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Here the baron interrupted him with a world of compliments and greetings, for, to tell the truth, he prided himself upon his courtesy and eloquence. The stranger attempted once or twice to stem the torrent of words, but in vain, so he bowed his head and suffered it to flow on. By the time the baron had come to a pause they had reached the inner court of the castle, and the stranger was again about to speak, when he was once more interrupted by the appearance of the female part of the family, leading forth the shrinking and blushing bride. He gazed on her for a moment as one entranced; it seemed as if his whole soul beamed forth in the gaze and rested upon that lovely form. One of the maiden aunts whispered something in her ear; she made an effort to speak; her moist blue eye was timidly raised, gave a shy glance of inquiry on the stranger, and was cast again to the ground. The words died away, but there was a sweet smile playing about her lips, and a soft dimpling of the cheek that showed her glance had not been unsatisfactory. It was impossible for a girl of the fond age of eighteen, highly predisposed for love and matrimony, not to be pleased with so gallant a cavalier.
In civilized life, where the happiness, and indeed almost the existence, of man depends so much upon the opinion of his fellow-men, he is constantly acting a studied part. The bold and peculiar traits of native character are refined away or softened down by the levelling influence of what is termed good-breeding, and he practises so many petty deceptions and affects so many generous sentiments for the purposes of popularity that it is difficult to distinguish his real from his artificial character. The Indian, on the contrary, free from the restraints and refinements of polished life, and in a great degree a solitary and independent being, obeys the impulses of his inclination or the dictates of his judgment; and thus the attributes of his nature, being freely indulged, grow singly great and striking. Society is like a lawn, where every roughness is smoothed, every bramble eradicated, and where the eye is delighted by the smiling verdure of a velvet surface; he, however, who would study nature in its wildness and variety must plunge into the forest, must explore the glen, must stem the torrent, and dare the precipice.
I mention this peaceful spot with all possible laud, for it is in such little retired Dutch valleys, found here and there embosomed in the great State of New York, that population, manners, and customs remain fixed, while the great torrent of migration and improvement, which is making such incessant changes in other parts of this restless country, sweeps by them unobserved. They are like those little nooks of still water which border a rapid stream where we may see the straw and bubble riding quietly at anchor or slowly revolving in their mimic harbor, undisturbed by the rush of the passing current. Though many years have elapsed since I trod the drowsy shades of Sleepy Hollow, yet I question whether I should not still find the same trees and the same families vegetating in its sheltered bosom.
Gold mineralisation at the Abu Marawat mine, central Eastern Desert of Egypt, is related to a system of massive and sheared, milky quartz veins cutting a sequence of Neoproterozoic island arc metavolcanic/volcaniclastic rocks and related banded iron formation (BIF). Sulphide-bearing quartz veins and related hydrothermal breccia bodies display a range of textures including sheared, boudinaged and recrystallised quartz, open space filling and microbreccia. These variable textures imply a complex history of crack-seal mechanism characterising the relation between mineral deposition and a major N-S-trending shear zone, during a late brittle-ductile deformation event which affected the area at about 550 Ma. Gold-base metal mineralisation is associated with brecciation and fracturing of the iron ore bands, close to silicified shears and related quartz veins. The auriferous quartz lodes are characterised by the occurrence of visible pyrite-chalcopyrite pyrrhotite sphalerite galena mineralisation. Gold is refractory in pyrite and chalcopyrite, but rare visible gold/electrum and telluride specks were observed in a few samples. Hydrothermal alteration includes pervasive silicification, pyritisation, sericitisation, carbonatisation confined to a delicate set of veins and altered shears, and a more widespread propylitic alteration assemblage (quartz + chlorite + pyrite + calcite epidote). Fluid inclusion petrography and microthermometric studies suggest heterogeneous trapping of a low-salinity (1.4-6.7 wt.% eq. NaCl) aqueous solution and a carbonic fluid. Evidence for fluid immiscibility during ore formation includes variable liquid/vapour ratios in inclusions along individual trails and bulk inclusion homogenisation into liquid and occasionally to vapour at comparable temperatures. The trapping conditions of intragranular aqueous-carbonic inclusions approximate 264-378 C at 700-1300 bar. Similar temperature estimates have been obtained from Al
Fracture propagation trajectories in gas-bearing shales depend on the interaction between the anisotropic mechanical properties of the shale and the anisotropic in-situ stress field. However, there is a general paucity of available experimental data on their anisotropic mechanical, physical and fluid-flow properties, especially at elevated confining pressures. A suite of mechanical, flow and elastic measurements have been made on two shale materials, the Whitby mudrock and the Mancos shale (an interbedded silt and mudstone), as well as Pennant sandstone, an isotropic baseline and tight-gas sandstone analogue. Mechanical characterization includes standard triaxial experiments, pressure-dependent permeability, brazilian disk tensile strength, and fracture toughness determined using double-torsion experiments. Elastic characterisation was performed through ultrasonic velocities determined using a cross-correlation method. Additionally, we report the results of laboratory-scale fluid injection experiments for the same materials. Injection experiments involved the pressurisation of a blind-ending central hole in a dry cylindrical sample. Pressurisation is conducted under constant volume-rate control, using silicon oils of varying viscosities. Breakdown pressure is not seen to exhibit a strong dependence on rock type or orientation, and increases linearly with confining pressure. In most experiments, a small drop in the injection pressure record is observed at what is taken to be fracture initiation, and in the Pennant sandstone this is accompanied by a small burst of acoustic energy. The shale materials were acoustically quiet. Breakdown is found to be rapid and uncontrollable after initiation if injection is continued. A simplified 2-dimensional model for explaining this is presented in terms of the stress intensities at the tip of a pressurised crack, and is used alongside the triaxial data to derive a characteristic flaw size from which the fractures have initiated
Pulsed discharges in high-pressure gases are of considerable interest as sources of nonequilibrium plasma for various technological applications: pollution control, pumping of laser media, plasma-assisted combustion, etc. Recently, attention has been attracted to the use of subnanosecond voltage fronts, producing diffuse discharges with radii of several millimeters. Such plasma structures, similar to pulsed glow discharges, are of special interest for applications due to quasi-uniformity of plasma parameters in relatively large gas volumes. This review presents the results of experimental and computational study of subnanosecond diffuse discharge formation. A description of generators of short high-voltage pulses with subnanosecond fronts and of discharge setups is given. Diagnostic methods for the measurement of various discharge parameters with high temporal and spatial resolution are described. Obtained experimental data on plasma properties for a wide range of governing factors are discussed. A review of various theoretical approaches used for computational study of the dynamics and structure of fast ionization waves is given; the applicability of conventional fluid streamer models for simulation of subnanosecond ionization waves is discussed. Calculated spatial-temporal profiles of plasma parameters during streamer propagation are presented. The efficiency of subnanosecond discharges for the production of reactive species is evaluated. On the basis of the comparison of simulation results and experimental data the effects of various factors (voltage rise time, polarity, etc.) on discharge characteristics are revealed. The major physical phenomena governing the properties of subnanosecond breakdown are analyzed. 2ff7e9595c
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