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  • 1
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1480)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 26 S.
    Series Statement: U.S. Geological Survey bulletin 1480
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0008(85-16)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 11 S. + 9 pl.
    ISBN: 0660120437
    Series Statement: Paper / Geological Survey of Canada 85-16
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Journal of applied electrochemistry 15 (1985), S. 23-27 
    ISSN: 1572-8838
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Electrical Engineering, Measurement and Control Technology
    Notes: Abstract An Ni-Mn-Zn alloy has been satisfactorily electrodeposited from a sulphate bath containing nickel sulphate (20–23 g dm−3), manganese sulphate (76–88 g dm−3), zinc sulphate (18–24 g dm−3), ammonium sulphate (30 g dm−3), thiourea (18g dm−3) and ascorbic acid (0.8 g dm−3) under various plating conditions, namely, current density 1.0–3.0 A dm−2; temperature 30–45° C; pH 2.7–4.2 and duration of electrolysis 15–30 min. Semibright, blackish-grey, thin films were generally deposited with the proportion of nickel and manganese in the deposits increasing with increasing current density, temperature and duration of electrolysis. However, the amount of zinc increased as the pH of the solution was raised. The cathode efficiency for alloy deposition increased linearly as the temperature or the pH of the solution was decreased, whereas at any particular pH and temperature it continuously rose with increasing current density or the time of deposition. The cathode polarization shifted to more negative values on increasing the current density and to less negative values at higher pH values and temperatures which consequently lowered the throwing power under the latter conditions.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2012-03-01
    Print ISSN: 0018-019X
    Electronic ISSN: 1522-2675
    Topics: Chemistry and Pharmacology
    Published by Wiley
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  • 5
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    Atlantic Oceanographic Institute
    In:  EPIC3Darmouth, Nova Scotia, Canada, Atlantic Oceanographic Institute
    Publication Date: 2015-12-04
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
    Format: image/jpeg
    Format: image/jpeg
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    Format: application/pdf
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  • 6
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    In:  http://aquaticcommons.org/id/eprint/16007 | 12051 | 2015-01-19 19:17:05 | 16007 | Indian Fisheries Association
    Publication Date: 2021-07-11
    Description: The toxicity of methyl amine was studied by finding out its LC 50 values for Catla catla fingerlings. On the basis of LC 50 values, the harmless concentration of methyl amine was found to be 12.8 ppm. This indicates that methyl amine is fairly toxic to C. catla fingerlings and needs care for its disposal in aquatic environment.
    Keywords: Biology ; Pollution ; cultured organisms ; chemical pollutants ; bioassays ; Catla catla ; freshwater
    Repository Name: AquaDocs
    Type: article
    Format: application/pdf
    Format: application/pdf
    Format: 549-553
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  • 7
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    Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research
    In:  EPIC3Polarforschung, Bremerhaven, Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research, 48(1/2), pp. 181, ISSN: 0032-2490
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: "Polarforschung" , peerRev
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  • 8
    Publication Date: 2023-07-10
    Description: The mass balance observations have been carried out on Chhota Shigri Glacier since 2002. Due to difficult glacier accessibility, dynamics, and involvement of different researchers, the measurement network differs in space over time. Further, almost all glaciological mass balance series are affected by the systematic biases due to specifically designed point mass balance network, and lack of basal and internal mass loss measurements. The goal of this study is to re-analyze the mass balances on Chhota Shigri Glacier and provide a homogenized series. We applied the nonlinear model of Vincent and others (2018) to capture the spatiotemporal changes in point mass balances and re-estimated the annual glacier-wide mass balances over 2002-2020. The nonlinear model also allows to detect the erroneous point measurements which are either corrected from the field notebooks or removed from the analysis. The mass balances are then homogenized applying the areal changes estimated using SPOT5 (2005) and Pléiades images (2014 and 2020), assuming a linear areal change. Finally, the mass balances are adjusted using the geodetic mass balances estimated by differencing ASTER and Pléiades DEMs (Oct 2003–Sept 2014) and Pléiades DEMs (Sept 2014–Sept 2020). The reanalyzed mean annual glacier-wide mass balance is estimated to be –0.47 ± 0.18 m w.e. a〈sup〉−1〈/sup〉 (equivalent to a cumulative mass loss of –8.40 m w.e.) with a standard deviation of 0.66 m w.e. a〈sup〉−1〈/sup〉 over 2002-2020. The glacier lost maximum mass of –1.29 ± 0.16 m w.e. in 2017/18 while gained a mass of 0.49 ± 0.19 m w.e. in 2004/05.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 9
