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ford manual transmission truck for salePlease choose a different delivery location or purchase from another seller.Please choose a different delivery location or purchase from another seller.Please try again. Please try your request again later. Now this widely acknowledged classic provides the foundation for an interactive, multimedia tutorial CD-ROM. The CD features color photographs of over 125 minerals; 3-D Models and Animations that permit users to view crystal symmetries, internal order, and molecular structure; and simulations, to illustrate basic principles of crystallography, crystal chemistry, and the systematic mineralogy of common rock-forming minerals. Chemical substitutions permit users to evaluate solid solution within crystal structure formulas, and hyperlinks link textual terms with graphic representation. Then you can start reading Kindle books on your smartphone, tablet, or computer - no Kindle device required. Full content visible, double tap to read brief content. Videos Help others learn more about this product by uploading a video. Upload video To calculate the overall star rating and percentage breakdown by star, we don’t use a simple average. Instead, our system considers things like how recent a review is and if the reviewer bought the item on Amazon. It also analyzes reviews to verify trustworthiness. Please try again later. LeviD 4.0 out of 5 stars It doesn't have a lot of the tables and graphs as a newer edition of Dana's Manual but it still has a lot of the same quality of information. After all not much has changed in the world of Mineralogy. It wasn't as big as a normal textbook so it takes up less room in my bag. Seller Review: The book was in slightly better condition than was advertised, and it is a very good book. The only slight problem I had was the shipping length, but that was more of the carrier's fault than the seller. Seller shipped book on the next business day. I paid for expedite shipping and assumed it was 2-3 business days, and it was 5 business days.https://www.cuisinermanger.fr/proshop/images/festo-spc-100-manual.xml
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Normally I wouldn't care, but when you are trying to study for an exam everyday matters.He LOVES mineralogy and already has several books on the subject. He immediately began devouring this book, following me around telling me all the 'interesting' things he's learning. (I don't really mind, it is nice to see him enthusiastic about something other than a video game.) The book might be considered a 'Mineralogy 101' and has been a very good textbook to introduce the science to my budding mineralogist. Not really having the same interest, I wouldn't be able to tell you if the book would be a good reference for someone already familiar with mineralogy. The discussions on mining techniques also caught his interest. All in all, I'm very pleased with my purchase, and so is my nephew.It could have been written more concisely, perhaps more simplisticly, but all the information is there, and from what I understand, past editions were more comprehensive than this 22nd edition. And yes, I agree with the previous posts regarding certain statements about crystal structures that require some sort of base level knowledge of chemistry or physics or math (i.e. symmetry concepts) in order to fully comprehend a particular passage, but that's what you get from an Ivy League PhD-er. I believe this text was designed for the third year student who should already have taken 1 semester each of at least chemistry and calculus. Although calculus isn't necessary for the class, it presupposes that you know and understand some basic conceptual geometry. I would suggest reading some basic introduction to mineralogy websites before tackling this book. Other texts simply do not cover as much material as found here, such as x-ray diffraction and optics. Still, a great text. Try getting some olders editions with less sub-subjects edited out for a real comprehensive text!I was told the 22nd edition would suffice since I could not afford the 23rd edition.http://www.sps.agro.pl/userfiles/festo-pneumatic-cylinder-manual.xml For those of you who are in the same boat and trying to cut corners, dont buy this book. I am not commenting on the quality of the book at all, I'm sure it is an excellent textbook. I am just warning those who expect to follow along in a class using the next edition. Its not just a matter of different page numbers or chapters, there is whole chapters missing.Authored by an old pro. Please try again.Please try again.Please try again. Please try your request again later. Includes outstanding illustrations, hand specimen photographs and transmission electron microscope structure projects. Then you