TY - JOUR
T1 - Soil solution chemistry of an Adirondack Spodosol
T2 - lysimetry and N dynamics
AU - Shepard, J. P.
AU - Mitchell, M. J.
AU - Scott, T. J.
AU - Driscoll, C. T.
PY - 1990
Y1 - 1990
N2 - Solutes were monitored from the soil of a beech-maple forest and an adjacent lake at the Huntington Forest in the Adirondack Mountains of New York. The predominant ions were Ca2+ and SO4 2-. For soil solutions collected by lysimeters, the highest concentrations of most ions (H+, K+, NH4 +, Ca2+, Mg2+, and NO3 -) occurred in O horizon leachates, and the lowest concentrations beneath the spodic B horizon. However, Al and SO4 2- concentrations were highest beneath the B horizon. Concentrations of NO3 - showed distinct seasonal variation. Values reached 60 μequiv. L-1 in the spring and decreased to near zero late in the growing season. Coefficients of variation (CV) differed among horizons. The E horizon was generally most variable (CV, 17 to 199%) and the B horizon the least (CV 19 to 166%). -from Authors
AB - Solutes were monitored from the soil of a beech-maple forest and an adjacent lake at the Huntington Forest in the Adirondack Mountains of New York. The predominant ions were Ca2+ and SO4 2-. For soil solutions collected by lysimeters, the highest concentrations of most ions (H+, K+, NH4 +, Ca2+, Mg2+, and NO3 -) occurred in O horizon leachates, and the lowest concentrations beneath the spodic B horizon. However, Al and SO4 2- concentrations were highest beneath the B horizon. Concentrations of NO3 - showed distinct seasonal variation. Values reached 60 μequiv. L-1 in the spring and decreased to near zero late in the growing season. Coefficients of variation (CV) differed among horizons. The E horizon was generally most variable (CV, 17 to 199%) and the B horizon the least (CV 19 to 166%). -from Authors
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U2 - 10.1139/x90-108
DO - 10.1139/x90-108
M3 - Article
AN - SCOPUS:0025584708
SN - 0045-5067
VL - 20
SP - 818
EP - 824
JO - Canadian Journal of Forest Research
JF - Canadian Journal of Forest Research
IS - 6
ER -