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DOI10.1073/pnas.2003451117
Seismic refraction tracks porosity generation and possible CO2 production at depth under a headwater catchment
Gu X.; Mavko G.; Ma L.; Oakley D.; Accardo N.; Carr B.J.; Nyblade A.A.; Brantley S.L.
发表日期2020
ISSN0027-8424
起始页码18991
结束页码18997
卷号117期号:32
英文摘要In weathered bedrock aquifers, groundwater is stored in pores and fractures that open as rocks are exhumed and minerals interact with meteoric fluids. Little is known about this storage because geochemical and geophysical observations are limited to pits, boreholes, or outcrops or to inferences based on indirect measurements between these sites. We trained a rock physics model to borehole observations in a well-constrained ridge and valley landscape and then interpreted spatial variations in seismic refraction velocities. We discovered that P-wave velocities track where a porosity-generating reaction initiates in shale in three boreholes across the landscape. Specifically, velocities of 2.7 ± 0.2 km/s correspond with growth of porosity from dissolution of chlorite, the most reactive of the abundant minerals in the shale. In addition, sonic velocities are consistent with the presence of gas bubbles beneath the water table under valley and ridge. We attribute this gas largely to CO2 produced by 1) microbial respiration in soils as meteoric waters recharge into the subsurface and 2) the coupled carbonate dissolution and pyrite oxidation at depth in the rock. Bubbles may nucleate below the water table because waters depressurize as they flow from ridge to valley and because pores have dilated as the deep rock has been exhumed by erosion. Many of these observations are likely to also describe the weathering and flow path patterns in other headwater landscapes. Such combined geophysical and geochemical observations will help constrain models predicting flow, storage, and reaction of groundwater in bedrock systems. © 2020 National Academy of Sciences. All rights reserved.
语种英语
scopus关键词carbon dioxide; carbonic acid; chlorite; ground water; mineral; pyrite; unclassified drug; Article; catchment area (hydrology); controlled study; dissolution; flow; gas; microbial respiration; oxidation; physical parameters; porosity; priority journal; rock; seismic refraction; soil; soil erosion; storage; surface property; velocity; weathering
来源期刊Proceedings of the National Academy of Sciences of the United States of America
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/160849
作者单位Gu, X., Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States, Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802, United States; Mavko, G., Stanford Rock Physics Laboratory, Stanford University, Palo Alto, CA 94305, United States; Ma, L., Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States; Oakley, D., Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802, United States; Accardo, N., Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States; Carr, B.J., Department of Geology and Geophysics, University of Wyoming, Laramie, WY 82071, United States; Nyblade, A.A., Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States; Brantley, S.L., Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States...
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Gu X.,Mavko G.,Ma L.,et al. Seismic refraction tracks porosity generation and possible CO2 production at depth under a headwater catchment[J],2020,117(32).
APA Gu X..,Mavko G..,Ma L..,Oakley D..,Accardo N..,...&Brantley S.L..(2020).Seismic refraction tracks porosity generation and possible CO2 production at depth under a headwater catchment.Proceedings of the National Academy of Sciences of the United States of America,117(32).
MLA Gu X.,et al."Seismic refraction tracks porosity generation and possible CO2 production at depth under a headwater catchment".Proceedings of the National Academy of Sciences of the United States of America 117.32(2020).
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