氮磷对引黄水库水中小球藻生长的影响

以济南市引黄水库中分离出的小球藻为研究对象,研究不同光温条件对其生长的影响;在此基础上设计了4因素3水平正交实验研究氮磷物质对小球藻生长的影响。结果表明,小球藻的最适生长温度为30℃,光强为6 000 lx;氮磷营养盐对藻类生长影响的重要性排序为硝酸盐磷酸盐氨氮亚硝酸盐。引黄水库氮磷含量较稳定,适于小球藻的生长,夏、秋季节应加强小球藻水华的监控预警。     

以再生水为补水的景观水体水华爆发特征调查和药剂应急控藻效果评价

采用现场调查和实验室验证的方法,对以再生水为景观补水的水华优势藻进行了分析。2年的现场调查表明,再生水在条件适合时极易发生水华,且水华的优势藻以小球藻为主。在实验室针对小球藻和铜绿微囊藻进行了竞争生长实验研究,在再生水的氮磷浓度范围内小球藻生长快于铜绿微囊藻,这也验证了再生水作为景观水补水时小球藻是优势藻现场调查结论。针对水华爆发初期和水华爆发验证时2种条件,比较研究了4种以化学成分为主的抑藻药剂对以小球藻为水华特征藻的控藻效果。结果表明,这4种药剂对水华的控制均具有一定的效果,并且水华初期实施药剂抑藻,药剂投加少,且效果好。对4种药剂进行急性毒性实验,只有S2一种药剂在安全浓度时对水华爆发初期有抑藻效果。     

海河干流天津段氮磷对藻类生长的影响及动力学分析

本实验以海河干流天津段水体为对象,对其中四种典型共存藻类(即铜绿微囊藻、小球藻、卵囊藻和席藻)在不同氮磷营养盐环境条件下的响应生长规律进行了过程表征及动力学研究。实验结果表明,N/P在10~40范围适宜藻类生长,N/P为10时藻类比增长率最大;氮浓度水平在2.0~15 mg·L~(-1)、磷浓度水平在0.2~1.5 mg·L~(-1)内,藻类比增长率随着氮磷浓度的升高而增大,当氮浓度为15 mg·L~(-1),磷浓度为1.5 mg·L~(-1)时达到最大,优势藻为卵囊藻;通过Monod藻类生长动力学分析得出,藻类最大比增长率为0.050 8,半饱和常数为0.157,表明目标河段水华暴发风险相对较低,且磷是藻生长限制性因子。     

水华束丝藻与铜绿微囊藻净化水体氮磷及其脂质积累过程比较

选取水华束丝藻与铜绿微囊藻作为典型水华蓝藻,探索水华蓝藻净化水体及合成生物柴油的潜力.采用氮磷浓度为NH4-N 7.5 mg/L,PO43--P 1.0 mg/L的模拟污水,重点考察了在光照强度与温度不同的条件下2种微藻对氮磷的去除率,并利用尼罗红荧光染色法测定了微藻中的中性脂含量.结果表明,2种藻对PO43--P的去除率均较高,最高达到98％,对NH4+-N的去除率稍低,最高为52％.水华束丝藻及铜绿微囊藻均具有较强积累中性脂的能力,适宜的温度与光照条件有利于微藻对氮磷的去除及细胞中脂类的积累.2种藻均在光照强度为12 000 lx时中性脂含量更高.水华束丝藻在温度为18 ～22℃条件下,生长更优,氮磷净化效果较好,中性脂积累能力更强.而铜绿微囊藻在温度为22～ 26℃时表现更好.     

附着藻类对浮游藻类生长抑制的试验研究

通过室内模拟实验,研究了在实验室条件下,以控制一定的温度、照度、pH值等条件,并设置氮磷比在10：1到25：1的范围内变化时,观测浮游藻类单独培养和浮游附着藻类混合培养时的生长竞争情况,为富营养化水体的水华控制提供一定的理论依据。另外,还探讨了以葡萄糖为外加碳源,对浮游藻类和附着藻类生长状况的影响。结果表明,在氮磷比为20：1时,浮游藻类单独培养和混合培养下的浓度差最高,其值为159×10^5 cells／L。随着氮浓度的增高,当温度越高时,附着藻类对浮游藻类的竞争优势越明显。同时浮游藻类比附着藻类更能适应较高的COD浓度。     

