滤渠-塘组合系统对城市旅游区降雨径流污染的离线截控作用

提出了一种控制城市旅游区降雨径流污染的滤渠-塘离线组合处理系统,并研究了该系统对降雨径流污染的离线截控作用.结果表明:无论从单次降雨事件还是从年度上分析,该系统通过有效地分流初期污染降雨径流,均可降低降雨径流中污染物的浓度和体积平均粒径,并对降雨径流中污染物的负荷具有较高的持留效率,是一种高效的处理系统,比较适用于土地利用相对紧张的城镇区域.2005年该系统对降雨径流中总悬浮物(TSS)、化学需氧量(COD)、总氮(TN)和总磷(TP)负荷的年持留率分别达到86.4%、85.5%、83.9%和82.9%.以2005年6月26日的次降雨事件为例,该系统对降雨径流水量的削减率为67.9%,对污染物中各种形态氮的去除效率高于磷,对TSS、COD、TN和TP负荷的持留率分别为97.0%、89.2%、94.9%和96.2%.该系统还可以有效地拦截降雨径流中的大部分颗粒物.     

城市区域绿色屋顶普及对水量水质的影响

绿色屋顶是城市降雨径流管理的主要措施之一,为了解绿色屋顶普及对城市流域降雨径流量和径流水质的影响,本文以重庆大学虎溪流域为研究载体,评估了绿色屋顶规模化应用与流域降雨产流和径流水质的响应关系.结果表明： 在城市流域进行屋面绿化有助于消减降雨径流以及产污负荷,且屋顶绿化规模和空间分布情景影响降雨径流水质.在屋顶占城市区域总面积的比例为25%、降雨持续时间15 min、降雨强度14.8 mm·h^-1的条件下,当区域内屋顶全部绿化时,峰值降雨径流降低5.3%,降雨径流总量降低31%;总悬浮物（TSS）、总磷（TP）、总氮（TN）的污染负荷分别降低40.0%、31.6%、29.8%,峰值浓度分别降低21.0%、16.0%、-12.2%,平均浓度分别降低13.1%、0.9%、-1.7%;随屋顶绿化率的增加,TSS、TP浓度消减率有所提高,而TN浓度消减率则呈降低趋势,靠近流域总出水口进行屋面绿化,更有利于径流水质的改善.     

污染物在农田溪流生态系统中的动态变化

氮是地表水体发生富营养化的主要因子,河流系统是氮输出的主要运移通道,养分在河流生态系统中的持留和趋向控制着污染物的输出。以巢湖流域一个受人为活动严重影响的农田源头溪流——六岔河为研究对象(包括4个渠道型、1个水塘型和3个河口型断面,对应长度分别为1．3km、0．15km和0．36km),设置9个监测点研究总氮(TN)、硝酸盐(NO3-N)、氨态氮(NH4^ -N)和总悬浮物(TSS)在溪流生态系统中的持留,评价人为严重干扰下的农田溪流生态系统在非点源污染物运移中的生态功能。结果表明：TN、NO3-N、NH4^ -N和TSS在溪流中的持留、释放受溪流的河流形态影响,水塘型和河口型断面是污染物持留的主要区域;TN、NO3-N、NH4^ -N和TSS在水塘型和河口型断面内的持留量分别占溪流持留量(基流、径流持留量的和)的61％、47％、75％和56％。降雨-径流过程中发生的持留是污染物持留的主要部分,TN、NO3-N、NH4^ -N和TSS的持留量分别占溪流持留量的93％、97％、89％和96％;渠道型断面是溪流最主要的内在污染源,污染物释放量占溪流释放量的90％以上;受水塘型断面出口处的水坝影响,位于水塘前的渠道型断面在基流和降雨-径流过程中均有效地持留污染物,而其余渠道型断面在不同水文条件下呈现出不同的持留特性。非点源污染物在溪流中的持留和释放的空间动态变化是溪流生态系统对自然和人为干扰的一种综合响应,有必要恢复溪流生态系统功能,控制农业非点源污染。     

Hydrological and nutrient budgets of freshwater and estuarine wetlands of Taylor Slough in Southern Everglades, Florida (U.S.A.)

