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You searched for subject:(sub seafloor). Showing records 1 – 2 of 2 total matches.

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Duke University

1. Worman, Stacey Lynn. Global Rates of Free Hydrogen (H2) Production by Serpentinization and other Abiogenic Processes within Young Ocean Crust .

Degree: 2015, Duke University

The main conclusion of this dissertation is that global H2 production within young ocean crust (<10 Mya) is higher than currently recognized, in part because current estimates of H2 production accompanying the serpentinization of peridotite may be too low (Chapter 2) and in part because a number of abiogenic H2-producing processes have heretofore gone unquantified (Chapter 3). The importance of free H2 to a range of geochemical processes makes the quantitative understanding of H2 production advanced in this dissertation pertinent to an array of open research questions across the geosciences (e.g. the origin and evolution of life and the oxidation of the Earth’s atmosphere and oceans). The first component of this dissertation (Chapter 2) examines H2 produced within young ocean crust [e.g. near the mid-ocean ridge (MOR)] by serpentinization. In the presence of water, olivine-rich rocks (peridotites) undergo serpentinization (hydration) at temperatures of up to ~500°C but only produce H2 at temperatures up to ~350°C. A simple analytical model is presented that mechanistically ties the process to seafloor spreading and explicitly accounts for the importance of temperature in H2 formation. The model suggests that H2 production increases with the rate of seafloor spreading and the net thickness of serpentinized peridotite (S-P) in a column of lithosphere. The model is applied globally to the MOR using conservative estimates for the net thickness of lithospheric S-P, our least certain model input. Despite the large uncertainties surrounding the amount of serpentinized peridotite within oceanic crust, conservative model parameters suggest a magnitude of H2 production (~1012 moles H2/y) that is larger than the most widely cited previous estimates (~1011 although previous estimates range from 1010-1012 moles H2/y). Certain model relationships are also consistent with what has been established through field studies, for example that the highest H2 fluxes (moles H2/km2 seafloor) are produced near slower-spreading ridges (<20 mm/y). Other modeled relationships are new and represent testable predictions. Principal among these is that about half of the H2 produced globally is produced off-axis beneath faster-spreading seafloor (>20 mm/y), a region where only one measurement of H2 has been made thus far and is ripe for future investigation. In the second part of this dissertation (Chapter 3), I construct the first budget for free H2 in young ocean crust that quantifies and compares all currently recognized H2 sources and H2 sinks. First global estimates of budget components are proposed in instances where previous estimate(s) could not be located provided that the literature on that specific budget component was not too sparse to do so. Results suggest that the nine known H2 sources, listed in order of quantitative importance, are: Crystallization (6x1012 moles H2/y or 61% of total H2 production), serpentinization (2x1012 moles H2/y or 21%), magmatic degassing (7x1011 moles H2/y or 7%), lava-seawater… Advisors/Committee Members: Pratson, Lincoln F (advisor).

Subjects/Keywords: Geology; Biogeochemistry; Geomorphology; Barchan Sand Dunes; Free Hydrogen Production; Global Estimates; Reduced Gases; Serpentinization; Sub-seafloor Microbes

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6th Edition):

Worman, S. L. (2015). Global Rates of Free Hydrogen (H2) Production by Serpentinization and other Abiogenic Processes within Young Ocean Crust . (Thesis). Duke University. Retrieved from http://hdl.handle.net/10161/10490

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16th Edition):

Worman, Stacey Lynn. “Global Rates of Free Hydrogen (H2) Production by Serpentinization and other Abiogenic Processes within Young Ocean Crust .” 2015. Thesis, Duke University. Accessed July 09, 2020. http://hdl.handle.net/10161/10490.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7th Edition):

Worman, Stacey Lynn. “Global Rates of Free Hydrogen (H2) Production by Serpentinization and other Abiogenic Processes within Young Ocean Crust .” 2015. Web. 09 Jul 2020.

