京杭运河常州段泥水界面无机氮交换过程模拟研究

分别在枯水期、平水期、丰水期利用原柱样静态释放实验对京杭运河常州段4个点位的无机氮界面交换过程进行模拟,并借助模拟结果对运河不同形态氮的界面循环过程进行了初步探讨。结果表明,全年NH+4N界面交换特征均表现为底泥向上覆水体释放,平均交换速率比较结果为平水期[182.3mg/(m2·d)]>丰水期[94.0mg/(m2·d)]>枯水期[29.5mg/(m2·d)],而底泥污染严重的下游点位释放通量高于其他断面;丰水期底泥为上覆水NO-3N的源,平水期和丰水期则成汇,且平水期底泥平均吸附速率若为枯水期的6倍;全年NO-2N交换过程表现底泥吸附的特征,枯水期交换速率极低,全年底泥DIN(总无机氮)输入量>输出量,底泥对高浓度上覆水NO-3N的吸附作用可能是底泥污染逐渐加重的原因。     

金鱼藻对工业废水中氨氮的去除行为研究

工业废水处理过程中,如何有效控制氨氮浓度,是废水排放重要的工艺之一。金鱼藻是常见的水生植物,对水质具有较强的净化作用,本实验通过模拟氨氮污染的培养环境,研究不同氮浓度对金鱼藻去除氮能力的影响。结果表明,氮浓度不高于10 mg/L时,处理7 d后水体中氨氮的去除率接近90%;在氨氮浓度分别为20 mg/L和50 mg/L时,经过35 d的处理,氨氮去除率分别为85%和66%,金鱼藻吸收富集的氮含量随着培养水体中氮浓度升高而增加,且不同部位间吸附含量在高浓度情况下差异较为明显。使用金鱼藻对实际工业废水进行氨氮去除处理,去除率达到73%。将植物吸附污染物应用在工业废水处理工艺中具有一定的前景,值得深入研究。     

福建泉州市东、西湖水体中氮的空间分布研究

初步探讨了东湖和西湖水体中氯的空间分布特征以及3种不同形态的氮与溶解氧的相关性.结果表明,(1)泉州东湖、西湖水体中总氮的平均含量分别为3.396、3.929mg/L,氨氮的平均含量分别为1.927、2.182mg/L,硝酸盐氮的平均含量分别为1.061、1.236mg/L,亚硝酸盐氮的平均含量分别为0.084、0.059 mg/L,东湖和西湖水体的主要氮素形式均是氨氮.(2)东湖出水口和位于动物园附近的采样点总氮、氨氮和亚硝酸盐氮浓度较其它采样点高,入水口、湖区北部及湖心区采样点的氨氤和硝酸盐氮的分布趋势基本一致.西湖东南部采样点总氮、氨氯、硝酸盐氯和亚硝酸盐氮的含量都较其它采样点高.(3)东湖水体的DO浓度与氨氛、硝酸盐氮和亚硝酸盐氯的含量都不具有相关性,而西湖水体的DO浓度与这3种形态氮显著相关.     

环境水质氨氮的快速检测

采用全固体混合试剂,将改进的水杨酸分光光度法应用于水质氨氮的测定.络合物的最大吸收波长为697 nm,表观摩尔吸光系数为2.00×104 L/(mol·cm),氨氮质量浓度在0.01 mg/L～1.00 mg/L之间符合比尔定律,反应产物颜色在3 h内保持稳定,常见的共存离子均不干扰测定,混合试剂保存期长,可用于环境水质氨氮的快速检测.     

