… The reference pressure P 0 in a corresponds to the stagnation pressure (see text). The
reference velocity u 0 in b is 100 m s −1 , except for run D3 when it is 140 m s −1 . …

Data analysis workflows in many scientific domains have become increasingly complex and
flexible. Here we assess the effect of this flexibility on the results of functional magnetic …

… by assuming different P–T dependencies of … 3 P This form corresponds to a reduction by 7
of the number of model parameters with respect to the corresponding form adopted in Papale (…

Eruption forecasting is a major goal in volcanology. Logically, but unfortunately, forecasting
hazards related to non-magmatic unrest is too often overshadowed by eruption forecasting, …

The eruptive dynamics of volcanic systems are largely controlled by the viscosity of
deforming magma. Here we report the results of a series of high-temperature, high-pressure …

We summarize major findings and best-practice recommendations from three Volcano
Observatory Best Practices (VOBP) workshops, which were held in 2011, 2013 and 2016. The …

… The model was initialized at a set of P-T-X-redox conditions relevant to the system being
investigated, as detailed in the following. The pressure range was 0.1–200 MPa, as within …

Probabilistic characterizations of possible future eruptive scenarios at Vesuvius volcano are
elaborated and organized within a risk-based framework. In the EXPLORIS project, a wide …

… Equation (32) shows that the fugacity coefficient of a component in a gas mixture can be
determined at any P–T if we know its partial molar volume as a function of P–T, and in particular, …

… This is well illustrated by the example of Figure 2 for liquids of diopsidic composition and
P … The model predictions obtained by using the model parameters from Papale (1997) and …