人工湖水生态系统构建方法研究

基于湖泊生态恢复的理论及工程实践经验,提出了新建人工湖水生态系统构建的一般方法。通过水生植物、水生动物的合理选种、水生植物的空间和时间配置以及水生动物食物网的合理构建,使各种群在整体上互补共生,形成结构合理、具有一定抵抗能力与自我恢复能力的水生态系统。以某新建人工湖为例,基于所提出的方法构建了其水生态系统。研究成果对人工湖水生态系统的构建和运行管理具有指导意义。     

湖泊水生植物对重金属元素吸收积累的初步研究

水生生物是生态系统的重要组成部分,它对物质循环、元素迁移及污水净化等起着重要作用。本文就湖泊水生植物对重金属元素的吸收、积累作用的初步研究作一介绍。一、湖泊水生植物对重金属元素的吸收积累特性     

湖泊富营养化调查和监测的若干问题

富营养化是一种营养物质过多积蓄而引起的水质污染现象,近代湖沼学也把这一现象当作湖泊演化过程中渐近衰亡的一种标志。 湖泊富营养化的主要危害表现为以下几个方面: 1.由于低级水生植物和浮游植物的大量生长繁殖.给工业用水和生活用水的处理造成困难,增加处理成本。 2.浮游植物的大量繁殖,在水温较高的季节常可引起“水华”现象,并使水     

浮萍植物在污水处理中的应用研究进展

浮萍科植物是漂浮生长在水流相对平缓的湖泊河湾水面上植物类群,整个植株完全退化为一个呈圆形或椭圆形的叶状体,主要是通过根或叶状体从水中吸收所需的氮磷等各种营养物质.浮萍科植物的氮磷含量和生长速率高并可以耐受多种污水条件,因此这个类群是污水处理生态工程中重要的水生植物类群.以浮萍为主的污水处理系统已得到较多的研究和应用,这类系统最大特点是浮萍的生长可以大量吸收污水中的氮磷,从而具有较高的氮磷去除率,同时生成的生物量可多种方式利用.因此利用这类系统对污水进行氮磷的处理与转化,并将生成的浮萍生物量适当地资源化利用是未来的发展方向.     

潜水丁坝在湖滨带生态恢复中的应用

为保护和稳固湖滨带,在太湖梅梁湾进行生态恢复研究,并成功地实施了示范工程.沿湖滨带共构筑14道潜水丁坝,每道长23～28 m,坝间距为40～80 m,坝上种植芦苇和菰.构筑的潜水丁坝能经受住太湖常见大风袭击和湖流淘蚀,芦苇和菰等长势良好,湖滨原有芦苇带在一定水深范围内每年向湖延伸2～5 cm,坝上其他水生植物和底栖动物螺蛳等自然繁衍.潜水丁坝所起作用为利用自然力改变岸边流场,使泥沙在湖滨带预定沉积区内沉积,减缓岸边侵蚀和降低沉积物再悬浮,从而为湖滨带水生植物生长创造良好的生境条件.研究发现,在微风条件下,潜水丁坝群能有效拦截麇集于岸边的蓝绿藻,并在湖滨带进行消化降解.研究提出的构筑潜水丁坝并种植水生植物的方案为湖滨带生态恢复提供了一种新的探索途径.     

水体富营养化和水花兰藻

国内外有很多风景优美的湖泊由于没有及时加强管理,以致湖泊中藻类大量滋生,使水体变混浊,有的甚至腥味四溢。这是因为这些湖泊中产生大量水花(或称为湖靛)而造成的。其结果不仅破坏了景色,还会影响鱼类生长,甚至对人畜也有危害。     

基于容量迭加法的乌梁素海承载力计算

湖泊承载力的计算一般建立在水环境容量的基础上,而水环境容量的确定涉及污染物降解系数。由于乌梁素海的挺水植物、浮水植物和沉水植物呈相间分布,时有共生,分布面积也各有差异,并伴生着多种藻类,因此该湖的降解系数的确定存在一定的难度。容量迭加的方法避开了降解系数确定的问题,其物理意义明确,容易操作。应用容量迭加的方法对乌梁素海2006年5～10月的COD、TN和TP的环境容量进行了计算。从结果可以看出,水生植物群落分布和水生植物量决定了湖区对污染物的降解能力,直接影响其水环境容量。在此基础上,确定了乌梁素海5～10月的水质承载力CCPZ,将当地的社会经济发展状况与湖泊水环境承载力结合起来。计算求得CCPZ=1.115>1.0(当CCPZ=1.0时,湖泊实际承载的社会发展与允许值平衡),说明集水流域中的社会经济发展水平超过了湖泊所允许的水环境承载力,需要调整产业结构,从污染源控制污染物的排放,降低对湖区水环境的压力,实现社会、经济和环境协调可持续发展。     

