Cross-hole tracer experiment reveals rapid fluid flow and low effective porosity in the upper oceanic crust

N. M. Neira, J. F. Clark, A. T. Fisher, C. G. Wheat, R. M. Haymon, K. Becker

Research output: Contribution to journalArticle

14 Scopus citations

Abstract

Numerous field, laboratory, and modeling studies have explored the flows of fluid, heat, and solutes during seafloor hydrothermal circulation, but it has been challenging to determine transport rates and flow directions within natural systems. Here we present results from the first cross-hole tracer experiment in the upper oceanic crust, using four subseafloor borehole observatories equipped with autonomous samplers to track the transport of a dissolved tracer (sulfur hexafluoride, SF6) injected into a ridge-flank hydrothermal system. During the first three years after tracer injection, SF6 was transported both north and south through the basaltic aquifer. The observed tracer transport rate of ∼2–3 m/day is orders of magnitude greater than bulk rates of flow inferred from thermal and chemical observations and calculated with coupled fluid-heat flow simulations. Taken together, these results suggest that the effective porosity of the upper volcanic crust through which much tracer was transported is <1%, with fluid flowing rapidly along a few well-connected channels. This is consistent with the heterogeneous (layered, faulted, and/or fractured) nature of the volcanic upper oceanic crust.

Original languageEnglish (US)
Pages (from-to)355-365
Number of pages11
JournalEarth and Planetary Science Letters
Volume450
DOIs
StatePublished - Sep 15 2016

Keywords

  • Juan de Fuca Ridge flank
  • abyssal hills
  • borehole observatory
  • hydrothermal circulation
  • ocean crustal properties
  • tracer injection experiment

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Fingerprint Dive into the research topics of 'Cross-hole tracer experiment reveals rapid fluid flow and low effective porosity in the upper oceanic crust'. Together they form a unique fingerprint.

  • Cite this