三峡库区大宁河流域非点源污染研究

以大宁河流域巫溪水文站控制流域为研究对象,应用分布式非点源污染模型SWAT,利用实测流量、泥沙负荷及氮、磷负荷数据对模型进行了率定和验证,并模拟了大宁河流域的径流量和营养物质氮、磷的排放.结果表明,月平均流量在率定期和验证期的效率系数分别达到了0.93和0.62;泥沙负荷的效率系数分别为0.70和0.34;氨氮和总磷的效率系数分别达到了0.31和0.37.大宁河流域污染物质的排放存在着较大的空间差异,有机氮和有机磷的5年平均排放量区间分别为2.01～38.15和0.35～5.89 ks/(hm2·a),其中,流域西南部子流域的有机氮和有机磷平均排放量最大,分别为38.15和5.89 ks/(hm2·a),是大宁河流域污染物排放的最敏感区域.     

流域水环境污染模拟及关键源区鉴别——以义乌江流域为例

以义乌江流域为研究区,应用SWAT模型模拟流域的径流、泥沙与水质过程,在分析流域内水文过程与污染负荷(总氮、总磷)时空分布特征的基础上,采用单位面积负荷指数法确定各子流域的氮磷流失强度,并划分5个等级,进而识别水环境污染的关键源区.结果表明:1)生活污染源是义乌江流域水环境污染的主要来源,氮磷的输入占比分别为52.7％...     

钱塘江流域污染负荷及水环境容量研究

采用排污系数法计算了钱塘江流域不同污染源COD和氨氮的污染负荷,研究了整个流域90%、75%和so%水文保证率下的水环境容量.以流域水质目标为出发点,考虑污染负荷和流域社会经济发展需求相协调的原则,确定了钱塘江流域水污染总量控制阶段性目标.     

基于SWAT模型的滹沱河流域氨氮污染负荷结构

基于SWAT模型研究了滹沱河流域内氨氮污染负荷结构,为区域水污染控制和水质改善提供依据。分析表明,不同水期各子流域氨氮污染负荷结构具有一定的差异性。从全年整体来看,生活氨氮污染负荷最大,农业次之,工业最小,与平、枯水期一致;丰水期农业氨氮污染负荷最大,生活次之,工业最小。     

吉林省招苏台河流域农业非点源污染特征研究

招苏台河吉林段为辽河重污染支流,以发展农业为主的产业结构使流域内非点源污染十分严重。采用输出系数法与地理信息系统(GIS)技术相结合,对2003—2012年流域农业非点源污染的组成结构、年际变化和空间分布特征进行研究。研究结果表明:(1)2003—2012年研究区农业非点源TN、TP负荷均呈先增后减趋势,TN负荷平均贡献率由高至低依次为种植业(52.62%)、畜禽养殖业(37.66%)、农村生活(9.72%);TP负荷平均贡献率依次为畜禽养殖业(51.58%)、种植业(30.36%)、农村生活(18.06%);(2)河流两岸1 000m缓冲区内农业非点源污染负荷相对集中,2012年缓冲区内TN、TP负荷分别为流域总负荷的50.30%、54.68%;(3)种植业和农村生活所产生的污染相对稳定,缓冲区内的畜禽养殖业是该流域农业非点源污染防治的重点和突破口。     

基于InfoWorks ICM模型的白龙江流域甘肃段水质模拟及分析

针对白龙江沿岸农业种植、畜禽养殖等产业发展影响河流水质的问题,以甘肃省南部白龙江流域为研究对象,采用改进输出系数模型计算丰、平、枯水年等典型水文情景下流域内工业、农村生活垃圾、农村生活污水、畜禽养殖、城镇生活污水、城镇径流和农田径流等污染源污染负荷,基于InfoWorks ICM构建了白龙江水动力水质模型,模拟分析COD、TN、NH₄⁺-N和TP等污染负荷分布特征,评估了最不利水文条件下白龙江水质污染风险,验证了该模型在流域水质污染模拟评估的适用性。研究结果表明,不同水文情景下污染物入河负荷主要来源存在显著差异,如丰水年和平水年农田径流是COD污染的主要来源,污染负荷分别达到1 382.56、1 058.98 t,而枯水年污染源主要是城镇径流。污染物负荷存在明显空间差异,研究区内子流域污染负荷空间分布不均匀,高污染负荷主要出现在中下游子流域。白龙江水质在汛期和非汛期差异较大,非汛期水质更差。通过模拟最不利水文情景(枯水年非汛期)发现,研究区内白龙江NH₄⁺-N浓度最大位置出现在中下游,最高可达1.4...     

