Naturally Occurring Radioactive Material (NORM VI) (NORM Material Radioactive Occurring Naturally Naturally Occurring Radioactive Material
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Radium What Is It? Radium Is a Radioactive Element That Occurs Naturally in Very Low Concentrations Symbol: Ra (About One Part Per Trillion) in the Earth’S Crust
Human Health Fact Sheet ANL, October 2001 Radium What Is It? Radium is a radioactive element that occurs naturally in very low concentrations Symbol: Ra (about one part per trillion) in the earth’s crust. Radium in its pure form is a silvery-white heavy metal that oxidizes immediately upon exposure to air. Radium has a density about one- Atomic Number: 88 half that of lead and exists in nature mainly as radium-226, although several additional isotopes (protons in nucleus) are present. (Isotopes are different forms of an element that have the same number of protons in the nucleus but a different number of neutrons.) Radium was first discovered in 1898 by Marie Atomic Weight: 226 and Pierre Curie, and it served as the basis for identifying the activity of various radionuclides. (naturally occurring) One curie of activity equals the rate of radioactive decay of one gram (g) of radium-226. Of the 25 known isotopes of radium, only two – radium-226 and radium-228 – have half-lives greater than one year and are of concern for Department of Energy environmental Radioactive Properties of Key Radium Isotopes and Associated Radionuclides management sites. Natural Specific Radiation Energy (MeV) Radium-226 is a radioactive Abun- Decay Isotope Half-Life Activity decay product in the dance Mode Alpha Beta Gamma (Ci/g) uranium-238 decay series (%) (α) (β) (γ) and is the precursor of Ra-226 1,600 yr >99 1.0 α 4.8 0.0036 0.0067 radon-222. Radium-228 is a radioactive decay product Rn-222 3.8 days 160,000 α 5.5 < < in the thorium-232 decay Po-218 3.1 min 290 million α 6.0 < < series. -
Investigation on the Regime of Pchelinski Bani Mineral
Pentchev P. et al. HYDROGEOLOGY OF THE DOLNA BANYA THERMAL WATER BASIN 50 years University of Mining and Geology “St. Ivan Rilski” Annual, vol. 46, part І, Geology and Geophysics, Sofia, 2003, рр.281-286 HYDROGEOLOGY OF THE DOLNA BANYA THERMAL WATER BASIN Pavel Pentchev Vassil Zahariev Boryana Deneva University of Mining and Geology University of Mining and Geology University of Mining and Geology "St. Ivan Rilski" "St. Ivan Rilski" "St. Ivan Rilski" Sofia 1700, Bulgaria Sofia 1700, Bulgaria Sofia 1700, Bulgaria E-mail:[email protected] E-mail:[email protected] Email:[email protected] ABSTRACT The study is devoted to mineral water occurrences at Kostenets, Dolna Banya, Momin prohod, Pchelinski bani, revealed within the Kostenets graben depression. Specific geological, hydrogeological and hydrochemical conditions of the above mentioned occurrences of mineral water are the reasons for treated them as parts of a common hydrogeological structure, denoted as Dolna Banya thermal water basin. Scope and boundaries of the basin are delineated. A description of individual mineral water occurrences is presented. The discharge of each of them is assessed on actual measurements and observations of discharge regime. The total outflow of mineral water from the occurrences of the Dolna Banya thermal water basin recently amounts to 53 l/s. The hydrochemical characteristic of mineral waters is presented as well as regularities in the distribution of composition and temperature. A conceptual computer model of the Dolna Banya thermal water basin is compiled and it is used for determining the cathcment areas for each of the mineral water occurrences. The model confirms hydraulic connection between specific parts of the basin and in the meanwhile studies the determination of Kostenets occurrence of mineral water as an autonomous part of the basin. -
22Sra 226Ra and 222Rn in ' SOUTH CAROLINA GROUND WATER