淀山湖底泥氮磷营养盐释放及其影响因素研究

通过大量现场实测数据,对建立的淀山湖水生态系统模型进行率定和验证,并利用该模型对淀山湖底泥氮磷营养盐释放机制进行了系统研究,模拟了温度、流量、入流负荷等因素对底泥氮磷营养盐释放的影响。模拟结果显示:(1)该模型较好地模拟了底泥释放的动态变化;淀山湖底泥无机磷具有一定的释放特性,无机氮以底泥吸附为主,底泥磷酸盐、氨氮、硝酸盐氮释放通量分别为-40~18、-15~75、-38~-10mg/(m2·d)。(2)不同季节下温度对底泥氮磷营养盐的释放影响作用不同。(3)在氮磷营养盐释放较明显的夏秋季节,流量对氮磷营养盐释放影响较大。(4)削减入流负荷会加快底泥氮磷营养盐的释放,当入流负荷削减达到95%时,底泥中氮磷营养盐开始全面转向正释放状态。淀山湖外源污染得到控制以后,沉积物中营养物将对水体水质构成威胁。     

固定化藻菌去除海水冲厕污水中氮磷的实验研究

采用海藻酸钠凝胶包埋固定小球藻和活性污泥,对冲厕海水污水（模拟）中的氮磷污染物进行去除实验。结果表明,在藻菌比为2：1,固定化藻菌对氮磷的去除率分别达到95．5％和92．2％。在N／P为10时,固定化藻菌对冲厕海水污水中氮磷的去除效果最好。25～30℃时固定化藻菌对氨氮和磷的去除率最好,温度过高时藻和细菌细胞的活性受到抑制。固定化藻菌体系处理冲厕海水污水的较佳pH范围在6．5～8．5之间。     

光照条件对跑道池光生物反应器内蛋白核小球藻生长特性的影响

本文采用多孔曝气管的曝气方式,以蠕动泵为藻液循环的动力,研究了气体流量、光照强度、光照周期等因素对跑道池光生物反应器内蛋白核小球藻生长与代谢特性的影响,并利用傅里叶红外光谱半定量法对不同光照条件下藻细胞内蛋白质、油脂以及多糖含量变化进行了分析。研究结果表明,适当的气体流量、光照强度和光照周期有利于跑道池内蛋白核小球藻细胞的生长和代谢。在本实验条件下,在最佳气体流量2 000 m L/min条件下,光照强度为3 500μW/cm2,光照周期为16∶8时最有利于蛋白核小球藻的生长;光照强度为2 000μW/cm2和光照周期为16∶8的条件均有利于藻细胞内油脂的积累。     

不同氮磷比对多年生水生植物生长特性影响的研究

从氮、磷等植物生长的环境因子出发,研究了高低氮磷营养水平下,不同氮／磷比例的富营养化水体对聚草（Myriophyllum spicatum）、黄花水龙（Jussiaea stipulacea Ohwi）、喜旱莲子草（Alternanthera philoxeroides）生长特性的影响。结果表明,聚草在氮磷比2：1时生物量最大,且生物量在高浓度水平处理明显大于低浓度水平处理（P〈0．01）;黄花水龙在氮磷比10：1～20：1时生物量最大,高低浓度水平处理问生物量无显著性差异;喜旱莲子草在较高氮磷比20：l～40：1时生物量最大,高浓度水平处理时生物量显著性高于低浓度水平处理（P〈0．05）。在低浓度水平处理时,氮为黄花水龙和喜旱莲子草生长的主要限制因子,磷为聚草生长的主要限制因子,且喜早莲子草叶绿素增长期较其他处理提前,而黄花水龙的叶绿素变化在高低营养水平下差异不显著。营养盐水平对聚草茎长和生物量的影响较对黄花水龙和喜旱莲子草的影响明显。     

RO浓水-废水联合培养小球藻的实验研究

为了实现微藻培养基的低成本化和废水资源化利用多重目的的耦合,对反渗透浓缩液(RO浓水)作为培养基培养小球藻(Chlorella sp.)的可行性及其影响因素进行了探讨。实验取一级、二级处理出水和消化反应上清液及3种废水与RO浓水混合液制成6种培养基培养小球藻,探究最佳培养基;在此基础上探究浓度与温度对小球藻生长的影响。结果表明,培养15 d后,3种添加了RO浓水的培养基比3种纯废水培养基更有利于小球藻的生长,其中消化反应上清液-RO浓水混合液是最佳培养基;浓水浓度0%~90%的该混合液中小球藻生物量增加315%~780%,且小球藻的生物量表现为随RO浓水浓度的增大先增加后减小的变化趋势,30%是小球藻最佳培养浓度;在10、20和30℃下,浓度0%~90%的培养基中小球藻生物量增加了140%~570%,各浓度中的小球藻均在20℃下生长最好。     

