Open AccessA new method for in situ soil gas diffusivity measurement and applications in the monitoring of subsurface CO 2 production
Author(s) -
Risk David,
Kellman Lisa,
Beltrami Hugo
Publication year - 2008
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2007jg000445
Subject(s) - thermal diffusivity , soil water , soil gas , soil science , environmental science , water content , moisture , subsurface flow , soil horizon , in situ , hydrology (agriculture) , geology , mineralogy , materials science , chemistry , groundwater , geotechnical engineering , physics , quantum mechanics , composite material , organic chemistry
Subsurface approaches to soil CO 2 monitoring are becoming increasingly important for process studies in terrestrial carbon research. When used in conjunction with a diffusion model to determine CO 2 production, subsurface methods require good estimates of effective soil gas diffusivity (D e ). Outlined here is a novel membrane probe and continuous flow system for in situ soil gas diffusivity measurements. Laboratory tests confirm performance across the range of CO 2 diffusivities found in natural soils. Field tests were performed across a range of soil moisture contents by artificially hydrating eight soils over a period of three to seven days. These soils were representative of a range of textural classes in eastern Nova Scotia, Canada. The absolute values of diffusivity, and also the rate at which diffusivity decreased with increasing soil moisture content were typically quite different from model predictions. When applied to subsurface CO 2 monitoring at two sites, the site‐specific diffusivity measurements greatly improved the accuracy of CO 2 production estimates. We observed a consistent and close correspondence between calculated profile CO 2 production and (independently measured) soil CO 2 surface flux. The subsurface CO 2 production estimates acquired using in situ gas diffusivity measurements allows detailed vertical profile resolution to be constructed over time. The majority of CO 2 was generated at shallow depths, but periodic contributions from deeper depths were important, particularly towards the end of the growing season.