Dams fragment streams and rivers, with >14,000 in New England alone, and have the potential to significantly alter the physical, chemical, and biological characteristics of lotic systems. For example, dams can alter temperature and dissolved oxygen (DO) regimes, which can, in turn, affect species distributions, whole system metabolism, and nutrient processing rates. Moreover, changes in temperature signal life history cues (e.g., emergence, egg-hatching, migration) for many species of aquatic organisms, and present another avenue for dams to alter biotic communities. Despite the prevalence of small dams in the landscape and their potential significant impacts on temperature and DO, dams have not been well-studied and published impacts vary widely across sites. Given the variation in impact, I sought to quantify the impacts of small dams to stream temperature and DO, and to determine the drivers of inter- and intra-site variation in response. To accomplish this, I deployed 160 continuous temperature data loggers at 30 small, surface-release dams in Massachusetts. The majority of sites (61%) had higher temperatures downstream of the dam compared to upstream and most (85%) experienced decreasing temperatures with increasing distance downstream of the dam, such that the warmest temperatures were located closest to the dam. At approximately half of the temperature sites, flow had a homogenizing effect on temperatures throughout the study reach, whereby impacts were more pronounced (e.g., more warming, faster decay rates) under periods of low flow than under high flow conditions. Magnitude of warming varied greatly among sites, and this variation was explained best by landscape position and reservoir volume, with dams in smaller watersheds and with larger reservoir volumes experiencing greater warming magnitudes. Forest cover, dam height, and the presence of an auxiliary spillway best predicted the downstream temperature decay rate, with temperatures cooling fastest downstream of shorter dams in forested basins that did not have an auxiliary spillway. I used continuous DO loggers upstream, within the impoundment, and downstream of 12 dams to identify dam impacts to DO. Most sites experienced lower DO (66%) within the impoundment compared to upstream; however, 58% of the sites showed no difference in diel ranges between these reaches. The effect of dams on downstream DO was mixed, with increases, no change, and decreases relative to upstream condition; however, the majority of sites (58%) experienced a suppressed downstream diel range relative to upstream. The upstream slope, basin size, and dam height drove the impoundment response, such that dams with steeper upstream reach slopes, located in smaller basins, and with shorter dam heights experienced the greatest decreases in impoundment DO relative to upstream. Differences between downstream and upstream DO were best explained by upstream slope and impoundment volume, whereby sites with steeper upstream reaches and larger volumes of water within the impoundment experienced the largest decreases in downstream DO when compared to upstream reaches. These results may help managers prioritize dam removal at sites where a dam is having larger and more negative (e.g., elevated temperatures, decreased DO) impacts, and therefore where the greatest benefits should occur following restoration.

Agricultural production and human activities in a watershed can expose the watershed to environmental degradation, pollution problems, and a decrease in water quality if resources and activities within a watershed are not managed carefully. In order to best utilize limited resources and maximize the results with respect to time and money spent on nonpoint source (NPS) pollution control and prevention, the environmental risk must be identified so that areas with a higher quantified environmental risk can be targeted. The objectives of the research presented in this master thesis were to develop a procedure to quantify environmental risk of nutrient loadings to surface waters and to demonstrate the procedure on a watershed. A procedure to quantify environmental risk of nutrient loadings to surface waters was developed. The risk is identified as the probability of occurrence of a nonpoint source (NPS) pollution event caused by a runoff event multiplied by the consequences to a biological or chemical endpoint. The procedure utilizes the NPS pollution model ANSWERS-2000 to generate upland pollutant loadings to receiving waters. The pollutant loading impact on stream water quality is estimated using the stream module of Hydrologic Simulation Program FORTRAN (HSPF). The risk is calculated as the product of probability of occurrence of a NPS event and consequences of that event. The risk quantification procedure was applied to a watershed in Virginia. Total phosphorus (TP) loadings were evaluated with respect to resultant in-stream dissolved oxygen (DO) concentration. The TP loadings were estimated in ANSWERS-2000 then the consequences were estimated in HSPF. The results indicated that risk was higher for the smaller, more frequent storms indicating that these smaller, more frequent loading events represent a greater risk to the in-stream water quality and ecosystem than larger events. While the probability of occurrence of lower TP loading was higher because they were caused by smaller, more frequent storms, the consequences were less for the same events. The developed procedure can provide watershed stakeholders and managers with a useful tool to quantify the environmental risk a watershed is exposed to as a result of different land management and development scenarios. The scenarios can then be compared to identify a risk level that is considered acceptable. The procedure can also be used by policymakers to set a cap on the risk a certain activity can expose a watershed to. / Master of Science

No description available.

