Location and brief characteristics of the construction area
The construction of new commercial sea port is planned to
be placed in the Krasnodar area on the western coast of Taman
peninsula in the region of
Panagiya cape, Tuzla dam and Chushka spit in the middle part
of the Kerch strait. (The general plan is on pic.1).
All complexes of the first stage of construction is intended
to place in the region of Panagiya cape (diagram of general
plan. pic.2).
Complexes of the second and third stages of construction,
placed in the region of Tuzla dam and Chushka spit, respectively
(diagram of general plan. pic.3).
First region (first stage of construction) Panagiya cape:
- the specialized container complex - 2 mln. t/yr;
- the specialized grain complex - 5 mln. t/yr;
- the specialized coal complex - 7-10 million.t/yr;
- the complex of oil and oil products - 5 mln. t/yr;
- the complex of liquefied natural gas - 2 mln. t/yr.
Second region (second stage of construction) Tuzla dam:
- complex on the transshipment of metal - 2 mln. t/yr;
- complex on the transshipment of mineral fertilizers - 3
mln. t/yr;
- complex on the transshipment of forest - 3 mln. t/yr.
The third region (third stage of construction) Chushka spit:
- ferry-boat complex with cargo turn-over up to 2 mln. t/yr.
Special feature of the future construction of new port in
the region of Tuzla dam is strongly developed soundings of
water area of Tamanskiy gulf, that practically excludes the
necessity of erection of any protecting structure.
The approximate estimation of sediment accumulation of the
ship channel and the future water area of a new port testifies
that this process is irregular in length, and a degree of
sediment accumulation is insignificant.
Restoration of a radical part of a spit - Tuzla dam in length
3780 m has substantially reduced penetration of storm waves
from Black sea. As consequence, rates of abrasion and washout
of northern and east coast of Tamanskiy gulf have essentially
decreased. Results of modeling investigations of influence
of Tuzla dam on lytho-morphodynamic processes in a coastal
zone have revealed stabilizing effect of this construction.
Decrease in a countercurrent from Tamanskiy gulf promotes
development of accumulation of deposits on a beach from the
Black Sea part of a dam and, thus, raises its protective properties.
|
