DOCSLIB.ORG

Part 3832—Locat

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Part 3832—Locat § 3830.97 43 CFR Ch. II (10–1–20 Edition) § 3830.97 What if I pay only part of the 3832.34 How may I use my mill site? service charges for a notice of in- tent to locate mining claims on Subpart D—Tunnel Sites SRHA lands? 3832.40 Tunnel sites. For notices of intent to locate min- 3832.41 What is a tunnel site? ing claims (NOITL) under the 3832.42 How do I locate a tunnel site? Stockraising Homestead Act (see part 3832.43 How may I use a tunnel site? 3838 of this chapter for information re- 3832.44 What rights do I have to minerals garding the Stockraising Homestead within my tunnel site? Act and NOITLs), BLM will not accept 3832.45 How do I obtain any minerals that I a NOITL unless we receive your pay- discover within my tunnel site? ment of the required service charges. Subpart E—Defective Locations BLM will return the NOITL to you without taking any further action. See 3832.90 Defects in the location of mining § 3830.21 of this part for the amount of claims and sites. the service charge for a NOITL. 3832.91 How do I amend a mining claim or site location if it exceeds the size limita- tions? Subpart F—Appeals AUTHORITY: 30 U.S.C. 22 et seq.; 43 U.S.C. 2, § 3830.100 How do I appeal a final de- 1201, 1457, 1740, 1744. cision by BLM? SOURCE: 68 FR 61069, Oct. 24, 2003, unless If you are adversely affected by a otherwise noted. BLM decision under parts 3830–3839, you may appeal the decision in accord- Subpart A—Locating Mining ance with parts 4 and 1840 of this title. Claims or Sites PART 3831—MINERAL LANDS § 3832.1 What does it mean to locate AVAILABLE FOR LOCATING MIN- mining claims or sites? ING CLAIMS OR SITES [RE- (a) Locating a mining claim or site SERVED] means: (1) Establishing the exterior lines of a mining claim or site on lands open to PART 3832—LOCATING MINING mineral entry to identify the exact CLAIMS OR SITES land claimed; and (2) Recording a notice or certificate Subpart A—Locating Mining Claims or Sites of location as required by state and Sec. Federal law and by this part. 3832.1 What does it mean to locate mining (b) You will find— claims or sites? (1) Location requirements in this 3832.10 Procedures for locating mining part; claims or sites. (2) Recording requirements in part 3832.11 How do I locate mining claims or 3833 of this chapter; sites? 3832.12 When I record a mining claim or (3) Requirements for transferring an site, how do I describe the lands I have interest in a mining claim or site in claimed? § 3833.30 of this chapter; and (4) Annual fee requirements for min- Subpart B—Types of Mining Claims ing claims and sites in parts 3834, 3835, 3832.20 Lode and placer mining claims. and 3836 of this chapter. 3832.21 How do I locate a lode or placer min- ing claim? § 3832.10 Procedures for locating min- 3832.22 How much land may I include in my ing claims or sites. mining claim? § 3832.11 How do I locate mining Subpart C—Mill Sites claims or sites? (a) You must follow both state and 3832.30 Mill sites. 3832.31 What is a mill site? Federal law. 3832.32 How much land may I include in my (b) Your lode or placer claim is not mill site? valid until you make a discovery with- 3832.33 How do I locate a mill site? in the boundaries of the claim. 960 VerDate Sep<11>2014 13:59 May 14, 2021 Jkt 250198 PO 00000 Frm 00970 Fmt 8010 Sfmt 8010 Y:\SGML\250198.XXX 250198 Bureau of Land Management, Interior § 3832.12 (c) To locate a claim or site, you rectangular subdivisions as much as must— possible; and (1) Make certain that the land on (2)(i) You must file either— which you are locating the claim or (A) A topographical map published by site is Federal land that is open to the U.S. Geological Survey with a de- mineral entry piction of the claim or site; or (2) Stake and monument the corners (B) A narrative or sketch describing of a mining claim or site which meets the claim or site and tying the descrip- applicable state monumenting require- tion to a natural object, permanent ments and the size limitations de- monument or topographic, hydro- scribed in § 3832.22 for lode and placer graphic, or man-made feature. claims, § 3832.32 for mill sites, and (ii) You must show on a map or § 3832.42 for tunnel sites; sketch the boundaries and position of (3) Post the notice of location in a the individual