Institute of Metals Division - Origin of Porosity in Castings of Magnesium-Aluminum and Other Alloys

The American Institute of Mining, Metallurgical, and Petroleum Engineers
E. J. Whittenberger F. N. Rhines
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
12
File Size:
1192 KB
Publication Date:
Jan 1, 1953

Abstract

The formation of casting porosity is viewed as a nucleation and growth process with solidification shrinkage and gas precipitation as cooperative driving forces. Experimental evidence evaluating the individual contribution of each force confirms the major premise that microporosity is nucleated by gas precipitation. Additional data disclose the effects of the identity and quantity of gas, the temperature range of freezing, and the freezing rate upon the amount and distribution of porosity in light metal castings. POROSITY, as it commonly occurs in metal castings, has been ascribed to the contraction that accompanies the freezing of the metal, to the evolution of dissolved gases from the liquid during cooling and freezing, and, most frequently, to a combination of the two.'" "Pipe" formation is universally associated with solidification shrinkage; spherical "gas holes" are understood to be retained bubbles of gas; but the origin of microporosity, which usually exhibits an irregular or scalloped outline when viewed in cross-section, remains a subject of continuing debate.", ' The present research constitutes an endeavor to show what parts are played respectively by shrinkage and gas evolution in the initiation and growth of micropores and what factors determine their number, size, shape, and distribution. A preliminary outline of the mechanism of cavity formation in castings will serve to coordinate the experimental findings that will be reported and will at the same time provide a general theory of the origin of casting porosity. Basic to the mechanism of cavity formation that will be proposed are the following established facts: 1—that liquid metals and alloys contract gradually during cooling down to the freezing range, where a relatively large contraction, known as the "solidification shrinkage," takes place (exceptions in bismuth and gallium being noted);' 2—that the capacity of liquid metals and alloys for dissolving gases diminishes with cooling until, in the freezing interval, a large decrease takes place (various exceptions being noted and excluded from present consideration) ;.: and 3—that freezing proceeds counter to the direction of heat flow, the freezing front most commonly being composed of a system of tapering dendrite stalks and side arms which are coarser the lower the freezing rate and which protrude into the liquid for a distance that is greater the longer the freezing temperature interval of the alloy and the smaller the thermal gradient.' The mechanism by which voids are generated
Citation

APA: E. J. Whittenberger F. N. Rhines  (1953)  Institute of Metals Division - Origin of Porosity in Castings of Magnesium-Aluminum and Other Alloys

MLA: E. J. Whittenberger F. N. Rhines Institute of Metals Division - Origin of Porosity in Castings of Magnesium-Aluminum and Other Alloys. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1953.

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