Systematic evaluation of sample preparation for fractionation of phytohormone salicylic acid in fresh leaves.

The determination of salicylic acid (SA), an important phytohormone responsible for stress signaling in plants, is of great importance in agricultural studies. However, a critical evaluation of the procedures for the extraction of the analytes and hydrolysis of the conjugated forms of SA is lacking in the literature and the available alternatives are complex, time-consuming, and laborious. In this study, the sample preparation methods for SA fractionation were critically evaluated to develop a simpler and faster alternative procedure. Microwave-assisted extractions were carried out with 2.0 g of fresh leaves and 8.0 mL of a 75% v/v ethanol:water solution at 40 °C for 10 min, followed by alkaline hydrolysis using 100 µL of 0.1 mol L-1 NaOH at 80 °C for 60 min. Free and total SA were determined in crude and hydrolyzed extracts, respectively, by fluorimetry after chromatographic separation of the sample matrix under isocratic elution (25% v/v acetonitrile/phosphate buffer) using a C18 column. Recovery experiments using methyl salicylate and acetylsalicylic acid model compounds demonstrated that the soft microwave-assisted extraction did not decompose the SA derivatives and that alkaline hydrolysis was quantitative. The proposed procedure was successfully applied for fractionation of SA in sugarcane, corn, and soybean leaves with extraction and hydrolysis yields up to 70 and 20% higher than those achieved in previously proposed approaches, respectively. The developed procedure is a simple, fast, and reliable alternative for SA fractionation in crude extracts without sample clean-up, and utilizes dilute reagents and green solvents.

Structural Modifications and Solution Behavior of Hyaluronic Acid Degraded with High pH and Temperature.

Hyaluronic acid (HA) is a macromolecule with valuable benefits over its range of molar masses (MM). Degradation studies are relevant to maintain the same purity level in biomedical studies when using HA of different MM. We degraded HA via high pH and temperature and evaluated its MM, solution behavior, and structure over time. After 24 h, low MM HA was predominant, and the MM decreased from 753 to 36.2 kDa. Dynamic light scattering (DLS) showed a decrease in the number of HA populations, and the solution tended to be less polydispersed. The zeta potential varied from - 10 to - 30 mV, close to the stable range. FTIR showed that the primary structure of HA was affected after only 48 h of reaction. These results are relevant for the production of low MM HA to be used or mixed with high MM HA, generating structured biomaterials for biomedical applications.

Environmental impacts caused by cemeteries and crematoria, new funeral technologies, and preferences of the Northeastern and Southern Brazilian population as for the funeral process.

Cemeteries and crematoria are the main funeral ways used in the world nowadays. It is a little-studied segment in the present days, mainly as for the possible environmental impacts in the environment, such as those derived from dental amalgam, prostheses, and dioxins, among other. This article aimed to identify the environmental impacts caused by cemeteries and crematoria and to point out new trends in funeral processes such as freeze-drying and alkaline hydrolysis. The study is justified due to the large part of the Brazilian population that do not know the environmental impacts caused by cemeteries and crematoria, as well as to bring information about the new processes. For that, a research was carried out with 400 people. The main results show that among all the funeral processes, the new freeze-drying process was opted by 33% of the sample. We also identified that the main reasons for choosing the funeral process were less environmental impact (28%), no after-death expenses (grave payment) (16.1%), and the possibility of putting away or throwing away the remains wherever you want (14.9%). Finally, new funeral processes were well accepted by the Brazilian population-those who were interviewed-due to their benefits.

Fast and sensitive collagen quantification by alkaline hydrolysis/hydroxyproline assay.

A preparative protein alkaline hydrolysis procedure, as part of a spectrophotometric collagen quantification method, is presented. The procedure is suitable for small amounts of fresh solid or liquid samples. Various aspects of the procedure, such as the NaOH concentration, time needed to hydrolyse different collagen contents, buffer strength of the reagent solution, pH control of the hydrolysate and spectrophotometric conditions, were evaluated. Compared to other procedures that use alkaline hydrolysis, the sensitivity of this procedure was increased by a factor of 5. Compared to the conventionally used Association of Official Analytical Chemists (AOAC) acid hydrolysis method, the reaction time was reduced from 16 h to 40 min and the amount of sample from 4 g to 3-20 mg, producing equivalent results when applied to porcine liver and sausage samples.