can start reading Kindle books on your smartphone, tablet, or computer - no Kindle device required. Includes outstanding illustrations, hand specimen photographs and transmission electron microscope structure projects.Full content visible, double tap to read brief content. It also analyzes reviews to verify trustworthiness. Please try again later. R. Swenson 5.0 out of 5 stars It covered all the topics I was interested in and then some. For example, it provides a concise review of chemistry that I found extremely helpful (been years since I had a chemistry class). I found the writing style easy to follow with a lot of illustrative sketches. If you are going to buy just one book on mineralogy, I would recommend this one.The next level for the serious rockhound.Mineralogy hasn't changed much in 60 years. This is a clear and insightful book that makes a great reference.Brilliant reference book!Page 1 of 1 Start over Page 1 of 1 Previous page Next page. The first page of the PDF of this article appears above. NOTE: We only request your email address so that the person you are recommending the page to knows that you wanted them to see it, and that it is not junk mail. We do not capture any email address. AAAS is a partner of HINARI, AGORA, OARE, CHORUS, CLOCKSS, CrossRef and COUNTER. Science ISSN 1095-9203.http://seasailing.us/node/2402 To protect our access to ETAS, the physical copy is temporarily not requestable. This edition comes with a CD-ROM. (source: Nielsen Book Data). Book and Media Review Dana's Manual of Mineralogy (Hurlbut, Jr.; Cornelius S.) Alonzo W. Quinn Cite this: J. Chem. Educ. 1952, 29, 10, 532 Publication Date (Print): October 1, 1952 Publication History Citations are the number of other articles citing this article, calculated by Crossref and updated daily. Find more information about Crossref citation counts. The Altmetric Attention Score is a quantitative measure of the attention that a research article has received online. Clicking on the donut icon will load a page at altmetric.com with additional details about the score and the social media presence for the given article. Find more information on the Altmetric Attention Score and how the score is calculated. Ratnawulan Ratnawulan, Ahmad Fauzi. Synthesis and Characterization of Forsterite (MgLogin with ACS ID Please reconnect By continuing to use the site, you are accepting our use of cookies. Read the ACS privacy policy. Close this message to accept cookies or find out how to manage your cookie settings. Total loading time: 0.206. Render date: 2021-07-06T01:42:15.341Z. Has data issue: true. Published online by Cambridge University Press: An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.Information. View more sellers starting from ? 4,664 Specifications Book Details Imprint Literary Licensing, LLC Dimensions Width 23 mm Height 226 mm Length 152 mm Weight 658 gr Read More Have doubts regarding this product. Post your question Safe and Secure Payments. Easy returns. 100 Authentic products. Request full-text Download citation Copy link Link copied Request full-text Download citation Copy link Link copied To read the full-text of this research, you can request a copy directly from the author. Request full-text PDF Citations (95) References (0). Microstructural examination of the gypsum powder ( Fig. 1) shows the appearance of flake-like structure of different sizes... Gypsum is found in the various forms such as calcium sulphate dihydrate (CaSO 4 A2H 2 O), calcium sulphate hemihydrate (CaSO 4-0.5H 2 O) and calcium sulphate anhydrite (CaSO 4 AH 2 O). The present article reviews the physico-chemical behaviour of gypsum, sources of gypsum in the soils, and also reveals the misconceptions on the suitable terminology used for soil containing gypsum. Further, the various methods proposed to identify the gypsum containing soil are discussed. The problems due to the phase transformation and its solubility characteristics of gypsum on the different construction activities are also reviewed in brief. The purpose of present article is to acquaint the impact of gypsum in the properties of different soils and to bring out the different methods available for stabilizing the gypsum containing soil. The refinements herein proposed aim to help understand the various aspects of gypseous soil and to institute the further research to be done in this topic. View Show abstract. Olivine is composed of a mixture of the magnesium-rich forsterite (Mg 2 SiO 4 ) and the iron-rich fayalite (Fe 2 SiO 4 ). Olivine has an orthorhombic structure with an independent SiO 4 tetrahedra linked by divalent ions in 6-fold coordination (Klein and Hurlbut, 1993). Serpentine (Mg 3 Si 2 O 5 (OH) 4 ) consists of a group of common rockforming hydrous magnesium phyllosilicate minerals... In all its