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By Lucas Beirão do Valle

Este artigo visa estudar polímeros como quitosana, amido entre outros com elevada disponibilidade como agentes aglomerantes no processo de pelotização de minério de ferro e discutir sobre o impacto da sua utilização. Os polímeros foram testados preliminarmente no teste de bancada (teste em pneu), para medir qualitativamente a tendência de aglomeração. Os polímeros com melhores resultados foram testados em escala piloto, que simula o processo industrial. Nos testes preliminares, o amido gelificado apresentou os melhores resultados de resistência física de pelotas verdes e secas. Entretanto, no teste piloto o amido não foi capaz de controlar a umidade superficial. Os outros polímeros não foram considerados promissores, principalmente devido ao controle da umidade superficial.

Aug 1, 2018

By Roger Chávez

Mediante el uso de las herramientas informáticas, tales como: Power Apps, SharePoint y Power Automate se desarrolló una aplicación para personal directamente encargado de las labores de evaluación y reparación de equipos, así como para personal de planeamiento y programación de mantenimiento, denominado “Soporte Mantenimiento Quebrada Honda” o por sus siglas “SMQH” versión 2.0.

Sep 29, 2023

By Lily Ruíz

El presente texto evalúa el relave minero de SIMSA con el objetivo de obtener un producto ecológico que pueda ser utilizado como mejorador cationico de suelos y restaure el equilibrio de los suelos ácidos de la selva peruana. Para ello, se desarrolló un trabajo a nivel de laboratorio, obteniéndose resultados satisfactorios. Posteriormente se pasó al nivel piloto donde a través de la experimentación se utilizó el relave en diferentes concentraciones para la producción agrícola y forestal, reafirmando los resultados en las mejoras de la productividad en suelos ácidos.

Sep 9, 2007

By Santiago Misari

Dentro de las labores de mecanización minera, la perforación y la voladura son operaciones unitarias que se relacionan con el proceso de minado por la labor de diseño y ejecución de los mismos. En este sentido, el presente trabajo señala las experiencias logradas en el uso de taladros largos y “Drop Raising” en voladura de chimeneas. De forma que se puedan eliminar los riesgos en el avance de producción de chimeneas, así como el uso de andamios metálicos, acelerar el ciclo de minado y disminuir los costos de voladura y perforación.

Sep 13, 2001

By Wagner Angelo da Silva

A crescente demanda por energia elétrica nas aeronaves modernas pode ser constatada pelo aumento da potência elétrica gerada a bordo, como exemplo o Boeing 787 produz 1000kVA, 200V trifásico, 400Hz variável contra 240kVA, 200V trifásico, 400Hz fixo produzido pelo Airbus A330, apesar de possuírem aproximadamente as mesmas dimensões. Devido à necessidade de redução de massa de transformadores, a frequência utilizada na geração de eletricidade na aeronave é de 400Hz o que acaba produzindo um aumento das perdas em núcleos de FeSi destes transformadores, principalmente pelo aumento das correntes parasitas no núcleo. Transformadores elétricos com núcleos de ligas amorfas a base de Fe vêm apresentando redução de até 70% das perdas no núcleo quando operados em 50Hz ou 60Hz. Assim, esse estudo visa discutir as vantagens e desvantagens do uso de transformadores elétricos com núcleos de ligas amorfas a base de Fe em aeronaves. Os resultados mostram que, com o desenvolvimento de novas ligas, tal utilização mostra-se viável devido a uma redução de peso de tais transformadores.

Aug 8, 2018

By Julio Tovar, Samuel Quisca

La lixiviación de metales pesados y la inestabilidad de taludes de los depósitos de relaves en la minería causan serios problemas ambientales de contaminación, que originan riesgos de salud y de seguridad de las poblaciones. Frente a esta problemática, es primordial eliminar o controlar los lixiviados tóxicos de los relaves y mejorar su estabilidad física, con el propósito de reducir el impacto ambiental de los contaminantes en los recursos de agua y suelos, así como asegurar la seguridad física de las relaveras, a fin de ganar la confianza de los stakeholder.

