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Why pile-supported building settled continuously after water level was stabilized during dewatering: Clues from interaction between pile and multi aquifers.

Authors :
Xue, Xiu-Li
Sun, Hai-Yu
Zeng, Chao-Feng
Chen, Hong-Bo
Zheng, Gang
Xu, Chang-Jie
Han, Lei
Source :
Journal of Hydrology. Jul2024, Vol. 638, pN.PAG-N.PAG. 1p.
Publication Year :
2024

Abstract

[Display omitted] • Pumping test is conducted to study the building settlement during pit dewatering. • Building settlement is observed lagging behind the water level decline. • We reveal the reasons for the lagging settlement based on numerical analysis. Dewatering in a multi-layered aquifer-aquitard system often causes groundwater drawdowns in multiple aquifers, which together lead to obvious settlement of adjacent pile-supported building. This paper documents an in-situ pumping test conducted in a multi-aquifer system. It indicates that an adjacent pile-supported building settled continuously after water level was stabilized. To clarify the possible reasons for this phenomenon, a series of numerical models were established, validated and employed to explore the load transfer behaviour between pile and multi-aquifers during different dewatering conditions. Results indicate that the appearances of several aquitards in the multi-aquifer system significantly block the hydraulic connection between different aquifers, leading to non-synchronized developments of groundwater drawdown and pile shaft resistance at different soil layers during pit dewatering, which eventually causes the lagging settlement of the building. In practical pit dewatering in multi-aquifer system, engineers should appropriately increase the monitoring time for the deformation of adjacent pile-supported buildings for avoiding missing the maximum settlement. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
00221694
Volume :
638
Database :
Academic Search Index
Journal :
Journal of Hydrology
Publication Type :
Academic Journal
Accession number :
178233184
Full Text :
https://doi.org/10.1016/j.jhydrol.2024.131539