In situ efficiency of ion exchange resins in studies of nitrogen transformation

Authors
Citation
Oj. Kjonaas, In situ efficiency of ion exchange resins in studies of nitrogen transformation, SOIL SCI SO, 63(2), 1999, pp. 399-409
Citations number
39
Categorie Soggetti
Environment/Ecology
Journal title
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL
ISSN journal
03615995 → ACNP
Volume
63
Issue
2
Year of publication
1999
Pages
399 - 409
Database
ISI
SICI code
0361-5995(199903/04)63:2<399:ISEOIE>2.0.ZU;2-O
Abstract
Mixed-bed ion-exchange resin bags have previously been used in studies of s oil N transformation rates with NH4-N and NO3-N being adsorbed From the sol ution percolating through the incubated soil core. An evaluation of the in situ adsorption efficiency of mixed-bed resin bags was performed by compari ng dissolved inorganic nitrogen (DIN, sum of NH4-N + NO3-N) accumulated in resins with DIN fluxes in throughfall (TF) and with DW concentrations in so il water. A significant correlation was found between DIN fluxes in TF and accumulated DIN in resins placed at the soil surface (r(2) = 0.92 for NO3-N , r(2) = 0.86 for NH4-N, P < 0.001). The ratio of accumulated DIN in resins to DIN flux in TF was significantly affected by season. A low but signific ant correlation was found between NO3-N concentrations in soil water and NO 3-N contents in resins deployed in the bottom of soil cylinders (r(2) = 0.3 4, P < 0.01), however, when only the winter periods were taken into account , the correlation improved (r(2) = 0.72, P < 0.001), As little water and fe w nutrients are removed from the soil water by the vegetation during the do rmant season, the conditions inside and outside the core were more comparab le, For NH4-N there was no correlation between accumulated amounts in the r esins and concentrations in soil water sampled at depths of 13 cm and 20 cm , respectively, probably due to the strong depth gradient in the NH4-N conc entrations of the soil, Although the resin bags were unable to adsorb all t he incoming DIN, they gave valuable information on smalt-scale input of N a nd on small-scale differences in NO3-N leaching.