Sep 29, 2023

By Humberto Napoli BELLEI

O Sol é a principal fonte de energia sustentável com enorme potencial na geração de energia elétrica. O Brasil como outros países do mundo estão começando a construção de fazendas solares. Atualmente as especificações das estruturas para construção das estruturas dos painéis utilizados nessas fazendas tem sido de aços pós galvanizados justificado pela questão de tempo de garantia, principalmente, devido a presença de furos e bordas que ficariam protegidos contra a corrosão pela grande quantidade de revestimento utilizado. Nesse trabalho serão apresentados resultados de um aço pré-galvanizado que se mostrou seguro e confiável na proteção contra a corrosão dos furos e bordas dos painéis. O estudo teve como base as informações obtidas após o aço ter sido testado no ensaio em câmara de névoa salina e de dados já conhecidos em ensaios de campo.

Oct 30, 2017

By Marden Valente de Souza

Com o início da utilização do EPC, modelo matemático de previsibilidade de propriedade mecânica, no laminador de tiras a quentes da ArcelorMittal Tubarão em 2012 como ferramenta de acompanhamento da qualidade, pode-se verificar o comportamento das propriedades mecânicas ao longo do comprimento das bobinas logo após sua laminação. Baseado nestes resultados verificou-se que, principalmente, para material com espessura superior a 9,50 mm ocorria uma queda de propriedade mecânica do topo, região indicada para amostragem conforme norma, para o centro de aproximadamente 30 MPa, apresentando todos os valores aprovados conforme especificação da norma. Após verificação por ensaio físico na região central e comprovação da indicação do modelo, modificou-se o processo para garantir um produto com propriedade mais uniforme mantendo a garantia de atendimento às normas ao longo de todo comprimento.

Aug 8, 2018

By José Raphael Olegário França

Separação eletrostática é o termo usado para todas as tecnologias de processamento que utilizam forças elétricas que atuam sobre partículas carregadas ou polarizadas sob um campo elétrico estático. O comportamento das partículas depende das suas propriedades elétricas, geométricos e tamanho das partículas. Portanto, a separação de espécies é possível se os parâmetros do campo elétrico e as propriedades elétricas diferentes das partículas são apropriados para o processo. No separador eletrostático de rotor as forças elétricas, combinadas com as forças gravitacionais e centrífugas agem sobre as partículas e são responsáveis pela separação mineral. No presente trabalho as forças eletrostáticas que agem no processo serão substituídas por um modelo de contato de coesão Hertz-Mindlin com JKR. O resultado apresentado, embora com limitações, conseguiu-se fazer uma boa estimativa do processo e alguns dos parâmetros do separador. Com a presente simulação é possível descrever o processo de separação além de permitir a redução de despesas de testes práticos, melhorar a compreensão das relações fundamentais, simular as influências dos diferentes parâmetros e por fim, estimar eventuais aumento de desempenho.

Aug 17, 2017

By J. W. Germundson

La Cerro de Pasco Corporation fue una de las primeras compañías mineras que utilizó el explosivo a base del nitrato de amonio en las operaciones de explotación de subsuelo. En este sentido, el objetivo del texto radica en el fomento de su uso para futuras subterráneas a través del conocimiento de la historia de los explosivos, los procesos y composición del nitrato de amonio, el empleo del explosivo AN-FO Mina Cerro de Pasco en el subsuelo, usos actuales de la AN-FO, análisis de costos y las reglas de seguridad.

Aug 20, 1963

By Alistair Burrows

Situated in the oblast of East Kazakhstan, the Ust-Kamenogorsk Metallurgical Complex has spent the past twenty years renovating and remodelling itself as a modern polymetallic sulphide smelting facility, and a regional centre of excellence for custom smelting. Along the way there have been changes to the company structure, introduction of new technologies, investments in expanded capacity, environmental improvements, and addition of new metal products and by-products to the site’s repertoire. These changes have been gradual and incremental, but taken together they represent a significant contribution to placing Kazakhstan’s sulphide smelting industry on a strong foundation for enduring success in the international custom smelting market. In achieving these changes, a workforce that was historically isolated from much of the world now has recognised expertise, internationally competitive skills, and confidence to embrace the future. Further improvements in energy efficiency, environmental compliance and polymetallic processing capabilities are challenges that UKMC stands ready to face.