动态顶空-箱式法在湖泊挥发性有机物释放观测中的应用

湖泊是挥发性有机物(VOCs)的重要自然源,适用的观测手段是湖泊VOCs释放研究的基础。该研究以人工观测池模拟水华水体,以动态顶空-箱式法收集水气界面释放的VOCs,联用甲烷-非甲烷总烃分析仪和飞行时间质谱仪,并辅以阀切换,实现野外2种场景VOCs释放的同时高时间分辨率在线观测。结果表明,合理设置参数后方法重现性好、精度高,相对偏差绝大部分在±10%内;直接进样-氢火焰离子化检测、膜富集-飞行时间质谱检测分别适用于水面释放甲烷和非甲烷VOCs的观测。人为引入浓藻的试验池甲烷、非甲烷VOCs释放速率分别为66.2、2.18 mg/(m²·d),而对照池则分别为2.39、1.15 mg/(m²·d),正午前后非甲烷VOCs释放强度大,傍晚至凌晨则甲烷释放强烈;经试验组、对照组的差异对比以及试验组内物质释放速率之间相关性分析,初步推断藻类释放了壬烷、癸烷、异戊二烯、苯乙烯、氯苯、二氯苯、三氯苯、三氯乙烯、四氯乙烯等物质。     

空气中肼监测标准方法研究——固体吸附采样/分光光度法

本方法适用于空气中低浓度肼的监测。含肼空气通过涂20％H_2SO_4的101白色担体采样管,所含的肼与H_2SO_4反应,生成稳定的N_2H_4·H_2SO_4,洗脱后与对二甲胺基苯甲醛反应,生成黄色的连氮化合物在460nm波长下测定吸光度。以1L/min流速、采集60min空气样的最小检出浓度为0.0012mg/m~3。在0.00714～1.00mg/m~3的浓度范围内,测定的总平均变异系数为7.4％。氯气、甲基肼和偏二甲肼氧化产物对测定有干扰。     

基于比值法解析老城区河段氮磷污染特征

2013年12月—2015年2月,对南淝河老城区约4 km河段水体和主要点源的氮、磷污染物进行测定,并利用碳氮比(CODCr/TN)、氮磷比(TN/TP)、氨氮百分含量(NH3-N/TN)等主要指标对所得数据进行分析研究。结果表明,南淝河老城区段水体的氮磷污染严重,氨氮百分含量接近甚至超过50%,具有一般城市生活污水的特征;氮磷比在春夏季处于藻类适宜的生长范围(9.0TN/TP22.6);整个水体处于低碳氮比水平(碳氮比小于2.5),不利于水体的净化;主要受上游望塘污水处理厂、城市生活污水和地表径流的影响。其主要支流四里河水体的氮磷污染亦相当严重,且氮、磷污染物的输入途径一致。     

杭州西湖水体生态环境参数的相互关系

采用 2 0 0 0年的西湖常规监测数据 ,分析了西湖水体中生态环境特征参数的季节变化和相互关系。分析表明 ,西湖水体各生态环境参数 ,除总氮外 ,均呈现出明显的季节性变化 ,总磷、溶性正磷酸盐、叶绿素 a和藻类季节变化一致 ,在夏季形成高峰 ,冬季最低 ;三无机氮高峰值出现在冬季 ,夏季含量为全年最低。 2 0 0 0年西湖水体总氮年均值为 2 .0 5 m g/L ,总磷年均值为 0 .12 6mg/L ,N/P大于 16,西湖属于磷控制型富营养湖泊。通过相关分析 ,从另一方面说明磷是西湖水体的限制因子 ;硝酸盐对西湖沉积物和湖水之间的磷酸盐平衡有一定的影响 ;硝酸盐对西湖水体中浮游植物生长繁殖可能有抑制作用     

贵阳市臭氧浓度变化及与气象因子的关联性

运用2013—2016年贵阳市环境空气自动监测站臭氧(O_3)的监测数据以及气象观测资料,分析该地区近地面O_3浓度的时空变化特征及与气象因子的关联性。结果表明,近年来贵阳市近地面O_3小时浓度均值有逐年升高趋势,增速为1. 1～5. 0μg/(m~3·a)。O_3浓度昼间变化呈明显单峰形分布,08:00左右出现最低值,15:00—16:00达到最大峰值,浓度高值主要分布在12:00—18:00。日照时数每增加1 h,则近地面O_3日最大8 h平均浓度增加8μg/m~3左右,日照时数大于8 h,则近地面O_3日最大8 h平均浓度超过100μg/m~3; O_3小时浓度与温度呈正相关(r=0. 724,α=0. 01),与相对湿度呈负相关(r=-0. 531,α=0. 01)。当日照时数大于8 h、温度超过25℃、相对湿度小于60%时,贵阳市近地面O_3容易出现高浓度值。     

