AN ASSESSMENT OF BALLAST SOURCE'S QUALITY AND LOCATIONS WITH RESPECT TO MDOT'S UPGRADE OF THE WOLVERINE RAILROAD LINE FOR HIGH SPEED RAIL USEAGE

The Michigan Department of Transportation is evaluating upgrading their portion of the Wolverine Line between Chicago and Detroit to accommodate high speed rail. This will entail upgrading the track to allow trains to run at speeds in excess of 110 miles per hour (mph). An important component of this upgrade will be to assess the requirement for ballast material for high speed rail. In the event that the existing ballast materials do not meet specifications for higher speed train, additional ballast will be required. The purpose of this study, therefore, is to investigate the current MDOT railroad ballast quality specifications and compare them to both the national and international specifications for use on high speed rail lines. The study found that while MDOT has quality specifications for railroad ballast it does not have any for high speed rail. In addition, the American Railway Engineering and Maintenance-of-Way Association (AREMA), while also having specifications for railroad ballast, does not have specific specifications for high speed rail lines. The AREMA aggregate specifications for ballast include the following tests: (1) LA Abrasion, (2) Percent Moisture Absorption, (3) Flat and Elongated Particles, (4) Sulfate Soundness test. Internationally, some countries do require a highly standard for high speed rail such as the Los Angeles (LA) Abrasion test, which is uses a higher standard performance and the Micro Duval test, which is used to determine the maximum speed that a high speed can operate at. Since there are no existing MDOT ballast specification for high speed rail, it is assumed that aggregate ballast specifications for the Wolverine Line will use the higher international specifications. The Wolverine line, however, is located in southern Michigan is a region of sedimentary rocks which generally do not meet the existing MDOT ballast specifications. The investigation found that there were only 12 quarries in the Michigan that meet the MDOT specification. Of these 12 quarries, six were igneous or metamorphic rock quarries, while six were carbonate quarries. Of the six carbonate quarries four were locate in the Lower Peninsula and two in the Upper Peninsula. Two of the carbonate quarries were located in near proximity to the Wolverine Line, while the remaining quarries were at a significant haulage distance. In either case, the cost of haulage becomes an important consideration. In this regard, four of the quarries were located with lake terminals allowing water transportation to down state ports. The Upper Peninsula also has a significant amount of metal based mining in both igneous and metamorphic rock that generate significant amount of waste rock that could be used as a ballast material. The main drawback, however, is the distance to the Wolverine rail line. One potential source is the Cliffs Natural Resources that operates two large surface mines in the Marquette area with rail and water transportation to both Lake Superior and Lake Michigan. Both mines mine rock with a very high compressive strength far in excess of most ballast materials used in the United States and would make an excellent ballast materials. Discussions with Cliffs, however, indicated that due to environmental concerns that they would most likely not be interested in producing a ballast material. In the United States carbonate aggregates, while used for ballast, many times don't meet the ballast specifications in addition to the problem of particle degradation that can lead to fouling and cementation issues. Thus, many carbonate aggregate quarries in close proximity to railroads are not used. Since Michigan has a significant amount of carbonate quarries, the research also investigated using the dynamic properties of aggregate as a possible additional test for aggregate ballast quality. The dynamic strength of a material can be assessed using a split Hopkinson Pressure Bar (SHPB). The SHPB has been traditionally used to assess the dynamic properties of metal but over the past 20 years it is now being used to assess the dynamic properties of brittle materials such as ceramics and rock. In addition, the wear properties of metals have been related to their dynamic properties. Wear or breakdown of railroad ballast materials is one of the main problems with ballast material due to the dynamic loading generated by trains and which will be significantly higher for high speed rails. Previous research has indicated that the Port Inland quarry along Lake Michigan in the Southern Upper Peninsula has significant dynamic properties that might make it potentially useable as an aggregate for high speed rail. The dynamic strength testing conducted in this research indicate that the Port Inland limestone in fact has a dynamic strength close to igneous rocks and much higher than other carbonate rocks in the Great Lakes region. It is recommended that further research be conducted to investigate the Port Inland limestone as a high speed ballast material.

Teofilo Petriella : Marxist Revolutionary

The paper will examine the role Teofilo Petriella played in splitting Italian communities through Marxist agitation. As a strike leader on Mesabi Iron Range and in Copper Country, Petriella traveled throughout the Great Lakes region. In each community he found supporters among the discontented miners, while also facing strong opposition from Catholic priests and middle class community leaders. By examining his activities in both regions, I will illustrate the connectivity of Italian communities around Lake Superior, while also addressing religious and class conflict amongst the populations.

