Academic literature on the topic 'Phosphate rock Florida'

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Journal articles on the topic "Phosphate rock Florida"

1

Liang, Haijun, Patrick Zhang, Zhen Jin, and David DePaoli. "Rare Earth and Phosphorus Leaching from a Flotation Tailings of Florida Phosphate Rock." Minerals 8, no. 9 (2018): 416. http://dx.doi.org/10.3390/min8090416.

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Phosphorite, or phosphate rock, is the raw material of phosphoric acid production. It has also been regarded as the most important secondary rare earth element (REE) resource due to low contents of rare earth elements contained in the ore. In Florida, there is about 19 Mt of phosphate rock mined annually. After beneficiation, the phosphate rock concentrate is utilized to produce phosphoric acid via a wet-process in which sulfuric acid is used to digest phosphate. During these processes, REEs and some phosphorus get lost in the byproducts including phosphatic clay, flotation tailings, phosphogypsum (PG), and phosphoric sludge. Recovering REEs and phosphorus from these wastes is beneficial to maximize the utilization of these valuable resources. This study focused on the effects of wet-process operating conditions on REE and phosphorus leaching from a kind of flotation tailing of Florida phosphate rock. The tailings were first beneficiated with a shaking table, and then a series of leaching tests were conducted on the shaking table concentrate. The results indicated that REEs had similar trends of leaching efficiency to those of phosphorus. Under the conditions of 16% phosphoric acid concentration in the initial pulp, a temperature of 75 °C, a stoichiometric ratio of sulfuric acid (H2SO4) to calcium oxide (CaO) of 1.1, and a weight ratio of liquid to solid of 3.5, REE and phosphorus leaching efficiencies reached relatively high values of approximately 61% and 91%, respectively. Analyses indicated that the phosphate ions (PO43−) in the leaching solution tended to combine with REE ions to form REE phosphates which precipitated into PG, but the other large amount of anions such as sulfate ions (SO42−) and fluoride ions (F−) took effect of steric hindrance to prevent PO43− from combining with REE cations. These two opposite effects determined the REE distribution between the leaching solution and PG.
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2

KUCEY, R. M. N., and M. E. LEGGETT. "INCREASED YIELDS AND PHOSPHORUS UPTAKE BY WESTAR CANOLA (Brassica napus L.) INOCULATED WITH A PHOSPHATE-SOLUBILIZING ISOLATE OF Penicillium bilaji." Canadian Journal of Soil Science 69, no. 2 (1989): 425–32. http://dx.doi.org/10.4141/cjss89-042.

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Greenhouse and field experiments were conducted to evaluate the effect of inoculation with a phosphate-solubilizing isolate of Penicillium bilaji on the yield and phosphate uptake by canola (Brassica napus L.). Under greenhouse conditions, P. bilaji inoculation did not affect canola pod or straw dry matter production, but did increase straw and pod P concentrations resulting from increased P uptake over uninoculated treatments. Addition of P at 20 mg kg−1 soil as Florida rock phosphate plus inoculation with P. bilaji resulted in P uptake by canola nearly equivalent to that resulting from the addition of monoammonium phosphate (MAP) alone at the same rate of P. Addition of Florida rock phosphate alone had much less effect on plant P uptake. Addition of P. bilaji generally increased dry matter yields and P uptake by canola in two field sites. Penicillium bilaji appears to be able to increase the uptake of P from sources unavailable for plant uptake; P uptake by control plants inoculated with P. bilaji absorbed as much P as that absorbed by uninoculated plants receiving MAP. Key words: Penicillium bilaji, Brassica napus, fertilizer efficiency, rock phosphate, monoammonium phosphate
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3

Blanchard, Frank N., Robert E. Goddard, and Barbara Saffer. "Application of Quantitative X-Ray Diffraction Analytical Methods to the Study of High-Magnesium Phosphorites." Advances in X-ray Analysis 29 (1985): 235–42. http://dx.doi.org/10.1154/s0376030800010314.

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Phosphorite is a sedimentary rock with a high enough content of phosphate minerals to bo of economic Interest. Most phosphorites are composed predominantly of m1crocrystall1no to cryptocrystalline carbonate fluorapatlte thenceforth In this report referred to simply by the mineral group name apatite). Florida produces roughly 1/3 of the world's supply of phosphate rock, most of which is used 1n the fe rtiliz e r Industry.Long term continuation of phosphorite mining In Florida will require exploitation of the extensive hlgh-magneslum phosphorite deposits south of the present mining d istrict 1n central Florida, and this will require new technology In order to produce beneficlated concentrates with less than 1% MgO, a limit Imposed by fe r tiliz e r processing technology. In order to develop benefication methods applicable to these ores, it is essential to know how Mg occurs in phosphorites. Dolomite, CaMg(C03)2, is the chief host of Mg In phosphorites from Florida. Magnesium may also be present, however, as a substituent In apatite (the chief phosphate.mineral in these deposits), as a minor substituent 1n calcite (CaCO3), in certain clay minerals (particularly palygorskite and to a lesser extent in some smectites), and/or in organic matter within the apatite particles.
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4

He, Z. L., H. Yao, D. V. Calvert, et al. "Dissolution characteristics of central Florida phosphate rock in an acidic sandy soil." Plant and Soil 273, no. 1-2 (2005): 157–66. http://dx.doi.org/10.1007/s11104-004-7400-5.

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5

Yeager, Thomas H., and Charles R. Johnson. "Response of Podocarpus macrophyllus to Rock Phosphate and Mycorrhizae." Journal of Environmental Horticulture 3, no. 4 (1985): 168–71. http://dx.doi.org/10.24266/0738-2898-3.4.168.