施肥方式对东北玉米种植区氮磷流失的影响

研究不同施肥方式下东北玉米单作种植体系氮磷流失规律,可为该地区农田面源污染防控及生态保护提供技术参考。试验设置农民习惯处理、优化施肥处理、秸秆还田处理和有机肥化肥混施处理,采用自然降雨条件室外模拟方法,分析不同施肥处理对东北玉米种植区径流淋溶氮磷流失的影响。结果表明,在东北地区玉米单作模式下,多雨年份优化施肥处理与农民习惯处理相比可降低15.8%的总氮流失负荷,降低7.3%的总磷流失负荷;秸秆还田处理可明显降低22.9%的总氮流失负荷及15.1%的总磷流失负荷;有机肥化肥混施处理降低总氮流失负荷13.6%,但增加总磷流失负荷13.9%;氮磷流失负荷以泥沙流失为主,淋溶流失其次。结合作物产量,在多雨年份,优化施肥处理和秸秆还田施肥处理是防控东北玉米区农田面源污染和保证作物产量的理想施肥方式。     

于桥水库流域污染负荷估算和管理效果评估

于桥水库流域非点源污染已成为政府高度关注的热点问题之一。使用非点源污染负荷模型PLOAD,以流域数字高程模型(DEM)、2010年土地利用现状图和不同土地利用的污染物输出系数等作为模型主要输入数据,结合流域现场调查监测等方式,对于桥水库流域的TN和TP污染负荷进行估算,分析污染物的空间分布特征,模拟实施不同管理实践下的流域TN和TP削减率。结果表明,于桥水库流域内TN和TP污染负荷分别约为223.4、19.5t/a,分布特点为"南部高于北部,河流和水库沿岸污染较重"。综合管理实践对TN和TP的削减率分别为24.49%、27.23%,其中农村人畜粪便管理、生态移民等的去除效果较显著。     

基于AnnAGNPS模型的灞河流域非点源污染模拟研究

以灞河流域下属子流域为研究对象,运用AnnAGNPS模型对流域内非点源污染特征进行了定量分析,并以非点源污染严重的灞河中游子流域为例,提出不同的非点源污染控制方案。结果表明:AnnAGNPS模型对径流模拟效果总体良好,率定期模拟相对误差(Re)基本在-10%～0,模拟效率系数(Ens)为0.65,相关系数(R~2)为0.81,验证期模拟Re基本在-50%～0,Ens为0.68,R~2为0.71。利用5次降雨事件数据考察AnnAGNPS模型对TN、TP污染负荷的拟合精度,AnnAGNPS模型对4次降雨的TN污染负荷模拟Re控制在-13%～5%,3次TP污染负荷模拟Re维持在-12%～40%;在非点源污染控制方案中,耕地变换成林地对TN、TP污染负荷的削减效果非常显著,假设灞河中游小流域耕地变为林地的转变率分别为30%、50%、100%时,TN污染负荷削减28.20%、43.01%、78.23%,TP污染负荷分别削减33.55%、53.94%、66.81%。     

永定河上游张家口地区水污染物排放负荷与贡献

运用源强系数法,估算永定河上游张家口地区不同来源水污染物的排放负荷,并评估不同污染源的贡献。结果表明:(1)永定河上游张家口地区COD排放负荷为97 533.43t/a;氨氮排放负荷为10 596.73t/a;总磷排放负荷为1 389.11t/a。(2)COD主要来自畜禽养殖业和城镇生活污水,分别占总排放负荷的53.66%和31.41%;氨氮主要来自城镇和农村生活污水,分别占总排放负荷的40.15%和27.04%;总磷主要来自畜禽养殖业和城镇生活污水,分别占总排放负荷的28.99%和26.54%。(3)从空间上看,宣化区COD、氨氮、总磷排放负荷均为最大,宣化区是永定河上游张家口地区水污染的主要贡献区。     

Distribution of nutrients,heavy metals,and PAHs affected by sediment dredging in the Wujin'gang River basin flowing into Meiliang Bay of Lake Taihu

This paper's survey of the pollution of the Wujin'gang River is important because it is one of the main rivers flowing into Meiliang Bay of Lake Taihu in eastern China. Trace metals (TMs) in this paper are described according to their pollution index (P _i). Cluster analysis and correlation analysis are utilized for group sites and to assess co-contamination. Toxicity effect analysis was conducted using individual sediment quality guideline quotients (SQGQs) and mean SQGQs. The results showed that sediment from the Wujin'gang River basin was affected by nutrients, heavy metals, and polycyclic aromatic hydrocarbons (PAHs), which are an essential contamination source for both Meiliang Bay and Zhushan Bay of Lake Taihu. The discharge of TMs has significant correlations to total nitrogen (TN) and total phosphorus (TP); however, no significant correlations were observed between the content of PAHs and TMs. Toxicity effect results show that sediment in the Wujin'gang River basin threatens sediment-dwelling organisms. The harmful effect was mainly caused by heavy metals especially Cd, Cr, Ni, and Cu. Sediment dredging is an effective way to control pollution from internal rivers especially for the pollution of TN and heavy metals in the Wujin'gang River basin.     

