O objetivo desta Tese foi avaliar o papel da macrófitas submersas em relação à qualidade da água, interações com o fitoplâncton e ciclagem biogeoquímica na Lagoa Mangueira, um grande lago raso subtropical, no sul do Brasil. Para alcançar estes objetivos, este trabalho conta com uma série de abordagens, como: levantamentos de campo, etapas experimentais e uso de modelos ecológicos para avaliar a influência de macrófitas sobre a dinâmica do ecossistema de estudo, cujas águas são intensamente exploradas para suprir a cultura de arroz em sua área de entorno. Ao longo de seus 200km de perímetro litorâneo, a Lagoa apresenta maciços estandes submersos de vegetação. A análise de qualidade da água e estrutura da comunidade fitoplanctônica ao longo de um gradiente de vegetação submersa, partindo da zona litorânea para a zona pelágica (sem vegetação), revelou menor disponilibidade de nutrientes como orto-fosfato (PO4) e menor concentração de clorofila-a (Clo-a), na área com vegetação submersa. Na zona pelágica, os maiores valores de Clo-a foram corroborados pela maior biomassa fitoplanctônica, sendo representada principalmente por espécies de cianobactérias. Tais evidências sugerem o efeito antagônico entre macrófitas e fitoplâncton, como a competição por nutrientes e alelopatia. Em laboratório, estes mecanismos puderam ser comprovados em experimentos de coexistência realizados em microcosmos com 4 espécies de macrófitas nativas e uma cepa da cianobactéria Microcystis aeruginosa. Os testes envolveram níveis distintos de intensidade luminosa e concentração de PO4 visando determinar limiares para a ocorrência de alelopatia. As espécies Cabomba caroliniana e Myriophyllum spicatum se demonstraram potencialmente alelopáticas enquanto que as espécies Ceratophyllum demersum e Egeria densa apresentaram elevada capacidade de absorção de PO4 (±0,35 mg.g-1d-1) reduzindo rapidamente a concentração deste nutriente a valores abaixo de 0,05 mg.L-1. Outra abordadem experimental foi conduzida para parametrizar a cinética da liberação de nutrientes e carbono de 5 espécies de macrófitas durante o processo de decomposição. Com o auxílio de modelos ecológicos, foi simulado o crescimento de macrófitas submersas em lagos subtropicais e temperados. Isto foi realizado visando avaliar a possibilidade de aumento da resilência do estado de dominância por macrófitas em lagos de baixa latidude devido ao crescimento contínuo da vegetação, ao contrário de lagos temperados, onde as plantas morrem sazonalmente em função do inverno rigoroso. Além disso, foram simulados cenários considerando a possibilidade de colapso da vegetação submersa na Lagoa Mangueira em função de intensa tomada da água da Lagoa para irrigação. Com base na modelagem, foi possível estimar limiares de eutrofização para a proliferação do fitoplâncton. Em suma, os resultados comprovaram os mecanismos de retroalimentação positiva de macrófitas submersas sobre a qualidade da água e importância de suas funções ecológicas para o estado trófico e gestão da Lagoa Mangueira. Além disso, este conjunto de informações constitui uma base teórico-prática para o manejo, restauração e conservação de lagos rasos subtropicais e tropicais. / The aim of this Thesis was to evaluate the role of the submerged macrophytes with respect to water quality and, interactions with phytoplankton and nutrient cycling in the large shallow subtropical Lake Mangueira, southern Brazil. To achieve these goals, this work counts with approaches in situ, in laboratory and aplication of ecological modelling to verifify the influence of the submerged vegetation over the dynamics of the ecosystem, whose water is intensively explored to irrigate rice crops around its surrounding area. Over the 200km of the lake littoral perimeter, several submerged macrophyte beds are established. The analysis of water quality and phytoplankton structure along a macrophyte-pelagic gradient revealed lower concentration of orto-phosphate (PO4) and chlorophyll-a (Chlo-a) in the vegetated area. At the pelagic zone, the higher Chlo-a values were corroborated by the higher biomass of phytoplankton, which was mostly composed by cyanobacteria species. Such evidences suggest the antagonistic relantionship between macrophytes and phytoplankton as nutrient competition and allelopathy. Experiments of coexistance, in microcosms, with 4 native submerged macrophytes and a toxic strain of the cyanobacteria Microcystis aeruginosa proved the occurrence of these mechanisms. The experiments included different levels of light intensity and orto-phosphate concentration (PO4) in the medium aiming to identify thresholds in which allelopathy is likely to occur. The macrophytes Cabomba caroliniana and Myriophyllum spicatum showed allelopathic potential while the species Ceratophyllum demersum and Egeria densa showed a high capacity for PO4 absorption (±0.35 mg.g-1d-1), being able to reduce this nutrient to lower levels than 0.05 mg.L-1. Another experimental approach was carried out to parameterize the leaching of nutrients and carbon from 5 macrophytes under decaying process. Moreover, ecological modelling was utilized to simulate the growth of submerged macrophytes in subtropical and temperate lakes. This was done aiming to evaluate the possibility of resilience enhancement of the clear water state in lakes of low latitude because the plants can grow continuously, in contrast with temperate lakes, where they die seasonally due to rigorous winter. In addition, simulation of scenarios considering the collapse of the vegetation in Lake Mangueira because of water uptake for rice crops were carried out in oder to provide elements for the ecosystem management. Through this approach, it was possible to forecast possible eutrophication thresholds for phytoplankton blomming. In conclusion, the results proved the the postive feed-back mechanisms exerted by the submerged macrophytes on the water quality and the importance of their ecological functions to the trophic state of Lake Mangueira. In addition, such information serve as theoretical and practical basis for the management, restoration and conservation of subtropical and tropical shallow lakes.

