Mineralogy and Alteration of the Phosphate Deposits of Florida
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2.0 Current Freight Rail System and Services in Florida
Investment Element of the 2010 Florida Rail System Plan 2.0 Current Freight Rail System and Services in Florida 2.1 Overview The Florida rail system is comprised of 2,786 miles of mainline track, which are owned by 15 operating line-haul railroads and terminal or switching companies, as well as 81 miles owned by the State of Florida. Florida’s rail system includes 2 Class I Railroads (CSX Transportation and Norfolk Southern Corporation), 1 Class II (Florida East Coast Railway), 11 Class III (Alabama and Gulf Coast Railway AN Railway, Bay Line Railroad, First Coast Railroad, Florida West Coast Railroad, Florida Central Railroad, Florida Midland Railroad, Florida Northern Railroad, Georgia and Florida Railway, Seminole Gulf Railway, and South Central Florida Express) and 1 railroad specializing in switching and terminals (Talleyrand Terminal).9 The largest operator in the State is CSX Transportation, which owns more than 53 percent of the statewide track mileage. In 2008, Florida’s railroads carried nearly 1.6 million carloads – 19 percent less than in 2006 – and approximately 83 million tons of freight, representing a 25 million ton (23 percent) decrease from 2006.10 During that year, railroads handled freight equivalent to roughly 5.0 million heavy trucks.11 Nonetheless, railroads continue to support thousands of jobs throughout the State and assist Florida’s industries to remain competitive with international and domestic markets for fertilizer, construction rock, consumer goods, paper products, processed 9 U.S. Class I Railroads are line-haul freight railroads with 2007 operating revenue in excess of $359.6 million (2006 operating revenues exceeding $346.7 million). -
Kosnarite Kzr2(PO4)3 C 2001-2005 Mineral Data Publishing, Version 1
Kosnarite KZr2(PO4)3 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal, pseudocubic. Point Group: 32/m. As rhombohedral pseudocubic crystals, to 0.9 mm, with {1012} and tiny {0001}. Physical Properties: Cleavage: Perfect on {1012}. Fracture: Conchoidal. Tenacity: Brittle. Hardness = 4.5 D(meas.) = 3.194(2) D(calc.) = 3.206 Optical Properties: Transparent to translucent. Color: Pale blue to blue-green, bluish gray, nearly colorless. Streak: White. Luster: Vitreous. Optical Class: Uniaxial (+). ω = 1.656(2) = 1.682(2) Cell Data: Space Group: R3c. a = 8.687(2) c = 23.877(7) Z = 6 X-ray Powder Pattern: Mt. Mica, Maine, USA. 4.329 (100), 3.806 (90), 2.928 (90), 6.41 (50), 4.679 (50), 2.502 (50), 1.903 (45) Chemistry: (1) (2) (3) P2O5 43.3 42.2 42.04 ZrO2 44.5 47.9 48.66 HfO2 0.5 0.9 FeO 0.2 < 0.1 MnO 1.0 < 0.1 Na2O 1.4 < 0.1 K2O 8.7 9.25 9.30 Rb2O 0.25 0.2 F 0.20 0.2 −O=F2 0.08 0.08 Total 99.97 100.57 100.00 (1) Mt. Mica, Maine, USA; by electron microprobe, total Fe as FeO, total Mn as MnO; corresponds to (K0.93Na0.08Rb0.01)Σ=1.02(Zr1.81Na0.15Mn0.07Fe0.01Hf0.01)Σ=2.05 [P1.02(O3.98F0.02)Σ=4.00]3. (2) Black Mountain, Maine, USA; by electron microprobe, total Fe as FeO, total Mn as MnO; corresponds to (K0.99Rb0.01)Σ=1.00(Zr1.96Hf0.02)Σ=1.98 [P1.00(O3.98F0.02)Σ=4.00]3. -
Geology of the Hugo Pegmatite Keystone, South Dakota
Geology of the Hugo Pegmatite Keystone, South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-B Geology of the Hugo Pegmatite Keystone, South Dakota By J. J. NORTON, L. R. PAGE, and D. A. BROBST PEGMATITES AND OTHER PRECAMBRIAN ROCKS IN THE SOUTHERN BLACK HILLS GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-P A detailed structural and petrologic study of a pegmatite containing seven zones and two replacement bodies UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page Abstract.. _ ________________________________________ 49 Mineral distribution and paragenesis of the entire Introduction. ______________________________________ 49 pegmatite_ _ ______________________-___---------_ 96 General geology. ___________________________________ 52 Comparison of the zonal sequence with that in other Metamorphic rocks_ ____________________________ 52 pegmatites. ______________________________________ 97 Roy and Monte Carlo pegmatites.- _ __---__-______ 53 Replacement features-______________________________ 100 Structure __________________________________________ 53 Review of the evidence for replacement in pegma Pegmatite units ____________________________________ 53 tites __ _____________________________________ 100 Zone 1 : Albite-quartz-musco vite pegmatite ________ 56 Replacement in the Hugo pegmatite.____-_____-_- 102 -
