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Surgil ESIA Report - Volume III - EKN

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“O’ZLITINEFTGAZ”<br />

open joint-stock company<br />

FS «Complex development of <strong>Surgil</strong> field<br />

with extracting of valuable components»<br />

Complex of Paleogene deposits is practically anhydrous and serves as the regional<br />

waterproof rock.<br />

2) Marlaceous-limestone complex of deposits is bedded over the described above complex<br />

and is from late Neogene (Miocene) period (carbonate formation – group of semihard<br />

rocks) and presented with limestones having interbeds of marls, argillas, gypsum and<br />

sandstones. The thickness of these deposits is 40-110m.<br />

Described complexes are overlain with thin cover of overburden such as loamy sands, loams and<br />

sands.<br />

In hydrogeological regard ground water in the area in question occur at a depth of over than<br />

25.0m. Ground water has low pressure rate, 3-30g/l salinity rate and clearly defined sulfate and sulfatechloride<br />

aggressiveness. This water can be used for the service purposes only.<br />

Soils are characterized with the solid residue rate which is 9,560-28,160mg/kg, chlorine ions<br />

concentration which is 1,240-10,560mg/kg and sulfate ions concentration which is 2,950-17,950mg/kg.<br />

In accordance with BC 2.03.11-96 «Corrosion protection for building structures» the soils with such<br />

chlorine ions concentration are strongly aggressive to the concretes based on Portland cement and<br />

Portland-slag cement according to SS 10178-85 and sulfate-resistant cements according to SS 22266-<br />

94. According to research performed by «O'ZLITINEFTGAZ» open joint-stock company the foundation<br />

soils in question are ranged from low to high degree of corrosive aggressiveness.<br />

During carrying out of geological engineering study at UGCC site they assigned three<br />

engineering-geological elements according to lithological profile (Attachment 1).<br />

The first engineering-geological element (EGE-1) is presented with interstratified loamy sands<br />

and loams with non-clearly defined interfaces which are plastered, macroporous and subsiding. Type of<br />

subsidence – I due to minor thickness.<br />

EGE-1 soils are widely spread in the upper part of profile. The thickness of the bed is up to 1.0m.<br />

Design resistance of soil in normal condition R 0 = 250kPa (2.5kgf/cm 2 ), in water-saturated condition R 0<br />

= 150kPa (1.5kgf/cm 2 ). Group of soil according to mining – p.366. EGE-1 soils are recommended to be<br />

removed due to their strength properties and deformation behavior.<br />

Table 1 – Physical-mechanical properties of EGE-1 soils<br />

Characteristic Unit Normative value<br />

Specific weight of soil particles g/cm 3 2.67<br />

Specific weight of soil g/cm 3 1.60<br />

Specific weight of dry soil g/cm 3 1.56<br />

Porosity % 41.6<br />

Porosity factor 0.712<br />

Natural humidity % 2.4<br />

Humidity 0.1<br />

Humidity at the yield point % 19.1<br />

Humidity at the rolling point % 13.3<br />

Plasticity number % 5.8<br />

Consistency index > 0<br />

Permeability coefficient m/d > 3.0<br />

Book 5. Declaration of environmental impact concerning UGCC construction<br />

12

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