The effects of oxygenation and aeration on water quality, rainbow trout (Oncorhynchus mykiss) production, and economics were compared at the Wytheville State Fish Hatchery (WSFH) for 270 days. Mean dissolved oxygen (DO) concentrations and delta DO were significantly higher (P < 0.001) in the oxygenated raceways (9.5 and 2.75 mg/L, respectively) compared to aerated raceways (7.4 and 0.57 mg/L). Total settleable solids loads were significantly greater (P < 0.001) in aerated raceways (10.3 g/L/day) than in oxygenated raceways (8.8 g/L/day). Dissolved nitrogen (%), total gas pressure, and other water quality parameters (CO2, nitrite nitrogen, alkalinity, pH, and TAN) did not differ significantly between the treatments (P > 0.05). Raceway trout production (kg/day), trout growth rates (grams), feed conversion rate (FCR), and fish survival were not significantly different between treatments (P > 0.05). Blood hematocrit (Hct) and percent visceral mass were significantly elevated (P < 0.001) in oxygenated raceways compared to aerated raceways at 46 and 14.4% and 44 and 13%, respectively. Carrying capacity estimates derived from fish loading trials were significantly different (P < 0.001) at 3,355 and 2,217 kg/raceway in oxygenated and aerated raceways, respectively. Estimates of carrying capacity calculated using a fish loading (Ld) equation were also significantly different (P < 0.001) at 1,530 and 990 kg for oxygenated and aerated raceways, respectively. Oxygen injection increased the cost of production by $0.20/kg, however, net present value analysis (NPV) of oxygenated and aerated raceways over 5 years at a 10% discount rate yielded estimates of $50,666.51 and $32,742.15, respectively. Oxygen injection is an effective means of increasing DO concentrations, reducing effluent solids loading, and increasing raceway carrying capacity. / Master of Science