Exhibit Specimen List FLORIDA SUBMERGED the Cretaceous, Paleocene, and Eocene (145 to 34 Million Years Ago) PARADISE ISLAND
Exhibit Specimen List FLORIDA SUBMERGED The Cretaceous, Paleocene, and Eocene (145 to 34 million years ago) FLORIDA FORMATIONS Avon Park Formation, Dolostone from Eocene time; Citrus County, Florida; with echinoid sand dollar fossil (Periarchus lyelli); specimen from Florida Geological Survey Avon Park Formation, Limestone from Eocene time; Citrus County, Florida; with organic layers containing seagrass remains from formation in shallow marine environment; specimen from Florida Geological Survey Ocala Limestone (Upper), Limestone from Eocene time; Jackson County, Florida; with foraminifera; specimen from Florida Geological Survey Ocala Limestone (Lower), Limestone from Eocene time; Citrus County, Florida; specimens from Tanner Collection OTHER Anhydrite, Evaporite from early Cenozoic time; Unknown location, Florida; from subsurface core, showing evaporite sequence, older than Avon Park Formation; specimen from Florida Geological Survey FOSSILS Tethyan Gastropod Fossil, (Velates floridanus); In Ocala Limestone from Eocene time; Barge Canal spoil island, Levy County, Florida; specimen from Tanner Collection Echinoid Sea Biscuit Fossils, (Eupatagus antillarum); In Ocala Limestone from Eocene time; Barge Canal spoil island, Levy County, Florida; specimens from Tanner Collection Echinoid Sea Biscuit Fossils, (Eupatagus antillarum); In Ocala Limestone from Eocene time; Mouth of Withlacoochee River, Levy County, Florida; specimens from John Sacha Collection PARADISE ISLAND The Oligocene (34 to 23 million years ago) FLORIDA FORMATIONS Suwannee -
O Lunar and Planetary Institute Provided by the NASA Astrophysics Data System WHITLOCKITE SATURATION
WHITLOCKITE SATURATION IN LUNAR BASALTS, J.E. Dickinson and P.C. Hess, Dept. of Geological Sciences, Brown University, Providence, RI 02912 As part of a continuing program initiated to evaluate the evolution of late-stage lunar magmas and the possible effects of crystallization of minor phases on their geochemistry, we have determined the saturation surface for whitlockite, Ca (PO ), in a liquid composition produced by crystallization of KREEP basalt 15386 lf~able1). Whitlockite is by far the most abundant phos- phate mineral in lunar rocks and in all probability is more abundant than other minor phases such as zircon, zirccnolite, monazite, and tranquillityite (1). Whitlockite is also an important component of mesosiderites, reported average modal phosphate abundances in mesosiderites ranging from 0.0-3.7% (avg. 1.9%) (2). Even higher phosphate abundances (up to 9.4%) have been observed in basaltic lithic clasts of presumed impact melt origin found in mesosiderites (3). Analyses of lunar whitlockites commonly show Ce203and Y203 contents up to 3 wt% and REE contents that may be as high as 1-2 wt% for La203and Nd203 de- creasing to levels of -0.1-0.2 wt% for the HREE (1). It has been shown that whitlockite is generally more enriched in REE's relative to chondrites than other minor phases in the same rock (4). Uranium and thorium may also be present in significant amounts although other minerals may contain more. Whit- lockite may, therefore, be an important reservoir of rare earth and heat producing elements. In addition, the amount of FeO and MgO in whitlockite is variable (Table 1). -
