大镜山水库底泥磷释放模拟研究

通过模拟实验,研究了从耗氧到厌氧转变过程中期间大镜山水库底泥磷的释放特征。结果表明:两处底泥均表现为磷的释放,大坝区底泥释放速率高于库中区的底泥;两个点底泥的磷释放速率均先升高后缓慢降低,在第2周达到最大值;大坝区域底泥总磷和可溶性总磷释放的最大速率分别为6.64mg·m-2·d-1和1.37mg·m-2·d-1,库中区底泥的总磷和可溶性总磷的释放速率最大值分别3.24mg·m-2·d-1和0.62mg·m-2·d-1;底泥上覆水的氧化还原电位和pH均趋下降趋势,它们是影响底泥磷释放的重要影响因子。     

不同覆盖方式对底泥内源营养盐释放的控制效果

通过底泥内源营养盐释放控制室内模拟试验,考察了塑料包被、斜发沸石、方解石、石英砂和硝酸钙5种覆盖材料对底泥氮磷释放效率的影响,系统分析了各自优劣程度,为实际环境中不同污染背景水体选择适宜的控制技术提供科学依据.结果表明: 不同覆盖材料对底泥总磷释放的控制效果依次为:塑料包被>硝酸钙>斜发沸石>方解石>石英砂;不同覆盖材料对底泥总氮释放的控制效果依次为:斜发沸石>塑料包被>方解石>石英砂>硝酸钙;不同覆盖材料对底泥硝态氮释放的控制效果依次为:塑料包被>斜发沸石>方解石>石英砂>硝酸钙;不同覆盖材料对底泥铵态氮释放的控制效果依次为:硝酸钙>石英砂>斜发沸石>方解石>塑料包被;温度和底泥内源营养盐释放有对应关系,水样中总磷、总氮和硝态氮浓度会随着温度上升而增加,而铵态氮浓度呈下降趋势.     

富营养化水体的水生植物净化试验研究

利用水生植物净化和底泥遮蔽的方法对养鱼池的富营养化水体进行控制研究．结果表明,金鱼藻等6种水生植物对水中总氮、总磷和硝态氮有较好的去除效果,而以狐尾藻和微齿眼子菜两种效果最好,1个月后对总氮的去除率分别为83．84％和77．54％,对硝态氮的去除率分别为95．85％和90．65％,磷的去除率都达到了91．7％．但对氨氮的去除效果稍差,1个月时去除效果只有14％～70％．底泥进行塑料遮蔽处理后在前期(15～20d)能控制底泥中营养盐的释放,但不能保持长久;并在后期表现出“补偿效应”．试验结果还表明。水生植物能有效提高水体透明度和水体观感,但对改善COD和DO的效果不明显．     

初春马来眼子菜分解对水体和底泥碳、氮和磷积累及释放的影响

通过实验室模拟初春温度(17℃)条件,研究了沉水植物马来眼子菜(Potamogeton malaianus Miq.)分解过程对其有机碳、总氮和总磷的释放,水体和底泥中有机碳、总氮和总磷含量以及水体中铵态氮和硝态氮含量的影响,同时对水体N2和N2O的释放状况进行了分析。结果表明:在70 d的实验周期内,马来眼子菜分解迅速,至实验结束时植株失重率达到86.92%,植株中有机碳量、总氮量和总磷量分别较实验初始时降低了88.51%、88.93%和86.63%;底泥中有机碳、总氮和总磷含量分别较实验初始时增加了5.56%、17.06%和2.17%。在马来眼子菜分解过程中,水体中的溶解氧含量和氧化还原电位均较对照明显降低,并呈现在实验初期迅速下降然后逐渐增加并趋于稳定的趋势;水体中的有机碳、总氮、总磷以及铵态氮含量均较对照大幅度增加,并呈现在实验初期迅速上升然后逐渐下降并趋于稳定的趋势;而水体中的硝态氮含量则呈先下降后上升再下降的趋势。水体中N2和N2O释放通量较对照明显增加,且在实验中期N2和N2O释放通量达到峰值。研究结果表明:随时间推移,马来眼子菜向水体释放的磷大部分沉积到底泥中,而氮则部分沉积到底泥中、部分以气体形式(N2和N2O)逸出水体。     

