Anisotropic thermal conductivity of natural Boom Clay

Research output: Contribution to journalArticlepeer-review

Standard

Anisotropic thermal conductivity of natural Boom Clay. / Dao, Linh-Quyen; Delage, Pierre; Tang, Anh-Minh; Cui, Yu-Jun; Pereira, Jean-Michel; Li, Xiang Ling; Sillen, Xavier; Chen, Guangjing (Peer reviewer).

In: Applied Clay Science, Vol. 101, No. 11, 11.2014, p. 282-287.

Research output: Contribution to journalArticlepeer-review

Harvard

Dao, L-Q, Delage, P, Tang, A-M, Cui, Y-J, Pereira, J-M, Li, XL, Sillen, X & Chen, G 2014, 'Anisotropic thermal conductivity of natural Boom Clay', Applied Clay Science, vol. 101, no. 11, pp. 282-287. https://doi.org/10.1016/j.clay.2014.09.003

APA

Dao, L-Q., Delage, P., Tang, A-M., Cui, Y-J., Pereira, J-M., Li, X. L., Sillen, X., & Chen, G. (2014). Anisotropic thermal conductivity of natural Boom Clay. Applied Clay Science, 101(11), 282-287. https://doi.org/10.1016/j.clay.2014.09.003

Vancouver

Dao L-Q, Delage P, Tang A-M, Cui Y-J, Pereira J-M, Li XL et al. Anisotropic thermal conductivity of natural Boom Clay. Applied Clay Science. 2014 Nov;101(11):282-287. https://doi.org/10.1016/j.clay.2014.09.003

Author

Dao, Linh-Quyen ; Delage, Pierre ; Tang, Anh-Minh ; Cui, Yu-Jun ; Pereira, Jean-Michel ; Li, Xiang Ling ; Sillen, Xavier ; Chen, Guangjing. / Anisotropic thermal conductivity of natural Boom Clay. In: Applied Clay Science. 2014 ; Vol. 101, No. 11. pp. 282-287.

Bibtex - Download

@article{dc1af9f36f1344b9a34bacf07cddb272,
title = "Anisotropic thermal conductivity of natural Boom Clay",
abstract = "The thermal conductivity of host rocks is an important parameter in the design of deep geological disposal of heat-emitting radioactivewaste. Due to bedding, heat transfer in sedimentary rocks is affectedbytheir transversally isotropic structure. In this work, an experimental program is run to measure the thermal conductivities of Boom Clay along various orientations with respect to the bedding plane by using the needle thermal probe technique. Measurements were performed on specimens obtained from cores drilled fromthe HADES Underground Research Laboratory (URL) at Mol, Belgium, at a depth of 223 m. The thermal conductivity values obtained are in good agreement with those previously published, confirming the thermal anisotropy of Boom Clay. Moreover, the observed changes in thermal conductivity with respect to the distance to the gallery provide further evidence on the extent of the Excavation Damaged Zone around the gallery.",
keywords = "Thermal conductivity, Boom Clay, thermal anisotropy, Excavation Damaged Zone, laboratory test",
author = "Linh-Quyen Dao and Pierre Delage and Anh-Minh Tang and Yu-Jun Cui and Jean-Michel Pereira and Li, {Xiang Ling} and Xavier Sillen and Guangjing Chen",
note = "Score = 10",
year = "2014",
month = nov,
doi = "10.1016/j.clay.2014.09.003",
language = "English",
volume = "101",
pages = "282--287",
journal = "Applied Clay Science",
issn = "0169-1317",
publisher = "Elsevier",
number = "11",

}

RIS - Download

TY - JOUR

T1 - Anisotropic thermal conductivity of natural Boom Clay

AU - Dao, Linh-Quyen

AU - Delage, Pierre

AU - Tang, Anh-Minh

AU - Cui, Yu-Jun

AU - Pereira, Jean-Michel

AU - Li, Xiang Ling

AU - Sillen, Xavier

A2 - Chen, Guangjing

N1 - Score = 10

PY - 2014/11

Y1 - 2014/11

N2 - The thermal conductivity of host rocks is an important parameter in the design of deep geological disposal of heat-emitting radioactivewaste. Due to bedding, heat transfer in sedimentary rocks is affectedbytheir transversally isotropic structure. In this work, an experimental program is run to measure the thermal conductivities of Boom Clay along various orientations with respect to the bedding plane by using the needle thermal probe technique. Measurements were performed on specimens obtained from cores drilled fromthe HADES Underground Research Laboratory (URL) at Mol, Belgium, at a depth of 223 m. The thermal conductivity values obtained are in good agreement with those previously published, confirming the thermal anisotropy of Boom Clay. Moreover, the observed changes in thermal conductivity with respect to the distance to the gallery provide further evidence on the extent of the Excavation Damaged Zone around the gallery.

AB - The thermal conductivity of host rocks is an important parameter in the design of deep geological disposal of heat-emitting radioactivewaste. Due to bedding, heat transfer in sedimentary rocks is affectedbytheir transversally isotropic structure. In this work, an experimental program is run to measure the thermal conductivities of Boom Clay along various orientations with respect to the bedding plane by using the needle thermal probe technique. Measurements were performed on specimens obtained from cores drilled fromthe HADES Underground Research Laboratory (URL) at Mol, Belgium, at a depth of 223 m. The thermal conductivity values obtained are in good agreement with those previously published, confirming the thermal anisotropy of Boom Clay. Moreover, the observed changes in thermal conductivity with respect to the distance to the gallery provide further evidence on the extent of the Excavation Damaged Zone around the gallery.

KW - Thermal conductivity

KW - Boom Clay

KW - thermal anisotropy

KW - Excavation Damaged Zone

KW - laboratory test

UR - http://ecm.sckcen.be/OTCS/llisapi.dll/open/ezp_137118

UR - http://knowledgecentre.sckcen.be/so2/bibref/11879

U2 - 10.1016/j.clay.2014.09.003

DO - 10.1016/j.clay.2014.09.003

M3 - Article

VL - 101

SP - 282

EP - 287

JO - Applied Clay Science

JF - Applied Clay Science

SN - 0169-1317

IS - 11

ER -

ID: 269423