Hydrological restoration of the Southern Everglades will result in increased freshwater flow to the freshwater and estuarine wetlands bordering Florida Bay. We evaluated the contribution of surface freshwater runoff versus atmospheric deposition and ground water on the water and nutrient budgets of these wetlands. These estimates were used to assess the importance of hydrologic inputs and losses relative to sediment burial, denitrification, and nitrogen fixation. We calculated seasonal inputs and outputs of water, total phosphorus (TP) and total nitrogen (TN) from surface water, precipitation, and evapotranspiration in the Taylor Slough/C-111 basin wetlands for 1.5 years. Atmospheric deposition was the dominant source of water and TP for these oligotrophic, phosphorus-limited wetlands. Surface water was the major TN source of during the wet season, but on an annual basis was equal to the atmospheric TN deposition. We calculated a net annual import of 31.4 mg m^–2 yr^–1 P and 694 mg m^–2 yr^–1N into the wetland from hydrologic sources. Hydrologic import of P was within range of estimates of sediment P burial (33–70 mg m^–2 yr^–1 P), while sediment burial of N (1890–4027 mg m^–2 yr^–1 N) greatly exceeded estimated hydrologic N import. High nitrogen fixation rates or an underestimation of groundwater N flux may explain the discrepancy between estimates of hydrologic N import and sediment N burial rates.     

Phosphorus and nitrogen retention in five Precambrian shield wetlands

Phosphorus and nitrogen mass balances of five wetlands (two beaver ponds, two conifer-Sphagnum swamps and one sedge fen) situated in three catchments in central Ontario, Canada, were measured. Monthly and annual input-output budgets of total phosphorus (TP), total nitrogen (TN), total organic nitrogen (TON), total inorganic nitrogen (TIN), ammonium ion (NH₄ ⁺ -N), nitrate (NO ₃ ^– -N) and dissolved organic carbon (DOC) were estimated for the five wetlands during the 1982–83 and 1983–84 water years. Except for the deepest beaver pond (3.2 m) which had annual TP retention of –44% (–0.030 ± 0.015 g m^–2 yr^–1), the wetlands retained < 0.001 to 0.015 g M^–2 yr^–1 ; however, this wasless than 20% of the inputs and the estimated budget uncertainties were equal to or greater than the retention rates. Annual TN retentions ranged from –0.44 to 0.56 g m^–2 yr^–1 (–12 to 4%) but were not significantly different from zero. The wetlands transformed nitrogen by retaining TIN (16 to 80% RT) and exporting an equivalent amount as TON (–7 to 102% RT). The beaver ponds, however, retained NO ₃ ^– while NH ₄ ⁺ was passed through or the outputs exceeded the inputs. In contrast, the conifer swamps retained both NH ₄ ⁺ and NO ₃ ^– . DOC fluxes into and out of the beaver ponds were equal (–18 and 4% RT) but output from the conifer swamps exceeded input by > 90%. Marked seasonal trends in nutrient retention were observed. Nutrient retention coincided with low stream flow, increased evapotranspiration and biotic uptake during the summer. Net nutrient export occurred during the winter and spring when stream flows were highest and biotic uptake was low.     

