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Transformation models and their applications in geotechnical design
Jianye Ching (National Taiwan University) Marcos Arroyo, Jieru Chen (contributor of SAND/7/2794), Celeste Jorge, Tim Länsivaara (contributor of F-CLAY/7/216), Dianqing Li, Paul Mayne, Kok-Kwang Phoon, Widjojo Prakoso, Marco Uzielli June 5 Geo-Risk 2017 Transformation models and their applications in geotechnical design
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Transformation models
Models that convert test results to design parameter Mostly based on generic/global dataset Kulhawy & Mayne (1990) How do these models perform? For a region For a specific site
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OCR versus su/v dataset
CLAY/10/7490 dataset 30 regions, 250+ studies All su converted to su(mob) Median estimate 95% confidence interval Transformation uncertainty Ching, J. and Phoon, K.K. (2014). Transformations and correlations among some clay parameters – the global database, Canadian Geotechnical Journal, 51(6),
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OCR versus su/v model
How does it perform for a region? Scandinavia dataset Courtesy of Tim Länsivaara 22 sites, 168 data points All su converted to su(mob) Median estimate Systematically biased 95% confidence interval Not genuine 95%
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OCR versus su/v model
What does it perform for specific site(s)? Individual site can have its own local trend Median estimate Systematically biased 95% confidence interval Typically too wide Ensemble global sites Unbiased Genuine 95%
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Global transformation models
Biased for a region or a specific site Wide confidence interval (conservative) Unbiased for ensemble global sites Genuine 95% confidence interval
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Future needs Intermediate transformation models
Site-specific models are good, but not enough data Large statistical uncertainty Global models can be biased and with wide CI Large transformation uncertainty Is there something in between that works well? Fusion between limited site-specific data and global data? Accumulate soil & rock databases Make them available to the public Web software & Apps Sinotech cooperation
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Thank you (Some useful global transformation models are at the end of Chapter 1)
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