By Athena C. Denivo, Pablo V. Lopez, Sissy Nikolaou, Alfred H. Brand, Ahmad Rahimian, Rudivien G. Josef

"The United States Tennis Association (USTA) Billie Jean King National Tennis Center (BJKNTC) site is located in the northeastern portion of the Flushing Meadows Corona Park area of Queens, N.Y. The site occupies some of the most difficult subsurface conditions for construction in the New York City (NYC) metropolitan area, with unique challenges from geotechnical, seismic and foundation design perspectives.At the USTA site, Paleozoic crystalline bedrock is found at a depth of roughly 300 to 400 ft (90 to 120 m) below grade. The geologic history of the site is complicated, starting from the early Pleistocene, when the ancient Hudson River temporarily changed course, flowing across Queens enroute to the Atlantic. It eventually carved a deep valley through the Cretaceous soils, in some places all the way down to bedrock. A series of glaciers advanced and retreated across the region during the Pleistocene times, filling the deep valley with layers of assorted glacial soils. At its southern edge, the last major glacier to flow across the region built up a ridge at the southern tip of Flushing Meadows known as the Harbor Hill terminal moraine. This ridge blocked the valley forming a dam, so as ice started melting away the valley filled up with a lake fed by glacial meltwater. Layers of clean outwash sand and varved silt and clay filled the glacial lake. The ice did not retreat in a steady manner, instead periodically readvancing over the previously deposited soil in the lake, then retreating far enough to let the lake drain temporarily into Long Island Sound, before readvancing again.As a result of this repeated sequence of retreat, advance, retreat, etc., there are places where a “crust” of desiccated soil formed when the lake drained, and areas with interlayers of outwash sand where ice readvanced into the lake. When the ice melted north of Long Island Sound, the glacial lake filling Flushing Meadows drained forming Flushing Creek. During the Holocene (roughly the last 11,000 years), as ice melted further away and sea-level rose, low lying areas filled with river sands and marine clays, along with coastal marsh deposits. Table 1 lists the soil design properties on site and Figure 1 exhibits the geologic section across the site."

Jan 1, 2015

"NAME…""Utah"" is derived from the name of the Indian tribe, variously spelled ""Yuta, “Ute"" ""Youta,"" ""Uta,"" ""Eutaw,"" and finally ""Utah."" It means ""in the tops of the mountains,"" or ""on the heights."" The state emblem is the ""Beehive,"" typical of industry. State nickname is ""Beehive State.""AREA…Utah is the tenth state in area. It contains 84,990 square miles, of which 2,806 miles are water. When admitted as a territory in 1850, Utah included all the area from the east line of California to the summit of the Rocky Mountains between the 37th and 42nd parallels, which embraced practically all of the present state of Nevada, all of western Colorado, part of Idaho and part of Wyoming, in addition to the present area of Utah.TOPOGRAPHY…Utah is generally mountainous, with several main ranges and also detached groups of mountains. The valleys are broad and level. The mean altitude of the state is 6,100 feet above sea level, which makes the state the third highest of the Union. The highest point in Utah is King's Peak (13,498) in the Uinta range. The lowest point is Beaverdam Creek (2,000) in Washington county.CLIMATE…The climate is diversified between mild temperate in the northern portion to semitropical in the southern portion. There are four distinct seasons. Snowfall is heavy at the greater altitudes and rare in the southern portion. Rainfall is moderate throughout the state. Extremes of heat and cold are unusual."

Jan 1, 1925

FEW whose good fortune it has been to gaze on the Utah Copper mine but will agree that it is one of the two or three most magnificent man-made spectacles in the world. Skyscrapered Manhattan Island perhaps is more inspiring; but there the effect is obtained by aggregating a thousand separate units. The Utah mine is a single thing- the biggest thing that men have made. By the end of 1931 there had been moved at Utah 222,000,000 cu. yd. of material, including ore and the waste rock that overlay it. This figure will be increased at an average rate of nearly 20,000,000 yd. per year. Excavations for the Panama Canal are estimated at 232,300,000 cu. yd., but the Canal is 50 miles long, and it is impossible to obtain a comprehensive view of the whole project at one time. The spectator, on the other hand, need only walk part way up the east slope of Bingham Canyon to see unfolded before him the whole panorama of the great copper mine. In the foreground is a huge pit bottomed for the time being 100 ft. below the normal floor of the canyon, which also is the elevation of the main railroad yard. Here from 500 to 800 standard steel railway cars, each of 80-ton capacity, are assembled daily to carry the ore to the concentrators. But the main part of the mine and that from which ore is now coming lies above this level. As can be seen in the accompanying photograph, a series of terraces or benches reaches to the top of the mountain that projects between the main branch of Bingham Canyon and Carr Fork. From bench A (the yard level) to bench W is a vertical distance of 1500 ft. In height the benches vary from 40 to 70 ft. and in width from 30 to 450 ft. The lower benches, as they skirt the mountain,

