Article
Energy & Fuels
Zhen Li, Erik Spangenberg, Judith M. Schicks, Thomas Kempka
Summary: The Mackenzie Delta is a permafrost-bearing region in the Canadian Arctic with high sub-permafrost gas hydrate reserves. The gas hydrates in the region are dominated by thermogenic methane migrated from deep hydrocarbon reservoirs. A numerical model simulation validates the hypothesis that dissolved methane from deeper reservoirs forms the gas hydrate accumulations in the delta. The simulation also reveals the impact of global temperature increase and Arctic Amplification effect on permafrost temperatures.
Article
Environmental Sciences
Julia A. Guimond, Cansu Demir, Barret L. Kurylyk, Michelle A. Walvoord, James W. Mcclelland, M. Bayani Cardenas
Summary: Groundwater discharge to the ocean along Arctic coastlines plays a significant role in carbon budgets and water quality. This study investigates the magnitude and drivers of groundwater discharge to Alaska's Beaufort Sea coast using unique coastal Arctic groundwater timeseries data. The results reveal temporally variable groundwater fluxes driven by wind-driven lagoon water level changes, with implications for nearshore biogeochemistry.
ENVIRONMENTAL RESEARCH LETTERS
(2023)
Article
Environmental Sciences
Julia A. Guimond, Aaron A. Mohammed, Michelle A. Walvoord, Victor F. Bense, Barret L. Kurylyk
Summary: This study investigates the impacts of sea-level change and land and ocean warming on coastal groundwater discharge using a hydrological model. The results show that the discharge can increase or decrease depending on the rate of warming and sea-level change.
ENVIRONMENTAL RESEARCH LETTERS
(2022)
Article
Geochemistry & Geophysics
H. Grob, M. Riedel, M. J. Duchesne, S. Krastel, J. Bustamante, G. Fabien-Ouellet, Y. K. Jin, J. K. Hong
Summary: The Canadian Arctic Southern Beaufort Sea has significant relict submarine permafrost and gas hydrate occurrences formed during previous glaciations. The degradation of submarine permafrost releases greenhouse gases, contributing to climate change. This study investigates the presence of submarine permafrost and gas hydrates on the outer continental shelf using seismic reflection indicators. The findings confirm the distribution of present submarine permafrost along the southern Canadian Beaufort Sea region and extend it to the outer continental shelf.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2023)
Article
Multidisciplinary Sciences
Nikolaus Froitzheim, Jaroslaw Majka, Dmitry Zastrozhnov
Summary: Thawing Arctic permafrost may release methane, accelerating anthropogenic global warming. Uncertainties remain regarding carbon stocks and methane emissions.
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
(2021)
Article
Energy & Fuels
Evgeny Chuvilin, Valentina Ekimova, Dinara Davletshina, Ekaterina Krivokhat, Vladimir Shilenkov, Boris Bukhanov
Summary: The development of the Arctic region faces challenges such as methane emission from permafrost. While the effects of temperature and pressure on gas hydrates have been studied, the chemical effects, such as salt migration, remain poorly understood. This study investigates the interaction of frozen hydrate-saturated sediments with NaCl solutions under different gas pressures.
Article
Ecology
Poornima Unnikrishnan, Reji Srinivas, Murugan Ramasamy, D. S. Suresh Babu
Summary: The study investigated submarine groundwater discharge and its behavior influenced by coastal geomorphology and geology. Numerical models were developed to estimate the magnitude of SGD from different catchments on the Southwest coast of India. The results showed significant differences in SGD flux between catchments, with potential implications for designing aquifer recharge options and optimum pumping quantities.
