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Week 5 is here!! We are in the final stretch of The One Room Challenge. A challenge that seemed a piece of cake at the beginning… when 6 full weeks were ahead. Now, here we are, almost at the end of a great journey to a organized and happy pantry.
This week's post will be on the shorter side my friends. Well, maybe not, you know how I like to talk.
The Ceiling-
OH MY GOODNESS!! I promise every time I open the door- there it is… all kinds of happiness when I look up! Pictures just do not do it justice- but next week at the final reveal- I am determined to capture the sheer awesomeness. Pinky promise.
The new light is fabulous and going from a two bulb light to a three bulb light is spectacular! The space is now well-lit. The motion sensor lights under the stairs are working out splendidly. No dark cavernous areas here!
All the "oops" from painting are cleaned up and the grout looks beautiful. The rug has been located bought and placed! It looks great!! I went with a super durable, washable (at least that is what the reviews say). In order to get the length I wanted at the price I wanted – I ordered two smaller rugs and will bind them together with upholstery thread. I decided to go with a more subdued rug in a ticking stripe for two reasons: 1) the ticking stripe reminded me of days of old 2) the gentle pattern and lighter colors allow my ceiling to embrace her stardom.
MANY items have been arriving via Amazon for storage options (we will see what works and what goes back). Baskets received their second coat of paint and look gorgeous. Amazing what a little paint will do (hey- I say that about myself, lol ).
One of the big projects for this week dealt with all my reusable bags, coolers and lunch boxes. Before we took on the pantry, I had the bags on the ground and tried to keep them neat. With a busy household that "organization" last all of 5 minutes. As I stood in my under utilized little room 5 weeks ago and tried to imagine a place of peace and organized harmony, I had a lightbulb moment! "Why not find crates to store all my stuff?" and "Why not add wheels for ease?" My mind began to crank on the idea, I realized that a crate just would not simply do. The whole concept centered on having things feel clean and crisp- using crates would mean at least 4 would be needed. Let us not forget to mention how short they would be (even with castors). I would see all the clutter peaking out everytime I enter the room. No Thank you. Building storage boxes really was the only way to go. Take a gander:
See? Are they not perfect for the space? We measured and chit chatted until we figured out the "how to" part. Sleek hardware was ordered and arrived yesterday.
This weekend they will be painted the same color as the pantry shelves. I had to test them out and for their little shallow selves- WOW! They can hide some clutter! I will show you at the final reveal.
What's Left-
I had really hoped to cruise in on this last week but I will be pushing to finish this race (que "Chariots of Fire" music). Who knew that a little pantry would pack such a punch on time? I know I should know but I was soo hopeful y'all.
Ok, so to pull off this beauty I need to:
- Finish restocking (yes I am still at it, ha!)
- Bind the two rugs
- Paint the rolling bins
- Create the "Grocery List" board
- Add a little more artwork
- Label a few baskets and jars (more like 50 million)
- Make hooks for the aprons (these are going to be so cool)
- Photograph this beauty
If you would like to catch up on all the progress, come on. 🙂
Week 1, Week 2, Week 3, Week 4
If you would like to see 20 AMAZING blogger/designers take on this challenge with featured sponsors click here.
If you would like to see more AMAZING blogger/designers take on this challenge as guest participants click here.
I promise- you will find kindred spirits with genuine creativity.
Fingers cross and say a prayer for me.
Let's finish the race!
Till Later,


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A heavy suspension awaits Gold Coast defender Steven May when he fronts the AFL tribunal.
The match review panel predictably referred May to the tribunal, with no option of an early plea, for the bump that concussed Brisbane Stefan Martin.
GWS key forward Jeremy Cameron received a four-match ban last month for a similar incident that left Brisbane defender Rhys Mathieson with a jaw fracture.
May has a poor tribunal record, he ran past the ball to take out Martin in Saturday night's match and the incident sparked remonstration from the Lions – all factors that will count against him.
His advocate Tony Burns, who also represented Cameron, will do well if he can restrict May's rough conduct ban to less than five matches.
May and Suns football manager Marcus Ashcroft will fly to Melbourne for the late-Tuesday afternoon hearing at Etihad Stadium.
The Suns backman unsuccessfully went to the tribunal last year after he knocked out Brisbane captain Tom Rockliff.
May could have accepted a two-match rough conduct ban, but instead served a three-match suspension.
Also last year, he was fined $1000 for rough conduct against St Kilda's Jack Lonie.
