Issue 50
G. Belokas, Frattura ed Integrità Strutturale, 50 (2019) 354-369; DOI: 10.3221/IGF-ESIS.50.30
Figure 2 : Graphical representation of the regression model.
Assuming that: a) x i variation for each x i
is an accurate observation, b) each x i and d) the uncertainties of the y i
is an independent observation, c) the error ε i
has a constant
observations are equivalent (otherwise weight coefficients are required), the best mean estimators for the linear regression coefficients are given by Eqs.(8,9). Observation x i can be a predetermined imposed loading (e.g. the σ n in direct shear and the σ 3 in the typical triaxial), while observation y i a measured reaction (e.g. the τ in direct shear and the σ 1 in the typical triaxial). , 1 1 1 1 2 2 , 2 1 , , 1 n n n n i i i i i i d y i i i i m xy n n n d x i x x y y x y y x S Cov x y n b r Var x y S x x (8)
i x
x
i
n
1
i
1
1
i
i
(9)
m m a y b x
, y i ) are the data measurements of the two dimensional sample, , y x are their mean values, S d,x and S d,y are the
In Eqs.(8,9) ( x i
sample standard deviation of x and y measurements (Eqs.(10,11)) and r xy
the Pearson sample correlation coefficient (given
by Eq.(12)). The r xy =1 the correlation is a perfect direct, i.e. increasing). Moreover, an unbiased estimate of the variance of y ( x ) with n-2 degrees of freedom is given by Eq.(13). The standard error estimators SE b and SE a of the b and a regression coefficients are given by Εqs.(14,15), re spectively. Some applications in civil and geotechnical engineering of the two variables linear model have been presented by Baecher & Christian [1], Pohl [8] and Kottegoda & Rosso [11], as for instance the case of a variation with depth. A classic example is the increasing undrained shear strength with depth. The application of this model in the Mohr – Coulomb strength failure criterion has some individual characteristics that will be presented later. is sensitive only to a linear relationship between two variables (| r xy |≤1, when r xy
1
n
2
S
x x
(10)
, d x
i
1 i
n
1
1
n
2
S
y y
(11)
, d y
i
1 i
n
1
i i i i i i i n x y x y n x x n y 2 2 2
(12)
r
xy
2
y
i
n
2
i
1 2
n S
ˆ ˆ
i i y a bx i
,
| var y x S
(13)
1
i
,
d
n
2
n
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