三峡库区澎溪河营养盐时空变化特征及富营养化评价

为考察三峡库区澎溪河营养盐的时空分布特征及营养状态,于2013~2014年对澎溪河不同断面透明度、高锰酸盐指数以及总氮、氨氮、总磷、叶绿素a的含量进行取样调查,对营养盐的时空变化特征进行分析,结合相关性分析,利用单因子法和综合营养状态指数法评价水体营养盐结构和营养状态。结果发现,澎溪河营养盐具有明显的季节差异性和空间分布差异性。相关性分析表明澎溪河上游河段叶绿素a含量与透明度、高锰酸盐指数、总氮含量、总磷含量的线性相关性不显著,而中段高阳渡口叶绿素a含量与总磷含量呈极显著正相关。单因子法评价结果显示,澎溪河水质为Ⅱ~Ⅲ类。水体综合营养状态指标范围为56~135,处于富营养至重度富营养化状态之间;春季3~5月及秋季10月,部分断面富营养化状态极高。     

自贡市釜溪河流域2011～2020年水质特征分析

为改善釜溪河断面水环境质量,采用河流水质单因子评价法,利用近十年的水质监测数据,分析自贡市釜溪河流域地表水环境质量的变化情况.结果表明:通过优化企业布局、生活污水厂提标改造、启用一体化应急处理设施、生态补水等方式,釜溪河流域水质总体呈好转趋势,2019年碳研所断面氨氮、总磷、溶解氧浓度分别较2011年变化了-91.0％...     

SWAT模型在茫溪河流域非点源污染研究中的应用

本研究采用美国农业部农业研究所开发的SWAT模型(Soil and Water Assessment Tool)对茫溪河流域非点源污染进行了模拟研究,构建了适用于茫溪河流域的非点源污染模型,对流域的非点源污染进行了模拟和分析。模拟结果显示:茫溪河流域污染特征以非点源污染为主;东茫溪河水系的泥沙、氮、磷等负荷均大于西茫溪河水系;单位泥沙负荷最大的区域为流域东北部、东部和东南部一带的深丘地区,是茫溪河流域的主要泥沙输出区;氮、磷负荷最大的区域为茫溪河中下游一带的平坝、浅丘地区,是茫溪河流域的主要氮、磷输出区;研究区内泥沙、营养物质的输出具有很强的时间规律,有机氮、有机磷的输出在雨季(6月~9月)会出现高峰,因此雨季是流域内非点源污染源输出的重点时段。     

四川仁寿球溪河流域总磷形态特征研究

为了解仁寿县球溪河流域总磷(TP)形态特征,于2018年6月对流域48个点位进行采样,分析流域TP组成及空间变异性。仁寿县球溪河流域TP以溶解态无机磷(DIP)为主,占比达到70.3%(sd.=18%)。不同支流、不同河段TP形态特征有所差别,与沿程地形地貌、土地使用类型、人口分布相关。上游河段受农业面源及山区河道冲刷影响PP比例相对较高;中游及下游受生活污染为主,DIP比例升高;部分支流下游河段受沉积物再悬浮及农业面源输入影响,PP比例有所升高。     

重庆市澎溪河湿地自然保护区湿地植物资源研究

以重庆市澎溪河湿地自然保护区为研究对象,对保护区内的湿地植物资源进行了全面调查.结果表明,保护区内湿地植物共有34科67属100种,主要的植被类型有4个植被型及宽叶香蒲群落(Typha latifolia )、水蓼群落(Polygonum hydropiper)等17个群系,并分析了植被分布特征和新生消落带的影响.鉴于湿地植物对生物多样性的保护和蕴含的巨大生产力,提出了湿地植物保护和利用的对策.     

基于SWAT模型污染防治措施对茫溪河水质改善影响研究

为了更好地开展茫溪河的污染防治,摸清茫溪河流域污染源贡献比例以及各种污防措施对水质改善效果十分必要。基于SWAT构建了茫溪河流域分布式水文和污染负荷模型,根据监测数据分析了茫溪河近年超标污染物,基于SWAT模型分析了茫溪河水质达标场景假设,包括污染源贡献率及生态补水、点源和面源等污染防治措施对水质改善的效果情况。结果表明,茫溪河流域超标项目集中在总磷和高锰酸盐指数;污染源中,面源相对于点源对高锰酸盐指数和总磷贡献率大些,特别是水土流失的贡献率最大,分别达到了42.8%和76.1%;生态补水对污染物浓度降低有一定影响,直排源和非直排源污染控制一定程度上使污染物浓度降低,达标率有所提升。基于SWAT模型的茫溪河水质达标场景分析对于推动水质改善具有积极的意义。     