As comunidades mudam no tempo e espaço em função de pressões decorrentes da estrutura do habitat e disponibilidade de recursos. O entendimento das relações ecológicas e interações das comunidades são essenciais para o manejo com objetivo de melhorar a qualidade da água através de interferências na cadeia trófica aquática e na dinâmica do ecossistema através de modelagem ecológica. O presente estudo foi desenvolvido em dois sistemas límicos subtropicais no extremo sul do Brasil: banhados temporários (‘campos de cultivo de arroz’) e um grande lago raso, lagoa Mangueira. O objetivo do trabalho nos banhados temporários constituiu-se em avaliar a dinâmica das comunidades planctônicas e íctica durante o desenvolvimento desses ecossitemas (um ciclo produtivo de cultivo de arroz). Nossos resultados evidenciaram um claro gradiente temporal direcionado pela disponibilidade de nutrientes no banhado temporário. Entretanto, as variáveis limnológicas não apresentaram nenhuma tendência espacial entre as estações amostrais. Através de regressão linear verificou-se correlação positiva entre clorofila a, nutrientes, biomassa zooplanctônica e, em especial, biomassa de copépodos. Por outro lado, biomassa de peixes e, particularmente, peixes planctívoros foram inversamente relacionados à concentração de clorofila a. Relações significativas entre o DOC com nutrientes, biomassa de plâncton e peixes foram igualmente identificadas ao longo do ciclo produtivo do arroz. Na lagoa Mangueira, sistema raso (zmed 3m), de 90 km de comprimento, o objetivo foi avaliar a distribuição espacial e temporal de plâncton e peixes em função da presença da macrófita emergente Zizaniopsis bonariensis. Além disso, foi verificada a existência de um gradiente longitudinal na lagoa e a estrutura da teia trófica do sistema. Análise de componentes principais e análise de redundância evidenciaram a presença de gradientes espacial (Norte/Sul) e temporal (sazonal) durante o estudo. Análise de similaridade (ANOSIM) aplicada às variáveis ambientais evidenciou diferenças significativas entre os extremos da lagoa (Norte e Sul). Transparência Secchi, DOC e clorofila a foram significativamente diferentes entre os pontos amostrais do Norte e Sul. Através de ANOVA verificou-se que os efeitos temporais sazonais são mais intensos no Norte da lagoa Mangueira. Com relação à estrutura da comunidade na lagoa Mangueira, a biomassa do bacterioplâncton, clorofila a, biomassa zooplanctônica e captura de peixes foram diferentes sazonalmente após a extração do efeito da estrutura de habitat, enquanto que no Sul apenas a clorofila a apresentou variação sazonal significativa. A estrutura de habitat (junto à Z. bonariensis e em água aberta) induziu diferenças significativas na concentração de clorofila a tanto no Norte como no Sul da lagoa Mangueira, após a extração dos efeitos decorrentes da sazonalidade. A captura de peixes também foi influenciada pela estrutura de habitat no Norte, após a extração do efeito sazonal. Análise de similaridade (ANOSIM) aplicada à comunidade de peixes também demonstrou diferenças significativas entre o Norte e o Sul da lagoa Mangueira, embora diferenças entre as áreas vegetadas e águas abertas não tenham sido verificadas. Biomassa dos peixes, número de capturas e riqueza específica foram diferentes entre os pontos amostrais. Baseado nas razões de δ13C and δ15N identificou-se a estrutura trófica da lagoa, bem como a posição trófica de espécies de peixes e as fontes de carbono do sitema. Análise de isótopos estáveis de nitrogênio permitiu a identificação de dois níveis tróficos de peixes na lagoa Mangueira. Macrófitas emergentes e perifíton foram identificadas como importantes fontes de carbono que sustentam a estrutura trófica do sistema. Análise de grupamento a partir de dados de δ13C e δ15N e de conteúdo estomacal identificou um arranjo perfeitamente filogenético entre as espécies de peixes analisadas, refletindo que, em sentido amplo, nichos alimentares são compartilhados por espécies taxonomicamente relacionadas. A dinâmica trófica da espécie de peixe dominante na lagoa, Oligosarcus jenynsii foi também analisada. Foram identificadas mudanças sazonais e ontogenéticas na dinâmica alimentar da espécie, evidenciando a grande plasticidade trófica associada com uma estratégia oportunista, característica de espécies carnívoras generalistas. As informações obtidas neste estudo permitiram identificar grande heterogeneidade espacial e claro gradiente longitudinal na lagoa Mangueira, tanto de fatores bióticos quanto abióticos, com reflexos na distribuição e abundância de plâncton e peixes. De posse destas informações foi possível alcançar um entedimento sobre a estrutura atual do sistema, bem como os direcionadores da sua dinâmica. A abordagem direcionada neste trabalho sobre o entendimento da estrutura atual de um lago raso subtropical possibilita futuros estudos na área da modelagem ecológica. A dinâmica das comunidades abordadas neste estudo vem subsidiar a parametrização de um modelo ecológico, com capacidade de estabelecer prognósticos, tendo como contorno, estressores naturais e antrópicos. / Biological communities change in time and space following driving pressures from differences in habitat structure and resource availability. Understanding the ecological role and interactions within aquatic community is essential for any management action trying to improve water quality by interferences in lake food web, ecosystem dynamics and modeling. The present study was carried out in two freshwater systems in Southern Brazil: an irrigated rice field and in a large shallow system, Mangueira Lake. The goal of this study in temporary wetlands was to evaluate the plankton and fish dynamics during a productive cycle. Our results evidenced a temporal gradient by nutrients availability in the temporary wetland studied. However, the limnological variables did not display any horizontal pattern among sampling stations. Linear regression showed a positive relationship between chlorophyll a and nutrients, zooplankton biomass and copepod biomass. In contrast, fish biomass and planktivorous fish biomass were inversely related to chlorophyll a. Statistically significant relationships between DOC with nutrients, plankton and fish biomass were also identified during the rice production cycle. In Mangueira Lake, a shallow system (zmed 3m) and 90 km long, the goal was to evaluate the spatial and temporal distribution of plankton and fish biomass as a function of the presence of the emergent macrophytes Zizaniopsis bonariensis. We also analyzed the existence of longitudinal gradient in lake and the food web structure in system. The PCA and RDA analyses showed the temporal (seasonal) and spatial (North/South) gradient during the study. Analysis of similarity (ANOSIM) applied to environmental variables showed significant differences between sampling sites (North and South). Secchi transparency, DOC and chlorophyll a were significantly different in North and South sampling sites. ANOVA results showed that season effects are stronger in the Northern sampling site. Concerning the community structure in the Mangueira Lake, bacterioplankton biomass, chlorophyll a, zooplankton biomass and fish captures were different seasonally after extracting the habitat structure effect, while in the Southern sampling site only chlorophyll a presented a seasonal significant variation. Habitat structure (by Z. bonariensis stands and open water samples) induced significant differences in chlorophyll a both in North and South samples after extracting seasonal effect. Fish captures do also responded to habitat structure in the North, after extracting the season effect. Analysis of similarity (ANOSIM) applied to fish community also showed significant differences between North and South, although no significant differences between vegetated and open water zones was observed. Fish biomass, number of captures, and richness were different between sampling sites. Based on the δ13C and δ15N ratios and analysis of stomach content of fish species, we provide also a description of food web structure, trophic positions of fish species and primary producers of system. Analysis of nitrogen isotope ratios yielded two fish trophic levels in Mangueira Lake. Emergent macrophytes and periphyton were important carbon source that sustain the food web structure of the system. Cluster analysis of δ13C and δ15N values and stomach content yielded a perfect phylogenetic arrangement of species. This result reflects that major feeding niches are shared by taxonomically related species. The feeding dynamics of the dominant fish species, Oligosarcus jenynsii was analysed by using analyses of stomach contents and stable isotopes signature. Seasonal and ontogenetic change in the feeding biology of O. jenynsii was identified, showing the high feeding plasticity, in addition to an opportunistic strategy of this generalist carnivore species. This study allows identifying a large spatial heterogeneity and clear longitudinal gradient both in biotic and abiotic factors, reflecting fish and plankton distribution and abundance. The evaluated parameters are intended to feed a mathematical model for the Mangueira Lake, looking for predictable scenarios from natural and anthropogenic stressors.

