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  • 1
    Keywords: Sustainability. ; Environmental sciences Social aspects. ; Energy policy. ; Energy and state. ; Environmental Law. ; Environmental management. ; Human ecology Study and teaching. ; Sustainability. ; Environmental Social Sciences. ; Energy Policy, Economics and Management. ; Environmental Law. ; Environmental Management. ; Environmental Studies.
    Description / Table of Contents: Chapter 1. Introduction -- Chapter 2. The state and trend of China's low-carbon development -- Chapter 3. End-use energy consumption & CO2 emissions -- Chapter 4. Power sector -- Chapter 5. Primary energy consumption and CO2 emissions -- Chapter 6. Non-CO2 GHG emissions -- Chapter 7. Technical support for long-term deep decarbonization -- Chapter 8. Investment & cost analysis for realizing a low emission strategy -- Chapter 9. Long-term low-carbon transition pathways -- Chapter 10. Strategic linchpins and policy safeguards -- Chapter 11. Global climate governance & international cooperation -- Chapter 12. Conclusions and policy recommendations.
    Abstract: This open access book introduces a multi-disciplinary and comprehensive research on China's long-term low-carbon emission strategies and pathways. After comprehensively considering China’s own socioeconomic conditions, policy design, energy mix, and other macro-development trends and needs, the research team has proposed suggestions on China’s low-carbon development strategies and pathways until 2050, with required technologies and policies in order to realize the goals of building a great modern socialist country and a beautiful China. These achievements are in conjunction with the climate goals set in the Paris Agreement alongside Global Sustainable Development. The authors hope that the research findings can serve as a reference for all sectors of Chinese society in their climate research efforts, offer support for the formulation and implementation of china’s national low-carbon development strategies and policies, and help the world to better understand China’s story in the general trend of global green and low-carbon development.
    Type of Medium: Online Resource
    Pages: XXXVIII, 333 p. 94 illus., 91 illus. in color. , online resource.
    Edition: 1st ed. 2022.
    ISBN: 9789811625244
    DDC: 304.2
    Language: English
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  • 2
    Call number: PIK N 613-91-0160
    Type of Medium: Monograph available for loan
    Pages: 308 pp.
    ISBN: 9022008096
    Series Statement: Simulation Monographs ;
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Beijing : Science Press
    Call number: M 98.0450
    Type of Medium: Monograph available for loan
    Pages: vii, 159 S.
    ISBN: 7030050447
    Series Statement: Solid earth sciences research in China
    Classification:
    Regional Geology
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Suhrkamp : Frankfurt am Main
    Call number: PIK E 703-00-0427
    Type of Medium: Monograph available for loan
    Pages: 148 p.
    Edition: 3. Auflage
    ISBN: 3518107696
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 5
    Call number: ZSP 16697-0009
    Pages: 105 S. : Abb. ; 30 cm
    ISSN: 0931-0800
    Series Statement: Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen 80
    Branch Library: AWI Library
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  • 6
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract. We employ data taken by the JADE and OPAL experiments for an integrated QCD study in hadronic e $^+$ e $^-$ annihilations at c.m.s. energies ranging from 35 GeV through 189 GeV. The study is based on jet-multiplicity related observables. The observables are obtained to high jet resolution scales with the JADE, Durham, Cambridge and cone jet finders, and compared with the predictions of various QCD and Monte Carlo models. The strong coupling strength, $\alpha_s$ , is determined at each energy by fits of ${\cal O}(\alpha_s^2)$ calculations, as well as matched ${\cal O}(\alpha_s^2)$ and NLLA predictions, to the data. Matching schemes are compared, and the dependence of the results on the choice of the renormalization scale is investigated. The combination of the results using matched predictions gives \[\alpha_s(M_{Z^0})=0.1187^{0.0034}_{0.0019}.\] The strong coupling is also obtained, at lower precision, from ${\cal O}(\alpha_s^2)$ fits of the c.m.s. energy evolution of some of the observables. A qualitative comparison is made between the data and a recent MLLA prediction for mean jet multiplicities.