江苏省沿海脊尾白虾养殖池塘重金属污染及潜在生态危害评价

于2020年对江苏省沿海脊尾白虾养殖区池塘的海水、沉积物和脊尾白虾肌肉组织中的重金属进行分析,同时采用单因子污染指数法和潜在生态风险指数法对其沉积物重金属进行评价。结果显示,养殖池塘水体中铜（Cu）、铅（Pb）、镉（Cd）和锌（Zn）的平均质量浓度分别为3.13,1.02,0.094和28.02 μg/L;沉积物中的平均质量分数分别为22.88,19.93,0.18和140.69 mg/kg;虾肌肉组织中的平均质量分数分别为12.49,0.50,0.18和28.65 mg/kg。生态环境质量评价结果表明,参照《海水水质标准》（GB 3097—1997）,水体中Cu、Pb和Cd的质量浓度达到一类标准,Zn的质量浓度达到二类标准,属于清洁水平;沉积物中重金属的质量分数均达到《海洋沉积物质量标准》（GB 18668—2002）一类标准,属于较清洁水平,潜在生态风险为Cd>Zn>Cu>Pb,整体为轻微生态风险等级,Cd为主要污染元素;虾肌肉组织中重金属Pb和Cd的质量分数均达到《无公害食品 海水虾》（NY 5058—2006）标准。     

Heavy metals in water, sediment and tissues of Liza saliens from Esmoriz–Paramos lagoon, Portugal

Esmoriz–Paramos lagoon is an ecosystem of great ecological importance that is located on the northwest coast of Portugal and has been degraded as a result of industrial and anthropogenic activities. Concentrations of heavy metals (Cr, Cu, Pb and Zn) were measured in water, sediment and in tissues (liver and muscle) of Liza saliens, which is the dominant fish from the lagoon. Comparisons between metal concentrations in water and sediments were made with those in tissues of fish caught at the lagoon. Metals in water were quantified predominantly bound to particulate and equalled or exceeded the limit of chronic reference values. Metal concentrations in sediments varied among sampled sites. The relative order of concentrations was “Zn > Cu ∼ Pb > Cr” the same pattern observed for metals in water. Metals in fish tissues showed higher concentrations in liver (262 mg Cu·Kg⁻¹ and 89 mg Zn·Kg⁻¹) than in muscle (<3 mg Cu·Kg⁻¹ and 26 mg Zn·Kg⁻¹), while Pb and Cr were not detected. These results suggest that Cu and Zn are the metals of major concern in the lagoon. Mullet detritivorous feeding habits, bioaccumulation pattern and the high sediment metals concentrations relative to the water suggest that sediments can be the most important source of contamination in this ecosystem. The positive relationship found between Cu in liver and fish length demonstrates that time of exposure is a crucial factor in bioaccumulation. Condition indices (K and HSI) in mullets from the lagoon were higher compared to mullets from sea, suggesting abnormal condition in the lagoon population. We conclude that metals chronic exposure in the lagoon can impose considerable fish stress. The results also show that the lagoon is an area of environmental concern.     

Eutrophication and Sedimentation Patterns in Complete Exploitation of Water Resources Scenarios: An Example from Northwestern Semi-arid Mexico

