Seasonal variability of NO3 - mobilization during flood events in a Mediterranean catchment: The influence of intensive agricultural irrigation
© 2014 Elsevier B.V. The temporal variability, hysteresis loops and various factors involved in the mobilization of nitrates (NO3 -) have been studied for a 3-year period at the Flumen River basin. Multivariate techniques (cluster analysis and pearson correlation matrix) were used to establish the r...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2015 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/113600 |
| Acceso en línea: | http://hdl.handle.net/10261/113600 |
| Access Level: | acceso abierto |
| Palabra clave: | Nitrate transport Hysteresis Irrigation return flows Flood events Agricultural practices |
| Sumario: | © 2014 Elsevier B.V. The temporal variability, hysteresis loops and various factors involved in the mobilization of nitrates (NO3 -) have been studied for a 3-year period at the Flumen River basin. Multivariate techniques (cluster analysis and pearson correlation matrix) were used to establish the relationship between the water discharge and NO3 - flushing, as well as to identify the agricultural and hydrometeorological parameters that influence its different mobilization trends. The relationship between changes in the NO3 - concentration (δC) and the overall dynamic of each hysteresis loop (δR) was also analyzed in order to describe the NO3 - trends according to the water discharge. A general dilution pattern of the NO3 - concentration was noted in the Flumen River with respect to the degree of water discharge caused by irrigation return flows. While fertilization increased the NO3 - concentration, the beginning of the irrigation season contributed to its dilution. However, in case of the NO3 - load, the maximum values occurred during high flow periods in the irrigation period, which suggested the influence of the irrigation flow on the NO3 - mass. The NO3 - load increased to 2753t and 1059t during the first and second phases of the study period, respectively, with an average specific yield of 1.33tkm-2 y-1. The NO3 - transport in the first phase of the study was 1722t during the irrigation season and 1031t during the non-irrigation period. Only 348t (13%) of NO3 - was exported during the flood events. However, in the course of the second phase of the study, the NO3 - load was 733t during the irrigation season and 326t during the non-irrigation period. In this case, 610t (57%) of nitrate was transported during the floods. These results revealed the clear influence of irrigation return flows on the NO3 - response in Flumen River. |
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