Validation of Zeolites to Maximize Ammonium and Phosphate Removal from Anaerobic Digestate by Combination of Zeolites in Ca and Na Forms Page 1
Validation of zeolites to maximize ammonium and phosphate removal from anaerobic digestate by combination of zeolites in Ca and Na forms Page 1 Abstract Ammonium and phosphate are fundamental nutrients for human life, but their excess in water can lead to eutrophication, an uncontrolled growth of biomass with a consequent deficit of oxygen (hypoxia) that can be really dangerous for water life. This excess is principally due to human activities such as industry and agriculture (detergents, fertilizers) and the problem is expected to grow during next years. Then, it is necessary to find an efficient, simple and low cost technology able to remove the nutrients from water in order to avoid environmental damages. Moreover, the population growth, the constant improvement in agriculture and the consequent increase in fertilizers demand have made the recovery of nutrient from water a real need, as it has been estimated that a 20% of the total needs of Europe could be recovered from wastewaters. Although both ammonium and phosphate have to be recovered from wastewater, their simultaneous removal by means of one adsorbent material has rarely been reported hitherto. The merit of using one material for the simultaneous removal is obvious, even if it has not been achieved yet. In general, most of the solutions proposed for the simultaneous removal of ammonium and phosphate are based on the use of two types of reagents. A large list of removal technologies, ranging from biological to physic-chemical methods, have been widely studied: in this work, zeolites in Ca and Na forms were evaluated as sorbents for phosphate and ammonium from synthetic water and real anaerobic digestate. -
2004 Freight Rail Component of the Florida Rail Plan
final report 2004 Freight Rail Component of the Florida Rail Plan prepared for Florida Department of Transportation prepared by Cambridge Systematics, Inc. 4445 Willard Avenue, Suite 300 Chevy Chase, Maryland 20815 with Charles River Associates June 2005 final report 2004 Freight Rail Component of the Florida Rail Plan prepared for Florida Department of Transportation prepared by Cambridge Systematics, Inc. 4445 Willard Avenue, Suite 300 Chevy Chase, Maryland 20815 with Charles River Associates Inc. June 2005 2004 Freight Rail Component of the Florida Rail Plan Table of Contents Executive Summary .............................................................................................................. ES-1 Purpose........................................................................................................................... ES-1 Florida’s Rail System.................................................................................................... ES-2 Freight Rail and the Florida Economy ....................................................................... ES-7 Trends and Issues.......................................................................................................... ES-15 Future Rail Investment Needs .................................................................................... ES-17 Strategies and Funding Opportunities ...................................................................... ES-19 Recommendations........................................................................................................ -
Tulane Studies Tn Geology and Paleontology Pliocene
