The Geological Evolution of the Water-Rock Interaction 2018
DOI: 10.31554/978-5-7925-0536-0-2018-379-382
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Geochemistry of Underground and Surface Waters in the Zone of Influence of the Ash Dump of Chita TPP-1

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Cited by 5 publications
(7 citation statements)
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“…Previously, the excess of permissible concentrations by it in borehole samples (point 2, Fig. 1), a spring (point 6) and the river Kadalinka in the drought period, we interpreted [5,6] as a consequence of the inflow of Si with the infiltration waters of the ash dump. But the data of the borehole 241 (point 3) which is located much closer to HAD and which Si concentrations in water is turned out to be below 10 mg / l ( Table I), show that its high contents can be formed in situ, the same nature of high concentrations in excess of MPC for Mn, Fe, Co and Ni.…”
Section: Resultsmentioning
confidence: 96%
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“…Previously, the excess of permissible concentrations by it in borehole samples (point 2, Fig. 1), a spring (point 6) and the river Kadalinka in the drought period, we interpreted [5,6] as a consequence of the inflow of Si with the infiltration waters of the ash dump. But the data of the borehole 241 (point 3) which is located much closer to HAD and which Si concentrations in water is turned out to be below 10 mg / l ( Table I), show that its high contents can be formed in situ, the same nature of high concentrations in excess of MPC for Mn, Fe, Co and Ni.…”
Section: Resultsmentioning
confidence: 96%
“…[2-4 and others] There are few publications describing the influence of coal energy on the geochemical characteristics of groundwater. In addition to our own works [5,6] we consider works of other scientists [7][8][9]. The purpose of this study is to present the nature and extent of the technogenic changes in the chemical composition of groundwater as a result of filtration leakages of one of the ash dumps, hence, expanding the database on the problem under consideration.…”
Section: Introductionmentioning
confidence: 99%
“…Hydrocarbonate composition of surface and underground waters is typical for these zonal and climatic conditions , Zhuldybina 2010, Zamana et al 2011. The hydrochemical composition of lake waters from a two-component -sodium hydrogen carbonate until the 60s of the last century was transformed into a three-component -sulfate-hydrocarbonate-chloride sodium-calcium-magnesium (Tsybekmitova 2016, Usmanova et al 2018 (Table 1). The water composition change was due to the ash dump leakage.…”
Section: Sampling Sitementioning
confidence: 99%
“…24 кн глубиной 77,2 м. Взаимодействие техногенных вод с золошлаками, почвами и породами приводит к понижению их кислотно-основных свойств [9]. В результате фильтрации через золошлаковые отложения фтор удаляется из фильтрующихся вод, что обусловлено процессом образования флюорита, по которому воды отстойника пересыщены [8]. В сравнении с водами отстойника в подземных водах уменьшается содержание кальция, но растут концентрации магния, за счет которого увеличивается жесткость воды [10].…”
Section: материалы и методы исследованияunclassified