REGIONAL STUDIES IN MARINE SCIENCE
(2021)
Article
Environmental Sciences
Jiawei Liu, Yuanqing Chen, Yiqing Wang, Mengran Du, Zijun Wu
Summary: This study investigated greenhouse gas emissions in a maricultural bay in north-eastern Hainan Island, China, and found that both submarine groundwater discharge and mariculture activities influenced the emissions. The emissions varied with tidal fluctuations and the main mechanism of methane emissions was acetate fermentation. The study highlights the importance of considering the link between submarine groundwater discharge and greenhouse gas emissions in maricultural bays when constraining global greenhouse gas fluxes.
SCIENCE OF THE TOTAL ENVIRONMENT
(2023)
Article
Energy & Fuels
Tao Yu, Guoqing Guan, Dayong Wang, Yongchen Song, Abuliti Abudula
Summary: In 2017, a successful offshore methane hydrate production test was conducted at well SHSC-4 in the Shenhu Area of the South China Sea, but the long-term gas production behavior remains unknown and further investigation is required. In this study, a multi-layered methane hydrate reservoir model was built based on the actual geological conditions at this site, and long-term simulations were conducted to predict hydrate dissociation and gas production behaviors in the reservoir, revealing that the majority of gas production originated from the free gas layer, followed by methane gas released from hydrate dissociation, while the three-phase layer contributed the least to gas recovery.
Article
Energy & Fuels
Pengfei Wang, Ying Teng
Summary: The heterogeneous distribution of hydrate in the experiment leads to local low temperature, which has a significant impact on the hydrate dissociation process. The methane production in the experiment is lower than the simulation, and the high water saturation in the Class 2 sample affects gas flow.
Article
Geochemistry & Geophysics
Ruiling Tang, Jinli Xu, Ziwan Chen, Bin Liu, Jinfeng Bai
Summary: This study examines the potential of using inert gas as a new tool for investigating gas hydrates in permafrost areas. By analyzing the inert gas anomalies near the ground surface of the Muli coalfield in the Qilian Mountains, the study shows that this method is not affected by marsh microorganisms and can be a practical tool for natural gas hydrate exploration in permafrost areas.
Article
Environmental Sciences
Zihan Zheng, Yuncheng Cao, Wenyue Xu, Duofu Chen
Summary: The lack of quantification of deep dissolved methane flux in hydrate systems limits our understanding of methane accumulation and distribution. This study proposes a numerical model to quantify the dissolved methane flux based on parameters related to gas bubble distribution. The model is then applied to ODP Site 995 at the Blake Ridge, showing consistent results with seismic data. The study also explores the influence of upward methane flux on hydrate accumulation and provides insights into regional methane flux estimation.
FRONTIERS IN MARINE SCIENCE
(2022)
Article
Thermodynamics
Yongchang Feng, Lin Chen, Yuki Kanda, Anna Suzuki, Atsuki Komiya, Shigenao Maruyama
Summary: Artificial fractures in methane hydrate reservoirs can significantly improve hydrate dissociation and gas production efficiency, particularly in the early depressurization stage. Higher fracture permeability may shorten the economical production stage but lead to higher production rates. Furthermore, fractures facilitate the flow of hot water into the sediment, enhancing production efficiency during the economical production stage.
Article
Energy & Fuels
Wenyuan Liu
Summary: In this study, a novel mathematical prediction model of hydrate formation risk in deepwater submarine pipelines was established. The model was applied and sensitivity analysis of typical factors was carried out. The model prediction results showed that the hydrate formation region often exists in submarine pipelines due to the low temperature of the seabed, and it increases with the decrease in seawater temperature. Additionally, the temperature drop and the length of the hydrate formation region decrease with the increase of gas transmission rate and gas transport temperature.
PETROLEUM SCIENCE AND TECHNOLOGY
(2023)
Article
Chemistry, Multidisciplinary
Lele Yang, Jing Wang, Yongliang Yang, Guangrui Sun
Summary: This study analyzed the changes in internal stress and hydrate saturation of the soil during the trial production of gas hydrates, calculating the failure stress of the hydrate deposit layer and verifying the feasibility of the method using the Mohr-Coulomb model. Numerical simulations were conducted to evaluate the stability of the soil, with findings showing that the hydrate decomposition range has the greatest impact on deformation.
