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  • 1
    Monograph available for loan
    Monograph available for loan
    Washington, DC : The World Bank
    Associated volumes
    Call number: 8/M 06.0344 ; PIK D 024-07-0264
    In: Disaster risk management series
    Description / Table of Contents: A global view of major natural disaster risk hotspots - areas at relatively high risk of loss from one or more natural hazards. It summarizes the results of an interdisciplinary analysis of the location and characteristics of hotspots for six natural hazards - earthquakes, volcanoes, landslides, floods, drought, and cyclones.
    Type of Medium: Monograph available for loan
    Pages: xi, 132 S. , graph. Darst., zahlr. Kt.
    ISBN: 0821359304
    Series Statement: Disaster risk management series 5
    Classification:
    B..
    Location: Reading room
    Location: A 18 - must be ordered
    Branch Library: GFZ Library
    Branch Library: PIK Library
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  • 2
    Call number: PIK E 704-93-0012
    Type of Medium: Monograph available for loan
    Pages: VIII, 255 S.
    ISBN: 9027714908
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
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    PANGAEA
    In:  Supplement to: Chen, Robert F; Bada, Jeffrey L (1994): The fluorescence of dissolved organic matter in porewaters of marine sediments. Marine Chemistry, 45(1-2), 31-42, https://doi.org/10.1016/0304-4203(94)90089-2
    Publication Date: 2024-03-09
    Description: The fluorescence of porewaters from marine sediment cores from six different areas was measured. In most cases, fluorescence was affected primarily by the diagenesis of organic carbon first through sulfate reduction and subsequently by methane generation. Typically, fluorescence, dissolved organic carbon (DOC), absorbance, alkalinity, and ammonium ion concentrations correlate quite well, increasing in the upper sections of anoxic sediments and co-varying in deeper sections of these cores. The good correlation of DOC with fluorescence in the three cores in which DOC was measured indicates that fluorescence can be used to make a first order estimate of DOC concentration in anoxic porewaters. Data are consistent with a model in which labile organic matter in the sediments is broken down by sulfur reducing bacteria to low molecular weight monomers. These monomers are either remineralized to CO2 or polymerize to form dissolved, fluorescent, high molecular weight molecules. The few exceptions to this model involve hydrothermally generated hydrocarbons that are formed in situ in the Guaymas Basin or are horizontally advected along the decollement in the Nankai Trench.
    Keywords: 131-808A; 131-808B; 131-808C; 64-478; 64-479; 67-496; 67-499_Site; 74-525_Site; COMPCORE; Composite Core; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Joides Resolution; Leg131; Leg64; Leg67; Leg74; North Pacific/Gulf of California/BASIN; North Pacific/Gulf of California/CHANNEL; North Pacific/TRENCH; Ocean Drilling Program; ODP; Philippine Sea; South Atlantic/CREST
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
    Publication Date: 2024-03-09
    Keywords: Alkalinity, total; Carbon, organic, dissolved; DEPTH, sediment/rock; Fluorescence; LATITUDE; LONGITUDE; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 171 data points
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  • 5
    Publication Date: 2024-03-09
    Keywords: 131-808A; 131-808B; 131-808C; 64-478; 64-479; 67-496; 67-499_Site; 74-525_Site; Absorbance; Alkalinity, total; Carbon, organic, dissolved; COMPCORE; Composite Core; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Fluorescence; Glomar Challenger; Joides Resolution; Leg131; Leg64; Leg67; Leg74; North Pacific/Gulf of California/BASIN; North Pacific/Gulf of California/CHANNEL; North Pacific/TRENCH; Ocean Drilling Program; ODP; Philippine Sea; Sample code/label; South Atlantic/CREST
    Type: Dataset
    Format: text/tab-separated-values, 313 data points
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  • 6
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    PANGAEA
    In:  Supplement to: You, Chen-Feng; Gieskes, Joris M; Chen, Robert F; Spivack, Arthur J; Gamo, Toshitaka (1993): Iodide, bromide, manganese, boron, and dissolved organic carbon in interstitial waters of organic carbon-rich marine sediments: observations in the Nankai accretionary prism. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 165-174, https://doi.org/10.2973/odp.proc.sr.131.116.1993
    Publication Date: 2024-03-09
    Description: This study of the interstitial water concentration-depth distributions of iodide, bromide, boron, d11B, and dissolved organic carbon, as represented by absorbance at 325 nm (yellow substance: YS) and laser-induced fluorescence (LIF), is a follow-up of the extensive shipboard program of interstitial water analysis during ODP Leg 131. Most of the components studied are associated with processes involving the diagenesis of organic matter in these sediments. Three zones of the sediment column are discussed separately because of the different processes involved in causing concentration changes: 1. The upper few hundreds of meters: In this zone, characterized by very high sedimentation rates (〉1200 m/m.y.), interstitial waters show very sharp increases in alkalinity, ammonia, iodide, bromide, YS, and LIF, mainly as a result of the diagenesis of organic carbon; 2. Whereas below 200 mbsf concentration gradients all show a decreasing trend, the zone at ~ 365 mbsf is characterized by concentration reversals, mainly due to the recent emplacement of deeper sediments above this depth as a result of thrust-faulting; 3. The décollement zone (945-964 mbsf) is characterized by concentration anomalies in various constituents (bromide, boron, d11B, manganese, LIF). These data are interpreted as resulting from an advective input of fluids along the zone of décollement as recent as ~ 200 ka. Possibly periodic inputs of anomalous fluids still seem to occur along this décollement zone.
