2.1. Complex Stress System of Pit-in-Pit Structure
Foundation pit engineering has strong practicality and particularity in the construction process; it needs to constantly monitor and analyze and dynamically adjust the project [
28]. In this section, the complex stress system of pit-in-pit is analyzed theoretically based on classical earth pressure theory [
29].
Figure 2 shows the complex stress system of the pit-in-pit structure, where the
w is the distance between the inner pit and the outer pit, the
h is the depth of the inner pit, and the
b is the width of the inner pit. At this time, the overall stress state of the foundation pit becomes complicated and the soil pressure of the outer pit needs to be calculated by finite element software [
30]. In the process of foundation pit excavation, as the soil is removed, the load on it is reduced, which will cause the soil at the bottom of the pit to produce an upward displacement tendency. If the excavation of the internal foundation pit continues, it will cause a change in the stress field and displacement field. Meanwhile, as the foundation pit system is in such a complex stress system, there is a great risk of settlement in the adjacent areas and on the surface caused by unloading.
Before the excavation of the foundation pit, the lateral earth pressure distribution curve of the soil was
OA and the static lateral pressure coefficient was
K0n. After the excavation of the foundation pit, the actual lateral earth pressure distribution curve became
BA′. Due to the influence of unloading, the soil below the bottom of the pit is in a super-consolidated state. At this time, the static earth pressure coefficient increases to
K0, where the
. The excavation of a pit within a pit will cause the earth pressure acting on the pit within a pit retaining body to develop from the static lateral earth pressure distribution curve
BA′ to the active earth pressure curve [
31]. When designing the retaining structure of a pit within a pit, if the stress path change is not considered but it is believed that the earth pressure develops from the curve
BA″ to the active earth pressure curve like in ordinary foundation pits, the magnitude of the earth pressure will be seriously underestimated. Thus, a complex stress system architecture involving the interaction of internal and external foundation pits is constructed, as shown in
Figure 3.
At the same time, for the finite soil pressure in the pit, the angle between the failure plane and the horizontal plane is no longer the fixed value in the classical Rankine and Coulomb soil pressure theory
. It is a function of the soil mechanical properties, the distance between the inner pit and the outer pit envelope, and the width and depth of the pit in the calculated depth [
32]. The above characteristics determine the complexity of the calculation of the force in the pit and the sensitivity of the parameters. When the pit in the pit is excavated in a special stratum, the complexity of the system will be further amplified [
33], so the compound instability effect of the pit in the collapsibility loess stratum needs to be discussed separately [
34].
2.2. Characteristics of Collapsible Loess Degraded by Water
Loess exhibits relatively high shear strength in a dry environment. However, when exposed to water, its shear strength decreases. The most important factors affecting the change in the soil shear strength are the weakening of cementation and the change of pores [
35], as shown in
Figure 4. The undisturbed loess structure was transformed by leaching, which provided favorable conditions for disintegration caused by water infiltration. The presence of matric suction further accelerates this infiltration, causing the pore pressure inside the soil to rapidly increase until disintegration occurs [
36].
For foundation pit engineering, when rainfall or groundwater begins to infiltrate the foundation pit soil, the soil strength is reduced to a critical value and instability failure will occur, as shown in
Figure 4. At the same time, for unsaturated loess, due to the influence of its compaction and structural strength [
37], the shear strength index of loess has its unique properties and the strength envelope also shows a special law, which does not fully conform to the Mohr–Coulomb criterion [
38].
According to Zhang Maohua’s analysis of the undrained shear test data of collapsible loess, the envelope line of unsaturated loess is not straight, but a broken line composed of two straight lines and the turning point of the broken line is related to the structural strength [
38]. The
is the normal stress at the critical point of structural strength and the two sections represent different structures and deformation forms of unsaturated loess. The front section maintains its original structure with small failure strain, while the latter section experiences significant structural changes and a loss of strength. The shear strength of collapsible undisturbed loess is expressed by a sectional line as follows:
The shear strength of soil is not only related to the properties of soil, but also to the drainage conditions, shear rate, stress state, stress history, and many other factors during the test, among which the most important are the drainage conditions during the test. According to the principle of effective stress, the effective stress strength parameter should be obtained from
.
Figure 5 shows the soil shear strength index obtained by Zhang Maohua through the triaxial CU test. The data obtained from the test are fitted through spline functions, in which the soil shear strength index also changes with the change in the water content
w, the cohesion index, and
c decrease with the increase in the water content, but the friction angle and effective friction angle fluctuate with the change in the water content.