Change in hydrossedimentological system of the lower course of the São Francisco river, by controlling the flow, has changed the characteristics of the aquatic ecosystem as well as the suspended sediment load. The objective of this study was to evaluate the suspended sediment load in the São Francisco river Chanel, and settlement of aquatic macrophytes species in a section of the right bank under different soil bioengineering techniques. The study area comprises a margin stretch of the São Francisco River in its lower course, located in the Amparo de São Francisco Municipality, Sergipe. The botanical material collection followed conventional methods, being held from April 2014 to September 2015, in a total of four sampling time, two in the rainy season and two in the dry season. Suspended sediments load were evaluated through 03 years (2013, 2014 and 2015) in 20, 40 and 60% of the channel depth in five different transects oriented by the presence or absence of erosion control techniques, as identified: 1- Vegetated Slope; 2- Vegetated Riprap; 3- Eroded Slope; 4- Cribwall; and 5- Vetiver grass Line, considering three of them (2, 4 and 5) with soil bioengineering techniques. In the collected material 66 species was identified in 23 families, showing the its richness and diversity in a small stretch of the São Francisco River. In assessing the macrophytes population, the wet period showed greater species richness, and among soil bioengineering techniques, the Cribwall presented the highest number of individuals. The sediment load was statistically different for the three evaluated years, and the highest values were presented in 2013, when the river had the highest discharge. Among the treatments, the Eroded Slope presented at a depth of 20% the lowest contribution of suspended sediment and the Vegetated Riprap the lower sediment load rate compared to other techniques. The strong presence of aquatic macrophytes in the river contributed to the protection of the slopes toe by dissipating the energy of the ebb and flow of the waves. A progressive decrease in total sediment suspended load was found throughout evaluated period, due not only to reduced river discharge, but also the protection provided by adopted erosion control techniques. / O regime hidrossedimentológico do baixo curso do rio São Francisco, por meio do controle da vazão, tem alterado as características do ecossistema aquático, bem como a produção e transporte de sedimentos em suspenção. O objetivo desse estudo foi avaliar a produção de sedimentos em suspensão no canal do Rio São Francisco, e povoamento de macrófitas aquáticas em um trecho da margem direita submetida a diferentes técnicas de Engenharia Natural. A área de estudo compreendeu um trecho de talude da margem direita do Rio São Francisco no seu baixo curso, localizada no Município de Amparo do São Francisco, Sergipe. A coleta do material botânico seguiu os métodos convencionais, tendo sido realizada no período de abril de 2014 a setembro de 2015, totalizando quatro amostragens, duas no período chuvoso e duas no período seco. Sedimentos em suspensão foram avaliados no período de 03 anos (2013, 2014 e 2015) a 20, 40 e 60% de profundidade do canal, em cinco diferentes transectos, orientados pela presença ou ausência de técnicas de controle de erosão, assim identificados: 1- Talude Vegetado; 2- Enrocamento Vegetado; 3- Talude Erodido; 4- Parede Krainer; e 5- Cordão de Vetiver, sendo que em três trechos da margem (2, 4 e 5) foram implantadas técnicas de Engenharia Natural. Do material coletado foram identificadas 66 espécies, distribuídas em 23 famílias, mostrando sua riqueza e diversidade em um pequeno trecho do Rio São Francisco. Na avaliação do povoamento de macrófitas, o período do inverno apresentou maior riqueza dessas espécies e a Parede Krainer foi o tratamento que apresentou maior número de indivíduos. O aporte de Sedimentos em Suspensão diferiu estatisticamente para os três anos de coleta, com destaque para o ano de 2013, quando o rio apresentou a maior vazão. Entre os tratamentos, o Talude Erodido apresentou na profundidade de 20% o menor aporte de sedimentos em suspensão e, o Enrocamento Vegetado os menores valores quando comparada às outras técnicas. A forte presença de macrófitas aquáticas, na margem do rio, contribuiu para a proteção da base dos taludes por dissipar a energia do fluxo e refluxo das ondas. Constatou-se um decréscimo progressivo nos sedimentos em suspensão na comparação do período avaliado, devido não somente à redução da vazão do rio, como também à proteção conferida pelas técnicas adotadas de controle de erosão.