Conselho Nacional de Desenvolvimento Científico e Tecnológico / Metals environment aquatic contamination has been a growing problem with serious consequences to life of different species over time, even after interrupted their emission into the environment. Among relevance metals, manganese (Mn) has shown importance to be related to several activities such as oil exploration, coal deposits extraction, fertilizer use in agriculture, among others. In living organisms, Mn is an essential trace element for a number of vital functions, and involves energy regulation by blood clotting. On the other hand, high concentrations of Mn can cause irreversible damage to living organisms primarily affecting central nervous system (CNS). Thus, waterborne Mn toxicity can switch from aquatic species, while metal bioaccumulation in marine fish or freshwater has been found around 0.2 to 19.0 mg/kg dry weight. In this study, silver catfish (Rhamdia quelen) were exposed to different Mn concentrations (4.2; 8.4 e 16.2 mg/L), under two different dissolved oxygen levels, normoxia (7.48 ± 0.28) and hypoxia (3.88 ± 0.41) for 15 days. At the end of protocol, Mn bioaccumulation as well parameters of oxidative stress and mitochondrial viability were evaluated in different tissues. In hypoxic conditions, the highest Mn concentration (16.2 mg/L) showed the lowest silver catfish kidney and brain lipoperoxidation (LPO) levels, while brain reduced glutathione (GSH) levels were increased in lower Mn concentration (4.2 mg/L) and kidney catalase activity was reduced in the same metal concentration, in relation to normoxia. Lowest Mn concentration (4.2 mg/L) in hypoxia showed higher gills mitochondrial viability, compared to normoxia. Hematocrit of silver catfish exposed to two highest Mn concentration (8.4 and 16.2 mg/L) was reduced in normoxia conditions while under hypoxia, these values were similar to control. Plasma except, Mn bioaccumulation in liver, kidney and gills were higher in normoxia than hypoxia. From these results is possible to suggest that hypoxia stimulates the development of adaptive mechanisms and/or hormesis in silver catfish exposed to Mn, mainly because the lower metal bioaccumulation occurred in this oxygen level. Contributing with this, under hypoxia, oxidative damage indicators were lower than those observed in normoxia, which were accompanied by changes in antioxidant system represented by GSH and catalase. In conclusion, our results show in the first time that silver catfish exposed to Mn contamination is able to show a better survival under hypoxia. These findings indicate need for continuing studies in search of molecular mechanisms involved in the adaptation and or hormesis processes, which were suggested here. / A contaminação do meio aquático por metais tem sido um problema crescente para à vida de diferentes espécies, mesmo depois de interrompida sua emissão no ambiente. Entre os metais de relevância, o manganês (Mn) apresenta importância por estar relacionado a uma série de atividades tais como exploração de petróleo, extrativismo em jazidas de carvão mineral, utilização de fertilizantes na agricultura, entre outros. Nos organismos vivos, o Mn constitui um oligoelemento essencial para uma série de funções vitais, e envolve desde a regulação da energia até coagulação sangüínea. Por outro lado, quando em concentrações elevadas, o Mn pode causar danos irreversíveis aos organismos afetando principalmente o sistema nervoso central (SNC). A toxicidade do Mn dissolvido na água pode variar entre as espécies aquáticas, a bioacumulação do metal em peixes marinhos ou de água doce tem sido encontrada em torno de 0,2 até 19,0 mg/kg de peso seco. No presente estudo, jundiás (Rhamdia quelen) foram expostos a diferentes concentrações de Mn (4,2; 8,4 e 16,2 mg/L), sob dois diferentes níveis de oxigênio dissolvido: normóxia (7,48±0,28 mg/L) e hipóxia (3,88±0,41 mg/L), durante 15 dias. Ao final do protocolo, a bioacumulação de Mn bem como, parâmetros de estresse oxidativo e a viabilidade mitocondrial foram avaliados em diferentes tecidos vitais. Em condições de hipóxia, a maior concentração de Mn (16,2 mg/L) mostrou os menores níveis de lipoperoxidação (LPO) em rim e encéfalo dos jundiás, enquanto os níveis de glutationa reduzida (GSH) encefálico foram aumentados na menor concentração de Mn (4,2 mg/L) e a atividade da catalase renal foi reduzida nesta mesma concentração de metal, em relação à normoxia. A menor concentração de Mn (4,2 m/L) em hipóxia proporcionou maior viabilidade mitocondrial das brânquias, em relação à normóxia. O hematócrito dos jundiás expostos às duas maiores concentrações de Mn (8,4 e 16,2 mg/L) foi reduzido em condições de normóxia, enquanto sob hipóxia, estes valores foram semelhantes ao grupo sem a presença do metal. Sob normóxia, a bioacumulação de Mn em fígado, rim e brânquias foi maior que sob hipóxia, excetuando o plasma. A partir desses resultados é possível sugerir que a hipóxia pode ter estimulado o desenvolvimento de mecanismos adaptativos ou de hormesis nos jundiás, em presença de Mn na água, principalmente porque neste nível de oxigênio, a bioacumulação do metal ocorreu em menor grau. Contribuindo com este resultado, sob hipóxia, os indicadores de danos oxidativos foram mais baixos que os observados sob normóxia, os quais foram acompanhados de alterações do sistema antioxidante representado pela GSH e catalase. Neste sentido, nossos resultados apontam para uma melhor sobrevivência da espécie em estudo, sob hipóxia, quando exposta ao Mn. Estes achados indicam a necessidade da continuidade dos estudos, em busca dos mecanismos moleculares envolvidos no processo de adaptação aqui sugeridos.

Water quality models in the Colorado River Basin have been developed for the basin, river, and individual reservoirs. They are used to support water quality programs within the basin. The models are periodically reviewed and updated to improve the accuracy of simulations. Improving the usefulness of the Lake Powell model, one of the key reservoirs in the basin, is the subject of this study. Lake Powell is simulated using a hydrodynamic and water quality model, CE-QUAL-W2. Previously the model has been used at Lake Powell to simulate hydrodynamics, temperature, and total dissolved solids with a reasonable degree of accuracy. An additional parameter, dissolved oxygen, will be added to the simulations and then calibrated with observed data to verify accuracy. Dissolved oxygen distributions in Lake Powell vary seasonally and change under different hydrologic cycles. They are a function of physical, biological, and chemical processes. Few measurements of these processes in Lake Powell exist. To compensate for the lack of data an empirical method of loading oxygen demand to the model is developed and tested. Observed limnological processes in the reservoir guide the development of the empirical methods. The methods are then tested in 16 year model simulations and compared with dissolved oxygen measurements from the 16 year period. By accurately reproducing the dissolved oxygen distributions the Lake Powell model will have improved accuracy and also broaden its usefulness.

