IODINE IN FRESH WATER OF MOUNTAIN CRIMEA. / Kayukova, E.P.; Berezkin, V.Yu.
Геология, геоэкология, эволюционная география: коллективная монография. Vol. XIX Санкт-Петербург : Издательство РГПУ им. А.И. Герцена, 2020. p. 188-192.Research output: Chapter in Book/Report/Conference proceeding › Article in an anthology › Research › peer-review
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TY - CHAP
T1 - IODINE IN FRESH WATER OF MOUNTAIN CRIMEA
AU - Kayukova, E.P.
AU - Berezkin, V.Yu.
PY - 2020
Y1 - 2020
N2 - The content of iodide ions in fresh waters of the Mountain Crimea has been studied. Atmospheric precipitation is the main source of iodine in the groundwater of the Quaternary aquifer, in the waters of the Lower and Upper Cretaceous aquifers, as well as in the waters of the weathered volcanic-sedimentary sediments of Karadag (J2b). There is a small degree of iodine deficiency here, since the concentration of iodine does not reach the lower limit of the standard of physiological usefulness of drinking water. The maximum concentrations of iodide ions are associated with the area of melange.
AB - The content of iodide ions in fresh waters of the Mountain Crimea has been studied. Atmospheric precipitation is the main source of iodine in the groundwater of the Quaternary aquifer, in the waters of the Lower and Upper Cretaceous aquifers, as well as in the waters of the weathered volcanic-sedimentary sediments of Karadag (J2b). There is a small degree of iodine deficiency here, since the concentration of iodine does not reach the lower limit of the standard of physiological usefulness of drinking water. The maximum concentrations of iodide ions are associated with the area of melange.
KW - IODINE
KW - FRESH WATERS
KW - MOUNTAINOU CRIMEA
UR - https://www.elibrary.ru/item.asp?id=44623627&pff=1
M3 - Article in an anthology
SN - 978-5-8064-2986-6
VL - XIX
SP - 188
EP - 192
BT - Геология, геоэкология, эволюционная география
PB - Издательство РГПУ им. А.И. Герцена
CY - Санкт-Петербург
ER -
ID: 74744281