绿色屋面降雨径流水质及消减污染负荷研究

2011年5月至11月对12场降雨时段的屋面径流和干湿沉降进行采样监测,比较了屋面径流(绿色屋面和沥青屋面)、干湿总沉降和降雨中污染物的浓度和污染负荷,并运用多元统计方法分析了降雨特征对绿色屋面径流水质的影响。结果表明,从径流水质层面上分析,绿色屋面是总悬浮物(TSS)的汇,对p H值有较好的中和作用,对于总磷(TP)、溶解态铜(DCu)和溶解态锌(DZn)是非源非汇,是电导率(EC)、总氮(TN)、氨态氮(NH+4-N)、硝态氮(NO-3-N)、化学需氧量(COD)、5日生化需氧量(BOD5)和溶解态铅(DPb)的源;从污染负荷的角度分析,绿色屋面是NH+4-N、TSS和BOD5的汇,对于TN、DPb、DCu、DZn、TP和COD是非源非汇,是NO-3-N的源;与控制屋面相比,绿色屋面可以消减TSS、TP、BOD5、COD、NH+4-N、DZn和DPb的污染负荷,分别消减了90.53%、49.38%、41.31%、36.48%、35.45%、28.27%和14.20%;但是增加了NO-3-N和TN的污染负荷,分别增加了821.02%和275.48%;绿色屋面径流污染物的浓度与降雨量、降雨历时和降雨强度呈负相关关系,而与降雨间隔呈正相关关系。研究结果为绿色屋面的科学设计及正确评价绿色屋面对径流水质的影响提供依据。     

Nutrient uptake and release in ponds under long-term and short-term lotus (Nelumbo nucifera) cultivation: Influence of compost application

Uptake and release of nutrients from ponds used for lotus cultivation were measured in ponds under short-term (1 yr) cultivation with compost application (pond I) and under long-term (20 yr) cultivation without compost application (pond II). Total inflow loads of TN (irrigation water, rainfall and compost) during lotus cultivation period in ponds I and II were 72.3 and 34.3 kg ha^?1 182 day^?1, respectively. TN removal rates in ponds I and II were 77.3 and 49.8% of total inflow load, respectively. Major removal mechanisms of TN were attributed to microbial processes and uptake by lotus. The total outflow loads (infiltration and runoff) of TN during the lotus cultivation period were 13.9 kg ha^?1 182 day^?1 (19.2% of total inflow TN load) for pond I, and 11.3 kg ha^?1 182 day^?1 (32.9% of total inflow TN load) for pond II. For TP the total inflow loads (irrigation water, rainfall and compost) during lotus cultivation in ponds I and II were 80.8 and 1.9 kg ha^?1 182 day^?1, respectively. TP removal rates in ponds I and II were 84.9 and ?274.1% of total input, respectively. Phosphorus removal was attributed to lotus uptake and soil adsorption. The total outflow loads (infiltration and runoff) of TP during lotus cultivation period were 10.1 kg ha^?1 182 day^?1 (12.5% of total inflow TP load) for pond I, and 6.6 kg ha^?1 182 day^?1 (355.6% of total inflow TP load) for pond II. TN and TP in runoff from pond I (with compost) was higher than that in pond II (without compost), showing that TN and TP in runoff were strongly influenced by compost addition. Therefore, in order to satisfy established water-quality standards, the amount of compost used in lotus cultivation should be evaluated.     

Retention of nitrogen, phosphorus and silicon in a large semi-arid riverine lake system

Lakes and reservoirs (impoundments) are often viewed as a sink for nutrients within the river continuum. To date, most studies on nutrient retention within impoundments are derived from the temperate climate zones of Europe and North America, only consider one nutrient, and are often short-term (1–2 years). Here, we present a long-term (17 year) data set and nutrient (nitrogen, phosphorus and silica) budget for two connected semi-arid lakes (the Lower Lakes) at the terminus of the River Murray, Australia. Most of the filterable reactive phosphorus and nitrate entering the lakes were retained (77 and 92%, respectively). Total phosphorus (TP) was also strongly retained (55% of the annual TP load on average) and the annual TP retention rates could be predicted as a function of the areal hydraulic loading rate (annual lake outflow/lake surface area). On average, there was a slight net retention (7%) of the annual total nitrogen (TN) load but a slight net export (6% of the load) of organic N. TN retention as function of the areal hydraulic loading rate was lower than expected from existing models, possibly because of high nitrogen fixation rates in the Lower Lakes. Silica was retained (39%) at similar rates to those observed in previous studies. There was also a marked increase in the TN:TP and TN:Si ratios within the lake (TN:TP~30 and TN:Si~0.67) compared to those entering (TN:TP~15, TN:Si~0.45), as a consequence of the relatively low net retention of nitrogen.     

