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Ammonium Adsorption by a Zeolite in a Static and a Dynamic System
Author(s) -
Weber M. A.,
Barbarick K. A.,
Westfall D. G.
Publication year - 1983
Publication title -
journal of environmental quality
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.888
H-Index - 171
eISSN - 1537-2537
pISSN - 0047-2425
DOI - 10.2134/jeq1983.00472425001200040023x
Subject(s) - clinoptilolite , zeolite , leaching (pedology) , ammonium , adsorption , chemistry , loam , soil water , ion exchange , inorganic chemistry , environmental chemistry , soil science , environmental science , ion , catalysis , organic chemistry
New types of soil amendments are being considered to reduce the leaching losses of N fertilizers. One such potential soil amendment is clinoptilolite, which is a natural zeolite with ion exchange properties and an affinity for the ammonium ion (NH 4 + ). The objectives of this study were to quantify the adsorption of ammonium (NH 4 ) by a clinoptilolite in a shaking study (static system) and to measure how effective this zeolite was in increasing NH 4 retention in soil leaching columns (dynamic system). A batch equilibrium shaking test showed that this zeolite adsorbed 4.3 times more NH 4 than the Nunn clay loam (Aridic Argiustoll) soil. When mixed together with the soil and placed in 6.35 cm (i.d.) by 30 cm long columns (dynamic system), the zeolite significantly reduced the leaching of NH 4 + only at a relatively high application rate (135 Mg ha −1 ). comparison of the two zeolite application methods at the highest zeolite rate (135 Mg ha −1 ) showed that banded treatments significantly reduced the leaching of NH 4 + , compared with treatments where zeolite was homogenously mixed with the entire soil volume. Indications are, however, that large quantities of clinoptilolite would be required to reduce NH 4 + leaching in fine‐textured soils.