claim or site by aliquot conspicuous place on the claim or site. part within the quarter section accu- The notice must include: rately enough for BLM to identify the (i) The name or names of the loca- mining claims or sites on the ground. tors; (iii) You may show more than one (ii) The date of the location; and claim or site on a single map or de- (iii) A description of the claim or scribe more than one claim or site in a site; single sketch— (iv) The name or number of the claim (A) If they are located in the same or site, or both, if the claim or site has general area; and both; (B) If the individual mining claims or (4) Record the notice or certificate of sites are clearly identified. location in the local recording office (iv) You are not required to employ a and the BLM State Office with jurisdic- professional surveyor or engineer to es- tion according to the procedures in tablish the location’s position on the part 3833; ground. (5) Follow all other relevant state (b) Lode claims. You must describe law requirements; and lode claims by metes and bounds begin- (6) Comply with the specific require- ning at the discovery point on the ments for lode claims, placer claims, claim and include a tie to natural ob- mill sites, or tunnel sites in this part. jects or permanent monuments includ- ing: § 3832.12 When I record a mining claim (1) Township and section survey or site, how do I describe the lands monuments; I have claimed? (2) Official U.S. mineral survey (a) General requirements. (1) All claims monuments; and sites. You must describe the land (3) Monuments of the National Geo- by state, meridian, township, range, detic Reference System; section and by aliquot part to the quar- (4) The confluence of streams or ter section. To obtain the land descrip- point of intersection of well-known tion, you must use an official survey gulches, ravines, or roads, prominent plat or other U.S. Government map buttes, and hills; or that is based on the surveyed or pro- (5) Adjoining claims or sites. tracted U.S. Public Land Survey Sys- (c) Placer claims. (1) You must de- tem. If you cannot describe the land by scribe placer claims by aliquot part aliquot part (e.g., the land is and complete lots using the U.S. Public unsurveyed), you must provide a metes Land Survey System and its rectan- and bounds description that fixes the gular subdivisions except when placer position of the claim corners with re- claims are— spect to a specified claim corner, dis- (i) On unsurveyed Federal lands; covery monument, or official survey (ii) Gulch or bench placer claims; or monument. In all cases, your descrip- (iii) Bounded by other mining claims tion of the land must be as compact or nonmineral lands. and regular in form as reasonably pos- (2) For placer mining claims that are sible and should conform to the U.S. on unsurveyed Federal lands or are Public Land Survey System and its gulch or bench placer claims: 961 VerDate Sep<11>2014 13:59 May 14, 2021 Jkt 250198 PO 00000 Frm 00971 Fmt 8010 Sfmt 8010 Y:\SGML\250198.XXX 250198 § 3832.20 43 CFR Ch. II (10–1–20 Edition) (i) You must describe the lands by vein, lode, or ledge and the vein, lode, protracted survey if the BLM has a or ledge extends through the endlines protracted survey of record; or of your lode claim, you have extra-lat- (ii) You may describe the lands by eral rights to pursue the down-dip ex- metes and bounds, if a protracted sur- tension of the vein, lode, or ledge to vey is not available or if the land is not the point where the vein, lode, or ledge amenable to protraction. intersects a vertical plain projected (3) If you are describing an associa- parallel to the end lines and outside tion placer claim by metes and bounds, the sideline boundaries of your lode you must meet the following require- claim if— ments, according to the number of per- (i) The top or apex of the vein, lode, sons in your association, as described or ledge lies on or under the surface in Snow Flake Fraction Placer, 37 Pub. within the interior boundaries of the Lands Dec. 250 (1908), in order to keep lode claim; and your claim in compact form and not (ii) The long axis, and therefore the split Federal lands into narrow, long or side lines, of the lode claim are sub- irregular shapes: stantially parallel to the course of the (i) A location by 1 or 2 persons must vein, lode, or ledge.
