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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Uranium-thorium dating. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (471 pages)
    Edition: 1st ed.
    ISBN: 9780080564883
    Series Statement: Issn Series ; v.Volume 13
    DDC: 546.431
    Language: English
    Note: Front Cover -- U-Th Series Nuclides in Aquatic Systems -- Copyright page -- Dedication to Karl K. Turekian -- Contents -- Contributors -- Chapter 1. Introduction -- 1. Overview -- 2. Organization of the Volume -- Acknowledgements -- References -- Chapter 2. U- and Th-Series Nuclides in the Atmosphere: Supply, Exchange, Scavenging, and Applications to Aquatic Processes -- 1. Introduction -- 2. Sources of U- and Th-Series Nuclides to the Atmosphere -- 3. Atmospheric Distributions -- 4. Aerosol Scavenging Residence Times Using 222Rn and its Daughters -- 5. Applications of Rn Daughters of Atmospheric Origin to Study Aquatic Processes -- 6. Processes across Aquatic Interfaces -- 7. Perspectives and Future Directions -- Acknowledgements -- References -- Chapter 3. U-Series Geochemistry in Weathering Profiles, River Waters and Lakes -- 1. Introduction -- 2. Radionuclide Fractionation in Surface Environments -- 3. Radioactive Disequilibria in Weathering Profiles and Soils -- 4. U Series in Rivers -- 5. Review of Models for U-Series Fractionation in Surficial Environments -- 6. U-Series Disequilibria in Lakes -- 7. Future Perspectives -- Acknowledgments -- References -- Chapter 4. Investigating Groundwater Processes Using U- and Th-Series Nuclides -- 1. Introduction -- 2. General Element Behavior in Groundwaters -- 3. Modeling Nuclide Transport in Aquifers -- 4. Obtaining Solutions to the Model Equations -- 5. Radon and Recoil Rates -- 6. Ra Isotopes -- 7. Th Isotopes -- 8. U Isotopes -- 9. 210Pb -- 10. Summary and Future Studies -- Acknowledgments -- References -- Chapter 5. Uranium- and Thorium-Series Nuclides as Tracers of Submarine Groundwater Discharge -- 1. Introduction -- 2. How U-Th Isotopes are Used to Quantify Submarine Groundwater Discharge (SGD) -- 3. Radium -- 4. Radon -- 5. Uranium -- 6. Synthesis of Existing Studies. , 7. Towards a Global Estimate of SGD -- 8. Perspectives and Future Directions -- Acknowledgments -- References -- Chapter 6. U- and Th-Series Nuclides in Estuarine Environments -- 1. Introduction: Estuarine Processes -- 2. Uranium -- 3. Thorium -- 4. Radium -- 5. Radon -- 6. Lead-210 and Polonium-210 -- 7. Future Studies -- References -- Chapter 7. U- and Th-Series Nuclides as Tracers of Particle Dynamics, Scavenging and Biogeochemical Cycles in the Oceans -- 1. Abundance and Distribution of U-Th Nuclides in the Sea -- 2. Introduction to Particle Cycling and Scavenging in the Ocean -- 3. The Scavenging Process as Understood from Thorium Isotopes -- 4. Scavenging and Th Speciation -- 5. 226Ra-210Pb-210Po -- 6. The Role of Particle Composition -- 7. Boundary Scavenging -- 8. Calibration of Vertical Particle Fluxes -- 9. Summary and Outlook -- References -- Chapter 8. The Bioaccumulation of U- and Th-Series Radionuclides in Marine Organisms -- 1. Introduction -- 2. Radionuclides of Interest and their Bioavailability -- 3. Models of Uptake and Trophic Transfer -- 4. Biodetritus and Vertical Transport -- 5. Potential Impacts of Natural Radioactivity -- 6. Synthesis and Conclusions -- 7. Future Outlook and Perspectives -- References -- Chapter 9. Ocean Circulation/Mixing Studies with Decay-Series Isotopes -- 1. Introduction -- 2. General Transport Equations -- 3. Basic Ocean Mixing/Circulation Models -- 4. Radium Isotopes for Tracing Oceanic Mixing/Circulation -- 5. Radon-222 as a Vertical Mixing Tracer in the Deep Sea -- 6. Actinium-227 as a Diapycnal Mixing Tracer in the Deep Sea -- 7. Tracing Ocean Circulation Using Particle-Reactive Radionuclides -- 8. Closing Remarks and Future Prospects -- Acknowledgments -- References -- Chapter 10. Uranium- and Thorium-Series Radionuclides in Marine Groundwaters -- 1. Introduction. , 2. U- and Th-Series Radionuclides in High-Temperature Marine Groundwaters: Hydrothermal Fluids -- 3. U- and Th-Series Radionuclides in Low-Temperature Marine Groundwaters: Sediment Pore Water -- 4. Future Directions -- Acknowledgments -- References -- Chapter 11. Sediment Signatures of U- and Th-Series Nuclides and their Application as Paleoceanographic Tracers -- 1. Introduction -- 2. Long-Lived U-Series Nuclides in Sediments -- 3. Short-Lived U-Series Nuclides in Sediments: Application to Sediment Mixing and Accumulation -- 4. Authigenic Uranium as a Tracer of Sediment Redox State -- 5. Use of 230Th as a Constant Flux Proxy -- 6. 