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Eutrophication

Eutrophication is a complex environmental phenomenon characterized by the excessive enrichment of aquatic ecosystems with nutrients, particularly nitrogen and phosphorus.
This process can lead to the rapid growth of algae and other aquatic plants, resulting in a depletion of dissolved oxygen and the degradation of water quality.
Eutrophication can have far-reaching consequences, impacting the delicate balance of aquatic ecosystems, threatening biodiversity, and posing risks to human health and economic activities.
Understanding and addressing eutrophication is crucial for the preservation of our waterways and the sustainable management of natural resources.
PubCompare.ai offers a powerful AI-driven platform to optimize eutrophication research, helping researchers locate the best protocols from literature, preprints, and patents, while enhancing reproducibility and accuracy through intelligent comparisons.
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Most cited protocols related to «Eutrophication»

Environmental variables were grouped into three categories based on the role that they play as coral stressors: (1) radiation variables, consisting of variables derived from temperature (mean SST, TSA and WSSTA magnitude and duration), UV-erythermal and wind speed data (doldrums index); (2) stress reinforcing variable (TSM and chlorophyll-a), representing sedimentation and eutrophication; and (3) stress reducing variables, consisting of SST variability and tidal range. Values of each variable that correspond with the approximately 4000 reef locations were extracted, and examined for normality and log10-transformations applied where necessary (Appendix S3). For each variable, a membership function with similar behavior pattern to a normal cumulative distribution function was used to characterize the relationship between coral exposure and a stress variable. Membership functions capture the degree to which the variable x is a member of a fuzzy set A using a suitably chosen function μ(x) [48] . Here we used spline-based logistic functions:
where xa and xb are control values and correspond to the lower and upper bound of a stressor values, respectively (Table 1). These were calculated for each variable as the mean value of minus or plus two standard deviations, respectively. Radiation and reinforcing variables were normalized using an increasing curve (Eq. 1) and stress reducing variables were normalized using a decreasing curve (Eq. 2) (Fig. 1).
Spatial Principal Component Analyses (SPCA) was used to combine the standardized variables within each category. Principal Component Analysis transforms each variable into a linear combination of orthogonal common components (output layers), or latent variables with decreasing variation. The linear transformation assumes the components will explain all of the variance in each variable. Hence, for each output the latent component layer carries different information, which is uncorrelated with other components. This enables a reduction of output maps because the last transformed map(s) may be discarded as they have little or no variation left and may be virtually constant. The component weightings were calculated using coefficients of linear correlation to weigh the contribution of factors in spatial principal component analysis [67] . SPCA was performed to synthesize the standardized variables within radiation, stress reducing, and stress reinforcing categories. A final composite map from each of these three groups was computed by summing PC's with contribution ratio >1, weighted by their respective contribution ratio (Equation 3; [68] , [16] ). where Yi is the ith principal component, while αi is its corresponding contribution ratio.
The output maps were standardized between zero and one, representing low and high exposure respectively. To combine the stress reducing and radiation variables, SPCA procedure described above was repeated with standardized radiation and reducing variables as the input variables. The output PC's were synthesized using a weighted sum equation (Eq. 3) to yield a layer with estimates of exposure to radiation taking into account the contribution from reducing variables. Fuzzy-integration-based approach was used to integrate the output from this procedure with the reinforcing variables into a single composite layer. [69] lists five fuzzy operators that are most useful for combining fuzzy data (AND, OR, sum, product and gamma). Given two fuzzy sets (standardized layers) A and B, the fuzzy sum operator produces a layer whose values are equal to or greater than each of the input layers A and B and results in an increased effect [69] . We therefore used fuzzy sum operator to reflect the reinforcing behaviour of sediment and eutrophication to radiation stress: where .is the membership value for i-th map, and i = A, B, n maps.
Coral reef location data was obtained from the Reef Base website (http://reefgis.reefbase.org/) and the Wildlife Conservation Society monitoring sites in the western Indian Ocean [70] (link). The location data were grouped into eleven oceanic provinces [9] (link) (Fig. 2). For the respective locations, exposure metrics as described above were extracted for the corresponding locations. Box plots of exposure metrics by stressors against the coral reef provinces were plotted.
