Morphogenetic structure of soils of the dry bottom of the aral sea

ISMONOV, Abduvaxob, DO‘SALIYEV, Alijon, MAMAJANOVA, O‘ktamxon

Ўзбекистон Миллий университети хабарлари · 2026-yil

Annotatsiya

The article describes in detail the morphogenetic features of desert sandy, takyr-like, residual takyr residual meadow soils. Fromthe very beginning (since 1960), it was noted that automorphic soils formed on large areas of land where water receded. Theformation of automorphic soils on the drained seabed is primarily due to the fact that groundwater has sunk below the level andhas little effect on soil formation. Also, the formation of the soil is associated with the lithological and geomorphologicalconditions of the area in a dry climate. It was noted that the formation of automorphic soils was manifested in the morphogeneticstructure of soils, that is, in the formation of salt crystals, the formation of rust spots in the lower parts of the layer.

Maqola ma’lumotlari
MualliflarISMONOV, Abduvaxob, DO‘SALIYEV, Alijon, MAMAJANOVA, O‘ktamxon
JurnalЎзбекистон Миллий университети хабарлари
NashriyotЎзбекистон Миллий университети
ISSN2181-7324, 3093-8996
Nashr sanasi2026-09-15
Jild3
Son3.2
Betlar57-60
TilIngliz
Indeksga qo‘shilgan2026-09-17

Maqolaning asl sahifasi

Kalit so‘zlar

Dry bottom of the Aral Sea, takyr-like, soils, groundwater, porous sands, lithology, Обсохщой дно Аральского моря, такыровидные, почво-грунты, грунтовые воды, пористые пески, литология., Orol dengiz qurigan tubi, taqirsimon, tuproq-gruntlar, sizot suvlari, g‘ovak qumlar, litologiya.

Iqtibos keltirish

APAISMONOV, Abduvaxob, DO‘SALIYEV, Alijon, & MAMAJANOVA, O‘ktamxon (2026). MORPHOGENETIC STRUCTURE OF SOILS OF THE DRY BOTTOM OF THE ARAL SEA. Ўзбекистон Миллий университети хабарлари, 3(3.2), 57-60. https://journals.nuu.uz/index.php/actanuuz/article/view/14899
GOST (OAK)ISMONOV, Abduvaxob, DO‘SALIYEV, Alijon, MAMAJANOVA, O‘ktamxon MORPHOGENETIC STRUCTURE OF SOILS OF THE DRY BOTTOM OF THE ARAL SEA // Ўзбекистон Миллий университети хабарлари. – 2026. – T. 3, № 3.2. – P. 57-60.
MLAISMONOV, Abduvaxob, DO‘SALIYEV, Alijon, and MAMAJANOVA, O‘ktamxon. “MORPHOGENETIC STRUCTURE OF SOILS OF THE DRY BOTTOM OF THE ARAL SEA.” Ўзбекистон Миллий университети хабарлари, 3(3.2), 57-60, 2026. https://journals.nuu.uz/index.php/actanuuz/article/view/14899
ChicagoISMONOV, Abduvaxob, DO‘SALIYEV, Alijon, and MAMAJANOVA, O‘ktamxon. “MORPHOGENETIC STRUCTURE OF SOILS OF THE DRY BOTTOM OF THE ARAL SEA.” Ўзбекистон Миллий университети хабарлари, 3(3.2), 57-60 (2026). https://journals.nuu.uz/index.php/actanuuz/article/view/14899
HarvardISMONOV, Abduvaxob, DO‘SALIYEV, Alijon, and MAMAJANOVA, O‘ktamxon (2026) ‘MORPHOGENETIC STRUCTURE OF SOILS OF THE DRY BOTTOM OF THE ARAL SEA’, Ўзбекистон Миллий университети хабарлари, 3(3.2), 57-60. https://journals.nuu.uz/index.php/actanuuz/article/view/14899
BibTeX
@article{ismonovabduvaxob2026,
  title = {MORPHOGENETIC STRUCTURE OF SOILS OF THE DRY BOTTOM OF THE ARAL SEA},
  author = {ISMONOV, Abduvaxob and DO‘SALIYEV, Alijon and MAMAJANOVA, O‘ktamxon},
  journal = {Ўзбекистон Миллий университети хабарлари},
  year = {2026},
  volume = {3},
  number = {3.2},
  pages = {57-60},
  url = {https://journals.nuu.uz/index.php/actanuuz/article/view/14899}
}

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