Suitability of Boulder Marl and Marsh Clay as Sealing Substrates for Landfill Capping Systems—A Practical Comparison
The effects of compaction on soil shrinkage behavior need to be considered for engineering long-term durable mineral liners of landfill capping systems. For this purpose, a new three-dimensional laser scanning device was coupled with a mathematical-empirical model to simultaneously determine the shr...
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doaj-2b5015709d1c4e2dab68957380f0ca462020-11-25T00:40:52ZengMDPI AGGeosciences2076-32632018-09-0181035610.3390/geosciences8100356geosciences8100356Suitability of Boulder Marl and Marsh Clay as Sealing Substrates for Landfill Capping Systems—A Practical ComparisonSteffen Beck-Broichsitter0Horst H. Gerke1Rainer Horn2Research Area 1 “Landscape Functioning”, Working Group “Hydropedology”, Leibniz-Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, GermanyResearch Area 1 “Landscape Functioning”, Working Group “Hydropedology”, Leibniz-Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, GermanyInstitute of Plant Nutrition and Soil Science, Christian Albrechts University Kiel, Christian-Albrechts-Platz 4, 24118 Kiel, GermanyThe effects of compaction on soil shrinkage behavior need to be considered for engineering long-term durable mineral liners of landfill capping systems. For this purpose, a new three-dimensional laser scanning device was coupled with a mathematical-empirical model to simultaneously determine the shrinkage behavior of a boulder marl (bm) and a marsh clay (mc). Therefore, both materials were precompacted in 200 soil cores (100 cm3) on the basis of the Proctor test results with five different degrees of compaction (bm1-bm5; mc1-mc5). Thus, the shrinkage behavior, intensity, and tendency were determined during a standardized drying experiment. The volume shrinkage index was used to describe the pore size dependent shrinkage tendency and was classified as high to very high (11.3–17.7%) for the marsh clay and medium (5.3–9.2%) for the boulder marl. Additionally, only the boulder marl (bm2), compacted up to 88% of Proctor density, could be installed as landfill bottom liner in drier locations if the local matric potentials did not exceed the previously highest observed drying range (i.e. values below −300 hPa), to avoid crack formation and generation.http://www.mdpi.com/2076-3263/8/10/356landfill capping systemsmineral linershrinkage intensity and tendency |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Steffen Beck-Broichsitter Horst H. Gerke Rainer Horn |
spellingShingle |
Steffen Beck-Broichsitter Horst H. Gerke Rainer Horn Suitability of Boulder Marl and Marsh Clay as Sealing Substrates for Landfill Capping Systems—A Practical Comparison Geosciences landfill capping systems mineral liner shrinkage intensity and tendency |
author_facet |
Steffen Beck-Broichsitter Horst H. Gerke Rainer Horn |
author_sort |
Steffen Beck-Broichsitter |
title |
Suitability of Boulder Marl and Marsh Clay as Sealing Substrates for Landfill Capping Systems—A Practical Comparison |
title_short |
Suitability of Boulder Marl and Marsh Clay as Sealing Substrates for Landfill Capping Systems—A Practical Comparison |
title_full |
Suitability of Boulder Marl and Marsh Clay as Sealing Substrates for Landfill Capping Systems—A Practical Comparison |
title_fullStr |
Suitability of Boulder Marl and Marsh Clay as Sealing Substrates for Landfill Capping Systems—A Practical Comparison |
title_full_unstemmed |
Suitability of Boulder Marl and Marsh Clay as Sealing Substrates for Landfill Capping Systems—A Practical Comparison |
title_sort |
suitability of boulder marl and marsh clay as sealing substrates for landfill capping systems—a practical comparison |
publisher |
MDPI AG |
series |
Geosciences |
issn |
2076-3263 |
publishDate |
2018-09-01 |
description |
The effects of compaction on soil shrinkage behavior need to be considered for engineering long-term durable mineral liners of landfill capping systems. For this purpose, a new three-dimensional laser scanning device was coupled with a mathematical-empirical model to simultaneously determine the shrinkage behavior of a boulder marl (bm) and a marsh clay (mc). Therefore, both materials were precompacted in 200 soil cores (100 cm3) on the basis of the Proctor test results with five different degrees of compaction (bm1-bm5; mc1-mc5). Thus, the shrinkage behavior, intensity, and tendency were determined during a standardized drying experiment. The volume shrinkage index was used to describe the pore size dependent shrinkage tendency and was classified as high to very high (11.3–17.7%) for the marsh clay and medium (5.3–9.2%) for the boulder marl. Additionally, only the boulder marl (bm2), compacted up to 88% of Proctor density, could be installed as landfill bottom liner in drier locations if the local matric potentials did not exceed the previously highest observed drying range (i.e. values below −300 hPa), to avoid crack formation and generation. |
topic |
landfill capping systems mineral liner shrinkage intensity and tendency |
url |
http://www.mdpi.com/2076-3263/8/10/356 |
work_keys_str_mv |
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