The Martin bump was assessed as careless conduct and severe impact to the head.
May took his eyes off the ball and his feet were off the ground when he concussed the Brisbane ruckman.
May apologised immediately after the match and again on Sunday.
Martin is rated a chance to play this weekend and the lack of a serious injury will work in May's favour.
Suns captain Gary Ablett also pushed Martin from behind immediately before May cannoned into him.
West Coast ruckman Scott Lycett was offered a one-match ban for his punch to the face of Richmond's Ty Vickery in Friday night's clash at Domain Stadium.
The blow was graded as intentional and low impact.
Also on Monday, seven other players were offered $1000 fines.
Brisbane's Darcy Gardiner and Port Adelaide pair Robbie Gray and Charlie Dixon were charged with striking.
Collingwood onballer Taylor Adams and Power midfielder Hamish Hartlett were fined for rough conduct, while Carlton's Nick Graham and Joel Hamling from the Western Bulldogs were charged with wrestling each other.

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Banded iron formations (BIF) are the protolith to most of the world's largest iron ore deposits. Previous hypogene genetic models for Paleoproterozoic "Lake Superior" BIF-hosted deposits invoke upwards, down-temperature flow of basinal brines via complex silica and carbonate precipitation/dissolution processes. Such models are challenged by the necessary SiO2 removal. Thermodynamic and mass balance constraints are used to refine conceptual models of the formation of BIF-hosted iron ore. These constraints, plus existing isotope and halogen ratio evidence, are consistent with removal of silica by down- or up-directed infiltration of high-pH hypersaline brines, with or without a contribution from basinal brines. The proposed link to surface environments suggest that Paleoproterozoic BIF-ore upgrade may provide a record of a critical time in the evolution of the Earth's biosphere and hydrosphere.
Banded iron formations (BIFs) record changing environmental conditions and are a precursor to the world's largest iron ore deposits. Vast volumes of BIFs were deposited on passive margins from ca. 2.6 Ga to the Great Oxygenation Event (GOE) at ca. 2.4 Ga (e.g., Beukes and Gutzmer, 2008). After 1.85 Ga, formation of iron formations essentially ceased until a restricted resurgence in the late Neoproterozoic (Young, 1976; Klein and Beukes, 1993) and more recent minor occurrences.
The temporal distribution of BIFs records a complex interplay between a cooling Earth and changes in mantle plume events, continental growth and tectonics, evolution of the biosphere and an increased flux of iron to the hydrosphere, which in turn had a fundamental control on the oxygen contents of the hydrosphere and redox state of the oceans (Isley and Abbott, 1999; Holland, 2005; Bekker et al., 2010). In most giant Paleoproterozoic BIF-hosted iron ore deposits (∼35 wt% Fe) the formation of high-grade (>58 wt% Fe) iron ore from Lake Superior–type BIF is thought to have occurred post 2.2 Ga, after the GOE (Taylor et al., 2001; Rasmussen et al., 2007; Thorne et al., 2009), so the BIF-ore upgrade provides a record of the changing chemistry of the hydrosphere and atmosphere in the Paleoproterozoic.
In the Hamersley province, Western Australia, the BIF-ore upgrade is proposed to involve basinal brines, meteoric fluids, and supergene enrichment (e.g., Morris et al., 1980; Barley et al., 1999; Taylor et al., 2001; Thorne et al., 2004, 2008). Silica removal is proposed to occur by upward, down-temperature flow of basinal brines (e.g., Thorne et al., 2004; Gutzmer et al., 2006; Thorne et al., 2008), and it is this stage of the BIF-ore upgrade that is explored in this paper.
The challenge for models that involve removal of SiO2 from BIF by down-temperature flow is that quartz solubility decreases with decreasing temperature (e.g., Manning, 1994), so fluid that moves down-temperature is a poor agent for quartz removal, unless large volumes of fluids enter the BIF in a silica-undersaturated state. Here, we combine numerical constraints with petrological, geochemical and isotopic characteristics of BIF-hosted iron ore from the Hamersley province, Western Australia, to constrain the conditions associated with silica loss and carbonate precipitation, and discuss the findings in the context of the temporal evolution of the world's atmosphere and oceans.
