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World Biochem 2019 & Regenerative Medicine 2019
Journal of Genetics and Molecular Biology | Volume 3
Page 43
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BIOCHEMISTRY AND ENZYMOLOGY
World Congress on
TISSUE ENGINEERING AND REGENERATIVE MEDICINE, STEM CELL RESEARCH
2
nd
Global Conference on
Joint Event on
IMPACT OF THE PROCESS OF EROSION ON THE PROPERTIES OF BLACK SOIL
SOILS OF THE SOUTHEASTERN PARTS OF THE GREAT CAUCASUS
Aliyev Z H
National Academy of Sciences, Azerbaijan
S
hamakhi region, situating in south-east slope of Great Caucasian has 393, 3 thousand hectare area. The area
of region is situated in 200-2500 m. height above seal level.
As in all regions of great caucasian, this region is belonged to low mountainous zone, from geological and geo-
morphologic point of view. In soil formation process, rocks play a great role in formation of their fertility. When
the rocks, rich with mineral elements are weathered in the region, absorbs into soil a great number of nourish-
ment elements. A lot of potassium and other elements are absorbed into the structure of soils, of which hydrom-
ica arises from fieldspar, mica and slates. In mountainous part of the region, soil former rocks mainly consist of
slates, marls and sandy. But in watersheds, basalt, marble and granites are met. In middle mountainous part
the rocks mainly consist of clayey slates, clay with lime mixture and sandy. As it is known, climate plays a very
great role in soil formation process. V V Dokuchayev, I P Gerasimov, I F Figurovski, A Shikhlinski , and others have
informed about a great role of climate in erosion formation process. Climate of Shamakhi region corresponds to
the climate of Middle Europe. Here, the minimum temperature is observed between 3rd ten days of december
and 2
nd
ten days of february. And the maximum temperature is observed in february, july-august months. Aver-
age yearly quantity of rains is about 460-600 mm. Mountain and meadow, mountain and forest, mountain-cher-
nozem, mountain and grey-dark brown soils have spread in region area. Because of our investigation covers
mountain-chernozem, we dwell on their main character V V Akimitsev, M A Salayev, G B Salamov, and others
have noted on spreading of chernozem inmountain zone of Azerbaijan. Chernozems have spread in limited area
in Great Caucasian and are strongly used under agriculture plants.
They have mainly developed in middle mountainous area of Shamakhi and Ismayilli regions. We have investi-
gated mountain-chernozems in Shamakhi region. Morphological description of soils types, flushed in average
degree and subjected to erosion is indicated below.Section 1: Divided in the region of Jabani village, gentle east
Bakharli slope. A 0-17 cm chernozem clayey, heap, hard, dry, plant roots, rootlets, worm ways, small stones, boils
for the impact of chlorine acid, the passage is clear. B 17-39 cm chernozem, upper layer is relatively light, clayey,
heap a little hard, root and rootlets, small stones, spots in brown vein form, wormways, damp, oils for the impact
of chlorine acid, passage is gradual.
Aliyev Z H, J Genet Mol Biol 2019, Volume 3
Aliyav Z H was professor in Institute of Erosion and Irrigation, Azerbaijan National Academy of Sciences, Azerbaijan.
Volqa_5@mail.ruBIOGRAPHY