蒙溪河流域水环境污染及演变趋势研究

研究采用Arc GIS确定蒙溪河流域研究范围,在此基础上进行水环境污染现状及演变趋势分析、污染源调查和水环境容量计算。结果表明:蒙溪河流域水质超标情况较严重,主要超标因子为:COD、TN和TP,COD和TP的压力主要集中在平水期,TN压力主要集中在枯水期;污染源汇入主要集中在4#-9#点位之间。蒙溪河流域污染物入河量从大到小依次为:农业面源、城镇生活污水、农村生活污水、规模化畜禽养殖、畜禽散养和底泥污染。蒙溪河流域达标需削减污染物量:COD为217.755t/a,NH_3-N为24.683t/a,TN为75.710t/a,TP为10.774t/a。     

北方河流湿地土壤NO3-N和NH4+-N的空间变化特征研究

以辽河保护区七星湿地为研究对象,通过对湿地土壤NO3--N和NH4+-N空间分布及湿地土壤含水量与pH指标分析,研究流域湿地土壤无机氮空间变化特征.研究结果表明,湿地土壤含水量影响NO3--N和NH4+-N的空间分布,湿地土壤含水量高,土壤中NO3--N的含量相对较高;湿地土壤含水量低,土壤中NH4+-N的含量相对较高...     

流域非点源分布式模型AnnAGNPS参数的不确定性研究

流域非点源分布式模型的不确定性研究成为目前的热点问题之一。本研究以宁波市章溪河流域为研究区,通过GIS软件AreView和AnnAGNPS模型,集成利用莫里斯分类筛选法,选取临界源面积、SCS曲线系数、水土保持因子、饱和导水率、氮磷吸收率、施肥量等6个因子进行敏感性分析。模拟结果表明,土壤饱和导水率、水土保持因子和径流曲线CN值对模型输出结果影响较大;水土保持因子对泥沙、总磷和总有机碳负荷的模拟结果影响最大,均呈显著负效应;径流曲线CN值对总氮负荷计算结果影响最大,呈显著正效应。     

濑溪河流域泸县段水污染源分析及对策研究

采用输出系数模型、等标污染负荷等方法,以研究区实测数据为基础,评价濑溪河泸县段水质现状,结合基于水文水质资料和文献数据的方法确定输出系数取值,估算了濑溪河泸县段COD、氨氮、总磷污染负荷并分析主要来源。结果表明,濑溪河泸县段水质现状较差,总磷为全流域首要污染物;濑溪河泸县段COD污染负荷的主要来源于城镇生活、工业生产,累计占总入河量的60%;氨氮污染负荷主要来自于城镇生活、农业面源,累计占总入河量的64%;总磷污染负荷主要来自农业面源、分散畜禽养殖,累计占总入河量的75%。建议进一步加快城镇生活污染治理设施建设,强化工业企业污染治理,完善农村农业污染防治,实施流域综合整治及生态修复。     

福州城市排污规划布局的水环境影响研究

以闽江下游福州城区段为研究区间,分析了闽江下游福州段的水环境质量现状,采用二维水动力-水质耦合模型研究了枯水期城市排污口布局和排污强度规划对水环境质量的影响。研究结果表明,感潮河段排污存在明显的污染物上溯现象,在东南区水厂至马尾水厂备用水源地之间形成高浓度污染团,洋里和连坂排污口对东南区水厂水源地水质影响最为显著,高潮时刻的高锰酸盐指数增量将达1.0mg/L,氨氮增量将达约0.15mg/L,叠加本底值后水质已接近Ⅲ类标准限值。建议逐步将取水口向城市上游淮安段转移,更换取消东南区水厂的取水口。     

闽江口海域化学需氧量与溶解氧周年变化特征分析

根据2008年1—12月的调查数据,对闽江口海域海水中的COD和DO分布状况与特征进行周年的研究表明,闽江口海域全年的COD含量为0．63～1．70mg／L,符合第一类海水水质标准,季节性变化的规律不明显,受闽江冲淡水的影响,海水中的COD平面分布呈现近岸高,向外逐渐降低的趋势。海水中的DO含量为5．46—8．03mg／L,海水中DO较充沛。尽管受闽江每年向闽江口海域输送大量COD的影响,但是海水中的COD含量仍然较低,该海域具有较大的COD环境容量。     

Distributions of median nutrient and chlorophyll concentrations across the Red River Basin, USA