The mineralogy of BIF, hydrothermally altered BIF, and iron ore varies (e.g., Thorne et al., 2004; Rosiere et al., 2008; Mukhopadhyay et al., 2008; Angerer and Hagemann, 2010) but some features are sufficiently common to allow generalization. BIF protolith (Figs. 1A, 1B1, and 1B2) consists of magnetite- and chert-rich bands, iron silicates ± diagenetic carbonates. Initial hydrothermal alteration (Figs. 1A, 1B3, and 1B4), which may be gradational, involves conversion of some of the silicates to carbonates. Subsequently, chert and quartz are replaced by iron-bearing carbonate with, in some cases, conversion of magnetite to hematite, often with no apparent change in volume. Reaction fronts may be gradual (millimeter to decimeter scale) or knife-sharp on the scale of individual bands. Quartz may be precipitated locally in fault zones within shear veins (e.g., Hagemann et al., 1999; Thorne et al., 2010).
The carbonate-bearing alteration assemblage (Figs. 1A, 1B5, and 1B6) is separated from almost pure (hypogene) hematite iron ore (Figs. 1A, 1B7, and 1B8) by a sharp or gradational reaction front. Carbonate loss is thought to occur without iron mobility on a scale greater than a few cm (Taylor et al., 2001). Carbonate dissolution continues in the weathering environment.
Upgrade of BIF in the Hamersley province, Western Australia, is thought to have occurred from 2.15 Ga onwards during the waning stages of the Opthalmian orogeny (Rasmussen et al., 2007). There is evidence for extensional faulting and orogenic collapse at the proposed time of ore upgrade (Müller et al., 2005) and it has been suggested that topographic relief drove circulation of surface-derived waters through the fault system at this time (e.g., Hagemann et al., 1999; Oliver and Dickens, 1999).
Constraints on ore upgrade in the Hamersley are provided by fluid inclusion, isotopic, and halide concentration measurements. Fluid inclusions in carbonates are hypersaline, up to 24 wt% CaCl2 equivalent, which were trapped at temperatures between 150 and 400 °C (Thorne et al., 2004; Brown et al., 2004), mainly at the lower end of this range. Quartz-hosted fluid inclusions (e.g., Brown et al., 2004) records periods of quartz growth, not quartz removal, so such inclusions may record either a different event, or a later stage of the silica dissolution event that is of interest here.
Iron oxide oxygen isotopes in unaltered BIF have δ18OVSMOW (Vienna Standard Mean Ocean Water) between 4‰ and 13‰, whereas hematite and magnetite in altered and mineralized rocks have δ18OVSMOW between −9‰ and −2.9‰ (Thorne et al., 2009). Carbon isotopes of carbonate minerals lie between −10‰ and 0‰, relative to Vienna Peedee belemnite (VPDB). The lower values are typical of unaltered BIF. Values in altered rocks could record equilbrium with either Paleoproterozoic ocean water or dolomite in the underlying Wittenoom Formation. Fluid inclusion Na/Br and Cl/Br ratios record overlapping populations of fluids: (1) seawater that has evaporated to halite saturation; and (2) meteoric waters that interacted with evaporites (Thorne et al., 2010).
Fluids in Equilibrium with BIF
Quartz solubility is sensitive to pressure, temperature (e.g., Manning, 1994), pH (Busey and Mesmer, 1977), and salinity (e.g., Shmulovich et al., 2006). Quartz and carbonate solubilities were calculated as a function of pressure, temperature and salt content (Fig. 2) using the methods outlined in the GSA Data Repository1. Calcite, rather than iron carbonate was used for the models because data for iron carbonates is sparse, but similar trends for iron carbonates are expected. Temperature is the first order control on quartz solubility, whereas calcite solubility depends strongly on pressure (Fig. 2A). Salinity-driven mineral precipitation/dissolution is minor for geothermal gradients <50 °C km−1 (Fig. 2B). There is no geothermal gradient for which silica dissolution is accompanied by carbonate precipitation in the observed quantities, so it is necessary to consider infiltration of out-of-equilibrium fluids.
Fluid out of Equilibrium with BIF
Relative positions of carbonation, desilicification, and oxidation fronts were calculated using the values given in Table DR1 (in the Data Repository), which are based on the assumption of infiltration an out-of-equilibrium, pH 9, SiO2-free, CO2-rich, O2-bearing fluid (O2 at 10% of present-day values). Front positions were normalized to that of the most advanced carbonation front (Fig. 1B). The oxidation front is predicted to proceed the smallest distance, as observed, though the position of this front is modified by post-hypogene meteoric fluid and supergene processes. The carbonation front is predicted to advance further than the desilicification front for any reasonable combination of input parameters. In reality, the desilicification front coincides with a sharp increase in carbonate content, which suggests a reaction-induced porosity control on fluid infiltration.
