FEATURES OF THE ACCUMULATION OF WATERSOLUBLE FLUORIDE IN THE SOILS AND PLANTS OF THE CARPATHIAN BIOSPHERE RESERVE

被引:0
|
作者
Kryuchenko, N. O. [1 ]
Zhovinsky, E. Ya. [1 ]
Paparga, P. S. [2 ]
机构
[1] NAS Ukraine, MP Semenenko Inst Geochem Mineral & Ore Format, 34 Acad Palladin Ave, UA-03142 Kiev, Ukraine
[2] Minist Ecol & Nat Resources Ukraine, Carpathian Biosphere Reserve, 77 Red Pleso Str, UA-90600 Rakhiv, Ukraine
来源
MINERALOGICAL JOURNAL-UKRAINE | 2024年 / 46卷 / 03期
关键词
watersoluble fluoride; soils; plants; altitudinal zones; steepness of slopes; Carpathian Biosphere Reserve;
D O I
10.15407/mineraljournal.46.03.066
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The results of research on the content of water-soluble fluorine in the soils and vegetation of the Carpathian Biosphere Reserve (KBR) are presented. Analyzes were performed using a spectrometric spectrometer with alizarin-complexone on a Specol 11 spectrophotometer. Based on the results of statistical processing of the analysis, the limits and background content of water-soluble fluorine were established in soils on the plots: Yasynska - 0.1-1.34 mg/kg (background - 1.1 mg/kg); Rakhivska - 0.1-2.86 mg/kg (background - 1.4 mg/kg); Bohdanska - 1.34-1.9 mg/kg, (background - 1.6 mg/kg) (total background content - 1.34 mg/kg). It was determined that in the soils of the areas located in the zone of tectonic disturbance (v. Kvasy) the content of fluorine is greater than the background (1.35-1.4 mg/kg), its intake occurs together with mineral waters and gases. It was found that the maximum content of water-soluble fluorine (1.6-2.6 mg/kg) in in sod-podzolic soils (light and medium loamy) of the Marmaros massif, which is associated with increased humidity and the presence of kaolinite component of clay minerals, which does not bind fluorine into hard-to-reach compounds, subalpine) and the content of water-soluble fluorine in soils, at the same time, a weak negative relationship between the steepness of slopes (gentle, steep, precipitous) and the content of water-soluble fluorine in soils (the lower the steepness of the slope, the higher the content of water-soluble fluorine) was found. Biogeochemical properties for water-soluble fluorine (according to the biological absorption coefficient, Ax) of nine types of plants were established: evergreen conifers (pins and branches) - Taxus baccata L. - 15.5; Thuja - 5, Abies alba - 5; birch family (branches and leaves) - Corylus avellana L. - 6.1, Alnus glutinosa (L.) P. Gaertn - 2.8; grasses (leaves and flowers) - Betonica officinalis L. - 4.6, Centaur & eacute;a jacea - 6, Senecio vulgaris L. - 4.3, Filipendula ulmaria - 3.9. The concentrator of water-soluble fluorine is the pins and branches of the Taxus baccata L.
引用
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页码:66 / 78
页数:13
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