Influência do butorfanol sobre os períodos de latência e de ação da ropivacaína pela via peridural na ovariossalpingo-histerectomia em cadelas

Avaliaram-se os períodos de latência e de duração do efeito do butorfanol associado à ropivacaína aplicados pela via peridural e a possibilidade de uso dessa associação como protocolo anestésico para realização de ovariossalpingo-histerectomia (OSH) em cadelas. Utilizaram-se 16 cadelas pré-medicadas com acepromazina e midazolam compondo dois grupos: no grupo 1 (n=8) aplicou-se ropivacaína isolada (0,3mL/kg) e no grupo 2 (n=8), butorfanol (0,1mg/kg) e ropivacaína (até o volume de 0,3mL/kg), pela via peridural. Consideraram-se nove momentos (M): M0 - animal sem anestesia, M1 - 15 minutos após medicação pré-anestésica; M2 - 30 minutos após a aplicação peridural; M3, M4 e M5 - correspondentes ao início do procedimento e ao pinçamento dos pedículos esquerdo e direito, respectivamente; M6 - ligadura da cérvix uterina; e M7 e M8 - início da laparorrafia e fim da sutura de pele, respectivamente. Foram avaliados os períodos de latência e ação do bloqueio, além da viabilidade de realização do procedimento cirúrgico por meio do bloqueio efetuado. O que recebeu ropivacaína + butorfanol apresentou sedação pronunciada e permitiu a realização de OSH em 75% dos animais, sem indução anestésica. Não houve diferença entre os grupos quanto aos períodos de latência e duração. A associação do butorfanol à ropivacaína proporcionou bloqueio anestésico compatível com a realização de OSH e período de latência curto, com duração de efeito suficiente para o procedimento cirúrgico

Spatial variability of physical and chemical attributes of some forest soils in southeastern of Brazil

Capão Bonito forest soils, São Paulo state, Brazil, have been used for forestry purposes for almost one century. Detailed knowledge about the distribution of soil attributes over the landscape is of fundamental importance for proper management of natural resources. The purpose of this study was to identify the variability and spatial dependence of chemical and physical attributes of Capão Bonito forest soils. A large soil database of regional land was raised and organized. Most of the selected variables were close to the lognormal frequency range. Soil texture presented a higher range in the A horizon, and the nugget effect and sill were greater in the B horizon. These differences are attributed to the parent material of the region (Itararé Geologic Formation), which presents uneven distribution of sediments. Chemical attributes related to soil fertility presented a higher spatial dependence range in the B horizon, probably as a result of more intensive management and erosion history of the superficial soil layer. Maps for some attributes were interpolated. These had specific areas of occurrence and a wide distribution along the perimeter of the Capão Bonito District Forest, allowing a future site-specific soil management

Protein kinase Cδ protects against bile acid apoptosis by suppressing proapoptotic JNK and BIM pathways in human and rat hepatocytes

Retained bile acids, which are capable of inducing cell death, activate protein kinase Cδ (PKC-δ) in hepatocytes. In nonhepatic cells, both pro- and antiapoptotic effects of PKC-δ are described. The aim of this study was to determine the role of PKC-δ in glycochenodeoxycholate (GCDC)-induced apoptosis in rat hepatocytes and human HUH7-Na-taurocholate-cotransporting polypeptide (Ntcp) cells. Apoptosis was monitored morphologically by Hoechst staining and biochemically by immunoblotting for caspase 3 cleavage. The role of PKC-δ was evaluated with a PKC activator (phorbol myristate acetate, PMA) and PKC inhibitors (chelerythrine, H-7, or calphostin), PKC-δ knockdown, and wild-type (WT) or constitutively active (CA) PKC-δ. PKC-δ activation was monitored by immunoblotting for PKC-δ Thr505 and Tyr311 phosphorylation or by membrane translocation. JNK and Akt phosphorylation and the amount of total bisindolylmaleimide (BIM) were determined by immunoblotting. GCDC induced the translocation of PKC-δ to the mitochondria and/or plasma membrane in rat hepatocytes and HUH7-Ntcp cells and increased PKC-δ phosphorylation on Thr505, but not on Tyr311, in HUH7-Ntcp cells. GCDC-induced apoptosis was attenuated by PMA and augmented by PKC inhibition in rat hepatocytes. In HUH-Ntcp cells, transfection with CA or WT PKC-δ attenuated GCDC-induced apoptosis, whereas knockdown of PKC-δ increased GCDC-induced apoptosis. PKC-δ silencing increased GCDC-induced JNK phosphorylation, decreased GCDC-induced Akt phosphorylation, and increased expression of BIM. GCDC translocated BIM to the mitochondria in rat hepatocytes, and knockdown of BIM in HUH7-Ntcp cells decreased GCDC-induced apoptosis. Collectively, these results suggest that PKC-δ does not mediate GCDC-induced apoptosis in hepatocytes. Instead PKC-δ activation by GCDC stimulates a cytoprotective pathway that involves JNK inhibition, Akt activation, and downregulation of BIM

Spatial variability of maximum annual daily rain under different return periods at the Rio de Janeiro state, Brazil

Knowledge of maximum daily rain and its return period in a region is an important tool to soil conservation, hydraulic engineering and preservation of road projects. The objective of this work was to evaluate the spatial variability of maximum annual daily rain considering different return periods, at the Rio de Janeiro State. The data set was composed by historical series of 119 rain gauges, for 36 years of observation. The return periods, estimated by Gumbel distribution, were 2, 5, 10, 25, 50 and 100 years. The spatial variability of the return periods was evaluated by semivariograms. All the return periods presented spatial dependence, with exponential and spherical model fitted to the experimental semivariograms. The parameters of the fitted semivariogram model were very similar; however, it was observed the presence of higher nugget effects for semivariograms of longer return periods. The values of maximum annual daily average rain in all the return periods increased from north to south and from countryside to the coast. In the region between the Serra do Mar range and the coast, besides increasing in magnitude, an increase in the spatial variability of the studied values with increasing return periods was also noticed. This behavior is probably caused by the orographic effect. The interpolated maps were more erratic for higher return periods and at the North, Northeast and Coastal Plain regions, in which the installation of new pluviometric stations are recommended