Physicochemical limnology of the Tongue River Reservoir,Montana

A one year physicochemical survey was conducted on the Tongue River Reservoir, a run of the river impoundment in southeastern Montana. The Tongue River was the only significant inflow and supplied 93, 96 and 97% of the nutrient, major ion and water inputs to the impoundment. Heat advected from inflowing water accounted for 17% of the energy gained during the summer heating cycle. The annual nutrient load to the reservoir from the river was 20.2 g m^–2 total nitrogen (TN) and 3.8 g m^–2 total phosphorus (TP). Due to the absence of reducing conditions at depth and the complex seasonal pattern of water movement through the reservoir, 99% of the TN load was discharged but 49% of the TP load was retained in the reservoir.     

基于暴雨径流管理模型(SWMM)的海绵城市低影响开发措施控制效果模拟

为解决城市化过程中遇到的水生态、水安全和水环境问题,以低影响开发(LID)为核心理念,我国提出了海绵城市这一新型城市雨洪管理概念.本研究利用芝加哥雨型和沈阳暴雨强度公式构建了不同重现期的降雨过程线,然后利用暴雨径流管理模型(SWMM)模拟分析了城市化前、城市化后和LID措施后3种情景方案的水文水质过程.结果表明: 随着降雨重现期的增大,LID措施减少的径流量逐渐增大,研究区径流量基本达到城市化前的水平.LID措施对总悬浮颗粒物(TSS)、化学需氧量(COD)的去除量较大,但TSS和COD排放量仍然远远高于城市化前,总氮(TN)和总磷(TP)的污染物排放量接近于城市化前的自然状态.随着雨强的增大,径流流速增大,LID措施消减的TSS、TP和COD量逐渐减小.     

Limnological characteristics of a subtropical constructed wetland in south Florida (USA)

The Everglades Nutrient Removal Project (ENRP) was a 1544 ha constructed wetland built by the South Florida Water Management District as part of Everglades restoration efforts. The limnology of this wetland is characterized over its 60-month operational history. The ENRP received agricultural runoff containing high levels of C, N, P and other dissolved constituents; had moderately high alkalinity with a circumneutral pH; and had low to moderate DO. The ENRP provided substantial treatment (concentration reduction from inflow to outflow) for Al, Fe, NH₄, NO_x, SRP, TP, TSS and turbidity (high-treatment variables), while Secchi depth increased markedly. These changes were judged biologically significant. Dissolved oxygen, and water temperature had well defined annual cycles, while some level of seasonality was noted for Al, alkalinity, Ca, conductivity, DOC, Fe, hardness, K, Mg, Mn, Na, NH₄, pH, Secchi depth, SiO₂, TOC, TN, turbidity, and TSS. The ENRP was P limited based on TN:TP molar ratios. Dissolved ions were dominated by Ca, Cl, Na, and HCO₃; the stoichiometric balance of both major and minor ions was similar throughout the wetland. The downstream settling of TSS was associated with increased light penetration, but did not appear important in sediment accretion. The adsorption of P to Ca, and perhaps Al and Fe, precipitates is thought to have been an important nutrient removal mechanism. Although there was little net reduction in DOC, we speculate that some incoming material was degraded and replaced by new DOC produced within the wetland.     

