EGU26-10767, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-10767
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Thursday, 07 May, 10:45–12:30 (CEST), Display time Thursday, 07 May, 08:30–12:30
 
Hall X5, X5.134
 Thermal imaging and fugitive CH4 emissions at Tenerife’s municipal solid waste landfill 
Paula Fuentes-Domínguez1,2, María Asensio-Ramos1, Ariadna E. Vidaña-Glauser1, Paola García-Luis1, Jasmina García-Báez1, Sergio González-Torres1, Víctor Ortega-Ramos1, Héctor de los Ríos-Díaz1,2, Nemesio M. Pérez1,2, Óscar Padrón1,2, Gladys V. Melián1,2, and Pedro A. Hernández1,2
Paula Fuentes-Domínguez et al.
  • 1Instituto Volcanológico de Canarias, Puerto de la Cruz, Tenerife, Canary Islands
  • 2Instituto Tecnológico y de Energías Renovables (ITER), Granadilla de Abona, Tenerife, Canary Islands

Fugitive methane (CH4) emissions from municipal solid waste landfills represent a significant and often underestimated source of greenhouse gases, particularly in complex sites with multiple cells at different operational stages. In this study, diffuse carbon dioxide (CO2) and CH4 emissions were investigated at the Tenerife municipal solid waste landfill (Canary Islands, Spain), combining ground-based flux measurements with thermal infrared imaging acquired by unmanned aerial vehicles (UAVs). 

Diffuse gas fluxes were measured using the accumulation chamber method across more than 1,700 sampling points distributed over active, sealed and closed landfill cells. CH4 emissions were quantified both directly, using an in situ CH4 sensor, and indirectly, by estimating CH4 fluxes from measured CO2 fluxes and CH4/CO2 concentration ratios in the chamber headspace. In parallel, UAV-based thermal surveys were conducted to explore surface temperature patterns and their potential relationship with diffuse gas emissions and landfill cover characteristics. 

Results show clear spatial variability in diffuse gas emissions linked to the operational status of the cells. Active and recently used cells exhibit higher and more spatially heterogeneous CH4 fluxes, while sealed and older cells are characterized by lower direct CH4 emissions but relatively higher indirect CH4 estimates. This discrepancy is attributed to CH4 oxidation and limited surface permeability, which reduce effective CH4 transfer to the atmosphere while allowing CO2 to diffuse more efficiently. 

The combined use of direct and indirect flux measurements together with thermal imaging provides complementary insights into landfill gas dynamics, allowing differentiation between effective atmospheric emissions and subsurface CH4 presence. This integrated approach improves the characterization of fugitive emissions and supports the assessment of landfill gas management efficiency. 

How to cite: Fuentes-Domínguez, P., Asensio-Ramos, M., Vidaña-Glauser, A. E., García-Luis, P., García-Báez, J., González-Torres, S., Ortega-Ramos, V., de los Ríos-Díaz, H., M. Pérez, N., Padrón, Ó., V. Melián, G., and Hernández, P. A.:  Thermal imaging and fugitive CH4 emissions at Tenerife’s municipal solid waste landfill , EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-10767, https://doi.org/10.5194/egusphere-egu26-10767, 2026.