Made available in DSpace on 2017-07-10T18:08:17Z (GMT). No. of bitstreams: 1 Ana Paula de Oliveira.pdf: 11086894 bytes, checksum: 428ff3baaac89e47e47de37f81ccdfc5 (MD5) Previous issue date: 2012-02-16 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior / The main objective of this study was to verify the influence of the macronutrient phosphorus in the lead bioaccumulation process, using the living aquatic macrophyte Eicchornia crassipes. In addition, the removal capacity of lead ions and some nutrients such as P, K, Ca and Fe, by the E. crassipes was verified, obtaining also information on how these are distributed within two compartiments of the plant: roots and leaves. For this, a set of metal removal/bioaccumulation experiments, in batch mode, was performed for different concentration ranges of metal and nutrients in hydroponic conditions. Several 5 L growing solutions based on the set of macro and micronutrients specified by Clark as being adequate to cultivate plants in hydroponic conditions were prepared, containing a mixture of lead (0, 5, 10, 15 and 20 mg L-1) and phosphorus (once, twice, four and eight times of 3,2 mg L-1) concentrations among other constant essential nutrient ones. At a greenhouse and using several 8 L containers approximately 80 g of living and healthy E. crassipes aquatic macrophytes were growded in each type of 5 L growing solution, restoring its former hydroponic and metal concentration condition at each two days time interval as well as monitoring the plant weight, the aqueous medium temperature and the pH values. After predefined collection time (2, 4, 8, 16 and 32 d), samples of growing solutions and plants were separated and measured some physico-chemical parameters and then stored in plastic bags for posterior analysis. Analysis of initial and residual concentrations of lead and nutrients available in the metal-doping Clark growing solutions as well as bioaccumalated metal concentrations in the dried plant samples (roots and leaves) were performed by SR-TXRF technique, except for phosphorus concentrations which were determined by a colorimetric method. According to the TXRF results, the adsorption/accumulation of lead ions in roots and leaves of the Eichhornia crassipes was slightly favoured by the presence of high phosphorus concentrations in the metal-doping Clark growing solutions. It can be noticed that the lead removal by roots is a quit process, occurring basically a high lead adsorption in the first days, whereas the lead bioaccumulation in leaves is a low process due to ocurr a low transportation rate of nutrients for aerial parts of the aquatic plant. Beside this, high lead concentrations in metal-doping Clark solutions have negatively influenced the accumulation of phosphorous in leaves as well as a low phosphorous adsorption in roots, suggesting that there is a detrimental effect on sorption and transport of phosphourous to the leaves by the presence of lead ions. On the other hand, it was observed a high systematically increasing of potassium concentration in roots whereas a reduction on potassium ones is occurring in leaves due to the presence of lead ions, suggesting that there is a migration process of potassium from leaves to roots. It could be occurring by different possible processes such as potassium complexation in roots or occupation of lead sites by potassium during the transportation of lead to aerial parts, reducing the potassium concentration in leaves. Further nutrient and metal adsorption/bioaccumulation experiments are necessary to understand better the translocation and accumulation process of nutrients such as phosphorus and potassium when lead ions are being adsorbed and transported within the internal structure of the aquatic plant. / O objetivo principal do trabalho foi verificar a influência do macronutriente fósforo no processo de bioacumulação do chumbo, utilizando a macrófita aquática Eicchornia crassipes viva. Além disso, verificou-se a capacidade de remoção de íons chumbo e alguns nutrientes como o P, K, Ca e Fe, pela E. crassipes, obtendo-se também informações de como estes são distribuídos dentro de dois compartimentos da planta: raízes e folhas. Para tanto, foi realizado um conjunto de experimentos de remoção/bioacumulação de metal, em batelada, para diferentes faixas de concentração de metal e nutrientes em condições hidropônicas. Foram preparadas várias soluções de cultivo com base no conjunto de macro e micronutrientes especificado por Clark como sendo adequado para cultivar plantas em condições de hidroponia, contendo uma mistura de chumbo (0, 5, 10, 15 e 20 mg L-1) e fósforo (uma, duas, quatro e oito vezes 3,2 mg L-1) entre outros nutrientes fundamentais em concentrações constantes. Em uma estufa e usando vários recipientes com capacidade de 8 L, aproximadamente 80 g da macrófita aquática E. crassipes viva e saudável, foram colocadas a crescer em 5 L de cada tipo de solução de crescimento, restaurando-se as condições iniciais hidropônicas e de concentração de metal a cada dois dias, bem como monitorando o peso da planta, a temperatura do meio aquoso e os valores de pH. Após o tempo de cultivo pré-definido (2, 4, 8, 16 e 32 d), amostras de solução de cultivo e planta foram separadas, medidos alguns parâmetros físico-químicos e armazenadas em sacos plásticos para posterior análise. Análises das concentrações inicial e residual de chumbo e de nutrientes disponíveis na solução de cultivo de Clark contendo metal, assim como concentrações de metal bioacumuladas nas amostras de planta seca (raízes e folhas), foram realizadas pela técnica SR-TXRF, exceto para as concentrações de fósforo, que foram determinadas por um método colorimétrico. De acordo com os resultados da TXRF, a adsorção/acumulação de íons de chumbo nas raízes e folhas da Eichhornia crassipes foi levemente favorecida pela presença de altas concentrações de fósforo nas soluções de cultivo de Clark contendo metal. Pode-se notar que a remoção de chumbo pelas raízes é um processo rápido, ocorrendo basicamente uma alta adsorção de chumbo nos primeiros dias, enquanto que a bioacumulação de chumbo nas folhas é um processo lento devido à ocorrência de uma baixa taxa de transporte de nutrientes para a parte aérea da planta aquática. Além disso, altas concentrações de chumbo na solução de Clark podem ter influenciado negativamente o acúmulo de fósforo nas folhas, bem como uma baixa adsorção de fósforo nas raízes, sugerindo que há uma relação prejudicial na adsorção de fósforo e seu transporte para as folhas pela presença de íons de chumbo. Por outro lado, observou-se um aumento sistemático na concentração de potássio nas raízes e redução na quantidade de potássio nas folhas devido à presença de íons de chumbo, sugerindo que há um processo de migração de potássio das folhas para as raízes. Isto pode ocorrer por diferentes processos, tais como a complexação de potássio nas raízes ou a ocupação de sítios de chumbo pelo potássio durante o transporte de metal para a parte aérea, reduzindo a concentração de potássio nas folhas. No entanto, são necessários mais experimentos de adsorção/bioacumulação de nutrientes e metal para melhor entendimento do processo de translocação e acumulação de nutrientes, como fósforo e potássio, quando íons de chumbo estão sendo adsorvidos e transportados dentro da estrutura interna da planta aquática.

Made available in DSpace on 2017-07-10T18:13:31Z (GMT). No. of bitstreams: 1 Cristina Viana Sales.pdf: 1033711 bytes, checksum: 66526bf26f60f186b7ec4f4ca78473c3 (MD5) Previous issue date: 2011-08-23 / The accumulation and deposition of high concentrations of organic matter cause the eutrophication of aquatic environments, and a sustainable alternative to the removal of these compounds is phytoremediation. This study evaluated the potential of two floating aquatic macrophytes, Eichhornia crassipes and Pistia stratiotes in the treatment of brewery wastewater. The treatment system consisted of eight experimental units, and the experimental design 2 treatments and 4 pseudoréplicas, each treatment was coupled to a mechanical filter in closed circulation system. We analyzed the parameters temperature, electrical conductivity, pH, dissolved oxygen, turbidity, COD, total phosphorus, nitrogen, nitrite and nitrate, and measure the biomass of macrophytes, the experiment lasted 21 days, with collections made weekly. Statistical analysis showed no statistical difference between treatments for the reduction of nutrients, however the two species E. crassipes and P. statiotes been proven effective in removing these nutrients. As for weight gain, E. crassipes had a higher growth compared to P. stratiotes. The use of phytoremediation is recommended for the treatment of brewery effluents due to low cost, easy maintenance and efficiency of aquatic macrophytes in removing nutrients that cause eutrophication of aquatic environments. / O acúmulo e deposição de elevadas concentrações de matéria orgânica provocam a eutrofização de ambientes aquáticos, e uma alternativa sustentável para a retirada destes compostos é a fitorremediação. Neste estudo avaliou-se o potencial de duas espécies de macrófitas aquáticas flutuantes, Eichhornia crassipes e Pistia stratiotes, no tratamento de efluente de cervejaria. O sistema de tratamento foi constituído de 8 unidades experimentais, sendo o delineamento experimental de 2 tratamentos com 4 pseudoréplicas, cada tratamento foi acoplado a um filtro mecânico, em sistema de circulação fechado. Foram analisados as variáveis temperatura, condutividade elétrica, pH, oxigênio dissolvido, turbidez, DQO, fósforo total, nitrogênio, nitrito e nitrato, e medida a biomassa das macrófitas aquáticas, o experimento teve duração de 21 dias, sendo as coletas feitas semanalmente. O estudo estatístico mostrou que não houve diferença estatística entre os tratamentos quanto à redução de nutrientes, no entanto as duas espécies E. crassipes e P. statiotes se mostraram eficazes na remoção desses nutrientes. Quanto ao ganho de peso, E. crassipes teve maior crescimento comparado a P. stratiotes. O uso da fitorremediação é recomendável para o tratamento de efluentes de cervejaria devido ao baixo custo, a fácil manutenção e a eficiência das macrófitas aquáticas na remoção de nutrientes que causam a eutrofização de ambientes aquáticos.