Volumes of Fluid Flow
Flow volumes were calculated for a single cubic meter of rock undergoing pH-driven quartz dissolution and scaled to estimate the volume needed to produce the observed SiO2 depletion on a scale comparable to observed small iron ore deposits (3 × 108 m3). The volume of fluid required is approximately ∼109 m3.
The observed silica removal and carbonate precipitation needed for formation of a kilometer-scale BIF-hosted Fe deposit is inconsistent with in-equilibrium fluid flow (Fig. 2), but could be produced by pervasive infiltration of ∼109 m3 of a high pH (pH > 9) fluid flowing up- or down- temperature.
Density- or topography-driven infiltration (McLellan et al., 2004) of dense hypersaline brines evolved on continental margins (Fig. 3) provides a plausible source of high-pH fluid. The pH of hypersaline lakes today is up to 10, and the CO2 content is high; reported alkalinities exceed 10,000 mg L−1 (Gosselin et al., 1994). These brines form on marginal platforms (Leach et al., 2010) and were present on the north Yilgarn margin in the Palaeoproterozoic (El Tabakh et al., 1999) and in Mesoproterozoic dolomitic argillites in the western United States (Gonzalez-Alvarez and Kerrich, 2011). The Yilgarn and Pilbara cratons may not have been adjacent at the time of ore formation, and the latitude of the Pilbara margin at that time is poorly known but existing constraints place the latitude within the range of those required for evaporite formation (Li, 2000). Fault zones in similar environments today are sufficiently permeable that proposed volumes could have flowed on a geologically reasonable timescale (Jones et al., 2002).
Carbon and oxygen isotopes of early carbonate and iron oxides in mineralized BIF are consistent with seawater derivation from Palaeoproterozoic seawater. High salinities and Na/Br and Cl/Br ratios record fluids typical of seawater that has evaporated to halite saturation (Thorne et al., 2010), which is also consistent with an involvement of evaporite-derived fluids. Temperatures of up to 250 °C are consistent with fluid inclusion evidence, and with other environments where voluminous quantities of surface-derived fluids infiltrate basement rocks (e.g., Gleeson and Yardley., 2003). However, temperatures >300 °C recorded by early assemblages at Mount Tom Price require a separate high-temperature alteration stage. SiO2 deposition in outflow zones from the flow system described have not been recorded, to date, but may prove difficult to recognize given that chert was a common sedimentary rock at this time.
Some geometric constraints in mineralized Pilbara BIFs favour an upwards flowing fluid (e.g., Dalstra and Rosiere, 2004). The Wittenoom Formation underlies many of the ore-bearing units, and has been proposed as a way for basinal brines to access the BIF (e.g., Taylor et al., 2001). Dolomite in the Wittenoom Formation contains numerous shale bands (Davy, 1975), and is separated from the BIF by the Si-bearing Mount McRae shale and Sylvia Formation, so fluids from this unit would be at, or close to, SiO2 saturation, unless fluids were focused solely within shale-free regions of the dolomite, such as the Paraburdoo Member (Thorne and Tyler, 1997). If this were the case then the dolomite in the Wittenoom Formation could have acted as an aquifer that supplied overlying iron formations with fluids derived either from faults that focused either down-flowing evaporitic brines with or without a contribution from upward-flowing basinal brines, as suggested by previous workers (e.g., Taylor et al., 2001).
Mafic and ultramafic rocks are present in the Pilbara (e.g., Barnes and Hoatson, 1994) and can equilibrate with water to provide high pH fluids, but such fluids are unlikely to have reached the BIF without interacting with Si-bearing rocks such as the Mount McRae shale.
Oxidized, sulfur-bearing, hypersaline brines produced on basin margins since 2.0 Ga have been linked to base metal sulfide deposition, including MVT (Mississippi Valley type) and SEDEX-Pb-Zn deposits (Leach et al., 2010). Such deposits older than 2.02 Ga have not been found; Archaean and Paleoproterozoic oceans were reduced and largely sulfur-depleted (e.g., Farquhar et al., 2010), so marginal hypersaline brines at 2.2 Ga, at the time of ore upgrade, could have had a significantly different composition to those today. It is interesting to speculate whether redox controls related to mobilization, transport, and deposition of Pb and Zn by Palaeoproterozoic evaporite-derived brines, such as a lack of sulfur (Leach et al., 2010) lack of oxidized source rocks and aquifers, or reduction of sulfate via rock-buffering in the immediate sub-surface, may have prevented formation of these deposit types prior to 2.02 Ga.
