Two new species of Crawfordia Pierce from South America, (Strepsiptera: Stylopidae)

Several stylopized specimens were found among the Hymenoptera collection of the Instituto Oswaldo Cruz (Rio de Janeiro, Brazil). A paper by Kogan & Oliveira (1966) described the parasites of Polybia represented among those specimens. I describe herein the first neotropical species of the genus Crawfordia parasitizing species of Psaenithia (Andrenidae, Panurgini). The presence of vestigial thoracic segmentation of the female cephalothorax is a peculiar trait of this genus of Strepsiptera. Triungulinids are described in detail for the first time in this genus.

Permanent demand excess as business strategy: an analysis of the Brazilian higher-education market

Many Higher Education Institutions (HEIs) establish tuition below the equilibrium price to generate permanent demand excess. This paper first adapts Becker’s (1991) theory to understand why the HEIs price in this way. The fact that students are both consumers and inputs on the education production process gives rise to a market equilibrium where some firms have excess demand and charge high prices, and others charge low prices and have empty seats.Second, the paper analyzes this equilibrium empirically. We estimated the demand for undergraduate courses in Business Administration in the State of São Paulo. The results show that tuition, quality of incoming students and percentage of lecturers holding doctorates degrees are the determining factors of students’ choice. Since the student quality determines the demand for a HEI, it is calculated what the value is for a HEI to get better students; that is the total revenue that each HEI gives up to guarantee excess demand. Regarding the “investment” in selectivity, 39 HEIs in São Paulo give up a combined R$ 5 million (or US$ 3.14 million) in revenue per year per freshman class, which means 7.6% of the revenue coming from a freshman class.

Propriedades cristalográficas de caulinitas de solos do ambiente tabuleiros costeiros, Amazônia e Recôncavo Baiano

Grande parte das propriedades e características dos solos estão relacionadas à quantidade e ao tipo de mineral na fração argila. Os objetivos deste trabalho foram caracterizar a fração argila e estudar as características cristalográficas das caulinitas de solos vermelhos e amarelos, visando ao entendimento das relações desse mineral com as características e propriedades dos solos dominantes na região dos Tabuleiros Costeiros e mais interioranos do Brasil. Para isso, determinou-se a relação argila grossa/argila fina e foram realizadas análises mineralógicas (qualitativa e quantitativa) por meio de DRX e aplicação do método Rietveld; caracterização espectral por ERD, para determinação da relação hematita/goethita; estimativa de propriedades cristalográficas (tamanho e microtensões), por DRX e utilizando modelos matemáticos; da superfície específica, por BET-N2; da fractalidade; do grau de desordem estrutural, por diversos índices; e análises de microscopia eletrônica de transmissão. Os resultados permitiram as seguintes conclusões: (a) a quantificação dos minerais de argila pelo método Rietveld revelou predomínio marcante das caulinitas em todos os solos estudados; (b) a análise dos espectros de DRX, aplicando-se o método Rietveld, sugere a coexistência de caulinitas triclínicas e caulinitas com caráter monoclínico; (c) as caulinitas menores que 0,2 µm de todos os solos foram similares em superfície específica BET-N2, dimensão média do cristalito no plano (001), grau de desordem estrutural e dimensão fractal, mas diferentes em sua morfologia, que se apresentou correlacionada com o material de origem.

Numerical modeling of the effect of variation of boundary conditions on vadose zone hydraulic properties

An accurate estimation of hydraulic fluxes in the vadose zone is essential for the prediction of water, nutrient and contaminant transport in natural systems. The objective of this study was to simulate the effect of variation of boundary conditions on the estimation of hydraulic properties (i.e. water content, effective unsaturated hydraulic conductivity and hydraulic flux) in a one-dimensional unsaturated flow model domain. Unsaturated one-dimensional vertical water flow was simulated in a pure phase clay loam profile and in clay loam interlayered with silt loam distributed according to the third iteration of the Cantor Bar fractal object Simulations were performed using the numerical model Hydrus 1D. The upper and lower pressure heads were varied around average values of -55 cm for the near-saturation range. This resulted in combinations for the upper and lower constant head boundary conditions, respectively, of -50 and -60 cm, -40 and -70 cm, -30 and -80 cm, -20 and -90 cm, and -10 and -100 cm. For the drier range the average head between the upper and lower boundary conditions was set to -550 cm, resulting in the combinations -500 and -600 cm, -400 and -700 cm, -300 and -800 cm, -200 and -900 cm, and -100 and -1,000 cm, for upper and lower boundary conditions, respectively. There was an increase in water contents, fluxes and hydraulic conductivities with the increase in head difference between boundary conditions. Variation in boundary conditions in the pure phase and interlayered one-dimensional profiles caused significant deviations in fluxes, water contents and hydraulic conductivities compared to the simplest case (a head difference between the upper and lower constant head boundaries of 10 cm in the wetter range and 100 cm in the drier range).