3种药剂对普通小球藻的抑制作用

针对再生水回用于景观水体生长的主要藻类普通小球藻,进行了药剂抑制实验。通过实验研究发现,在小球藻生长的对数期分别投入不同剂量的2-甲基乙酰乙酸乙酯（EMA）、大麦秸萃取液（BSE）和异噻唑啉酮3种抑藻药剂后,小球藻的生长受到不同程度的抑制。其中,EMA对藻类的抑制效果甚微,最大抑藻率仅为31%,且对小球藻的生长有低促高抑的作用。BSE对小球藻有明显的抑制作用,且药效期长、不复发;当投加浓度为1 mg/L,能起到抑制藻类生长的作用;当投加浓度为10 mg/L,能起到杀灭水体藻类的作用。异噻唑啉酮可有效抑制小球藻生长,5 mg/L的投加浓度就能起到杀灭水体藻类的作用,且药效期长、不复发。     

太湖北部藻类生长旺盛期大气氮、磷沉降特征

按照<大气降水样品的采集与保存标准>(GB/T 153580.2-92)收集大气N、P沉降物和降水量,并测定了2007年5～11月太湖北部梅梁湾藻类生长旺盛期间大气TN、TP的干、湿沉降通量.结果表明,太湖北部梅粱湾大气TN月湿沉降通量和月总沉降通量的变化趋势均呈双峰型特征,与当地梅雨和台风侵袭时的降水量呈明显正相关,并且TN的月湿沉降通量高于月干沉降适量,但降水量最少的11月则相反;大气TP月干、月湿沉降通量呈相互交替的变化趋势.大气N沉降物中主要以溶解性氮(TDN)为主,平均约占91.4%;而P沉降物中溶解性磷(TDP)占的比例相对较低,平均约为65.1%.经测定,2007年太湖北部梅梁湾TN和TP的年沉降通量分别为2 976、84.0 kg/km2,相比2002年7月至2003年6月分别下降34.4%和78.7%;2007年太湖北部梅粱湾大气TN的年沉降量高达6 958 t,远超过太湖湖泊生态系统理论允许的TN年沉降量.     

Study on the dynamics of algal bloom and its influence factors in Tolo Harbour, Hong Kong.

In this paper, the semi-enclosed bay named Tolo Harbour and Channel in Hong Kong, which was frequently attacked by red tides, was used as a case study. Data sets related to marine water quality, river nutrients, and meteorological conditions recorded between 1988 and 1999 were chosen for statistical analysis. A multivariate analysis showed that algal growth, represented by the chlorophyll a concentration, had obvious spatial and temporal variations in the study area. The chlorophyll a concentration had a consistently decreasing trend from the inner part of the Harbour and surface waters to the outer part and bottom waters. The temporal variations had a markedly seasonal variation with high bioproductivity in spring and winter. There were long-term fluctuations in the chlorophyll a concentration with a high-low-high pattern in the study period. Nutrients and hydrological and meteorological conditions were important factors of algal bloom. Besides nitrogen, which was the most critical factor of algal bloom for the whole water body, total phosphorus in the surface waters and phosphate (PO4) and silica (SiO2) in the bottom waters also showed strongly positive or negative correlations with the chlorophyll a level. For the meteorological conditions, global solar radiation was the key factor of massive algal bloom in the study period, while rainfall and wind direction were the most important factors of seasonal variation.     

Influence of algal bloom degradation on nutrient release at the sediment–water interface in Lake Taihu, China

Algal bloom could drastically influence the nutrient cycling in lakes. To understand how the internal nutrient release responds to algal bloom decay, water and sediment columns were sampled at 22 sites from four distinct regions of China’s eutrophic Lake Taihu and incubated in the laboratory to examine the influence of massive algal bloom decay on nutrient release from sediment. The column experiment involved three treatments: (1) water and sediment (WS); (2) water and algal bloom (WA); and (3) water, sediment, and algal bloom (WSA). Concentrations of dissolved oxygen (DO), total nitrogen (TN), total phosphorus (TP), ammonium (NH ₄ ⁺ -N), and orthophosphate (PO ₄ ^3? -P) were recorded during incubation. The decay of algal material caused a more rapid decrease in DO than in the algae-free controls and led to significant increases in NH ₄ ⁺ -N and PO ₄ ^3? -P in the water. The presence of algae during the incubation had a regionally variable effect on sediment nutrient profiles. In the absence of decaying algae (treatment WS), sediment nutrient concentrations decreased during the incubation. In the presence of blooms (WSA), sediments from the river mouth released P to the overlying water, while sediments from other regions absorbed surplus P from the water. This experiment showed that large-scale algal decay will dramatically affect nutrient cycling at the sediment–water interface and would potentially transfer the function of sediment as “container” or “supplier” in Taihu, although oxygen exchange with atmosphere in lake water was stronger than in columns. The magnitude of the effect depends on the physical–chemical character of the sediments.     