We thank Rob Kerrich, Hilke Dalstra, and an anonymous reviewer for perceptive, knowledgeable reviews. Thanks for funding and support are due to a Curtin Research and Teaching Fellowship, Australian Research Council Discovery DP1090475 to Evans, and Core to Crust Fluid Systems funding to McCuaig and Hagemann. This is TiGeR publication number 423.


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Ahon Sa Hirap, Inc. Recognized as a Truelift Aspirant
Truelift announced this week that it has recognized Ahon Sa Hirap, Inc. (ASHI) with it's Aspirant Milestone. Truelift cites ASHI's committment to rigorous standards and good practices in serving the poor and tracking client outcomes:
"ASHI has established a strong Social Performance Management Framework by using the Progress out of Poverty Index (PPI) developed by Grameen Foundation. It has defined a clear population target using the PPI score and is working toward its mission. The PPI is also used to track the progress made by their clients out of poverty between cycles. Its good practices using the PPI have allowed ASHI to obtain a PPI Basic & Advanced PPI certification in 2011."


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Some say that an excellent bra can last in between 6 months to a year, depending upon how often it is used and washed. To make bras last for a long period of time, they must be alternated and cleaned up with lingerie wash-- by hand or in an underwear bag-- then hung to dry.
But the concern still stays: How does one know precisely when to obtain rid of an old bra? Well, it's easy: Pay attention to the clues the bra is giving!
5 Tell-Tale Sings You Required a New Bra:
Cups: Your breasts must fill the cups of your bra without any excess spilling over or any gaping. If there is space in between your breasts and the cups, you might need to tighten your bra straps.
Band: The band covers completely around the body. When buying a brand-new bra, the band needs to feel tight on the loosest hook setting. If there is a lot of area or if you are able to easily pull your bra away from your body from the front, then the band is too big.
Gore: The gore, or center front piece of the bra between the cups, should lay flat versus your body. If the gore is coming off of your body, then the cups of your bra are too small.
Wings: The wings are the 2 parts of the bra that wrap around your body and attach in the back. There need to be at least 1/4 inch of space between one's armpit and the top of the wing.
5. Straps: Straps are not the greatest area of support on a bra; 90% of support originates from the band. However, if your straps are constantly dropping even after tightening them, it might be due to the fact that your band is too huge and riding up in the back, causing your straps to slide off your shoulders. If your straps are digging into your shoulders, you need a smaller sized band size and a larger cup.
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Crushing Equipment
- PE Jaw Crusher
- PEW Jaw Crusher
- PF Impact Crusher
- PFW Impact Crusher
- PY Cone Crusher
- HJ Series Jaw Crusher
- HPC Cone Crusher
- HPT Cone Crusher
- HST Cone Crusher
- CS Cone Crusher
- Hammer Crusher
- VSI Crusher
- VSI5X Crusher
Grinding Equipment
- Raymond Mill
- Ball Mill
- LM Vertical Grinding Mills
- LUM Ultrafine Vertical Roller Mill
- MTM Trapezium Grinder
- MTW Milling Machine
- SCM Ultrafine Mill
- T130X Reinforced Ultrafine Mill
Feeding & Conveying
Screening & Washing
Portable & Mobile
- Hydraulic-driven Track Mobile Plant
- K Series Mobile Crushing Plant
- Mobile Cone Crusher
- Mobile Impact Crusher
- Mobile Jaw Crusher
Beneficiation Equipment
Mineral Processing Plant
- Barite processing plant
- Basalt stone processing plant
- Bauxite processing plant
- Calcite mining and processing plant
- Carbon grinding plant
- Clay processing plant
- Coal beneficiation plant
- Construction Recycle Plant
- Copper ore beneficiation plant
- Dolomite stone processing plant
- Feldspar processing plant
- Feldspar stone processing plant
- Gold ore concentration plant
- Granite stone processing plant
- Gypsum mining equipment
- Iron ore beneficiation plant
- Kaolin processing plant
- Limestone crushing plant
- Limestone Processing Plant
- Manganese processing plant
- River stone processing plant
- Sand Making Plant
- Silica sand processing plant
- Silver mining plant
- Talc processing plant
Customer Case
- 150-200TPH Cobble Crushing Plant
- 300TPH Cobble Crushing Line In Russia
- Aggregates for Concrete in Nigeria
- Andesite Crushing Plant In Indonesia
- Copper Ore Crushing Plant in Chile
- Crushing Plant in Mali
- Granite Crushing Plant in Sri Lanka
- Laos iron ore processing plant
- Limestone and Granite Crush Plant in Iran
- Limestone Crushing Line in Algeria
- Limestone Grinding in Belgium
- Pebble and Basalt Production Line in Panama
- Rod Mill Grinding Line in China
- Sand Making Plant Designed by SKY in UAE
- Tungsten Crusher in Kazakhstan
- Ultrafine Powder Milling Plant in India
- Vietnam 300TPH Granite Crushing Plant
- Vietnam 350-400TPH Cobble Crushing Plant
If you do not find what you need, you can choose to chat online, we can customize for you, provide all the solutions.Chat Online
Established in 1987, SKY has had 30 years of experience in mining machine industry. So far, SKY has complete R&D, production , sales and service system, becoming a distinguished manufacturer in mining machine industry and competing the world market with global famous enterprises.