大型水生植物在水污染治理中的应用研究进展

大型水生植物在水污染治理中可以发挥多种作用。通过自身的生长代谢可以大量吸收氮、磷等水体中的营养物质 ,而其中一些种类还可以富集不同类型的重金属或吸收降解某些有机污染物 ;通过促进微生物的生长代谢 ,可以使水中大部分可生物降解有机物 (BOD)降解 ;通过抑制低等藻类的生长 ,控制富营养化的表现形式等。根据不同的生活型特点 ,利用大型水生植物进行污水处理和水体修复的方式也多种多样 ,主要包括 :以漂浮植物为主的塘系统和以挺水植物为主的人工湿地系统等。本文从生态功能发挥的角度探讨了植物对污染物降解的机理 ,并对以大型水生植物为核心的各种污水处理系统的研究进展与现状进行了综述 ,指出了利用大型水生植物进行水污染治理的研究与应用中存在的问题和发展方向     

大型水生植物在水污染治理中的应用研究进展

大型水生植物在水污染治理中可以发挥多种作用。通过自身的生长代谢可以大量吸收氨、磷等水体中的营养物质，而其中一些种类还可以富集不同类型的重金属或吸收降解某些有机污染物；通过促进微生物的生长代谢，可以使水中大部分可生物降解有机物（BOD）降解；通过抑制低等藻类的生长，控制富营养化的表现形式等。根据不同的生活型特点，利用大型水生植物进行污水处理和水体修复的方式也多种多样，主要包括：以漂浮植物为主的塘系统和以挺水植物为主的人工湿地系统等。本文从生态功能发挥的角度探讨了植物对污染物降解的机理，并对以大型水生植物为核心的各种污水处理系统的研究进展与现状进行了综述，指出了利用大型水生植物进行水污染治理的研究与应用中存在的问题和发展方向。     

浮萍植物在污水处理中的应用研究进展

浮萍科植物是漂浮生长在水流相对平缓的湖泊河湾水面上植物类群，整个植株完全退化为一个呈圆形或椭圆形的叶状体，主要是通过根或叶状体从水中吸收所需的氮磷等各种营养物质。浮萍科植物的氮磷含量和生长速率高并可以耐受多种污水条件，因此这个类群是污水处理生态工程中重要的水生植物类群。以浮萍为主的污水处理系统已得到较多的研究和应用，这类系统最大特点是浮萍的生长可以大量吸收污水中的氮磷，从而具有较高的氮磷去除率，同时生成的生物量可多种方式利用。因此利用这类系统对污水进行氮磷的处理与转化，并将生成的浮萍生物量适当地资源化利用是未来的发展方向。     

The effects of lake acidification on aquatic macrophytes--a review

Acidification of lakes results in a number of chemical, physical and biological changes. This review initially outlines the major floristic changes that occur in acidifying and limed lakes. The different types of evidence (historical comparisons, inter-lake comparisons and palaeoecological studies) are considered. These studies emphasise the replacement of calcicole species and others such as the isoetids with Juncus bulbosus and Sphagnun spp. in acidifying lakes. The review then discusses the way in which the various alterations in lake conditions affect the physiology of the macrophytes, particularly with changes in the availability of carbon, a change from nitrate to ammonium as a nitrogen source and the effects of an alteration in the Lake light climate. The population biology, community ecology and ecosystem functioning of macrophytes are discussed, especially where competitive processes may seem more important in determining community change than physiological processes. Particular consideration is paid to the types of evidence of floristic change that are useful and the importance of undertaking experimental studies at the correct scale to determine which factors may be causally related to the floristic evidence.     

Four decades of research on the Swedish large lakes Mälaren, Hjälmaren, Vättern and Vänern: the significance of monitoring and remedial measures for a sustainable society

The large lakes of Sweden, M?laren, Hj?lmaren, V?ttern and V?nern, have been subjected to water-quality monitoring for almost four decades. Physicochemical variables, plankton and benthic invertebrates have been regularly assessed. Hydrological and sediment conditions, macrophytes, fish, primary production, bacteria and attached algae have been periodically investigated. The human impact, including industrial activities, was reflected in excessive amounts of organic matter, nutrients, metals and persistent organic compounds. From the late 1960s all municipal sewage works in the catchments of the lakes were upgraded to the highest technical standard, including chemical precipitation of phosphorus, and phosphorus discharge from the sewage works was thereby reduced by 90-95%. In addition, industries were obliged to restrict discharge of harmful substances. The reactions of the lakes to the remedial measures are discussed as well as the value of various indicators. The studies were instrumental in designing a national lake monitoring program. Additionally, results from large lake monitoring have contributed to the establishment of national water-quality criteria including, physical, chemical, and biological indicators.     

