Abstract

Municipal solid waste (MSW) compressibility is normally a challenging task to study because it is affected by several parameters that are not easy to simulate in the laboratory. Here, a large-scale oedometer was developed to evaluate the compressibility of MSW, which can apply different levels of temperature to the specimens. In real MSW landfills, the anaerobic decomposition reactions act as a thermal source, raising MSW temperatures. Due to the nonstandard height-to-diameter ratio, the mobilized inner wall friction was investigated and stress distribution in the MSW specimen was corrected. Then, a series of compressibility tests on fresh MSW were performed at 25°C, 45°C, and 65°C, and the horizontal and vertical permeabilities of MSW at each loading stage were measured. The results showed that MSW softened and the compression indices increased with increasing temperature. This softening in MSW and particles led to a decrease in MSW permeability.

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Acknowledgments

The authors thank the Geotechnical Laboratory of Iran University of Science and Technology (IUST). The authors are also grateful to Nader Shariatmadari, Zeraati, and Azarbara for their assistance.

Notation

The following symbols are used in this paper:
A
area of the cross section (m2);
An
anisotropy of permeability (dimensionless);
Cc
compression index (dimensionless);
Cc
modified compression index (dimensionless);
Cr
modified unloading index (dimensionless);
Cα
=coefficient of creep compression (dimensionless);
Cα
modified coefficient of creep compression (dimensionless);
c
geomaterial cohesion (kPa);
D
inner cell diameter (mm);
fi
interfacial friction at the ith layer of geomaterial (kPa);
Gs
geomaterial-specific gravity (dimensionless);
H0
sample height (m);
i
hydraulic gradient (dimensionless);
K0
coefficient of at-rest lateral earth pressure (dimensionless);
kx
horizontal permeability coefficient (cm/s);
ky
vertical permeability coefficient (cm/s);
q
applied pressure (kPa);
t
time (min);
V
quantity of water (mL);
z
depth in the geomaterial sample (cm);
β
Bjerrum–Burland coefficient (dimensionless);
ΔH0
variation in the sample height (m);
ΔlogP
variation in normal effective stress (dimensionless);
Δlogt
variation in time (dimensionless);
Δɛ
variation in strain (dimensionless);
δ
interface friction angle (°);
γ
unit weight of the geomaterial (kN/m3);
σb
vertical stress at the bottom of the sample (kPa);
σt
vertical stress at the top of the sample (kPa);
σz
normal stress at depth z (kPa);
φ
geomaterial internal friction angle (°); and
ω
geomaterial moisture content (%).

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 23Issue 3March 2023

History

Received: May 9, 2022
Accepted: Sep 27, 2022
Published online: Dec 26, 2022
Published in print: Mar 1, 2023
Discussion open until: May 26, 2023

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Ph.D. Student, School of Civil Engineering, Iran Univ. of Science and Technology, Narmak, Tehran 16846-13114, Iran. ORCID: https://orcid.org/0000-0003-2090-1968. Email: [email protected]
Assistant Professor, School of Civil Engineering, Iran Univ. of Science and Technology, Narmak, Tehran 16846-13114, Iran (corresponding author). ORCID: https://orcid.org/0000-0001-5313-6444. Email: [email protected]
Ali Akbar Heshmati [email protected]
Assistant Professor, School of Civil Engineering, Iran Univ. of Science and Technology, Narmak, Tehran 16846-13114, Iran. Email: [email protected]
Professor, Dept. of Materials Science and Technology, Federal Univ. of Bahia, 02 Aristides Novis St., Salvador, BA 40210-630, Brazil. ORCID: https://orcid.org/0000-0001-6656-1116. Email: [email protected]

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