3.1. Geology and geomorphology
This area belongs to Zagros zone. There are some active faults such as Aghajari fault (in 70 km distance), Ahwaz fault (in 60 km distance), and white fault (in 80 km distance). This area is located in a low possibility zonation of occurring earthquake with 0.2 g, according to the Iranian earthquake code.
This area is located near the Persian Gulf and is categorizes as lowland regions. Also, this lowland area is filled with soil, and now it has an elevation in the range of 1.3-3.1 m. In addition, it has two major estuaries with the name of Zangi Estuary (800 m width) and Jafary Estuary (400 m width). The general profile of soil in this area includes soft soil, sludge, and salt until 10 m depth, then medium-stiff soil to 20 m depth, and finally compacted sand.
NaCl Salt in this area exists in 2 forms. The first one is a mixture of salt and soil. The second one is a pure salt layer. The underground water table is in the range of 0.2 to 3.4 m in winter.
3.2. Field site investigation
For this study, 41 boreholes by drilling method and continuous coring with a depth of 11 to 25 m used for determining geotechnical site investigation in the Special Economic Petrochemical Zone, southwest of Iran. Boreholes describe as BH101 to BH141 are illustrated in Fig. 3.
3.2.1. Pressuremeter tests
This field test is very useful for determining the stress-strain behavior of soil. It is performed with a radial expandable probe inside the borehole. The type of pressuremeter used in this study is P.B.P. (Pre-Bored Pressuremeter) with the name of Ménard Pressuremeter. Table 1 illustrate the pressuremeter test results.
Table 1. Pressuremeter Results in Special Economic Petrochemical Zone, Iran
Borehole
|
Depth, m
|
Soil Type
|
α
|
Em, kg/cm2
|
E`s, kg/cm2
|
Es, kg/cm2
|
PL, kg/cm2
|
Em/PL
|
G, kg/cm2
|
Ks, kg/cm3
|
BH-138
|
2-3.5
|
CL
|
0.67
|
66
|
98.5
|
61.4
|
1.25
|
5.26
|
2.34
|
3.84
|
6-7.5
|
CL
|
0.67
|
63
|
94
|
58.6
|
1.27
|
4.97
|
2.25
|
3.69
|
9-10.5
|
CL
|
0.67
|
60
|
89.6
|
55.8
|
1.14
|
5.21
|
2.13
|
3.48
|
BH-139
|
1-2.5
|
SM
|
0.34
|
66
|
194.1
|
121
|
1.47
|
4.5
|
2.45
|
3.87
|
4-5.5
|
SM
|
0.34
|
71
|
208.8
|
130.1
|
1.48
|
4.87
|
2.62
|
4.14
|
7-8.5
|
SM
|
0.34
|
54
|
158.8
|
99
|
1.73
|
3.11
|
1.96
|
3.14
|
9-11
|
SM
|
0.34
|
60
|
176.5
|
110
|
1.7
|
3.54
|
2.23
|
3.52
|
BH-140
|
1-2.5
|
ML
|
0.5
|
94
|
188
|
117.1
|
2
|
4.71
|
3.36
|
5.51
|
3.5-5
|
ML
|
0.5
|
74
|
148
|
92.2
|
1.7
|
4.38
|
2.56
|
4.34
|
6.5-8
|
CL
|
0.67
|
64
|
95.5
|
59.5
|
1.72
|
3.7
|
2.26
|
3.71
|
10-11.5
|
CL
|
0.67
|
82
|
122.4
|
76.3
|
1.74
|
4.71
|
2.93
|
4.8
|
BH-141
|
1-2.5
|
ML
|
0.5
|
82
|
164
|
102.2
|
1.67
|
4.9
|
2.92
|
4.87
|
5-6.5
|
CL
|
0.67
|
75
|
111.9
|
69.7
|
1.67
|
4.51
|
2.69
|
4.4
|
9.5-11
|
CL
|
0.67
|
66
|
98.5
|
61.4
|
1.73
|
3.81
|
2.35
|
3.85
|
3.2.2. Vane shear test
Vane shear test is an in situ tests for evaluating undrained shear strength. The Standard code of this test is ASTM D2573. This test has been used for site investigation in soft soils. The results of field vane shear tests are illustrated in Table 2.
Table 2. Vane shear test results
Borehole
|
Depth, m
|
Soil Type
|
Su (Peak)
(kg/cm2)
|
Su (Residual)
(kg/cm2)
|
Sensitivity
|
Remarks
|
BH-106
|
7
|
Silty Clay
|
0.11
|
0.08
|
1.37
|
Slightly sensitive
|
BH-110
|
9
|
Silty Clay
|
0.05
|
0.03
|
1.67
|
Slightly sensitive
|
BH-113
|
7
|
Sandy Silty Clay
|
0.11
|
0.05
|
2.20
|
Medium Sensitive
|
BH-113
|
11
|
Sand
|
0.27
|
0.17
|
1.59
|
Slightly sensitive
|
BH-114
|
11
|
Silty Clay
|
0.07
|
0.04
|
1.75
|
Slightly sensitive
|
3.2.3. Salt Sub Layers in PETZONE
From 41 boreholes, 6 number of them have salt sub layers. Table 3, depicted salt layers in various boreholes. The Standard Penetration value is between 4 to 10 until the depth of 11 m. Thickness of salt sub layers vary from 0.2 to 2.8 m.