铜锈环棱螺对藻华水体沉积物-水界面营养盐通量的影响

于2008年在室内小型试验模拟生态系统中进行了为期1个月的铜锈环棱螺生物干扰对底泥耗氧率和上覆水营养盐通量的影响试验,根据铜锈环棱螺放养密度设置了3个处理组和1个对照组。与试验前相比,培养1个月后,所有处理组和对照组的底泥耗氧率均显著下降;各处理组的底泥耗氧率初期高于对照组,后期低于对照组,且密度高的处理组其底泥耗氧率高于密度低的处理组。除12月7日外,对照组沉积物始终向上覆水释放铵氮,且释放量逐渐减小,而各处理组中,除试验初期沉积物向上覆水释放铵氮外,试验中后期均表现为吸收铵氮。除试验初期外,处理组和对照组中亚硝酸盐+硝酸盐通量主要表现为向上覆水中释放,且处理组1与对照组间存在显著差异(P<0.05)。磷酸盐通量主要表现为,试验初期沉积物向上覆水中释放,后期被沉积物吸收。本试验结果表明,短期内铜锈环棱螺的生物干扰增加了底泥耗氧率,但其长期效应可使底泥耗氧率下降,铜锈环棱螺的存在促进了沉积物中的总体硝化速率,加快了沉积物中的N循环。     

柳树对水体氮素的去除率及其吸收动力学

在水培条件下,研究了2种柳树(Salix integra)无性系(“一支笔”和“微山湖”)对模拟富营养化水体中氮素的吸收状况,并采用常规耗竭法探讨了柳树幼苗根系对NH4+-N、NO3--N的吸收动力学特征.结果表明:2种柳树无性系对低浓度模拟富营养化水体中总氮的去除率均达90％以上,是高浓度情况下的2倍;对低浓度模拟污水中总磷的去除率达80％,高浓度下则达92％,且“一支笔”对总氮、总磷的吸收效果优于“微山湖”;2种柳树无性系对氮素的吸收均表现为水体中营养物质浓度越高,去除效果越好;只有NH4+-N或NO3--N存在时,“微山湖”的最大吸收速率和亲和力高于“一支笔”;当有其他氮源影响时,2种柳树无性系对NH4+-N和NO3--N的吸收效率则下降至50％;研究表明,柳树对富营养化水体的生态修复作用较强,是进行面源污染生态修复的优良树种.     

白洋淀菹草对富营养化水体总磷的净化

利用白洋淀区域鲥鯸淀、王家寨和小淀3个淀区的水体、底泥和菹草组成室内静态的模拟生长体系,研究白洋淀菹草在不同水体及底泥环境下的生长状况,以及不同菹草生长体系对水体总磷的净化效果.结果表明:鲥鯸淀菹草生长体系对水体总磷的净化效果最佳,最大去除率为87.9%,单位生物量对水体总磷的最大去除率为2.2%;王家寨和小淀菹草生长体系对水体总磷的最大去除率分别为47.4%和76.9%,单位生物量对水体总磷的最大去除率分别为0.9%和1.4%.3个菹草生长体系的底泥对水体总磷吸附的最大百分比分别为9.1%、7.4%和7.7%.菹草生长体系的TP-t和v-t拟合方程表明,水体中总磷浓度及其去除速率随时间的延长以负指数形式衰减.     

鲤对浅水湖泊水质影响的围隔实验研究

鲤是我国浅水湖泊常见鱼类,鲤可以通过扰动底泥、牧食浮游动物、排泄营养盐等途径影响湖泊水质。为了研究鲤对浅水湖泊水质的影响,论文于2009年6月23日至8月18日在暨南大学明湖进行原位围隔实验。实验分为三个处理组(三组围隔):(1)在围隔中放养鲤(放鱼组);(2)在围隔底部放置塑料隔网,在隔网上部空间放养鲤(放鱼放网组);(3)围隔中不放隔网也不放鲤(空白对照组)。实验结果表明:鲤可以显著增加水体悬浮物、总氮、总磷和叶绿素a含量,显著降低了水体透明度。而鲤是否扰动底泥对水体悬浮物、总氮、总磷和叶绿素a含量等指标的影响不显著。 因此,该研究中鲤对浅水湖泊的影响可能主要是通过排泄等途径实现的,鲤扰动底泥对水质的影响不大。     

石头口门水库流域土地利用／覆被变化对非点源污染负荷的影响

应用L-THIA (Long-Term Hydrologic Impact Assessment )模型,模拟吉林省石头口门水库流域1986 年至2000 年的非点源污染负荷,定量评价土地利用/覆被变化对非点源污染负荷的影响.研究结果表明:1 )1986 ～2000 年期间,研究区土地利用/覆被变化的主要特点为:水田和旱田增加,草地和裸地减少;土地利用/覆被变化对非点源污染负荷的影响非常显著;2 )1986年、1995 年、2000 年三个时段内研究区各非点源污染负荷呈现先增加后减少的趋势,泥沙和总氮的变化幅度较大,总磷的变化幅度相对较小;整个研究时段内表现为总磷的变化幅度大于泥沙和总氮;3 )农田、林地、居民地的变化对非点源污染负荷影响明显,属于非点源污染的敏感区,其面积的较小变化均可引起污染负荷的较大变动;4 )林地和草地转化为农田导致各非点源污染物负荷均增加,其中草地转化为农田的区域较小(5 km2 ),但导致总磷污染增加了255.52 kg ;农田变为居民地和林地导致污染负荷减少,林地转化为草地使得泥沙、总磷污染增加,总氮污染减少.     

