4.7 Article

Soil solution fluxes and composition trends reveal risks of nitrate leaching from forest soils of Italy

期刊

CATENA
卷 200, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.catena.2021.105175

关键词

Soil solution chemistry; Atmospheric deposition; Nitrate leaching; Forest soils; Mediterranean; Nitrogen

资金

  1. European Union under the Regulation (EC) of the European Parliament [2152/2003]
  2. European Union under the Regulation (EC) of the Council of 17 November 2003 concerning monitoring of forests and environmental interactions in the community (Forest Focus) [2152/2003]
  3. LIFE project FutMon (Further Development and Implementation of an EU-level Forest Monitoring System) [LIFE07 ENV/D/000218]
  4. LIFE project SMART4Action (Sustainable Monitoring and Reporting To Inform Forest-and Environmental Awareness and Protection) [LIFE13 ENV/IT/000813]

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Atmospheric emissions of nitrogen and sulphur have accelerated anthropogenic acidification in forest ecosystems. High nitrogen deposition in Italy has led to increased tree growth and organic carbon sequestration, but also poses risks of nutrient imbalances and soil acidification. Monitoring in Italy has shown soil solution pH increase in most sites due to decreased sulphate deposition, while nitrogen deposition impedes pH increase in some areas.
Although acidification is a natural soil formation process, atmospheric emissions of nitrogen and sulphur have exposed forest ecosystems to accelerated anthropogenic acidification for many decades. In Italy nitrogen deposition loads are high, and among the highest in Europe. Data from the Italian ICP-Forests monitoring network have shown that nitrogen deposition increases tree growth, and consequently the organic carbon sequestration. However, the accumulation of nitrogen in the ecosystem could cause nutrient imbalances and contribute to soil acidification. Within this context, we investigated the temporal changes of atmospheric deposition and soil solution concentration in the Italian ICP-Forests using the non-parametric Seasonal Mann Kendall (SMK) test. Further, we applied input-output models, to evaluate the capabilities of the soil-forest system to retain deposited nitrogen and thus protect underground waters. Increase of soil solution pH was observed in most of the sites, likely due to sulphate deposition decrease with a concomitant high and stable natural exchangeable base deposition. For the sites around the Po plain, however, high levels of nitrogen deposition impede pH increase. The site with the maximum mineral N deposition showed signs of active acidification. The analysis of the fluxes of nitrogen compounds demonstrates a complete retention of the ammonium forms, which further contribute to acidification through nitrification. Furthermore, the Italian monitoring network showed that the retention of nitrogen in the soil-forest system was effective since the observed N fluxes in mineral soil were strongly reduced compared to mineral N input in most of the plots. In spite of this, significant NO3- fluxes from the subsoil were observed in sites with high deposition, and also in the southernmost site which is exposed to relatively low mineral N loads. Drivers other than pollution should also be considered since N can follow different pathways at different time scales, influencing N leaching independently from the amount of deposition.

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