Load more

Recommended publications
  • Ecological and Geographical Features of Ontogenesis of Holocene Soils of Kamianets-Podilskyi Fortress
    SHS Web of Conferences 100, 05006 (2021) https://doi.org/10.1051/shsconf/202110005006 ISCSAI 2021 Ecological and Geographical Features of Ontogenesis of Holocene Soils of Kamianets-Podilskyi Fortress Roman Malyk1*, Andriy Kyrylchuk1, Zinovy Pankiv1, and Ihor Kasiyanyk2 1Ivan Franko National University of Lviv, 79000, University str. 1, Lviv, Ukraine 2Ivan Ogienko National University of Kamianets-Podilskyi, 32301, Ogienko str. 61, Kamianets-Podilskyi, Ukraine Abstract. The article analyzes the degree of study of the genetic features of Holocene soils of beligerative complexes. A detailed description of natural and anthropogenic conditions and factors determining the geography, genesis and ecological condition of modern and buried soils of beligerative structures of Kamianets-Podilskyi Fortress is given. Considerable attention is paid to the problem of ontogenesis of the dominant natural and anthropogenic soils within the study area, represented by urborendzins and constructional soils. The morphogenetic features of these soils have been studied. The soils of the beligerative complex are represented by naturally anthropogenic soils – urborendzins and constructional soils. They are polygenetic with complex phylogeny and their genesis includes at least two onogenesis. For a long time soils have been evolving naturally in form of typical rendzin, but have undergone quantitative and qualitative changes due to intensive anthropogenic activity. The genetic profile of soils is characterized by significant variability of morphological traits, the presence of eluvium of soil- forming rocks in the entire soil layer. the studied Holocene soils (modern and buried) are an integral part of the historical and cultural lands and need protection, as they contain information about the evolution of the territory and ways of its use.
    [Show full text]
  • An Idea of Multi-Functional Storage Reservoirs in Mountain Regions
    International Journal of Modern Engineering Research (IJMER) www.ijmer.com Vol.3, Issue.1, Jan-Feb. 2013 pp-396-400 ISSN: 2249-6645 An Idea of Multi-Functional Storage Reservoirs in Mountain Regions Jan Jaremski Rzeszow University of Technology, Rzeszow, Poland Abstract: The paper presents possibilities of construction of multi-functional reservoir in mountain regions, especially those with soft rocks. Construction of relatively small reservoir instead of big ones and taking the area configuration into account allows eliminating expensive embankments and insists to construction of cofferdams. The cofferdam can be formed of the occurring rock eluvium. Such idea was analyzed for the south of Poland. At present we can observe the climate changes accompanied by increase of the weather dynamics and unusual intensity of extreme phenomena. Mineralogical composition of rocks or their eluvia occurring in the considered area is usually not taken into account while forecasting of such phenomena. The proposed tests on determination of the eluvium areas especially susceptible to formation of mud avalanches in the mountains sites. Keywords: flysch eluvium, reservoir, rock eluvium , mud avalanches , swelling I. INTRODUCTION The climate variation has been observed recently. They are accompanied by increase of the weather dynamics and unusual intensity of extreme phenomena. Precipitations are very intense and they are accompanied by landslides and mud avalanches, or long-lasting droughts. A lack of suitable retention causes a fast flow of discharge water to the seas. Mineralogical composition of rocks or their eluvia occurring in the considered area is usually not taken into account while forecasting of such phenomena. Colloidal activity, a state of colloidal bonding and crystallization strongly influence formation of avalanches, strength of the mixtures and reversibility of their reactions with participation of clay minerals.