published_or_final_version / Civil Engineering / Doctoral / Doctor of Philosophy

Wastewater disposal often has deleterious impacts on the receiving environment. Low levels of dissolved oxygen are of particular concern. Here I investigate the impacts on dissolved oxygen and carbon chemistry of screened municipal wastewater in the marine waters off Victoria, B.C., Canada. I analyzed data from a series of undersea moorings, ship-based monitoring, and underwater remotely-operated vehicle video. I used these observations to construct a two-layer box model of the nearfield receiving environment. Despite the lack of more advanced treatment, dissolved oxygen levels near the outfalls are well above the commonly used 63 umol kg-1 hypoxic threshold and that the outfalls’ impact on water column oxygen is likely less than a few umol kg-1. Likewise, dissolved inorganic carbon is not elevated and pH not depressed compared to the surrounding region. Strong tidal currents and the cold, well-oxygenated waters of Victoria’s marine environment give these waters a high assimilative capacity for organic waste. / Graduate / 0595 / 0403 / 0543 / jeremykrogh@gmail.com

I investigated seasonal and inter-site variation in factors influencing diel dissolved oxygen (DO) metabolism at four streams in the Virginia Coastal Plain. Data were collected monthly from January to August 2008 to characterize DO metabolism (diel DO amplitude, production, respiration), incident solar radiation (PAR), dissolved nutrients, fine benthic materials (mass, C:N, Chlα) and hydrology (discharge, water transit time, transient storage). Reach-scale metabolism estimates were determined using the one-station diurnal DO technique and transit time and transient storage were determined by conservative tracer additions. Incident solar radiation was the primary determinant of DO metabolism as streams experiencing higher light levels (Herring and Powell Creeks) exhibited greater diel DO amplitudes, production and respiration. Streams with greater riparian shading (Courthouse and Crump Creeks) exhibited lower DO metabolism despite their higher nutrient concentrations. Higher incident solar radiation was associated with greater benthic algal biomass at some (Herring, Crump, and Courthouse Creeks) but not all (Powell Creek) sites. Diel DO amplitudes were significantly and positively correlated with benthic Chlα and incident solar radiation at less shaded sites. These factors were not significant predictors of DO amplitude, production or respiration at more shaded sites.

Este trabalho apresenta a calibração e o desenvolvimento de um tanque de reaeração, equipamento que gera turbulência com intensidade controlável por meio de grade oscilante. Foram realizadas adequações ao projeto inicial de construção do tanque, idealizado por ROMA, onde se buscou o equilíbrio e as limitações de funcionamento para que, em futuros trabalhos, o tanque possa ser utilizado sob condições adequadas sem a presença de \"ruídos\" que venham a interferir nos resultados. A calibração do tanque foi realizada levantando-se o coeficiente de reaeração \'K IND.2\' para dois tipos de grades, 256 malhas/\'M POT.2\' e 1024 malhas/\'M POT.2\' constituídas por barras de seção medindo 10 x 10 mm, em diversas freqüências de oscilações sob condições controladas de temperatura e umidade relativa do ar. Com auxílio de um medidor eletroquímico de oxigênio dissolvido e de um contador de rotação, pôde-se acompanhar a reoxigenação da água e avaliar a freqüência de oscilação das grades. A desaeração da massa de água, necessária para a calibração do tanque, foi promovida por Stripping provocado por cavitação forçada à temperatura ambiente com injeção de nitrogênio. A taxa de reaeração \'K IND.2\' foi calculada por medidas da variação do oxigênio dissolvido em função do tempo provocada por agitação mecânica para determinada freqüência de oscilação da grade. Os resultados obtidos forneceram as curvas de reaeração em função da freqüência de oscilação e do tipo de grade utilizada em cada ensaio que, através do uso de planilha eletrônica, determinaram-se os valores de concentração de saturação (Cs) e coeficiente de reoxigenação (\'K IND.2\') com o uso de regressão não linear. / This work presents a reaeration tank development and its calibration, equipment that generates controlled intensity turbulence produced by oscillating grid. An adaptation on the original design idealized by Roma was made improving the equilibrium of the oscillating grid mechanism and defining the limits of functionality of the device. These are important aspects for future research on experimental turbulence generation since that the use of equipment free of undesirable disturbing noise are of fundamental importance. Tank calibration was obtained through the evaluation of the reaeration coefficient \'K IND.2\' using two types of oscillating grids, 256 and 1024 meshes/\'M POT.2\', constructed with 10 x 10 \'MM POT.2\' square section bars. Experimental runs were conducted under controlled conditions of air temperature and humidity, for several oscillating frequencies for each grid. The necessary water mass desaeration was obtained by ambient temperature stripping, induced by forced cavitation and nitrogen injection. Reaeration coefficients were calculated from data obtained from dissolved oxygen concentration measurements as function of time for each grid size and oscillating frequency combination. As results, reaeration curves with reaeration coefficients as function of oscillating frequency and grid type are presented.