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Rice grass used for water phytoremediation with varying concentrations of 17α-ethinylestradiol hormone = Capim arroz na fitorremediação de água com concentrações variadas do hormônio 17α-etinilestradiol Texto completo
2019
Rayssa Thainá de Paiva Alves | Braga, Luana Aparecida Silvestre | Braga, Luana Aparecida Silvestre | Fernandes, Katiúcia Dias | Andrade, Sandro José de | Alley Michael da Silva Procópio
17α-ethinylestradiol (EE2), an endocrine disruptor (ED) excreted by women and is found in contraceptive and hormone replacement pills used at menopause. An increase in EDs requires alternative means of water and sewage treatment, since these compounds threaten human health and the environment, even at trace levels. Phytotechnology stands out from other processes because it is sustainable, given that plants are used to recover the contaminated environment. Thus, the objective of this study was to evaluate rice grass performance in the removal of 17α-ethinylestradiol (EE2), and determine the effect of this hormone on the root anatomy and chlorophyll content of the species. A completely randomized design was used with 4 replications: EE2 concentration composed of 4 study treatments (420, 300, 180 and 60 μg L-1 EE2) and 2 control treatments (positive and negative). The effect of the treatments was evaluated over time (1, 7 and 15 days). EE2 removal from the solution was analyzed by HPLC. Chlorophyll was analyzed by UVvis spectrophotometry, showing that EE2 does not interfere with the photosynthetic activity of rice grass. Aerenchyma was analyzed by microphotographs of root sections, revealing a higher proportion in plants exposed to the hormone, indicating morpho-anatomical adaptations to survive in this medium. Thus, it can be concluded that rice grass has significant phytoremediation potential after 7 days’ exposure, surviving and adapting to the contaminated environment, and can be used to complement water and sewage treatments. = O 17α-etinilestradiol (EE2) é um interferente endócrino (IE) liberado pelo organismo feminino e encontrado em remédios contraceptivos e de reposição hormonal na menopausa. A ascensão dos IEs requer meios alternativos de tratamento de água e esgoto, pois esses compostos ameaçam a saúde humana e o meio ambiente, mesmo em nível traço. A fitotecnologia vem se distinguindo dos demais processos por ser sustentável, tendo em vista que a recuperação do meio contaminado é feita através de plantas. Assim, objetivou-se com este trabalho avaliar o capim arroz na remoção do 17α-etinilestradiol (EE2), bem como verificar o efeito desse hormônio na anatomia radicular e no teor de clorofila dessa espécie. O experimento foi conduzido em delineamento inteiramente casualizado, com 4 repetições. Os tratamentos consistiram das concentrações de EE2 (420, 300, 180 e 60 μg L-1), mais dois controles (positivo e negativo). O efeito dos tratamentos foi avaliado no tempo, sendo: 1, 7 e 15 dias (tempo de remediação). A análise da remoção do EE2 da solução foi feita por HPLC. A análise da clorofila foi feita por espectrofotômetro UV-vis e mostrou que o EE2 não interfere na atividade fotossintética de capim arroz. A análise dos aerênquimas foi executada por microfotografias de secções das raízes, revelando maior proporção de aerênquimas nas plantas que tiveram contato com o hormônio, indicando adaptações morfoanatômicas para sobreviverem nesse meio. Sendo assim, a espécie tem alto potencial fitorremediador com 7 dias de exposição, sobrevivendo e se adaptando no ambiente contaminado, podendo ser empregada como complemento em tratamentos de água e esgoto.
Mostrar más [+] Menos [-]Metal partitioning in sediments and mineralogical controls on the acid mine drainage in Ribeira da Água Forte (Aljustrel, Iberian Pyrite Belt, Southern Portugal) Texto completo
2012
Maia, Flávia | Pinto, Cláudia | Waerenborgh, João Carlos | Gonçalves, Mário A. | Prazeres, Cátia | Carreira, Ondina | Sério, Susana
This work focuses on the geochemical processes taking place in the acid drainage in the Ribeira da Água Forte, located in the Aljustrel mining area in the Iberian Pyrite Belt. The approach involved water and stream sediment geochemical analyses, as well as other techniques such as sequential extraction, Mössbauer spectroscopy, and X-ray diffraction. Ribeira da Água Forte is a stream that drains the area of the old mine dumps of the Aljustrel mine, which have for decades been a source of acid waters. This stream flows to the north for a little over than 10km, but mixes with a reduced, organic-rich, high pH waste water from the municipal waste water pools of the village. This water input produces two different results in the chemistry of the stream depending upon the season: (i) in the winter season, effective water mixing takes place, and the flux of acid water from the mine dumps is continuous, resulting in the immediate precipitation of the Fe from the acid waters; (ii) during the summer season, acid drainage is interrupted and only the waste water feeds the stream, resulting in the reductive dissolution of Fe hydroxides and hydroxysulfates in the stream sediments, releasing significant quantities of metals into solution. Throughout the year, water pH stays invariably within 4.0–4.5 for several meters downstream of this mixing zone even when the source waters come from the waste water pools, which have a pH around 8.4. The coupled interplay of dissolution and precipitation of the secondary minerals (hydroxides and sulfates), keeps the system pH between 3.9 and 4.5 all along the stream. In particular, evidence suggests that schwertmannite may be precipitating and later decomposing into Fe hydroxides to sustain the stream water pH at those levels. While Fe content decreases by 50% from solution, the most important trace metals are only slightly attenuated before the solution mixes with the Ribeira do Rôxo stream waters. Concentrations of As are the only ones effectively reduced along the flow path. Partitioning of Cu, Zn and Pb in the contaminated sediments also showed different behavior. Specific/non-specific adsorption is relevant for Cu and Zn in the upstream branch of Ribeira da Água Forte with acid drainage conditions, whereas the mixture with the waste water causes that the association of these metals with oxyhydroxide to be more important. Metals bound to oxyhydroxides are on the order of 60–70% for Pb, 50% for Cu and 30–60% for Zn. Organic matter is only marginally important around the waste water input area showing 2–8% Cu bound to this phase. These results also show that, although the mixing process of both acid and organic-rich waters can suppress and briefly mitigate some adverse effects of acid drainage, the continuing discharge of these waste waters into a dry stream promotes the remobilization of metals fixed in the secondary solid phases in the stream bed back into solution, a situation that can hardly be amended back to its original state.
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