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Publication 2011
chlorophyll a' Coral Coral Reefs Eutrophication Gamma Rays Microtubule-Associated Proteins Radiation Wind
For the ECOALIM dataset, several system perimeters were defined (Fig 1): field gate, storage-agency gate, plant gate, and harbour gate. The field gate is relevant for assessing impacts of on-farm feed production (i.e. crops produced and directly used on-farm). Feed formulation by feed companies requires additional perimeters: plant gate for the co-products of cereals, oilseeds and protein crops (e.g. meals) as well as for industrial products (e.g. amino acids) processed in France; storage-agency gate for cereals (perimeter includes grain drying); and harbour gate for imported feed ingredients.
The impacts considered were climate change with (CCLUC) or without land-use change (CC), eutrophication (EU), acidification (AC), land occupation (LO), non-renewable (CEDNR) and total energy demand (CEDTOT) and P demand (PD). PD was included to account for the non-renewable P resource incorporated in fertilisers and feeds. The other impact categories are usually included in agricultural LCAs.
When a production process generates multiple final co-products, it is necessary to allocate the process’s impacts to the co-products. In ECOALIM, impacts of co-products of cereals and maize, as well as oils and meals, were calculated using economic allocation. To perform this allocation based on the relative economic value of each co-product, the Olympic five-year (2008–2012) average price of each co-product was calculated. The functional unit used is kilogram of feed ingredient at the reference water content, which is the usual functional unit for feed ingredients.
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Publication 2016
Agricultural Crops Amaurosis congenita of Leber, type 1 Amino Acids Cereals Climate Change Eutrophication Maize Oils Perimetry Plants Proteins
The Eco-indicator 99 method belongs to the methods used for modeling environmental impact at the level of an environmental mechanism’s final points. The characterizing process is performed for 11 impact categories within the three largest groups which are referred to as impact areas or damage categories. The impact areas include human health, ecosystem quality, and resources [45 (link),46 (link)]. The first damage category condenses respiratory and carcinogenic effects, effects on climate change, ozone layer depletion, and ionizing radiation into one value expressed in DALY (disability adjusted life-years). The damage to ecosystem quality is expressed in terms of the percentage of species that have disappeared in a certain area due to the environmental load (percentage of vascular plant species km2yr). Ecotoxicity covers the percentage of all species present in the environment living under toxic stress (PAF: Potentially affected fraction). Regarding acidification/eutrophication, the damage to a specific target species (vascular plants) in natural areas is modeled (PDF: Potentially disappeared fraction). The damage category covering resource extraction gives a value expressed in MJ surplus energy to indicate the quality of the remaining mineral and fossil resources Table 2 [47 ].
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Publication 2019
Carcinogens Climate Change Ecosystem Eutrophication Homo sapiens Impacts, Environmental Minerals Ozone Layer Depletion Radiation, Ionizing Respiratory Rate Tracheophyta
In situ observations for data validation were selected across a diverse geographic area under a variety of atmospheric and aquatic conditions (Kilpatrick et al. 2001 (link)) to ensure a comprehensive validation dataset. Representative estuaries were selected from the NOAA National Estuarine Eutrophication Assessment regions (Table 1; Bricker et al. 2007 ). Mobile Bay is an open bay system in the Gulf of Mexico with a subtropical climate and annual air temperatures of 22°C. Mid-Atlantic estuaries include New York and New Jersey locations and coastal ocean sites with temperate climates and annual air temperatures of 12°C. South Carolina estuaries are in the South Atlantic region in a temperate climate with annual mean air temperatures of 19°C. Puget Sound is a fjord system in the Pacific region with annual air temperature of 10°C. Barnegat Bay, Mobile Bay, and Puget Sound estuaries also are identified as part of the National Estuarine Program to restore water quality and ecological integrity.
Representative lakes were selected from the nine National Aquatic Resources Survey ecoregions (Herlihy et al. 2008 (link)). The lakes by region are summarized in Table 1. The Coastal Plains region includes the Gulf Coast from Florida to eastern Texas with flat topography. Lake Champlain is a major waterbody in the Northern Appalachians region that includes the Adirondack Mountains within the cold climate zone. The Northern Plains region is dry, with short summers and long winters. The Southern Appalachians region has a wet temperate climate contrary to the Southern Plains region, which has a dry temperate climate. The Temperate Plains region is mild in climate, with balanced winters and summers. The Upper Midwest region is known for cold winters and short summers. The Western Mountains region is sub-arid and the Xeric region is warm and dry.