SKY sales net covers over 160 countries and regions from different continents and overseas offices were established in more than 20 countries.
Mill scale - Wikipedia
Mill scale, often shortened to just scale, is the flaky surface of hot rolled steel, consisting of the iron oxides iron(II) oxide (FeO), iron(III) oxide (Fe2O3), and iron(II,III) oxide (Fe3O4, magnetite) , Thus mill scale can be removed from steel surfaces by flame cleaning, pickling, or abrasive blasting, which are all tedious operations.Know More
Enhancing the Kinetcs of Mill Scale Reduction: An Eco-Friendly ,
6 Aug 2013 , N B Dhokey ENHANCING THE KINETICS OF MILL SCALE REDUCTION: , Sample Boat Mill • Chemical Weight Analysis To determine percentage by weight , Element Actual Values (%) 1 Fe 9689 2 Si 099 RESULTS AND , reaction "v" can be related RESULTS AND DISCUSSIONS Vantoff Equation.Know More
Study of Kinetics of Mill Scale Reduction: For PM Applications ,
8 Aug 2014 , Recovery of iron powder from iron oxide in mill scale could be , Vantoff equation was used for determining the first-order kinetics of the.Know More
Generation Transport and Uses of Mill Scale | ispatguru
23 Sep 2014 , Mill scale is the flaky surface of hot worked steel and is formed by , The FeO content is determined separately by a wet chemical , for the determination of metallic iron in direct reduced iron that can be applied to mill scalKnow More
Recycling of electric arc furnace (EAF) dust for use in steel making ,
16 Jul 2014 , , consisting of EAF dust agglomerate to coke particles, mill scale and ceramic , by calcium ferrite (spinel CaFe2O4) and magnetite (Fe3O4), which is, the , the lower percentage of the EAF dust in the mixture results in the , to identify the mechanism to optimize the removal of zinc mill scale was not usedKnow More
Mill Scale, Ferrous Waste Streams and Other Recycled Minerals
Mill Scale and other by-products such as slags and powders , Many factories mix a few percentages of this material with their iron ore fines before they are , We can supply higher grade materials for steel making or lower grades for cement use , FE-Mat-2 Keep our website bookmarked and check back for updated bulk.Know More
Patent US4995912 - Mill scale de-oiling - Google Patents
Mill scale can account for up to about six (6) weight percent of the total iron , published in Technische Mittellunger Krupp, Forschungsberichte, volume 33, no , 571 496 567FeO 160 146 283 150 154Met Fe <1 <1 <1 <1 04Fe2 O3.Know More
Corrosion Terminology - C's - NACE International
carbonsteel—alloyof carbon and iron containing up to 2 mass percent , cementite—iron carbide(Fe3C) when referred to as a microstructural constituent of steel , checking—thedevelopment of slight breaks in a coating that do not penetrate to , isswabbed onto a steel surface to determine whether mill scale is presentKnow More
Treating Or Using Mill Scale Patents and Patent Applications (Class ,
Method of manufacturing Fe and Ni containing material, ferronickel mass , the liquid waste can be maintained to a pH level of 05 to 25; precipitating Fe , In this manner, it is possible to produce mill scale briquettes of high strength and density , Office and the public generally to determine quickly from a cursory inspection.Know More
Relationship between grinding time of mill scale and the , - Ijser
the physicochemical properties and the degree of reduction of mill scale briquettes via , Mechanical activation pretreatment of minerals by intensive milling can improve the , The number of drops was determined for each briquette , Oxygen mass: indicates the mass of oxygen percent in mill scale in the form of FeO andKnow More
What exactly is Mill Scale and what is done about it - Finishing
In order to discuss this issue knowledgeably I would like to know: , A Mill scale consists primarily of magnetite, Fe3O4, of characteristic blue-gray "steely" colorKnow More
Indian Standard: GUIDELINES FOR UTILIZATION AND DISPOSAL ,
, basis, as it is the right of all humans to know and speak the laws that govern them , For example, solid wastes which are to be recycled to sintering plant should be , Mill Scale—While steel ingots or other sections are heated in soaking pits or , Fe = 32-35, SiO2 = 7-9 Al2O3 = 6-7, MgO = 3-4 C = 21-24 (80-90 percent.Know More
Conversion of Mill Scale Waste into Valuable Products via , - Hindawi
