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In Situ Estimation of the Gaseous Nitrous Oxide Diffusion Coefficient in a Sandy Loam Soil
Author(s) -
Bochove Eric,
Bertrand Normand,
Caron Jean
Publication year - 1998
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1998.03615995006200050004x
Subject(s) - loam , diffusion , thermal diffusivity , porosity , soil science , gaseous diffusion , soil gas , soil water , mass diffusivity , nitrous oxide , analytical chemistry (journal) , atmosphere (unit) , chemistry , mineralogy , environmental science , thermodynamics , environmental chemistry , physics , electrode , organic chemistry
The estimation of gas exchanges with the soil is important when assessing gas emission to the atmospheric environment or gas consumption by the soil. This estimation often requires the measurement of the diffusion coefficient of the investigated gas. The aim of this study was to develop an experimental method creating limited soil disturbance and based on simple calculation procedures to determine the diffusion coefficient, D s , for N 2 O in soils. This objective was achieved using a N 2 O mass flow meter that supplied a continuous and constant flow of gas from below the soil surface until a steady‐state N 2 O concentration gradient with depth was obtained. The coefficients of diffusion were calculated daily for 6 d, under steady‐state concentration gradient, using Fick's first law. The mean value of the diffusion coefficient for N 2 O was 1.26 × 10 ‐6 m 2 s ‐1 (CV = 25%) at 0.16 m 3 m ‐3 of air‐filled porosity. This value was validated by a transient‐state laboratory method using soil cores and compared with empirical estimations of D s from air‐filled porosity determinations. The two experimental methods produced similar values for D s and both provided more accurate estimates than the empirical models. The proposed method can be applied to other gases provided an empirical model relating D s to D o (gas diffusivity in free air) is first established. A theoretical study identified the threshold air‐filled porosity values below which the flux density must be adjusted to maintain the validity of the D s calculations.