Trends in eutrophication research and control

Abstract

Eutrophication is the natural ageing process of lakes. It is characterized by a geologically slow shift from in-lake biological production driven by allochthonous (external to the water body) loading of nutrients, to production driven by autochthonous (in-lake) processes. This shift typically is accompanied by changes in species and biotic community composition, as an aquatic ecosystem is ultimately transformed into a terrestrial biome. However, this typically slow process can be greatly accelerated by human intervention in the natural biogeochemical cycling of nutrients within a watershed; the resulting cultural eutrophication can create conditions inimical to the continued use of the water body for humandriven economic purposes. Excessive algal and rooted plant growth, degraded water quality, extensive deoxygenation of the bottom water layers and increased fish biomass accompanied by decreased harvest quality, are some features of this process.Following the Second World War, concern with cultural eutrophication achieved an intensity that spurred a significant research effort, culminating in the identification of phosphorus as the single most significant, and controllable, element involved in driving the eutrophication process. During the late 1960s and throughout the 1970s, much effort was devoted to reducing phosphorus in wastewater effluents, primarily in the developed countries of the temperate zone. These efforts generally resulted in the control of eutrophication in these countries, albeit with varying degrees of success. The present effort in the temperate zone, comprising mostly developed nations, has now shifted to the control of diffuse sources of a broader spectrum of contaminants that impact human water use.In the developing countries of the inter-tropical zone, however, rapidly expanding populations, a growing industrial economy and extensive urbanization have only recently reached an intensity at which cultural eutrophication can no longer be ignored. Further, initial attempts at applying temperate zone control measures in this region have been largely unsuccessful. Modification of the temperate zone eutrophication paradigm will be needed, especially to address the differing climatic and hydrological conditions, if cultural eutrophication is to be contained in this region, where eutrophication-related diseases continue to be a primary cause of human distress.

Coastal nutrification in Brazil: A review of the role of nutrient excess on coral reef demise

“…A concept largely used in limnology to explain the process by which lakes gradually age and become more productive, it is characterized by a geologically slow shift from in-lake biological production driven by allochthonous (external to the water body) loading of nutrients to production driven by autochthonous (in-lake) processes (Rast and Thornton, 1996). This shift typically is accompanied by changes in species and biotic community composition as the aquatic ecosystem ultimately is transformed into a terrestrial biome.…”

“…Excessive algal and rooted plant growth, degraded water quality, extensive deoxygenation of the bottom-water layers, and increased fish biomass accompanied by decreased harvest quality are some features of this process (Rast and Thornton, 1996). Therefore, cultural or anthropogenic eutrophication may result in water quality deterioration caused by excessive plant nutrients from anthropogenic sources (Havens et al, 1996).…”

Removal of blue-green algae using the hybrid method of hydrodynamic cavitation and ozonation

“…To date, the quality of most natural waters in many developed countries has been improved from a decidedly eutrophic to a mesotrophic concentration [1,2]. However, algal blooms are increasingly severe in many developing countries [3,4] and it is necessary to remove nutrients, as well as algae, from water courses to ensure an adequate supply of drinking water, clean water for fishing and for use in industrial production.…”

Water Quality Degradation Effects on Freshwater Availability:Impacts of Human Activities

“…These contributions were even greater during flood years, such as in 1993 when Iowa (4.5 percent of the drainage basin area) contributed about 35 percent of the N flux. Hypoxia also occurs in fresh waters and has likewise been attributed to excess nutrient transport to lakes or reservoirs (Ryding and Rast, 1989;Rast and Thornton, 1996).…”