An introduction to heat transfer

Estimates of the amount of water outgassed from Mars, based on the composition of the atmosphere, range from 6 to 160 m, as compared with 3 km for the Earth. In contrast, large flood features, valley networks, and several indicators of ground ice suggest that at least 500 m of water have outgassed. The two sets of estimates may be reconciled if early in its history, Mars lost part of its atmosphere by impact erosion and hydrodynamic escape.

Water on Mars

Introduction to heat transfer

Pulse and pulse reverse plating—Conceptual,advantages and applications

Giant magnetoresistance (GMR) is observed in a new type of nanostructured material consisting of magnetic multilayered nanowires formed by electrodeposition into nanometer-sized pores of a template polymer membrane. The composition of these nanowires is modulated over nanometer length scales with distinct magnetic and nonmagnetic metallic layers. Magnetoresistance measurements with the current perpendicular to the layers were performed on the array of parallel nanowires. GMR of about 15% was observed at room temperature on Co/Cu multilayered nanowires. (C) 1994 American Institute of Physics.

Giant magnetoresistance in magnetic multilayered nanowires

Experimental investigations in a recirculating wind tunnel of the mechanisms of formation of accretionary lapilli have demonstrated that growth is controlled by collision of liquid-coated particles, due to differences in fall velocities, and binding as a result of surface tension forces and secondary mineral growth. The liquids present on particle surfaces in eruption plumes are acid solutions stable at ≪ 100% relative humidity, from which secondary minerals, e.g. calcium sulphate and sodium chloride, precipitate prior to impact of accretionary lapilli with the ground. Concentric grain-size zones within accretionary lapilli build up due to differences in the supply of particular particle sizes during aggregate growth. Accretionary lapilli do not evolve by scavenging of particles by liquid drops followed by evaporation — a process which, in wind tunnel experiments, generates horizontally layered hemispherical aggregates. Size analysis of particles in the wind tunnel air stream and particles adhering to growing aggregates demonstrate that the aggregation coefficient is highly grain-size dependent. Theoretical simulation of accretionary lapilli growth in eruption plumes predicts maximum sizes in the range 0.7–20 mm for ash cloud thicknesses of 0.5–10 km respectively.

The origin of accretionary lapilli

THE aggregation of fine ash particles has an important role in controlling the deposition of widely dispersed volcanic ash. Here we report measurements of electrical charge on ash particles falling from the eruption columns of Sakurajima volcano in Japan. Absolute charge to mass (q/m) ratios ranged from +3 to +6x10-4C kg-1 and from -2 to -5 x 10-4 C kg-1. The average q/m ratio ranged from +2 to +5x10-5 C kg-1. The generation of electrostatic charge may result from triboelectric effects in the plume, or from fracture-induced charging. Charge on ash particles provides attractive forces large enough to cause the aggregation of smaller particles and the adhesion of dust to larger particles. Particle aggregation may explain the polymodal grain-size distributions commonly found in ash-fall deposits, and the proximal deposition of fine ash, as well as the distal deposition of coarse particles in these deposits. Our data suggest that electrostatic effects greatly influence the dispersal and deposition of ash during explosive volcanic eruptions.

Charge measurements on particle fallout from a volcanic plume

We have observed ‘‘giant magnetoresistance’’ in short‐period Cu/Co‐Ni‐Cu alloy superlattices electrodeposited from a single electrolyte under potentiostatic control. The superlattices were grown on polycrystalline Cu substrates which were removed before transport measurements were made. Room‐temperature magnetoresistances of over 15% in applied magnetic fields of up to 8 kOe were observed in superlattices having Cu layer thicknesses of less than 10 A.

Giant magnetoresistance in electrodeposited superlattices

Pressure changes associated with the ascent and bursting of gas slugs in liquid-filled vertical and inclined conduits.

Seismic signals generated during the flow and degassing of low-viscosity magmas include long-period (LP) and very-long-period (VLP) events, whose sources are often attributed to dynamic fluid processes within the conduit. We present the results of laboratory experiments designed to investigate whether the passage of a gas slug through regions of changing conduit diameter could act as a suitable source mechanism. A vertical, liquid-filled glass tube featuring a concentric diameter change was used to provide canonical insights into potentially deep or shallow seismic sources. As gas slugs ascend the tube, we observe systematic pressure changes varying with slug size, liquid depth, tube diameter, and liquid viscosity. Gas slugs undergoing an abrupt flow pattern change upon entering a section of significantly increased tube diameter induce a transient pressure decrease in and above the flare and an associated pressure increase below it, which stimulates acoustic and inertial resonant oscillations. When the liquid flow is not dominantly controlled by viscosity, net vertical forces on the apparatus are also detected. The net force is a function of the magnitude of the pressure transients generated and the tube geometry, which dictates where, and hence when, the traveling pressure pulses can couple into the tube. In contrast to interpretations of related volcano-seismic data, where a single downward force is assumed to result from an upward acceleration of the center of mass in the conduit, our experiments suggest that significant downward forces can result from the rapid deceleration of relatively small volumes of downward-moving liquid.

https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005JB003718

Stephen Lane

Papers

The origin of accretionary lapilli

Charge measurements on particle fallout from a volcanic plume

Giant magnetoresistance in electrodeposited superlattices

Pressure changes associated with the ascent and bursting of gas slugs in liquid-filled vertical and inclined conduits.

Gas slug ascent through changes in conduit diameter: Laboratory insights into a volcano‐seismic source process in low‐viscosity magmas