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Collapse of U.S. 35 Highway Bridge, Point Pleasant, West Virginia, December 15, 1967 (HAR-71/01)

National Transportation Safety Board · 1970-12-16 · 202 pages · text by OCR, confidence 99%

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- 00 - Surface Number of Pits Average Pit Depth, in. Maximum Pit Depth, in. Two inch wide strip, pinhole to outside edge, south face Half inch nearest hole 31 0.014 0.038 Remainder of surfaces 7 0.003 0.013 Two inch wide strip, pinhole to outside edge, north face Five inches nearest hole 60 0.027 0.053 Outer four inches 42 0.049 0.105 Pinhole surface (normally in contact with the pin) First 6/16" from north face 4 0.0045 0.006 Next 9/16" from north face 27 0.005 0.007 Next 10/16" from north face 51 0.006 0.008 Remaining 6/16" to south face 23 0.0075 0.012 d. Reference 25, "Examination of Point Pleasant Bridge Eyebars," dated May 18, 1970, reports the studies conducted by U. S. Steel as a part of the work of the special task group appointed to investigate the mechanism by which the crack in eyebar No. 330 grew to critical size. The specimen was taken from eyebar C9-C11 north chain, south bar, which contained a tight crack similar to the pre-existent crack in eyebar No. 330. As noted in the discussion of the work by the Battelle group, this specimen was broken open by a static load to extend the crack at the USS laboratory. The general appearance of the piece retained by USS for examination is shown in Figure 24a. Four distinct regions were noted in the fracture surface, designated A, B, C, and D in Figure 24b. When first examined, the black oxides in region A were noted to be wet with water. An attempt was made to measure the pH, but there was not sufficient water for a valid reading. Within five minutes, the surface was dry. This region marks the limits of the crack originally in the piece. Zones B, C, and D were formed when the specimen was loaded to failure. Zones B and C were both gray in color, but zone D was light in color, and a zone of definite fast fracture. In addition to examination of all regions by fractography using the scanning electron microscope, the material present in zone A was checked for the presence of certain elements with the x-ray spectroscopy attachment, by electron probe analysis, and by x-ray diffraction techniques. The black oxides were identified as iron oxides (Fe₃O₄ and possibly Fe₂O₃), and other particles in this region contained calcium, silicon, chlorine, aluminum, and sulfur. The calcium and silicon were frequently associated, and most sulfur indications were associated with manganese, indicating that these particles may have been manganese sulfide from the underlying steel. An azide test for detection of sulfide was conducted on zones A and D. Both zone A and zone D gave moderate indications, with that in zone A being somewhat

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Document, cited by the archive. The PDF is mirrored here; the original link is under it. The text was read from the page images by an OCR model (mean confidence 99%); expect the odd misread word. 202 pages are in the text index: search them above, or from the library's search.