30 Aug 2015 , The results reveal that mill scale waste can be converted into , was dumped in landfills and resulted in leaching of some percentages of , Al2O3, and Na2CO3) chemical compositions were determined , As indicated from XRD analysis the constituents of mill scale were Fe2O3, Fe3O4, and FeO phasKnow More
Effect of processing parameters on scale formation during hot steel ,
The principal phase of the scale formed in hot-rolled steel strips is stoichiometric , tertiary scale forms on the steel surface after descaling or between each mill stand, , The thickness of these three phases will be different with the changes of , for the Fe sites detected, were the same for all the samples and the percentage.Know More


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University Tutorial Services
Fall Semester 2017
Tutoring services will soon be active for this Fall semester, with upcoming: Tutor Hiring & Training, Course Support listing, Session Schedules Established, and Start-up on August 30th.
Announcements or Operational Issues:
Tutoring requests will be accepted beginning at 9am the first day of classes Tuesday, August 22nd, in person via the lab manager on duty in Rm. 208 D. D. Dougherty Hall. Scheduling confirmation will begin as new fall schedules are posted by tutors, with the first start-up sessions beginning on Wednesday, August 30th. Tutors participate in start-up training during the first week, and this time is also set aside for them to establish their own academic life and personal transition to the semester. As you wait on your sessons to begin, attend class, take good notes and keep up with your reading. Your professor will also inform you of their office hours on the first day of class. Take advanage of all resources as you begin this fall semester!
We will do our best to accommodate requests to the degree possible. Keep in mind that our services are funded primarily for freshman and sophomore course support, and tutor hiring and availability is also based on the level of demand (requests) for particular coursework.
For more information you may call 262-3060 from 9am-8pm Monday-Thursday, 9am-5pm Friday, or email us at firstname.lastname@example.com. We typically do not ask or expect tutors to alter their posted times to meet tutee needs. Please plan on attending all (weekly) sessions to maintain your position on their schedule. If you feel you no longer need assistance, you may officially drop your spot with advance notice.
How to request appointment based tutoring
To request a tutor and schedule a tutoring session, students must complete a Request for Tutoring form which is located in the tutoring lab (room 208 D. D. Dougherty). The tutoring lab is staffed to receive requests Monday through Thursday, 9am-8pm, and Fridays 9am-5pm.
With the assistance of the tutoring lab manager, a tutoring session will be scheduled and the student will complete a Tutee Contract form. This form clarifies what is expected of students attending sessions, provides the tutor's name, and specifies the date and time of the appointment. Tutors are given 48 hours notice in from the time of scheduling to the appointment date. No-shows or repeated cancellations will result in the student being removed from the tutor's schedule and may jeopardize future access to tutoring services. If no spots are currently available that work for you, your request form is placed in an "Active Hold" file and our lab managers will continue to check your request for matches as new times are posted. Though we will make every attempt to keep you informed as to the status of your request, you are welcome at any time to check back in with us or to alter the times that you are available.
Help Labs - Tutoring that occurs in a group setting on a drop-in basis
If you are unsure about the need for a regular appointment and just want a setting to work on your assignments and ask questions as they arise, you may want to consider attending a Departmental Help Lab . These centers have posted hours and do not require you to commit to regular attendance. The University Writing Center does require an appointment. Click on the UWC link to get information about this great resource in Rm. 204 of Belk Library.
About Your Tutor
Your tutor has been approved by the academic department relative to your course and has either been trained in learning skills or has demonstrated proficiency in these areas. The University Tutorial Services places a high priority on hiring tutors with patience, strong communication skills, and a pleasant personality.