231Pa/230Th: Proxy for Particle Flux and Productivity -- 7. 231Pa/230Th: Proxy of Ocean Circulation -- 8. Modeling Studies -- 9. Manganese Crusts and Nodules -- 10. Summary and Outlook -- Acknowledgments -- References -- Appendix A. Charts of the 238U, 235U, 232Th, and 241Am Decay Series with Principal Modes of Decay, their Intensities and Energies -- 1. Introduction -- 2. Sources of Data -- References -- Appendix B. Systematics of Radioactive Decay -- 1. Overview of Decay Equations -- 2. Examples of Applications -- References -- Author Index -- Subject Index.
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  • 2
    Type of Medium: Book
    Pages: S. 1363 - 1567 , Ill., graph. Darst
    Series Statement: Deep sea research 56.2009,18
    Language: English
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  • 3
    Book
    Book
    Amsterdam : Elsevier
    Keywords: Uranium-thorium dating ; Water chemistry ; Hydrogeologie ; Grundwasser ; Thorium ; Uran ; Grundwasserstrom ; Tracer ; Meereskunde ; Thorium ; Uran ; Radionuklid ; Hydrogeochemie ; Biogeochemie ; Paläoozeanographie ; Methode ; Anwendung ; Hydrogeologie ; Grundwasser ; Thorium ; Uran ; Grundwasserstrom ; Tracer ; Meereskunde ; Radionuklid ; Hydrogeochemie ; Biogeochemie ; Paläoozeanographie ; Methode ; Anwendung
    Type of Medium: Book
    Pages: XII, 458 S. , Ill., graph. Darst., Kt.
    Edition: 1. ed.
    ISBN: 0080452124 , 9780080450124 , 0080450121
    Series Statement: Radioactivity in the environment vol. 13
    Language: English
    Note: Includes bibliographical references and index
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  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © The Authors, 2006. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Marine Chemistry 100 (2006): 213-233, doi:10.1016/j.marchem.2005.10.013.
    Description: Thorium-234 is increasingly used as a tracer of ocean particle flux, primarily as a means to estimate particulate organic carbon export from the surface ocean. This requires determination of both the 234Th activity distribution (in order to calculate 234Th fluxes) and an estimate of the C/234Th ratio on sinking particles, to empirically derive C fluxes. In reviewing C/234Th variability, results obtained using a single sampling method show the most predictable behavior. For example, in most studies that employ in situ pumps to collect size fractionated particles, C/234Th either increases or is relatively invariant with increasing particle size (size classes 〉1 to 100’s μm). Observations also suggest that C/234Th decreases with depth and can vary significantly between regions (highest in blooms of large diatoms and highly productive coastal settings). Comparisons of C fluxes derived from 234Th show good agreement with independent estimates of C flux, including mass balances of C and nutrients over appropriate space and time scales (within factors of 2-3). We recommend sampling for C/234Th from a standard depth of 100 m, or at least one depth below the mixed layer using either large volume size fractionated filtration to capture the rarer large particles, or a sediment trap or other device to collect sinking particles. We also recommend collection of multiple 234Th profiles and C/234Th samples during the course of longer observation periods to better sample temporal variations in both 234Th flux and the characteristic of sinking particles. We are encouraged by new technologies which are optimized to more reliably sample truly settling particles, and expect the utility of this tracer to increase, not just for upper ocean C fluxes but for other elements and processes deeper in the water column.
