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Direct measurement of atmospheric dry deposition to natural surfaces in a semiarid region of north central India

2003; American Geophysical Union; Volume: 108; Issue: D20 Linguagem: Inglês

10.1029/2002jd003194

2156-2202

Ranjit Kumar, Abha Rani, K. Maharaj Kumari, S. S. Srivastava,

Atmospheric Ozone and Climate

Dry deposition flux of major ions (Na + , K + , Ca 2+ , Mg 2+ , NH 4 + , F − , Cl − , NO 3 − and SO 4 2− ) to natural surfaces e.g., leaf of Ashok ( Polyalthia longifolia ) and Cassia ( Cassia siamea ), were determined at Dayalbagh, a suburban site of semiarid region. Dry deposition flux was highest for Ca 2+ on both Ashok and Cassia while lowest for Na + on Ashok leaf and F − on Cassia leaf. Overall average dry deposition fluxes varied from 0.27 mg m −2 d −1 to 3.98 mg m −2 d −1 . The deposition was comparatively higher to Cassia leaf than Ashok. The high deposition flux to Cassia leaf may be due to surface roughness as shown by scanning electron micrographs. The sum of major cations (Na + , K + , Ca 2+ , Mg 2+ ) and NH 4 + was higher than sum of major anions (F − , Cl − , NO 3 − and SO 4 2− ). It indicates that dry deposition at present site is alkaline in nature and difference in the sum of major cations and major anions might be due to unmeasured carbonate and bicarbonate ions as well as organic anions (formate and acetate). Deposition flux of SO 4 2− and NO 3 − is relatively lower than Ca 2+ and Mg 2+ . Seasonally dry deposition fluxes were higher in monsoon or summer for cationic species while for anionic species fluxes were higher in winter or monsoon. Average dry deposition velocity of major ions on Ashok and Cassia leaf varied from 0.41 to 2.36 cm s −1 , while seasonally values varied from 0.32 to 4.04 cm s −1 . The variation in deposition velocity may be due to meteorological conditions and surface characteristics.