【摘要】 在上海市城市河岸带人工绿地建设了微区径流场,进行了5次模拟降雨径流实验,研究了人工绿地岸带下渗流中氮浓度和去除率的时空变化。结果表明:人工绿地岸带对垂直下渗流中氮有显著的净化作用,且主要集中于土壤的0～30cm以内,TN和NH4+去除率在39.9%和39.8%以上,NO3-+NO2-去除率除11月为负值外,其余月份均在10.0%以上;在30～60cm深度,由于土壤氮的析出导致径流中氮浓度增加,去除率降低;而60～90cm深度的去除率增加。径流场内下渗流中氮浓度具有明显的水平空间变化,随距入水端距离的增加,30cm深度下渗流中氮浓度先上升后下降;人工绿地岸带对下渗流中氮的净化作用均随淹水时间的延长呈降低趋势,且季节变化明显,在10月和4月具有较高的去除率,0～30cm内TN、NH4+和NO3-+NO2-的去除率可分别达63.5%、89.1%和41.6%以上。更多还原

【Abstract】 In order to study nitrogen removal in vertical infiltration of runoff by artificial green belt near urban riparian,a micro catchment area was constructed at Changfeng green belt of Suzhou River riparian.Meanwhile permeability of Changfeng green belt was measured by double ring method and soil samples were collected for analysis of physicochemical properties.In situ pore water samplers were used to collect samples of vertical infiltration at different depth in the micro catchment area,which were distributed from surface runoff flowing 1 m,11 m,18 m,21 m at depth of 30 cm,60 cm and 90 cm.3 pore water samplers were buried at each depth.The water in Suzhou River containing higher nitrogen concentrations than the corresponding type Ⅴ standard values of the GB 3838-2002 National Environmental Quality Standards for Surface Water was fit to simulate runoff.Therefore,5 rainfall runoff stimulation experiments were carried out at Changfeng artificial green belt using water of Suzhou River at October,November of 2010 and April,June,August of 2011.Spatial variation of nitrogen in vertical infiltration and removal rate by artificial green belt were analyzed and compared.The results showed that the permeability of Changfeng green belt was 0.9 mm/min,which was medium in urban green belt of Shanghai.The physicochemical properties of the soil samples showed a distinct spatial difference.So Changfeng green belt was a typical municipal green belt.There was significant removal for nitrogen in vertical infiltration of runoff by artificial green belt of riparian,particularly in the layer at 0-30 cm in each experiment.Removal rates of TN and NH4+ by soil in layer at 0-30 cm were above 39.9% and 39.8% respectively.But the accumulative removal rates at 0-60 cm decreased due to the increase of nitrogen concentrations in vertical infiltration at the depth of 30-60 cm.The nitrogen concentrations in layer of 60-90 cm descended which caused the accumulative removal rates at 0-90 cm higher than those at 0-60 cm.Compared with the stimulated rainfall runoff,i.e.,the water of Suzhou Creek,the infiltrated water samples collected at different depth had a different nitrogen composition.The percentage composition of NO3-+NO2-in TN increased in the vertical infiltration,but the NH4+ was quite the contrary.There was conspicuous spatial variation of nitrogen in vertical infiltration at different sites in catchment area.With the increase of flow distance of surface runoff,concentration of nitrogen in vertical infiltration in layer at 0-30 cm would firstly increase and then decrease.Nitrogen removal rate of green belt would decrease with the waterlogging time increasing.The nitrogen removal rates varied with month.There were higher removal rates in April and October because there were suitable climate and edaphic condition.Removal rates of TN,NH4+ and NO3-+NO2-by soil in layer at 0-30 cm exceeded 63.5%,89.1% and 41.6% respectively in April and October.In general,urban riparian zone,which was made up of artificial green belt,could remove much nitrogen and be an important parclose for nitrogen discharged into groundwater and urban rivers by vertical infiltration of runoff.更多还原