What is the primary way that nitrogen and phosphorus end up in bodies of water?
Increases in contaminant loading are also likely; for example, from urban runoff and intensified agricultural production. We do not consider contaminants further because their effects are often site-specific and sporadic. Show
View chapterPurchase book Read full chapter URL: https://www.sciencedirect.com/science/article/pii/B978012384703400438X Sustainability modelingIbrahim Dincer, Azzam Abu-Rayash, in Energy Sustainability, 2020 6.4.1.3.4 Eutrophication potentialEutrophication is a leading cause of impairment for many coastal marine and freshwater ecosystems. It is characterized by excessive growth of algae and plant due to increased availability of one or more limiting growth factors, which are needed to conduct photosynbook. Eutrophication is characterized by phosphate equivalence (PO4-eq) in life cycle impact assessments. Eutrophication is often detrimental to plants and ecosystems and leads to the vulnerability of economic and social structures. The following equation illustrates the calculation of the EP score (Hacatoglu, 2014): (6.14)YEP=XEP(T)XEP where XEP represents the actual life cycle emissions of PO4 per capita per year. XEP(T) represents the target value, which is calculated using the following equation (Hacatoglu, 2014): (6.15)XEP(T)=EPref×αEP where EPref represents the global annual per capita of PO4 emissions and αEP represents the adjustment factor. View chapterPurchase book Read full chapter URL: https://www.sciencedirect.com/science/article/pii/B9780128195567000061 Sustainable Water-Treatment TechnologyParimal Pal, in Industrial Water Treatment Process Technology, 2017 10.1.3 Innovation in Recovery of Nutrients from Industrial WastewaterEutrophication of surface water from industrial and municipal wastewater often results in the destruction of many natural water bodies around the world. Nutrients like nitrogen and phosphates encourage such eutrophication. Algal bloom makes water bodies unfit for human use. However, eutrophication can largely be overcome by cutting the entry of nutrients to water bodies through municipal and industrial discharge. A recently developed hybrid technology [4] has the potential to solve this problem. This new technology integrates chemical and biological treatments with membrane separation and effectively separates the nutrients from ammoniacal industrial wastewater. The nutrients are recovered as valuable struvite fertilizer for subsequent use in agriculture and planned plantation. This novel approach simultaneously turns waste into a valuable resource, protects surface bodies from hazardous waste contamination, makes the treated water reusable, and adds economy to the wastewater-treatment technology. The associated cost is low and the plant operation promises continuous improvement of the water environment. As this technology is operationally fast, efficient, and economically attractive it is a sustainable technology. View chapterPurchase book Read full chapter URL: https://www.sciencedirect.com/science/article/pii/B9780128103913000102 21st European Symposium on Computer Aided Process EngineeringVanina Estrada, ... M. Soledad Diaz, in Computer Aided Chemical Engineering, 2011 1 IntroductionEutrophication in most water bodies is an important environmental problem. It is caused by increasing nutrient loading associated to urban, industrial and agricultural activities. Eutrophication is associated to accelerated growth of phytoplankton (algal blooms). The presence of certain species of cyanobacteria within the blooms is of special care, as they may produce hepato- and neurotoxins that can severely compromise human and animal health. To address nutrient point sources, such as urban and industrial, much effort has been devoted to the development of wastewater treatment processes and facilities (Gernaey et al., 2004; Karuppiah and Grossmann, 2008). However, nonpoint nutrient sources, such as those associated to agricultural activities, have not received much attention (Estrada et al., 2009). In particular, increased eutrophication can be a key feature associated to the large-scale production of biofuels from energy crops when compared to fossil fuels. The life cycle wide emissions of nutrients depend on the application and losses of fertilisers during the agricultural production of biofuel feedstocks. External restoration techniques for nonpoint sources include the construction of artificial wetlands nearby the water bodies to remove nutrients and, in this way, decrease nutrient loading. Within in-lake restoration strategies, biomanipulation is based on the trophic chain theory and it has been applied to control phytoplankton growth in lakes and reservoirs. The basic idea is to keep a high grazing pressure on the phytoplankton community by the herbivore zooplankton by performing zooplanktivorous fish removal (Sondegaard et al., 2007). Another in-lake restoration strategy is hypolimniom aeration, so as to precipitate phosphorous compounds to the sediment, not becoming available for phytoplankton production. Three dimensional eutrophication models have been proposed for large lakes with horizontal uneven distributions (Hu et al., 2006) and for costal systems (Moll and Radach, 2003). In this work, we formulate a three-dimensional eutrophication model, based on a previous one-dimensional model (Estrada et al.; 2010) for a reservoir that provides drinking water for two cities in Argentina. The model is based on first principles, with parameters that have been tuned with collected data from the specific reservoir under study (Estrada et al., 2009). It includes dynamic mass balances for three phytoplankton groups and main nutrients. The model is developed within a control vector parametrization dynamic optimization framework in which the water body has been spatially discretized in volume elements. Numerical results provide quantitative information for planning restoration strategies over a one year horizon, as well as its effect on algae growth and nutrient concentration. View chapterPurchase book Read full chapter URL: https://www.sciencedirect.com/science/article/pii/B9780444542984500350 Background knowledge and tools for prediction of ecological impactsHans F. Burcharth, ... Alberto Lamberti, in Environmental Design Guidelines for Low Crested Coastal Structures, 2007 d) Broad-scale eutrophicationEutrophication (anthropogenic nutrient enrichment) is a common phenomenon in enclosed bays and estuaries due to a combination of agricultural run-off and human and agricultural wastes (Correggiari et al., 1992). It can also scale up to larger areas such as the northern Adriatic, parts of the Baltic and the southern North Sea and possibly the Irish Sea, resulting in eutrophic seas (Allen et al., 1998). On a large scale, atmospheric input of nitrogen can also be important. Eutrophication causes several effects in the marine ecosystem. Higher concentration of nutrients will lead to an increase in the abundance of phytoplankton and consequently greater food resources for filter-feeders such as mussels. However, the likelihood of harmful algal blooms (e.g. red tides) will also increase causing anoxia and thus killing macroalgae and marine invertebrates (Southgate et al., 1984). Macroalgal growth, for example ephemeral green algae, will also be faster in eutrophic conditions, in many instances being able to outpace grazing activities. On LCS, eutrophic waters coupled with high levels of disturbance will create optimal conditions for proliferation of slippery green algae. Sediments, in turn, will tend to become muddy and compact, leading to substantial changes in the chemical gradients in the sediment (e.g., anoxia) which will, in turn, modify the infaunal composition (i.e., reduction of diversity, and proliferation of opportunistic species). Impacts of eutrophication will be worse on the landward side of LCS, where water movement is significantly reduced, particularly if the structures are connected to the shore by groynes. View chapterPurchase book Read full chapter URL: https://www.sciencedirect.com/science/article/pii/B9780080449517500348 Environmental Biotechnology and SafetyM. Pell, A. Wörman, in Comprehensive Biotechnology (Second Edition), 2011 6.24.1 IntroductionEutrophication of water courses, lakes, and marine environments is a major issue in most parts of the world. Looking back 150 years, the urban situation in the emerging industrial part of the world led to the introduction of water-based systems for conveying and discharge of sewage. At first, the wastewater was disposed into nearby watercourses and lakes. As the populations grow, this was not a sustainable solution – the natural wetlands became overloaded as evident from the odors. This untenable situation led to the development of more active treatment systems such as shallow ponds and sand filters. In 1914, the activated sludge technique was introduced by Arden and Lockett, a technique that still probably is the most common technique for wastewater treatment (WWT) in the industrial part of the world. In the 1960s, eutrophication became evident due to the high amounts of plant nutrients discharged from sewage treatment plants. The first and maybe the simplest solution was to remove phosphorus by chemical precipitation. The European Commission and national authorities have gradually, over the latest couple of decades, sharpened the treatment demands, especially with regard to nitrogen, in order to avoid further eutrophication in the sea. Hence, WWT today probably is more focused on removing phosphorus and nitrogen than pathogens. It is still argued whether phosphorus or nitrogen is limiting for the eutrophication process, that is, should either one or both of these elements be eliminated. Simply put, biological WWT can be defined as a natural process in which organisms assist in environmental cleanup simply through their own life-sustaining activities. By studying the organisms in natural ecosystems, the biologists have explored their function and capacity to degrade organic matter and transform nutrients. Such information has then been used by engineers to design effective WWT systems, that is, the biological processes have been concentrated into well-regulated units. In addition, knowledge of geochemistry, hydrology, etc., is an essential component of a successful system for treating polluted waters. Hence, globally, WWT probably is the most common biotechnological process. Though the same biological processes are the basis for most WWT systems, there are probably innumerable technological solutions for achieving the goal. The numbers of techniques are as many as there are sanitary engineers. However, the techniques may be categorized as follows: (1) soil filters and wetlands – terrestrial ecosystems working as natural filters; natural water courses, lakes, and wetlands; soils receiving irrigated wastewater; constructed wetlands and ponds; soil or sand absorption systems; and trickling filters and (2) treatment plants – rotating biological contactors; fluidized beds; and activated sludge systems including sequencing batch reactors (SBRs). This array of techniques describes the systems on a scale from natural ecosystems