惠州西湖底泥中氮磷特征的初步研究

惠州西湖为典型的亚热带城市浅水湖泊。为了调查该湖泊底泥性质了解底泥对水质的影响。2004年8月在惠州西湖5个子湖（南湖、丰湖、平湖、菱湖和鳄湖）采集了6个底泥柱样,对其含水率、烧失量（LOI）、总氮（TN）、总磷（TP）、藻类可利用性磷（AAP）和粒度的垂向特征进行了初步研究。结果表明,各子湖中南湖内源负荷最大,底泥中的LOI、TN、TP和AAP含量高于其他湖区数倍以上,表层值较高,表明曾遭受过严重的污染,而其它湖区的垂向变化不明显。底泥成分以粘土、粉砂为主,水体混浊度高可能与底泥粒径较小以及鱼类和游船活动的强扰动性有关。     

赣江流域土地利用方式对河流水质的影响

赣江是鄱阳湖的最大支流,是鄱阳湖水污染物的主要来源,查明流域土地利用方式对赣江水质的影响和鄱阳湖的水环境保护具有重要意义。基于2012年对赣江7个主要支流NH+4-N、TP、CODMn和DO浓度的每月测定结果,通过不同空间尺度和土地类型等级划分,利用相关分析和冗余分析研究土地利用方式对赣江流域河流水质的影响。研究结果表明,子流域的土地利用方式对TP的影响大于缓冲区;对CODMn的影响在丰水期大于缓冲区,在枯水期小于缓冲区;对NH+4-N的影响在丰水期与缓冲区接近,在枯水期小于缓冲区;DO受土地利用方式的影响较小。水田中的丘陵水田是赣江水体TP和丰水期CODMn的主要来源;平原水田是枯水期CODMn的主要来源。居民建设用地中的城镇用地是赣江水体TP、NH+4-N和丰水期CODMn的主要来源,农村用地是CODMn的主要来源。水域中的水库坑塘是赣江水体TP和丰水期NH+4-N、CODMn的主要来源。     

Design and performance of a filtration-adsorption pool train and drawing water system for small urban recreational water pollution control

A filtration-adsorption pool train (FAPT) and drawing water (DW) system was developed to control the small urban recreational water pollution at a senior hotel in Shanghai, China. The results from one year of operation indicated that the system had successfully achieved the water quality objectives: compared with the water quality before the treatment system worked, the average concentrations of SS, COD_Mn, BOD₅, NH₃-N, TP and Chla were reduced by 79%, 39.5%, 45%, 36%, 44.3% and 70%, respectively, and DO and transparency were improved by 27% and 134%, respectively. The customers enjoyed a recreational, aesthetic and educational amenity along the ring pond. Therefore, it was conducted that the FAPT-DW system was an effective measure for small recreational waters, especially in urban areas with limited land resources.     

Remediation of Nitrogen-Contaminated Sediment Using Bioreactive,Thin-layer Capping with Biozeolite

In situ amendment of nitrogen-contaminated sediment using bioreactive, thin-layer capping (BTC) with biozeolite (i.e., zeolite with heterotrophic nitrifiers as well as aerobic denitrifiers attached) was studied herein. BTC with biozeolite for nitrogen-contaminated sediment management was evaluated through long-term (170 days) sediment incubation laboratory experiments. The results showed that BTC with relatively small dose rates (<10 kg m^?2) of biozeolite reduced the total nitrogen (TN) concentration in overlying water by over 90%, so it was effective in reducing the amount of N released from sediment. Higher-dose rates of biozeolite capping achieved an even higher removal efficiency. With the DO concentration of 1.5 ～ 6.5 mg L^?1 in overlying water, the reduction efficiency of TN in overlying water using BTC was higher than that less than 1 mg L^?1. In BTC systems, biological regeneration (i.e., heterotrophic nitrifiers attached to zeolite can regenerate the zeolite ion exchange capacity for ammonium) occurred in biozeolite which was saturated with ammonium during the nitrification period. In addition, TN contents in surface sediment in BTC systems were reduced at different levels after the experiment. These findings indicate that the BTC can be a feasible remedial approach to reduce N in overlying water and sediment in eutrophic water bodies. In the BTC, N load was reduced by the added biozeolite through adsorbing ammonium (NH₄⁺-N), converting NH₄⁺-N into nitrate nitrogen (NO₃^?-N) and nitrogen gas (N₂), and assimilating inorganic nitrogen.     

