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muddy or sandy soil types (Juillie and Sherwood 1983) [3].Salts have partially cemented the sand, which is typically very
loose to medium compact. The lagoon sediments known as "muddy Sabkha" are primarily made up of sand- and carbonate-
based mud's. The extensive ramification of names for things makes it more difficult to define Sabkha numerous Middle
Eastern situations with high water tables [4]. The most accurate description of the[5] have reported on the sabkha system
as the big (in dimension or size), flat saline, (horizontal terrains with slight, unnoticeable slopes)Aeration zones (due to the
dry and hot environment), located either in coastal areas (referred to as coastal Sabkhas) or inland Sabkhas further inland
(also known as continental or inland sabkhas) a lot of dry, semi-tropical nations [5].
The low shear strength and high compressibility of Sabkha soils are troublesome. Therefore, these soils provide a
considerable risk of settlement and/or bearing capacity failure, and structures should not be erected on them. Due to the
diversity and quantity of salts they contain, these soils display a broad range of behavior variations. Common salts include
gypsum (Ca SO4 2H2O), calcium carbonate (CaCO3), calcium sulphate (anhydrite), and halite (NaCl) salt, once dried,
functions as a binder that improves soil's shear strength and lowers its compressibility. When salt dissolves in water, it
alters the soil structure, resulting in a loose and unstable matrix. This transformation increases the soil's compressibility,
heightening the risk of collapse, while simultaneously reducing its shear strength. Numerous methods for enhancing the
geotechnical properties of Sabkha soil have been extensively documented in academic literature [6]. Among these methods
are grouting removal and compaction, geosynthetic reinforcement, vibroflotation, stone columns, dynamic compaction,
removal and replacement, and preloading. The effectiveness of the augmentation approach is contingent on a number of
variables, including the kind, quantity, and solubility of salts, soil permeability, temperature, and chemical qualities of
groundwater.
Based on the soil's particle size, some studies have categorized sabkha soil into two groups: sandy Sabkhas and muddy
Sabkhas. In most cases, muddy Sabkha (a kind of lagoon silt) is composed of a sand-based carbonate mud. Sandy sabkha is
relatively loose to medium-density soil that occasionally has salts acting as a partial cement [7][8]. In Sabkha soils, high
moisture concentrations, or "Sabkha brine," are commonly seen. Using ASTM D 4643, the water content of sabkha soils in
the Arabian Gulf was calculated and found to be about 25%. (Al-Shayea et al. 2003) [9]. Additionally, it was discovered
that the Sabkha soil in Sohar, Oman, had a natural water content of 25.64 percent (Al-Alawi et al. 2020) [10]. But Jizan
Sabkha soil had a natural water content that varied from 16.7 to 63.5 percent [11]. According to Al-Homidy et al. [12],
Sabkha soil has a natural water content that ranges from 8 to 65%. In general, climate circumstances and the kind of soil
(i.e., coastal Sabkha or continental soil) influence the change of the natural water content.
1.1 Formation of the Sabkha
Sabkha is produced by the constant interaction of brines and sediment [13]. Minerals and sedimentary topographies are
among the various aspects of Sabkha deposits linked to the original deposition framework. Several elements influence the
creation of Sabkha, such as:
1. Climate consists of precipitation, humidity, temperature, and wind speed.
2. Geochemical: contains both minerals and brine chemistry
3. Geomorphological: groundwater table and surface gradient and
4. Hydrological: This may be an independent cause or effect of the first three.
5. Biological: consists of the burrowers and algal mats
The reactions that characterize Sabkha soil and its environs may be the consequence of the collaboration and interaction of
the components above [14].
1.2 Chemical Stabilization
Al-Amoudi [15] investigated how two chemical stabilizing agents affected the density and compressive strength
(unconfined) of Sabkha. Experience the flavor of Sabkha Lime and cement were used to improve the soil quality in eastern
Saudi Arabia. They used five doses on soil samples collected at two moisture levels (16 and 22 percent) (0, 2.5, 5, 7, and 10
percent). Following standard compaction tests and sample preparation, unconfined compressive strength was evaluated
repeatedly during curing. In all cases, the findings show that a moisture content of around 30 percent is best, and that
increasing the cement content raises the maximum dry density. Sabkha mixtures stabilized with lime did not have a
noticeably greater maximum dry density than those that were not. Further, for cement additions of 7.5 and 10%, data reveal
that the strength of cement-stabilized Sabkha rises even after 90 days of cure. Since Lime Sabkha mixes could not attain
their full strength until 90 days after curing, this suggests that extensive curing is necessary to develop strength. Statistics
indicate that cement plays a crucial role in maintaining the stability of Sabkha at its natural moisturelevel.The solidification
of Sabkha resulted in a progressive enhancement of its structural integrity over time.Al-Amoudi et al. [16] looked at how
adding dust from limestone, cement, and lime altered Sabkha's salty and dry characteristics. It came from an eastern Saudi
Arabian area. After 7 days, we subjected the samples to industry-standard compacted and unconfined compressive strength
tests. Aiban et al. [17] evaluated the efficiency of lime-stabilized Sabkha Soil in Ras Al-Ghar. Saudi Arabia's Eastern
Province. Lab experiments including soil characterization, compaction, unconfined, and triaxial compression were
performed on soil samples collected at varying depths. There are noticeable differences in the moisture and lime content
between cleaned and unwashed Sabkha soils. When soil samples were compacted at a higher moisture content than was
desirable, they found that adding 5% lime boosted the soil's strength. They also found that the strength of the soil was
affected by the amount of salt present, the curing regime, and the amount of moisture in the mold throughout the curing