polymorphs, lizardite, antigorite, and chysotile are the most common serpentine minerals found in nature. The structure of serpentine consists of an overlapping sheet of SiO 4 tetrahedra and a sheet of Mg octahedral (brucite-like) in which the -OH base is bonded (Klein and Hurlbut, 1993). Both olivine and serpentine make up the dominant contents of mine waste rock and tailings in ultramafic deposits, such as nickel mines, diamond mines, PGE mines and former asbestos mines (Hitch et al., 2010)... This is mainly the result of the link between the grinding limit and the type of materials in use. The Moh's hardness for serpentine is 2.5-4 and olivine is 6.5-7 (Klein and Hurlbut, 1993). The presence of serpentine content results in an easier aggregation for TAW than TSO.. Ultra-fine grinding and mechanical activation of mine waste rock using a planetary mill for mineral carbonation Article Jan 2017 INT J MINER PROCESS Jiajie Li Michael Hitch In order to mitigate the effects of climate change, a worldwide effort is being launched to use ultramafic mine waste as feedstock for CO2 sequestration by mineral carbonation. To enhance the rate of mineral carbonation at any specific mine site, it is important to develop individualized methods for use at that specific mine site, and with respect to its particular waste mineralogy. This study examines mechanical activation as the pre-treatment method for ultramafic mine waste containing forsterite and serpentine. Particle size distribution, specific surface area, microstructure and direct aqueous mineral carbonation were measured to test the effects of mechanical activation. The Rietveld method was used to analyze the microstructure of untreated and mechanically-activated material. It was found that, as a result of the grinding energy input on olivine, particle size was decreased, surface area was increased, crystallite size was reduced and micro-strain was accumulated. During the dry mechanical activation of mine waste, serpentine content was partially dehydrated and converted to olivine. The concurrent grinding of serpentine with olivine promoted the formation of new surface area, but it hindered the disordering of the crystal structure of forsterite. Forsterite makes up the majority of the content and contributes to CO2 sequestration under selected carbonation conditions. For the purposes of mineral carbonation, the mechanical activation of mine waste is preferable to simply grinding pure olivine. The essential minerals of Chalki basalt to andesitic basalts are plagioclase (labradorite, An 51-61; andesine, An 35 to An 42; and oligoclase, An 22). Moreover, there is sodic plagioclase (albite, An 0.1 to An 04) whose coexistence with the other more calcic plagioclase means that albitization had occurred. The other essential mineral is pyroxene (endiopside, en 66-68 wo 27-28 fs 05-06; and subcalcic augite, en 72 wo 14 fs 14). Olivine (Fo 80-81) is also present. According to the NiO content (0.11-0.12 wt) in olivine grains, they are interpreted to be originated tectonically. The prevalent chlorite in all the samples is mainly diabantite and penninite, indicating chloritization after the ferromagnesian olivine and pyroxene. Serpentine (type lizardite and chrysotile) is also recorded as lesser alteration product after the forsteritic olivine. Rare secondary hornblende (type magnesiohornblende) is also found. The spinel group as accessory minerals is defined as magnetite, chromian magnetite, and chromian spinel giving the imprints of their metamorphic origin due to low temperature sub-sea metamorphism and also of alpine type. These ARDs are generated as abundant pyrite becomes exposed to atmospheric conditions as a result of glacier retreat. The proglacial zone contains lagoons, springs, streams and wetlands, scant vegetation, and intense fluvioglacial erosion. This work reports a comprehensive identification and the results of sampling of the lagoons and springs belonging to the microbasin, which is the headwaters of the Pachacoto River, as well as mapping results based on the hydrochemical data obtained in our study. The physical properties and water chemistry of 12 springs and 22 lagoons from the proglacial zone are also presented. Fe-SO4(-2) concentrations confirm the intense process of pyrite oxidative dissolution. The affected lagoons show higher concentrations of SO4(2-) and SiO2, and elements as Fe, Al, Mg, Mn, Zn, Co, and Ni, which are related to the alteration of pyrite and the dissolution of aluminosilicate minerals. Schwertmannite-goethite appears to be the most important mineral phases controlling the Fe solubility at a pH of 2-3.5. Moreover, they act as a sorbent of trace elements (As, Sb, V, Pb, Zn, Cr), which is an efficient mechanism of natural attenuation. The Pachacoto River located 5.5 km downstream from this