Some thmc controls on the evolution of fracture permeability

Research output: Chapter in Book/Report/Conference proceedingChapter

Abstract

The significant controls exerted on the evolution of fracture permeability by ambient conditions of stress, temperature, and chemical potential are illustrated for contrasting rock types. Natural and artificial fractures in Berea Sandstone, Arkansas Novaculite, and Bellefonte Limestone are confined within an x-ray transparent pressure cell and water flow-through tests conducted. The samples are monitored for change in permeability that evolves concurrently with the circulation of the water, and for net mineral efflux that accompanies this circulation. Periodic imaging by x-ray CT is used to define source areas of mineral efflux and its redistribution, and to provide constraint to phenomenological models that describe the observed behaviour. Vastly different behaviours are observed between the fractures present within the varied host materials - some gape with net mineral efflux, and some seal. These responses are viewed within the framework of the competition between mass mobilized by pressure solution, and net free-face dissolution or precipitation on the fracture walls, and in the matrix. Viewed in this context, the surprising range of behaviours, observed under similar THMC conditions in these three contrasting material types, may be unravelled.

Original languageEnglish (US)
Title of host publicationElsevier Geo-Engineering Book Series
PublisherElsevier Ltd
Pages63-71
Number of pages9
EditionC
DOIs
StatePublished - Jan 1 2004

Publication series

NameElsevier Geo-Engineering Book Series
NumberC
Volume2
ISSN (Print)1571-9960

Fingerprint

permeability
Minerals
mineral
X rays
pressure solution
Chemical potential
Sandstone
Limestone
Seals
Water
water flow
Dissolution
dissolution
Rocks
limestone
Imaging techniques
matrix
rock
temperature
water

All Science Journal Classification (ASJC) codes

  • Geotechnical Engineering and Engineering Geology

Cite this

Elsworth, D. (2004). Some thmc controls on the evolution of fracture permeability. In Elsevier Geo-Engineering Book Series (C ed., pp. 63-71). (Elsevier Geo-Engineering Book Series; Vol. 2, No. C). Elsevier Ltd. https://doi.org/10.1016/S1571-9960(04)80023-5
Elsworth, Derek. / Some thmc controls on the evolution of fracture permeability. Elsevier Geo-Engineering Book Series. C. ed. Elsevier Ltd, 2004. pp. 63-71 (Elsevier Geo-Engineering Book Series; C).
@inbook{15544929b1bc4123991670fb4dc6c610,
title = "Some thmc controls on the evolution of fracture permeability",
abstract = "The significant controls exerted on the evolution of fracture permeability by ambient conditions of stress, temperature, and chemical potential are illustrated for contrasting rock types. Natural and artificial fractures in Berea Sandstone, Arkansas Novaculite, and Bellefonte Limestone are confined within an x-ray transparent pressure cell and water flow-through tests conducted. The samples are monitored for change in permeability that evolves concurrently with the circulation of the water, and for net mineral efflux that accompanies this circulation. Periodic imaging by x-ray CT is used to define source areas of mineral efflux and its redistribution, and to provide constraint to phenomenological models that describe the observed behaviour. Vastly different behaviours are observed between the fractures present within the varied host materials - some gape with net mineral efflux, and some seal. These responses are viewed within the framework of the competition between mass mobilized by pressure solution, and net free-face dissolution or precipitation on the fracture walls, and in the matrix. Viewed in this context, the surprising range of behaviours, observed under similar THMC conditions in these three contrasting material types, may be unravelled.",
author = "Derek Elsworth",
year = "2004",
month = "1",
day = "1",
doi = "10.1016/S1571-9960(04)80023-5",
language = "English (US)",
series = "Elsevier Geo-Engineering Book Series",
publisher = "Elsevier Ltd",
number = "C",
pages = "63--71",
booktitle = "Elsevier Geo-Engineering Book Series",
address = "United Kingdom",
edition = "C",

}

Elsworth, D 2004, Some thmc controls on the evolution of fracture permeability. in Elsevier Geo-Engineering Book Series. C edn, Elsevier Geo-Engineering Book Series, no. C, vol. 2, Elsevier Ltd, pp. 63-71. https://doi.org/10.1016/S1571-9960(04)80023-5

Some thmc controls on the evolution of fracture permeability. / Elsworth, Derek.

Elsevier Geo-Engineering Book Series. C. ed. Elsevier Ltd, 2004. p. 63-71 (Elsevier Geo-Engineering Book Series; Vol. 2, No. C).

Research output: Chapter in Book/Report/Conference proceedingChapter

TY - CHAP

T1 - Some thmc controls on the evolution of fracture permeability

AU - Elsworth, Derek

PY - 2004/1/1

Y1 - 2004/1/1

N2 - The significant controls exerted on the evolution of fracture permeability by ambient conditions of stress, temperature, and chemical potential are illustrated for contrasting rock types. Natural and artificial fractures in Berea Sandstone, Arkansas Novaculite, and Bellefonte Limestone are confined within an x-ray transparent pressure cell and water flow-through tests conducted. The samples are monitored for change in permeability that evolves concurrently with the circulation of the water, and for net mineral efflux that accompanies this circulation. Periodic imaging by x-ray CT is used to define source areas of mineral efflux and its redistribution, and to provide constraint to phenomenological models that describe the observed behaviour. Vastly different behaviours are observed between the fractures present within the varied host materials - some gape with net mineral efflux, and some seal. These responses are viewed within the framework of the competition between mass mobilized by pressure solution, and net free-face dissolution or precipitation on the fracture walls, and in the matrix. Viewed in this context, the surprising range of behaviours, observed under similar THMC conditions in these three contrasting material types, may be unravelled.

AB - The significant controls exerted on the evolution of fracture permeability by ambient conditions of stress, temperature, and chemical potential are illustrated for contrasting rock types. Natural and artificial fractures in Berea Sandstone, Arkansas Novaculite, and Bellefonte Limestone are confined within an x-ray transparent pressure cell and water flow-through tests conducted. The samples are monitored for change in permeability that evolves concurrently with the circulation of the water, and for net mineral efflux that accompanies this circulation. Periodic imaging by x-ray CT is used to define source areas of mineral efflux and its redistribution, and to provide constraint to phenomenological models that describe the observed behaviour. Vastly different behaviours are observed between the fractures present within the varied host materials - some gape with net mineral efflux, and some seal. These responses are viewed within the framework of the competition between mass mobilized by pressure solution, and net free-face dissolution or precipitation on the fracture walls, and in the matrix. Viewed in this context, the surprising range of behaviours, observed under similar THMC conditions in these three contrasting material types, may be unravelled.

UR - http://www.scopus.com/inward/record.url?scp=77957031661&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=77957031661&partnerID=8YFLogxK

U2 - 10.1016/S1571-9960(04)80023-5

DO - 10.1016/S1571-9960(04)80023-5

M3 - Chapter

AN - SCOPUS:77957031661

T3 - Elsevier Geo-Engineering Book Series

SP - 63

EP - 71

BT - Elsevier Geo-Engineering Book Series

PB - Elsevier Ltd

ER -

Elsworth D. Some thmc controls on the evolution of fracture permeability. In Elsevier Geo-Engineering Book Series. C ed. Elsevier Ltd. 2004. p. 63-71. (Elsevier Geo-Engineering Book Series; C). https://doi.org/10.1016/S1571-9960(04)80023-5