Bulk Atmospheric Deposition in the Southern Po Valley (Northern Italy)
A study on pH and chemical composition of precipitation was carried out in two Italian sites, one urban (site 1) and one rural (site 2), located approximately 30 km far from Bologna, during a 3-year period. No significative site variation was found. In both locations, bulk deposition pH ranged from...
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| creator | Pieri, Linda Matzneller, Philipp Gaspari, Nicola Marotti, Ilaria Dinelli, Giovanni Rossi, Paola |
| description | A study on pH and chemical composition of precipitation was carried out in two Italian sites, one urban (site 1) and one rural (site 2), located approximately 30 km far from Bologna, during a 3-year period. No significative site variation was found. In both locations, bulk deposition pH ranged from slightly acid to slightly alkaline, despite the volume weighted mean concentration of acidic species, NO ₃ ⁻ and SO ₄ ²⁻ (67.4 and 118.4 μeq l⁻¹ in site 1 and 88.7 and 103.8 μeq l⁻¹ in site 2), that were similar to those of typical acidic rainfall region. This might be ascribed to the neutralization reaction of the Ca²⁺, attributed to the calcareous soil and the frequent dusty air mass intrusion from the Sahara. The pair correlation matrix and the analysis of the main components suggested also ammonium and other crustal elements as neutralization agents. The depositional rate of SO ₄ ²⁻ and NO ₃ ⁻ , chemical elements of agricultural interest, amounted to 38 and 28 and 32 and 35 kg ha⁻¹ for site 1 and site 2, respectively. These supplies of nutrient were not negligible and had to be considered on cultivated lands. NH ₄ ⁺ deposition rate on site 2 was 7 kg ha⁻¹, 23% over site 1, probably due to nitrogen fertilization in the fields around the monitoring station. In site 1, SO ₄ ²⁻ presented a seasonal trend, indicating that its principal source was the residential heating. Results emphasized that the entity of the bulk deposition acidification is linked not only to the ions local emission sources (fossil fuel combustions, heating, and fertilizers) but also to the surrounding territory and the prevalent wind that transports through kilometers air masses which may contain acidic and alkaline species. |
| doi_str_mv | 10.1007/s11270-009-0238-y |
| format | Article |
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No significative site variation was found. In both locations, bulk deposition pH ranged from slightly acid to slightly alkaline, despite the volume weighted mean concentration of acidic species, NO ₃ ⁻ and SO ₄ ²⁻ (67.4 and 118.4 μeq l⁻¹ in site 1 and 88.7 and 103.8 μeq l⁻¹ in site 2), that were similar to those of typical acidic rainfall region. This might be ascribed to the neutralization reaction of the Ca²⁺, attributed to the calcareous soil and the frequent dusty air mass intrusion from the Sahara. The pair correlation matrix and the analysis of the main components suggested also ammonium and other crustal elements as neutralization agents. The depositional rate of SO ₄ ²⁻ and NO ₃ ⁻ , chemical elements of agricultural interest, amounted to 38 and 28 and 32 and 35 kg ha⁻¹ for site 1 and site 2, respectively. These supplies of nutrient were not negligible and had to be considered on cultivated lands. NH ₄ ⁺ deposition rate on site 2 was 7 kg ha⁻¹, 23% over site 1, probably due to nitrogen fertilization in the fields around the monitoring station. In site 1, SO ₄ ²⁻ presented a seasonal trend, indicating that its principal source was the residential heating. 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No significative site variation was found. In both locations, bulk deposition pH ranged from slightly acid to slightly alkaline, despite the volume weighted mean concentration of acidic species, NO ₃ ⁻ and SO ₄ ²⁻ (67.4 and 118.4 μeq l⁻¹ in site 1 and 88.7 and 103.8 μeq l⁻¹ in site 2), that were similar to those of typical acidic rainfall region. This might be ascribed to the neutralization reaction of the Ca²⁺, attributed to the calcareous soil and the frequent dusty air mass intrusion from the Sahara. The pair correlation matrix and the analysis of the main components suggested