TULANE STUDIES TN GEOLOGY AND PALEONTOLOGY Volu me 22, Number 2 Sepl<'mber 20. l!J8~) PLIOCENE THREE-TOED HORSES FROM LOUISIANA. WITH COMMENTS ON THE CITRONELLE FORMATION EAHL M. MANNING MUSP.UM OF'GEOSCIF:NCE. LOUISJJ\NA STATE UNIVF:RSlTY. JJATO.\I ROI.JG/<. LOL'/S//\;\':1 and llRUCE J. MACFADDlrn DEJ>ARTM/<:NTOF NATUH/\LSCIENCES. F'LORJD/\ MUSf:UM Of<'NJ\TUIV\/, lllSTOUY UNIVERSITY OF FLOH!IJJ\. GJ\/NESVlU.E. Fl.OH/DA CONTENTS Page T. ABSTRACT 3.5 II INTRODUCTION :l5 Ill. ACKNOWLEDGMENTS :rn TV . ABBREVIATIONS :l7 V. SYSTEMATIC PALEONTOLOGY ;37 VI. AGE OF THE TUNICA HILLS HIPPARIONINES 38 VIL STRATIGRAPHIC PROVENIENCE 38 Vlll. PLIOCENE TERRESTRIAL VERTEBRATES OF THE GULF AND ATLANTIC COASTAL PLAIN .JO IX. COMMENTS ON THE CITRONELLE FORMATION .JI X. AGE OF THE CITRONELLE 42 XL TH E CITRONELLE FORMATION IN nm TUNICA HILLS .t:1 XII. LITERATURE CITED l.J January of 1985, the senior author was L ABSTRACT shown a large collection of late Pleistocene Teeth and metacarpals of early Pliocene (Rancholabrean land-mammal agel ver (latest Hemphillian land-mammal age) tebrate fossils from the Tunica Hills of three-toed (hipparionine) horses are de Louisiana (Fig. I) by Dr. A. Bradley scribed from the Tunica Hills of West McPherson of Centenary College, Feliciana Parish in east-central Louisiana. Shreveport. McPherson and Mr. Bill Lee An upper molar perta ins to Nannippus of Balon Rouge had collected fossils from minor, known from the Hcmphillian of that area since about 1981. Among the Central and North America, and two teeth standard assemblage of Rancholabrean and two distal metacarpals pertain to a re taxa (e.g. -
Monazite, Rhabdophane, Xenotime & Churchite
Monazite, rhabdophane, xenotime & churchite: Vibrational spectroscopy of gadolinium phosphate polymorphs Nicolas Clavier, Adel Mesbah, Stephanie Szenknect, N. Dacheux To cite this version: Nicolas Clavier, Adel Mesbah, Stephanie Szenknect, N. Dacheux. Monazite, rhabdophane, xenotime & churchite: Vibrational spectroscopy of gadolinium phosphate polymorphs. Spec- trochimica Acta Part A: Molecular and Biomolecular Spectroscopy, Elsevier, 2018, 205, pp.85-94. 10.1016/j.saa.2018.07.016. hal-02045615 HAL Id: hal-02045615 https://hal.archives-ouvertes.fr/hal-02045615 Submitted on 26 Feb 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Monazite, rhabdophane, xenotime & churchite : vibrational spectroscopy of gadolinium phosphate polymorphs N. Clavier 1,*, A. Mesbah 1, S. Szenknect 1, N. Dacheux 1 1 ICSM, CEA, CNRS, ENSCM, Univ Montpellier, Site de Marcoule, BP 17171, 30207 Bagnols/Cèze cedex, France * Corresponding author: Dr. Nicolas CLAVIER ICSM, CEA, CNRS, ENSCM, Univ Montpellier Site de Marcoule BP 17171 30207 Bagnols sur Cèze France Phone : + 33 4 66 33 92 08 Fax : + 33 4 66 79 76 11 [email protected] - 1 - Abstract : Rare-earth phosphates with the general formula REEPO4·nH2O belong to four distinct structural types: monazite, rhabdophane, churchite, and xenotime. -
Mineral Collecting Sites in North Carolina by W
.'.' .., Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie RUTILE GUMMITE IN GARNET RUBY CORUNDUM GOLD TORBERNITE GARNET IN MICA ANATASE RUTILE AJTUNITE AND TORBERNITE THULITE AND PYRITE MONAZITE EMERALD CUPRITE SMOKY QUARTZ ZIRCON TORBERNITE ~/ UBRAR'l USE ONLV ,~O NOT REMOVE. fROM LIBRARY N. C. GEOLOGICAL SUHVEY Information Circular 24 Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie Raleigh 1978 Second Printing 1980. Additional copies of this publication may be obtained from: North CarOlina Department of Natural Resources and Community Development Geological Survey Section P. O. Box 27687 ~ Raleigh. N. C. 27611 1823 --~- GEOLOGICAL SURVEY SECTION The Geological Survey Section shall, by law"...make such exami nation, survey, and mapping of the geology, mineralogy, and topo graphy of the state, including their industrial and economic utilization as it may consider necessary." In carrying out its duties under this law, the section promotes the wise conservation and use of mineral resources by industry, commerce, agriculture, and other governmental agencies for the general welfare of the citizens of North Carolina. The Section conducts a number of basic and applied research projects in environmental resource planning, mineral resource explora tion, mineral statistics, and systematic geologic mapping. Services constitute a major portion ofthe Sections's activities and include identi fying rock and mineral samples submitted by the citizens of the state and providing consulting services and specially prepared reports to other agencies that require geological information. The Geological Survey Section publishes results of research in a series of Bulletins, Economic Papers, Information Circulars, Educa tional Series, Geologic Maps, and Special Publications. -
