Effect of alkalis, phosphorus, and water on the surface tension of haplogranite melt

By N. Bagdassarov, A. Dorfman, Donald Bruce Dingwell. 2000

171 citations recorded by the source corpus.

Subfields: Biomedical Engineering, Geochemistry and Petrology, Water Science and Technology

View Paper: https://www.semanticscholar.org/paper/de4f90546be86a6bb135b61276ede9dbd2999f81

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Biomedical Engineering

1. O. Bachmann
2. G. Bergantz

In Geochemistry and Petrology

1. O. Bachmann
2. G. Bergantz

In Water Science and Technology

1. O. Bachmann
2. G. Bergantz

Citations in the corpus

• Gas percolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies (2006, methodology): “We, therefore, chose van Genuchten parameters that were characteristic of sandstone and scaled them using the interfacial tension value of Bagdassarov et al. (2000).”
• BND (bubble number density) decompression rate meter for explosive volcanic eruptions (2006, unknown): “Bagdassarov et al. (2000) also provide the values of dσ / dCW.”
• The rheology of two-phase magmas: A review and analysis (2013, background): “Surface tension in silicate melts is strongly dependent on dissolved water content, varying from around 0.05 Nm− 1 for hydrousmelts (Mangan and Sisson, 2005) to around 0.3 Nm−1 for anhydrous melts (Bagdassarov et al., 2000).”