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Título : | FEBEX-DP: Thermo-hydro-mechanical postmortem analysis of bentonite performed at CIEMAT. |
Autor : | Villar, María Victoria Iglesias, Rubén Javier Gutiérrez-Álvarez, Carlos Carbonell, Beatriz Campos, Rocío Campos, G. Martín, Pedro Luis Castro, Beatriz |
Palabras clave : | FEBEX-DP bentonite properties THM analyses buffer performance |
Fecha de publicación : | 1-mar-2021 |
Citación : | NAGRA technical report;NAB 16-24 |
Resumen : | This document collects the results obtained by CIEMAT referring to the THM characterisation
of the samples. Many of these results are also summarised and included in the synthesis report
collecting results of the bentonite characterisation obtained by all the project partners NAB-16-
017 (Villar 2018). The results concerning the mineralogical and geochemical characterisation
are reported in the NAB-16-025 (Fernández et al. 2018). The FEBEX project (Full-scale Engineered Barriers Experiment) studies the behaviour of
components in the near-field for a high-level radioactive waste (HLW) repository in crystalline
rock. The project was based on the Spanish reference concept for disposal of radioactive waste
in crystalline rock (AGP Granito): the waste canisters are placed horizontally in drifts and
surrounded by a clay barrier constructed from highly-compacted bentonite blocks (ENRESA
1995). As part of this project, an “in-situ” test, under natural conditions and at full scale, was
performed at the Grimsel Test Site (GTS, Switzerland), an underground laboratory managed by
NAGRA (ENRESA 2000, 2006). The thermal effect of the waste was simulated by means of
heaters, whereas hydration was natural. The test was monitored, thereby obtaining data on the
evolution of temperature, total pressure, water content, water pressure, displacements and other
parameters continuously, in different parts of the barrier and the host rock. This information is
then used to compare with the predictions of the thermo-hydro-mechanical (THM) and thermohydro-
geochemical (THG) models.
The basic components of the test (Fig. 1) were: the gallery, measuring 70 m in length and 2.3 m
in diameter, excavated through the Aare granite; the heating system, made up of two heaters
placed inside a liner installed concentrically with the gallery and separated from each other by a
1.0 m distance, with dimensions and weights analogous to those of the real canisters. The clay
barrier is formed by blocks of compacted bentonite; the instrumentation, the monitoring and
control system for data acquisition as well as supervision and control of the test both run
autonomously and remotely from Madrid. Up to 632 sensors of very diverse types were initially
installed for monitoring the different thermo-hydro-mechanical processes that occurred in both
the clay barrier and the surrounding rock throughout the entire life of the test. The gallery was
closed by a concrete plug.
The clay barrier consisted of FEBEX bentonite, which was extracted from the Cortijo de
Archidona deposit (Almería, Spain). The physico-chemical properties of the FEBEX bentonite,
as well as its most relevant thermo-hydro-mechanical and geochemical characteristics obtained
during the projects FEBEX I and II were summarised in the final reports of the project
(ENRESA 2000, 2006) and later documents (Villar & Gómez-Espina 2009). To build the clay
barrier, various types of blocks were manufactured from the bentonite in the shape of 12-cm
thick circular crown sectors. The blocks were arranged in vertical slices consisting of concentric
rings. In the heater areas the interior ring was in contact with the steel liner, whereas in the nonheater
areas a core of bentonite blocks replaced the heaters (Fig. 2). The geometry and
dimensions of the blocks are shown in Fig. 2, Fig. 3 and Tab. 1. The thickness of the bentonite
barrier in the heater areas was 65 cm (distance from liner to granite). The bentonite slices were
numbered from the back of the gallery towards the front, and those in which sensors were
installed were called “instrumented sections” and given a distinctive reference letter. The
backfilled area was sealed with a plain concrete plug placed into a recess excavated in the rock.
The blocks were obtained by uniaxial compaction of the FEBEX clay with its hygroscopic
water content at pressures between 40 and 45 MPa, resulting in dry densities of 1.69-1.70 g/cm3.
The initial dry density of the blocks was selected by taking into account the probable volume of
the construction gaps and the need to have a barrier with an average dry density of 1.60 g/cm3
(ENRESA 2000). |
URI : | http://documenta.ciemat.es/handle/123456789/1123 |
Aparece en las colecciones: | Informes de Medio Ambiente
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