Erosion of the nocturnal boundary layer in the central Amazon during the dry season

In this study, the erosion of the nocturnal boundary layer (NBL) was analyzed in the central Amazon during the dry season of 2014, using data from the GoAmazon 2014/5 Project and high-resolution model outputs (PArallelized Les Model - PALM). The dataset consisted of in situ (radiosonde) and remote sensing instruments measurements (Ceilometer, Lidar, Wind Profiler, microwave radiometer, and SODAR). The results showed that the NBL erosion occurred, on average, two hours after sunrise (06:00 local time), and the sensible heat flux provided more than 50% of the sensible heating necessary for the erosion process to occur. After the erosion, the convective phase developed quickly (175.2 m h-1). The measurements of the remote sensors showed that the Ceilometer, in general, presented satisfactory results in relation to the radiosondes for measuring the height of the planetary boundary layer. The PALM simulations represented well the NBL erosion, with a small underestimation (≈ 20 m) at the beginning of this phase. In the final phase of NBL erosion and in the initial stage of the development of the convective boundary layer (CBL), the model presented satisfactory results, with heights of CBL ranging from 800 m to 1,650 m, respectively. (AU)

Evaluation of impaired left ventricular relaxation with normal ejection fraction by kinetic energy of blood flow in early diastole / 中华超声影像学杂志

Objective To evaluate the left ventricular(LV) impaired relaxation(IR) by kinetic energy of blood flow in early diastole (Ek) in patients with normal ejection fraction(EF).Methods 42 patients with impaired LV relaxation while normal EF (IR group) and 38 controls volunteers with normal LV relaxation (NR group) underwent conventional echocardiography and real-time three-dimensional echocardiography (RT-3DE).Pulsed-wave (PW) Doppler imaging and PW tissue Doppler imaging (PWTDI) were performed in all the subjects.PW Doppler imaging indices included peak E velocities (VE),peak A velocities (VA) and VE/VA.PW-TDI indices included velocities of septal and lateral sides of the mitral annulus in early diastole Se',Le'),then the average of Se' and Le' described as e') were calculated.RT3DE indices included end diastolic volume EDV),ejection fraction EF) and flow volume of peak E QE).Results There were significant difference between Ek of two groups P ＜0.05).There were significant positive correlation between Ek and e' in both the two groups P ＜0.05).And Ek was less influenced by age or systolic blood pressure.Area under curve of the ROC of Ek was 0.654,sensitivity was 63.2 ％ and specificity was 61.9％,respectively.And the specificity of Ek was higher than that of e' and VE/VA.Conclusions Ek was less influenced by age or afterload,which can be used to detect impaired LV relaxation.

Kinetic Energy of Emerging Neutrons Produced by Photodisintegration in a Medical Linear Accelerator / Energía cinética de neutrones emergentes producidos por fotodesintegración en un acelerador médico lineal

When a gamma photon interacts with a target nucleus a nuclear reaction can be generated, producing as a consequence the expulsion of particles from the atomic nucleus, this process is called photodisintegration. For this work, are of interest nuclear reactions of photodisintegration in which neutrons are ejected due to the interaction of photons with atomic nuclei of different materials in a linear accelerator for medical use. In this paper, the kinetic energy of photoneutrons produced by interactions with atomic nuclei of 184W, 63Cu, 27Al and 12C, which are some of the materials that constitute the head of a medical linear accelerator, is calculated. Also, the nuclei present in the construction materials of the room and the maze of the accelerator, such as, 23Na, 40Ca and 28Si, as also in the human body, ²H, 14N and 16O, are considered. It derives an exact theoretical expression, which has a linear dependence of the energy of the produced neutrons relative to the incident photon energy. It is found that, in the majority of cases, just photons with energies above 10 MV contribute to the production of neutrons. The values calculated from the expression obtained in this work are in good agreement with those reported in the literature, that are obtained by other approaches.

Cuando un fotón gamma interactúa con un núcleo blanco una reacción nuclear puede ser generada, produciendo como consecuencia la expulsión de partículas del núcleo atómico, este proceso se denomina fotodesintegración. Para este trabajo, son de interés las reacciones nucleares de fotodesintegración en las que los neutrones son expulsados debido a la interacción de los fotones con los núcleos atómicos de diferentes materiales en un acelerador lineal para uso médico. En este trabajo, la energía cinética de fotoneutrones producidos por la interacción con los núcleos atómicos de 184 W, 63 Cu, 27 Al y 12 C, que son algunos de los materiales que constituyen el cabezal de un acelerador lineal médico, es calculada. Además, los núcleos presentes en los materiales de construcción de la sala y el laberinto del acelerador, como por ejemplo, 23Na, 40Ca y 28Si, como también en el cuerpo humano, ²H, 14N y 16O, son considerados. Se obtiene una expresión exacta teórica, la cual tiene una dependencia lineal de la energía de los neutrones producidos en relación a la energía del fotón incidente. Se ha encontrado que, en la mayoría de los casos, sólo los fotones con energías por encima de 10 MV contribuyen a la producción de neutrones. Los valores calculados a partir de la expresión obtenida en este trabajo están en buen acuerdo con los reportados en la literatura, los cuales se obtienen mediante otros métodos.

Erosividade e características da chuva correlacionadas com perdas de solo em Alagoinha - PB / Erosivity, rain characteristics and soil losses at Alagoinha, state of Paraíba, Brazil

Visando estabelecer o parâmetro da chuva quemelhor expresse a sua capacidade potencial de causar erosão, foram estudadas, para o período de 1981 a 1989, correlações lineares simples entre 13 características da chuva e as perdas de solo provocadas por erosão hídrica em solo classificado como Terra Roxa Estruturada localizada na Estação Experimental de Alagoinha, Paraíba, pertencente a Empresa Estadual de Pesquisa Agropecuária da Paraíba. As características da chuva testadas como estimadores da erosividade foram: quantidade de chuva;energia cinética total; segmentos de chuva com energia cinética igual ou superior a 25 mm/h; intensidades máximas de chuva em 5, 10, 15, 30 e 60 minutos; produto da energia cinética total pelas intensidades máximas em 5, 10, 15, 30 e 60 minutos. As correlações obtidas indicam que a característica da chuva produto da energia cinética total pela intensidade máxima em 15 minutos é a que melhor se correlaciona com as perdas de solo na região em estudo; entretanto, não houve diferença significativa entre as características produto da energia cinética total pela intensidade máxima em 15 minutos e produto da energia cinética total pela intensidade máxima em 30 minutos. O valor médio anual para a precipitação em Alagoinha - PB no período de 1981 a 1989 foi de 3423 MJ.mm/ha.h.

The objective of this study was to establish a rain parameter that can be used to express the potential capability of the rain to cause soil erosion. Datafrom 1981 to 1989 were used in simple linear corre letions among 13 rain characteristics and soil tosses using individual erosive rains in an Alfisol soil of Alagoinha Experimental Station of "Empresa Estadual de Pesquisa Agropecuária", State of Paraíba, Brazil. The rain characteristics tested were: total precipitation; total kinetic energy; kinetic energy higher than 25 milimeters ; rain intensity at 5, 10, 15, 30 and 60 minutes; product between kinetic energy and rain intensity at 5, 10, 15, 30 and 60 minutes. The corre lations obtained among rain characteristics and soil tosses, indicated that the rain characteristic energy-intensity in 15 minutes is better correlated to soil losses. However, there was no difference between energy-intensity in 15 minutes and energy-intensity in 30 minutes characteristics. The médium year value of the erosivity (EI30) obtained for Alagoinha during the studied period was 3.423 MJ.mm/ha, h.