Exact(2)
Highest surface heat flow values correspond to the Central System and northern part of the Tajo Basin.
It has been observed that the highest surface heat transfer coefficients can be achieved using an intermediate nozzle-to-surface distance of 5 mm and a 2.8% nanoparticle volume fraction.
Similar(6)
In regions with high surface heat flow, such as areas of active volcanism or mantle upwelling beneath thinned continental crust, geothermal gradients of 40 to 100 °C (104 to 212 °F) per kilometre (0.6 mile) prevail, giving rise to high temperatures at relatively shallow levels of the crust.
Fusion reactor first wall services on the conditions of high surface heat flux and intense neutron irradiation.
This concept needs limited extrapolations from today's plasma physics assumptions insofar it allows high surface heat fluxes (up to 15 MW m−2).
Considering the high surface heat flow in this region, we infer that these low-velocity anomalies are associated with the high temperatures or partial melting at the uppermost mantle (Hearn and Ni, 1994; Hu et al., 2001).
In contrast, in the convex-downward seafloor regions, the BSR was shallower and the values were higher than those in the surrounding areas (Fig. 7), apparently because rapid erosion caused high surface heat flow values.
In a moderately interactive spacing, high surface heat fluxes are achieved, while at a large spacing, the RJRC flames operate almost independently from each other.
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