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-09-18
    Description: Due to limited in-situ observations, the glaciohydrological modelling is challenging in the Himalaya-Karakoram (HK) region. The present study reconstructs the runoffs in the Chandra-Bhaga basin, where a good amount of in-situ data is available. The SPHY (spatial processes in hydrology), a fully distributed high-resolution hydrological model, is applied over 1979-2020 using ERA5 reanalysis, Globcover land use and HiHydrosoil satellite products. The model is calibrated using 5 years (2010-2015) of in-situ catchment-wide runoff at the Chhota Shigri Glacier catchment outlet and validated with the available 6 years (2000-2006) of in-situ basin-wide runoff at the Chandra-Bhaga basin outlet. The modelled mean annual runoff for the Chandra-Bhaga basin is estimated as 57.79 ± 10.4 m3s-1 over 1979-2020. Maximum runoff occurs during summer-monsoon months, with a peak in July (132.74 ± 59.25 m3s-1). Glacier melt and snowmelt from the glacierized basin area, snowmelt from the non-glacierized basin area, rainfall-runoff and baseflow contribute 38%, 28%, 22% and 12%, respectively, to the total runoff at the basin outlet. The most sensitive model parameters are ‘GlacF’, which differentiates between the amount of glacier melt resulting in direct runoff and ‘Tm’, the threshold temperature for melting. The analysis also indicates that the hydrology of the Chandra-Bhaga basin is mainly dominated by summer precipitation. The study, using sufficient amount of in-situ data at the glacier catchment scale provides reliable reconstructed long-term runoffs for the basin.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 10
    Publication Date: 2024-02-26
    Description: The Bakreswar geothermal province represents a medium enthalpy geothermal system with its Bakreswar and Tantloie hot springs. It lies within the Chotanagpur Granite Gneissic Complex in the eastern part of the Indian Peninsula. The province has a high heat flow and a high geothermal gradient of 90°C/km. Magnetotelluric data from 95 sites in a frequency range of 10 kHz–10 Hz were acquired over the Bakreswar geothermal province to obtain an electrical conductivity model and map the geothermal reservoir with its fluid pathways and related geological structures. Subsurface conductivity models obtained from three-dimensional inversions of the Magnetotelluric data exhibit several prominent anomalies, which are supplemented by gravity results. The conductivity model maps three features which act as a conduit (a) a northwest–southeast trending feature, (b) an east–west trending feature to the south of the northwest–southeast trending feature (which lies 1 km north of the Oil and Natural Gas Corporation fault marked by previous studies) and (c) shallow conducting features close to Bakreswar hot spring. The northwest–southeast trending feature coincides with the boundary of the high-density intrusive block. This northwest–southeast trending feature provides the pathway for the meteoric water to reach a maximum depth of 2.7 km, where it gets heated by interacting with deep-seated structures and then it rises towards the surface. The radiogenic process occurring within the granites of Chotanagpur Granite Gneissic Complex provides the heat responsible for heating the meteoric water. The northwest–southeast and east–west trending features are responsible for the transport of meteoric water to deeper depths and then towards the shallow regions of the Earth. The near surface features close to the Bakreswar hot spring are responsible for carrying the water further towards the hot spring. The resistivity of these structures plotted as a function of salinity and temperatures for saline crustal fluids suggests the involvement of meteoric water. Further, applying Archie's law to this resistivity suggests that the conduit path has a porosity greater than 10%. This study successfully maps the anomalous structures which might foster the migration of geothermal fluid in Bakreswar geothermal province.
    Type: info:eu-repo/semantics/article
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