Abstract Freshwater ecosystems are severely threatened by a variety of anthropogenic stressors. In order to keep track with at least part of the changes, it is important to efficiently assess and monitor freshwater biological diversity. Biological assessment programs are developed to detect human-induced changes in the ecological state of aquatic systems. These programs typically rely on the assumption that environmental conditions are the sole drivers of biological communities occupying a site and, thus, these local communities would correctly inform about environmental conditions. Recently, this background principle of current bioassessment methods has faced some criticism, stemming from the idea that community structuring is a more complex process than just a mere result of local environmental conditions. In this thesis, I studied the natural and anthropogenic drivers of freshwater biodiversity. I was particularly interested if the various biodiversity metrics studied showed any spatial patterns and if so, for which reasons these patterns might occur. To obtain a comprehensive picture of spatial patterns in biodiversity, I studied multiple spatial contexts, biological groups and indices. I found that environmental conditions were not the only drivers of freshwater biodiversity. Instead, different spatial patterns, likely stemming from dispersal processes, were surprisingly powerful drivers of aquatic communities and index values derived from them. The spatial context (i.e. spatial extent and connectivity) of the aquatic study systems likely played a major role in structuring biodiversity. I also found that the distinct biological groups and indices studied were partly related to different predictor variables. The findings of this thesis are of importance to the development of new bioassessment methods. The results of this thesis also suggest that the spatial context of the study setting should be acknowledged when interpreting results based on current bioassessment methods. / Tiivistelmä Makeanveden ekosysteemit ovat hyvin alttiita ihmistoiminnalle. Ekosysteemissä mahdollisesti tapahtuvien muutosten havaitseminen vaatii tehokkaita vesistöjen ekologisen tilan ja luonnon monimuotoisuuden arviointi- ja seurantamenetelmiä. Näiden menetelmien toimintaperiaatteen yleisenä tausta-ajatuksena on, että biologiset yhteisöt määräytyvät paikallisten ympäristöolojen mukaan. Tietyn paikan yhteisön oletetaan siis heijastavan kyseisen paikan ympäristön tilaa. Viime aikoina tausta-ajatus paikallisten ympäristöolojen merkityksestä ainoana eliöyhteisöjä muovaavana tekijänä on kuitenkin kohdannut kritiikkiä. Kriitikot painottavat, että biologisten yhteisöjen rakenteeseen vaikuttavat monet muutkin asiat kuin paikalliset ympäristöolosuhteet ja niissä tapahtuvat ihmisperäiset muutokset. Väitöskirjassani tutkin sisävesien luonnon monimuotoisuuteen vaikuttavia tekijöitä. Olin erityisen kiinnostunut siitä, näkyykö tutkituissa biologisissa parametreissa maantieteellisessä tilassa ilmeneviä spatiaalisia säännönmukaisuuksia. Saadakseni mahdollisimman laaja-alaisen käsityksen luonnon monimuotoisuudessa esiintyvistä spatiaalisista säännönmukaisuuksista, tutkin useaa spatiaalista kontekstia, eliöryhmää ja indeksiä. Tutkimuksessa selvisi, että paikalliset ympäristöolosuhteet eivät ole ainoita luonnon monimuotoisuuteen vaikuttavia tekijöitä. Erilaiset spatiaaliset säännönmukaisuudet, todennäköisesti eliöiden levittäytymiseen liittyvien seikkojen aiheuttamina, olivat yllättävän yleisiä makeiden vesien eliöyhteisöjen rakenteessa ja niihin perustuvien indeksien arvoissa. Tutkimussysteemien spatiaalinen konteksti (alueen laajuus ja paikkojen väliset spatiaaliset suhteet) selvästi vaikutti luonnon monimuotoisuutta kuvastavien indeksien arvojen vaihteluun. Lisäksi selvisi, että eri eliöryhmät ja indeksit olivat useimmiten liitoksissa hyvin erilaisiin selittäviin muuttujiin, osoittaen, että nämä mittarit kuvastavat eri asioita. Väitöskirjassa esitetyt havainnot on tärkeää huomioida vesistöjen ekologisen tilan ja luonnon monimuotoisuuden arviointi- ja seurantamenetelmiä kehitettäessä. Spatiaalisen kontekstin merkitys olisi hyvä huomioida myös nykyisten arviointi- ja seurantamenetelmien tuottamien tulosten tulkinnassa.