also ammonium and other crustal elements as neutralization agents. The depositional rate of SO ₄ ²⁻ and NO ₃ ⁻ , chemical elements of agricultural interest, amounted to 38 and 28 and 32 and 35 kg ha⁻¹ for site 1 and site 2, respectively. These supplies of nutrient were not negligible and had to be considered on cultivated lands. NH ₄ ⁺ deposition rate on site 2 was 7 kg ha⁻¹, 23% over site 1, probably due to nitrogen fertilization in the fields around the monitoring station. In site 1, SO ₄ ²⁻ presented a seasonal trend, indicating that its principal source was the residential heating. Results emphasized that the entity of the bulk deposition acidification is linked not only to the ions local emission sources (fossil fuel combustions, heating, and fertilizers) but also to the surrounding territory and the prevalent wind that transports through kilometers air masses which may contain acidic and alkaline species.</description><subject>Acid rain</subject><subject>Acidic soils</subject><subject>Acidification</subject><subject>Air masses</subject><subject>Ammonium</subject><subject>Analysis</subject><subject>Applied sciences</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Calcareous soils</subject><subject>Chemical elements</subject><subject>Climate Change/Climate Change Impacts</subject><subject>Cultivated lands</subject><subject>Earth and Environmental Science</subject><subject>Electrolytes</subject><subject>Environment</subject><subject>Environmental monitoring</subject><subject>Exact sciences and 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chemical composition of precipitation was carried out in two Italian sites, one urban (site 1) and one rural (site 2), located approximately 30 km far from Bologna, during a 3-year period. No significative site variation was found. In both locations, bulk deposition pH ranged from slightly acid to slightly alkaline, despite the volume weighted mean concentration of acidic species, NO ₃ ⁻ and SO ₄ ²⁻ (67.4 and 118.4 μeq l⁻¹ in site 1 and 88.7 and 103.8 μeq l⁻¹ in site 2), that were similar to those of typical acidic rainfall region. This might be ascribed to the neutralization reaction of the Ca²⁺, attributed to the calcareous soil and the frequent dusty air mass intrusion from the Sahara. The pair correlation matrix and the analysis of the main components suggested also ammonium and other crustal elements as neutralization agents. The depositional rate of SO ₄ ²⁻ and NO ₃ ⁻ , chemical elements of agricultural interest, amounted to 38 and 28 and 32 and 35 kg ha⁻¹ for site 1 and site 2, respectively. These supplies of nutrient were not negligible and had to be considered on cultivated lands. NH ₄ ⁺ deposition rate on site 2 was 7 kg ha⁻¹, 23% over site 1, probably due to nitrogen fertilization in the fields around the monitoring station. In site 1, SO ₄ ²⁻ presented a seasonal trend, indicating that its principal source was the residential heating. Results emphasized that the entity of the bulk deposition acidification is linked not only to the ions local emission sources (fossil fuel combustions, heating, and fertilizers) but also to the surrounding territory and the prevalent wind that transports through kilometers air masses which may contain acidic and alkaline species.</abstract><cop>Dordrecht</cop><pub>Dordrecht : Springer Netherlands</pub><doi>10.1007/s11270-009-0238-y</doi><tpages>15</tpages></addata></record> |
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| subjects | Acid rain Acidic soils Acidification Air masses Ammonium Analysis Applied sciences Atmospheric Protection/Air Quality Control/Air Pollution Calcareous soils Chemical elements Climate Change/Climate Change Impacts Cultivated lands Earth and Environmental Science Electrolytes Environment Environmental monitoring Exact sciences and technology Fertilization Fertilizers Fossil fuels Heating Hydrogeology Neutralization Nitrates Pollution Polyethylene Potassium Precipitation Rain Rain and rainfall Rural areas Soil Science & Conservation Sulfates Water Quality/Water Pollution |
| title | Bulk Atmospheric Deposition in the Southern Po Valley (Northern Italy) |
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