    [Show full text]
  • Journal of Geochemical Exploration 164 (2016) 122–135
    Journal of Geochemical Exploration 164 (2016) 122–135 Contents lists available at ScienceDirect Journal of Geochemical Exploration journal homepage: www.elsevier.com/locate/jgeoexp Three-dimensional geochemical patterns of regolith over a concealed gold deposit revealed by overburden drilling in desert terrains of northwestern China Bimin Zhang a,b,c,⁎, Xueqiu Wang b,c, Qinghua Chi b,c, Wensheng Yao b,c,HanliangLiub,c, Xin Lin b,c a School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China b Institute of Geophysical and Geochemical Exploration, CAGS, Langfang 065000, China c Key Laboratory for Geochemical Exploration Technology, MLR, Langfang 065000, China article info abstract Article history: Desert terrains are widespread in northwestern and northern China, and these areas present particular Received 22 December 2014 challenges for exploration. In recent years, partial extraction techniques have been proven to be effective in Revised 9 June 2015 the search for concealed deposits in arid desert terrains in some cases. However, we still lack an understanding Accepted 13 June 2015 of the dispersion patterns of ore-forming elements in regolith. In this study, air reverse circulation drillings Available online 19 June 2015 were used to create three-dimensional (3D) distribution patterns of elements in regolith over the Jinwozi gold deposit in China, which is covered by tens of metres of regolith, in order to trace the migration of elements Keywords: Geochemical patterns and to understand the dispersion
    [Show full text]
  • Annex: Soil Groups, Characteristics, Distribution and Ecosystem Services
    Status of the World’s Main Report Soil Resources Annex Soil groups, characteristics, distribution and ecosystem services © FAO | Giuseppe Bizzarri © FAO INTERGOVERNMENTAL TECHNICAL PANEL ON SOILS Disclaimer and copyright Recommended citation: FAO and ITPS. 2015. Status of the World’s Soil Resources (SWSR) – Main Report. Food and Agriculture Organization of the United Nations and Intergovernmental Technical Panel on Soils, Rome, Italy The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. ISBN 978-92-5-109004-6 © FAO, 2015 FAO encourages the use, reproduction and dissemination of material in this information product. Except where otherwise indicated, material may be copied, downloaded and printed for private study, research and teaching purposes, or for use in non-commercial products or services, provided that appropriate acknowledgement of FAO as the source and copyright holder is given and that FAO’s endorsement of users’ views, products or services is not implied in any way.
    [Show full text]
  • Relationship Between the Lithology of Active-Layer Materials and Mean Annual Ground Temperature in the Former Ussr
    RELATIONSHIP BETWEEN THE LITHOLOGY OF ACTIVE-LAYER MATERIALS AND MEAN ANNUAL GROUND TEMPERATURE IN THE FORMER USSR V.N. Konishchev Department of Cryolithology and Glaciology, Faculty of Geography, Moscow State University, Moscow 119899, Vorobyovy Gory, Russia. e-mail: [email protected] Abstract The accummulation of quartz particles within the 0.05-0.01 mm grain size fraction and of the feldspar parti- cles within the 0.1-0.05 mm fraction due to freeze-thaw was confirmed by experimental data and laboratory investigations of cryogenic soils. A cryogenic weathering index (CWI) is proposed to estimate the role of cryo- genic weathering in soil formation. The general zonality of the CWI has already been defined. This permits one to express more precisely the relation between CWI values and mean annual ground temperature. This is obtained for different geocryologi- cal conditions. Introduction the dimensions of the microfractures and defects that characterize the surface of mineral particles. Various types of stability coefficients, expressed as the Detailed study of cryogenic disintegration allows one ratio of stable to unstable minerals, are widely used as to differentiate globally the physical weathering palaeo-geographical indicators (e.g., Gaigalas et al., processes. The special index for cold regions which 1975). From the palaeo-geographical point of view, this characterizes the distribution of major rock-forming ratio reflects the general relation between the processes minerals over the granulometric spectrum is called the of physical and chemical weathering. cryogenic weathering index (CWI). Cryogenic weathering of polymictic source rocks and unconsolidated deposits is associated with strong QF11/ CWI = [1] physico-chemical disintegration of major rock-forming QF22/ minerals and the accumulation of the latter in definite granulometric fractions.
