FEATURES OF THE ISFARA GROUNDWATER DEPOSIT
This article systematically analyzes the geological structure and hydrogeological characteristics of the Isfara groundwater deposit,
which is an integral part of the Fergana hydrogeological basin. The study provides a detailed description of the stratigraphy and
lithological composition of the Quaternary deposits of the region, in particular the Sokh, Tashkent, Mirzachul and Syrdarya
complexes. The results of many years of scientific research on the hydrodynamic regime of the Isfara River cone spread, sources
of groundwater saturation and the balance of consumption are summarized.
1. Tarasov, Yu.I. (1983). Farg‘ona viloyatining Beshariq tumani hududi yerlarini sug‘orish uchun Isfara daryosi konus
chiqarmasi to‘rtlamchi davr yotqiziqlari yer osti suvlarini dastlabki qidirish ishlari. Isfara GGG.
2. Boyboboyev, I.U. (1985). Farg‘ona viloyatining Beshariq tumani hududi yerlarini sug‘orish uchun Isfara daryosi konus
chiqarmasi sharqiy qismi to‘rtlamchi davr yotqiziqlari yer osti suvlarini dastlabki qidirish ishlari natijalari. Rapqon GGG.
3. Zayitov, R. (2010). Suv xo‘jaligi sharoitlarining o‘zgarishi va 570 km² yangi sug‘oriladigan yerlarni o‘zlashtirish natijasida
Isfara koni yer osti suvlarining bashorat qilingan resurslarini qayta baholash bo‘yicha mintaqaviy gidrogeologik tadqiqotlar
olib borish. Olmazor GGG.
4. Begmatov, R.M. (2004). Farg‘ona viloyatida yer osti suvlarining rejimi va muvozanatini o‘rganish bo‘yicha gidrogeologik
tadqiqotlar. Farg‘ona GGS.
5. БАЙМУРЗАЕВ, Е. (2025). OPTIMIZATION OF OPEN CULTIVATION CONDITIONS FOR THE ARAL STRAIN OF MICROALGA DUNALIELLA SALINA TO OBTAIN CAROTENOID-RICH BIOMASS. «ACTA NUUz», 3(3.2.1), 39–41. Retrieved from https://journals.nuu.uz/index.php/actanuuz/article/view/10240
Copyright (c) 2026 «ACTA NUUz»
This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.
.jpg)
1.png)