Acquisition and compilation of water-quality data for an 11-yr time period (1996-2006) from 589 stream and river stations were conducted to support nutrient criteria development for the multistate Red River Basin shared by Arkansas, Louisiana, New Mexico, Oklahoma, and Texas. Ten water-quality parameters were collected from six data sources (USGS, Arkansas Department of Environmental Quality, Louisiana Department of Environmental Quality, Oklahoma Conservation Commission, Oklahoma Water Resources Board, and Texas Commission on Environmental Quality), and an additional 13 parameters were acquired from at least one source. Median concentrations of water-quality parameters were calculated at each individual station and frequency distributions (minimum, 10th, 25th, 50th, 75th, 90th percentiles, and maximum) of the median concentrations were calculated. Across the Red River Basin, median values for total nitrogen (TN), total phosphorus (TP), and sestonic chlorophyll-a (chl-a) ranged from < 0.02 to 20.2 mg L(-1), < 0.01 to 6.66 mg L(-1), and 0.10 to 262 microg L(-1), respectively. Overall, the 25th percentiles of TN data specific to the Red River Basin were generally similar to the USEPA-recommended ecoregion nutrient criteria of 0.31 to 0.88 mg L(-1), whereas median TP and chl-a data specific to the Red River Basin showed 25th percentiles higher than the USEPA-recommended criteria (0.010-0.067 mg TP L(-1); 0.93-3.00 microg chl-a L(-1)). The unique location of the Red River Basin in the south-central United States places it near the boundaries of several aggregate ecoregions; therefore, the development of ecoregion nutrient criteria likely requires using data specific to the Red River Basin, as shown in these analyses. This study provided basin-specific frequency distribution of median concentrations of water-quality parameters as the first step to support states in developing nutrient criteria to protect designated uses in the multijurisdictional Red River Basin.     

IMPACTS OF CLIMATE CHANGE ON MISSOURI RWER BASIN WATER YIELD1

ABSTRACT: Water from the Missouri River Basin is used for multiple purposes. The climatic change of doubling the atmospheric carbon dioxide may produce dramatic water yield changes across the basin. Estimated changes in basin water yield from doubled CO₂ climate were simulated using a Regional Climate Model (RegCM) and a physically based rainfall‐runoff model. RegCM output from a five‐year, equilibrium climate simulation at twice present CO₂ levels was compared to a similar present‐day climate run to extract monthly changes in meteorologic variables needed by the hydrologic model. These changes, simulated on a 50‐km grid, were matched at a commensurate scale to the 310 subbasin in the rainfall‐runoff model climate change impact analysis. The Soil and Water Assessment Tool (SWAT) rainfall‐runoff model was used in this study. The climate changes were applied to the 1965 to 1989 historic period. Overall water yield at the mouth of the Basin decreased by 10 to 20 percent during spring and summer months, but increased during fall and winter. Yields generally decreased in the southern portions of the basin but increased in the northern reaches. Northern subbasin yields increased up to 80 percent: equivalent to 1.3 cm of runoff on an annual basis.     

嘉陵江下游饮用水氟化物时空变异特征研究

饮用水中可溶性氟化物是公众摄入氟的主要途径,其含量水平影响人体健康.分别于2015～2017年的丰水期和枯水期6次随机采集监测了嘉陵江下游52个饮用水样中氟化物含量,并基于地理信息系统平台和健康风险指数法进行了评价.结果表明,该区域饮用水中氟化物浓度平均为0.20～0.25 mg/L.除2015年部分样点外,其余样点的...     

FACTORS AFFECTING PESTICIDE OCCURRENCE AND TRANSPORT IN A LARGE MIDWESTERN RIVER BASIN1

ABSTRACT: Several factors affect the occurrence and transport of pesticides in surface waters of the 29,400 km² White River Basin in Indiana. A relationship was found between pesticide use and the average annual concentration of that pesticide in the White River, although this relationship varies for different classes of pesticides. About one percent of the mass applied of each of the commonly used agricultural herbicides was transported from the basin via the White River. Peak pesticide concentrations were typically highest in late spring or early summer and were associated with periods of runoff following application. Concentrations of diazinon were higher in an urban basin than in two agricultural basins, corresponding to the common use of this insecticide on lawns and gardens in urban areas. Concentrations of atrazine, a corn herbicide widely used in the White River Basin, were higher in an agricultural basin with permeable, well‐drained soils, than in an agricultural basin with less permeable, more poorly drained soils. Although use of butylate and cyanazine was comparable in the White River Basin between 1992 and 1994, concentrations in the White River of butylate, which is incorporated into soil, were substantially less than for cyanazine, which is typically applied to the soil surface.     

