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

<strong>Table 1:</strong> Summary of all input values in the seismic attenuation model. <em>P</em> = pressure; <em>beta</em> = bubble volume fraction; <em>r</em> = bubble radius; <em>H₂O_melt</em> = water dissolved in the melt; <em>rho_melt</em> = melt density; <em>eta_melt</em> = melt viscosity; <em>deltaP_g</em> = gas overpressure;<em> H</em> = Henry’s law solubility constant; <em>DH₂O</em> = water diffusivity. <strong>ACKNOWLEDGEMENTS</strong> 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. <strong>REFERENCES</strong> Burnham, C.W., 1975. Water and magmas: a mixing model. Geochim. Cosmochim. Acta, 39, 1077–1084. Giordano, D., Russell, J.K., Dingwell, D.B., 2008. Viscosity of magmatic liquids: a model. Earth Planet. Sci. Lett., 271, 123–134. Lange, R.A., Carmichael, I.S.E., 1987. Densities of Na₂O-K₂O-CaO-MgO-FeO-Fe₂O₃-Al₂O₃-TiO₂-SiO₂ liquids: New measurements and derived partial molar properties. Geochim. Cosmochim. Acta, 51, 2931–2946. Pistone, M., Caricchi, L., Fife, J.L., Mader, K., Ulmer, P., 2015. In situ X-ray tomographic microscopy observations of vesiculation of bubble-free and bubble-bearing magmas. Bull. Volcanol., 77, doi:10.1007/s00445-015-0992-1. Pitzer, K.S., Sterner, S.M., 1994. Equations of state valid continuously from zero to extreme pressures for H₂O and CO₂. J. Chem. Phys., 101, 3111–3116. Ni, H., Zhang, Y., 2008. H₂O diffusion models in rhyolitic melt with new high pressure data. Chem. Geol., 250, 68–78.**表1：** 地震衰减模型（seismic attenuation model）中所有输入参数汇总。*P* = 压力；*β* = 气泡体积分数；*r* = 气泡半径；*H₂O_melt* = 熔体中溶解的水；*ρ_melt* = 熔体密度；*η_melt* = 熔体黏度；*ΔP_g* = 气体超压；*H* = 亨利定律溶解度常数（Henry’s law solubility constant）；*D_H₂O* = 水扩散系数。 **致谢** 本研究得到瑞士国家科学基金会（Swiss National Science Foundation）资助：项目编号200020–120221授予P.U.，项目编号P3000P2_154574、PZ00P2_16816及UGA校长基金授予M.P.。J.L.F.感谢CCMX为激光加热系统的研发提供资助。我们致谢如下：PSI提供瑞士光源（SLS）TOMCAT光束线的同步辐射束流时间；G. Mikuljan（PSI）、U. Graber（苏黎世联邦理工学院ETH–Zurich）、B. Putlitz（洛桑大学UNIL）提供技术支持；V. Lyakhovsky与O. Lamb对本文稿进行审阅分析；以及C. Huber负责编辑统筹工作。本研究生成的数据已汇总于各图表与表格中。M.P.、J.L.F.、L.C.、E.R.、P.U.与F.M.开展了实验室实验。N.T.设计了本地震衰减模型。量化信息最终由M.P.、K.M.、J.L.F.与N.T.敲定。全体作者均参与了本文稿的撰写，并声明无利益冲突。 **参考文献** Burnham, C.W., 1975. 水与岩浆：混合模型. 《地球化学与宇宙化学学报》（Geochim. Cosmochim. Acta）, 39, 1077–1084. Giordano, D., Russell, J.K., Dingwell, D.B., 2008. 岩浆液体黏度模型. 《地球与行星科学通讯》（Earth Planet. Sci. Lett.）, 271, 123–134. Lange, R.A., Carmichael, I.S.E., 1987. Na₂O-K₂O-CaO-MgO-FeO-Fe₂O₃-Al₂O₃-TiO₂-SiO₂体系液体的密度：新测量结果与导出的偏摩尔性质. 《地球化学与宇宙化学学报》（Geochim. Cosmochim. Acta）, 51, 2931–2946. Pistone, M., Caricchi, L., Fife, J.L., Mader, K., Ulmer, P., 2015. 无气泡与含气泡岩浆脱气的原位X射线断层显微观测. 《火山学通报》（Bull. Volcanol.）, 77, doi:10.1007/s00445-015-0992-1. Pitzer, K.S., Sterner, S.M., 1994. H₂O与CO₂从常压到极端压力下连续适用的状态方程. 《化学物理学报》（J. Chem. Phys.）, 101, 3111–3116. Ni, H., Zhang, Y., 2008. 流纹岩熔体中的H₂O扩散模型及新高压数据. 《化学地质学》（Chem. Geol.）, 250, 68–78.