    [Show full text]
  • Final Decision Document for Other Contamination Sources Interim Response Action Shell Section 36 Trenches, Rma
    798308 - R8 SDMS FINAL DECISION DOCUMENT FOR OTHER CONTAMINATION SOURCES INTERIM RESPONSE ACTION SHELL SECTION 36 TRENCHES, RMA Prepared by MK-Environmental Services Denver, Colorado 80203 Prepared for Shell Oil/Holme Roberts & Owen Denver, Colorado 80203 April 1990 4^ DEPARTMENT OF THE ARMY PROGRAM MANAGER FOR ROCKY MOUNTAIN ARSENAL coMMCNCE crrv. COLORAOO aoo22-2iao May 3, 1990 llfLT TO ATTtNTiea or: Interim Response Division Mr. George Roe Shell Oil Company P.O. Box 4320 Houston, Texas 77210 Dear Mr. Roe: This letter serves to advise you of the finalization of the Decision Documents for the Army Complex Disposal Trenches and the Shell Section 36 Trenches Interim 0U23 Response Actions at Rocky Mountain Arsenal Since no dispute was raised, the Draft Final Decision Documents that were issued March 30, 1990, shall serve as the Final Decision Documents. Enclosed with this letter are replacement white covers and text pages for your copies of the documents. Comments were received from the U.S. Environmental Protection Agency (EPA) and the State of Colorado. Neither of the two Decision Documents were disputed. A brief response to the general comments and concems is provided below. Specific comments provided wQl be discussed with the Organizations and State (OAS) during the design phase. Comments were received from both the EPA and State on the Army Complex Disposal Trenches document. The Army agrees that all-party discussions need to be held to discuss design issues prior to the release of the Draft Implementation Document. Text changes for the Final version, however, will not be made except for page 5-2 which will update the Chronology of Events section.
    [Show full text]
  • He-Ar Isotopes and Trace Gas Compositions of Fluid Inclusions in Massive Sulphides from the Yushui Copper-Polymetallic Deposit, South China: Metallogenic Implications
    minerals Article He-Ar Isotopes and Trace Gas Compositions of Fluid Inclusions in Massive Sulphides from the Yushui Copper-Polymetallic Deposit, South China: Metallogenic Implications 1, 2,3, 2,3,4,5, 1 2,3,5 Yi Huang y, Zhongwei Wu y, Xiaoming Sun * , Yan Wang , Guiyong Shi , Wei Zhai 2,3,5 and Yao Guan 6 1 South China Sea Institute of Planning and Environmental Research, State Oceanic Administration, Guangzhou 510300, China; [email protected] (Y.H.); [email protected] (Y.W.) 2 School of Marine Sciences, Sun Yat-sen University, Guangzhou 510006, China; fi[email protected] (Z.W.); [email protected] (G.S.); [email protected] (W.Z.) 3 Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering, Guangzhou 510006, China 4 School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275, China 5 Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, China 6 Fourth Institute of Oceanography, Ministry of Natural Resources, Beihai 536000, China; [email protected] * Correspondence: [email protected]; Tel.: +86-020-84110968 These authors contributed equally to this work. y Received: 29 March 2019; Accepted: 24 April 2019; Published: 29 April 2019 Abstract: The Yushui ore deposit, located in the middle section of the Yong’an-Meixian Hercynian depression, is a medium-sized Cu-polymetallic massive sulphide deposit in Eastern Guangdong Province, South China. This deposit is characterized by unusually high copper grade (up to 50–60 wt. % Cu). Other metallic elements, such as lead, zinc and silver, are also economically important in the Yushui ore bodies.