Assessment of manure-application effects upon the runoff water quality by algal assays and chemical analyses

The effects of manure-application mode, rate to soil, and rainfall characteristics on the quality of agricultural runoff water have been assessed by means of the algal-growth-potential test (AGPT) and chemical analyses. This study used two modes of manure application (i.e. surface mode and incorporation mode), three manure-application rates (0, 150, 300 kg N ha(-1)), and two rainfall intensities and times (i.e. 11 mm h(-1) for 142 min and 22 mm h(-1) for 71 min). The effects of the dilution of runoff water on algal growth were also examined. The algal yields obtained with runoff from soil with the incorporated manure mode are similar to those from soil without manure application and are lower than those with the surface mode of manure application. A higher manure-application rate increases the load of nutrients in the runoff and subsequently the algal yield. The dilution of runoff water can stimulate or limit the algal growth, depending on the concentration of toxicants, N (nitrogen) and P (phosphorus) from runoff and in the aquatic diluting medium. A lower rainfall intensity plus a longer rainfall time increases algal productivity. This study showed that N is the limiting factor to algal growth at low dilution but that, at high dilution or with the incorporation mode of manure application, P becomes the limiting factor to algal growth.     

Water mass interaction in the confluence zone of the Daning River and the Yangtze River—a driving force for algal growth in the Three Gorges Reservoir

Increasing eutrophication and algal bloom events in the Yangtze River Three Gorges Reservoir, China, are widely discussed with regard to changed hydrodynamics and nutrient transport and distribution processes. Insights into water exchange and interaction processes between water masses related to large-scale water level fluctuations in the reservoir are crucial to understand water quality and eutrophication dynamics. Therefore, confluence zones of tributaries with the Yangtze River main stream are dedicated key interfaces. In this study, water quality data were recorded in situ and on-line in varying depths with the MINIBAT towed underwater multi-sensor system in the confluence zone of the Daning River and the Yangtze River close to Wushan City during 1 week in August 2011. Geostatistical evaluation of the water quality data was performed, and results were compared to phosphorus contents of selective water samples. The strongly rising water level throughout the measurement period caused Yangtze River water masses to flow upstream into the tributary and supply their higher nutrient and particulate loads into the tributary water body. Rapid algal growth and sedimentation occurred immediately when hydrodynamic conditions in the confluence zone became more serene again. Consequently, water from the Yangtze River main stream can play a key role in providing nutrients to the algal bloom stricken water bodies of its tributaries.     

Wastewater nutrient removal by Chlorella pyrenoidosa and Scenedesmus sp

Two different species of photosynthetic microalgae, Chlorella pyrenoidosa and Scenedesmus sp., were grown in settled and activated sewage filtrates at two different inoculum sizes, aimed to reduce nutrient load from wastewater. Higher growth rates were recorded in cultures with higher inoculum size, and algal cells usually grew better in settled sewage than in activated sewage. As algae started to grow and multiply, both nitrogen and phosphorus content in wastewater decreased significantly. The removal rate was rapid during the first week of growth and more than 2/3 of wastewater N and P was reduced. After the initial period, the removal rate slowed down. At the end of this study, more than 80% of total-P and inorganic N present in settled sewage were reduced but such removal efficiency was lower in activated sewage. In general, high inoculum size of algal cells provided more N and P removal than low inoculum, and Chlorella cells performed better than Scenedesmus. These results suggest that cultivation of Chlorella seems to be one of the feasible methods to reduce the amount of nitrogen and phosphorus entering the nearby coastal water, thus preventing the eutrophication problem. It is also clear that algal ponds with high inoculum size might be more suitable to be installed as a secondary rather than a tertiary treatment process.     