Climate change affects lake ecosystems in many ways by direct and indirect temperature impacts on hydrophysical structure, hydrology, chemical cycles and on biological interactions. The identification of these climate signals can be complicated and superimposed by other environmental changes, such as land use changes. The aim of this thesis was to seperate temperature effects from effects of management and other environmental influences and to understand the underlying complex processes causing significant changes of ecosystem states. This understanding is important for decisions of lake and reservoir managers to counteract unfavorable consequences of climate change. For the recent study, long-term data of meteorological, hydrophysical and biological variables (phytoplankton, crustacean zooplankton, fish) of the German drinking water reservoir Saidenbach were analysed. Based on this long-term data set, strong indicators for climate induced changes have been identified. In particular, increasing water temperatures since 1975, earlier break up of ice covers and an altered hydrophysical structure could be detected. Thereby, stratification stability increased and turbulent mixing decreased in summer. The water of the reservoir warmed more than the tributaries resulting in a trend to deeper entrainment of the inflows. As further indicators of climate change, an increased annual biomass of phytoplankton and species shifts in the phytoplankton community in spring and summer had been observed. During the spring mass development, the diatom Aulacoseira subarctica became dominant in recent years with warm winters and early ice-out. Its unusual spatial pattern with occurrences in aphotic depths could be explained by easier resuspension compared to other diatoms. By being resuspended first and establishing a high inoculum, A. subarctica profits from an earlier ice-out and earlier full circulation. In spite of a reduced nutrient loading to the epilimnion, in summer, the diatom Fragilaria crotonensis was displaced increasingly by cyanobacteria. This species shift could be explained well by the hydrophysical regime shift. Although, the annual total phytoplankton biomass increased since 1990, the crustacean zooplankton in Saidenbach reservoir did not seem to profit from improved food resources. To the contrary, Daphnia abundances reduced tremendously. We could show that the influcence of fish stocks were underestimated. The stocked silvercarp may have contributed up to 70 % of the total zooplanktivorous fish biomass which had a temperature and density dependent effect. The faster growth of Daphnia at higher temperatures could not compensate for the more actively grazing fish when stock of zooplankitvorous fish was too high. Still, temperature was identified as the most important factor that explained 29 % of the zooplankton phenology, while the second most important predictors were zooplanktivorous fish biomass and nutrient loading, explaining 18 % of the variance. The importance of submerged macrophytes in shallow lakes is well investigated. To increase also the understanding of their impact and their role during climate change on water quality in deep lakes, a model for stratified lakes that includes submerged macrophytes was developed. The simulations showed that macrophyte effects were mainly positive for water quality and macrophytes in deep lakes were able to potentially reduce summer phytoplankton, especially cyanobacteria by 50 % in 11 m deep and still by 15 % in 100 m deep oligotrophic lakes. Nutrient competition with phytoplankton contributed most to this macrophyte effect. In conclusion, for deep lake restoration the re-establishment of submerged macrophytes might be as important as for shallow lakes. The full lake model includes hydrophysical and ecological submodules and thus will allow further comprehensive climate simulations and the evaluation of the effectivity of adaptive strategies and scenarios for deep lakes and reservoirs. / Der Klimawandel beeinflusst Seeökosysteme vielfältig durch direkte und indirekte Temperatureffekte auf die hydrophysikalische Struktur, die Hydrologie, chemische Kreisläufe und biologische Interaktionen. Die Identifikation von Klimasignalen kann durch Landnutzungs- und weitere Umweltveränderungen überlagert werden. Ziel dieser Arbeit war es, Temperatureffekte von Effekten zu unterscheiden, die durch Gewässermanagement oder anderen Umweltveränderungen verursacht werden. Weiterhin sollten komplexe Prozesse verstanden werden, die zu signifikanten Veränderungen in Seeökosystemen führen. Dieses Verständnis ist für Talsperren- und Gewässermanager von besonderer Bedeutung, um ungewünschten Folgen des Klimawandels entgegenwirken zu können. Für die Studie wurden Langzeitdaten für meteorologische, hydrophysikalische und biologische Variablen (Phytoplankton, Crustaceen-Zooplankton, Fischbesatz) der Talsperre Saidenbach ausgewertet. Mehrere Indikatoren für die Auswirkungen des Klimawandels konnten basierend auf diesen Daten identifiziert werden. Diese gehören insbesondere eine Erhöhung der Wassertemperatur seit 1975, zeitigere Eisaufbrüche und eine veränderte Schichtungsstruktur. Dabei wurde im Sommer die Schichtungsstabilität höher und die Intensität der Durchmischung geringer. Das Wasser in der Talsperre erwärmte sich stärker als die Zuflüsse, wodurch diese sich zunehmend tiefer und unterhalb der Thermokline einschichten. Eine zunehmende jährliche Phytoplanktonbiomasse und Artenwechsel innerhalb der Planktongemeinschaft sind weitere Indikatoren für Klimafolgen. Die Kieselalge Aulacoseira subarctica erlangte in Jahren mit warmen Wintern und zeitigen Eisaufbrüchen eine Dominanz während der Frühjahrsentwicklung. Das ungewöhnliche Auftreten dieser Art in aphotischen Tiefen konnte durch eine leichtere Resuspension im Vergleich zu anderen Kieselalgen erklärt werden. Durch zeitige Resuspension gleich nach Eisaufbruch kann A. subarctica ein hohes Inokulum etablieren. Trotz reduzierter Nährstoffzufuhr ins Epilimnion wurde im Sommer die Kieselalge Fragilaria crotonensis vermehrt durch Cyanobakterien verdrängt, was jedoch gut mit den Änderungen der hydrophysikalischen Struktur erklärt werden kann. Obwohl seit 1990 insgesamt mehr Phytoplankton zur Verfügung steht konnte das Crustaceen- Zooplankton in der Talsperre Saidenbach nicht von diesen verbesserten Nahrungsbedingungen profitieren. Die Daphnia-Abundanzen waren seit 1990 stark verringert. Es konnte gezeigt werden, dass der Einfluss des Fischbesatzes unterschätzt wurde und die künstlich ins System eingebrachten Silberkarpfen zeitweise bis zu 70% der zooplanktivoren Fischbiomasse ausgemacht haben. Zoo- planktivore Fische haben einen temperatur- und dichteabhängigen Effekt auf das Zooplankton. Das schnellere Populationswachstum von Daphnia kann bei hohem Besatz mit zooplanktivoren Fischen nicht die erhöhte Fraßaktivität der Fische ausgleichen. Dennoch konnte Temperatur als der wichtigste Einflussfaktor auf die Phänologie des Zooplanktons identifiziert werden, gefolgt von zooplanktivorem Fisch und Nährstoffzufuhr. Die Wichtigkeit von submersen Makrophyten in Flachseen ist gut untersucht. Um den Einfluss von Makropyhten auf die Wasserqualität während des Klimawandels auch in tiefen Seen abschätzen zu können, wurde ein komplexes Seemodell entwickelt. Die Simulationen zeigen, dass sich Makrophyten hauptsächlich positiv auf die Wassergüte auswirken und zur Reduktion von Phytoplankton, insbesondere von Cyanobakterien im Sommer, beitragen. In einem 11 m tiefen See betrug die Reduktion 50 %, in 100 m tiefen oligotrophen Seen immer noch 15 %. Die Konkurrenz um Nährstoffe mit dem Phytoplankton war dabei die ursächliche Makrophyten-Plankton-Interaktion. Submerse Makrophyten könnten für die Restaurierung von tiefen Seen folglich genauso wichtig sein, wie für Flachseen. Das komplette Seemodell enthält hydrophysikalische und ökologische Module und ermöglicht damit weitere umfassende Simulationen zur Untersuchung der Auswirkungen des Klimawandels und zur Evaluation von Adaptionsstrategien für Seen und Talsperren.

