Жарияланымдар / Публикации

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  • Некоторые метрики заблокированы вашими 
    Тип записи:Публикация,
    CURRENT SOIL STATE OF POPULATIONS OF SEDUM HYBRIDUM L. AND SEDUM EWERSII LEDEB. FOUND IN THE ZAILIY ALATAU
    (Al-Farabi Kazakh National University, 2024-01-01)
    Tatyana Kobylina
    ;
    Бекзат Тыныбеков
    ;
    Akmaral Nurmahanova
    ;
    Gulmira Satybaldiyeva
    ;
    Gulbanu Aueskhanovna Sadyrova
    The article describes the natural soil conditions of Sedum hybridum L. and Sedum ewersii Ledeb—populations area based on the results of field and laboratory soil studies of soils. Soil types, morphological features, chemical composition, nutrient elements, amount of humus, absorbed bases and salt composition, and mechanical composition of soils are determined. The following soil types were identified during field studies: Kokzhailau Gorge (population 1) – chernozem, Turgeni Gorge (population 2) – chernozem, near Kastek River (population 3) – chestnut soil. The humus content in the 0-80 cm layer of chernozem (population 1) of Kokzhailiau gorge is very high, ranging from 5.55-12.81%, the reaction of the soil medium is within pH 7.10-7.40, i.e. CO2 content ranges from 0.16 to 0.34. On chernozems of Turgeni gorge (population 2) humus content in 0-60 cm layer is very high, within 5.90-20.88%, reaction of soil medium within pH 6.15-7.07, amount of CO2 within 0.21-0.34. On chestnut soils near the Kastek River (population 3), the humus content in the 0-73 cm layer was in the range of 1.57-6.92%, the pH ranged from 7.13-8.23, i.e. it was alkaline, the CO2 content was in the range of 0.16 - 0.34. The composition of salts in the chernozems of the Kokzhailau gorge: CO3 - not detected; HCO3- - 0,24- 0,48 ; Cl- – 0.04; CO4- – 0,12-0,92; Sa+ – 0,29-0,49; Mg 2+ – 0,20-0,98; Na+ – 0,05-0,06; To+ – 0,05-0,23; The amount of salts is 0.060-0.083%. It was found that the soils of all 3 populations are not saline, since the amount of salts does not exceed the salinity limit.
  • Некоторые метрики заблокированы вашими 
    Тип записи:Публикация,
    Regional Variation in Plant Community Composition and Soil Properties of Alcea nudiflora Habitats Along an Elevational Gradient in the Trans-Ili Alatau, Kazakhstan
    (PAGEPress (Italy), 2026-10-09)
    Akerke Abil
    ;
    ;
    Серик Бакиров
    ;
    Zhansaya Abdukadirova
    ;
    Wild plant populations in mountain ecosystems often depend on specific combinations of soil, vegetation and microsite conditions. Alcea nudiflora (Lindl.) Boiss. is a poorly studied Malvaceae species in Central Asia, and its population structure across different soil and vegetation conditions in the Trans-Ili Alatau remains insufficiently documented. We assessed three natural populations of A. nudiflora along an elevational gradient in the Trans-Ili Alatau, Kazakhstan: P1 at 900 m a.s.l., P2 at 1438 m a.s.l. and P3 at 1620 m a.s.l. Floristic composition, vegetation structure, ontogenetic stages and soil physicochemical properties were analysed using field surveys, 10 × 10 m plots, soil descriptions, laboratory analyses and exploratory ordination. P1 occurred in relatively open meadow–shrub vegetation and showed the strongest coenotic expression of A. nudiflora, with 62 individuals recorded within the 100 m2 vegetation plot and a broad representation of major ontogenetic stages. In P2, A. nudiflora remained a regular component of shrub–meadow and forest-edge vegetation, whereas in P3, the species occurred sparsely and was restricted to meadow openings, forest-edge gaps, and local microsites. Surface soil properties varied among habitats. In the upper horizon, P1 had 3.67% humus, 95.2 mg kg−1 readily hydrolysable N, 36.0 mg kg−1 available P2O5, 610 mg kg−1 available K2O, pH 8.41 and 4.28% CO2; P2 had 3.72% humus, 39.2 mg kg−1 readily hydrolysable N, 44.8 mg kg−1 available P2O5, 450 mg kg−1 available K2O, pH 8.23 and 0.54% CO2. PCA explained 37.1%, 33.8% and 9.4% of variance on PC1–PC3, summarizing gradients of nutrients, texture, carbonates and alkalinity. The results indicate that population status is associated with surface soil conditions, vegetation structure and microsite availability rather than elevation alone.