2013
DOI: 10.1016/s1004-9541(13)60561-3
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Volumetric and Transport Properties of Aqueous NaB(OH)4 Solutions

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Cited by 27 publications
(47 citation statements)
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“…e calculated results in these literatures [13,14] are in agreement with those with the Pitzer model in the systems NaBO 2 −H 2 O and K 2 B 4 O 7 −H 2 O [9,10]. e concentration of boron species was calculated in references [12][13][14][15], and it was considered that the activity coefficients of all boron ions were 1.0. Although the calculation may not be correct, the calculated results can also describe the distribution of boron species in the solution.…”
Section: Introductionsupporting
confidence: 54%
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“…e calculated results in these literatures [13,14] are in agreement with those with the Pitzer model in the systems NaBO 2 −H 2 O and K 2 B 4 O 7 −H 2 O [9,10]. e concentration of boron species was calculated in references [12][13][14][15], and it was considered that the activity coefficients of all boron ions were 1.0. Although the calculation may not be correct, the calculated results can also describe the distribution of boron species in the solution.…”
Section: Introductionsupporting
confidence: 54%
“…Boron form depends on boron concentration, pH, temperature, and ionic strength [11]. With the pH values in the solution and equilibrium constant between different boron species, the distribution of boron species was calculated [12][13][14][15]. e calculated results in these literatures [13,14] are in agreement with those with the Pitzer model in the systems NaBO 2 −H 2 O and K 2 B 4 O 7 −H 2 O [9,10].…”
Section: Introductionmentioning
confidence: 69%
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“…To that end, cell-specific rates were calculated from measured AOM rates per volume of Parameters are set to baseline values if not noted otherwise. Temperature T is set to 281.15 K; Aqueous diffusion coefficient: D CO2 = 1.91 × 10 −9 m 2 s −1 , D H2 = 6.31 × 10 −8 m 2 s −1 (Schulz, 2000), D CO3 = 1.19 × 10 −9 m 2 s −1 , D H+ = 6 × 10 −9 m 2 s −1 , D OH = 5.27 × 10 −9 m 2 s −1 (Gupta et al, 2006); D B(OH)4 = 9.56 × 10 −10 m 2 s −1 (Zhou et al, 2013). sediment, combined with reported cell densities.…”
Section: Comparison Of Model Simulations To Measured Sediment Aom Ratesmentioning
confidence: 97%
“…Aqueous diffusion coefficient: D CO2 = 1.91 × 10 −9 m 2 s −1 , DnormalH2 = 6.31 × 10 −8 m 2 s −1 (Schulz, ), D CO3 = 1.19 × 10 −9 m 2 s −1 , D H+ = 6 × 10 −9 m 2 s −1 , D OH = 5.27 × 10 −9 m 2 s −1 (Gupta et al, ); D B(OH)4 = 9.56 × 10 −10 m 2 s −1 (Zhou et al, ).…”
Section: Modelling Proceduresmentioning
confidence: 99%