooling the plant and soil below the prevailing temperatures, for an appreciable chilling of the air is often noticed when irrigation is being applied on a large scale. I t is sometimes suggested that it might be better to use surface water rather than borehole water simply because it tends to have a rather higher temperature, and it is not unknown for growers to attempt to heat the water artificially before applying it. In the following experiments the temperature changes which occurred in the water used during irrigation were measured by means of insulated copper/constantan calibrated thermocouples connected to an eight-point recording potentiometer, and using a thermostatically controlled hot junction.In the field, a 40-gallon tank was fitted with an immersion-heater and connected through a pump to an oscillating sprayline. One of the thermocouples was enclosed in a polythene tube, fitted over one of the nozzles on the sprayline, and measured the temperature of the water leaving the line. At a distance of about 12 ft from the sprayline a rectangular framework of area 5 sq ft, fitted with a trough of polythene sheet, was arranged at ground level with a slope of about 30 degrees, so that any water falling within the framework would be channelled rapidly into a large polythene funnel. The funnel was supported in a shallow trench, shielded from direct sun, and had another thermocouple fitted into its stem together with a simple constant-level device, so that the water level was always just above the thermocouple. Another exactly similar framework and funnel was placed alongside the first. When the sprayline was working, an almost continuous flow of water was maintained over the thermocouples in the funnels. The air wet-and dry-bulb temperatures were recorded by further thermocouples placed in a nearby Stevenson screen.