Water requirements to supply human needs lead water stakeholders to store more water during surplus periods to fulfil the demand during – not only – scarcity periods. At the reservoirs, mostly those in semi-arid regions, water level then fluctuates extremely between rises and downward during one single year. Besides of water management implications, changes on physical, chemical and biological dynamics of these drawdown and refilling are little known yet. This paper shows the results, throughout a year, on solids, nutrients (N and P), chlorophyll-a, and sedimentation changes on the dynamics, when the former policy was applied in a reservoir from the semi-arid Northwestern Mexico. Water level sinusoidal trend impinged changes on thermal stratification and mixing, modifying nutrient cycling and primary producer responses. According to nitrogen and phosphorus concentration as well as chlorophyll-a, reservoir was mesotrophic, becoming hypertrophic during drawdown. Nutrient concentrations were high (1.22 ± 0.70 and 0.14 ± 0.12 mg P l⁻¹), increasing phosphorus and lowering N:P significantly throughout the study period, although no intensive agricultural, no urban development, neither industrial activities take place in the watershed. This suggests nutrient recycling complex mechanisms, including nutrient release from the sediment–water interface as the main nutrient pathway when shallowness, at the same time as mineralization, increases. Outflows controlled nitrogen and phosphorus availability on the ecosystem while organic matter depended on river inflows. As on other subtropical aquatic ecosystems, nitrogen limited primary productivity (Spearman correlation R = 0.75) but chlorophyll-a seasonal pattern showed an irregular trend, prompting other no-nutrient related limitants. Shallowness induced a homogeneous temporal pattern on water quality. This observed temporal variability was mainly explained statistically by changes on solids (mineral and organic), chlorophyll-a and flows (62.3%). Annual sedimentation rates of total solids ranged from 11.73 to 16.29 kg m⁻² year⁻¹ with organic matter comprising around 30%. N:P ratio on sedimentation rates were as high as could be expected in a resuspension dominated ecosystem, and spatially inverse related with N:P ratio on bottom sediments. Distance from river inlet into the reservoir reveals a marked spatial heterogeneity on solid and nitrogen sedimentation, showing the system dependence on river inflows and supporting resuspension as the main phosphorus pathway. Accretion rates (2.19 ± 0.40 cm year⁻¹) were not related to hydrological variability but decreased with the distance to the river input. Total sediment accumulation (9,895 tons km⁻² year⁻¹) denotes siltation as other serious environmental problem in reservoirs but possibly not related with operational procedures.     

Seasonal variations of water column nutrients in the inner area of Ariake Bay, Japan: the role of muddy sediments

To investigate seasonal variations of nutrient distribution in the mudflat–shallow water system, we conducted field surveys once a month from August 2007 to July 2008 in the inner area of Ariake Bay (IAB), Japan. The NH₄ ⁺–N concentration of the water column increased in autumn because of the high NH₄ ⁺ release from the sediments, ranging from 850 to 3,001 μmol?m^?2?day^?1. The NO₃ ^?–N concentration was maximal in January, which was thought to be caused by NO₃ ^? release from the oxic sediments and by NO₃ ^? regeneration due to water column nitrification. The PO₄ ^3?–P concentration of the water column was high in summer–autumn due to the high PO₄ ^3? release from the reduced sediments, ranging from 22 to 164 μmol?m^?2?day^?1. We estimated the total amounts of DIN and PO₄ ^3?–P release (R _DIN and $ {R_{{\mathrm{P}{{\mathrm{O}}_4}}}} $ , respectively) from the muddy sediment area of the IAB. In summer–autumn, R _DIN and $ {R_{{\mathrm{P}{{\mathrm{O}}_4}}}} $ corresponded to about 47.7 % of DIN input and about 116.6 % of PO₄ ^3?–P input from the river, respectively. Thus, we concluded that the muddy sediments were an important source of nutrients for the water column of the IAB during summer–autumn. In addition, we found that phosphorus necessary for the growth of Porphyra (Porphyra yezoensis, Rhodophyceae) would be insufficient in the water column when phosphorus during the Porphyra aquaculture period is supplied only from the river. Therefore, the phosphorus release from the muddy sediments was thought to play an important role in the sustainable production of Porphyra in Ariake Bay.     

