Featured
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Article |
Fluid migration in low-permeability faults driven by decoupling of fault slip and opening
Decoupled fault slip and opening, leading to rapid fluid pressurization after initial failure, drives high-pressure fluid migration in low-permeability faults, according to modelling and in situ observations from a borehole fluid-injection experiment.
- Frédéric Cappa
- , Yves Guglielmi
- & Jens Birkholzer
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Article |
Sedimentary basins reduce stability of Antarctic ice streams through groundwater feedbacks
A machine-learning-based mapping of Antarctic subglacial geology suggests sedimentary basins lie beneath some of the most dynamic ice streams, increasing their vulnerability to rapid ice retreat.
- Lu Li
- , Alan R. A. Aitken
- & Bernd Kulessa
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Perspective |
Confronting the water potential information gap
Continuous and discoverable observations of water potential could vastly improve understanding of biophysical processes throughout the soil–plant–atmosphere continuum and are achievable thanks to recent technological advances.
- Kimberly A. Novick
- , Darren L. Ficklin
- & Jeffrey D. Wood
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Article |
Tributary channel networks formed by depositional processes
Drainage divides between coastal plain channel networks can be constructed through depositional, rather than erosional, processes according to a lidar-based topographic analysis of the Gulf of Mexico coastal plain.
- John M. Swartz
- , Benjamin T. Cardenas
- & Paola Passalacqua
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Article |
Rapid and sensitive response of Greenland’s groundwater system to ice sheet change
Greenland’s groundwater system responds rapidly to ice-sheet change, according to borehole observations from underneath the ice-sheet margin.
- Lillemor Claesson Liljedahl
- , Toby Meierbachtol
- & Neil Humphrey
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News & Views |
Irrigation and the Palu landslides
Wet rice cultivation in the Palu Valley, Indonesia, prepared the ground for the devastating liquefaction-induced landslides that were triggered by the Mw 7.5 earthquake in 2018, suggest two studies of the spatial relationship between landslide morphology and irrigation.
- Phil R. Cummins
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Article |
Hydrogeological constraints on the formation of Palaeoproterozoic banded iron formations
Banded iron formations could not have formed by postdepositional oxidation, according to four million hydrogeological box model iterations that failed to reproduce secondary oxidation on reasonable timescales.
- Leslie J. Robbins
- , Sean P. Funk
- & Kurt O. Konhauser
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News & Views |
Training machines in Earthly ways
Geoscientists are training computers to learn from a wide range of geologic data and, in the process, the machines are teaching geoscientists about the workings of Earth.
- Chris Marone
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Article |
Dry Juan de Fuca slab revealed by quantification of water entering Cascadia subduction zone
The Juan de Fuca plate, which subducts below the Cascades, is remarkably dry, according to reconstructions of water content based on seismic data. Decompression rather than hydrous melting must therefore be responsible for Cascades volcanism.
- J. P. Canales
- , S. M. Carbotte
- & H. Carton
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Article |
Fluid-driven metamorphism of the continental crust governed by nanoscale fluid flow
Fluid flow in Earth’s crust redistributes minerals. Nanoscale imaging and molecular dynamics simulations suggest this flow is controlled by electrokinetic transport phenomena, highlighting the importance of nanoscale processes in metamorphism.
- Oliver Plümper
- , Alexandru Botan
- & Bjørn Jamtveit
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Commentary |
Beyond the water balance
The terrestrial water cycle is often assessed annually at catchment scale. But water stored in catchments is poorly mixed, and at timescales often well beyond the calculation of annual water balance.
- Jeffrey J. McDonnell
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Article |
Global aquifers dominated by fossil groundwaters but wells vulnerable to modern contamination
Groundwater that predates the Holocene is commonly assumed to be unaffected by modern contamination. A global analysis of fossil groundwater suggests that modern contaminants are present in deep wells that tap fossil aquifers.
- Scott Jasechko
- , Debra Perrone
- & James W. Kirchner
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Article |
Mobility and persistence of methane in groundwater in a controlled-release field experiment
Most monitoring of methane well leakage focuses on emissions of methane gas to the atmosphere. In a controlled-release field experiment, significant methane also persisted in aquifer groundwater due to lateral migration along bedding planes.
- Aaron G. Cahill
- , Colby M. Steelman
- & Beth L. Parker
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Article |
Potentially exploitable supercritical geothermal resources in the ductile crust
The brittle–ductile transition is thought to control crustal permeability. Laboratory experiments and model simulations show that permeability is also stress dependent and ductile granitic rocks may have enough permeability to host geothermal resources.
- Noriaki Watanabe
- , Tatsuya Numakura
- & Noriyoshi Tsuchiya
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News & Views |
Indo-Gangetic groundwater threat
Increasing groundwater extraction supports hundreds of millions of people across the Indo-Gangetic Basin. Data suggests that despite the increase in withdrawals, groundwater depletion is localized and the most widespread threat is contamination.
