Materials Map

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (1/1 displayed)

  • 2023Environmental impact of solution pH on the formation and migration of iron colloids in deep subsurface energy systems.7citations

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Chart of shared publication
Bargar, John R.
1 / 3 shared
Kovscek, Anthony R.
1 / 2 shared
Frouté, Laura
1 / 1 shared
Noël, Vincent
1 / 2 shared
Bland, Garret
1 / 1 shared
Lowry, Gregory V.
1 / 3 shared
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2023

Co-Authors (by relevance)

  • Bargar, John R.
  • Kovscek, Anthony R.
  • Frouté, Laura
  • Noël, Vincent
  • Bland, Garret
  • Lowry, Gregory V.
OrganizationsLocationPeople

article

Environmental impact of solution pH on the formation and migration of iron colloids in deep subsurface energy systems.

  • Bargar, John R.
  • Kovscek, Anthony R.
  • Wielinski, Jonas
  • Frouté, Laura
  • Noël, Vincent
  • Bland, Garret
  • Lowry, Gregory V.
Abstract

Deep subsurface stimulation processes often promote fluid-rock interactions that can lead to the formation of small colloidal particles that are suspected to migrate through the rock matrix, partially or fully clog pores and microfractures, and promote the mobilization of contaminants. Thus, the goal of this work is to understand the geochemical changes of the host rock in response to reservoir stimulation that promote the formation and migration of colloids. Two different carbonate-rich shales were exposed to different solution pHs (pH = 2 and 7). Iron and other mineral transformations at the shale-fluid interface were first characterized by synchrotron-based XRF mapping. Then, colloids that were able to migrate from the shale into the bulk fluid were characterized by synchrotron-based extended X-ray absorption structure (EXAFS), scanning electron microscopy (SEM), and single-particle inductively coupled plasma time-of-flight mass spectrometry (sp-icpTOF-MS). When exposed to the pH = 2 solution, extensive mineral dissolution and secondary precipitation was observed; iron-(oxyhydr)oxide colloids colocated with silicates were observed by SEM at the fluid-shale interfaces, and the mobilization of chromium and nickel with these iron colloids into the bulk fluid was detected by sp-icpTOF-MS. Iron EXAFS spectra of the solution at the shale-fluid interface suggests the rapid (within minutes) formation of ferrihydrite-like nanoparticles. Thus, we demonstrate that the pH neutralization promotes the mobilization of existing silicate minerals and the rapid formation of new iron colloids. These Fe colloids have the potential to migrate through the shale matrix and mobilize other heavy metals (such as Cr and Ni, in this study) and impacting groundwater quality, as well produced waters from these hydraulic fracturing operations.

Topics
  • nanoparticle
  • impedance spectroscopy
  • pore
  • mineral
  • nickel
  • chromium
  • scanning electron microscopy
  • precipitation
  • iron
  • spectrometry
  • X-ray fluorescence spectroscopy
  • time-of-flight mass spectrometry
  • extended X-ray absorption fine structure spectroscopy