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A Proposed method to estimate in situ dissolved gas concentrations in gas-saturated groundwater

Tamamura, Shuji*; Miyakawa, Kazuya   ; Aramaki, Noritaka*; Igarashi, Toshifumi*; Kaneko, Katsuhiko*

Groundwater saturated with gas forms bubble under atmospheric pressure, bothering most authorized methods to determine in-situ dissolved gas concentrations. To circumvent this problem, a simple theory to quantify effect of $rm bubble formation on in-situ dissolved gas concentration was developed: Pressure ({it P$_{i},rm original $}$ [bar]) of a gas component "${it i}$" (e.g., CH$$_{4}$$, CO$$_{2}$$ and H$$_{2}$$) in equilibrium with in-situ dissolved concentration (${it C $_{i},rm original $}$ [mol L $$^{-1}$$]) was related to partial pressure of the $rm bubble ({it P $_{i},rm bubble $}$ [bar]) emerged from groundwater in the form: ${it P$_{i},rm original $}$ = ${it P $_{i},rm bubble $}$ + $$Delta$$ ${it P}$ (k${it i}$' ${it P $_{i},rm bubble $}$/($$Sigma$$ ${it j}$k${it j}$' ${it P $_{ j },rm bubble $}$)), where $$Delta$$ ${it P}$ [bar] is groundwater pressure difference before and after the $rm bubble formation, and j refers to all gas components in the system including "{it i.}$" The k${it $_{i}$}$' and k${it $_{j}$}$' corresponds to the Henry's constant [bar L mol$$^{-1}$$] of ${it i}$ (k${it $_{i}$}$) and ${it j}$ (k${it $_{j}$}$), respectively, except for k$$_{CO2}$$', which is pH-dependent function. Dissolved CH$$_{4}$$ concentrations were successfully estimated by the model within the error of $$pm$$ 4.0% from the direct measurements by the sealed sampler method. Similar TIC concentration in the groundwater before and after the rm bubble formation was consistent with the model prediction. The wide application of the model is suggested without selecting sampling locations.

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