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Shoot and root dry weights of greenhouse-grown mycorrhizal and nonmycorrhizal Podocarpus macrophyllus were not different after 8 months. Shoot dry weights were not different for plants grown in the 2 pine bark: 1 moss peat: 1 sand (v/v/v) medium amended with Florida rock phosphate (14% P) at either 0.54, 1.08, 2.16, 4.32, or 8.64 mg P/cm3 (14.5, 29, 58, 116, or 232 oz P/yd3, respectively) of medium (2300 cm3/container) or 0.27 mg P/cm3 (7.25 oz P/yd3) from superphosphate (9% P). Root dry weights for plants grown without a P amendment were greater than for plants grown with rock phosphate amendments of 0.54 and 1.08 mg P/cm3. Growing medium extract P levels 51 days after potting and thereafter were 2 ppm or less for the rock phosphate treatments, while P levels for the superphosphate-amended mediunl decreased from 169 ppm on day 51 to 9 ppm on day 236. Phosphorus accumulated by shoot and root tissues exhibited a similar relationship to shoot and root dry weights.
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6

Dodor, Daniel E., Yoshihiro Tokashiki, Kazuhiro Oya, and Moritaka Shimo. "Dissolution of phosphate rock fertilisers in some soils of Okinawa, Japan." Soil Research 37, no. 1 (1999): 115. http://dx.doi.org/10.1071/s98061.

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The ability of phosphate rock (PR) to dissolve rapidly in soil is a primary concern in its direct application as P fertiliser. The dissolution of 4 PR materials (Togo, South Africa, Florida, Morocco PRs) in 15 soil samples in Okinawa was investigated in a closed-incubation system for 7 days. The fertilisers were mixed with the soils at rates of addition of 600–1200 µg Ca/g soil. The extent and rate of dissolution of the PRs were determined by measuring the increase in extractable Ca of the fertilised soils compared with unfertilised soils, i.e. the delta Ca (ΔCa) technique. Generally, the amounts of dissolution of 3 of the PRs were very low (mean 6·7% for Togo PR, 13·6% for South Africa PR, and 20·8% for Florida PR). However, Morocco PR dissolved to an appreciable extent (mean 60·8%), suggesting that it can be an alternative P source, especially in the red and yellow soils of Okinawa. Soil properties identified as affecting dissolution were different for the different PRs. In order to predict the suitability of Morocco PR for Okinawan soils, the extent of its dissolution was related to soil properties in a multiple regression analysis. Results indicated that the best regression model for predicting the amount of dissolution was the combination of pH, Ca saturation, and Truog P (r2 = 0·55**). Measured values of percentage dissolution of Morocco PR were significantly correlated with calculated percentages (r = 0·844***), indicating that the equation obtained could offer a rapid estimation of amount of dissolution of Morocco PR in Okinawan soils.
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7

Liang, H., P. Zhang, Z. Jin, and D. DePaoli. "Rare-earth leaching from Florida phosphate rock in wet-process phosphoric acid production." Minerals & Metallurgical Processing 34, no. 3 (2017): 146–53. http://dx.doi.org/10.19150/mmp.7615.

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8

Mao, Xiaoyun, Qin Lu, Wei Mo, Xiaoping Xin, Xian Chen, and Zhenli He. "Phosphorus Availability and Release Pattern from Activated Dolomite Phosphate Rock in Central Florida." Journal of Agricultural and Food Chemistry 65, no. 23 (2017): 4589–96. http://dx.doi.org/10.1021/acs.jafc.7b01037.

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9

Al-Wakeel, Mohamed I., C. L. Lin, and Jan D. Miller. "Significance of liberation characteristics in the fatty acid flotation of Florida phosphate rock." Minerals Engineering 22, no. 3 (2009): 244–53. http://dx.doi.org/10.1016/j.mineng.2008.07.011.

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10

Laurino, Joseph P., Jack Mustacato, and Zachary J. Huba. "Rare Earth Element Recovery from Acidic Extracts of Florida Phosphate Mining Materials Using Chelating Polymer 1-Octadecene, Polymer with 2,5-Furandione, Sodium Salt." Minerals 9, no. 8 (2019): 477. http://dx.doi.org/10.3390/min9080477.

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To meet the growing global demand for rare earth elements (REEs), nontraditional mining sources of these metals are being investigated. Phosphate ore and phosphate mining wastes have been identified as possible alternative sources to REEs. In this study, REEs were extracted from Florida phosphate mining materials using mineral and organic acids. The REEs were then recovered at high efficiencies using a chelating polymer, 1-octadecene, polymer with 2,5-furandione, sodium salt. At pH 1.5, the chelation polymer effectively bound nearly 100% of the rare earth elements extracted from the solids. Overall extraction and recovery yields were between 80% for gadolinium and 8% for praseodymium from amine tailings, between 70% for terbium and 7% for praseodymium from phosphogypsum, between 56% for scandium and 15% for praseodymium from phosphate rock, and between 77% for samarium and 31% for praseodymium from waste clay. These results suggest that this chelating polymer efficiently recovers rare earth elements from acidic extracts of phosphate mining waste products.
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Books on the topic "Phosphate rock Florida"

1

El-Shall, Hassan E. Characterization of future Florida phosphate resources: Final report. Florida Institute of Phosphate Research, 1994.

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2

Cathcart, James Bachelder. Mineralogy and chemistry of samples from drill hole in the southern extension of the Land-Pebble Phosphate District, Florida: Economics of phosphate mineralogy and chemistry in an area of possible future mining. U.S. G.P.O., 1991.

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3

Burnett, William C. Release of radium and other decay-series isotopes from Florida phosphate rock: Final report. The Institute, 1988.

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4

Wilemon, G. M. Leaching of phosphate values from two central Florida ores using H₂SO₄-methanol mixtures. U.S. Dept. of the Interior, Bureau of Mines, 1987.

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