2002
DOI: 10.1007/s00254-001-0484-9
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New evidence for the combined influence of vapor condensation and thermal convection on groundwater monitoring wells

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Cited by 6 publications
(5 citation statements)
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“…Free convective flows in boreholes or monitoring wells and their adulterating effects on in-situ measurements and groundwater samples were reported by Solodov et al (2002) and systematically investigated by Börner (2006, 2008). Strong convective flow within the fluid column may adversely affect fluid samples.…”
Section: Introductionmentioning
confidence: 99%
“…Free convective flows in boreholes or monitoring wells and their adulterating effects on in-situ measurements and groundwater samples were reported by Solodov et al (2002) and systematically investigated by Börner (2006, 2008). Strong convective flow within the fluid column may adversely affect fluid samples.…”
Section: Introductionmentioning
confidence: 99%
“…Rayleigh's theory is commonly used to conduct thermal stability analyses and evaluate the potential for the occurrence of thermally driven convection (or mixing) in boreholes and groundwater wells (Solodov et al 2002; Love et al 2007; Berthold and Börner 2008; Berthold 2010). Thermally driven convection occurs in vertical water columns when the thermal Rayleigh number (RaT$$ {Ra}_T $$) exceeds the critical thermal Rayleigh number (RaTC$$ {Ra}_{TC} $$; Rayleigh 1916), where a dimensionless Rayleigh number for thermal driven convection RaT$$ {Ra}_T $$ can be determined as: RaTgoodbreak=italicge(normalT)r4hvd$$ {Ra}_T=\frac{ge\left(\Delta \mathrm{T}\right){r}^4}{hvd} $$ where g$$ g $$ is the gravity acceleration (m s −2 ), e$$ e $$ is the thermal expansion coefficient of water (°K −1 ), ∆T is the temperature gradient within the well water column (°K), r$$ r $$ radius of the well water column (m), h$$ h $$ is the height of the water column (m), v is the kinematic viscosity of water (m 2 s −1 ), and d$$ d $$ is the thermal diffusivity of water (m 2 s −1 ).…”
Section: Methodsmentioning
confidence: 99%
“…Rayleigh's theory is commonly used to conduct thermal stability analyses and evaluate the potential for the occurrence of thermally driven convection (or mixing) in boreholes and groundwater wells (Solodov et al 2002;Love et al 2007;Berthold and Börner 2008;Berthold 2010). Thermally driven convection occurs in vertical water columns when the thermal Rayleigh number (Ra T ) exceeds the critical thermal Rayleigh number (Ra TC ;Rayleigh 1916), where a dimensionless Rayleigh number for thermal driven convection Ra T can be determined as:…”
Section: Dissolved Gas Concentration Estimatesmentioning
confidence: 99%
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