    [Show full text]
  • Study of Desert Soil Horizons: a Review
    Kheyrodin and Kheyrodin, World J. Biol. Med. Science Volume 2 (4), 89-99, 2015 Indexed, Abstracted and Cited: ISRA Journal Impact Factor, International Impact Factor Services (IIFS), Directory of Research Journals Indexing (DRJI), International Institute of Organized Research and Scientific Indexing Services, Cosmos Science Foundation (South-East Asia), Einstein Institute for Scientific Information {EISI}, Directory of Open Access Scholarly Resources, citefactor.org journals indexing Directory Indexing of International Research Journals World Journal of Biology and Medical Sciences Published by Society for Advancement of Science® ISSN 2349-0063 (Online/Electronic) Volume 2, Issue- 4, 89-99, October to December, 2015 WJBMS 2/04/45/2015 All rights reserved www.sasjournals.com A Double Blind Peer Reviewed Journal / Refereed Journal [email protected]/[email protected] REVIEW ARTICLE Received: 03/07/2015 Revised: 03/09/2015 Accepted: 05/09/2015 Study of Desert Soil Horizons: A Review Sadaf Kheyrodin and *Hamid Kheyrodin Islamic Azad University, Mashhad Branch, Iran *Faculty of Desert Science, Semnan University, Iran ABSTRACT Horizons are defined in most cases by obvious physical features, chiefly color. Desert soils form in areas where the demand for water by the atmosphere (evaporation) and plants (transpiration) is much greater than precipitation. Deserts cover 20 to 33% of the Earth’s land surface, and can be found in the tropics, at the poles, and in between. Most desert soils are called Aridisols (dry soil). However, in really dry regions of the Sahara and Australian outback, the soil orders are called Entisols. Entisols are new soils, like sand dunes, which are too dry for any major soil horizon development.
    [Show full text]
  • State of Alaska Department of Natural Resources Division of Geological and Geophysical Surveys
    STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL AND GEOPHYSICAL SURVEYS Walter J. Hickel, Governor Glenn A. Olds, Commissioner Thomas E. Smith, Direaor and State Geologist July 1992 Report of Investigations 92-2 RECHARGE AREA EVALUATION FOR MOONLIGHT SPRINGS, NOME, ALASKA BY J.A. Munter, M.A. Maurer, M.G. Inghram, and W.A. Petrik Division of Water In cooperation with the City of Nome STATE OF ALASKA Department of Natural Resources DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS According to Alaska Statute 41, the Alaska Division of Geological and Geophysical Surveys is charged with conducting 'geological and geophysical surveys to determine the potential of Alaskan land for production of metals, minerals, fuels, and geothermal resources; the lacations and supplies of ground water and construction materials; the potential geologic hazards to buildings, roads, bridges, and other installations and structures; and shall conduct such other surveys and investigations as will advance knowledge of the geology of Alaska. " Administrative functions are performed under the direction of the State Geologist, who maintains his office in Fairbanks. The locations of DGGS offices are listed below: 794 University Avenue 400 Willoughby Avenue Suite 200 3rd Floor Fairbanks, Alaska 99709-3645 Juneau, Alaska 99801 (907) 474-7 147 (907) 465-2533 Geologic Materials Center 18225 Fish Hatchery Road P.O. Box 772116 Eagle River, Alaska 99577 (907) 696-0070 This report, printed in Fairbanks, Alaska, is for sale by DGGS for $3. DGGS publications may be inspected at the following locations. Address mail orders to the Fairbanks office. Alaska Division of Geological & Geophysical Surveys 794 University Avenue, Suite 200 Fairbanks, Alaska 99709-3645 Department of Natural Resources Public Information Center 3601 C Street, Suite 200 Anchorage, Alaska 991 10 U.S.
    [Show full text]
  • Modeling of the Evolution of Steppe Chernozems and Development of the Method of Pedogenetic Chronology
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by DSpace at Belgorod State University Modeling of the Evolution of Steppe Chernozems and Development of the Method of Pedogenetic Chronology F. N . Lisetskii", V. F. S to lb a \ and P. V. Goleusov" a Belgorod National Research University, ul. Pobedy 85, Belgorod, 308015 Russia bAarhus University, Nordre Ringgade 1, Aarhus С DK-8000, Denmark e-mail: [email protected], [email protected] Received March 17, 2015 Abstract—Geoarchaeological methods were used to study chronosequences of surface soils in the steppe zone and to trace soil evolution during the Late Holocene in northwestern Crimea. It was found that the morpholog­ ical and functional “maturity” of the humus horizons in steppe chernozems of the Late Holocene was reached in about 1600-1800 yrs. After this, their development decelerated irreversibly. The maximum concentration of trace elements accumulated in these horizons in the course of pedogenesis was reached in 1400 yrs. A new method of pedogenetic chronology based on the model chronofunction of the development of irreversible results of pedogenesis over time is suggested. Original pedochronological data and growth functions—the most suitable models for simulating pedogenesis over the past three thousand years—suggest that the development of morphological features of soil as an organomineral natural body follows growth patterns established for biolog­ ical systems. Keywords: geoarchaeology, chronofunctions, modeling, humus horizon, trace elements, steppe zone DOI: 10.1134/S1064229316080056 INTRODUCTION method has become an efficient approach to studying soil evolution [7, 31, 33, 35, 40, 48].