模拟降雨下喀斯特坡耕地土壤养分输出机制

喀斯特区坡耕地水土及养分流失不仅是该区土地质量退化、土地生产力衰退主要原因,同时也是该区地下水质污染的重要因素。为揭示喀斯特坡耕地地表和地下二元空间结构下的土壤养分流失机制,以喀斯特坡耕地为研究对象,通过模拟其地表微地貌及地下孔(裂)隙构造特征,采用人工模拟降雨试验研究不同雨强下喀斯特坡耕地地表及地下水土及其氮、磷、钾流失特征。结果表明:(1)小雨强(50mm/h)和中雨强下(70mm/h),喀斯特坡耕地坡面产流主要以地下产流为主;大雨强下(90mm/h),地表径流高于地下径流;产沙方式则表现为由小雨的地表和地下产沙并重到中大雨强的地表产沙为主的一个转变过程。(2)在降雨侵蚀过程中,径流各养分输出浓度均表现出一定的初期冲刷效应,受土壤吸附作用影响,雨强对全钾(TK)和全氮(TN)的影响较全磷(TP)明显。(3)地表径流、地表泥沙和总泥沙各养分输出负荷均随雨强增大而增加,坡面径流泥沙总的TK输出负荷以泥沙为主,而TN和TP输出负荷则以径流为主;TP和TN在径流的输出负荷上以地下径流输出为主(其中TP地表负荷比在11.6%—46.2%,TN在7.0%—48.5%之间),而TK则以二者并重(地表负荷比在43.5%—57.0%之间);各养分在泥沙的输出负荷上则均以地表泥沙流失为主,其负荷比均在54.5%以上。研究结果可为喀斯特区坡耕地水土流失及养分流失的源头控制提供基本参数和科学依据。     

Biogeochemical storm response in agricultural watersheds of the Choptank River Basin,Delmarva Peninsula,USA

Stream discharge and chemistry (total suspended solids TSS, nitrogen N, and phosphorus P) were monitored for 15 months in six agricultural watersheds on the U.S. Mid-Atlantic coastal plain. Watersheds with similar land uses and a range of hydric soils were used to test the hypothesis that hydric soils generate large storm discharges due to low permeability, resulting in watershed areas with high loss rates of N, P, and TSS. To test the hypothesis, discharge was monitored continuously, and a flow separation method quantified the base and stormflow contributions. Another primary goal was to measure base and stormflow chemistry to quantify N, P, and TSS export. Baseflow chemistry was monitored monthly, and 31 storm events were sampled. Baseflow chemistry varied little over the 15 months, but stormflow chemistry was dynamic, with three major patterns: (1) TSS and particulate N and P had large, brief peaks during the rising limb of storm hydrographs; (2) phosphate and ammonium had broader peaks close to maximum discharges; and (3) nitrate concentrations decreased during the rising limb, slowly returning to pre-storm levels. Event water yields were correlated with volume-weighted mean concentrations (VWMs) of N, P, and TSS, providing a basis for estimating VWMs of unsampled events. Export coefficients (kg ha^?1 year^?1) ranged over 22–33 for TN, 0.9–1.4 for TP, and 240–1140 for TSS. Most P and TSS export occurred during storms (71–99%), while most N export occurred during baseflow (52–84%). The discharge data did not support the hypothesis, and watershed slope, not hydric soils, was the major control on storm discharge. Surface ponding of water on hydric soils intercepted runoff, reducing the impacts of the low infiltration rates.     

生物浮岛与漂浮植物对开放池塘水质净化效果

采用自主研发流量可控的密闭漂浮性水槽开展河道原位模拟实验, 研究了挺水植物菖蒲(种植于浮岛上)与漂浮植物凤眼莲对受到城市污水污染的开放池塘水质净化效果以及系统中氮磷等污染物的归趋。结果表明, 菖蒲和凤眼莲对水体藻类密度和叶绿素a削减率达到90%以上, 对COD_Mn浓度削减率达到45%以上。经过10 m长水槽后, 种植了凤眼莲的水槽水体其TN和TP浓度分别由3.71和0.24 mg/L降低至1.71和0.09 mg/L, 而设置有菖蒲浮岛的水槽其水体TN和TP浓度则分别降低至2.69和0.16 mg/L。在水体N、P的总削减量中, 凤眼莲吸收作用分别占84.31%和77.52%, 而在菖蒲浮岛系统中, 菖蒲的吸收作用仅分别占7.72%和8.55%, 菖蒲净化系统中氮、磷的物理沉淀量显著高于凤眼莲组, 分别达到35.26%和51.58%, 但仍有57%和39%以上的氮和磷去向未知, 推测可能与浮岛上生长的生物膜有关。研究结果可为选用凤眼莲和浮岛植物修复技术进行污染水体生态修复理论研究与实践运用提供借签和参考。     

