Table 1 from GRL paper on "Seismic attenuation during magma vesiculation: A combination of laboratory constraints and modeling"

Table 1: Summary of all input values in the seismic attenuation model. P = pressure; beta = bubble volume fraction; r = bubble radius; H2Omelt = water dissolved in the melt; rhomelt = melt density; etamelt = melt viscosity; deltaPg = gas overpressure; H = Henry’s law solubility constant; DH2O = water diffusivity.

ACKNOWLEDGEMENTS

Swiss National Science Foundation grants 200020–120221 to P.U., grants P3000P2_154574 and PZ00P2_16816 and UGA Presidential Funds to M.P. supported this study. J.L.F. thanks the CCMX for funding the development of the laser-based heating system. We acknowledge: the PSI for provision of synchrotron radiation beamtime at the TOMCAT beamline of the SLS; G. Mikuljan (PSI), U. Graber (ETH–Zurich), and B. Putlitz (UNIL) for technical support; V. Lyakhovsky and O. Lamb for their review analysis of our manuscript; and C. Huber for editorial handling. The data generated in this study are summarized in figures and table. M.P., J.L.F., L.C., E.R., P.U., and F.M. carried out the laboratory experiments. N.T. designed the seismic attenuation model. The quantitative information was finalised by M.P., K.M., J.L.F., and N.T.. All authors were instrumental in the resulting manuscript and declare no conflicts of interest.

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