THE EFFECTS OF AMMONIUM-SULFATE DEPOSITION AND ROOT SINKS ON SOIL SOLUTION CHEMISTRY IN CONIFEROUS FOREST SOILS

Citation
M. Carnol et al., THE EFFECTS OF AMMONIUM-SULFATE DEPOSITION AND ROOT SINKS ON SOIL SOLUTION CHEMISTRY IN CONIFEROUS FOREST SOILS, Biogeochemistry, 38(3), 1997, pp. 255-280
Citations number
36
Categorie Soggetti
Environmental Sciences","Geosciences, Interdisciplinary
Journal title
ISSN journal
01682563
Volume
38
Issue
3
Year of publication
1997
Pages
255 - 280
Database
ISI
SICI code
0168-2563(1997)38:3<255:TEOADA>2.0.ZU;2-S
Abstract
The effects of enhanced (NH4)(2)SO4 deposition on soil solution cation and anion concentrations and annual ionic fluxes were followed using a standardised experimental protocol in six European coniferous forest s with contrasting soil types, pollution inputs and climate. Native so il cores containing a ceramic suction cup were installed in the field, roofed and watered every two weeks with local throughfall or local th roughfall with added (NH4)(2)SO4 at 75 kg NH4+-N ha(-1) a(-1). Living root systems were established in half of the lysimeters. Untreated thr oughfall NH4+-N deposition at the sites ranged from 3.7 to 29 kg ha(-1 ) a(-1). Soil leachates were collected at two weekly intervals over 12 months and analysed for volume, and concentrations of major anions an d cations. Increases in soil solution NO3- concentrations in response to N additions were observed after 4-9 months at three sites, whilst o ne sandy soil with high C:N ratio failed to nitrify under any of the t reatments. Changes in NO3- concentrations in soil solution controlled soil solution cation concentrations in the five nitrifying soils, with Al3+ being the dominant cation in the more acid soils with low base s aturation. The acidification responses of the soils to the (NH4)(2)SO4 additions were primarily related to the ability of the soils to nitri fy the added NH4+. pH and soil texture seemed important in controlling NH4+ leaching in response to the treatments, with two less acidic, cl ay/clay loam sites showing almost total retention of added NH4+, whils t nearly 75% of the added N was leached as NH4+ at the acid sandy soil s. The presence of living roots significantly reduced soil solution NO 3- and associated cation concentrations at two of the six sites. The v ery different responses of the six soils to increased (NH4)(2)SO4 depo sition emphasise that the establishment of N critical loads for forest soils need to allow for differences in N storage. capacity and nitrif ication potential.