Soil aeration and redox potential as function of pore connectivity unravelled by X-ray microtomography imaging
Creators: name: Dorau, Kristof
name: Uteau, Daniel
name: Hövels, Maren Pia
name: Peth, Stephan
name: Mansfeldt, Tim
Publisher: name: Oxford [u.a.] : Wiley-Blackwell
Year: 2022
Subjects: subject: air-filled pore connectivity
subject: air-filled pore volume
subject: environmental monitoring
subject: image analysis
subject: redox potential
subject: soil aeration
subject: soil heterogeneity
subject: X-ray computed microtomography
subject: aeration
subject: electrode
subject: heterogeneity
subject: porosity
subject: soil surface
subject: Dewey Decimal Classification::600 | Technik::630 | Landwirtschaft, Veterinärmedizin
subject: Dewey Decimal Classification::600 | Technik::640 | Hauswirtschaft und Familienleben
subject: Dewey Decimal Classification::500 | Naturwissenschaften::550 | Geowissenschaften

description: Platinum (Pt)-tipped electrodes are frequently employed to measure the soil redox potential (EH). Thereby, the timely transition from reducing towards oxidising soil conditions is one of the most important biogeochemical changes that can occur in soil. This condition is mainly linked to the air-filled pore volume (ε) and pore geometries. However, even when the Pt electrodes are located in close vicinity to each other, EH readings behave non-uniformly, presumably due to the millimetre scaled heterogeneity of pore spaces controlling oxygen (O2) availability and transport. In this study, we examined the ε distribution and pore connectivity in the close vicinity of a Pt electrode during an artificial evaporation experiment using an undisturbed soil sample (Ah-horizon, Calcaric Gleysol). We combined physio-chemical methods with non-destructive X-ray computed microtomography (μCT) and 3D-image analysis. μCT scans were conducted at three-time points, that is, reducing conditions with EH &lt; −100 mV (CT-1), the transition from reducing towards oxidising conditions with an EH increase &gt; 5 mV h−1 (CT-2), and oxidising conditions with EH &gt; 300 mV (CT-3). We observed that the shift from reducing towards oxidising conditions took place at an air-filled porosity (εCT) of ~0.03 cm3 cm−3, which matches very with gravimetrically calculated data obtained by tensiometry of ε ~0.05 cm3 cm−3. Besides the relation of EH and ε, image analysis revealed that a connected εCT (εCT_conn) of ~0.02 cm3 cm−3 is needed to enable enhanced O2 diffusion from the soil surface towards the Pt surface and facilitate a straightforward EH response. We conclude that εCT_conn is a critical parameter to assess aeration processes in temporarily water-saturated soils to characterise a switch in redox conditions. Highlights: Usually, soil redox dynamics are related to the air-filled porosity (εCT) but here its connected portion (εCT_conn) was found more relevant. 3D X-ray computed microtomography imaging close to a redox electrode enabled us to understand the soil aeration process. Connected εCT (εCT_conn) of ~0.02 cm3 cm−3 facilitated oxidising soil conditions. εCT_conn is a critical parameter to assess the aeration process in temporarily water-saturated soils. © 2021 The Authors. European Journal of Soil Science published by John Wiley &amp; Sons Ltd on behalf of British Society of Soil Science.