Phosphorus fractions and adsorption characteristics of floodplain sediments in the lower reaches of the Hanjiang River, China

The phosphorus fractions and adsorption characteristics of seven floodplain sediment samples collected in the lower reaches of China’s Hanjiang River were studied. Most phosphorus fractions showed a marked downstream increase in response to point-source inputs from urban areas. Total phosphorus (TP) contents in the sediments ranged from 603.68 to 945.25 mg.kg⁻¹. Inorganic phosphorus (IP) was the major component of TP, and calcium-bound phosphorus (Ca–P) was the major fraction of IP. The distribution characteristics of the phosphorus contents were affected by sediment grain size and hydrodynamic conditions. The maximum phosphorus adsorption capacities (Q _max) and the half-saturation concentration (k) were obtained using an improved Langmuir model. Native adsorbed exchangeable phosphorus content (w _NAP) and the zero-equilibrium phosphorus concentration value (c _EPC0) were subsequently calculated. The effects of sediment grain size, temperature, and disturbance on the phosphorus adsorption isotherms were also studied. The results showed that phosphorus adsorption on floodplain sediments was primarily chemisorption; the particle concentration effect played a more important role at a disturbance intensity of 150 r.min⁻¹ (on a shaker table) than at 100 r.min⁻¹.     

Spatial and seasonal variability of pore water phosphorus concentration in shallow Lake Swarzędzkie,Poland

Pore waters play an important role in phosphorus dynamics in aquatic ecosystems. Phosphorus concentrations in pore waters are much higher than above the bottom. This is confirmed by the results of this study concerning the hypereutrophic lake. Pore water was analyzed at 11 sampling stations in the upper layer of bottom sediments. This water was separated by centrifugation and phosphorus level was measured spectrophotometrically with ascorbic acid as a reducer. Total phosphorus concentration in pore waters ranged from 0.5 to 8.1 mgP l^− 1 (mean 3.2 mgP l^− 1). Mean phosphorus concentration in pore water samples of this lake was the highest in summer and the lowest in winter. High concentrations were observed in samples from the pelagial and low from the macrophyte zone.     

连续流动注射间接测定空气中的五氧化二磷

建立连续流动注射间接测定空气中五氧化二磷的方法。空气中的五氧化二磷用过氯乙烯滤膜或滤筒采样,加入去离子水反应生成正磷酸,过滤、洗涤、定容后运用连续流动注射仪进行测定。优化了抗坏血酸浓度、硫酸浓度、钼酸盐浓度以及恒温室温度等影响显色的因素。最佳条件下,实际样品五氧化二磷加标回收率为96.0%~102%,相对标准偏差在4%以下;采样体积为300 L时,方法检出限为0.001 6 mg/m~3。t检验结果表明,所建方法与现行国标法的测定结果无显著性差异。方法分析速度快、重现性好、灵敏度高,适用于空气中五氧化二磷的测定。     

Application of GIS in the study of mass transport of pollutants by Adyar and Cooum Rivers in Chennai, Tamilnadu

Residential, industrial, commercial, institutional and recreational activities discharge degradable and non-degradable wastes that reach the coastal water through rivers and cause coastal pollution. In the present study, mass transport of pollutants by Adyar and Cooum Rivers to the coastal water as a result of land-based discharges was estimated during low tide. The lowest and the highest flow recorded in Adyar varied from 514.59 to 2,585.08×10⁶ litres/day. Similarly, the flow in Cooum River fluctuated between 266.45 and 709.34×10⁶ litres/day. The present study revealed that the Adyar River transported 53.89–454.11 t/d of suspended solids, 0.06–19.64 t/d of ammonia, 15.95–123.24 t/d of nitrate and 0.4–17.86 t/d of phosphate, 0.004–0.09 kg/d of cadmium, 0.15–1.29 kg/d of lead and 3.03–17.58 kg/d of zinc to the coastal water owing to its high discharge. Similarly, the Cooum River transported 11.87–120.06 t/d of suspended solids, 0.08–58.7 t/d of ammonia, 6.11–29.25 t/d of nitrate and 0.66–10.73 t/d of phosphate, 0.003–0.021 kg/d of cadmium, 0.02–0.44 kg/d of lead and 1.36–3.87 kg/d of zinc. A higher concentration of suspended solids was noticed in post monsoon and summer months. An increase in the mass transport of ammonia, nitrate, phosphate in summer months (April and May) and an increase in the mass transport of cadmium, lead and zinc were observed in monsoon months (October–December) in both the rivers. Thus mass transport of pollutants study reveal that Cooum and Adyar Rivers in Chennai contribute to coastal pollution by transporting inorganic and trace metals significantly through land drainage.     

