Accelerated Diffusion Bonding Using Induced Forces

1976 ◽  
Vol 98 (1) ◽  
pp. 65-68
Author(s):  
T. J. Morin

Classical diffusion bonding has always connoted nonproduction-like conditions such as extremely high pressures for long times, protective environments, and excessive cleanliness requirements. The attractive characteristics are that diffusion bonds are normally produced at comparatively low temperatures and they have parent metal properties. This paper presents a technique whereby high pressures are selectively applied to the interfacial region of the two parts being joined at temperatures approximately 90–95 percent of the parent metal melt range. The parts to be joined are heated rapidly using “induction heating” techniques. The mating surfaces and the areas immediately adjacent to them are the only portions of the parts that are significantly heated in most applications. As soon as the proper temperature range has been reached, the heating current is shut off and an intense magnetic field is forced or driven through the parts. The orientation and direction of this moving magnetic field is such that a large pulsed current is caused to flow on both sides of and parallel to the interface. These large currents attract each other and give rise to substantial pressures normal to the interface, thereby producing intimate contact on a microscopic scale, allowing for rapid diffusion. There is also some preferential super heating in the interfacial zone for a few milliseconds only but greatly enhancing diffusion conditions. Results of the application of this technique to several material combinations are discussed along with photomicrographs of joined sections.

1989 ◽  
Vol 178 ◽  
Author(s):  
Joseph A. Larbi ◽  
Jan M. Bijen

AbstractThe evolution and distribution of calcium hydroxide, CH, and the development of microstructure during the hydration of three low-calcium fly ash-Portland cement blends with water-solids ratio (w/s) of 0.40 have been investigated. During the first month of hydration, the CH content of the blends was found to be relatively higher than the plain mix, if a dilution effect due to replacement of cement by an inert material is taken into account. After 28 days of hydration the CH content in the blends began to decrease. SEM observations of specimens revealed the occurrence of large, well-crystallized CH plates in intimate contact with some of the fly ash particles at younger ages and even after six months of aging. The study also showed that the chemistry of the pore solution in contact with the hydrating cement system and the characteristics of the fly ashes, such as the glass content and the fineness of the ash particles seem to exert major influences on the rate of evolution of CH in the fly ash blends. Semi-quantitative X-ray diffraction analyses performed on specimens cast against polypropylene plastic plates used to “model coarse aggregates” showed reduction in the thickness of the interfacial zone for the fly ash-Portland cement pastes from about 60μm to less than 15μm within one month of hydration. In the case of the plain Portland cement paste no significant change was observed. The degree of orientation of CH crystals within the interfacial region also was significantly affected by the fly ashes, although by this age of hydration the CH data showed little or no evidence of pozzolanic reaction.


1974 ◽  
Vol 20 (7) ◽  
pp. 353-356 ◽  
Author(s):  
R. Swami ◽  
V. S. Pandey ◽  
B. A. P. Tantry

SPE Journal ◽  
2013 ◽  
Vol 18 (02) ◽  
pp. 319-330 ◽  
Author(s):  
Dai Makimura ◽  
Makoto Kunieda ◽  
Yunfeng Liang ◽  
Toshifumi Matsuoka ◽  
Satoru Takahashi ◽  
...  

Summary Molecular simulation is a powerful technique for obtaining thermodynamic properties of a system of given composition at a specific temperature and pressure, and it enables us to visualize microscopic phenomena. In this work, we used simulations to study interfacial phenomena and phase equilibria, which are important to CO2-enhanced oil recovery (EOR). We conducted molecular dynamics (MD) simulation of an oil/water interface in the presence of CO2. It was found that CO2 was enriched at the interfacial region under all thermal conditions. Whereas the oil/water interfacial tension (IFT) increases with pressure, CO2 reduces the IFT by approximately one-third at low pressure and one-half at higher pressure. Further analysis on the basis of our MD trajectories shows that the O=C=O bonds to the water with a “T-shaped” structure, which provides the mechanism for CO2 enrichment at the oil/water interface. The residual nonnegligible IFT at high pressures implies that the connate or injected water in a reservoir strongly influences the transport of CO2/oil solutes in that reservoir. We used Gibbs ensemble Monte Carlo (GEMC) simulation to compute phase equilibria and obtain ternary phase diagrams of such systems as CO2/n-butane/N2 and CO2/n-butane/n-decane. Simulating hydrocarbon fluids with a mixture of CO2 and N2 enables us to evaluate the effects of N2 impurity on CO2-EOR. It also enables us to study the phase behavior, which is routinely used to evaluate the minimum miscibility pressure (MMP). We chose these two systems because experimental data are available for them. Our calculated phase equilibria are in fair agreement with experiments. We also discuss possible ways to improve the predictive capability for CO2/hydrocarbon systems. GEMC and MD simulations of systems with heavier hydrocarbons are straightforward and enable us to combine molecular-level thinking with process considerations in CO2-EOR.


1986 ◽  
Vol 108 (2) ◽  
pp. 323-329 ◽  
Author(s):  
R. Kumar ◽  
R. J. Adrian

In a simulation of the lifting of an atmospheric inversion layer in the laboratory, measurements have been made to understand the dynamics in the interfacial region capped by a stable, linearly stratified layer. Instantaneous values of vertical and horizontal components of velocity have been measured using a two-component dual-beam laser Doppler anemometer. Temperature fluctuations have been made simultaneously. Detailed measurements of all relevant horizontally averaged one-point moments including heat flux and third-order joint vertical velocity–temperature moments have been obtained. The negative heat flux region is well defined in the entrainment zone, and varies in thickness with different stable layer temperature gradients. The entrainment mechanism is probably most important only in the top part of the interfacial zone. The present data supplement data obtained in the atmosphere, and they compare favorably with the existing data in the literature.


2017 ◽  
Vol 95 (8) ◽  
Author(s):  
Guillaume Voisin ◽  
Silvano Bonazzola ◽  
Fabrice Mottez

1978 ◽  
Vol 67 (5-6) ◽  
pp. 435-438 ◽  
Author(s):  
A.E. Delsante ◽  
N.E. Frankel

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