- Scott Fendorf
- & Shawn G. Benner
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Letter |
Fault-controlled hydration of the upper mantle during continental rifting
The mechanisms for mantle hydration are unclear. Seismic images offshore from Spain reveal a correlation between the amount of seawater-altered rocks and the extent of fault slip, suggesting that faults control water flux into the Earth.
- G. Bayrakci
- , T. A. Minshull
- & J. K. Morgan
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Letter |
Gold enrichment in active geothermal systems by accumulating colloidal suspensions
How gold ore deposits form in the absence of a magmatic source for gold is unclear. Analysis of hydrothermal fluids from the Reykjanes geothermal field reveals that gold can become trapped as a colloidal suspension and accumulate over time.
- Mark Hannington
- , Vigdis Harðardóttir
- & Kevin L. Brown
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Editorial |
Groundwater exposed
Groundwater flow meddles with hydrological, environmental and geological processes. As water scarcity issues mount for people living above ground, the vast stores of freshwater in the subsurface require research attention.
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Commentary |
Drought in the Anthropocene
Drought management is inefficient because feedbacks between drought and people are not fully understood. In this human-influenced era, we need to rethink the concept of drought to include the human role in mitigating and enhancing drought.
- Anne F. Van Loon
- , Tom Gleeson
- & Henny A. J. Van Lanen
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Letter |
Groundwater flow as a cooling agent of the continental lithosphere
Groundwater flow redistributes heat in the Earth’s crust. Numerical simulations of groundwater flow show net cooling of groundwater basins, as well as cooling of the underlying lithosphere in areas where groundwater flows over large distances.
- Henk Kooi
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Letter |
Substantial proportion of global streamflow less than three months old
Streamflow is a mixture of precipitation of various ages. Oxygen isotope data suggests that a third of global river discharge is sourced from rainfall within the past few months, which accounts for less than 0.1% of global groundwater.
- Scott Jasechko
- , James W. Kirchner
- & Jeffrey J. McDonnell
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News & Views |
How much and how old?
A global picture of the age structure and flow path of groundwater is lacking. Tritium concentrations and numerical modelling shed light on both the most recently replenished and the longest stored groundwater within Earth's continents.
- Ying Fan
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Article |
The global volume and distribution of modern groundwater
Groundwater recharged less than 50 years ago is vulnerable to contamination and land-use changes. Data and simulations suggest that up to 6% of continental groundwater is modern—forming the largest component of the active hydrologic cycle.
- Tom Gleeson
- , Kevin M. Befus
- & M. Bayani Cardenas
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Correspondence |
Initiation of the Lusi mudflow disaster
- M. R. P. Tingay
- , M. L. Rudolph
- & Chi-Yuen Wang
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Letter |
Stable runoff and weathering fluxes into the oceans over Quaternary climate cycles
The effect of glacial–interglacial cycles on surface weathering rates has been unclear. A beryllium-based proxy for weathering shows minimal variations in the input of silicate weathering products to the oceans for the past two million years.
- Friedhelm von Blanckenburg
- , Julien Bouchez
- & Kate Maher
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Letter |
Continental degassing of 4He by surficial discharge of deep groundwater
Helium-4 is produced in the Earth’s crust and degassed to the atmosphere. Measurements of 4He and 81Kr dating in an aquifer in Brazil suggest that most crustal 4He reaches the atmosphere by the discharge of deep groundwater at the surface.
- Pradeep K. Aggarwal
- , Takuya Matsumoto
- & Thomas Torgersen
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News & Views |
Hydrogeochemical precursors
Earthquake prediction is a long-sought goal. Changes in groundwater chemistry before earthquakes in Iceland highlight a potential hydrogeochemical precursor, but such signals must be evaluated in the context of long-term, multiparametric data sets.
- S. E. Ingebritsen
- & M. Manga
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Letter |
Changes in groundwater chemistry before two consecutive earthquakes in Iceland
Precursor events to earthquakes are rarely reproduced. Measurement of groundwater chemistry in Iceland between 2008 and 2013 reveals distinct changes prior to two consecutive >M5 earthquakes.
- Alasdair Skelton
- , Margareta Andrén
- & Ingrid Kockum
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Letter |
Seismic precursors linked to highly compressible fluids at oceanic transform faults
Earthquakes on oceanic transform faults are often preceded by foreshock swarms. A theoretical model suggests that circulating hydrothermal fluids, which compress as the fault rocks expand and deform, cause this precursor seismic activity.
