Soil Behaviour Type Index

Soil Behaviour Type Index 1

The soil behaviour type index (I_c) in Soil_Behaviour_Type_Index_1 is defined as:

I_c=((C_1 - log_{10} Q_t)^2 + (log_{10}F_r+C_2)^2)^{0.5}\\ \ \\ Q_t=\frac{q_c-\sigma_{v0}} {P_a} \left(\frac{P_a} {\sigma'_{v0}}\right)^n\\ \ \\ \left(\frac{P_a}{\sigma'_{v0}}\right) \leq 1.7 \\ \ \\ F_r=\frac{f_s}{q_t-\sigma_{v0}}\times 100 \text {%}

     I_c is calculated using n=1, if I_c> I_{\text{c break}}, then it's been accepted, otherwise it's calculated using n=0.5. If I_c< I_{\text{c break}} break then it's accepted, otherwise it's calculated using n=0.7.

Robertson and Wride (1998)

Where:

     C_1 is 3.47 in the published formula, and is stored in the Soil_Behaviour_Type_Index_1_C1 field. 
     C_2is 1.22 in the published formula, and is stored in the Soil_Behaviour_Type_Index_1_C2 field.

The constants are stored on CPT_POINT_CORRELATION_PARAMETERS and CPT_PROJECT_CORRELATION_PARAMETERS tables.

Transition zones

A Trasition Zone in Soil_Behaviour_Type_Index_Transition_1 for a certain depth is considered when:
     2.3<I_c<2.9;
     The rate of I_c change is rapid (slope of I_c vs. depth above and below of the current depth > 5) 
     and crosses the I_c=2.6 line.

Soil Behaviour Type Index 2

The soil behaviour type index (I_c) in Soil_Behaviour_Type_Index_2 is defined as:

I_c=\sqrt {[C_1-log_{10}Q_t(1-B_q)]^2+[C_2+C_3 \cdot log_{10}F_r]^2}

Jefferies and Davies (1993), NCHRP Synthesis 368 p 27

Where:
     C_1 is 3 in the published formula, and is stored in the Soil_Behaviour_Type_Index_2_C1 field. 
     C_2 is 1.5 in the published formula, and is stored in the Soil_Behaviour_Type_Index_2_C2 field. 
     C_3 is 1.3 in the published formula, and is stored in the Soil_Behaviour_Type_Index_2_C3 field.

The constants are stored on CPT_POINT_CORRELATION_PARAMETERS and CPT_PROJECT_CORRELATION_PARAMETERS tables.

Soil Behaviour Type Index 3

The non-normalised Soil Behaviour Type Index (I_{SBT}) in Soil_Behaviour_Type_Index_3 is defined as:

I_{SBT}= \left(\left(C_1-log \left( \frac{(q_c)}{p_a}\right)\right)^2+(log(R_f)+C_2)^2\right )^{0.5}

Robertson (2010), CPT 10, paper 2-56 (http://www.cpt10.com/PDF_Files/2-56RobSBT.pdf)

Where:
     C_1 is 3.47 in the published formula and is stored in the Soil_Behaviour_Type_Index_3_C1 field.
     q_t is taken from the Total_Cone_Resistance field on the CPT_DATA table.
     q_c is taken from the Cone_Resistance field on the CPT_DATA table.
     p_a is the Atmospheric pressure, 101.4 kPa, and is set in the Formula Tool.
     R_f is taken from the Friction_Ratio field on the CPT_DATA table.
     C_2 is 1.22 in the published formula and is stored in the Soil_Behaviour_Type_Index_3_C2 field.

The constants are stored on CPT_POINT_CORRELATION_PARAMETERS and CPT_PROJECT_CORRELATION_PARAMETERS tables.

Soil Behaviour Type Index 4

The soil behaviour type index (I_c) in Soil_Behaviour_Type_Index_4 is defined as:

I_c=\sqrt {[C_1-log_{10}Q_t(1-B_q)+1]^2+[C_2+C_3 \cdot log_{10}F_r]^2}

Been and Jefferies (1992), Soil liquefaction, a critical state approach, pp. 206-207

Where:
     C_1 is 3 in the published formula, and is stored in the Soil_Behaviour_Type_Index_4_C1 field. 
     C_2 is 1.5 in the published formula, and is stored in the Soil_Behaviour_Type_Index_4_C2 field. 
     C_3 is 1.3 in the published formula, and is stored in the Soil_Behaviour_Type_Index_4_C3 field.

The constants are stored on CPT_POINT_CORRELATION_PARAMETERS and CPT_PROJECT_CORRELATION_PARAMETERS tables.

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