WATER QUALITY CHARACTERISTICS OF AGRICULTURAL PUMPAGE IN THE UPPER ST. JOHNS RIVER,FLORIDA1

Several large agricultural pumps, located in the upper St. Johns River Basin, Florida, and representative of the numerous pumps operating in the basin, were monitored during the spring and summer of 1982. These pumps have rated capacities ranging from 36 to 334 ft³/s and drain various quantities of improved pasture, row crop, and citrus land uses. The combined total pumping capacity of the pumps in this study is approximately equal to the average flow at US 192, near Melbourne (691 cfs). Results indicate high nutrient and suspended solids loading to the river, but the relative magnitude of each parameter varies with pump site and date. The row crop/Mary A pump (267 ft³/s capacity) exhibited the poorest water quality of the sampled pumps and appeared to have the greatest pollutional potential. The average suspended solids loading rate from the Mary A pump was high (37,900 Kg/day). The average total nitrogen (TN) and total phosphorus (TP) discharge concentrations at this pump were also high, with values of 3.96 mg/L and 0.79 mg/L, respectively. As expected, nutrient loading rates reflected discharge rates, to a large degree. Average TN loading rates for the pumping stations varied from 86 to 1935 Kg/day while TP loading ranged from 7 to 390 Kg/day. Nutrients from pumping are contributing factors to the increasing aquatic plant growth and algal blooms in the area. Poor quality discharge water, as well as rapid rises in water level from the cumulative discharges resulting in dead marsh vegetation and accompanying oxygen sags, have been suggested as causative factors for fish kills in the area.     

Vegetation and carbon sequestration and their relation to water resources in an inland river basin of Northwest China

In the Heihe River Basin in the arid inland area of northwest China, the distribution of water resources in vegetation landscape zones controls the ecosystems. The carbon sequestration capacity of vegetation is analyzed in relation to water resources and vegetation growing conditions. During the last 20 years, the vegetation ecosystems have degenerated in the Heihe River Basin. Simulation using the C-FIX model indicates that, at present, the total amount of NPP of vegetation accounts for about 18.16 TgC, and the average value is 106 gC/m(2)/yr over the whole basin. NPP has generally the highest value in the upperstream mountain area, middlestream artificial oases area, downstream river bank area, alluvial fan and the terminal lake depression where vegetation grows relatively well. The lowest value is found in the vast downstream desert and Gobi area. Protection of vegetation ecosystems and enhancement of carbon sequestration require such inland river basins as the Heihe River Basin to be brought under management in a comprehensive way, taking water as a key, to carry out a rational and efficient allocation and utilization of water resources.     

SELENIUM BUDGETS FOR LAKE POWELL AND THE UPPER COLORADO RWER BASIN1

ABSTRACT: A selenium budget for Lake Powell, Utah-Arizona was determined based on selenium loads at the principal stream input sites to and the output site from the lake. Based on data collected during 1985-1994, 83 percent of the selenium entering Lake Powell is accounted for at the output site. The rest of the selenium may be incorporated by lake sediment or used by the biota. Considerably more selenium per unit area is produced from the Colorado River Basin above the Colorado River-Green River confluence than from the Green River Basin and the San Juan River Basin combined. The Gunnison River Basin and the Grand Valley in Colorado produce an estimated 31 and 30 percent of the selenium that reaches Lake Powell, respectively. Irrigation-related activities are thought to be responsible for mobilizing 71 percent of the selenium that reaches Lake Powell. Selenium concentrations in water at Imperial Dam on the Colorado River upstream of the United States-Mexico international border are similar to those at the output site of Lake Powell. Therefore, most selenium observed in downstream areas of the Colorado River therefore probably is derived mostly from the Colorado River Basin above Lake Powell.     

Urea Fluctuations in Stream Baseflow across Land Cover Gradients and Seasons in a Coastal Plain River System

Urea‐N is a component of bioavailable dissolved organic nitrogen (DON) that contributes to coastal eutrophication. In this study, we assessed urea‐N in baseflow across land cover gradients and seasons in the Manokin River Basin on the Delmarva Peninsula. From March 2010 to June 2011, we conducted monthly sampling of 11 streams (4 tidal and 7 nontidal), 2 wastewater treatment plants, an agricultural drainage ditch, and groundwater underlying a cropped field. At each site, we measured urea‐N, DON, dissolved organic carbon (DOC), total dissolved nitrogen (TDN), NO₃^?‐N, and NH₄⁺‐N. In general, urea‐N comprised between 1% and 6% of TDN, with the highest urea‐N levels in drainage ditches (0.054 mg N/L) and wetland‐dominated streams (0.035–0.045 mg N/L). While urea‐N did not vary seasonally in tidal rivers, nontidal streams saw distinct urea‐N peaks in summer (0.038 mg N/L) that occurred several months after cropland fertilization in spring. Notably, the proportion of wetlands explained 78% of the variance in baseflow urea‐N levels across the Manokin watershed. In wetland‐dominated basins, we found urea‐N was positively related to water temperature and negatively related to DOC:DON ratios, indicating short‐term urea‐N dynamics at baseflow were more likely influenced by instream and wetland‐driven processes than by recent agricultural urea‐N inputs. Findings demonstrate important controls of wetlands on baseflow urea‐N concentrations in mixed land‐use basins.