辽河流域辽宁段水环境演变与流域经济发展的关系

以流域为单元进行社会经济发展与环境保护调控,是实现可持续发展的有效途径,因此以流域为单元开展社会经济发展与水环境变化相互作用的研究方兴未艾。运用多元线性回归分析,选取社会经济指标(第一产业生产总值、第二产业生产总值、年末总人口)为自变量,水质指标(化学需氧量、氨氮浓度)为因变量定量研究了2001—2010年辽河水环境演变与流域内社会经济发展之间的关系;并采用经济增长指标(人均GDP)、水环境指标(化学需氧量、氨氮浓度)作为模型中指标,进行了环境库兹涅茨曲线模拟与分析。根据研究结果推断:第二产业生产总值、人口是影响辽河水质化学需氧量浓度变化的社会经济重要因素,影响氨氮浓度变化的因素众多;辽河流域经济增长与水环境之间的关系曲线不完全符合典型的库兹涅茨曲线特征。随着经济快速增长,应在开展工业点源污染达标排放控制的同时,加强农业面源污染的治理力度。     

Nitrogen dynamics in a eutrophic lake sediment

Nitrogen flux from sediment of a shallow lake and subsequent utilization by water hyacinth (Eichhornia crassipes [Mart] Solms) present in the water column were evaluated using an outdoor microcosm sediment-water column. Sediment N was enriched with ¹⁵N to quantitatively determine the movement of NH₄-N from the sediment to the overlying water column. During the first 30 days. 48% of the total N uptake by water hyacinth was derived from sediment ¹⁵NH₄-N. This had decreased to 14% after 183 days. Mass balance of N indicates that about 25% sediment NH₄-N was released into the overlying water, but only 17% was assimilated by water hyacinth. NH₄-N levels in the water column were very low, with very little or no concentration gradients. NH₄-N levels in the interstitial water of the sediment were in the range of 30–35 mg L^–1 for the lower depths (> 35 cm), while in the surface 5 cm of depth NH₄-N levels decreased to 3.2 mg L^–1. Simulated results also showed similar trends for the interstitial NH₄-N concentration of the sediment. The overall estimated NH₄-N flux from the sediment to the overlying water was 4.8 µg cm^–2 day^–1, and the soluble organic N flux was 5.8 µg N cm^–2 day^–1. Total N flux was 10.6 µg N cm^–2 day^–1.     

Assessment of Water Quality and Identification of Polluted Risky Regions Based on Field Observations & GIS in the Honghe River Watershed,China

Water quality assessment at the watershed scale requires not only an investigation of water pollution and the recognition of main pollution factors, but also the identification of polluted risky regions resulted in polluted surrounding river sections. To realize this objective, we collected water samplings from 67 sampling sites in the Honghe River watershed of China with Grid GIS method to analyze six parameters including dissolved oxygen (DO), ammonia nitrogen (NH₃-N), nitrate nitrogen (NO₃-N), nitrite nitrogen (NO₂-N), total nitrogen (TN) and total phosphorus (TP). Single factor pollution index and comprehensive pollution index were adopted to explore main water pollutants and evaluate water quality pollution level. Based on two evaluate methods, Geo-statistical analysis and Geographical Information System (GIS) were used to visualize the spatial pollution characteristics and identifying potential polluted risky regions. The results indicated that the general water quality in the watershed has been exposed to various pollutants, in which TP, NO₂-N and TN were the main pollutants and seriously exceeded the standard of Category III. The zones of TP, TN, DO, NO₂-N and NH₃-N pollution covered 99.07%, 62.22%, 59.72%, 37.34% and 13.82% of the watershed respectively, and they were from medium to serious polluted. 83.27% of the watershed in total was polluted by comprehensive pollutants. These conclusions may provide useful and effective information for watershed water pollution control and management.     