工艺条件对鸟粪石法回收磷耗碱量的影响及其理论计算

通过分析磷回收过程中存在的各种耗碱因素,推导出耗碱量的理论计算公式,计算出了不同工艺条件下的理论耗碱量,并与小型连续搅拌反应-沉淀磷回收过程的实验实测值进行比较。结果表明,耗碱量的理论计算值与实验测定值的平均相对误差为13.20%,说明计算方法可用于耗碱量的工程估算;耗碱量随出水pH值的增大而急剧增加,随废水中氨氮含量和磷初始浓度的增加都近似于线性增加,但随镁磷比的增加基本不变。因此,从节约废水处理成本的角度看,磷回收过程中pH值应控制在9.2-9.3,氮磷比控制在3.0-5.0,镁磷比控制在1.1-1.2为佳。磷回收过程的药剂消耗量与废水中磷的浓度和工艺条件有关,以磷初始浓度为124 mg/L,N/Mg/P=5∶1.2∶1,出水pH值为9.20的回收过程为例,处理毎吨废水需消耗片碱0.5313 kg,成本约为1.328元,需消耗氯化镁（含六个结晶水）0.9758 kg,成本约为0.634元。因此,处理每吨废水的药剂成本约为1.962元,其中耗碱约占67.7%。     

N:P ratios,light limitation,and cyanobacterial dominance in a subtropical lake impacted by non-point source nutrient pollution

A long-term (28-year) data set was used to investigate historical changes in concentrations of phosphorus (P), nitrogen (N), N:P ratios, and Secchi disk transparency in a shallow subtropical lake (Lake Okeechobee, Florida, USA). The aim was to evaluate changes in the risk of N2-fixing cyanobacterial blooms, which have infrequently occurred in the lake's pelagic zone. Predictions regarding bloom risk were based on previously published N:P ratio models. Temporal trends in the biomass of cyanobacteria were evaluated using phytoplankton data collected in 1974, 1989-1992, and 1997-2000. Concentrations of pelagic total P increased from near 50 microg l-1 in the mid-1970s to over 100 microg l-1 in the late 1990s. Coincidentally, the total N:P (mass) ratio decreased from 30:1 to below 15:1, and soluble N:P ratio decreased from 15:1 to near 6:1, in the lake water. Published empirical models predict that current conditions favor cyanobacteria. The observations confirm this prediction: cyanobacteria presently account for 50-80% of total phytoplankton biovolume. The historical decrease in TN:TP ratio in the lake can be attributed to a decreased TN:TP ratio in the inflow water and to a decline in the lake's assimilation of P, relative to N. Coincident with these declines in total and soluble N:P ratios, Secchi disk transparency declined from 0.6 m to near 0.3 m, possibly due to increased mineral turbidity in the lake water. Empirical models predict that under the turbid, low irradiance conditions that prevail in this lake, non-heterocystous cyanobacteria should dominate the phytoplankton. Our observations confirmed this prediction: non-N2-fixing taxa (primarily Oscillatoria and Lyngbya spp.) typically dominated the cyanobacteria community during the last decade. The only exception was a year with very low water levels, when heterocystous N2-fixing Anabaena became dominant. In the near-shore regions of this shallow lake, low N:P ratios potentially favor blooms of N2-fixing cyanobacteria, but their occurrence in the pelagic zone is restricted by low irradiance and lack of stable stratification.     

Spatiotemporal distributions of nutrients in the downstream from Gezhouba Dam in Yangtze River, China

Introduction

From December 2008 to November 2009, an investigation of water quality was performed in the 70-km long downstream from Gezhouba Dam in Yangtze River.

Methods

Twelve sites in all were chosen. Nine parameters of water quality including the total phosphorus, the total nitrogen, chlorophyll a (Chl.a), nitrite, nitrate, ammonia, water temperature, DO, and pH were monitored almost monthly. The multivariate statistical technique (cluster analysis) and the nonparametric method (Kruskal?CWallis Test and Spearman??s rank correlation) were applied to evaluate the spatiotemporal variations of water quality data sets.

Results and discussion

According to the Chinese environmental quality standards for surface water (GB3838-2002), the water quality in the river section investigated can attain to the III water standards except total nitrogen. Further analysis indicated that there were no significant spatial differences in these parameters of water quality, but the sampling date had a significant effect. The temporal variation of water quality can be related to the discharge of Gezhouba Dam and moreover be affected by the reservoir regulation. During the discharge, the discharge increased the concentration of total phosphorus and then decreased the N:P ratio, which helps to the occurrence of algae blooms. The high consternation of phosphorus and the low N:P ratio show that the water body can be in the process of eutrophication during the discharge of Gezhouba Dam. In fact, Chl.a had begun to rise in the same period.