Variations in source apportionments of nutrient load among seasons and hydrological years in a semi-arid watershed: GWLF model results

Quantifying source apportionments of nutrient load and their variations among seasons and hydrological years can provide useful information for watershed nutrient load reduction programs. There are large seasonal and inter-annual variations in nutrient loads and their sources in semi-arid watersheds that have a monsoon climate. The Generalized Watershed Loading Function model was used to simulate monthly nutrient loads from 2004 to 2011 in the Liu River watershed, Northern China. Model results were used to investigate nutrient load contributions from different sources, temporal variations of source apportionments and the differences in the behavior of total nitrogen (TN) and total phosphorus (TP). Examination of source apportionments for different seasons showed that point sources were the main source of TN and TP in the non-flood season, whereas contributions from diffuse sources, such as rural runoff, soil erosion, and urban areas, were much higher in the flood season. Furthermore, results for three typical hydrological years showed that the contribution ratios of nutrient loads from point sources increased as streamflow decreased, while contribution ratios from rural runoff and urban area increased as streamflow increased. Further, there were significant differences between TN and TP sources on different time scales. Our findings suggest that priority actions and management measures should be changed for different time periods and hydrological conditions, and that different strategies should be used to reduce loads of nitrogen and phosphorus effectively.     

合肥市南淝河不同排口表层沉积物磷形态分布特征

对合肥市南淝河不同排口处表层沉积物进行了采样,并采用修正后的标准测试程序SMT和钼锑抗紫外分光光度法测定了其中的总磷(TP)、无机磷(IP)、有机磷(OP)、铁/铝磷(Fe/Al-P)和钙磷(Ca-P),同时分析了各形态磷之间以及与沉积物有机质之间的相关性。结果表明,由于各排口附近不同的水动力条件,污染状况以及沉积环境,各排口表层沉积物总磷(TP)的质量分数存在显著差异,其值在771.23~3 065.36 mg/kg之间,除二里河排口(S15)沉积物磷以钙磷(CaP)为主外,其他采样点表层沉积物磷均以铁/铝磷(Fe/Al-P)为主,各形态P的最低值均在位于南淝河上游的S4点,TP、IP、Fe/Al-P的最大值均出现在位于望塘污水厂排口下游60 m处的S6点,潜在释放磷比例最大值在南淝河上游受农业面源污染影响较大的S3点。沉积物各形态磷之间存在着不同程度的相关性,各形态磷与有机质存在着显著的正相关。以上结果表明,南淝河沉积物磷形态分布特征受排口类型影响显著,其中城市污水处理厂尾水可能是受纳水体沉积物重要的磷源。     

Historical trend of nitrogen and phosphorus loads from the upper Yangtze River basin and their responses to the Three Gorges Dam

Excessive inputs of nitrogen and phosphorus (N and P) degrade surface water quality worldwide. Impoundment of reservoirs alters the N and P balance of a basin. In this study, riverine nutrient loads from the upper Yangtze River basin (YRB) at the Yichang station were estimated using Load Estimator (LOADEST). Long-term load trends and monthly variabilities during three sub-periods based on the construction phases of the Three Gorges Dam (TGD) were analyzed statistically. The dissolved inorganic nitrogen (DIN) loads from the upper YRB for the period from 1990 to 2009 ranged from 30.47?×?10⁴ to 78.14?×?10⁴ t, while the total phosphorus (TP) loads ranged from 2.54?×?10⁴ to 7.85?×?10⁴ t. DIN increased rapidly from 1995 to 2002 mainly as a result of increased fertilizer use. Statistics of fertilizer use in the upper YRB agreed on this point. However, the trend of the TP loads reflected the combined effect of removal by sedimentation in reservoirs and increased anthropogenic inputs. After the TGD impoundment in 2003, decreasing trends in both DIN and TP loads were found. The reduction in DIN was mainly caused by ammonium consumption and transference. From an analysis of monthly loads, it was found that DIN had a high correlation to discharges. For TP loads, an average decrease of 4.91 % in October was found when the TGD impoundment occurred, but an increase of 4.23 % also occurred in July, corresponding to the washout from sediment deposited in the reservoir before July. Results of this study revealed the TGD had affected nutrient loads in the basin, and it had played a role in nutrient reduction after its operation.     