at one end to high-technology solutions at the other end. In the choice of WWT system to be used, many factors such as influent water characteristics, desirable effluent water quality, costs for building and maintenance, and population density and dimensioning have to be considered. This article gives a general background on the microbial cell and biological processes important in all WWT; focuses on the importance of understanding the interaction between hydraulic performance and microbial processes to achieve effective nitrogen removal; and outlines the function of two common systems: the constructed wetland, requiring in-depth knowledge on hydraulic properties, and the activated sludge process, relying on advanced control and optimization. Finally, the article gives some perspectives on the future development of biological WWT systems and their use. View chapterPurchase book Read full chapter URL: https://www.sciencedirect.com/science/article/pii/B9780080885049003810 Watershed EventsDaniel A. Vallero Ph.D., in Paradigms Lost, 2006 The Death of Lake Erie: The Price of Progress?The demise of Lake Erie in the 1960s was emblematic of the environmental challenge growing out of the industrial and petrochemical revolutions of the nineteenth and twentieth centuries in the West. Companies, municipalities, and people in general had seemingly perceived water to be completely elastic in its ability to absorb any amount and type of pollution. Any waste that needed to be disposed of was directly discharged into surface waters, such as rivers, lakes, and oceans. Lake Erie provides numerous lessons. For those of us who were learning the new language of environmental science, Lake Erie gave us a new paradigm, one of optimism where even highly polluted waters could be saved. For the decades that followed the 1960s, water bodies began to recover from even extremely polluted conditions. Although the science of limnology (the study of freshwater systems) had been well established within the hydrologic and biological science communities, the problems in Lake Erie helped to propel it into a much wider application. For example, eutrophication of freshwaters, especially ponds and lakes, became better understood in the context of Lake Erie (see the discussion box, “Eutrophication”). EutrophicationHealthy water bodies contain sufficiently low amounts of contaminants and sufficiently high amounts of dissolved oxygen (DO) to support a balance of aquatic life. The DO concentrations in surface waters can be reduced by both natural and human factors. Evidence of a healthy water body is its trophic state. Every lake fits into a particular trophic state, according to its degree of eutrophication, and all lakes change their trophic status over time. All lakes, even the most pristine, are undergoing nutrient enrichment and filling. Lakes can be divided into three categories based on trophic state—oligotrophic, mesotrophic, and eutrophic. These categories reflect a lake’s nutrient and clarity levels. Limnologists refer to healthy water bodies as oligotrophic systems; that is, they contain little plant nutrients and are often continuously cool and clear. Oligotrophic waters have very low production of organic matter by photosynthesis and can support diverse animal life and collect optimal amounts of nutrients, mainly phosphorous and nitrogen, from natural sources, such as decomposing plant matter. When a water body becomes enriched in dissolved nutrients, especially phosphorous and nitrogen, they stimulate the growth of aquatic plant life, which can lead to the depletion of dissolved oxygen (DO). This is known as eutrophication. Oligotrophic lakes (see Figure 4.1) are generally clear, deep, and free of weeds or large algae blooms. Though aesthetically appealing, they are low in nutrients and do not support large fish populations. Nutrient concentrations, such as phosphorous and nitrogen, are limiting, and aquatic macrophytes (large plants) and algae are less abundant. Oligotrophic water bodies typically have accumulated little plant debris on the bottom over the years since aquatic macrophytes and algae are less abundant. They generally have water clarity greater than four meters (i.e., the distance one can see down into the water) since the amounts of free-floating algae are low, as well as the absence of presence of coloring agents in dissolved substances and low concentrations of suspended particles. Fish and wildlife populations generally will be small because food and habitat are often limited. Oligotrophic water bodies usually do not support abundant populations of sportfish such as large-mouth bass and bream, and it usually takes longer for individual fish to grow in size in oligotrophic waters. However, oligotrophic lakes often develop a food chain capable of sustaining a very desirable fishery of large game fish, but these conditions can deteriorate in a short amount of time due to fishing pressure increases. FIGURE 4.1. Oligotrophic lake system. A mesotrophic lake (see Figure 4.2) can support moderate populations of living organisms. These lakes have moderate concentrations of nutrients and moderate growth of plant life, such as algae and/or macrophytes, owing to the moderate concentrations of nutrients (especially N and P). There is evidence of slight sediment buildup and organic accumulations. Clarity is between 2 and 4 m, so a mesotrophic lake is usually “swimmable and fishable,” to use a phrase made famous by the Federal Water Pollution Control Act of 1972. FIGURE 4.2. Mesotrophic lake system. Eutrophic waterbodies (see Figure 4.3) may be dominated by algal growth