    Keywords: 131-808A; 131-808B; 131-808C; Boron; Bromine; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Fluorescence; Iodide; Joides Resolution; Leg131; Manganese; Ocean Drilling Program; ODP; Philippine Sea; Sample code/label; Yellow substance; δ11B
    Type: Dataset
    Format: text/tab-separated-values, 334 data points
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  • 7
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2018. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 32 (2018): 389-416, doi:10.1002/2017GB005790.
    Description: Carbon cycling in the coastal zone affects global carbon budgets and is critical for understanding the urgent issues of hypoxia, acidification, and tidal wetland loss. However, there are no regional carbon budgets spanning the three main ecosystems in coastal waters: tidal wetlands, estuaries, and shelf waters. Here we construct such a budget for eastern North America using historical data, empirical models, remote sensing algorithms, and process‐based models. Considering the net fluxes of total carbon at the domain boundaries, 59 ± 12% (± 2 standard errors) of the carbon entering is from rivers and 41 ± 12% is from the atmosphere, while 80 ± 9% of the carbon leaving is exported to the open ocean and 20 ± 9% is buried. Net lateral carbon transfers between the three main ecosystem types are comparable to fluxes at the domain boundaries. Each ecosystem type contributes substantially to exchange with the atmosphere, with CO2 uptake split evenly between tidal wetlands and shelf waters, and estuarine CO2 outgassing offsetting half of the uptake. Similarly, burial is about equal in tidal wetlands and shelf waters, while estuaries play a smaller but still substantial role. The importance of tidal wetlands and estuaries in the overall budget is remarkable given that they, respectively, make up only 2.4 and 8.9% of the study domain area. This study shows that coastal carbon budgets should explicitly include tidal wetlands, estuaries, shelf waters, and the linkages between them; ignoring any of them may produce a biased picture of coastal carbon cycling.
    Description: NASA Interdisciplinary Science program Grant Number: NNX14AF93G; NASA Carbon Cycle Science Program Grant Number: NNX14AM37G; NASA Ocean Biology and Biogeochemistry Program Grant Number: NNX11AD47G; National Science Foundation's Chemical Oceanography Program Grant Number: OCE‐1260574
    Description: 2018-10-04
    Keywords: Carbon cycle ; Coastal zone ; Tidal wetlands ; Estuaries ; Shelf waters
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 8
    ISSN: 1520-4804
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    College Park, Md. : American Institute of Physics (AIP)
    Journal of Mathematical Physics 32 (1991), S. 464-465 
    ISSN: 1089-7658
    Source: AIP Digital Archive
    Topics: Mathematics , Physics
    Notes: This paper will amend an earlier paper that derives the real form of Schrödinger's equation. It will remove certain difficulties that are: (1) the problem of gauge invariance and (2) the apparent nonlocality in the inverse Hamiltonian operator. The mathematical tools used here are fairly simple: method for the real dispersive waves of Sommerfeld and Brillouin and the Green's theorem.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    College Park, Md. : American Institute of Physics (AIP)
    Journal of Mathematical Physics 30 (1989), S. 83-86 
    ISSN: 1089-7658
    Source: AIP Digital Archive
    Topics: Mathematics , Physics
    Notes: A unique relationship between the real part and the imaginary part of a wave function that obeys the time-dependent Schrödinger equation is derived. Thence the real form of the Schrödinger equation for the case of a nonconservative time-dependent potential V=V(x,t) is obtained. Earlier work on this subject is found to be inadequate, applicable only to the conservative system. The results obtained here were first sought by Schrödinger but can be used in ways other than his original intention and purposes. Some unresolved issues relating to the nature of the dependency of Im(ψ) and Re(ψ) are also discussed.
    Type of Medium: Electronic Resource
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