Diffuse source apportionment of the Po river eutrophying load to the Adriatic sea: assessment of Lombardy contribution to Po river nutrient load apportionment by means of an integrated modelling approach

The source apportionment of the annual nutrient load carried by the Po river to the Adriatic sea has been studied.

An integrated modelling approach was applied to the Lombardy plain area, which covers about 34% of the Po river watershed area and accounts for about 50% of the point sources’ loads carried by the river. To extract all the information available from direct instream measurements, two different modelling tools were alternatively used. The source apportionment was investigated considering both dry and wet weather scenarios. In order to quantify the apportionment in dry-weather conditions, the Lombardy portion of the Po river basin was modelled by using the US-EPA QUAL2E model. Such a simulation allowed to assess a significant contribution (about 50% of the total dry-weather load) of a not rain-driven diffuse pollution component (i.e. groundwater, springs, lake emissaries). Moreover, to estimate the rain-driven surface runoff contribution to the instream total load, the Lombardy plain area was also modelled by means of the US-DA SWAT model. SWAT results indicate a runoff contribution to the Po river instream total load of about 10 000 t N yr⁻¹ and 1300 t P yr⁻¹ (i.e. approximately the 10–20% of the total annual Lombardy nutrient load). At the event scale (i.e. the single rainstorm event) the runoff contribution may rise up to 30–80% of the total instream load. Finally, the total annual nitrogen load at the Po basin closure was estimated for the period 1985–2001. Out of a total annual load of 140 000 t N yr⁻¹, Lombardy accounts for 43% (point plus diffuse sources). The rain-driven diffuse sources constitute the 20% of the overall total load, the point sources account for 40%, whereas the remaining 40% is mainly constituted by “dry-weather diffuse sources” (i.e. groundwater, springs, lake emissaries).     

Will urban expansion lead to an increase in future water pollution loads?—a preliminary investigation of the Haihe River Basin in northeastern China

Urban expansion is a major driving force changing regional hydrology and nonpoint source pollution. The Haihe River Basin, the political, economic, and cultural center of northeastern China, has undergone rapid urbanization in recent decades. To investigate the consequences of future urban sprawl on nonpoint source water pollutant emissions in the river basin, the urban sprawl in 2030 was estimated, and the annual runoff and nonpoint source pollution in the Haihe River basin were simulated. The Integrated Model of Non-Point Sources Pollution Processes (IMPULSE) was used to simulate the effects of urban sprawl on nonpoint source pollution emissions. The outcomes indicated that the urban expansion through 2030 increased the nonpoint source total nitrogen (TN), total phosphorous (TP), and chemical oxygen demand (COD) emissions by 8.08, 0.14, and 149.57 kg/km², respectively. Compared to 2008, the total nonpoint emissions rose by 15.33, 0.57, and 12.39 %, respectively. Twelve percent of the 25 cities in the basin would increase by more than 50 % in nonpoint source TN and COD emissions in 2030. In particular, the nonpoint source TN emissions in Xinxiang, Jiaozuo, and Puyang would rise by 73.31, 67.25, and 58.61 %, and the nonpoint source COD emissions in these cities would rise by 74.02, 51.99, and 53.27 %, respectively. The point source pollution emissions in 2008 and 2030 were also estimated to explore the effects of urban sprawl on total water pollution loads. Urban sprawl through 2030 would bring significant structural changes of total TN, TP, and COD emissions for each city in the area. The results of this study could provide insights into the effects of urbanization in the study area and the methods could help to recognize the role that future urban sprawl plays in the total water pollution loads in the water quality management process.     