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Publication 2018
Climate Cold Climate Cold Temperature Estuaries Eutrophication Fjord Sound Water, Body
We emphasize that the analysis above should be considered conservative in its estimate of emissions. First, we reduced the emphasis on high-end estimates of global area by using gamma distributions to minimize the impact of especially high estimates. Second, we did not include any potential impacts on deep sediment C (>1 m depth), in part because of limited available science. These layers often contain more C per hectare than all the near-surface carbon combined [24] and have been found to be impacted by land-use change in the few cases studied [23] . This means that even our high-end scenario of 100% C loss upon conversion is actually much less than all of the ecosystem carbon. Third, the low-end scenario of 25% C loss upon conversion effectively assumes that all land-use changes in coastal systems across the entire globe could retain 75% of all near-surface carbon (if most C in disturbed systems is merely buried or redistributed) – an extremely conservative assumption. Fourth, we did not include the loss of annual sequestration of sediment carbon that occurs due to vegetation removal or hydrological isolation that reduces new sediment inputs.
Regarding other greenhouse gases such as methane (CH4) or nitrous oxide (N2O), excluding changes in these components is likely either a neutral or conservative approach. In highly saline wetlands (>18 ppt), sediment C sequestration rates exceed CH4 emission rates in CO2-equivalent units [55] , suggesting that the net effect of losing both sequestration and CH4 emissions with disturbance should be an increase in greenhouse gas emissions. In lower salinity wetlands (salinity 5–18 ppt), CH4 emissions and sequestration are approximately in balance [56] , except perhaps for oligohaline systems (<5 ppt) that are a small portion of the global area we evaluated. Finally, we conservatively did not consider evidence that common disturbances, such as conversion to shrimp ponds, that cause eutrophication have been shown to stimulate CH4 emissions [27] . Eutrophication is likely to also increase N2O emissions if the system receives high nitrate loading; otherwise it is not necessary to account for changes in N2O fluxes because emissions from anaerobic sediments are negligible in the absence of nitrate loading.
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Publication 2012
Carbon Carbon Sequestration Ecosystem Eutrophication Eye Gamma Rays Greenhouse Gases isolation Methane Microphthalmos Nitrates Saline Solution Salinity Wetlands

Most recents protocols related to «Eutrophication»

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Publication 2023
Concept Formation COVID 19 Epidemics Eutrophication Food Forests Genetic Heterogeneity Head Joints Optimism Pressure Rivers Silk Silver Water Resources
We calculate the ANPS pollution emissions from crops, animal breeding, aquaculture, and rural community sources (shown in Table 1). Unabsorbed nutrients from chemical fertilizers used in agriculture leach into groundwater and surface water due to rain and irrigation, and this causes surface water eutrophication and groundwater nitrate pollution [30 ,31 ]. Incineration of farmland crop residue or crop residue dumping will cause organic matter and microorganisms to enter the water body and cause water pollution [32 ,33 ,34 ]. According to the second survey report of pollution sources in China in 2016, livestock and poultry manure ranked first among all pollution sources from the agricultural sector. The feces, urine, and sewage generated during the livestock and poultry breeding process lead to a large amount of loss of nitrogen and phosphorus entering waterways [35 ,36 ]. Aquaculture also results in pollution due to excessive inputs of bait, the production of excrement, and the use of chemicals and antibiotics [37 ]. Finally, with the improvement of the living standards in China’s rural areas, the discharge of domestic sewage is increasing which has become one of the main sources of water pollution [38 ]. All of these sources are accounted for in our analysis.
ANPS pollution can be calculated for different sources with differences in the geographic characteristics of pollutants [39 ,40 ,41 ]. The equations used to calculate the Total Nitrogen (TN), Total Phosphorus (TP), and COD emissions from agricultural production units in each province every year are provided in Table 2.
In each equation, the loading coefficient, λ , is for N, P, and COD for each pollutant (details of the loading coefficients for all sources are in the Supplementary Materials). For fertilizer, aquaculture, and rural domestic sewage, the pollution is estimated by multiplying the variable from Table 1 by the respective loading coefficient. For example, the total amount of the kth fertilizer (1 = nitrogen fertilizer, 2 = phosphate fertilizer, 2 = compound fertilizer) input is Tk ; the loading coefficient s of N and P in the kth fertilizer are λkFn and λkFp . The emissions of nitrogen and phosphorus, Fn and FP , equal Tk multiplies Tn×λkFn and Tp×λkFp .