Article
Geosciences, Multidisciplinary
Matthew A. Thomas, Alejandro Mota, Benjamin M. Jones, R. Charles Choens, Jennifer M. Frederick, Diana L. Bull
FRONTIERS IN EARTH SCIENCE
(2020)
Article
Geosciences, Multidisciplinary
Rodrigo Chi-Duran, Margaret S. Avery, Nicholas Knezek, Bruce A. Buffett
GEOPHYSICAL RESEARCH LETTERS
(2020)
Article
Environmental Sciences
Sayedeh Sara Sayedi, Benjamin W. Abbott, Brett F. Thornton, Jennifer M. Frederick, Jorien E. Vonk, Paul Overduin, Christina Schadel, Edward A. G. Schuur, Annie Bourbonnais, Nikita Demidov, Anatoly Gavrilov, Shengping He, Gustaf Hugelius, Martin Jakobsson, Miriam C. Jones, DongJoo Joung, Gleb Kraev, Robie W. Macdonald, A. David McGuire, Cuicui Mu, Matt O'Regan, Kathryn M. Schreiner, Christian Stranne, Elena Pizhankova, Alexander Vasiliev, Sebastian Westermann, Jay P. Zarnetske, Tingjun Zhang, Mehran Ghandehari, Sarah Baeumler, Brian C. Brown, Rebecca J. Frei
ENVIRONMENTAL RESEARCH LETTERS
(2020)
Article
Geochemistry & Geophysics
B. A. Buffett
Summary: In this study, 3-D numerical calculations were used to assess the transition to turbulence in precessional flow, indicating that the transition to turbulence occurs near Re=500, higher than the typical value for stable Ekman layers. Complications due to fluid stratification or a magnetic field may suppress the transition to turbulence, reducing the likelihood of turbulent Ekman layers in the Earth's core.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2021)
Article
Geochemistry & Geophysics
William K. Eymold, Jennifer M. Frederick, Michael Nole, Benjamin J. Phrampus, Warren T. Wood
Summary: Methane hydrates are solid structures containing methane that form under low temperature and high pressure conditions. This study developed a workflow to predict methane hydrate occurrence using statistical and machine learning methods. Results suggest that elevated hydrate formation is associated with high seafloor total organic carbon values at depths greater than 500 meters below sea level near Blake Ridge.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2021)
Article
Geochemistry & Geophysics
Daniel A. Frost, Margaret S. Avery, Bruce A. Buffett, Bethany A. Chidester, Jie Deng, Susannah M. Dorfman, Zhi Li, Lijun Liu, Mingda Lv, Joshua F. Martin
Summary: In this study, an interdisciplinary analysis is used to co-constrain core-mantle boundary heat flow and test the thermal boundary layer theory. The seismic properties consistent with a thermal boundary layer are described, and support for the existence of a long-lived basal mantle molten layer through much of Earth's history is provided.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2022)
Article
Geochemistry & Geophysics
William Davis, Bruce Buffett
Summary: Recent studies have shown that time variations in the Earth's axial magnetic dipole field are influenced by both deterministic and random elements, with the slowest decay mode and turbulent diffusion playing key roles. The amplitude and timescale of variations in dipole field generation, including contributions from both velocity and internal magnetic field variations, also have a significant impact on the field's behavior. Applying these findings to the palaeomagnetic field suggests that reversal rates are highly sensitive to changes in the field generation process.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2022)
Article
Geosciences, Multidisciplinary
Rodrigo Chi-Duran, Margaret S. Avery, Bruce A. Buffett
Summary: The acceleration of Earth's magnetic field at high latitudes is attributed to waves in the core, with potential involvement of magnetic Rossby waves and zonal MAC waves. Observations suggest that these waves may propagate within a stratified layer at the top of the core, and the predicted stratification will lead to a slowing down and change in propagation direction of high-latitude features.
