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Limestone dimensions

Limestone Production. Because more than 99% of U.S. limestone is sold or used as cmshed and broken stone, rather than dimension-stone, most of the description of limestone s extraction and processing herein focuses on the former (Fig. 4). Most stone is obtained by open-pit quarrying methods. Underground mining is pursued by some important operations, but the toimage quarried exceeds that mined by nearly 20-fold. There is, however, a slight trend toward increased mining which should continue. [Pg.168]

Some devices employ impact (hammers) and others employ crushing by nipping (roils or jaws). Within limits, kinetic energy and dimensions of crushing elements can be selected to give a desired reduction ratio. Because of the deformability of solid materials, however, a theoretical limit does exist to the size of particles that can be crushed. These limits are 1 jum for quartz and 3-5 jum for limestone. The products of crushing these sizes, of course, can be very much smaller, so that really there is no practical lower limit to grinding. [Pg.339]

This cycle is typical for the mining of narrow, steeply dipping veins (typical of metal ores), and for massive deposits of limestone, salt, and dimension stone, where the vertical extent of the valuable mineral is 6 meters or higher. [Pg.15]

In this paper, we describe an onsite weathering experiment designed to identify acid-rain increased dissolution of carbonate rock. This experiment is based on the measurement of the change in rainfall-runoff composition from the interaction of a rock surface with incident acid rain 2. The experiment involves conducting long-term exposures of two commercially and culturally important calcium carbonate dimension stones (i.e., Indiana Limestone (commercial name for Salem Limestone) and Vermont Marble (commercial name for Shelburne Marble)) (3-5). This technique appears to give a direct measurement of the chemical dissolution of carbonate rock from the combined reactions of wet and dry deposition. Preliminary results from the initial months of onsite operation are presented to illustrate the technique. [Pg.227]

Shelburne Marble from Vermont, used for example in the Jefferson Memorial, and Salem Limestone from Indiana, as used in the National Cathedral, were obtained as sample stock materials. Each of the two stone stocks was selected as a monolithic block and was cut into slabs measuring 610 x 305 x 51 mm, under the supervision of NAPAP personnel (7-8). Selected slabs were used to fabricate briquettes, which were employed for several of the damage studies. Briquette dimensions are shown in Figure 2. Surface finishes typical of those provided on stone used for exteriors of buildings were employed on what would become the skyward surfaces of slabs and briquettes an 80-grit ground surface was produced on marble, and a "smooth planar... [Pg.268]

Figure 2. Dimensions of wedge-shaped briquettes employed as specimens of marble and limestone. Also shown are locations of areas sampled in layers to assess depth of chemical alteration caused by atmospheric exposure. Figure 2. Dimensions of wedge-shaped briquettes employed as specimens of marble and limestone. Also shown are locations of areas sampled in layers to assess depth of chemical alteration caused by atmospheric exposure.
Fig. 6. (A) Location of the mapped foreshore transect (see Fig. 5) the Main Limestone is exposed above in a 15-20 m cliff section 175 m south of the foreshore. (B) Map of dolomite-cemented fractures on a 100 m x 20 m transect some fractures extend landward of the transect. (C) Summary of fracture orientations measured across the transect. (D) Summary of fracture dimensions measured across the transect. Fig. 6. (A) Location of the mapped foreshore transect (see Fig. 5) the Main Limestone is exposed above in a 15-20 m cliff section 175 m south of the foreshore. (B) Map of dolomite-cemented fractures on a 100 m x 20 m transect some fractures extend landward of the transect. (C) Summary of fracture orientations measured across the transect. (D) Summary of fracture dimensions measured across the transect.
Migration of Plutonium into Dense Stone Samples. Thin wafers or disks of dense Illinois Niagara limestone and basalt from the EBR-II site were fabricated. The dimensions were approximately 25 mm 1n diameter and 1.5 mm 1n thickness. The wafers were waxed into the high pressure chromatographic apparatus as shown in Fig. 2. [Pg.31]

The problem considered here is a geometrically simple one in two dimensions designed to simulate isothermal flow and reaction in a medium in which some percentage of the rock is reactive (e.g, a carbonate cement) while the remainder is treated as inert (e.g, a quartz sandstone at low temperature). The analysis presented here should apply in most respects to the case where the entire rock is reactive (e.g., a pure limestone), although in this instance the flow can no longer be treated as Darcian. The problem as formulated here is essentially the same as that considered by Ortoleva et al. (2). Although our formulation is based on a one-component system, the results should be broadly applicable to relatively simple multi-component reactions (e.g., calcite dissolution). [Pg.215]