Macrophyte development and habitat characteristics in Sweden's large lakes

The four largest Swedish lakes, V?nern, V?ttern, Hj?lmaren, and M?laren, were surveyed by means of aerial IR-color photography in the 1970s. Along small slope gradients in all lakes the emergent communities extended to a width of hundreds of meters, while the extent on steeper slopes was a few meters. Because of the fractionate shape, L. M?laren has a very long shoreline, which promotes vegetation growth in the transition zone between land and water. Sheltered conditions are numerous and water lilies and other floating leaved and freely floating plants are abundant. Emergent as well as submerged macrophytes grow vigorously in the northernmost part of the oligotrophic lake V?ttern. In L. V?nern exposed shores pre-dominate, but sheltered bays and archipelagos are overgrown with reeds. In the shallow lake Hj?lmaren monospecific stands of Phragmites australis are dominant. Recurrent surveys of L. M?laren and L. V?nern in the 1990s showed changes that could be connected to the watertable fluctuations, which have been stabilized since the first investigation. Reeds and water lilies expanded in sheltered parts of the lakes, while the distribution of reed stands growing at their deep limit decreased.     

Effects of taxonomy,sediment, and water column on C:N:P stoichiometry of submerged macrophytes in Yangtze floodplain shallow lakes,China

Carbon (C), nitrogen (N) and phosphorus (P) are the three most important essential elements limiting growth of primary producers. Submerged macrophytes generally absorb nutrients from sediments by root uptake. However, the C:N:P stoichiometric signatures of plant tissue are affected by many additional factors such as taxonomy, nutrient availability, and light availability. We first revealed the relative importance of taxonomy, sediment, and water column on plant C:N:P stoichiometry using variance partitioning based on partial redundancy analyses. Results showed that taxonomy was the most important factor in determining C:N:P stoichiometry, then the water column and finally the sediment. In this study, a significant positive relationship was found between community C concentration and macrophyte community biomass, indicating that the local low C availability in macrophytes probably was the main reason why submerged macrophytes declined in Yangtze floodplain shallow lakes. Based on our study, it is suggested that submerged macrophytes in Yangtze floodplain shallow lakes are primarily limited by low light levels rather than nutrient availability.

     

The change of gaseous carbon fluxes following the switch of dominant producers from macrophytes to algae in a shallow subtropical lake of China

Successions of lake ecosystems from clear-water, macrophyte-rich conditions into turbid states with abundant phytoplankton have taken place in many shallow lakes in China. However, little is know about the change of carbon fluxes in lakes during such processes. We conducted a case study in Lake Biandantang to investigate the change of carbon fluxes during such a regime shift. Dissolved aquatic carbon and gaseous carbon (methane (CH₄) and carbon dioxide (CO₂)) across air–water interface in three sites with different vegetation covers and compositions were studied and compared. CH₄ emissions from three sites were 0.62±0.36, 0.70±0.36, and 1.31±0.57 mg m⁻² h⁻¹, respectively. Correlation analysis showed that macrophytes, rather than phytoplankton, directly positively affected CH₄ emission. CO₂ fluxes of three sites in Lake Biandantang were significantly different, and the average values were 77.8±20.4, 52.2±14.1 and 3.6±26.8 mg m⁻² h⁻¹, respectively. There were an evident trend that the larger macrophyte biomass, the lower CO₂ emissions. Correlation analysis showed that in different sites, dominant plant controlled CO₂ flux across air–water interface. In a year cycle, the percents of gaseous carbon release from lake accounting for net primary production were significantly different (from 39.3% to 2.8%), indicating that with the decline of macrophytes and regime shift, the lake will be a larger carbon source to the atmosphere.     

Evaluation of aquatic environmental fate of 2,4,6-trichlorophenol with a mathematical model

A mathematical model, Simplified Approach for Fate Evaluation of Chemicals in Aquatic Systems (SAFECAS), was applied to evaluate fate of 2,4,6-trichlorophenol(TCP) in three types of aquatic environments; a river, an oligotrophic lake, and an eutrophic lake.Since phenols are dissociative substances, equilibrium constants and rate constants for transfer and transformation processes were measured or estimated as a function of pH.Results suggest that most of TCP is distributed to the water phase in aquatic environments, and is almost removed by the advective outflow in the river and by the photodegradation in lakes.     