Hydroxyapatite and Fluorapatite in Conservative Dentistry and Oral Implantology—A Review
materials Review Hydroxyapatite and Fluorapatite in Conservative Dentistry and Oral Implantology—A Review Kamil Pajor, Lukasz Pajchel and Joanna Kolmas * Analytical Group, Department of Analytical Chemistry and Biomaterials, Faculty of Pharmacy with Laboratory Medicine Division, Medical University of Warsaw, 02-097 Warsaw, Poland * Correspondence: [email protected] Received: 29 July 2019; Accepted: 20 August 2019; Published: 22 August 2019 Abstract: Calcium phosphate, due to its similarity to the inorganic fraction of mineralized tissues, has played a key role in many areas of medicine, in particular, regenerative medicine and orthopedics. It has also found application in conservative dentistry and dental surgery, in particular, as components of toothpaste and mouth rinse, coatings of dental implants, cements, and bone substitute materials for the restoration of cavities in maxillofacial surgery. In dental applications, the most important role is played by hydroxyapatite and fluorapatite, i.e., calcium phosphates characterized by the highest chemical stability and very low solubility. This paper presents the role of both apatites in dentistry and a review of recent achievements in the field of the application of these materials. Keywords: hydroxyapatite; fluorapatite; dentistry; calcium phosphates 1. Introduction In recent decades, one has been able to observe huge progress in the field of dentistry. This results not only from the development of dental techniques and methods of therapy but also from significant developments in biomaterial engineering. The science of biomaterials is constantly increasing due to innovative modifications of already known materials or completely new biomaterials for applications in dentistry. Biodegradable polymers, bioactive ceramics, bioglass or metals covered with a layer of material facilitating osseointegration and, above all, composite materials are the main directions in the development of dental biomaterials [1–4]. -
“From Bone Valley to 'Far Places': a Global Environmental History of The
Edward D. Melillo – Please do no cite or copy without author’s permission “From Bone Valley to ‘Far Places’: A Global Environmental History of the 1919 Phosphate Miners’ Strike in Mulberry, Florida” Edward Melillo, Amherst College Introduction In her 1942 autobiography, Dust Tracks on a Road, writer Zora Neale Hurston vividly depicted the miners of Polk County, Florida, their “sweating black bodies, muscled like gods…. They go down in the phosphate mines and bring up the wet dust of the bones of pre-historic monsters, to make rich land in far places, so that people can eat.”1 Hurston’s narrative suspended readers between the immediacy of sinew and bone and the remoteness of the “far places” that reconstituted their soils with fertilizer from Florida’s phosphorus-rich fossil deposits. Among the sites where Hurston gathered folklore for the Works Projects Administration (WPA) in the late 1930s was the town of Mulberry, thirty-two miles (52 km) east of Tampa in Polk County. This railroad outpost in Florida’s “Bone Valley” region—a zone where phosphate-laden skeletons accumulated millions of years ago when much of the area was beneath the ocean—has long been a place where the gritty labors of a southern community converged with the demands of distant environments.2 This article chronicles a 1919 strike during which 3,000 black and white miners from the International Union of Mine, Mill, and Smelter Workers targeted seventeen of 1 Zora Neale Hurston, Dust Tracks on a Road: An Autobiography (1942; New York: HarperCollins, 2006), 147. 2 On May 6, 1935, United States President Franklin Delano Roosevelt created the WPA by Executive Order #7034.