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Understanding the transport processes in lakes and other aquatic systems is vitally important since much of the living biomass is transported by the water, along with nutrients, contaminants, suspended particles, and other materials important to biogeochemical processes. The hydrodynamic processes therefore determine the environmental conditions that affect the biogeochemistry. The physical processes that control the hydrodynamics of large lakes are complex, and depend on a balance of characteristics of the lake (geometry, stratification, etc.) and forcing conditions (meteorological, hydrological) that change over various spatial and temporal scales. Using data from several extensive field campaigns, including measurements of velocity and thermal structure at multiple locations over several seasons, an extensive set of CTD data, and a 15 year long bi-weekly water quality dataset at multiple locations, we analyze the physical forces controlling the dynamics of a large, narrow and deep lake, and the response of the lake to these forces. The study site is Cayuga Lake, the second largest of the Finger Lakes of central New York State, USA (latitude 43N). It is a long (60 km), narrow (less than 6 km) and deep (maximum 130 m) lake. The bathymetry at the south end of the lake slopes up to a shallow shelf, not unlike a coastal estuary, which receives discharges from both natural and anthropogenic sources, and on which sharp spatial and temporal gradients in water quality exist. The geometry of the lake and the prevailing winds in the region lead to the generation of large amplitude internal waves, which develop to be highly nonlinear. Shoaling of these waves on the southern shelf are shown to lead to the intermittent upwelling of hypolim- netic water on to the shelf, creating sharp spatial gradients in water quality (e.g., TP and chlorophyll-a concentrations) on the shelf. We analyze the internal wave field of the lake and the nonlinear processes associated with it, and the factors that lead to the sharp spatial gradients observed on the shelf. We show that a subtle balance of forces controls mixing and transport in the various regions of the lake and propose an explanation for a persistent anomaly in chlorophyll-a concentration observed in one region of the lake.
This textbook describes in detail the fundamental equations that govern the fate and transport of contaminants in the environment, and covers the application of these equations to engineering design and environmental impact analysis relating to contaminant discharges into rivers, lakes, wetlands, groundwater, and oceans. The third edition provides numerous end-of-chapter problems and an expanded solutions manual. Also introduced in this edition are PowerPoints slides for all chapters so that instructors have a ready-made course. Key distinguishing features of this book include: detailed coverage of the science behind water-quality regulations, state-of-the-art methods for calculating total maximum daily loads (TMDLs) for the remediation of impaired waters, modeling and control of nutrient levels in lakes and reservoirs, design of constructed treatment wetlands, design of groundwater remediation systems, design of ocean outfalls, control of oil spills in the ocean, and the design of systems to control the quality of surface runoff from watersheds into their receiving waters. In addition, the entire book is updated to provide the latest advances in the field of water-quality control. For example, concepts such as mixing zones are expanded to include physical nature and regulatory importance of mixing zones, practical aspects of outfall and diffuser design are also included, specific details of water-quality modeling are updated to reflect the latest developments on this topic, and new findings relating to priority and emerging pollutants are added.
In recent decades it has become increasingly urgent to protect human health and wellbeing from the possible negative consequences of man's economic activities, both at the actual production sites and in areas where the im pact is felt. These negative effects have gradually become more and more widespread, presenting a major hazard to the natural environment, taking on an international character, and assuming global proportions. For the countries of Europe and North America, transport of pollutants and acid rain across boundaries is a serious problem. After the Chernobyl reactor accident, regular measurements of radioactive isotopes became im perative. It is obvious that drastic measures, including steps taken on an interna tionallevel, are required to limit the negative anthropogenic impact on the environment. Under the conditions of this growing man-caused impact on nature, the existing ecological reserves of the biosphere should be husbanded especially carefully. We must determine the regimes of rational utilization of these reserves and of judicious management of the natural environment, thereby maintaining a high quality of the biosphere and preserving nature's regener ative capacity. Reliable methods should be developed to keep the environ ment from being overloaded and to safeguard the elements of the biosphere from injury. Given such a situation, it is of particular importance to have objective information about the critical factors of the human impact and the actual state of the biosphere, as well as to obtain forecasts of its future state.
Arranged logically to follow the most widely adopted course structure, this text will leave students with a full understanding of the unique structure, function, and living patterns of all vertebrates.
By the year 2000, the number of people at risk from volcanic hazards is likely to increase to around half a billion. Since 1980, significant advances have been made in volcano monitoring, the data from which provides the sole scientific basis for eruption prediction. Here, internationally renowned and highly experienced specialists provide 25 comprehensive articles covering a wide range of related topics: monitoring techniques and data analysis; modelling of monitoring data and eruptive phenomena; volcanic hazards and risk assessment; and volcanic emergency management. Selected case histories of recent volcanic disasters, such as Mount Pinatubo in the Philippines, demonstrate that effective communication - between scientists, civil authorities, the media and the population at risk - is essential to reducing the danger.