    Type of Medium: Electronic Resource
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  • 7
    Publication Date: 2019
    Description: 〈span〉〈div〉Abstract〈/div〉A few, thin, Mississippian siliciclastic limestone beds, interbedded with ammonoid (uppermost 〈span〉Eumorphoceras〈/span〉 Zone)-bearing shales within the South Syncline Ridge section on the Nuclear Test Site in southern Nevada, contain an abundant, low-diversity assemblage of late Serpukhovian/late Chesterian calcareous foraminifers dominated by the archaediscaceans 〈span〉Neoarchaediscus altiluminis〈/span〉, 〈span〉Brenckleina rugosa〈/span〉, 〈span〉Eosigmoilina robertsoni〈/span〉, and 〈span〉Betpakodiscus〈/span〉 of the group 〈span〉B〈/span〉. 〈span〉attenuatus〈/span〉. These limestone beds were deposited in a shallow-water, clastic facies of the Scotty Wash Formation and, based on common conodont occurrences, correlate southeast to the Bird Spring Formation below the Mississippian-Pennsylvanian GSSP at Arrow Canyon, Nevada. The South Syncline Ridge foraminifers are comparable to those found in coeval beds at Arrow Canyon and represent the only other known foraminiferal assemblage to exist in association with uppermost 〈span〉Eumorphoceras〈/span〉 Zone ammonoids in North America outside of Arkansas in the southern Midcontinent. Reconciliation of regional conodont and ammonoid zonations shows that the range of eosigmoiline foraminifers (〈span〉E〈/span〉. 〈span〉robertsoni〈/span〉 and 〈span〉B〈/span〉. 〈span〉rugosa〈/span〉), now generally considered an upper Serpukhovian index, extends from a position either just below or at the lower-upper boundary of the Serpukhovian Stage into the lower part of the Bashkirian Stage in North America; their upper range falls within the lower part of the 〈span〉Homoceras〈/span〉 ammonoid zone beginning in the upper part of the Serpukhovian Stage. Discussion of the foraminiferal taxa includes support for retaining the genus 〈span〉Betpakodiscus〈/span〉 rather than synonymizing it under 〈span〉Tubispirodiscus〈/span〉, as proposed by some specialists during the past few years.〈/span〉
    Print ISSN: 0096-1191
    Electronic ISSN: 1943-264X
    Topics: Geosciences
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  • 8
    Publication Date: 2019
    Description: 〈span〉〈div〉Abstract〈/div〉Pyrite (FeS〈sub〉2〈/sub〉) is a typical container of Pt in ores of magmatic and hydrothermal origin and in some carbonrich ores of sedimentary-diagenetic origin. Knowledge of the state of Pt disseminated in the matrix of pyrite, including local atomic environment (type of atoms in the nearest and distant coordination shells, coordination numbers, interatomic distances) and oxidation state, is necessary for physical-chemical modeling of platinum group element mineralization and for the improvement of Pt ore extraction and processing technologies. Here we report results of an investigation of local atomic structure of synthetic Pt-bearing pyrites by means of X-ray absorption spectroscopy (XAS). Synthesis experiments, performed at 580° and 590°C in a Pt-saturated system by means of salt-flux method, yielded crystals of pyrite with concentrations of Pt up to 4 wt %. Scanning electron microscopy (SEM) and electron probe microanalysis (EPMA) showed that the distribution of Pt within the pyrite grains is of zonal character, but within the distinct zones Pt is distributed homogeneously. Negative correlation between the concentrations of Pt and Fe was