TY - JOUR
T1 - Throughfall chemistry in Engelmann spruce - subalpine fir forest in north central Colorado
AU - Arthur, M. A.
AU - Fahey, T. J.
PY - 1993
Y1 - 1993
N2 - Higher concentrations of nutrient cations (Ca, Mg, Na, and K) were found in throughfall than in bulk precipitation, indicating canopy leaching of nutrients and dry deposition onto the canopy followed by wash-off. Ammonium was retained by the canopy. Concentrations of anions (NO3, SO4, and ortho-P) were similar in throughfall and bulk precipitation. Large additions of organic acids to throughfall from foliage were inferred from a 5-fold increase in dissolved organic carbon and a large charge-balance deficit (23%) in throughfall relative to bulk precipitation (8%). Canopy evaporation was estimated at 27%, accounting for a 37% increase in the concentration of dissolved substances in throughfall. Dry deposition resulted in large additions of most cation nutrients and N, but not SO4. Ratios of NO3 to SO4 in wet fall (0.8) and bulk precipitation (1.1) were high and result from proximity to NOx sources in the urban corridor to the east. -from Authors
AB - Higher concentrations of nutrient cations (Ca, Mg, Na, and K) were found in throughfall than in bulk precipitation, indicating canopy leaching of nutrients and dry deposition onto the canopy followed by wash-off. Ammonium was retained by the canopy. Concentrations of anions (NO3, SO4, and ortho-P) were similar in throughfall and bulk precipitation. Large additions of organic acids to throughfall from foliage were inferred from a 5-fold increase in dissolved organic carbon and a large charge-balance deficit (23%) in throughfall relative to bulk precipitation (8%). Canopy evaporation was estimated at 27%, accounting for a 37% increase in the concentration of dissolved substances in throughfall. Dry deposition resulted in large additions of most cation nutrients and N, but not SO4. Ratios of NO3 to SO4 in wet fall (0.8) and bulk precipitation (1.1) were high and result from proximity to NOx sources in the urban corridor to the east. -from Authors
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U2 - 10.1139/x93-096
DO - 10.1139/x93-096
M3 - Article
AN - SCOPUS:0027868906
SN - 0045-5067
VL - 23
SP - 738
EP - 742
JO - Canadian Journal of Forest Research
JF - Canadian Journal of Forest Research
IS - 4
ER -