point showed a strong natural attenuation, with a pH of 6.9 and low concentration of metals. This mitigating process is possible due to (i) the formation of precipitates that retain toxic elements and (ii) the mixing with natural waters that promote dilution, which favor the increase of pH until circumneutral conditions. Igneous rocks are the major constituent of the Earth's crust and are formed by the crystallization and solidification of molten magma. For the application of Asaad's model (equation (7)), Veerendra and Chaudhary model (equation (8)), Pande and Chaudhary model (equation (9)), Zeb et al.Igneous rocks are one of the major constituents of the Earth’s crust and are formed by the crystallization and solidification of molten magma. In this work, the thermal transport properties of porous igneous basalt rocks are measured using Transient Plane Source (TPS) technique under ambient conditions with air as saturant in pore spaces. Data are presented for fifteen samples of volcanic basalt rocks having different porosity values ranging from 0.267 to 9.432 by volume, taken from the place of Warsak near Peshawar city, located in the north of Pakistan. The porosity and density parameters are measured using the American Society of Testing and Materials (ASTM) standards. The mineral compositions of the samples are analyzed by X-ray fluorescence (XRF) technique. The specific gravity is predicted using the chemical composition of basalts and is compared with the experimental results. The thermal conductivity and thermal diffusivity values of the measured samples are also predicted using the mixing law and empirical models and results are compared with the measured data. Results show that the thermal conductivity of the studies of basalt samples decreases with the increase in porosity values, whereas no significant change has been observed in the thermal diffusivity data. Measured data are significant for geothermal modeling and in predicting heat losses in buildings wherever basalt rocks are used. Long term residency of fibres in the lung can result in asbestosis (fibrosis) and may lead to lung cancer or mesothelioma (Ross, 1981). Klein and Hurlbut, 1993). General compositional fields are shown as shaded areas and representative tielines across miscibility gaps are included.. Electron microscope investigation of fibrous amphiboles in selected samples from Hawks Nest, Giffen Well and Sequioa iron ore deposits, northern Gawler Craton, South Australia Technical Report Full-text available May 1998 John L Keeling Stuart Mcclure Twelve drill hole samples from iron ore prospects at Hawks Nest, Giffen Well and Sequoia in the northern Gawler Craton, South Australia were examined by scanning electron microscope for the presence of asbestiform amphiboles. Asbestiform actinolite was identified in a late stage cross-cutting amphibole vein in one sample from the Kestrel deposit at Hawks Nest. Six samples contained amphibole showing either cleavage or close-spaced parting that had the potential to produce variable amounts of acicular fibres of a size small enough to be respirable. Fibrous amphibole associated with banded iron formation in the Gawler Craton presents a potential health hazard to workers involved in any future mining, milling and tailings disposal operations involved with development of these resources. A code of practice should be developed and implemented for drilling, sampling and storage of samples from iron ores suspected of containing asbestiform amphiboles. The choice of a particular method depends on the properties of raw materials, the melting temperature and size requirements. The resulting material is distinguishable from natural opal by its regularity; under magnification, the patches of color are seen to be arranged in a lizard skin or chicken wire pattern.. Development of glass-ceramics from soda lime silica glass waste by sintering method for opal imitation Article Jan 2017 D. Bootkul Nattawat Kulrat Somsak Dangtip Saweat Intarasiri Natural opal, an amorphous, hydrous form of silica (SiO2-n-H2O), has been one of the favored precious gemstones for many centuries. Though beautiful, opal is very fragile and is damaged quite easily. Thus, opals of all varieties have been synthesized experimentally and commercially. The objective of this project was to synthesize and to compare crystalline opals. In this work, the development of powder sintered glass ceramics process based on soda-lime-silica glass waste with silica powder enable jewelry applications. There is a great potential for such materials with novel functionalities for artificial gemstone application, i.e. opal forming. Several techniques were applied for characterizing the ingots. The chemical analysis was performed by Energy Dispersive X-ray Fluorescence (ED-XRF). The mineralogical