Federal Authority and the Development of Corporate Mining, 1807-1847

While the 1913-1914 copper country miners’ strike undoubtedly plays an important role in the identity of the Keweenaw Peninsula, it is worth noting that the model of mining corporations employing large numbers of laborers was not a foregone conclusion in the history of American mining. Between 1807 and 1847, public mineral lands in Missouri, in the Upper Mississippi Valley, and along the southern shore of Lake Superior were reserved from sale and subject to administration by the nation’s executive branch. By decree of the federal government, miners in these regions were lessees, not landowners. Yet, in the Wisconsin lead region especially, federal authorities reserved for independent “diggers” the right to prospect virtually unencumbered. In doing so, they preserved a comparatively egalitarian system in which the ability to operate was determined as much by luck as by financial resources. A series of revolts against federal authority in the early nineteenth century gradually encouraged officers in Washington to build a system in the copper country in which only wealthy investors could marshal the resources to both obtain permits and actually commence mining operations. This paper will therefore explore the role of the federal government in establishing a leasing system for public mineral lands in the years previous to the California Gold Rush, highlighting the development of corporate mining which ultimately set a stage for the wave of miners’ strikes in the late nineteenth and early twentieth centuries.

View of the stamping mills

Publication information: Copper Company, Burton Mass. : Printed by Beals and Greene, 1845

Indian Camp

on verso: No. 84. Indian Camp. Birch bark canoes on bank of Kaministiquia River, Canada.

Algal bioassays with leachates and distillates from western coal /

Mode of access: Internet.

Collections of the Minnesota Historical Society.

(cont) The source of the Mississippi / by N.H. Winchell -- Prehistoric man at the headwaters of the Mississippi River / by J.V. Brower -- Charter members of the Minnesota Historical Society and its work in 1896 / by Alex. Ramsey -- History of agriculture in Minnesota / by James J. Hill -- History of mining and quarrying in Minnesota / by Warren Upham -- History of the discovery of the Mississippi River and the advent of commerce in Minnesota / Russell Blakeley -- Reminiscences of persons and events in the early days of the Minnesota Historical Society / by William H. Kelley -- Fort Snelling from its foundation to the present time / by Richard W. Johnson -- Sully's expedition against the Sioux, in 1864 / by David L. Kingsbury -- State-building in the West / by Charles E. Flandrau -- Obituaries.

Sand bar at extreme north end of Grand Island

verso: Sand bar at extreme north end of Grand Island where north stream flows into Lake Superior at low gradient

Shore line of G.I.

continued from verso: showing high banded Cambrian sandstone cliffs rising abruptly from Lake Superior along the w. edge of the island

[untitled] Estate of Mr. H.C. Dudley . Duluth, Minnesota.

Blue, black pencil on tracing papers; indicates streets along Lake Superior and Dudley residence off London Road. 27x21 cm. No scale. [from photographic copy by Lance Burgharrdt]

Indian Village and Rapids Sault St. Marie

On verso: The Picturesque of Lake Superior. Photographed by B.F. Childs. C.B. Brubaker, Publisher. Houghton, Mich.

Geological reconnaissance of a portion of Algoma and Thunder bay districts, Ontario,

Appendices: I. Notes on some fossils from the Cambro-Silurian and Silurian rocks of the Albany river drainage system in northwestern Ontario, by J. F. Whiteaves.--II. Lists of insects, by J. F. Fletcher.

Génomique des populations et association génotype-phénotype des écotypes de touladi du Lac Supérieur

L’apparition et le maintien d’écotypes adaptés à différentes niches écologiques, en situation de sympatrie, est régit par une multitude de facteurs. Ceux-ci sont essentiels pour la compréhension des processus évolutifs impliqués mais aussi pour la gestion et la conservation des populations en question. Le touladi (Salvelinus namaycush) est un salmonidé reconnu pour la présence d’écotypes liée à l’utilisation des ressources et de l’habitat à travers l’Amérique du Nord. Un total de quatre écotypes a été décrit vivant dans le lac Supérieur, se différenciant par l’habitat utilisé, l’alimentation, la morphologie ainsi que l’ostéologie. L’objectif principal de la présente étude était de quantifier l’étendue de la différentiation génétique entre les différents sites d’échantillonnage ainsi qu’entre les différents écotypes. Un second objectif était d’identifier des marqueurs potentiellement sous sélection entre les différents écotypes reflétant de possibles adaptations locales. Pour ce faire, un total de 486 individus, représentant les quatre écotypes pour chacun des quatre sites d’échantillonnages, a été génotypé à 6822 SNPs (polymorphisme de nucléotide simple). De plus, des analyses morphométriques ont été effectuées afin de caractériser l’ampleur de la divergence morphologique entre les écotypes à chacun des sites. Les résultats ont montré une différentiation génétique, bien que faible, plus prononcée entre les sites d’échantillonnage qu’entre les écotypes à chacun de ces sites. Des indices indiquant la présence de sélection divergente ont aussi été décelés entre les écotypes ou en association avec des variations morphologiques, dont certains marqueurs représentant des traits importants dans la divergence des différents écotypes. Les résultats de cette étude permettront une meilleure gestion et conservation des populations de touladi du lac Supérieur en plus d’éclairer le choix possible de populations sources pour l’ensemencement des autres Grands Lacs.