Propolis obtained by means of alkaline hydrolysis and action on Staphylococcus aureus / Própolis obtida por hidrolise alcalina e ação sobre Staphylococcus aureus

The Brazilian propolis is investigated for its antibacterial properties. The aim of this work was to establish the extraction and purification method to display the antibacterial activity. Propolis of Apis mellifera was obtained from bee hives cultivated in Parana State, Brazil. In this study, we used ATCC 25923 Staphylococcus aureus strains and 158 Staphylococcus aureus strains isolated from cows with clinical mastitis. Extraction and partial purification: Several fractions were obtained during the partial purification: a crude ethanolic extract of propolis, a resinous material in ethanolic solution and an alkaline hydrolysis water-soluble compounds solution. The results show that the alkaline hydrolysis water-soluble compounds solution had a minimal inhibitory concentration of approximately 155.46 µg/mL for Staphylococcus aureus. In this work, we obtained an aqueous solution of organic compounds extracted from Apis mellifera propolis that bears physical-chemical and biological characteristics capable to inhibit the proliferation of Gram-positive bacteria.

A própolis brasileira é investigada por suas propriedades antibacterianas. O objetivo deste trabalho foi estabelecer o método de extração e purificação para demonstrar a atividade antibacteriana. A própolis de Apis mellifera foi obtida de colméias de abelhas oriundas do Estado do Paraná, Brasil. Neste estudo, foram usados cepas de Staphylococcus aureus ATCC 25923 e 158 cepas de Staphylococcus aureus isolados de vacas com mastite clínica. Várias frações foram obtidas durante a purificação parcial: um extrato etanólico bruto de própolis, um material resinoso em solução alcoólica e uma solução de compostos solúveis por hidrólise alcalina em água. Os resultados mostram que a solução de compostos solúveis por hidrólise alcalina em água apresentou uma concentração inibitória mínima de cerca de 155,46 mg/mL para Staphylococcus aureus. Neste trabalho foi obtida uma solução aquosa de compostos orgânicos extraídos da própolis de Apis mellifera que possui características físico-químicas e biológicas capazes de inibir a proliferação de bactérias Gram positivas.

A model to explain high values of pH in an alkali sodic soil

For alkali sodic soils (pH>8.5), the "hydrolysis of exchangeable sodium" has been used as a possible explanation for the alkalinity production and rise in pH of these soils. As an alternative to this hypothesis, a model was developed to simulate and to explain that the alkalinity production and rise in pH is possible in a soil that accumulates alkaline sodium salts and CaCO3. Several simulations were performed by using different combinations of CO2 partial pressures (P), presence or absence of MgCO3, along with experimental values of exchangeable sodium percentage (ESP) and ion concentrations in saturation extracts from an alkali sodic soil (named Pantanal). A hypothetical system with similar conditions to the Pantanal soil but with a Gapon selectivity coefficient (KG) of 0.01475 (mmol L-1)-1/2 was also considered. Good agreement was obtained between experimental and predicted values for pH and ion concentrations in the soil solution when the model (without MgCO3) was applied to the Pantanal soil. However, KG values calculated for the Pantanal soil were generally higher than 0.01475 (mmol L-1)-1/2. Moreover, high pH values and elevated ionic strength were obtained when a KG of 0.01475 (mmol L-1)-1/2 was used at high ESP (similar to those found in the Pantanal soil). KG values obtained for the Pantanal soil and the results obtained in the simulation of the hypothetical system are suggesting that a value higher than 0.01475 (mmol L-1)-1/2 should be used to adequately simulate the behavior of the Pantanal soil at low ionic strength and high ESP values.

