

same formula as K0: (P0 –U0) → σ’h
KD is an ‘amplified’ K0, because (P0 – U0)
is an ‘amplified’ σ’h,
due to penetration KD well correlated to K0 and OCR (clay)

KD = 2 in NC clay (OCR = 1)
KD > 2 in OC clay (OCR > 1)
same formula as K0: (P0 –U0) → σ’h
KD is an ‘amplified’ K0, because (P0 – U0)
is an ‘amplified’ σ’h,
due to penetration KD well correlated to K0 and OCR (clay)
KD = 2 in NC clay (OCR = 1)
KD > 2 in OC clay (OCR > 1)
Experimental
Kamei & Iwasaki 1995
Theoretical
Finno 1993
Theoretical
Yu 2004
Experimental
Marchetti 1980
Theoretical
2004 Yu