Over the centuries, limestone has been used extensively as an aggregate in building and construction. It has been used as aggregate in lime-based concrete since Roman times, and, more recently, in cement-based concrete. Although limestone cannot readily be dressed, it has been used extensively in building in both the rough-hewn form and as cut dimension stone. [Pg.3]

A small tonnage of limestone is used in the production of dimension stone. The process is outlined in section 4.7. [Pg.26]

Marble and other limestones are used in relatively small tonnages as dimension stone for ornamental purposes such as facing buildings and tombstones. [Pg.36]

The manufacturing plant occupies an area rectangular in shape 5,310 feet by 2,860 feet with the long dimension running north and south. With the exception of the liquid air production, the sequence of manufacture is from north to south. The raw materials limestone, coal and coke arc unloaded from a trestle at the north end of the manufacturing area and started into the process. All materials... [Pg.40]

A suitable sample for an X-ray spectrometer is normally circular with a diameter of 30—40 mm and thickness about 3-5 mm. For oxide materials a choice must be made between either direct pelletization of the powdered sample, or fusion of the sample with a suitable flux to form a glass bead of the appropriate dimensions. This choice rests between speed and accuracy, with direct pelletization being faster, and fusion potentially more accurate. As a general rule pelletization may be used for raw material and raw meal analysis, when the seams are reasonably pure, and when only two materials are employed (i.e., chalk/limestone and clay/shale). [Pg.481]

Suggest the optimum outlet dimension of a conical hopper in a silo storing moist crushed limestone of 1350 kg/m density. The results of characterizing the limestone using in terms of failure properties are presented in Tables 3.12 through 3.14. [Pg.172]

The mass and energy balance for a 15 by 300 ft (4.57 by 92 m) kiln for the dolomitic limestone calcination process is presented here. The procedure starts with information on the kiln dimensions and layout (Figure 9.2) followed by process audit, which provides the necessary... [Pg.246]

The tables that follow go through a site survey. Table 9.1 covers the ambient air to the cooler. Table 9.2 covers the cooling air to the burner. Table 9.3 covers the coal conveying air, and Tables 9.4 and 9.5 cover the limestone and the dust. Table 9.6 covers the properties of the natural gas input and the kiln exit gas. Table 9.7 covers the kiln dimensions and shell temperatures. [Pg.247]

Figure 40.5 Transverse serial sections of Lobothryis sp. (Fig. 40.2, 17-20) from the Hosselkus Limestone, (Carnian), Brock Mountain, northern California, LACMIP 28681, showing ventrally concave hinge plates (sections 0.7-1.7) with ventrally directed crural bases (1.5-2.6), crural processes (4.8), low arched transverse band (7.1) and anterior flanges (traced to 7.8). Dimensions of specimen length (brachial valve) 25.0 mm width 22.5 mm thickness 15.8 mm. Scale bar is 1.33 mm for sections 0.0-0.7 (top row, left), I.I-2.8 2.7mm for sections 0.7 (top row, right), 1.9 (centre, second row), 3.4-7.S 6.25 mm for section 7.1 (centre, bottom row). Figure 40.5 Transverse serial sections of Lobothryis sp. (Fig. 40.2, 17-20) from the Hosselkus Limestone, (Carnian), Brock Mountain, northern California, LACMIP 28681, showing ventrally concave hinge plates (sections 0.7-1.7) with ventrally directed crural bases (1.5-2.6), crural processes (4.8), low arched transverse band (7.1) and anterior flanges (traced to 7.8). Dimensions of specimen length (brachial valve) 25.0 mm width 22.5 mm thickness 15.8 mm. Scale bar is 1.33 mm for sections 0.0-0.7 (top row, left), I.I-2.8 2.7mm for sections 0.7 (top row, right), 1.9 (centre, second row), 3.4-7.S 6.25 mm for section 7.1 (centre, bottom row).
This crystal structure is shown in Fig. 1.17. There is a second form known as Parawollastonite , which occurs chiefly in limestone blocks ejected from volcanoes. This has a monoclinic crystal structures with unit cell dimensions ... [Pg.43]


See other pages where Limestone dimensions is mentioned: [Pg.170]    [Pg.406]    [Pg.68]    [Pg.1011]    [Pg.1217]    [Pg.406]    [Pg.9]    [Pg.3]    [Pg.132]    [Pg.339]    [Pg.291]    [Pg.413]    [Pg.12]    [Pg.465]    [Pg.64]    [Pg.34]    [Pg.128]    [Pg.161]    [Pg.338]    [Pg.427]    [Pg.656]    [Pg.670]    [Pg.969]    [Pg.170]    [Pg.285]    [Pg.628]    [Pg.24]    [Pg.619]    [Pg.216]   


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Limestone

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