ABSTRACT
Se describe, analiza y reporta por primera vez la formación de un humedal costero en el sur de Salaverry (La Libertad, Perú). Se realiza la comparación del número de especies con otros humedales ubicados en áreas costeras de la región, empleando para ello imágenes satelitales de acceso público e información biológica. Se obtuvo una serie de tiempo suficiente para plantear una hipótesis sobre su formación, calculando el NDVI (Índice de Vegetación de Diferencia Normalizada) y NDMI (Índice de Humedad de Diferencia Normalizada) para confirmar su estabilidad e influencia. El resultado del análisis sugiere que el humedal sur de Salaverry se formó hace quince años por dos aportes antrópicos: filtraciones de agua dulces desde terrenos agrícolas y agua de mar usada para el bombeo del material dragado en las inmediaciones del Puerto de Salaverry. Por sus características ecosistémicas, el humedal se encontraría en las primeras etapas de sucesión ecológica, y a pesar de origen espontáneo, estaría operando como una laguna costera salobre que atrae fauna oportunista, principalmente aves.
The formation of a coastal wetland located south of Salaverry (La Libertad - Peru) is first described, analyzed, and reported, and their biodiversity is compared with regional wetlands located at coastal areas, using publically access satellite imagery and biological information. An adequate time-series was obtained to hypothesize their formation, calculating the NDVI (Normalized difference vegetation index) and NDMI (Normalized Difference Moisture Index) to confirm the stability and influence. The analysis suggests that the wetland south of Salaverry was formed fifteen years ago by two human sources: freshwater infiltration from farmlands and seawater used to pump the dredged material in the vicinity of the Salaverry Port. Because of its ecosystemic features, the wetland would be at the first stages of the ecological succession, and despite its spontaneous origin, it will be functioning as a brackish coastal lagoon attracting opportunistic fauna, mainly birds.
ABSTRACT
Biosolids are the product of wastewater or municipal solid waste collected through sewerage treatment; theprocesses of obtaining the biosolids involve various treatment processes, which include digestion, thermalstabilization, thickening, dewatering, and drying, in order to obtain free pathogen granules. These processesundergone by wastewater in the treatment plant ultimately clean the wastewater and remove the solids whichare further treated to an acceptable standard for beneficial soil amendments. The application of biosolids areconsidered to improve soil organic matter, moisture content, and provided essential nutrients, such as nitrogenand phosphorus in arable land as potential plant nutrients supplements for crop optimum yield. Incubationstudies on the biosolids-amended soils have shown significant increases in soil phosphorus content beingreleased as plant available P in the soil, and therefore could be a good source of phosphorus in deficientnative phosphorus soil. Field-scale experiments on wheat are grown with sewage sludge have also shown yieldproduction comparable to mineral fertilizer-treated soils. This review is thereby aimed at explaining the conceptbehind the mineralization and mobilization of biosolids phosphorus in soil. In this review paper, an overviewof the method of preparations, origin, and sources, its application in agriculture and the environment, chemicalcomposition, the environmental risk, soil amendments potentials of the biosolid sand regulatory, and globalperspective of sewage sludge disposal all are reviewed. From the review, it was concluded that mineralizationand mobilization of biosolids phosphorus in soil have beneficial input to both environment and soil nutrientamendment. It is thereby recommended that more research studies should be carried out on the mineralizationand mobilization of another essential element, such as nitrogen and biochar although more research should bedone with respect to mineralization and mobilization of biosolids phosphorus in soil.