Cette thèse a été codirigée par le Dr. Florent Chazarenc / Les marais filtrants artificiels sont communément utilisés pour le traitement des eaux usées municipales, mais ils peuvent aussi traiter une large gamme d’effluents à l’aide de différents types de marais filtrant et ce sous une variété de climats. Les plantes jouent un rôle central dans l’épuration des eaux, mais on peut se demander si ce rôle est le même sous toutes les conditions et ce pour les différentes espèces de plantes. Dans le cadre de cette étude, j’ai évalué l’influence de la présence ainsi que de l’espèce de plantes selon des conditions extrêmement différentes : 1) traitement de rejet de serre hydroponique par un marais filtrant à flux horizontal en conditions hivernales, 2) traitement des boues par un marais à flux vertical en conditions estivales. / Constructed wetlands (CWs) are commonly used to treat municipal wastewater, but they can also handle a wide range of effluents by using different types of CWs and under a variety of climatic conditions. Plants play a central role in CWs, but it is still unknown if the presence of plants or the choice of the species have the same influence under different conditions. In this study, I evaluated the influence of the presence and the species of plants under two very different conditions: 1) treatment of hydroponic wastewater by a horizontal flow CW in winter conditions, 2) sludge treatment by a vertical flow CW in summer conditions.

Les proliférations nuisibles de la cyanobactérie filamenteuse benthique Lyngbya wollei qui forme des tapis déposés sur les sédiments ont augmenté en fréquence au cours des 30 dernières années dans les rivières, lacs et sources de l'Amérique du Nord. Lyngbya wollei produit des neurotoxines et des composés organiques volatils (géosmin, 2-méthylisobornéol) qui ont des répercussions sur la santé publique de même que des impacts d'ordre socioéconomiques. Cette cyanobactérie est considérée comme un habitat et une source de nourriture de piètre qualité pour les invertébrés en raison de sa gaine robuste et de sa production de toxines. Les proliférations de L. wollei ont été observées pour la première fois en 2005 dans le fleuve Saint-Laurent (SLR; Québec, Canada). Nous avons jugé important de déterminer sa distribution sur un tronçon de 250 km afin d'élaborer des modèles prédictifs de sa présence et biomasse en se basant sur les caractéristiques chimiques et physiques de l'eau. Lyngbya wollei était généralement observé en aval de la confluence de petits tributaires qui irriguent des terres agricoles. L’écoulement d’eaux enrichies à travers la végétation submergée se traduisait par une diminution de la concentration d’azote inorganique dissous (DIN), alors que les concentrations de carbone organique dissous (DOC) et de phosphore total dissous (TDP) demeuraient élevées, produisant un faible rapport DIN :TDP. Selon nos modèles, DOC (effet positif), TP (effet négatif) et DIN :TDP (effet négatif) sont les variables les plus importantes pour expliquer la répartition de cette cyanobactérie. La probabilité que L. wollei soit présent dans le SLR a été prédite avec exactitude dans 72 % à 92 % des cas pour un ensemble de données indépendantes. Nous avons ensuite examiné si les conditions hydrodynamiques, c'est-à-dire le courant généré par les vagues et l'écoulement du fleuve, contrôlent les variations spatiales et temporelles de biomasse de L. wollei dans un grand système fluvial. Nous avons mesuré la biomasse de L. wollei ainsi que les variables chimiques, physiques et météorologiques durant trois ans à 10 sites le long d'un gradient d'exposition au courant et au vent dans un grand (148 km2) lac fluvial du SLR. L'exposition aux vagues et la vitesse du courant contrôlaient les variations de biomasses spatiales et temporelles. La biomasse augmentait de mai à novembre et persistait durant l'hiver. Les variations interannuelles étaient contrôlées par l'écoulement de la rivière (niveau d'eau) avec la crue printanière qui délogeait les tapis de l'année précédente. Les baisses du niveau d'eau et l'augmentation de l'intensité des tempêtes anticipées par les scénarios de changements climatiques pourraient accroître la superficie colonisée par L. wollei de même que son accumulation sur les berges. Par la suite, nous avons évalué l'importance relative de L. wollei par rapport aux macrophytes et aux épiphytes. Nous avons examiné l'influence structurante de l'échelle spatiale sur les variables environnementales et la biomasse de ces producteurs primaires (PP) benthiques. Nous avons testé si leur biomasse reflétait la nature des agrégats d'habitat basées sur l'écogéomorphologie ou plutôt le continuum fluvial. Pour répondre à ces deux questions, nous avons utilisé un design à 3 échelles spatiales dans le SLR: 1) le long d'un tronçon de 250 km, 2) entre les lacs fluviaux localisés dans ce tronçon, 3) à l'intérieur de chaque lac fluvial. Les facteurs environnementaux (conductivité et TP) et la structure spatiale expliquent 59% de la variation de biomasse des trois PP benthiques. Spécifiquement, les variations de biomasses étaient le mieux expliquées par la conductivité (+) pour les macrophytes, par le ratio DIN:TDP (+) et le coefficient d'extinction lumineuse (+) pour les épiphytes et par le DOC (+) et le NH4+ (-) pour L. wollei. La structure spatiale à l'intérieur des lacs fluviaux était la plus importante composante spatiale pour tous les PP benthiques, suggérant que les effets locaux tels que l'enrichissement par les tributaire plutôt que les gradients amont-aval déterminent la biomasse de PP benthiques. Donc, la dynamique des agrégats d'habitat représente un cadre général adéquat pour expliquer les variations spatiales et la grande variété de conditions environnementales supportant des organismes aquatiques dans les grands fleuves. Enfin, nous avons étudié le rôle écologique des tapis de L. wollei dans les écosystèmes aquatiques, en particulier comme source de nourriture et refuge pour l'amphipode Gammarus fasciatus. Nous avons offert aux amphipodes un choix entre des tapis de L. wollei et soit des chlorophytes filamenteuses ou un tapis artificiel de laine acrylique lors d'expériences en laboratoire. Nous avons aussi reconstitué la diète in situ des amphipodes à l'aide du mixing model (d13C et δ15N). Gammarus fasciatus choisissait le substrat offrant le meilleur refuge face à la lumière (Acrylique>Lyngbya=Rhizoclonium>Spirogyra). La présence de saxitoxines, la composition élémentaire des tissus et l'abondance des épiphytes n'ont eu aucun effet sur le choix de substrat. Lyngbya wollei et ses épiphytes constituaient 36 et 24 % de l'alimentation in situ de G. fasciatus alors que les chlorophytes, les macrophytes et les épiphytes associées représentaient une fraction moins importante de son alimentation. Les tapis de cyanobactéries benthiques devraient être considérés comme un bon refuge et une source de nourriture pour les petits invertébrés omnivores tels que les amphipodes. / Harmful proliferations