- Louis Géli
- , Jean-Michel Piau
- & Thomas Driesner
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Letter |
Sandstone landforms shaped by negative feedback between stress and erosion
The formation and preservation of sandstone landforms such as pillars and arches is enigmatic. Experiments and numerical modelling show that load-bearing material weathers more slowly, and thus the internal stress field can shape and stabilize sandstone landforms.
- Jiri Bruthans
- , Jan Soukup
- & Jaroslav Rihosek
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Commentary |
Missing a trick in geothermal exploration
Expansion of geothermal energy use across the globe is restricted by out-of-date prejudices. It is time for geothermal exploration to be extended to a broader range of environments and rejuvenated with the latest insights from relevant geoscience disciplines.
- Paul L. Younger
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Article |
Groundwater activity on Mars and implications for a deep biosphere
The subsurface of Mars could potentially have contained a vast microbial biosphere. An evaluation of the possibility of groundwater upwelling, which might provide clues to subsurface habitability, reveals evidence in the deep McLaughlin crater for clays and carbonates that probably formed in an alkaline, groundwater-fed lacustrine setting.
- Joseph R. Michalski
- , Javier Cuadros
- & Shawn P. Wright
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Correspondence |
Reply to 'Overestimated water storage'
- Yadu N. Pokhrel
- , Naota Hanasaki
- & Taikan Oki
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Commentary |
Asia's water balance
Multiple factors determine how much water is and will be available in the river basins of Asia. To expose hotspots and help adaptation, these factors must be assessed together at the basin level.
- W. W. Immerzeel
- & M. F. P. Bierkens
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Review Article |
Regional strategies for the accelerating global problem of groundwater depletion
The world's largest freshwater resource is groundwater. A review of our understanding of groundwater depletion suggests that although the problem is global, solutions must be adapted to specific regional requirements at the aquifer scale.
- Werner Aeschbach-Hertig
- & Tom Gleeson
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News & Views |
Human-induced shaking
In 2011, a modest earthquake in southern Spain seriously damaged the city of Lorca. Analysis of surface deformation suggests that the quake was caused by rupture of a shallow fault patch brought closer to failure by the pumping of water from a nearby aquifer.
- Jean-Philippe Avouac
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Letter |
The 2011 Lorca earthquake slip distribution controlled by groundwater crustal unloading
Earthquake rupture is influenced by stress conditions in the crust before the quake. Analysis and modelling of surface deformation caused by the May 2011 earthquake in Lorca, Spain, indicate that groundwater extraction influenced the pattern of fault rupture.
- Pablo J. González
- , Kristy F. Tiampo
- & José Fernández
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Article |
Groundwater arsenic concentrations in Vietnam controlled by sediment age
Arsenic contamination of groundwater threatens the health of millions of people in southeast Asia. Measurements in an arsenic-contaminated aquifer in Vietnam point to sediment age as a key determinant of groundwater arsenic concentrations.
- Dieke Postma
- , Flemming Larsen
- & Andrew S. Murray
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Letter |
Mitigating land loss in coastal Louisiana by controlled diversion of Mississippi River sand
The Bonnet Carré Spillway diverts floodwaters from the Mississippi River to Lake Pontchartrain, and was opened for 42 days during the 2011 flood. According to measurements of the newly deposited sediments, at least 31–46% of the river’s sand load was diverted into the spillway at this time, suggesting that such diversions can help mitigate coastal wetland loss.
- Jeffrey A. Nittrouer
- , James L. Best
- & Gary Parker
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Letter |
Model estimates of sea-level change due to anthropogenic impacts on terrestrial water storage
Changes in terrestrial water storage are likely to affect sea level, but comprehensive and reliable data are scarce. Simulations of global terrestrial water stocks and flows, with an integrated model that specifically accounts for human activities, indicate that groundwater depletion and reservoir storage have together led to a sea-level rise of about 0.66 mm yr−1 between 1961 and 2003, about 36% of the observed rise.
- Yadu N. Pokhrel
- , Naota Hanasaki
- & Taikan Oki
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Article |
Pulses of carbon dioxide emissions from intracrustal faults following climatic warming
Carbon capture and geological storage represents a potential means of managing atmospheric carbon dioxide levels. An analysis of a 135,000 palaeorecord shows that pulses of carbon dioxide leakage from a natural reservoir in Utah are associated with episodes of glacial unloading.
- Niko Kampman
- , Neil M. Burnside
- & Mike J. Bickle
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Letter |
Western Arctic Ocean freshwater storage increased by wind-driven spin-up of the Beaufort Gyre
An increasing amount of freshwater has been stored in the Arctic Ocean over the past few decades. Satellite measurements of sea surface height reveal a spin-up of the Beaufort Gyre in the western Arctic that is associated with changes in the wind field, and is estimated to have led to the additional storage of about 8,000 km3 of freshwater.
- Katharine A. Giles
- , Seymour W. Laxon
- & Sheldon Bacon