Em solos alcalino sódicos (pH>8,5), a "hidrólise de sódio trocável" tem sido usada como uma possível explicação para a produção de álcali e elevação do pH nestes solos. Como uma alternativa a essa hipótese, um modelo foi desenvolvido para simular e explicar que a produção de álcali e elevação do pH é possível num solo que acumula sais alcalinos de sódio e CaCO3. Várias simulações foram feitas fazendo uso de diferentes combinações da pressão parcial de CO2 (P), presença ou ausência de MgCO3, com valores experimentais da porcentagem de sódio trocável (ESP) e concentrações de íons em extratos de saturação de um solo sódico alcalino (chamado Pantanal). Um sistema hipotético com condições similars ao solo Pantanal mas com um coeficiente de selectividade de Gapon (KG) de 0,01475 (mmol L-1)-1/2 foi, também, considerado. Boa concordância foi obtida entre os valores experimentais e os predezidos para o pH e concentração de íons na solução do solo quando o modelo (sem MgCO3) foi aplicado ao solo Pantanal. Porém, valores de KG calculados para o solo Pantanal estiveram muito acima de 0,01475 (mmol L-1)-1/2. Além disso, elevados valores de pH e da força iónica foram obtidos quando o KG de 0,01475 (mmol L-1)-1/2 foi usado a altos ESP. Valores de KG obtidos para o solo Pantanal e os resultados achados na simulação do sistema hipotético sugerem que um valor maior de 0,01475 (mmol L-1)-1/2 poderia ser empregado adequadamente para simular o comportamento do solo Pantanal a baixa força iônica e altos valores de ESP.

A model to explain high values of pH in an alkali sodic soil

For alkali sodic soils (pH>8.5), the "hydrolysis of exchangeable sodium" has been used as a possible explanation for the alkalinity production and rise in pH of these soils. As an alternative to this hypothesis, a model was developed to simulate and to explain that the alkalinity production and rise in pH is possible in a soil that accumulates alkaline sodium salts and CaCO3. Several simulations were performed by using different combinations of CO2 partial pressures (P), presence or absence of MgCO3, along with experimental values of exchangeable sodium percentage (ESP) and ion concentrations in saturation extracts from an alkali sodic soil (named Pantanal). A hypothetical system with similar conditions to the Pantanal soil but with a Gapon selectivity coefficient (KG) of 0.01475 (mmol L-1)-1/2 was also considered. Good agreement was obtained between experimental and predicted values for pH and ion concentrations in the soil solution when the model (without MgCO3) was applied to the Pantanal soil. However, KG values calculated for the Pantanal soil were generally higher than 0.01475 (mmol L-1)-1/2. Moreover, high pH values and elevated ionic strength were obtained when a KG of 0.01475 (mmol L-1)-1/2 was used at high ESP (similar to those found in the Pantanal soil). KG values obtained for the Pantanal soil and the results obtained in the simulation of the hypothetical system are suggesting that a value higher than 0.01475 (mmol L-1)-1/2 should be used to adequately simulate the behavior of the Pantanal soil at low ionic strength and high ESP values.

Em solos alcalino sódicos (pH>8,5), a "hidrólise de sódio trocável" tem sido usada como uma possível explicação para a produção de álcali e elevação do pH nestes solos. Como uma alternativa a essa hipótese, um modelo foi desenvolvido para simular e explicar que a produção de álcali e elevação do pH é possível num solo que acumula sais alcalinos de sódio e CaCO3. Várias simulações foram feitas fazendo uso de diferentes combinações da pressão parcial de CO2 (P), presença ou ausência de MgCO3, com valores experimentais da porcentagem de sódio trocável (ESP) e concentrações de íons em extratos de saturação de um solo sódico alcalino (chamado Pantanal). Um sistema hipotético com condições similars ao solo Pantanal mas com um coeficiente de selectividade de Gapon (KG) de 0,01475 (mmol L-1)-1/2 foi, também, considerado. Boa concordância foi obtida entre os valores experimentais e os predezidos para o pH e concentração de íons na solução do solo quando o modelo (sem MgCO3) foi aplicado ao solo Pantanal. Porém, valores de KG calculados para o solo Pantanal estiveram muito acima de 0,01475 (mmol L-1)-1/2. Além disso, elevados valores de pH e da força iónica foram obtidos quando o KG de 0,01475 (mmol L-1)-1/2 foi usado a altos ESP. Valores de KG obtidos para o solo Pantanal e os resultados achados na simulação do sistema hipotético sugerem que um valor maior de 0,01475 (mmol L-1)-1/2 poderia ser empregado adequadamente para simular o comportamento do solo Pantanal a baixa força iônica e altos valores de ESP.