compositions of the samples were determined by X-ray diffraction analysis. Raman spectroscopy was applied for optical characterization. The results were compared with a natural common opal. The present experiments demonstrated that the common milky opal can be synthesized by the technique, as the crystalline phase of opal structure was identified by XRD measurement. Devido a ausencia de dados especificos referentes a composicao dos plagioclasios das principais unidades litologicas da area, foi estabelecido, com base nos dados ponderados de geoquimica ( de Na e Ca) das rochas da bacia, um plagioclasio com a seguinte composicao teorica (Tabela 6): Na 0,63 Ca 0,37 Al 1,37 Si 2,63 O 8.. Plagioclase Dissolution Rate in a Granite-Gneiss Watershed of a Moist Tropical Mountain Forest Article Full-text available Aug 2018 Amanda Cristine Santos da Costa Carla Semiramis Silveira William Zamboni de Mello C. B. D. PINTO A 180 ha area in the headwater of Paquequer watershed, a drainage system located at the Teresopolis municipality, was selected for the evaluation of chemical weathering from collected river water samples in February and August 2013 in a granitic-gnaissic substrate free of direct anthropogenic influence for being located in a conservation unit (Serra dos OrgaosNational Park). The study area has a native forest cover, an altitude range of 1100-1900 m and an average annual rainfall of 2800 mm. The dissolved elements (Na, Mg, Ca, K, Si, Al) were analyzed by inductively coupled plasma spectrometries and the anions. Cl and SO42-, by ion chromatography. These results, combined with the concentration data of nitrogen and phosphorus compounds (Alvim, 2016), the atmospheric deposition (Rodrigues, 2006), and the litogeochemistry (Zorita, 1979; Tupinamba, 1999; Tupinamba et al., 2012) were used to generate the dissolution model of mineral, employing the PHREEQC software. The mass balance indicate Na as the main chemical specie due to weathering. Mineralogical data show plagioclase, quartz, kfeldspar and biotite as substrate’s most abundant minerals, among which only plagioclase has sodium in its composition. According to Goldich’s series (mineral stability to weathering), plagio clase was identified as the main weathered mineral in this assemblage, being consumed at a rate of 649 mol ha-1year-1 and forming the minerals kaolinite and gibbsite, with the release of a minimum of Considering plagioclase as the main mineral responsible for Na flux in the basin, stoichiometric calculations in association with Si ratio, it was estimated that only from the plagioclase weathering, the soil should be composed by 14 of kaolinite and 86 of gibbsite in percentage relative of the two mineral phases. The quantitative analysis of the mineralogy (Rietveld method) confirmed the calculations, showing a soil composition 7 kaolinite e 93 gibbsite, and attested the importance of plagioclase weathering in fluvial hydrogeochemistry and soil composition. The experiment was conducted at two different soil depths: 5-10 and 50-55 cm from the surface. The parental rock used in the experiment is composed of dolomite and magnesite with variable proportion of accessory minerals and minor elements. Soil mineral and chemical composition as well as its texture was also characterized. Meteorological conditions at the site together with temperature and CO2 in both soil levels were monitored. Sets of tablets were retrieved after 6 and 12 months of the start of the experiment to account for seasonal weathering. Different lithologies do not have significant differences in weathering, although a large inter-sample variability is attributed to variable size and distribution of the porosity. Rock tablets examined under scanning electron microscopy prior and after exposure to natural environment show that most of the material lost occurred along cracks, edges or large porous. Although dissolution is a common process, most of the weathering is due to crystal detachment. Higher soil moisture and concentration of CO2 were found deeper in the soil, which likely enhanced the dissolution of carbonate. However, physical weathering dominated weight loss of rock tablets at both soil depths; especially at the 5- 10 cm level where soil thermal and moisture cycles were more frequent and ample. Since the conditions at the average contact between soil and bedrock are similar to those at the 50-55 cm depth, we consider that this is a more reliable denudation rate for the studied location during the studied period. The calculated weathering rate suggests that denudation has a limited contribution to the thinning of bedrock over caves at this site. Therefore, we consider that the formation of unroofed caves in this region most likely results from the thinning of bedrock cover over caves due to collapse of