Performance of an ecological treatment system at three strengths of dairy wastewater loading

Ecological treatment systems, which rely on renewable resources, have successfully treated municipal and industrial effluents with reduced costs compared to conventional methods, but their capacity to treat dairy wastewater is unknown. In order for ecological treatment systems to be practical for agriculture they must be able to treat a significant portion of a dairy's daily wastewater production. In this study, the impact of three strengths of dairy wastewater on effluent water quality was assessed. Three ratios of wastewater and city water—(1) one part wastewater:three parts city water, (2) one part wastewater:one part city water, and (3) two parts wastewater:one part city water—were each pumped into an ecological treatment system. Influent and effluent water samples were analyzed for PO₄-P, TP, TN, NH₄-N, NO₃-N, total suspended solids (TSS), and carbonaceous biochemical oxygen demand (CBOD₅). Influent dairy wastewater volumetric loading rates were much greater than those of municipal wastewater. Regardless of influent wastewater strength, concentrations of all measured variables were significantly reduced between the influent and effluent of the ecological treatment system. At the lowest wastewater strength, PO₄-P was reduced 39%, TN 83%, and NH₄-N 89%, while at the highest wastewater strength, PO₄-P was reduced 41%, TN 79%, and NH₄-N 70%. Increased wastewater strength required greater aerobic treatment volume to reduce concentrations of NH₄-N and CBOD₅.     

非点源污染输出对土地利用和社会经济变化响应的案例研究

为研究三峡库区(重庆段)自2006年10月蓄水(156m)以来,非点源污染输出对土地利用及社会经济背景变化响应的时空分异特征,综合考虑库区典型土地利用变化模式及社会经济背景,选取三峡库区腹地奉节县、忠县、库尾江津区及主城沙坪坝区为研究对象,使用动态输出系数模型法,以2007年、2010年和2013年3期遥感影像为数据源,分析了研究区2007年到2013年非点源污染TN、TP负荷量随土地利用类型改变及社会经济的发展而产生的时空变化特征。研究表明,6年间,研究区污染物TN从2007年的12126.9t上升到2013年的12692.3t,TP从2007年的394.6t上升到2013年的407.2t。就各典型区县而言,城市发展新区江津区非点源污染负荷呈上升趋势,TN、TP负荷量涨幅分别达到了28.6%和24.1%;而库尾城市快速扩展的沙坪坝区则呈现下降趋势,非点源污染TN、TP负荷量分别下降了48.8%和68.9%;仍保持传统农业的奉节县和忠县变化不大。     

滇池流域退耕区植物群落构建对地表径流污染物的削减效应

为探索不同群落的构建在滇池流域的实际应用,以确定削减污染物最优植物群落的配置方式,该研究选取地表径流悬浮物(SS)、COD含量、总氮(TN)、总磷(TP)、氨氮(NH_4~+-N)、硝氮(NO_3~--N)六个指标作为主要的分析对象,在滇池流域退耕区开展了不同植物群落配置对地表径流污染物削减效应的试验研究。结果表明:三个植物群落对SS、COD、TN、TP、NO_3~--N在2014年和2015年间均表现出显著性的削减趋势,且三个植物群落对SS、TP和NO_3~--N的削减率均在45%以上,但并未对NH_4~+-N表现出削减效果。不同植物群落对污染物的削减效应存在一定的差异性,但是三个不同群落与年度的交互作用对SS、COD、TN、TP、NO_3~--N五个养分指标的削减并没有表现出显著的差异性。从整体上来看,三种植物群落类型中,以乔-灌-草构建的立体式植物群落对地表径流污染物的削减效果最佳。     

