Characteristics of desert sandy soils formed in the dry bottom of the aral sea

DUSALIEV, ALIJON, ISMONOV, Abduvaxob, MAMAJANOVA, O‘ktamxon

Ўзбекистон Миллий университети хабарлари · 2026-yil

Annotatsiya

In recent years, because of the strengthening of natural and anthropogenic factors, the non-drainage of the Amu Darya and SyrDarya waters into the Aral Sea has led to the predominant formation of various soils on the dried sea bottom. When studying thedegree of salinity of desert-sandy soils in studies, it was found that in the surface layer of soil in section 47, i.e., in layers at adepth of 0-9 and 9-50 cm, the salinity of the soil is of the chloride-sulfate type, and the lower The soil profile layers are sulfate-chloride and saline; low salinity is noted. The amount of humus in the surface layer of the studied desert sandy soils, 0-9 cm and9-50 cm layers, is fixed in the range from 0.418% to 0.528%.

Maqola ma’lumotlari
MualliflarDUSALIEV, ALIJON, ISMONOV, Abduvaxob, MAMAJANOVA, O‘ktamxon
JurnalЎзбекистон Миллий университети хабарлари
NashriyotЎзбекистон Миллий университети
ISSN2181-7324, 3093-8996
Nashr sanasi2026-09-10
Jild3
Son3.2
Betlar36-38
TilIngliz
Indeksga qo‘shilgan2026-09-11

Maqolaning asl sahifasi

Kalit so‘zlar

Dry bottom of the Aral Sea, proof-soil, easily soluble salts, sand dunes., Обсохщое дно Аральское море, прочво-грунт, легкорастворимые соли, песчаное барханы., Orol dengizi qurigan tubi, tuproq-grunt, suv tuz rejimi, transformatsiyasi, keltirma, qum barhan.

Iqtibos keltirish

APADUSALIEV, ALIJON, ISMONOV, Abduvaxob, & MAMAJANOVA, O‘ktamxon (2026). CHARACTERISTICS OF DESERT SANDY SOILS FORMED IN THE DRY BOTTOM OF THE ARAL SEA. Ўзбекистон Миллий университети хабарлари, 3(3.2), 36-38. https://journals.nuu.uz/index.php/actanuuz/article/view/14878
GOST (OAK)DUSALIEV, ALIJON, ISMONOV, Abduvaxob, MAMAJANOVA, O‘ktamxon CHARACTERISTICS OF DESERT SANDY SOILS FORMED IN THE DRY BOTTOM OF THE ARAL SEA // Ўзбекистон Миллий университети хабарлари. – 2026. – T. 3, № 3.2. – P. 36-38.
MLADUSALIEV, ALIJON, ISMONOV, Abduvaxob, and MAMAJANOVA, O‘ktamxon. “CHARACTERISTICS OF DESERT SANDY SOILS FORMED IN THE DRY BOTTOM OF THE ARAL SEA.” Ўзбекистон Миллий университети хабарлари, 3(3.2), 36-38, 2026. https://journals.nuu.uz/index.php/actanuuz/article/view/14878
ChicagoDUSALIEV, ALIJON, ISMONOV, Abduvaxob, and MAMAJANOVA, O‘ktamxon. “CHARACTERISTICS OF DESERT SANDY SOILS FORMED IN THE DRY BOTTOM OF THE ARAL SEA.” Ўзбекистон Миллий университети хабарлари, 3(3.2), 36-38 (2026). https://journals.nuu.uz/index.php/actanuuz/article/view/14878
HarvardDUSALIEV, ALIJON, ISMONOV, Abduvaxob, and MAMAJANOVA, O‘ktamxon (2026) ‘CHARACTERISTICS OF DESERT SANDY SOILS FORMED IN THE DRY BOTTOM OF THE ARAL SEA’, Ўзбекистон Миллий университети хабарлари, 3(3.2), 36-38. https://journals.nuu.uz/index.php/actanuuz/article/view/14878
BibTeX
@article{dusalievalijon2026,
  title = {CHARACTERISTICS OF DESERT SANDY SOILS FORMED IN THE DRY BOTTOM OF THE ARAL SEA},
  author = {DUSALIEV, ALIJON and ISMONOV, Abduvaxob and MAMAJANOVA, O‘ktamxon},
  journal = {Ўзбекистон Миллий университети хабарлари},
  year = {2026},
  volume = {3},
  number = {3.2},
  pages = {36-38},
  url = {https://journals.nuu.uz/index.php/actanuuz/article/view/14878}
}

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