The Lago Maggiore watershed is the area most affected by acid deposition in Italy. Trend analysis was performed on some long-term (15-30 years) series of chemical analyses of atmospheric deposition, four small rivers draining forested catchments and four high mountain lakes. An improvement in the quality of atmospheric deposition was detected, due to decreasing sulphate concentration and increasing pH values. Similar trends were also found in high mountain lakes and in small rivers. However, atmospheric deposition is still carrying a huge, steady flux of nitrogen compounds (nitrate and ammonium), which is causing increasing nitrogen saturation in forest ecosystems and increasing nitrate levels in rivers. Besides atmospheric deposition, an important factor controlling water acidification and recovery is the weathering of rocks and soils, which may be influenced by climate warming. A further factor is the episodic deposition of Saharan calcareous dust, which contributes significantly to base cation deposition.

Trends in the chemistry of atmospheric deposition and surface waters in the Lago Maggiore watershed

Rogora M;Marchetto A;Mosello R
2001

Abstract

The Lago Maggiore watershed is the area most affected by acid deposition in Italy. Trend analysis was performed on some long-term (15-30 years) series of chemical analyses of atmospheric deposition, four small rivers draining forested catchments and four high mountain lakes. An improvement in the quality of atmospheric deposition was detected, due to decreasing sulphate concentration and increasing pH values. Similar trends were also found in high mountain lakes and in small rivers. However, atmospheric deposition is still carrying a huge, steady flux of nitrogen compounds (nitrate and ammonium), which is causing increasing nitrogen saturation in forest ecosystems and increasing nitrate levels in rivers. Besides atmospheric deposition, an important factor controlling water acidification and recovery is the weathering of rocks and soils, which may be influenced by climate warming. A further factor is the episodic deposition of Saharan calcareous dust, which contributes significantly to base cation deposition.
2001
Istituto di Ricerca Sulle Acque - IRSA
Istituto di Ricerca sugli Ecosistemi Terrestri - IRET
trend
atmospheric depositi
nitrogen
stream water chemist
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/30441
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