observed in the synthesized pyrite grains. The slope of the correlation line corresponds to the formation of the solid solution in the Pt-Fe-S system and/or to the formation of PtS〈sub〉2〈/sub〉. The XAS experiments revealed the existence of two forms of Pt in pyrite. The main form is the solid solution Pt(IV), which isomorphically substitutes for Fe. The Pt-S distance in pyrite is ~0.1 Å longer than that of Fe-S in pure pyrite. The distortion of the pyrite crystal structure disappears at 〈span〉R〈/span〉 〉2.5 Å. The second Pt-rich form was identified by means of high-resolution transmission electron microscopy (HRTEM) as nanosized inclusions of PtS〈sub〉2〈/sub〉. Heating experiments with in situ registration of X-ray absorption spectra resulted in partial decomposition (dissolution) of PtS〈sub〉2〈/sub〉 nanosized inclusions with the formation of the solid solution (Fe〈sub〉1–x〈/sub〉Pt〈sub〉x〈/sub〉)S〈sub〉2〈/sub〉. Therefore, the PtS〈sub〉2〈/sub〉 nanosized particles can be considered as a quench product. Our data demonstrate that both Pt solid solution and PtS〈sub〉2〈/sub〉 nanosized inclusions (at high Pt content) can exist in natural Pt-bearing pyrites.〈/span〉
    Print ISSN: 0361-0128
    Electronic ISSN: 1554-0774
    Topics: Geosciences
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  • 9
    Publication Date: 2000-10-01
    Print ISSN: 1434-6044
    Electronic ISSN: 1434-6052
    Topics: Physics
    Published by Springer
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  • 10
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    PANGAEA
    In:  Supplement to: Lisitzina, Nadezhda A; Butuzova, Galina Yu; Volkov, Igor I; et al. (1979): Lithology and Geochemistry of Pacific Sediments (Transpacific Profile). Geological Institute of the Russian Academy of Sciences, Transactions, vol. 334. Moscow, Nauka Publ. (V.N. Kholodov, Ed.), 263 pp
    Publication Date: 2023-05-12
    Description: The book is devoted to comprehensive study of composition of sediments from the North Pacific Ocean. The sediments have been divided characterized by their lithologic and facial types, grain size composition and mineralogy. Influence of volcanism on formation of mineral and chemical composition of these sediments has been shown. Regularities of distribution of sediment accumulation rates and of a number of chemical elements on the Transpacific profile have been found. Determining role of mechanical fractionation in their localization has been shown.
    Keywords: Archive of Ocean Data; ARCOD; DM9; DM9-611; DM9-612; DM9-613; DM9-615; DM9-625; DM9-626; DM9-627; DM9-628; DM9-629; DM9-641; DM9-643; DM9-645; DM9-647; DM9-649; DM9-651; DM9-653; DM9-655; DM9-668; DM9-669; DM9-670; DM9-671; DM9-672; DM9-673; DM9-674; DM9-675; DM9-677; DM9-678; DM9-685; DM9-686; Dmitry Mendeleev; GC; Grab; GRAB; Gravity corer; MULT; Multiple investigations; Northeast Pacific; North Pacific; Northwest Pacific; OKEAN; Okean Grab; PC; Piston corer; VITYAZ; Vityaz (ex-Mars); Vityaz-29; VITYAZ3625-GC; VITYAZ3784-GC; VITYAZ4285-GR-2; VITYAZ4331-GR-2; VITYAZ4362-GR-2; VITYAZ6158-GC; VITYAZ6159-GC; VITYAZ6160-PC; VITYAZ6161-PC; VITYAZ6162-GC; VITYAZ6163-GC; VITYAZ6164-GC; VITYAZ6165-GR-2; VITYAZ6166-GC; VITYAZ6167-GC; VITYAZ6168-GC; VITYAZ6169-GC; VITYAZ6171-GC; VITYAZ6172-GC; VITYAZ6173-GC; VITYAZ6174-PC; VITYAZ6175-GC; VITYAZ6176-GC
    Type: Dataset
    Format: application/zip, 6 datasets
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