Monitoring of Aerial Pollutants Emitted from Swine Houses in Korea

This on-site survey study was performed to determine the concentrations and emissions of aerial contaminants in the different types of swine houses in Korea and then to present beneficial information available for Korean pig producers to manage optimal air quality in swine house. The swine houses investigated in this research were selected based on three criteria; manure removal system, ventilation mode and growth stage of swine. Mean concentrations of aerial pollutants in swine houses were 8 ppm for ammonia, 300 ppb for hydrogen sulfide, 2 mg m⁻³ for total dust, 0.6 mg m⁻³ for respirable dust, 4 log(cfu m⁻³) for total airborne bacteria and 3 log(cfu m⁻³) for total airborne fungi, respectively. Mean emissions based on pig (liveweight; 75 kg) and area (m²) were 250 and 340 mg h⁻¹ for ammonia, 40 and 50 mg h⁻¹ for hydrogen sulfide, 40 and 50 mg h⁻¹ for total dust, 10 and 15 mg h⁻¹ for respirable dust, 1.0 and 1.3 log(cfu) h⁻¹ for total airborne bacteria and 0.7 and 1.0 log(cfu) h⁻¹ for total airborne fungi, respectively. In general concentrations and emissions of gases were relatively higher in the swine houses managed with deep-pit manure system with slats and mechanical ventilation mode than the different swine housing types whereas those of particulates and bioaerosol were highest in the naturally ventilated swine houses with deep-litter bed system.     

Examination of reactive phosphate fluxes in an eutrophicated coastal area

Reactive phosphate (RP) fluxes over sediment in an eutrophic bay were obtained under different conditions. The results were assessed together with water column, sediment solid, and liquid-phase parameters. The RP fluxes ranged from 0 to 1,300 μgatP × m^-2d^-1 day depending on the sediment site and other variables. At stations with relatively high net RP fluxes, the clay fraction was >3% and disproportionate with salinity, which explained why the RP effluxes decreased by inhibition of the organic coating on particulate matter with increased SO₄ ⁻² ions and good competition of RP anions with SO₄ ⁻². The RP flux in Fe/RP ratios >2 in surface water decreased to approach a minimum asymptotically, which was thus defined with a hyperbolic curve to determine the maximum rate of the RP flux (J_RP). The [RP_porewater]_initial/[RP_ambient] _initial ratios were suggested to govern the net RP flux regionally, so the critical value where the RP flux turns positive could indicate eutrophication with Chl-a values <500 μg/g. So, this study investigated the phosphate fluxes between sediment and water column and determined the factors influencing the RP fluxes in the inner bay of Izmir.     

Assessment of nitrogen and phosphate balance and the roles of bacteria and viruses at the water-sediment interface in the Allal El Fassi reservoir (Morocco)

Balances of nitrogen and phosphate were studied in the Allal El Fassi reservoir (Morocco); the results showing that nitrogen input (296 mg m^?2 d^?1) was 161 % higher than output (183 mg m^?2 d^?1). Phosphate input (35.65 mg m^?2 d^?1) was 865 % higher than output (4.12 mg m^?2 d^?1), causing a progressive increase in the internal phosphate stock. Sedimentation flux was equally high (53.80 and 18 mg m^?2 d^?1) for both nitrogen and phosphate input, mainly from the Sebou River and in particulate form which immediately settles upon arrival in the reservoir. The release of nitrogen and phosphate from the sediment (5.40 and 1.15 mg m^?2 d^?1, respectively) depended on physicochemical and biological (bacteria and viruses) variability and the calcareous nature of the catchment basin. Calcium-bound phosphate prevailed in the reservoir. Drastic control of phosphate input is suggested to avoid accumulation of calcium-bound phosphate which may dissociate and thereby contribute to eutrophication.