### Abstract

Direct measurement of a permeability function, k(psi) (where psi = suction), of an unsaturated soil is often tedious and time-consuming. Thus, researchers have proposed various semiempirical predictive methods to determine k(psi) indirectly from a soil-water characteristic curve (SWCC) or a particle-size distribution. Also, stress effects on k(psi) are generally not considered. To explore any stress effect on k(psi), a new 1-m-high stress-controllable soil column is developed to measure stress-dependent SWCC (SDSWCC) and k(psi) of soils directly. The objectives of this paper are to investigate the effects of (1) two stress-state variables (matric suction and net normal stress) and (2) a drying-wetting cycle on both SDSWCC and k(psi) of a compacted decomposed silty clay. Each compacted soil column is subjected to an evaporation-ponding cycle under various vertical net normal stresses. The variations of pore-water pressure and volumetric water content (VWC, theta(w)) profiles with time are measured instantaneously. The k(psi) is hence determined by using the instantaneous profile method. At a given average vertical net normal stress, the measured k(psi) exhibits a remarkable hysteresis loop, whereas the k(theta(w)) seems to be less hysteretic. The effects of the vertical net normal stress appear to be more pronounced than that of the drying-wetting cycle on k(theta(w)). As average vertical net normal stress is increased from 4 to 78 kPa, the measured permeability decreases by up to two orders of magnitude at a given VWC. DOI: 10.1061/(ASCE)GT.1943-5606.0000560. (C) 2012 American Society of Civil Engineers.

Original language | English |
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Pages (from-to) | 58-68 |

Number of pages | 11 |

Journal | Journal of Geotechnical and Geoenvironmental Engineering |

Volume | 138 |

Issue number | 1 |

DOIs | |

Publication status | Published - Jan 2012 |

### Cite this

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**Measurements of drying and wetting permeability functions using a new stress-controllable soil column.** / Ng, C. W. W.; Leung, A. K.

Research output: Contribution to journal › Article

TY - JOUR

T1 - Measurements of drying and wetting permeability functions using a new stress-controllable soil column

AU - Ng, C. W. W.

AU - Leung, A. K.

PY - 2012/1

Y1 - 2012/1

N2 - Direct measurement of a permeability function, k(psi) (where psi = suction), of an unsaturated soil is often tedious and time-consuming. Thus, researchers have proposed various semiempirical predictive methods to determine k(psi) indirectly from a soil-water characteristic curve (SWCC) or a particle-size distribution. Also, stress effects on k(psi) are generally not considered. To explore any stress effect on k(psi), a new 1-m-high stress-controllable soil column is developed to measure stress-dependent SWCC (SDSWCC) and k(psi) of soils directly. The objectives of this paper are to investigate the effects of (1) two stress-state variables (matric suction and net normal stress) and (2) a drying-wetting cycle on both SDSWCC and k(psi) of a compacted decomposed silty clay. Each compacted soil column is subjected to an evaporation-ponding cycle under various vertical net normal stresses. The variations of pore-water pressure and volumetric water content (VWC, theta(w)) profiles with time are measured instantaneously. The k(psi) is hence determined by using the instantaneous profile method. At a given average vertical net normal stress, the measured k(psi) exhibits a remarkable hysteresis loop, whereas the k(theta(w)) seems to be less hysteretic. The effects of the vertical net normal stress appear to be more pronounced than that of the drying-wetting cycle on k(theta(w)). As average vertical net normal stress is increased from 4 to 78 kPa, the measured permeability decreases by up to two orders of magnitude at a given VWC. DOI: 10.1061/(ASCE)GT.1943-5606.0000560. (C) 2012 American Society of Civil Engineers.

AB - Direct measurement of a permeability function, k(psi) (where psi = suction), of an unsaturated soil is often tedious and time-consuming. Thus, researchers have proposed various semiempirical predictive methods to determine k(psi) indirectly from a soil-water characteristic curve (SWCC) or a particle-size distribution. Also, stress effects on k(psi) are generally not considered. To explore any stress effect on k(psi), a new 1-m-high stress-controllable soil column is developed to measure stress-dependent SWCC (SDSWCC) and k(psi) of soils directly. The objectives of this paper are to investigate the effects of (1) two stress-state variables (matric suction and net normal stress) and (2) a drying-wetting cycle on both SDSWCC and k(psi) of a compacted decomposed silty clay. Each compacted soil column is subjected to an evaporation-ponding cycle under various vertical net normal stresses. The variations of pore-water pressure and volumetric water content (VWC, theta(w)) profiles with time are measured instantaneously. The k(psi) is hence determined by using the instantaneous profile method. At a given average vertical net normal stress, the measured k(psi) exhibits a remarkable hysteresis loop, whereas the k(theta(w)) seems to be less hysteretic. The effects of the vertical net normal stress appear to be more pronounced than that of the drying-wetting cycle on k(theta(w)). As average vertical net normal stress is increased from 4 to 78 kPa, the measured permeability decreases by up to two orders of magnitude at a given VWC. DOI: 10.1061/(ASCE)GT.1943-5606.0000560. (C) 2012 American Society of Civil Engineers.

U2 - 10.1061/(ASCE)GT.1943-5606.0000560

DO - 10.1061/(ASCE)GT.1943-5606.0000560

M3 - Article

VL - 138

SP - 58

EP - 68

JO - Journal of Geotechnical and Geoenvironmental Engineering

JF - Journal of Geotechnical and Geoenvironmental Engineering

SN - 1090-0241

IS - 1

ER -