Placement of ion-exchange membranes for monitoring nutrient release from flooded soils

Placement of Plant Root Simulator (PRS®) probes (ion-exchange membranes in a plastic support) may strongly influence nutrient supply measurements and their relationship to nutrient loss to overlying water due to gradients in ion activity and redox potential with depth. A laboratory study was conduct...

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Veröffentlicht in:Canadian Journal of Soil Science 2018-12, Vol.98 (4), p.709-715
Hauptverfasser: Bremer, E, Miller, J.J, Curtis, T
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container_title Canadian Journal of Soil Science
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creator Bremer, E
Miller, J.J
Curtis, T
description Placement of Plant Root Simulator (PRS®) probes (ion-exchange membranes in a plastic support) may strongly influence nutrient supply measurements and their relationship to nutrient loss to overlying water due to gradients in ion activity and redox potential with depth. A laboratory study was conducted with two soils contrasting in potential nutrient loss (manured vs. unamended control) to determine the impact of probe placement (vertical, horizontal, and flat on the soil surface) on nutrient supply rate. The supply rates of the redox-sensitive nutrients Mn and Fe were generally 1–2 orders of magnitude lower for PRS probes placed on the soil surface than buried vertically. In contrast, the supply rate of P and K varied by 1–2 orders of magnitude between soils, but placement impacts were modest or absent. The ratio between manured and control soils in water P concentration was identical to that of soil P supply rate determined with PRS probes placed flat on the soil surface. All placements were effective in demonstrating the increased potential for loss of P and K from the manured soil, but only measurements from PRS probes placed on the soil surface were closely related to loss of the redox-sensitive nutrients Mn and Fe.
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A laboratory study was conducted with two soils contrasting in potential nutrient loss (manured vs. unamended control) to determine the impact of probe placement (vertical, horizontal, and flat on the soil surface) on nutrient supply rate. The supply rates of the redox-sensitive nutrients Mn and Fe were generally 1–2 orders of magnitude lower for PRS probes placed on the soil surface than buried vertically. In contrast, the supply rate of P and K varied by 1–2 orders of magnitude between soils, but placement impacts were modest or absent. The ratio between manured and control soils in water P concentration was identical to that of soil P supply rate determined with PRS probes placed flat on the soil surface. All placements were effective in demonstrating the increased potential for loss of P and K from the manured soil, but only measurements from PRS probes placed on the soil surface were closely related to loss of the redox-sensitive nutrients Mn and Fe.</abstract><cop>Ottawa</cop><pub>Canadian Science Publishing</pub><doi>10.1139/cjss-2018-0082</doi><tpages>7</tpages></addata></record>
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source Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Alma/SFX Local Collection
subjects Environmental monitoring
Flooded soils
Ion exchange
Iron
Manganese
manured soils
Membranes
Nutrient loss
Nutrient release
Nutrients
perte de phosphore
phosphorus loss
Placement
Plant roots
Probes
qualité de l’eau de surface
Redox potential
Soil water
sols amendés avec du fumier
surface water quality
terres humides
Water depth
wetland
title Placement of ion-exchange membranes for monitoring nutrient release from flooded soils
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