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模型模拟土壤性质和植被种类对再生水灌溉水盐运移的影响
引用本文:吕斯丹,陈卫平,王美娥.模型模拟土壤性质和植被种类对再生水灌溉水盐运移的影响[J].环境科学,2012,33(12):4108-4114.
作者姓名:吕斯丹  陈卫平  王美娥
作者单位:中国科学院生态环境研究中心城市与区域生态国家重点实验室,北京,100085
基金项目:国家自然科学基金项目(41173123)
摘    要: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).

关 键 词:再生水  灌溉  土壤盐分  土壤性质  植被  ENVIRO-GRO模型
收稿时间:5/9/2012 12:00:00 AM
修稿时间:2012/7/27 0:00:00

Simulation of Effects of Soil Properties and Plants on Soil Water-salt Movement with Reclaimed Water Irrigation by ENVIRO-GRO Model
L&#; Si-dan,CHEN Wei-ping and WANG Mei-e.Simulation of Effects of Soil Properties and Plants on Soil Water-salt Movement with Reclaimed Water Irrigation by ENVIRO-GRO Model[J].Chinese Journal of Environmental Science,2012,33(12):4108-4114.
Authors:L&#; Si-dan  CHEN Wei-ping and WANG Mei-e
Institution:State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China;State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China;State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
Abstract: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 loam
Keywords:reclaimed water  irrigation  soil salinity  soil properties  plants  ENVIRO-GRO model
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