TY - JOUR
T1 - In situ observations of silica nanoparticle growth in geothermal brine at the Sumikawa geothermal station, Japan, by dynamic light scattering
AU - Tamura, Ryo
AU - Inoue, Hitoshi
AU - Hanajima, Eri
AU - Ikeda, Risa
AU - Osaka, Yuji
AU - Yanaze, Takumi
AU - Kusakabe, Minoru
AU - Yonezu, Kotaro
AU - Yokoyama, Takushi
AU - Tsukamoto, Katsuo
AU - Marumo, Katsumi
AU - Ueda, Akira
N1 - Publisher Copyright:
© 2018 Elsevier Ltd
PY - 2019/1
Y1 - 2019/1
N2 - Silica nanoparticle growth in geothermal brine was examined during the polymerization of silicic acid by observation with dynamic light scattering (DLS) at the Sumikawa geothermal station, examining raw (pH 6.6), pH adjusted (pH 8), and diluted brines (100 to 60%). The monosilicic acid concentration rapidly decreased over time in the raw brine but was almost constant in the samples with lower silicic acid concentrations. The average polysilicic acid particle diameter in the raw brine rapidly increased, from 1 to 6 nm, within 5 min (stage I) and then was almost constant at 7 nm for the subsequent 30 min (stage II).
AB - Silica nanoparticle growth in geothermal brine was examined during the polymerization of silicic acid by observation with dynamic light scattering (DLS) at the Sumikawa geothermal station, examining raw (pH 6.6), pH adjusted (pH 8), and diluted brines (100 to 60%). The monosilicic acid concentration rapidly decreased over time in the raw brine but was almost constant in the samples with lower silicic acid concentrations. The average polysilicic acid particle diameter in the raw brine rapidly increased, from 1 to 6 nm, within 5 min (stage I) and then was almost constant at 7 nm for the subsequent 30 min (stage II).
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U2 - 10.1016/j.geothermics.2018.10.008
DO - 10.1016/j.geothermics.2018.10.008
M3 - Article
AN - SCOPUS:85055354139
SN - 0375-6505
VL - 77
SP - 304
EP - 312
JO - Geothermics
JF - Geothermics
ER -