More coefficients need to be included for livestock poultry and crop residue. When calculating the emissions from livestock and poultry farming, Tz is the end-of-period or slaughtering quantity of the zth livestock and poultry (1 = poultry, 2 = pigs, and 3-cattle) and θzL is the growth cycle of the zth livestock and poultry. The growth cycle of θzL is 140, 180, and 365 days for poultry, pigs, and cattle respectively. The loading coefficient s, λzLn, λzLp, λzLn , are multiplied by Tz and θzL to get Ln , Lp , Lcod , the emissions of N, P, and COD from livestock and poultry farming. For crop residue, the yield of the mth crop is Tm ; the crop residue production coefficient of the mth crop is φm ; the loading coefficient s of N, P, and COD in the crop residue are λSn , λSp , λSc ; Sn , Sp , Sc are the total amount of N, P, COD emissions from crop residue which come from Tm multiplied by φk and λSn , λSp , λSc .
Finally, we add up the emissions from all pollution sources to obtain the ANPS pollution emissions of i = 1, …, 31 provinces (municipalities and autonomous regions) from t = 2010 to 2019 (Details of the calculation process are in the Supplementary Materials): ANPSit=wTNit(Fnit+Snit+Lnit+Enit+Anit)+wTPit(Fpit+Spit+Lpit+Epit+Apit)+wCODit(SCODit+LCODit+ECODit+ACODit)
where ANPSit is the ANPS pollution emissions in the ith province in the tth year; the weights of TN, TP, and COD emissions, wTNi,t , wTPi,t , and wCODi,t , are calculated by the entropy method [42 ,43 ] (Entropy method is one of the common methods to determine weight and is a relatively objective and widely used than the analytic hierarchy process and coefficient of variation method. This paper draws on the improvement of entropy method made by Yang and Sun (2015), and adds time variable for analysis, so as to realize the comparison between different years.). It is worth emphasizing that we consider the differences in topography, climate, farming methods, crops, or breeding types of each province (municipalities and autonomous regions), and we use different loading coefficients for each area. However, the loading coefficients are held constant. Hence, if policies affect practices that reduce the amount of pollution generated by an activity, this will not be captured in our analysis.
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Publication 2023
Animals Antibiotics, Antitubercular ARID1A protein, human Cattle Climate Crop, Avian Entropy Environmental Pollutants Eutrophication Feces Fowls, Domestic Incineration Livestock Nitrates Nitrogen Nutrients Patient Discharge Phosphates Phosphorus Pigs Rain Rural Communities Sewage Urine Water, Body Water Pollution
Lake Ińsko (53°26′36″ N, 15°32′33″ E) and Wisola (53°24′46″ N, 15°32′49″ E) are located in north-western Poland. Compared with other lakes of the Polish Plain, Lake Ińsko is large (486.6 ha) and deep (maximum depth 41.3 m, mean depth 12.9 m) [44 (link)]. Lake Wisola has a water surface area of 181.5 ha, a mean depth of 5.9 m and a maximum depth of 15.4 m [31 (link)]. The two lakes differ in the degree of eutrophication and anthropopressure. Studies conducted in the years 1970–2010 showed significant changes in the water quality of Lake Ińsko and its trophic gradient, from mesotrophy to signs of eutrophication [44 (link)]. Based on the saturation of the hypolimnion with oxygen, Filipiak et al. [31 (link)] classified Lake Ińsko as a α-mesotrophic subtype (oxygen saturation > 20%) and Lake Wisola as β-mesotrophic (oxygen saturation < 20%).
Lake Ińsko was negatively influenced by nearby urban development (the town of Ińsko), which was reflected in a higher concentration of nitrogen, phosphorus compounds and sulphates [45 ]. However, at the end of the 1990s and in the 2000s, the lake reverted to a mesotrophic state [44 (link)] characterized by a moderate susceptibility to deterioration and the second class of water purity [46 ]. According to Kubiak et al. [44 (link)], the improvement most likely resulted from the changes in soil use in the catchment area, as less phosphorus and nitrogen compounds flowed into the lake, as well as from the improved sewage disposal system in the town of Ińsko. Lake Wisola is a flow-through reservoir fed by the Iński Canal (W7) (Figure 1); however, the outflow sometimes stops as a result of periodic stoppages in the inflow of water through the Iński Canal, and Lake Wisola becomes drainless.
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Publication 2023
Compounds, Nitrogen Compounds, Phosphorus Eutrophication Nitrogen Oxygen Oxygen Saturation Phosphorus Pulp Canals Sewage Sulfates, Inorganic Susceptibility, Disease Urban Development
Life cycle assessment (LCA) is the methodology identified by the European Commission for measuring and evaluating the environmental impacts connected to the life cycle of a product, such as global warming, ozone depletion, smog creation, eutrophication, acidification, toxicity, and resource depletion [35 (link)]. Global warming is the main impact category used, representing the climate change impact caused by human activities [36 ].
