TY - JOUR
T1 - SO2 gas reactions with silicate glasses
AU - Renggli, Christian J.
AU - King, Penelope L.
PY - 2018
Y1 - 2018
N2 - Sulfur dioxide (SO2(g)) is an important gas species in most common volcanic settings on Earth including subduction zones (Shinohara 2013). The relative abundances of SO2(g) may vary at a volcano over time with the highest rates of SO2(g) emissions occurring during eruptive degassing and lesser amounts emitted continuously during quiescent degassing, resulting in a large total amount of SO2(g) integrated over time of the order of 10 Mt/a (McCormick et al. 2013; Shinohara 2013; Henley and Hughes 2016). Much of the emitted SO2(g) is released at high temperatures
AB - Sulfur dioxide (SO2(g)) is an important gas species in most common volcanic settings on Earth including subduction zones (Shinohara 2013). The relative abundances of SO2(g) may vary at a volcano over time with the highest rates of SO2(g) emissions occurring during eruptive degassing and lesser amounts emitted continuously during quiescent degassing, resulting in a large total amount of SO2(g) integrated over time of the order of 10 Mt/a (McCormick et al. 2013; Shinohara 2013; Henley and Hughes 2016). Much of the emitted SO2(g) is released at high temperatures
UR - http://www.scopus.com/inward/record.url?scp=85058472845&partnerID=8YFLogxK
U2 - 10.2138/rmg.2018.84.6
DO - 10.2138/rmg.2018.84.6
M3 - Article
SN - 1529-6466
VL - 84
SP - 229
EP - 255
JO - Reviews in Mineralogy and Geochemistry
JF - Reviews in Mineralogy and Geochemistry
IS - 1
ER -