    [Show full text]
  • Record of Decision, Operable Unit 2
    SDMS Document DECLARATION STATEMENT RECORD OF DECISION SITE NAME AJ^ LOCATION White Chemical Corporation Site (EPA ID#NJD980755623) Newark, Essex County, New Jersey Operable Unit 2 for Soils, Buildings and Above-Ground Storage Tanks STATEMENT OF BASIS AND PURPOSE This decision dociunent presents the Selected Remedy to address contaminated soils, sump sediments, buildings and tanks at the White Chemical Corporation Superfund Site (Site) in Newark, New Jersey, which was chosen in accordance witii the Comprehensive Enviroronental Response, Compensation and Liability Act, as amended, and, to the extent practicable, the National Oil and Hazardous Substances Pollution Contingency Plan. This decision is based on the Administrative Record file for the Site. The State of New Jersey concurs with the Selected Remedy. ASSESSMENT OF THE SITE The response action selected in this Record of Decision (ROD) is necessary to protect public health or welfare or the ravironment fi-om actual or threatened releases of hazardous substances fix>m the Site into the envirormient. DESCRPTION OF THE SELECTED REMEDY The Selected Remedy addresses an estimated 21,185 cubic yards of contaminated soil, nine on- site buildings and above-ground storage tanks on the Site. A previous ROD was signed on September 26,1991. The 1991 ROD required appropriate secxurity measures, stabilization of the Site, on-site treatment or neutralization of contaminated material, off-site treatment, recycling or disposal of contaminated material, decontamination and off-site disposal or recycling of empty drmns and containers, decontamination of on-site storage tanks and process piping, and appropriate environmental monitoring. An additional action will be necessary to address groundwater contamination imderlying the Site.
    [Show full text]
  • JOURNAL of Geology, Geoecology
    ISSN 2617-2909 (print) JOURNAL of Geology, ISSN 2617-2119 (online) GEOGRAPHY And Journ.Geol.Geograph. Geoecology Geology, 29(1), 30–39. Journal home page: geology-dnu-dp.ua doi: 10.15421/112003 Yaroslav M. Bilanchyn, Irуna V. Leonidova, Darya V. Bulysheva Journ.Geol.Geograph.Geoecology,29(1),30–39. Specificity of genetic nature and classification characteristics of Zmiiny Island chernozem soils Yaroslav M. Bilanchyn1, Irуna V. Leonidova2, Darya V. Bulysheva2 1Odessa Mechnikov National University, Odessa, Ukraine 2Odessa State Agrarian University, Odessa, Ukraine, [email protected] Received: 03.08.2019 Abstract. Even the first researchers of the nature of the small (20.5 hectares) rocky Zmiiny Received in revised form: 10.09.2019 Island in the northwestern Black Sea region visually diagnosed the soil there with black Accepted: 26.01.2020 earth. Since 2003, the staff of the Department of Soil Science and Soil Geography of the Odessa National University named by I.U.Mechnikov ONU began the study of factors and processes of soil formation, soils and soil cover of Zmiiny Island territory. It was found out that on the inter-rocky areas of the island un- der the steppe grassy vegetation on the gravelly-stony eluvium or eluvium-deluvium of dense rocks formed unusually high humus (up to 14-18%) undeveloped and short-profile chernozem soils. However, the diagnostic and classification of these soils remains unclear. The purpose is to characterize the specificity of the genetic nature of the island soils and to determine their diagnostic and
    [Show full text]