GEOPHYSICAL RESEARCH LETTERS
(2021)
Article
Geochemistry & Geophysics
B. A. Buffett, M. S. Avery, W. Davis
Summary: Observations of relative paleointensity reveal various asymmetries in the time dependence of the virtual axial dipole moment (VADM). Stochastic models are used to examine the origin of this behavior, and it is found that a model generating the dipole through a series of impulsive events in time can better explain the observed asymmetry.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2022)
Review
Environmental Sciences
Benjamin W. Abbott, Michael Brown, Joanna C. Carey, Jessica Ernakovich, Jennifer M. Frederick, Laodong Guo, Gustaf Hugelius, Raymond M. Lee, Michael M. Loranty, Robie Macdonald, Paul J. Mann, Susan M. Natali, David Olefeldt, Pam Pearson, Abigail Rec, Martin Robards, Verity G. Salmon, Sayedeh Sara Sayedi, Christina Schadel, Edward A. G. Schuur, Sarah Shakil, Arial J. Shogren, Jens Strauss, Suzanne E. Tank, Brett F. Thornton, Rachael Treharne, Merritt Turetsky, Carolina Voigt, Nancy Wright, Yuanhe Yang, Jay P. Zarnetske, Qiwen Zhang, Scott Zolkos
Summary: Climate change poses a threat to the global permafrost domain, and protecting permafrost ecosystems is crucial for human rights, biosphere integrity, and global climate. Strengthened emissions reduction targets and support for local communities are necessary to preserve intact ecological communities and carbon sinks within the permafrost domain.
FRONTIERS IN ENVIRONMENTAL SCIENCE
(2022)
Article
Geochemistry & Geophysics
D. Holdenried-Chernoff, B. A. Buffett
Summary: Fluctuations in the paleomagnetic field suggest that the dipole decay time is shorter than expected. The short decay time can be explained by turbulent diffusion, and mean-field theory can quantitatively account for the dynamo results. The predicted decay time depends on the amplitude and length scale of the flow that interacts with the magnetic field. By extending these predictions to the paleomagnetic field, it is found that the inferred decay time requires a bulk root-mean-square velocity less than 0.8-1.2 mm/s.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2022)
Article
Geochemistry & Geophysics
Quentin Nicolas, Bruce Buffett
Summary: Recent geomagnetic observations show localized oscillations in the field's secular acceleration at high latitudes with a period of about 20 years. This study examines the hypothesis that these observations are the result of MAC waves generated in Earth's core. By evaluating several generation mechanisms using dynamo simulations, the Lorentz force is found to be the most effective in producing high-latitude MAC waves with amplitudes consistent with observed oscillations.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2023)
Article
Geosciences, Multidisciplinary
Rodrigo Chi-Duran, Bruce A. Buffett
Summary: The rapid growth of magnetic-field observations through SWARM and other satellite missions has led to the development of new approaches for their analysis. The method of dynamic mode decomposition (DMD) is used in this study to analyze the geomagnetic radial field and its secular variation at high latitudes. The analysis reveals five modes, with one representing a slowly evolving background state and the other four describing a pair of waves. These waves have periods of approximately 19.1 and 58.4 years, and their characteristics are consistent with previous predictions and reports.
GEOPHYSICAL RESEARCH LETTERS
(2023)
Article
Physics, Multidisciplinary
Daria Holdenried-Chernoff, David A. King, Bruce A. Buffett
Summary: This paper introduces a stochastic fluid motion model for studying the generation of the geomagnetic field and obtains statistical properties similar to observations. This model helps to understand the long-term evolution of the geomagnetic field.
JOURNAL OF PHYSICS A-MATHEMATICAL AND THEORETICAL
(2023)
Article
Geosciences, Multidisciplinary
Matthias Morzfeld, Bruce A. Buffett
NONLINEAR PROCESSES IN GEOPHYSICS
(2019)