Report No. 95 WRRI 22sRa 226Ra AND 222Rn IN ' SOUTH CAROLINA GROUND WATER: MEASUR~MEN-T TECHNIQUES AND ISOTOPE RELATIONSHIPS GlANNll\li FCUN~On o;: t,GR!CUL.TU~~tcoNOMlC2' ~~J.i\2Y J\li·iU ('lJ ~C 4· 1982 WATER RESOURCES RESEARCH INSTITUTE CLEMSON UNIVERSITY Clemson, .South Carolina JANUARY 1982 Water Resources Research Institute Clemson University Clemson, South Carolina 29631 ! 228Ra, 226Ra AND 222 Rn IN SOUTH CAROLINA GROUND WATER: MEASUREMENT TECHNIQUES AND ISOTOPE RELATIONSHIPS by Jacqueline Michel, Philip T. King and Willard S. Moore Department of Geology University of South Carolina Columbia, South Carolina 29208 The work upon which this puhlication is based was supported in part by funds provided by the Office of Water Research and Technology, project !!' No. OWRT-B-127-SC, U.S. Department of the Interior, fvashington, D. C., as authorized by the Water Research and Development Act of 1978 (PL95-467). r Project agreement No. 14-34-0001-9158 Period of Investigation: October 1979 - September 1980 Clemson University Water Resources Research Institute Technical Report No. 95 Contents of this publication do not necessarily reflect the views and policies of the Office of Water Research and Technology, U.S. Department of Interior, nor does mention of trade names or cormnercial products con stitute their endorsement or recommendation for use by the U.S. Goverrtment. ACKNOWLEDGEMENTS Much appreciation goes to Lewis Shaw, Rossie Stephens, Jim Ferguson and a large number of district personnel at the South Carolina Department of Health and Environmental Control who assisted us in field collection and provided much helpful information. Dr. -
Navigation Map of Bulgaria Including Offroadmap by Offroad-Bulgaria.Com Version 2021 Q1
Navigation Map of Bulgaria Including OFFRoadMap by OFFRoad-Bulgaria.com Version 2021 Q2 The purpose of this map is to provide accessible, accurate and up-to-date information for your GPS devices. Despite all efforts made by the creators to achieve this goal, the roads and the data included in this digital map are intended to be used as guidance only and should not be used solely for navigation. The creators of this map make no warranty as to the accuracy or completeness of the map data. In no event will the creators of this map be liable for any damages whatsoever, including but not limited to loss of revenue or profit, lost or damaged data, and expenses, arising in any way from or consequential upon the use of, or the inability to use this digital map. Contents: - Registering your map - Usage details - OFRM Geotrade 2021 Q2 variants - Coverage >>>>> REGISTRATION <<<<< To register your OFRM Geotrade map, please visit out website www.karta.bg. Click on “Create profile” in the top right corner of the screen and create your personal account. When done, the Support page will load automatically. Click on the button “Register OFRM Geotrade” and enter the 25-symbol map serial number and GPS model to activate your map’s update subscription (if your map includes one). To obtain the 25-symbol serial number, connect your GPS device to your computer via USB cable. If you have a GPS device with preloaded OFRM map, you will find the serial number in file “serial.txt” in the root folder of your device’s base memory or in the file “gmapsupp.unl” in folder “Garmin” (or folder “Map” on the newer models of the nüvi series and the new Drive series) of your device’s base memory. -
Espaço E Economia, 10 | 2017 Alternative Tourism in Bulgaria – General Characteristics 2
Espaço e Economia Revista brasileira de geografia econômica 10 | 2017 Ano V, número 10 Alternative tourism in Bulgaria – general characteristics Turismo alternativo na Bulgária – características gerais Le tourisme alternatif en Bulgarie : traits générales Turismo alternativo en Bulgaria: características generales. Milen Penerliev Electronic version URL: http://journals.openedition.org/espacoeconomia/2921 DOI: 10.4000/espacoeconomia.2921 ISSN: 2317-7837 Publisher Núcleo de Pesquisa Espaço & Economia Electronic reference Milen Penerliev, « Alternative tourism in Bulgaria – general characteristics », Espaço e Economia [Online], 10 | 2017, Online since 17 July 2017, connection on 19 April 2019. URL : http:// journals.openedition.org/espacoeconomia/2921 ; DOI : 10.4000/espacoeconomia.2921 This text was automatically generated on 19 April 2019. © NuPEE Alternative tourism in Bulgaria – general characteristics 1 Alternative tourism in Bulgaria – general characteristics Turismo alternativo na Bulgária – características gerais Le tourisme alternatif en Bulgarie : traits générales Turismo