Your tutor will challenge you to do your best and will expect you to come to your sessions prepared, focused and directed. They are to serve as your guide as you work to understand the concepts and complete your assigned work. Tutors will not complete assignments for students and are free to terminate a session(s) if they feel you are placing inappropriate expectations on them. Tutors may ask you to consider making changes in your study habits and/or your behaviors related to classroom learning.


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In manufacturing & distribution, safety is an area of top concern, for both the protection of workers and financial ramifications for companies. We spent some time at ProMat with Kelly Kamlager from Ladder Industries to examine the importance of safety and compliance for industrial companies.
Safety – A Manufacturing & Distribution Hot Button
November 3, 2015
by Scott Stone
Tags: hiring, OSHA, Safety & Ergonomics, warehousing
Posted in Material Handling, News, ProMat, Safety & Ergonomics| No Comments »


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Active Database Software News
FlySpeed Database Tools
FlySpeed DB Migrate 3.4 is released.
July 11, 2017
We're glad to announce the new minor version of FlySpeed DB Migrate. The new version is available for download at the download page.
What's new in FlySpeed DB Migrate v. 3.4?
- Support for MS SQL Server 2016 and Azure SQL Database has been added.
- Other minor improvements and bug fixes are made.
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Latest Comments
"I am very confused as to how much yarn to buy. please explain"
"This is very unusual. These are adorable. I read the instructions and it's very easy to make. I have everything I need to make them so these are going on my to do list. I should make two pair because my best friend will see mine and want a pair too. Thank you for sharing this one."
"She said " 61/5000 I love!!! It's very cute and super easy. Thank you very much )""
"These are adorable. I read the instructions and it's very easy to make. I have everything I need to make them so these are going on my to do list. I should make two pair because my best friend will see mine and want a pair too. Thank you for sharing this one."
Open Wide Zippered Pouch
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You'll love this Open Wide Zippered Pouch for storing your everyday essentials. You can keep your keys, makeup, pens, phone, wallet, and anything else you need during the day right in the palm of your hand with this DIY clutch purse. Your daughter or granddaughter can also use DIY accessories like this to store their pens and pencils for school. It's so versatile!
Use fabric scraps you have laying around your craft room to put together this easy sewing pattern. By using scraps, your pouch is sure to be one-of-a-kind.
If you liked this pouch made out of fabric scraps, you'll love these 43 Scrap Fabric Projects
Estimated CostUnder $10
Time to CompleteIn an evening
Primary TechniqueFabric Crafts
Project TypeMake a Project
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Sep 13, 2017
this tutorial makes use of scraps! That's amazing. I can get some scaps because I really need another clutch.
Marilyn B
Jun 06, 2017
I made this cute little zippered clutch for my daughter out of an animal print fabric scrap and lined it with a stiff interfacing and interior lining fabric. I put a fabric tab on the zipper and also included a little simple pocket inside for extra storage. She loves it! Thank you for a super idea and instructions!
May 26, 2017
This type of pouch has so many different uses. Plus, it's a great way to use up old scraps.
Jun 01, 2016
I love making something useful out of my old scraps. Great pattern!
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Autumn Harvest Pumpkin Tea Cozy
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Safety First: String of Sexual Attacks by Ride-Sharing Drivers Prompts Congressional Action
On March 18, 2015 By Ryan Dewey March 19, 2015
Congress took another step this week in ensuring that we all have safe rides home on Saturday nights. A group of Congressional Democrats penned a letter to the CEOs of Uber, Sidecar, and Lyft demanding that the companies require their drivers to undergo more thorough background checks. This letter comes in the wake of [...]Continue Reading →
The Dangers of Dating Websites
On April 21, 2011 By Yoshana Jones April 23, 2011
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The popularity of dating websites has increased in recent years due to their easy accessibility to users and the busyness of working professionals. We have all seen the dating websites' commercials that virtually promise that your true love is only a mouse-click away. The couples appear to be in love while kissing [...]
Your Past May Haunt You @ CriminalSearches.com
On August 5, 2008 By JETLaw August 5, 2008
Do you want to find out more about your next door neighbor? Considering accepting a date but want to make sure your potential suitor isn't a weirdo? Worried about your new friend's erratic behavior? While in the past it was very difficult to obtain criminal conviction records without traveling to courthouses and getting past [...]Continue Reading →
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