Biodiversity and water quality variations in constructed wetland of Yongding River system

This research was carried on in constructed wetlands of Guan-Ting Reservoir, Beijing, China, from 2004 to 2005. The phytoplankon community was composed of 8 divisions (94 species, including genus and varieties) and the average cell density was 980.93× 10⁴ cells per liter. The dominant divisions were Chlorophyta (36.8%), Bacillariophyta (31.0%) and Cyanophyta (23.4%). The removal rate of phytoplankton density was 72.7%. There was a positive linear correlation between phytoplankon density and total phosphorus. Here, 7 families (13 species) of aquatic vasular plants were found, which constituted emerging and submerging macrophyte communities. In the wetland system, the zooplankton community consisted of Protozoa, Rotifera, Cladocera and Copepoda (70 species). The average density was 4883 individuals per liter. Protozoan and Rotifera were the dominant groups and the removal rate of their density was 81.9%. The correlation between zooplankton and phytoplankton presented a quadratic curve. Also, the zoobenthos community contained Olisochaeta, Uniramia, Crustacea and Mollusca (15 species). The average density was 5670 individuals per m² (62.3% was Uniramia) and the removal rate of their density was 92.4 %. The wetland system reduced COD_Mn, BOD₅, TN, NH_3-N, NO_3-N, TP (total phosphor), PO_4-P and SS in the water of Yong Ding River at 52.9%–99.1%.     

Effects of Land Use,Topography and Socio-Economic Factors on River Water Quality in a Mountainous Watershed with Intensive Agricultural Production in East China

Understanding the primary effects of anthropogenic activities and natural factors on river water quality is important in the study and efficient management of water resources. In this study, analysis of Variance (ANOVA), Principal component analysis (PCA), Pearson correlations, Multiple regression analysis (MRA) and Redundancy analysis (RDA) were applied as an integrated approach in a GIS environment to explore the temporal and spatial variations in river water quality and to estimate the influence of watershed land use, topography and socio-economic factors on river water quality based on 3 years of water quality monitoring data for the Cao-E River system. The statistical analysis revealed that TN, pH and temperature were generally higher in the rainy season, whereas BOD₅, DO and turbidity were higher in the dry season. Spatial variations in river water quality were related to numerous anthropogenic and natural factors. Urban land use was found to be the most important explanatory variable for BOD₅, COD_Mn, TN, DN, NH₄ ⁺-N, NO₃ ⁻-N, DO, pH and TP. The animal husbandry output per capita was an important predictor of TP and turbidity, and the gross domestic product per capita largely determined spatial variations in EC. The remaining unexplained variance was related to other factors, such as topography. Our results suggested that pollution control of animal waste discharge in rural settlements, agricultural runoff in cropland, industrial production pollution and domestic pollution in urban and industrial areas were important within the Cao-E River basin. Moreover, the percentage of the total overall river water quality variance explained by an individual variable and/or all environmental variables (according to RDA) can assist in quantitatively identifying the primary factors that control pollution at the watershed scale.     

Study on ecological protection and rehabilitation technology of a reservoir-type water source in the northeastern region of China

ABSTRACT

Surface water is the main source of water for human life and production. The quality of water affects living conditions and the overall health of people. Ecological protection and restoration engineering technology, combining ecological revetment and an ecological floating bed, is applied to a selected shallow beach experimentation area of a reservoir water source area in Northeast China. According to local conditions, the ecological revetment plants were identified as Goosegrass, sedges, and water grasses, and other local species of Polygonum hydropiper bagen, reeds, and bulrushes were identified as ecological floating bed plants. Regular monitoring of water quality in the experimentation area and a control area showed that the ecological protection and restoration technology can effectively reduce the concentrations of BOD₅ (five day biochemical oxygen demand), COD (chemical oxygen demand), TN, NH₃-N, NO₃^?-N, TP, TDP, Mn, Zn, Fe, Pb, total coliforms, and other indicators of surface water in the experimentation area. The BOD₅, COD, Max TN, NH₃-N, NO₃^?-N, TP, and TDP reduction rates were 84.76%, 57.14%, 86.76%, 83.78%, 89.26%, 94.02%, and 95.89%, respectively, with the implementation of water pollution prevention and the purifying shoal.     

太湖水华程度及其生态环境因子的时空分布特征

湖泊水华是全世界面临的严重生态环境问题之一,对人类和生态系统健康都有重大影响。由于湖泊水华受流域面源、点源污染、气候、水文因子以及湖泊生态系统自身特征等众多因素影响,水华是否爆发、其严重程度及时空分布特征呈现明显的复杂性。以我国太湖为研究区域,基于近年的水华及水环境的监测数据,用自组织特征映射神经网络对太湖不同监测点的水华程度进行了自动聚类分析。结果表明,太湖水华程度呈现为明显的无水华、轻度、中度和重度水华4类。不同程度水华的叶绿素a、水温、COD_(Mn)、营养盐、浮游植物生物量以及藻种(蓝藻、绿藻、硅藻)结构的时空差异显著,不同变量间的关系复杂,有助于深入认识太湖近年水华发生的时空变异特性。