Poplar tree (Populus balsamifera L.) as indicator of mercury emission from a point source / D. V. Yusupov, E. E. Lyapina, E. M. Tursunalieva [et al.]

Уровень набора: ChemosphereАльтернативный автор-лицо: Yusupov, D. V., geologist, Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences, 1977-, Dmitry Valerievich;Lyapina, E. E., geochemist, Senior lecturer of Tomsk Polytechnic University, Candidate of geological-mineralogical sciences, 1981-, Elena Evgenievna;Tursunalieva, E. M., Elena Muratovna;Osipova, N. A., geochemist and geoecologist, Associate Professor of Tomsk Polytechnic University, Candidate of chemical sciences, 1958-, Nina Aleksandrovna;Baranovskaya, N. V., geochemist, Professor of Tomsk Polytechnic University, Doctor of biological sciences, 1970-, Nataliya VladimirovnaКоллективный автор (вторичный): Национальный исследовательский Томский политехнический университет, Инженерная школа природных ресурсов, Отделение геологииЯзык: английский.Страна: .Резюме или реферат: The article provides original data on the ecological and geochemical characteristics of the distribution of Hg in the leaves and annual rings of balsam poplar (P. balsamifera L.) in the zone of influence of lithium production (Novosibirsk). In 2017 high Hg concentration (1300 ng/g) in the poplar leaves was recorded in the northeastern part of the city near the industrial facility of the lithium plant. The investigation showed a clear trend of increased Hg accumulation in the poplar leaves during the growing season. The maximum average Hg content was detected in the leaf litter in 2006 (1153–2425 ng/g). However, the average Hg content in the soil is 294 ng/g, which is significantly lower than the threshold limit value (2100 ng/g). Studies of changes in the content of Hg with the height of the crown of the tree revealed an increase in the upwind side of the emission source, the concentration of Hg in the leaves is on average 1.5 times higher than on the side of the "wind shadow". Hg in poplar leaves, leaf litter, and soils is mainly found in free and physically bonded forms - the most mobile, prone to increased migration, transformation and methylation under environmental conditions. According to the Hg content in the poplar cores, an increase in the Hg input near the source was established with the beginning of Li production - in the period 1967–1985 years (441 ng/g) with a subsequent decrease to 6 ng/g in 2000–2017..Аудитория: .Тематика: электронный ресурс | труды учёных ТПУ | Hg | urban area | poplar leaves | annual rings | dendro-biogeochemistry | lithium plant | листья | города | годовые кольца | биогеохимия Ресурсы он-лайн:Щелкните здесь для доступа в онлайн
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The article provides original data on the ecological and geochemical characteristics of the distribution of Hg in the leaves and annual rings of balsam poplar (P. balsamifera L.) in the zone of influence of lithium production (Novosibirsk). In 2017 high Hg concentration (1300 ng/g) in the poplar leaves was recorded in the northeastern part of the city near the industrial facility of the lithium plant. The investigation showed a clear trend of increased Hg accumulation in the poplar leaves during the growing season. The maximum average Hg content was detected in the leaf litter in 2006 (1153–2425 ng/g). However, the average Hg content in the soil is 294 ng/g, which is significantly lower than the threshold limit value (2100 ng/g). Studies of changes in the content of Hg with the height of the crown of the tree revealed an increase in the upwind side of the emission source, the concentration of Hg in the leaves is on average 1.5 times higher than on the side of the "wind shadow". Hg in poplar leaves, leaf litter, and soils is mainly found in free and physically bonded forms - the most mobile, prone to increased migration, transformation and methylation under environmental conditions. According to the Hg content in the poplar cores, an increase in the Hg input near the source was established with the beginning of Li production - in the period 1967–1985 years (441 ng/g) with a subsequent decrease to 6 ng/g in 2000–2017.

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