Numerous studies and reports on loess have confirmed that for loess in different regions, the change in the shear strength index is different [
39,
40], but all change with the water content, which is determined by the essential characteristics of loess. The general expression of the soil shear strength index is as follows:
2.3. Compound Instability Effect
Many scholars have studied the excavation mechanical response of pit-in-pit, and these studies point to the conclusion that the excavation of pit-in-pit will build a complex stress system structure involving the interaction of internal and external foundation pits. At the same time, for the above complex stress system, the traditional method of calculating the Rankine soil pressure formula will have a large numerical deviation from the actual situation [
19].
Tan, Y et al. studied the mechanical response characteristics of pits within pits in special strata [
19]. The research proves that for the complex stress system of pit-in-pit, the traditional engineering experience and calculation method are very likely to fail when excavation is carried out in the stratum with special mechanical properties. However, it is a pity that there is no research on the mechanical response characteristics of pits in collapsible loess areas. Pit excavation involves the secondary excavation unloading of the excavated soil in the foundation pit, which causes the redistribution of soil stress and horizontal displacement, and makes the mechanism and performance of the pile in the transition zone more complicated [
41]. If precipitation or water table action occurs in the construction stage, the collapse action will make the stress state of the support structure in the transition zone more complicated and difficult to predict. Xie et al. [
32] calculated the passive soil pressure of the foundation pit under the condition of pit-in-pit. According to the relative position relationship between the inner and outer pits, the sliding modes could be divided into four forms, as shown in
Figure 6, and the passive soil pressure was derived accordingly.
It is assumed that: (1) the soil is rigidly shaped and the friction between the soil and the outer pit envelope is not considered; (2) the wall is vertical and the sliding surface is plane; (3) the soil is in a passive state, sliding upward, without considering the friction between the sliding soil and the pit support structure in the pit; and (4) the limited soil is
c,
homogeneous soil. When the slip surface does not pass through the inner pit (case ④), the slip soil is triangular and the shear failure angle is as shown in Equation (3) [
32].
The sliding soil does not belong to the category of finite soil because the sliding surface does not pass through the inner pit. At this time, the shear failure angle is a fixed value, which is completely consistent with the results obtained from the classical soil pressure theory. When
, the entire inner pit is inside the sliding soil (case ①) and the shear failure angle is as shown in Equation (4) [
32].
When the shear failure angle
is no longer a fixed value, but a function of the soil mechanical properties, calculated depth, pit width, and depth, its general expression is as shown in Equation (5).
When the positional relationship of the foundation pit is as in case ②, the shear failure angle is as shown in Equation (6).
Different from case ①, the distance between the inner pit and the outer pit envelope also becomes a factor affecting the shear failure angle of the slip surface.
When the positional relationship of the foundation pit is as in case ③, the shear failure angle is as shown in Equations (7) and (8).
When
,
When
,
In case ③, the shear failure angle decreases with the increase in the distance between the inner pit and the outer pit envelope and the depth of the inner pit. The nonlinearity of the shear failure angle increases with the increase in the calculated depth. In
Section 2.2, a general expression of the shear strength of loess under water immersion has been obtained
. When the water content changes, the change in the soil shear strength index will affect the soil pressure distribution in the pit, as shown in Equations (3)–(8). At the same time, when the friction angle (
) changes, the relative position relationship between the internal foundation pit and the external foundation pit may change, for example, when the water content increases,
will change and the relative relationship ③ of the internal and external foundation pit can be changed from the original mode to mode ②, as shown in
Figure 6.
In the actual process of immersion, the moisture content in different regions of the soil is not the same, and the spatial distribution of the moisture content in the inner and outer pits will be a function of time. Therefore, the soil pressure distribution in the collapsible loess formation is a complex function of the soil parameters, the relationship between the internal and external pit positions, and the time of immersion.
To find the critical analytic solution of the failure mode, case ① is taken as an example. Assume that the expression of
c(
w) and
ϕ(
w) with the moisture content is shown in Equation (9) [
25], where
c0,
ϕ0 are the initial moisture content state parameters and
α,
β are the deterioration coefficients. At this time, the driving displacement of the difference between the passive earth pressure
Ep in the outer pit and the active earth pressure
Ea in the inner pit is calculated, as shown in Equation (10), where
.
When the shear force and shear strength of the slip surface are balanced, it can be derived that
, also because
. The critical moisture content obtained by a simultaneous solution is shown in Equation (11).