In the last few decades, LCA analysis has been applied in many areas, including the agri-food industry. However, few studies have focused on beekeeping supply chains [37 (link),38 ], and their results were closely linked to honey yield.
The methodology applied in the present study was based on Pignagnoli et al. [39 (link)], with some important advances concerning the database used, data collection, and calculations.
The analysis considered two productive seasons in order to increase the robustness of the results and provide more information about beekeeping production, taking into account some climate parameters. The 2020 original case study was performed ex novo, given that a new hypothesis was taken into consideration.
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Publication 2023
Climate Climate Change Europeans Eutrophication Honey Impacts, Environmental Ozone Depletion Smog
Sanabria Lake is situated in the NW of Spain (42 7′30″ N, 06 3′00″ W) between the provinces of León and Zamora at an altitude of 1004.1 m above sea level. It was formed by glacial erosion after the Würm glaciation in the Pleistocene, and it is the only lake formed by a terminal moraine in the Iberian Peninsula57 . Sanabria Lake belongs to the Duero River Basin that has a total drainage surface of 127.3 km258 and its main tributary is the Tera River. The surface of the lake is 3.46 km258 . It is divided longitudinally into two basins, one in the west with maximum depth of 46 m and another in the east with maximum depth of 51 m48 . The shoreline length is 9518 m and the maximum width is observed in the eastern basin (1530 m)48 . Regarding its mixing characteristics, Sanabria Lake is a warm, monomictic, holomictic lake56 (link). The mixing period extends from late November to early March, when a thermocline normally appears56 (link). No anoxic conditions have been observed in any layer of the water column during the thermal stratification54 (link),56 (link),58 . Sanabria Lake is considered as oligotrophic to oligomesotrophic in view of its low levels of chlorophyll a, nutrient concentration, phytoplanktonic biovolume values and production rates50 (link),54 (link)–56 (link),58 . The oligotrophic state of the lake is a result of its geology. Its drainage basin runs over an acid rock substrate (gneiss and granodiorites) of low solubility, making the water very poor in salts59 . The lake is part of the Sanabria Lake Natural Park (BOE 1978), a protected area that supports a population of 2 small villages (~ 200 residents), one in the north and the other in the west side of the lake. During the summer, the National Park receives a high influx of tourists and there are three camping sites, all located on the east side of the lake. Since 2012, the Duero International Biological station has raised concerns that Sanabria Lake is undergoing an eutrophication process due to contamination from a deficient sewage depuration system60 . However, studies based on pigment measurements and microscopy observation of the phytoplankton community do not support the eutrophication scenario and confirm the current oligotrophic state of the lake54 (link),55 (link).
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Publication 2023
Acids Anoxia Biopharmaceuticals Chlorophyll A Drainage Eutrophication Microscopy Nutrients Phytoplankton Pigmentation Rivers Sewage

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More about "Eutrophication"

Eutrophication, the excessive enrichment of aquatic ecosystems with nutrients like nitrogen and phosphorus, can lead to rapid algal growth, oxygen depletion, and water quality degradation.
This complex environmental phenomenon has far-reaching consequences, impacting aquatic biodiversity, human health, and economic activities.
Understanding and managing eutrophication is crucial for sustainable water resource management.
PubCompare.ai, an AI-powered platform, can optimize eutrophication research by helping researchers locate the best protocols from literature, preprints, and patents, while enhancing reproducibility and accuracy through intelligent comparisons.
This streamlines the research process and delivers enhanced results.
Eutrophication research often utilizes tools like SPSS (Statistical Package for the Social Sciences) v20 and SPSS Statistics 19 for statistical analysis, Axio Observer Z1 for microscopic observations, Spectroquant NOVA 60 for water quality measurements, and Origin 8.0 for data visualization and analysis.
PubCompare.ai can integrate with these tools, providing a comprehensive solution for eutrophication research.
By leveraging the insights from MeSH term descriptions and metadescriptions, researchers can explore the full scope of eutrophication, including related terms like nutrient enrichment, algal blooms, hypoxia, and aquatic ecosystem degradation.
This holistic approach, combined with the capabilities of PubCompare.ai, empowers researchers to achieve enhanced results in their eutrophication studies.