大型水生植物对骆马湖氮、磷元素的影响

对骆马湖有草区和无草区水体和沉积物中氮、磷元素含量分析,结果表明:无草区水体中总氮、总磷含量高于有草区;有草区表层沉积物总氮含量随时间变化明显,而无草区表层沉积物总氮含量随时间的变化很小;有草区与无草区表层沉积物中总磷含量的时间变化并无明显差异;有草区表层沉积物总氮含量基本上均高于无草区,而有草区表层沉积物总磷含量均要低于无草区。骆马湖有草区与无草区采样点沉积物碱性磷酸酶活性大小在58.41～315.07 mg/(kg.h)范围内变化,有草区的碱性磷酸酶的活性普遍低于无草区的碱性磷酸酶活性。在湖泊中种植大型水生植物确实可以减少水体污染,达到净化水质的目的。     

Metal accumulation by submerged macrophytes in eutrophic lakes at the watershed scale

Metal concentrations (Al, Ba, Ca, K, Li, Mg, Na, Se, Sr and Ti) in submerged macrophytes and corresponding water and sediments were studied in 24 eutrophic lakes along the middle and lower reaches of the Yangtze River (China). Results showed that these eutrophic lakes have high metal concentrations in both water and sediments because of human activities. Average concentrations of Al and Na in tissues of submerged macrophytes were very high in sampled eutrophic lakes. By comparison, Ceratophyllum demersum and Najas marina accumulated more metals (e.g. Ba, Ca, K, Mg, Na, Sr and Ti). Strong positive correlations were found between metal concentrations in tissues of submerged macrophytes, probably because of co-accumulation of metals. The concentrations of Li, Mg, Na and Sr in tissues of submerged macrophytes significantly correlated with their corresponding water values, but not sediment values.     

Nutrient dynamics and the eutrophication of shallow lakes Kasumigaura (Japan), Donghu (PR China), and Okeechobee (USA)

We compared the nutrient dynamics of three lakes that have been heavily influenced by point and non-point source pollution and other human activities. The lakes, located in Japan (Lake Kasumigaura), People's Republic of China (Lake Donghu), and the USA (Lake Okeechobee), all are relatively large (> 30 km2), very shallow (< 4 m mean depth), and eutrophic. In all three lakes we found strong interactions among the sediments, water column, and human activities. Important processes affecting nutrient dynamics included nitrogen fixation, light limitation due to resuspended sediments, and intense grazing on algae by cultured fish. As a result of these complex interactions, simple empirical models developed to predict in-lake responses of total phosphorus and algal biomass to external nutrient loads must be used with caution. While published models may provide 'good' results, in terms of model output matching actual data, this may not be due to accurate representation of lake processes in the models. The variable nutrient dynamics that we observed among the three study lakes appears to be typical for shallow lake systems. This indicates that a greater reliance on lake-specific research may be required for effective management, and a lesser role of inter-lake generalization than is possible for deeper, dimictic lake systems. Furthermore, accurate predictions of management impacts in shallow eutrophic lakes may require the use of relatively complex deterministic modeling tools.     

Reproductive status, blood chemistry, gill histology and growth of perch (Perca fluviatilis) in three acidic lakes

Perch (Perca fluviatilis L.) were sampled soon after spawning in three small acidic lakes (pH 4.3-6.1, Al(lab) 5-106 microg litre(-1), Ca2+ 0.01-0.08 mmol litre(-1)) and in one circumneutral lake (pH 5.9-6.4, Al(lab) 4-12 microg litre(-1), Ca2+ 0.06-0.07 mmol litre(-1)) in southern Finland. Due to the delayed spawning of perch in the acidic lakes, sampling in those lakes was performed later than in the reference lake. In spite of that, the gonadosomatic index (GSI) of males in all the acidic lakes was significantly greater than in the reference lake. Of the two lakes with similar low water pH, the effects on reproduction were more prominent in the lake with higher water Al content. The plasma Ca2+ concentrations of females in the acidic lakes were significantly smaller than in the females of the reference lake. The low female:male plasma Ca2+ ratio (1.0-1.32) depicted delay of spawning. Stress in perch in acidic water was also seen in elevated blood haematocrit values, especially in females. On the other hand, a low plasma Cl- level, a common response to acidic water in salmonids, was not detected in perch in the most acidic lakes. The amount of Al accumulated in the gill epithelium was highest in the most acidified lake with high Al concentration, but was also pronounced in a lake with low pH and low Al concentration.