Jan 1, 1933

By O. J. Hollister

Jan 1, 1888

By F. F. Claussen

The method of making silver ingots in use at this Mint being radically different from that employed at any other Mint of the United States or, so far as known to me, any Mint in the world, there may be some interest in a description of the apparatus used and a brief history of its distinguishing feature, viz., the rotary ingotmould, which, though not a recent improvement, is comparatively unknown. The furnaces used for silver-ingot-melting are four in number and have a capacity of some seventy thousand standard ounces of silver per day of eight hours. This output is increased, when the exigencies of the service demand it, to one hundred thousand ounces. They are built of fire-brick and elevated 21/2 feet from the floor of the melting-room, in order to have space to place iron boxes and to work, in case a crucible breaks in the furnace and its contents run into the ash-pit. The furnaces are circular in horizontal section, 2 $ feet in diameter and 29 feet high inside in the clear, and rest on castiron plates, with top-plates of the same, and sides encased in boileriron. The furnace-covers are also of cast-iron, dome-shaped, and are handled by means of a small crane and lever. The furnaces stand in sets of two, and one crane and one ingot-machine serves two furnaces. The crucibles used are made specially for this purpose of a mixture of black-lead and fire-clay; the size known as No. 200 will contain and safely melt, without danger of slopping over, from 8600 to nearly 10,000 ounces of standard silver; and this is the usual weight of the ingot-melt at this Mint, as against 1800 ounces at the Carson City mint and 2600 to 3000 ounces at Philadelphia and San Francisco. Each crucible will endure, on the average, ten melts. The crucible stands in the center of the furnace, on the bottom of an old one, cut down to a height of about three inches. The fuel used is coke. Experience has shown that, notwithstanding the higher first cost, Connellsville coke is cheaper than Alabama coke and much more suitable to the work. A small triangular black-

Jan 1, 1888

By G. Lavagnino

The old Telegraph mine lies on both sides of Bear gulch, a short branch of Upper Bingham canon, and nearly in the center of the group of mines called the Bingham Mines, about twenty-seven miles southwest of Salt Lake City. It is considered, by local miners as the most important mine of the district. The geological formation consists of Weber quartzites, with subordinate conformable limestones and shales, alternating with porphyritic rocks. These widen towards and connect with the massive backbone of the Oquirrh mountains, while the quartzite develops itself on the slope broken through by Bingham canon. The porphyry not only runs between the strata, but also cuts across them, isolating large portions near the mountain mass, and again on a smaller scale it penetrates some joints in the quartzite. It is a crystalline felspathic rock, containing variable proportions of quartz, mica, hornblende, chlorite, and iron pyrites as accessories. In places, it takes a less distinct or almost uniform fine-grained structure. It has a gray or greenish, and, when much altered, also a reddish or even white color. The quartzite is a fine-grained or almost compact grayish-white or bluish or reddish quartz-rock, containing in places fine scales of mica and grains of iron pyrites as accessories. The raised, folded, or broken masses show well-defined bedding-joints, and their general dip is 35 to 50 degrees towards north or northwest. In the porphyry occur metalliferous veins with a prevailing N.E.S.W. strike. These are in general narrow veins; their principal contents are not dissimilar from those of the other deposits; but there is considerably less oxidation near the surface and the ore is mostly richer in silver and gold. In the quartzite the ore-deposits generally occur on the joints of bedding. The more important deposits occur either in clearlydefined contact-veins or, more often, in somewhat vaguely-defined mineralized zones, that could be called contact-zones. These comprise several masses of more or less altered or decomposed rocks and the newly-distributed products of their mechanical and chemical decomposition, such as breccia and clay in seams or in more irregular bodies..