of the filamentous cyanobacterium L. wollei forming conspicuous benthic mats on the bottom sediment have been reported with increasing frequency in the last 30 years in rivers, lakes, and springs in North America. It is a known producer of neurotoxins and volatile organic compounds (geosmin, 2-methylisoborneol) thus exerting socioeconomic and public health impacts. Lyngbya wollei is also considered a poor nutritional source for invertebrates because of its robust sheath and toxin production. Proliferation of L. wollei in St. Lawrence River (SLR; Quebec, Canada) was first noticed in 2005. We deemed important to determine its distribution over a 250 km stretch of the SLR to elaborate predictive models of its presence and biomass based on chemical and physical characteristics. Lyngbya wollei was generally found downstream of the inflow tributaries draining farmlands. As enriched waters flowed slowly through submerged vegetation, dissolved inorganic nitrogen (DIN) concentration dropped but dissolved organic carbon (DOC) and total dissolved phosphorus (TDP) remained high, leading to a low DIN:TDP ratio. Models identified DOC (positive effect), TP (negative effect), and DIN:TDP (negative effect) as the most important variables explaining L. wollei distribution. The risk of L. wollei occurrence in the SLR was correctly forecasted in 72%-92% of all cases with an independent data set. We then examined if hydrodynamic conditions, namely currents generated by waves and river flow, control spatial and temporal variations of L. wollei biomass in a large river system. We measured L. wollei biomass together with meteorological, physical, and chemical variables over three years at 10 sites along a gradient of exposure to current and wind in a large (148 km2) fluvial lake of SLR. Wave exposure and current velocity controlled spatial and temporal biomass variations. Biomass increased from May to November and persisted during winter. Interannual variations were primarily controlled by river flow (water level) with spring discharge dislodging mats from the previous year. As anticipated under climate change scenarios, drops in water level and rising storm intensity may lead to an increase in the areas colonized by L. wollei, together with more frequent episodes of mat disruption and beach fouling. Additionally, we evaluated the relative importance of L. wollei with respect to macrophytes and epiphytes. We assessed the influence of the spatial scale in structuring environmental variables and biomass of these benthic primary producers (PP). We also test to which extent their biomass reflected the nature of patches based on ecogeomorphology or the river continuum. To address these two questions, we used a nested design at 3 spatial scales within the SLR: 1) along a 250-km-long upstream-downstream river stretch, 2) among three fluvial lakes located within that river stretch and 3) within each fluvial lake. Environmental factors (conductivity and TP) and spatial structure together explained 59% of the variability in biomass of all three benthic PP. Spatial variability of biomass was best explained by conductivity (+) for macrophytes, DIN:TDP ratio (+) and water extinction coefficient (+) for epiphytes and DOC (+) and NH4+ (-) for L. wollei mats. Within-lake structure was the most important spatial component for all benthic PP, suggesting that local effects, such as enrichment by the inflow of tributaries, rather than upstream-downstream gradients, determined the biomass and composition of benthic PP. Therefore patch dynamics represents a general framework which adequately covers the spatial variability and wide variety of environmental conditions experienced by aquatic organisms found in large rivers. Finally, we investigated the ecological role of L. wollei mats in aquatic ecosystems, especially as a food source and shelter for the amphipod Gammarus fasciatus. We offered amphipods a choice between mats of L. wollei and either chlorophytes or an artificial mat made of acrylic wool in laboratory experiment. Moreover, we reconstructed in situ amphipod diet using mixing model (δ13C and δ15N). Gammarus fasciatus selected the substratum offering the best light refuge (Acrylic > Lyngbya = Rhizoclonium > Spirogyra). Presence of saxitoxins, tissue elemental composition and epiphyte abundance had no significant effect on substratum choice. Lyngbya wollei and its epiphytes constituted 36 and 24% of the in situ diet of G. fasciatus whereas chlorophytes, macrophytes and associated epiphytes represented a less important fraction of its diet. Benthic cyanobacterial mats should be considered a good shelter and food source for small omnivorous invertebrates such as amphipods.

An experimental study was carried out to evaluate the performance of pilot scale constructed wetlands for the treatment of domestic wastewater in Addis Ababa, Ethiopia. Three parallel sets of constructed wetlands; consisting of one Horizontal Flow (HF), one Vertical Flow (VF) and one hybrid of HF and VFconstructed in series were built in Addis Ababa. The wetland systems had identical wetland fill media and macrophytes but with different wastewater flow types. The total surface area of the wetland systems was 72 m2 /24 m2 for each/ and designed to treat 3.15 m3 of domestic wastewater per day. Triplicate grab samples were taken from the influent and effluents every 15 days for one year and analyzed within 24 hours. Temperature, pH, DO and EC were measured onsite and the nutrient content of macrophytes was determined twice during the monitoring period. During the first 12 months monitoring period, the average removal efficiencies of the HFCW, VFCW and hybrid CW were: BOD (89.1%, 92.2% and 93.4%), COD (80.6%, 82.1% and 84.0%), TSS (89.1, 83.8% and 84.7%), NH4 + (58.6%, 66.2% and 65.4%), NO3 - (64.0%, 71.5% and 73.5%), TN (49.1%, 54.9% and 58.7%), PO4 3- (45.4%, 50.3% and 48.4%), TP (58.0%, 51.7% and 54.4%) and FC (98.6%, 96.6% and 96.5%), respectively. The hybrid system showed relatively higher removal efficiencies for most pollutants. Again, the wetland systems showed relatively higher percent reduction during the dry seasons /from Dec - May/. The areal removal rate constants of BOD5, TN, PO4 3- and TP were higher than the literature values while the values of COD and TSS were lower compared to the literature values. Concerning the nutrient content of the wetland plant, the average TN contents of the below-ground and above-ground plant part were 1.56% and 2.27% for the HFCW, 1.75% and 2.74% for the VFCW and 1.80% and 2.63% for the hybrid system, respectively. Meanwhile, the average TP contents of the belowground and above-ground plant part were 0.139% and 0.064% for the HFCW, 0.167% and 0.067% for the VFCW and 0.115% and 0.065% for the hybrid systems, respectively. In general, the results showed that properly designed constructed wetland systems could be used as effective wastewater treatment method in Ethiopia. / Environmental Sciences / Ph. D. (Environmental Sciences)