alternativo en Bulgaria: características generales. Milen Penerliev 1 Alternative tourism is a form of tourism which represents an alternative to the conventional mass tourism. Its forms are small-scale, low-density, divided into forms practiced in urban (religious, cultural, business) and rural areas. Alternative tourism is an attempt to preserve, protect and improve the quality of the existing resource base, which is fundamental for tourism itself. Alternative tourism is featured by active encouragement and care for the development of additional andspecific attractions as well the infrastructure, which are based on the local resources, while at the same time aiding the latter. It has an impact on the quality of life in the region, improves the infrastructure and increases the educational and cultural level of the local community. -
Experimental Γ Ray Spectroscopy and Investigations of Environmental Radioactivity
Experimental γ Ray Spectroscopy and Investigations of Environmental Radioactivity BY RANDOLPH S. PETERSON 216 α Po 84 10.64h. 212 Pb 1- 415 82 0- 239 β- 01- 0 60.6m 212 1+ 1630 Bi 2+ 1513 83 α β- 2+ 787 304ns 0+ 0 212 α Po 84 Experimental γ Ray Spectroscopy and Investigations of Environmental Radioactivity Randolph S. Peterson Physics Department The University of the South Sewanee, Tennessee Published by Spectrum Techniques All Rights Reserved Copyright 1996 TABLE OF CONTENTS Page Introduction ....................................................................................................................4 Basic Gamma Spectroscopy 1. Energy Calibration ................................................................................................... 7 2. Gamma Spectra from Common Commercial Sources ........................................ 10 3. Detector Energy Resolution .................................................................................. 12 Interaction of Radiation with Matter 4. Compton Scattering............................................................................................... 14 5. Pair Production and Annihilation ........................................................................ 17 6. Absorption of Gammas by Materials ..................................................................... 19 7. X Rays ..................................................................................................................... 21 Radioactive Decay 8. Multichannel Scaling and Half-life ..................................................................... -
ERASMUS – Europos Sąjungos Studijų Programa, Pavadinta XVI A
GEOLOGIJOS STUDIJOS 69 ERASMUS Europos Sàjungos studijø programa, pavadinta XVI a. humanisto Erazmo Roterda- mieèio (1469-1536) vardu ir skirta skatinti aukðtøjø mokyklø studentø ir dëstytojø studijø programø mainus tarp ES universitetø. ERASMUS programa pradëta 1987 m. Atkûrus Lietuvos nepriklausomybæ, galimybë dalyvauti ðioje programoje atsirado ir Lietuvos universitetams. Vilniaus universiteto geologiniø katedrø dëstytojai ir studentai taip pat dalyvauja ávairios paskirties ir trukmës programos priemonëse. Viena ið tæstiniø priemoniø yra INTENSYVIOS ERASMUS PROGRAMOS (IEP), kurios yra teminës, jø trukmë apie dvi savaites. Hidrogeologijos ir inþinerinës geologijos katedra nuo 2002 m. kartu su Kylio (progra- mos koordinatorius), Cagliari, Gento, Grenados, Sofijos ir Tulûzos universitetais dalyvauja vienoje tæsti- nëje IEP, skirtoje Europos poþeminio vandens naudojimo ir apsaugos nuo pavirðinës tarðos problemoms. IEP renginiai jau yra vykæ Grenadoje, Cagliari ir Vilniuje. Ketvirtasis Europos hidrogeologinis IEP renginys vyko pretendentës á ES nares Bulgarijos sostinëje Sofijoje. Jame dalyvavo VU Hidrogeologijos ir inþinerinës katedros doktorantë Aurelija Baublytë (ren- ginyje ji perskaitë paskaità) bei du I kurso magistrantai Daiva Kukytë ir Þygimantas Palaitis. Spausdindama IEP dalyvës doktorantës Aurelijos Baublytës straipsná, G.A. redakcija nori atkreipti geo- loginiø katedrø studentø dëmesá, kad ERASMUS programa leidþia paávairinti studijas, ágyti naujø þiniø, paþinti kitø ðaliø geologijà, sukaupti patyrimo bendraujant su kitø ðaliø studentais ir specialistais. Intensyvios ERASMUS programos dalyviai ekskursijos metu. Participants of Intensive ERASMUS Program during a field trip. Bulgarija, dar vadinama raudonøjø roþiø ða- kurortuose, kur yra daug sveikatingumo centrø, limi, besididþiuojanti savo vynuogynais ir ið jø ga- kurie medicininëms procedûroms naudoja na- minamu vynu, yra pietryèiø Europos valstybë, uþ- tûraliø gydomøjø savybiø turinèias priemones. imanti apie 22 proc. -