    Description: Individuals and science efforts discussed herein were supported by many national science programs, including the U.S. National Science Foundation and U.S. Department of Energy. S.F. and J.C.M. acknowledge the support provided to the International Atomic Energy Agency (IAEA) Marine Environment Laboratory by the Government of the Principality of Monaco. T.T. acknowledges support from the Australian Antarctic Science Program. K.B. was supported in part by a WHOI Ocean Life Institute Fellowship.
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: 640962 bytes
    Format: application/pdf
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  • 5
    Publication Date: 2022-05-25
    Description: Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Marine Chemistry 100 (2006): 234-249, doi:10.1016/j.marchem.2005.10.014.
    Description: Over the past few decades, the radioisotope pair of 238U/234Th has been widely and increasingly used to describe particle dynamics and particle export fluxes in a variety of aquatic systems. The present paper is one of five review articles dedicated to 234Th. It is focused on the models associated with 234Th whereas the companion papers (same issue) are focused on present and future methodologies and techniques (Rutgers van der Loeff et al.), C/234Th ratios (Buesseler et al.), 234Th speciation (Santschi et al.) and present and future applications of 234Th (Waples et al.). In this paper, we review current 234Th scavenging models and discuss the relative importance of the non steady state and physical terms associated with the most commonly used model to estimate 234Th flux. Based on this discussion we recommend that for future work the use of models should be accompanied by a discussion of the effect that model and data uncertainty have on the model results. We also suggest that future field work incorporate repeat occupations of sample sites on time scales of 1-4 weeks in order to evaluate steady state versus non steady state estimates of 234Th export, especially during high flux events (〉 ca. 800 dpm m-2 d-1). Finally, knowledge of the physical oceanography of the study area is essential, particularly in ocean margins and in areas of established upwelling (e.g. Equatorial Pacific). These suggestions will greatly enhance the application of 234Th as a tracer of particle dynamics and flux in more complicated regimes.
    Description: This paper grew out of discussion held at the “Future Applications of 234Th in Aquatic Systems” workshop held at Woods Hole Oceanographic Institution in August, 2004 (see: http://www.geol.sc.edu/cbnelson/Thmeeting/). We are grateful to the US National Science Foundation Chemical Oceanography Program (OCE 0354757) for its support of the workshop. We thank the US National Science Foundation, the National Oceanic and Atmospheric Administration and the Belgian Science Policy for their support of many of the field and modeling efforts described in this paper.
    Keywords: Th-234 ; Model ; Scavenging ; Export ; Particle dynamics
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: 2096326 bytes
    Format: application/pdf
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  • 6
    Publication Date: 2018-03-09
    Description: A mass balance for the naturally-occurring radium isotopes (224Ra, 223Ra, 228Ra, and 226Ra) in Jamaica Bay, NY, was conducted by directly estimating the individual Ra contributions of wastewater discharge, diffusion from fine-grained subtidal sediments, water percolation through marshes, desorption from resuspended particles, and water exchange at the inlet. The mass balance revealed a major unknown source term accounting for 19–71% of the total Ra input, which could only be resolved by invoking a source from submarine groundwater. Shallow (〈 2 m depth) groundwater from permeable sediments in Jamaica Bay was brackish and enriched in Ra relative to surface bay waters by over two orders of magnitude. To balance Ra fluxes, a submarine groundwater input of 0.8 × 109–9.0 × 109 L d− 1 was required. This flux was similar for all four isotopes, with individual estimates varying by less than a factor of 2. Our calculated groundwater flux was 6- to 70-fold higher than the fresh groundwater discharge to the bay estimated by hydrological methods, but closely matched direct flow rates measured with seepage meters. This suggests that a substantial portion of the discharge consisted of recirculated seawater. The magnitude of submarine groundwater discharge varied seasonally, in the order: summer 〉 autumn 〉 spring. Chemical analyses suggest that the recirculated seawater component of submarine groundwater delivers as much dissolved nitrogen to the bay as the fresh groundwater flux.
    Type: Article , PeerReviewed
    Format: text
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  • 7
    Publication Date: 2020-03-20
    Description: The MedFlux project was devised to determine and model relationships between organic matter and mineral ballasts of sinking particulate matter in the ocean. Specifically we investigated the ballast ratio hypothesis, tested various commonly used sampling and modeling techniques, and developed new technologies that would allow better characterization of particle biogeochemistry. Here we describe the rationale for the project, the biogeochemical provenance of the DYFAMED site, the international support structure, and highlights from the papers published here. Additional MedFlux papers can be accessed at the MedFlux web site (http://msrc.sunysb.edu/MedFlux/).
    Type: Article , PeerReviewed
    Format: text
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