blocks from their ceilings. Plus recemment, l’interet sur l’activite sismique tout au long des systemes de failles associees aux limites de plaques, a conduit a la caracterisation du remplissage sedimentaire des bassins en environnement cotier avec un fort potentiel de preservation et donc d’enregistrement des deformations et perturbations liees a une activite tectonique.Le travail presente dans ce memoire a pour objective de developper une analyse du risque naturel, particulierement le risque de seismes et tsunamis dans la bordure nord de Venezuela, sur la trace sous-marine active de la faille decrochante d’El Pilar.Dans ce contexte la texture, mineralogie et geochimie de la sequence sedimentaire d’un petite appendice de la fosse de Cariaco appele golfe de Cariaco, a ete etudie a partir des differentes techniques (analyse de taille de particules, fluorescence X semi-quantitative, mesures de perte a feu, Pyrolise Rock-Eval et proprietes magnetiques). Comme resultat d’une caracterisation detaillee des sediments et d’un control chronologique detaille base sur la datation radiocarbonique et la correction de l’effet reservoir (potentiellement accumule sur les differents fractions organiques datees), nous avons mis en evidence un particulier depot silto-argileux, fortement detritique, d’une ample distribution spatiale, dont l’age le plus probable correspond au seisme historique de 1853, qui a affecte la ville de Cumana. On interprete la conjugaison de ces deux singularites comme la consequence d’un glissement sous-marin et d’une modification morphologique majeure concomitante dans le seuil qui connecte la fosse et le golfe de Cariaco. Dans cette chaine d’evenements, ce depot serait le produit de la decantation du sediment en suspension remobilise et l’augmentation du Br est la manifestation d’un changement hydrogeochimiquemarque pour une majeure influence marine sur le golfe. Pour etablir un point de reference pour l’evaluation du potentiel et de la qualite d’enregistrement de l’activite sismique dans le golfe de Cariaco, un deuxieme site lie a la plaque Caraibe fait partie de cette recherche. Il s’agit de l’arc des Petites Antilles, siege d’une activite sismique et volcanique importante, resultat d’une subduction. Les carottes ici prelevees et etudiees avec la meme approche sedimentologique, ont enregistre la trace d’un evenement sismique recent, plus probablement le seisme de Redonde de 1974. Cet evenement correspond a un depot silto-sableux, non stratifie et acoustiquement transparent. Les profils sismiques montrent que la relation geometrique de facies similaires (de faible energie) avec l’escarpement co-sismique, implique une origine seisme-induite, a difference des turbidites, dont leur origine peut etre influencee par la superposition complexe de plusieurs mecanismes declencheurs. However, other fractions, especially tailings from the processing of sulfide minerals such as pyrite (FeS 2 ), may cause environmental and ecological risks due to their oxidation tendency in the presence of water or air. The presence of sulfur compounds favors the occurrence of metal acid leaching, which contaminates water with bioaccumulative metals, rendering it unsuitable for domestic and agricultural use (Klein and Hurlbut, 1993; Evangelou 1995).. Biomining of iron-containing nanoparticles from coal tailings Article Full-text available Sep 2019 Appl Microbiol Biotechnol Danielle Maass Morgana De Medeiros Machado Beatriz Cesa Rovaris Dachamir Hotza Sulfur minerals originating from coal mining represent an important environmental problem. Turning these wastes into value-added by-products can be an interesting alternative. Biotransformation of coal tailings into iron-containing nanoparticles using Rhodococcus erythropolis ATCC 4277 free cells was studied. The influence of culture conditions (stirring rate, biomass concentration, and coal tailings ratio) in the particle size was investigated using a 2? full factorial design. Statistical analysis revealed that higher concentrations of biomass produced larger sized particles. Thus, the culture conditions that produced smaller particles ( View Show abstract. The Earth's crust is composed of 47 oxygen and 28 silicon, by weight. Mica is occasionally referred to as mineral clay, but it is in a separate mineral group (Klein and Hurlbut, 1993). Mica is mostly confused with illite, which is chemically similar to muscovite except that it has lower aluminium content and holds more water.. Evaluation of asphalt mastic containing mica due to aging Article Full-text available Jun 2016 P I CIVIL ENG-TRANSP Rafiqul A. Tarefder Umme Amina Mannan Md Arifuzzaman Asphalt concrete consists of coarse aggregate, fine aggregates, fillers and binder. Previous studies show that the presence of mica reduces the strength of asphalt concrete.