Bulgarian Properties for Sale and Rent
Offer: Development land in Kostenets in Kostenets Ref. No.: Bo 62762 URL address of the offer: https://www.bulgarianproperties.com/62762 Development land in Kostenets Price € 36 600 € 34 600 The price has been reduced by € 2 000 (5.46%) Location: Kostenets For sale Type of property: Development land Area features : In town. , In town Area: 1730.00 m2 Garden: no Condition: read text Authorised agency Responsible agent Sergey Pelovski Sofia Mobile: +359 882 817 459 Phone: +359 2 425 68 21 Address: 22, Zlaten Rog Str., floor 4, office 7, Sofia 1407 Skype: bulgarianproperties.com For sale - development land Large, sunny plot only 200m from the center of Kostenets. It is situated at the foot of Rila, in the eastern part of Kostenetsky-Dolnobanska valley, some 61 km southeast of Sofia. Because of its beautiful nature and the richness of mineral springs, the area is extremely popular. The plot is facing an asphalt road. There is electricity and water in the property. There are 3 national resorts in Kostenets municipality: • Momin Prohod • Kostenets Villas (in the village of Kostenets) • Pchelin baths, north of Pchelin village Page 1 Offer: Development land in Kostenets in Kostenets Ref. No.: Bo 62762 URL address of the offer: https://www.bulgarianproperties.com/62762 Kostenets is located next to the Trakia motorway, which makes access to the city very convenient. Viewings We are ready to organize a viewing of this property at a time convenient for you. Please contact the responsible estate agent and inform them when you would like to have viewings arranged. We can also help you with flight tickets and hotel booking, as well as with travel insurance. -
Analysis of Isotopes of Radium, Uranium and Thorium. 210Pb-210Po
Analysis of isotopes of radium, uranium and thorium. 210Pb-210Po Per Roos Risø National Laboratory for Sustainable Energy, Technical university of Denmark Radium isotopes Adsorption of Ra on MnO2 & direct alpha spectrometry Coating of polyamid (Nylon) with MnO2 (KMnO4 solution) ……half-life of Ra-224 is 88h Very thin MnO2 layer, poor yield but excellent resolution Electrodeposited sources Direct 20 days 6 months Analysis of 226Ra in water • Weigh up a suitable amount of water (10 litre is mostly sufficient). • Add HNO3 to pH 1-2. • Add 133Ba tracer (ca 10 Bq). • Add about 13 ml of a 0.2M KMnO4. • Adjust pH to about 8-9 with ammonia. • Add 15 ml 0.3M MnCl2 and stir for some 5 minutes. • Adjust with KMnO4 or MnCl2 to make the sample water phase slightly pink. • Collect the precipitate and centrifuge • Dissolve precipitate in 1M HCl-1%H2O2. • Add about 2g K2SO4+1ml H2SO4 and dilute to 100 ml with water. • Heat the sample to dissolve the K2SO4 completely. • Add 30 mg Pb2+. Heat for 20 minutes and stir. • Centrifuge the precipitate and discard supernate. • Wash precipitate with 100 ml of a solution of 0.2M H2SO4 and 0.1 M K2SO4 • Centrifuge the precipitate and discard supernate • Dissolve the PbSO4-precipitate with 3ml 0.1M EDTA at pH 10. • Transfer the solution to the scintillation vial (low diffusion PE-vial). • Wash centrifuge tube with 2 ml 0.1M EDTA and transfer to Scintillation vial. • Add 10ml OptiFluor 0 and fill with deionised water to total 20 ml. • Allow for ingrowth of 222Rn during 3 weeks and measure by LSQ. -
Radionuclides Notice of Data Availability Technical Support Document
