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Environmental and Engineering Geoscience; August 2007; v. 13; no. 3; p. 217-228; DOI: 10.2113/gseegeosci.13.3.217
© 2007 Association of Engineering Geologists
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Stress-strain Measurements of Deforming Aquifer Systems That Underlie Shanghai, China

Yun Zhang1, Yu-Qun Xue1, Ji-Chun Wu1, Shu-Jun Ye1 and Qin-Fen Li2

1 Department of Earth Sciences, Nanjing University, Nanjing, China
2 Shanghai Institute of Geological Survey, Shanghai, China


Figure 01
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Figure 1. Location map and administrative divisions of Shanghai, and the locations of extensometer groups

 

Figure 02
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Figure 2. A conceptual hydrogeologic model of Shanghai

 

Figure 03
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Figure 3. The annual amount of groundwater pumped and recharged in Shanghai from 1961 to 2000

 

Figure 04
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Figure 4. The developing history of land subsidence in Shanghai. (a) Average cumulative subsidence of Shanghai. (b) Cumulative subsidence at Labor Park, Shanghai

 

Figure 05
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Figure 5. The annual net amount of groundwater pumped from individual aquifers from 1961 to 2000

 

Figure 06
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Figure 6. Variation of groundwater level with time. (a) Confined aquifer one, two, and four. (b) Confined aquifer three and five

 

Figure 07
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Figure 7. Land subsidence and compaction of individual strata at extensometer group four

 

Figure 08
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Figure 8. (a) Compaction variation of soft clay layers one and two and groundwater level change in confined aquifer one. (b) The relation of compaction strain and effective stress change from January 1981 to December 2002

 

Figure 09
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Figure 9. (a) Compaction variation of soft clay three and groundwater level change in confined aquifer two. (b) Effective stress change versus strain of soft clay three from January 1981 to December 2002

 

Figure 10
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Figure 10. (a) Compaction variation of sand layer three and four and groundwater level change in confined aquifer three. (b) Effective stress change versus strain of sand layers three and four from January 1981 to December 2002

 

Figure 11
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Figure 11. (a) Compaction variation of sand layer five and groundwater level change in confined aquifer four. (b) Effective stress change versus strain of sand layer five from January 1981 to December 2002

 

Figure 12
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Figure 12. Creep curves of Shanghai clay and sand

 





JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
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