Dechlorination and organohalide-respiring bacteria dynamics in sediment samples of the Yangtze Three Gorges Reservoir

Several groups of bacteria such as Dehalococcoides spp., Dehalobacter spp., Desulfomonile spp., Desulfuromonas spp., or Desulfitobacterium spp. are able to dehalogenate chlorinated pollutants such as chloroethenes, chlorobenzenes, or polychlorinated biphenyls under anaerobic conditions. In order to assess the dechlorination potential in Yangtze sediment samples, the presence and activity of the reductively dechlorinating bacteria were studied in anaerobic batch tests. Eighteen sediment samples were taken in the Three Gorges Reservoir catchment area of the Yangtze River, including the tributaries Jialing River, Daning River, and Xiangxi River. Polymerase chain reaction analysis indicated the presence of dechlorinating bacteria in most samples, with varying dechlorinating microbial community compositions at different sampling locations. Subsequently, anaerobic reductive dechlorination of tetrachloroethene (PCE) was tested after the addition of electron donors. Most cultures dechlorinated PCE completely to ethene via cis-dichloroethene (cis-DCE) or trans-dichloroethene. Dehalogenating activity corresponded to increasing numbers of Dehalobacter spp., Desulfomonile spp., Desulfitobacterium spp., or Dehalococcoides spp. If no bacteria of the genus Dehalococcoides spp. were present in the sediment, reductive dechlorination stopped at cis-DCE. Our results demonstrate the presence of viable dechlorinating bacteria in Yangtze samples, indicating their relevance for pollutant turnover.     

Assessing the effect of natural controls and land use change on sediment yield in a major Andean River: the Magdalena drainage basin, Colombia

The Magdalena River, a major fluvial system draining most of the Colombian Andes, is a world-class river, in the top 10 in terms of sediment load (approximately 150 MT/yr). In this study, we explore the major natural factors and anthropogenic influences behind the patterns in sediment yield on the Magdalena basin and reconstruct the spatial and temporal pattern of deforestation and agricultural intensification across the basin to test the relationships between land use change and trends in sediment yield. Our results show that sediment yield for the whole Magdalena catchment can be explained by natural variables, including runoff and maximum water discharge. These two estimators explain 58% of variance in sediment yield. Temporal analyses of sediment discharges and land use show that the extent of erosion within the catchment has increased over the last 10 to 20 years. Many anthropogenic influences, including a forest decrease by 40% in a 20-year period, an agriculture and pasture increase by 65%, poor soil conservation and mining practices, and increasing rates of urbanization, may have accounted for the overall increasing trends in sediment yield on a regional scale.     

Modeling mercury fluxes and concentrations in a Georgia watershed receiving atmospheric deposition load from direct and indirect sources

This paper presents a modeling analysis of airborne mercury (Hg) deposited on the Ochlockonee River watershed located in Georgia. Atmospheric deposition monitoring and source attribution data were used along with simulation models to calculate Hg buildup in the subwatershed soils, its subsequent runoff loading and delivery through the tributaries, and its ultimate fate in the mainstem river. The terrestrial model calculated annual watershed yields for total Hg ranging from 0.7 to 1.1 microg/m2. Results suggest that approximately two-thirds of the atmospherically deposited Hg to the watershed is returned to the atmosphere, 10% is delivered to the river, and the rest is retained in the watershed. A check of the aquatic model results against survey data showed a reasonable agreement. Comparing observed and simulated total and methylmercury concentrations gave root mean square error values of 0.26 and 0.10 ng/L, respectively, in the water column, and 5.9 and 1 ng/g, respectively, in the upper sediment layer. Sensitivity analysis results imply that mercury in the Ochlockonee River is dominated by watershed runoff inputs and not by direct atmospheric deposition, and that methylmercury concentrations in the river are determined mainly by net methylation rates in the watershed, presumably in wetted soils and in the wetlands feeding the river.     

晋江西溪流域茶园降雨径流产污特征

在野外模拟降雨条件下,开展了晋江西溪流域茶园和裸地的径流产沙及氮磷养分流失过程对比实验,研究结果表明,在相同降雨强度下,3种下垫面径流和产沙量顺序均为:裸地＞2年茶园＞4年茶园,径流量与产沙量之间呈显著正相关.对地表径流水相而言,2年茶园、4年茶园和裸地的TN流失量分别为:461.29、129.38和107.86 mg/m2;NO3-N流失量分别为:286.42、98.58和103.00 mg/m2,均占TN流失量的60％以上;NH4-N流失量分别为:48.67、16.19和4.42 mg/m2;Tp流失量分别为:34.71、16.47和23.88 mg/m2.对径流泥沙相而言,2年茶园、4年茶园和裸地的TN流失量分别为:379.28、44.81和747.16 mg/m2,占流失总量的比重在25.72％～87.93％之间;TP流失量分别为:27.94、4.17和58.85 mg/m2,占流失总量的比重在53.42％ ～68.36％之间.茶园的N、P主要随径流流失,而裸地以泥沙迁移为主.这说明茶叶种植具有一定的水土保持效应,且种植年限较长的茶园可显著减少随径流泥沙进入水体中的N、P元素.