为推动再生水安全灌溉,本研究运用ENVIRO-GRO模型模拟了不同土壤性质、植被条件下土壤盐分的分布规律及累积趋势,探讨了土壤性质和植被种类对再生水灌溉水盐运移的影响.研究发现,不同土壤初始含盐量下,经多年重复模拟后最终达到统一的平衡状态;而不同土壤质地下,随着灌溉年份的增加,壤土、黏壤土中的土壤ECe年均值逐渐增加直到平衡,砂壤土中的土壤ECe年均值逐渐减少直到平衡,平衡时土层中的ECe值砂壤土〈壤土〈黏壤土.3种植被下,大叶黄杨、油松的土壤ECe值增加量小于早熟禾;土壤盐分在土层中的空间、时间分布也均有所不同.此外,不同模拟情景下,土壤盐分累积都不会影响植被的生长(黏壤土除外),但均出现轻度盐渍化(砂壤土除外).
In order to promote safe irrigation with reclaimed water and prevent soil salinisation,the dynamic transport of salts in urban soils of Beijing under irrigation of reclaimed water was simulated by ENVIRO-GRO model in this study.The accumulation trends and profile distribution of soil salinity were predicted.Simultaneously,the effects of different soil properties and plants on soil water-salt movement and salt accumulation were investigated.Results indicated that soil salinity in the profiles reached uniform equilibrium conditions by repeated simulation,with different initial soil salinity.Under the conditions of loam and clay loam soil,salinity in the profiles increased over time until reaching equilibrium conditions,while under the condition of sandy loam soil,salinity in the profiles decreased over time until reaching equilibrium conditions.The saturated soil salinity(ECe) under equilibrium conditions followed an order of sandy loamloamclay loam.Salt accumulations in Japan euonymus and Chinese pine were less than that in Blue grass.The temporal and spatial distributions of soil salinity were also different in these three types of plants.In addition,the growth of the plants was not influenced by soil salinity(except clay loam),but mild soil salinization occurred under all conditions(except sandy loam).