Κυριακή 3 Φεβρουαρίου 2019

Importance of root uptake of 14CO2 on 14C transfer to plants impacted by below-ground 14CH4 release

Publication date: May 2019

Source: Journal of Environmental Radioactivity, Volume 201

Author(s): Masakazu Ota, Taku Tanaka

Abstract

14C-labelled methane (14CH4) released from deep underground radioactive waste disposal facilities can be a below-ground source of 14CO2 owing to microbial oxidation of 14CH4 to 14CO2 in soils. Environmental 14C models assume that the transfer of 14CO2 from soil to plant occurs via foliar uptake of 14CO2. Nevertheless, the importance of 14CO2 root uptake is not well understood. In the present study, below-ground transport and oxidation of 14CH4 were modeled and incorporated into an existing land-surface 14CO2 model (SOLVEG-II) to assess the relative importance of root uptake and foliar uptake on 14CO2 transfer from soil to plants. Performance of the model in calculating the below-ground dynamics of 14CH4 was validated by simulating a field experiment of 13CH4 (as a substitute for 14CH4) injection into subsoil in a wheat field in the UK. The proposed model simulation was then applied to 14C transfer in a hypothetical ecosystem impacted by continuous 14CH4 input from the water table (bottom of 1-m thick soil), which simulated continuous release of 14CH4 from a deep underground radioactive waste disposal facility. The contrast between the results obtained from the model calculation that assumed different distributions of roots (rooting depths of 11 cm, or 97 cm) and methane oxidation (characterized by e-folding depths of 5 cm, 20 cm, or 80 cm) in the soil provided insight into the relative importance of root uptake and foliar uptake pathways. In the shallowly rooted ecosystem with rooting depth of 11 cm, foliar uptake of 14CO2 was significant, accounting for 80% of the 14C accumulation (as organic 14C) in the plant (leaf compartment). By contrast, in a deeply rooted ecosystem (rooting depth of 97 cm), where the root penetrated to depths close to the water-table, more than half (63%) the 14C accumulated in the plant was transferred via the root uptake pathway. We found that 14CO2 root uptake (thus 14C accumulation in the plant) in this ecosystem depended on the distribution of methane oxidation in the soil; all 14C accumulated in the plant was transferred by the root uptake pathway when methane oxidation occurred at considerable depths (e-folding depths of 20 cm, or 80 cm) in the soil. The high level of 14CO2 root uptake was ascribed to the oxidation of added 14CH4 (i.e., production of 14CO2) in the deep part of the soil and the subsequent high level of root uptake of the deep soil-water containing 14CO2. These results indicate that 14CO2 root uptake contributes significantly to 14CO2 transfer to plants if 14CH4 oxidation occurs at great depths and roots penetrate deeply into the soil. It is recommended that current environmental 14C models must be refined to consider the importance of the root uptake pathway to ensure that dose estimates of 14CH4 release from deep underground waste disposal facilities are accurate.



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