Jan 1, 1888

By William P. Blake

The Rainbow Lode is situated at Walkerville, in the Summit Valley mining district, Silver Bow County, Montana Territory, about one mile from Butte City. It was so named ill 1876 by Mr. J. E. Clayton, in recognition of the broadly-sweeping curve of the outcrop across the rounded surface of the eastern slope of a granitic mountain, at an elevation of about 6000 feet above the sea-level. It is on the western side of the range which divides the waters of the Missouri from those of the Columbia. History.—The history of the district is an instructive one. The water-courses and flanks of the hills were worked for years for placer gold. Millions of dollars' worth of low-grade gold have been washed out of the surface gravels below the veins of the district. Missoula Gulch and Silver Bow creek, just below Butte, are noted for their rich placers, and they continue to yield largely, producing within narrow limits from $50,000 to $100,000 dollars' worth of golddust yearly. It is ragged vein-gold, and evidently is near its parent source. It is no doubt derived from the disintegration of the veins of the district, and this conclusion was soon forced upon the miners. The veins which were seen outcropping boldly upon the slopes above them were located, and prospecting commenced. These outcrops were found heavily stained and blackened with oxide of manganese, and were porous and honey-combed in places, showing that the quartz was formerly filled with pyritous ores, and that these ores had decomposed and dissolved away, leaving, however, portions of the precious metal behind, especially at and near the surface of the ground. Assays of the croppings gave variable and often contradictory results; but the fact. that these were the outcrops of lodes bearing gold and silver in depth was patent to any experienced observer of mineral veins. The lodes of the district were first brought prominently to notice by Mr. Clayton in 1876, and in October of that year the Alice mine, upon the central portion of the lode, was opened by Mr. Marcus Daly, now so well known as the superintendent of the Anaconda Copper mine, upon another extremely interesting lode, in the same region.

Jan 1, 1888

By A. Faber du Faur

At the request of some of the members to whom I have shown a collection of specimens of sulphur from southern Utah, I herewith present some notes relating to the mines and the method of extracting the sulphur from the ore. In preparing these notes I have borrowed from a paper by Prof. G. vom Rath, published in the Neue Jahrbuch fur Mineralogie, vol. i., 1884, dated Salt Lake City, December, 1883. The Cove Creek sulphur-bed, now worked by the Dickert & Myers Sulphur Co., is in Beaver county, near the line of Millard county. It was first discovered by Mr. Ferdinand Dickert in 1869 ; other beds in the same neighborhood mere found by him from 1872 to 1875, making altogether 22 mining claims. The want of railroad communication prevented the early development of these claims; but in 1883 Mr. F. Dickert put up a plant for extracting sulphur from the ore, which proved a perfect success; and in 1885 the property was transferred to a stock company organized under the laws of Utah. The railroad station nearest to the Cove Creek mines is Black Rock, on the Utah Central Railroad, 204 miles south from Salt Lake City, and about 26 miles west of the mines. The road from Black Rock to the mines passes through desert and lava-bed, to the road leading from Kanosh to Beaver, which latter road it joins near Cove Creek fort, a square stone enclosure, erected by the Mormons for protection against the Indians. Cove Creek fort is situated near the eastern limit of a plain bounded on the west at a distance of about 12 miles by the Mineral range, and on the east by the Sulphur mountains, forming part of the Tushar mountains. To the northwest the plain runs into the Sandy desert. About 3 miles from the fort rises a solitary hill about 1000 feet above the

Jan 1, 1888

ANY suitable characterization of the Utah Copper enterprise (now the Utah Copper Division of Kennecott Copper Corporation) involves the use of superlatives. If comparative records were compiled, after the fashion of baseball, the big opencut mine at Bingham Canyon, Utah, undoubtedly would hold dozens of championships in the mining world. For example, a few can be set down as follows: (1) The mine is the biggest man-made hole (excavation) in the crust of the earth! At the end of 1955 the total quantity of material moved (ore and overburden) was 1,673,000,000 tons or approximately 800,000,000 cubic yards. This is about3% times the yardage of earth moved in the original digging of the Panama Canal. It exceeds by fifty per cent the quantity dug in the justly famous Hull-Rust Mahoning open-pit iron mine on the Mesabi Range in Minnesota. (2) It holds first place among the mines of the world as to aggregate tonnage of ore mined and milled (734,000,000 tons at the end of 1955). (3) It holds first place among the mines of the world as to the aggregate quantity of metal produced (13,047,000,000 Ib- 6,523,500 tons-of refined copper). This is more than the actual production of all the mines in the United States during the eight-year period 1948 to 1955 inclusive. (4) In 1943, Utah established these world records: Tons of ore milled in a 24-hr day.. ................. 108,000 Tons of ore and waste moved in a 24-hr day.. ....... 235,000 Tons of ore milled in one month. ................... 3,074,000 Tons of ore milled in a year. ....................... 35,375,000 Pounds of copper produced in a year……….. 639,0000,000

Jan 1, 1957