摘要
Sod moisture maintenanre is very important for the plant growth in arid regions. For the hottest 10 days(July 21~31, 2002), soil volumetric water content, sensitive and latent heat flux over oasis situated in the middlereaches of the Heihe River basin, were simulated for a range of drip irrigation schemes using the nos-hydrostaticmesoscale atmospheric model MM5 with 1 km horizontal resolution. From the 10-day simulation, the following re-sults were obtained that 500 m3 · hm-2 would be appropriate to maintain stable and sufficient soil moisture for oasis.A greater volume of irrigation water would not only waste water resources but also increase soil moisture to satura-tion levels, lower soil oxygenation and harm crops. While with lesser volume, evapotranspiration would exceed thewater input, leading to drought conditions. Additionally, the 500 m3 hm -2 weter for July 21~31 is only half of theminimal quota and one-third of maiunial quota for traditional irrigation over the same period. So drip irrigation isclearly a water-saving irrigation method, which could allow significant savings of the limited water resources in thearid region of Northwest China.