Radionuclides Notice of Data Availability Technical Support Document March 2000 Targeting and Analysis Branch Standards and Risk Management Division Office of Ground Water and Drinking Water United States Environmental Protection Agency Prepared by: USEPA Office of Ground Water and Drinking Water in collaboration with USEPA Office of Indoor Air and Radiation United States Geological Survey Preface Under the authority of the Safe Drinking Water Act (SDWA) and its amendments, EPA sets drinking water standards for contaminants, which potentially pose a threat to public health via a public drinking water source. In 1976, EPA promulgated National Interim Primary Drinking Water Regulations (NIPDWR) for three categories of radionuclides: gross alpha emitters, radium 226 and 228 combined, and gross beta and photon emitters. The 1976 NIPDWRs for these radionuclides regulated: 1. gross alpha at 15 picoCuries per liter (pCi/L)(excluding radon and uranium); 2. radium-226 and radium-228 combined at 5 pCi/L; 3. and beta/photon emitters at a 4 millirem dose of radioactivity. The 1986 reauthorization of the Safe Drinking Water Act (SDWA) declared the interim standards for these radionuclides to be final National Primary Drinking Water Regulations (NPDWR). The 1986 amendment also required standards to be set as close to the maximum contaminant level goal (MCLG; the health goal) as possible. At that time, radionuclides did not have an MCLG. In 1991 (56 FR 33050), EPA proposed: < A Maximum Contaminant Level Goal (MCLG) of zero for all radionuclides; < A -
Bulgarian Economy” 2007-2013
OP “Development of the Competitiveness of the Bulgarian Economy” 2007-2013 Project “Promoting the advantages of investing in Bulgaria” BG 161PO003-4.1.01-0001-C0001, with beneficiary InvestBulgaria Agency, has been implemented with the financial support of the European Union through the European Fund for Regional Development and the national budget of the Republic of Bulgaria. INVEST IN BULGARIA CONTENT 1. Introduction 4 2. General overview of Bulgaria 8 2.1. Geography 10 2.2. Demographic profile 16 2.3. Main cities 18 2.4. History 28 2.5. Political profile 40 2.6. Economic profile 42 3. Human resources 52 3.1. Universities 56 3.2. Schools 64 4. Cost of doing business 68 4.1. Taxes 70 4.2. Salaries 71 4.3. Land and rents 72 4.4. Utilities 74 5. Infrastructure 76 6. Government support 84 7. Key sectors and success stories 90 7.1. Food and beverage industry 92 7.2. IT 106 7.3. Electrical engineering and electronics 122 7.4. Healthcare and medical tourism 136 7.5. BPO 144 7.6. Mechanical engineering 154 7.7. Transport and logistics 166 7.8. Chemistry and related industries 174 7.9. Other sectors 190 8. Other information 194 Introduction Bulgaria stands for a critical mass of highly-qualified, well- educated professionals who bring together proven practical understanding of business with high-level theoretical skills to deliver efficient, cost -effective international solutions. A. T. Kearney The three factors which contributed to a decision in favor of Bulgaria as a place to invest included: access to our core raw material, country’s geographic location and the current tax situation. -
GEOTHERMAL OPPORTUNITIES in EASTERN EUROPE: a Survey
GEOTHERMAL OPPORTUNITIES in EASTERN EUROPE: A Survey January 1996 Prepared by: Dr. L.R. Lawrence, Jr. Bojan Stoyanov Bob Lawrence & Associates, Inc. 424 N. Washington Street Alexandria, VA 22314 TABLE OF CONTENTS I. INTRODUCTION .....................................................1 II. ALBANIA ...........................................................3 III. BULGARIA .........................................................5 IV. THE CZECH REPUBLIC AND SLOVAKIA (THE FORMER CZECHOSLOVAKIA) ...................................12 V. FEDERAL REPUBLIC OF GERMANY EASTERN FEDERAL STATES .........................................19 VI. HUNGARY .........................................................24 VII. POLAND ...........................................................31 VIII. ROMANIA .........................................................39 IX. THE FORMER YUGOSLAVIA: SLOVENIA, CROATIA, BOZNIA, YUGOSLAVIA (SERBIA AND MONTENEGRO) AND MACEDONIA ..................................................45 X. CONCLUSION ......................................................54 INTRODUCTION Since the times of earliest man, the multitude of geothermal springs in Eastern Europe have been known and utilized for basic human needs. The use of many of these springs for bathing goes back as far as recorded history. More recent uses, such as greenhouses, building heat, and geothermal electric generation are just now being considered and employed. The Springs, themselves, often became focal points for habitation, and small villages and cities grew up around the