Vancouver:

Worman SL. Global Rates of Free Hydrogen (H2) Production by Serpentinization and other Abiogenic Processes within Young Ocean Crust . [Internet] [Thesis]. Duke University; 2015. [cited 2020 Jul 09]. Available from: http://hdl.handle.net/10161/10490.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Worman SL. Global Rates of Free Hydrogen (H2) Production by Serpentinization and other Abiogenic Processes within Young Ocean Crust . [Thesis]. Duke University; 2015. Available from: http://hdl.handle.net/10161/10490

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation


Delft University of Technology

2. Siemes, K. Establishing a sea bottom model by applying a multi-sensor acoustic remote sensing approach.

Degree: 2013, Delft University of Technology

Detailed information about the oceanic environment is essential for many applications in the field of marine geology, marine biology, coastal engineering, and marine operations. Especially, knowledge of the properties of the sediment body is often required. Acoustic remote sensing techniques have become highly attractive for classifying the sea bottom and for mapping the sediment properties, due to their high coverage capabilities and low costs compared to common sampling methods. In the last decades, a number of different acoustic devices and related techniques for analyzing their signals have evolved. Each sensor has its specific application due to limitations in the frequency range and resolution. In practice, often a single acoustic tool is chosen based on the current application, supported by other non-acoustic data where required. However, different acoustic remote sensing techniques can supplement each other, as shown in this thesis. Even more, a combination of complementary approaches can contribute to the proper understanding of sound propagation, which is essential when using sound for environmental classification purposes. This includes the knowledge of the relation between acoustics and sediment properties, the focus of this thesis. Providing a detailed three dimensional picture of the sea bottom sediments that allows for gaining maximum insight into this relation is aimed at. Chapters 4 and 5 are adapted from published work, with permission: DOI:10.1121/1.3569718 (link: http://asadl.org/jasa/resource/1/jasman/v129/i5/p2878_s1) and DOI:10.1109/JOE.2010.2066711 (link: http://ieeexplore.ieee.org/xpl/articleDetails.jsp?tp=&arnumber=5618582&queryText%3Dsiemes) In reference to IEEE copyrighted material which is used with permission in this thesis, the IEEE does not endorse any of the TU Delft's products or services. Advisors/Committee Members: Simons, D.G., Hermand, J.P.O.F.G..

Subjects/Keywords: acoustic remote sensing; marine sediment; sub-seafloor; environmental characterization; single-beam echosounder; multibeam echosounder; seismic profiling; chirp; geoacoustic inversion; phenomenological approach; model-based approach; density; compressional sound speed; acoustic attenuation; sediment samples; fine-grained sediments; gas

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6th Edition):

Siemes, K. (2013). Establishing a sea bottom model by applying a multi-sensor acoustic remote sensing approach. (Doctoral Dissertation). Delft University of Technology. Retrieved from http://resolver.tudelft.nl/uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; urn:NBN:nl:ui:24-uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; urn:NBN:nl:ui:24-uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; http://resolver.tudelft.nl/uuid:92e94609-ec37-43e5-ad01-3817756d30f6

Chicago Manual of Style (16th Edition):

Siemes, K. “Establishing a sea bottom model by applying a multi-sensor acoustic remote sensing approach.” 2013. Doctoral Dissertation, Delft University of Technology. Accessed July 09, 2020. http://resolver.tudelft.nl/uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; urn:NBN:nl:ui:24-uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; urn:NBN:nl:ui:24-uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; http://resolver.tudelft.nl/uuid:92e94609-ec37-43e5-ad01-3817756d30f6.

MLA Handbook (7th Edition):

Siemes, K. “Establishing a sea bottom model by applying a multi-sensor acoustic remote sensing approach.” 2013. Web. 09 Jul 2020.

Vancouver:

Siemes K. Establishing a sea bottom model by applying a multi-sensor acoustic remote sensing approach. [Internet] [Doctoral dissertation]. Delft University of Technology; 2013. [cited 2020 Jul 09]. Available from: http://resolver.tudelft.nl/uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; urn:NBN:nl:ui:24-uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; urn:NBN:nl:ui:24-uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; http://resolver.tudelft.nl/uuid:92e94609-ec37-43e5-ad01-3817756d30f6.

Council of Science Editors:

Siemes K. Establishing a sea bottom model by applying a multi-sensor acoustic remote sensing approach. [Doctoral Dissertation]. Delft University of Technology; 2013. Available from: http://resolver.tudelft.nl/uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; urn:NBN:nl:ui:24-uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; urn:NBN:nl:ui:24-uuid:92e94609-ec37-43e5-ad01-3817756d30f6 ; http://resolver.tudelft.nl/uuid:92e94609-ec37-43e5-ad01-3817756d30f6

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