or by larger plant growth. If algae-dominated, the water may have a green, cloudy appearance from the colonies of algae suspended or floating in the water. If plant-dominated, the submersed macrophytes will decrease the concentrations of the green pigment, chlorophyll, and use much of the nutrient concentrations, making for clearer water. Thus clarity as indicated by Secchi depth readings are higher than if the water body were an algae-dominated eutrophic system. This makes trophic state classification based on appearance very difficult. FIGURE 4.3. Eutrophic lake system. Like almost everything in the environment, there is an optimal range between too little and too much nutrient loading. A minimal amount of nutrients is needed in any ecosystem, but when this amount is exceeded, as was the case for Lake Erie some decades ago, algal growth can become prolific. In the right balance, algae serve as food sources and are crucial to energy and mass balances in aquatic systems. Out of balance, however, the algae use up too much of the DO needed by fish and other aquatic organisms. The nutrients find their way into water bodies through numerous avenues, but the major categories are either point sources or nonpoint sources. As the name implies, point sources deliver nutrients and other pollutants to surface waters from a single point, such as a pipe, conduit, outfall structure, or ditch. Non-point pollutants are those that flow over broad expanses, such as runoff from agricultural practices, mining, roads, neighborhoods, and urbanized areas. Another nonpoint source of pollutants is the atmosphere. In fact, atmospheric deposition can be the largest source of many contaminants. The nutrients can take on many physical and chemical properties. For example, nitrogen can be in solid phase, such as in a commercial fertilizer, in liquid phase, such as when ammonia is dissolved in runoff water, or in gas phase, such as when ammonia or nitric acid is found in soil pores. The chemical forms can also be diverse, such as when conditions make for a reduced form, for example, ammonia, or in an oxidized form, such as nitrite or nitrate. Thus, the process of eutrophication includes elevated biological productivity resulting from increased input of nutrients or organic matter into aquatic systems. For lakes, which do not flow as rapidly as streams, such increased biological productivity usually leads to decreased lake volume because organic detritus accumulates. Natural eutrophication continues as aquatic systems fill in with organic matter. This is contrasted with cultural eutrophication, which is exacerbated by human activities and the consequent point and nonpoint pollution. In retrospect, the death sentence to Lake Erie was premature. The assumptions of the time were that things could not change enough to return biodiversity to the lake ecosystem. Thankfully, these predictions were wrong. However, the Great Lakes are still vulnerable. In fact, some new problems have emerged, whereas others have been solved. To wit, the invasion of opportunistic species that are threatening the diversity of enormous regions; notably the appearance and proliferation of the zebra mussel (Dreissenia polymorpha) throughout much of the Great Lakes (see the discussion in Chapter 6). View chapterPurchase book Read full chapter URL: https://www.sciencedirect.com/science/article/pii/B9780750678889500065 How Green and Does it CleanJason P. Marshall, Heidi Wilcox, in Developments in Surface Contamination and Cleaning, 2015 6.3.10 EutrophicationEutrophication is the process by which a body of water becomes enriched in dissolved nutrients (as phosphates), stimulating the growth of aquatic plant life usually resulting in the depletion of dissolved oxygen. Table 1.5 lists more specifics on the various categories and thresholds for the DfE assessment. Table 1.5. DfE Master Criteria Cleaning Productsa [18] CategoryThresholdsAcute mammalian toxicityRoute (units)Median lethal dose/concentrationOral, LD50 (mg/kg-bw) (by weight)2000Dermal, LD50 (mg/kg-bw)2000Inhalation, LC50 (vapor/gas) (mg/L)20Inhalation, LC50 (dust/mist/fumes) (mg/L)5R20: Harmful by inhalation What is the primary way that nitrogen and phosphorus and up in bodies of water like the Chesapeake Bay?Major Sources of Nitrogen and Phosphorus
The largest source of pollution to the Bay comes from agricultural runoff, which contributes roughly 40 percent of the nitrogen and 50 percent of the phosphorus entering the Chesapeake Bay. The fastest growing source of nitrogen pollution to the Bay is polluted runoff.
What is the primary way that nitrogen and phosphorus end up in bodies of water like the Chesapeake Bay quizlet?What is the primary way that nitrogen and phosphorus end up in bodies of water like the Chesapeake Bay? Water in runoff and streamflow transports nitrogen and phosphorus from fertilizer into the body of water.
How does phosphorus and nitrogen enter water?Nitrogen is most likely to come from transportation, industry, agriculture and fertilizer application, while increased phosphorus is more commonly the result of sewage waste, amplified soil erosion and runoff from urban watersheds.
What is the main way in which excess phosphorus and nitrogen get into bodies of water to result in eutrophication?The sources of excess phosphate are phosphates in detergent, industrial/domestic run-offs, and fertilizers. With the phasing out of phosphate-containing detergents in the 1970s, industrial/domestic run-off, sewage and agriculture have emerged as the dominant contributors to eutrophication.
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