From 41 boreholes, 6 number of them have salt sub layers. Table 3, depicted salt layers in various boreholes. The Standard Penetration value is between 4 to 10 until the depth of 11 m. Thickness of salt sub layers vary from 0.2 to 2.8 m.
Table 3. Salt layers in various boreholes
Row
|
Borehole
|
Depth, m
|
Thickness, m
|
G.W.L.
|
Soil description
|
S.P.T.
|
1
|
BH 101
|
2.3-2.5
|
0.2
|
0.4
|
Salt with peat, wet, white
|
5
|
2
|
BH 102
|
2.1-2.5
|
0.4
|
0.9
|
Salt with peat, very hard, wet, white
|
61
|
3
|
BH 102
|
2.5-3
|
0.5
|
0.9
|
Salt with peat, wet, white
|
4
|
4
|
BH 105
|
2.7-3
|
0.3
|
1.5
|
Salt with ooze & peat, soft, wet, white
|
3
|
5
|
BH 110
|
2.7-4.3
|
1.6
|
0.8
|
Salt with ooze & peat, soft, wet, light gray
|
3
|
6
|
BH 110
|
4.3-5.0
|
0.7
|
0.8
|
Silty clay with salt, wet, light gray
|
2
|
7
|
BH 116
|
5.0-7.2
|
2.2
|
1.8
|
Silty clayey sand with ooze & salt, loose, wet, dark, gray
|
9
|
8
|
BH 122
|
5.3-5.6
|
0.3
|
1.5
|
Salt, very hard, wet, white
|
28
|
9
|
BH 122
|
11.0-12.2
|
1.2
|
1.5
|
Salt with ooze, firm, wet, gray
|
12
|
10
|
BH 122
|
12.2-15.0
|
2.8
|
1.5
|
Silty clay with salt and ooze, wet, dark gray
|
30
|
11
|
BH 122
|
15.0-17.0
|
2.0
|
1.5
|
Silty clay with salt and ooze, hard, wet, dark gray
|
32
|
3.3. Sand and Salt Properties for Experimental Tests
For conducting laboratory tests, sand materials were obtained from PETZONE, Mahshahr in the Southwest of Iran. Unit Weight of this soil is 26.29 kN/m3, and it categorizes as SM due to the Unified system of soil categorization. For soil stabilization and modeling liquefiable sand, water content is considered as 30 %. Figure 4 illustrates the salt layer in the depth 4-5 m below the ground. Also, figure 5 depict sieve analysis of sand material. In the mass mixing method this salty layer will mix with above, and below the soil and a combination of treated salty soil with cement will produce.
There are Interlayers of salt beneath the ground in the southwest of Iran. Shallow salt layers are not compact, but deeper salt converts to salt rock with a density in the range of 20-25 kN/m3 and compression strength of more than 15kPa. In this research for investigating the effects of salt on soil, treatability studies performed. As illustrated in the Scanning Electron Microscope images, Fig. 6, shallow salts are completely in the crystal form, which are soft soils, but deeper denser salts have less crystal shape.
In soil stabilization of various soil types in the southwest of Iran, type two Portland cement has been used. General properties of this type of Portland cement with a specific gravity of 31.5 kN/m3 are presented in Table 4.
Table 4. General properties of Portland cement used in this study
Oxides
|
Content, %
|
CaO
|
60-70
|
SiO2
|
17-25
|
Al2O3
|
3-8
|
Fe2O3
|
0.5-0.6
|
MgO
|
0.5-4
|
SO3
|
2-3.5
|
Na2O
|
0.5-3
|
3.4. Sample Preparation
The sand and salt were collected from a site in PETZONE, Mahshahr petrochemical zone in the Southwest of Iran. The procedure of sample preparation was similar to that is described by Chew et al. (2004). First, salt, and sand samples were dried at 105 °C for 24 h. Then, 90 % of sand was mixed with 10% salt. After that, 30 % water was mixed thoroughly with the mixture of salty sand to obtain slurries. The higher water content samples were chosen to simulate the water content increase taking place in a mass mixing process in the field. Cement slurry at a water-cement ratio (w/c) of 0.6 was then added to the sample and thoroughly mixed. The amount of cement in a slurry form that was added to salty soil was 2, 4, 6, 8, and 10% by mass of dry soil. The mixture was then placed in 5 layers into PVC molds 35 mm in diameter and 70 mm in height for the unconfined compression test. To remove entrapped air bubbles, the placement of the samples into the molds was accompanied by a tapping action around the molds. Each treated salty sand preloaded by 0, 9, and 45 kPa. Steel rods were used for imposing preload to the salty sand. Curing periods of 120 days were chosen to determine the long-term effect. Unconfined compression tests were performed on the samples at an axial deformation rate of 1 mm/min. Figure 7, illustrates apparatuses used for preloading salty sand.