Modeling the hydrochemistry of the Choptank River Basin using GWLF and Arc/Info: 1. Model calibration and validation

We modeled nutrient export in the ChoptankRiver Basin on the coastal plain of the Chesapeakedrainage, using a modified version of alumped-parameter, hydrochemical model (GWLF).Calibration was performed using long-term (WY1980–WY1990)hydrochemistry data from a gauged site. Thecalibrated model reproduced water yields, TN, and TPexport with cumulative errors of <1% over the11-year calibration period and with annual RMS errorsof 10–50%. Model validation was done withindependent measurements at the same gauged site(WY1991 to WY1996) and at another nearby independentlygauged site (WY1991 to WY1995). Local adjustment ofthe groundwater recession coefficient and thedissolved N concentration in agricultural stormflowwas essential for successful application at the secondsite. GWLF appears to be a useful model for estimationof fluxes of water, N and P from ungauged areas withaccuracies of 10–50% at annual time scales.     

硝化细菌对加州鲈池塘水质影响及底质净化作用

为研究有益菌硝化细菌(Nitrifying bacteria)对加州鲈(Micropterus salmoides)高密度养殖池塘水质及底质的影响,在模拟加州鲈高密度养殖池塘单独施用硝化细菌,通过检测养殖水体pH、氨氮(NH4+-N)、亚硝酸盐氮、总氮(TN)及总磷(TP)等水质指标,底质沉积物中有机物、全氮及全磷等指标以及池塘浮游动植物量,以评价硝化细菌处理对加州鲈高密度养殖水体水质影响及底质净化作用。结果表明,硝化细菌能够稳定养殖水体pH,降低水体亚硝酸盐氮浓度,减缓养殖水体TN浓度上升,去除底质沉积物中有机物及全磷含量,有机物去除率达54.17%,全磷去除率达43.34%。硝化细菌处理前期浮游动植物总量高于对照池塘,后期逐渐减少并趋于稳定。     

辽宁中部城市群城市非点源污染负荷评估

过去几十年我国经历了快速城市化过程,这使得不透水面大幅度增加,导致地表径流和洪峰流量增加,进入水体的污染物增多。城市非点源污染已成为河流水体恶化、生态系统退化的重要原因。在快速城市化过程中,城市群已成为城市化发展的新阶段。位于同一流域的各城市所产生的城市非点源污染导致城市群流域水环境问题越来越突出,成为制约城市群流域可持续发展的关键因素之一。现有的关于城市非点源的研究多集中于城市内部小尺度,对城市群大尺度的研究亟需发展。以位于浑河太子河流域的辽宁中部城市群为例,在沈阳市不同功能区和不同下垫面进行降雨径流采样,基于事件平均浓度（Event Mean Concentration, EMC）法和SWMM（Storm Water Management Model）模型相结合的方式,定量评估城市群流域城市非点源污染负荷。研究结果表明：路面径流中城市非点源污染物浓度、负荷量及其单位面积负荷要高于屋面径流和透水面径流。辽宁中部城市群TP、TN、COD、TSS的年均城市非点源污染负荷分别为265.52、852.89、2249.71、192496.74 t/a,重金属Cd、Ni、Pb、Cr、Cu、Zn的年均城市非点源污染负荷分别为347.99、9932.62、25861.29、28360.41、36068.30、138840.42 kg/a。沈阳市城市非点源污染负荷最高,但其单位面积负荷最低。本研究基于更为精细的城市下垫面划分,综合考虑城市功能区划、下垫面类型和降雨强度,更为准确的评估了辽宁中部城市群流域的城市非点源污染负荷。该研究能够为高度城市化流域城市非点源污染防控和水环境综合治理提供科学依据。