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1.
Sci Total Environ ; 844: 157238, 2022 Oct 20.
Article in English | MEDLINE | ID: mdl-35810907

ABSTRACT

Tropical streams have been intensively impacted by agricultural activities. Among the most important agricultural activities in Brazil, sugarcane production represents a large impact for economic development and for environmental conditions. Permeating sugarcane fields, several headwater streams can be affected by sugarcane cultivation, in special, aquatic biogeochemical cycles because of the deforestation, fertilization, crop residues and higher temperatures in the tropics. In this study, we analyzed the effects of sugarcane cultivation on methane fluxes and concentrations, assuming that carbon cycles are influenced by agricultural activities in headwater streams. Our study aimed to (1) measure methane fluxes and concentrations in tropical streams located in Southeastern Brazil, (2) Analyze whether seasonal cycles influence methane fluxes and concentrations, (3) Evaluate the influence of sugarcane cultivation on methane fluxes and (4) Analyze the association between water chemistry in the methane concentrations in tropical streams. We found mean fluxes of CH4 of 0.280 mmol m-2 d-1, with higher fluxes during the summer and in streams draining preserved catchments. The average CH4 concentrations were 0.695 µmol L-1, with higher values during the summer and in streams draining preserved catchments. Methane concentrations in the studied streams was influenced by dissolved oxygen (negatively), dissolved organic carbon (negatively), water velocity (positively) and conductivity (negatively). Methane concentrations were significantly higher than concentrations found in Temperate Grasslands, Savannas & Shrublands and similar to concentrations found in other tropical biomes (excluding Tropical & Subtropical Moist Broadleaf Forests which receives large amounts of organic inputs). We conclude that sugarcane influence methane concentrations and fluxes in tropical streams by reducing the organic matter availability provided by the native vegetation in soil and water.


Subject(s)
Methane , Rivers , Agriculture , Carbon Dioxide , Forests , Rivers/chemistry , Water
2.
Arch Environ Contam Toxicol ; 82(1): 131-141, 2022 Jan.
Article in English | MEDLINE | ID: mdl-34797381

ABSTRACT

Pesticides can cause harmful effects to aquatic communities, even at concentrations below the threshold limit established as guidelines for the water bodies by environmental agencies. In this research, an input of the herbicide 2,4-dichlorophenoxyacetic acid (i.e., 2,4-D) was simulated under controlled conditions in a 500-m-long reach of a first-order tropical stream in Southeastern Brazil. Two water samplings at eight stations investigated the stream longitudinal contamination profile. The ecotoxicological effects were analyzed using Eruca sativa L. seed germination assays and the acute and chronic toxicity tests with the neotropical cladoceran Ceriodaphnia silvestrii. Physicochemical parameters of water quality were evaluated to characterize the study area and quantify 2,4-D concentrations along the stream to assess pesticide retention. The 2,4-D concentration was reduced by approximately 50% downstream in the samplings, indicating that the herbicide was retained along the stream. Moreover, C. silvestrii reproduction in long-term assays decreased approximately 50% in the stations with higher concentrations of 2,4-D than the laboratory control. After contamination, E. sativa L. showed a lower average root growth (1.0 cm), statistically different from the control (2.2 cm). On the other hand, similar growth values were obtained among the background and the most downstream stations. Our study highlighted the relevance of reviewing and updating herbicide guidelines and criteria to prevent possible ecological risks.


Subject(s)
Cladocera , Pesticides , Water Pollutants, Chemical , 2,4-Dichlorophenoxyacetic Acid/toxicity , Animals , Toxicity Tests, Chronic , Water Pollutants, Chemical/toxicity
3.
Eng. sanit. ambient ; 24(2): 391-402, mar.-abr. 2019. tab, graf
Article in Portuguese | LILACS-Express | LILACS | ID: biblio-1012044

ABSTRACT

RESUMO A sonda solúvel flutuante (SSF) é considerada uma técnica de baixo custo para a estimativa do coeficiente de transferência de massa de oxigênio na interface ar-água (KL). Essa técnica se baseia no fato que KL pode ser correlacionado com a velocidade de dissolução do sólido solúvel (VS), uma vez que ambos os parâmetros são influenciados pela turbulência na superfície do escoamento. O objetivo do presente estudo consistiu em calibrar uma nova configuração da SSF. Experimentos de reaeração superficial e dissolução da sonda solúvel foram realizados em dois aparatos experimentais (tanque agitado por jatos e um canal hidráulico circular), de modo que diferentes níveis de turbulência foram produzidos. Os resultados mostraram forte correlação entre KL e VS; r = 0,953 para experimentos realizados no tanque e r = 0,895 para experimentos realizados no canal. A nova configuração da SSF forneceu razão KL.VS -1 crescente em função do número de Reynolds, indicando que a relação entre os dois parâmetros é dependente da turbulência. Conclui-se que a técnica SSF possui elevado potencial. Entretanto, para que se possa atribuir utilidade definitiva, verificações em cursos d'água naturais e em equipamentos com estrutura de turbulência diferentes das utilizadas neste estudo ainda são necessárias.


ABSTRACT The floating solid soluble probe is a low-cost technique for estimating the mass transfer coefficient of oxygen in the air-water interface (Ka). This technique is based on the fact that Ka can be correlated with the dissolution rate of a soluble solid (VS), since both parameters are influenced by the surface turbulence. The aim of this study was to calibrate a new floating solid soluble probe configuration. Surface reaeration experiments and dissolution of the soluble solid probe were performed in two experimental apparatus (jets stirred tank and a circular hydraulic channel), in which different levels of turbulence were produced. The results showed a strong correlation between Ka and VS, r = 0.953 for experiments performed on the tank and r = 0.895 for experiments performed on the channel. The new floating solid soluble probe configuration provided an increasing Ka.VS -1 ratio as a function of the Reynolds number, indicating that the relationship between these two parameters depends on the surface turbulence. We conclude that the floating solid soluble probe technique has a high potential, despite calibrations in natural water bodies and equipment with a turbulence structure different from those used in this study are still necessary to definitive utility.

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