Aging and the lateralization of oscillatory activities related to external and internal motor preparation

Selection of action may rely on external guidance or be motivated internally, engaging partially distinct cerebral networks. With age, there is an increased allocation of sensorimotor processing resources, accompanied by a reduced differentiation between the two networks of action selection. The present study examines the age effects on the motor-related oscillatory patterns related to the preparation of externally and internally guided movements. Thirty-two older and 30 younger adults underwent three delayed motor tasks with S1 as preparatory and S2 as imperative cue: Full, laterality instructed by S1 (external guidance); Free, laterality freely selected (internal guidance); None, laterality instructed by S2 (no preparation). Electroencephalogram (EEG) was recorded using 64 surface electrodes. Motor-Related Amplitude Asymmetries (MRAA), indexing the lateralization of oscillatory activities, were analyzed within the S1-S2 interval in the mu (9-12 Hz) and low beta (15-20 Hz) motor-related frequency bands. Reaction times to S2 were slower in older than younger subjects, and slower in the Free than in the Full condition in older subjects only. In the Full condition, there were significant mu MRAA in both age groups, and significant low beta MRAA only in older adults. The Free condition was associated with large mu MRAA in younger adults and limited low beta MRAA in older adults. In younger subjects, the lateralization of mu activity in both Full and Free conditions indicated effective external and internal motor preparation. In older subjects, external motor preparation was associated with lateralization of low beta in addition with mu activity, compatible with an increase of motor-related resources. In contrast, absence of mu and limited low beta lateralization in internal motor preparation was concomitant with reaction time slowing and suggested less efficient cerebral processes subtending free movement selection in older adults, indicating reduced capacity for internally driven action with age.

Myocardial infarct size and mortality depend on the time of day-a large multicenter study.

BACKGROUND: Different studies have shown circadian variation of ischemic burden among patients with ST-Elevation Myocardial Infarction (STEMI), but with controversial results. The aim of this study was to analyze circadian variation of myocardial infarction size and in-hospital mortality in a large multicenter registry. METHODS: This retrospective, registry-based study was based on data from AMIS Plus, a large multicenter Swiss registry of patients who suffered myocardial infarction between 1999 and 2013. Peak creatine kinase (CK) was used as a proxy measure for myocardial infarction size. Associations between peak CK, in-hospital mortality, and the time of day at symptom onset were modelled using polynomial-harmonic regression methods. RESULTS: 6,223 STEMI patients were admitted to 82 acute-care hospitals in Switzerland and treated with primary angioplasty within six hours of symptom onset. Only the 24-hour harmonic was significantly associated with peak CK (p = 0.0001). The maximum average peak CK value (2,315 U/L) was for patients with symptom onset at 23:00, whereas the minimum average (2,017 U/L) was for onset at 11:00. The amplitude of variation was 298 U/L. In addition, no correlation was observed between ischemic time and circadian peak CK variation. Of the 6,223 patients, 223 (3.58%) died during index hospitalization. Remarkably, only the 24-hour harmonic was significantly associated with in-hospital mortality. The risk of death from STEMI was highest for patients with symptom onset at 00:00 and lowest for those with onset at 12:00. DISCUSSION: As a part of this first large study of STEMI patients treated with primary angioplasty in Swiss hospitals, investigations confirmed a circadian pattern to both peak CK and in-hospital mortality which were independent of total ischemic time. Accordingly, this study proposes that symptom onset time be incorporated as a prognosis factor in patients with myocardial infarction.

Thyroid hormone in biodegradable nerve guides stimulates sciatic nerve regeneration: a potential therapeutic approach for human peripheral nerve injuries.

It has been already demonstrated that thyroid hormone (T3) is one of the most important stimulating factors in peripheral nerve regeneration. We have recently shown that local administration of T3 in silicon tubes at the level of the transected rat sciatic nerve enhanced axonal regeneration and improved functional recovery. Silicon, however, cannot be used in humans because it causes a chronic inflammatory reaction. Therefore, in order to provide future clinical applications of thyroid hormone in human peripheral nerve lesions, we carried out comparative studies on the regeneration of transected rat sciatic nerve bridged either by biodegradable P(DLLA-(-CL) or by silicon nerve guides, both guides filled with either T3 or phosphate buffer. Our macroscopic observation revealed that 85% of the biodegradable guides allowed the expected regeneration of the transected sciatic nerve. The morphological, morphometric and electrophysiological analysis showed that T3 in biodegradable guides induces a significant increase in the number of myelinated regenerated axons (6862 +/- 1831 in control vs. 11799 +/- 1163 in T3-treated). Also, T3 skewed the diameter of myelinated axons toward larger values than in controls. Moreover, T3 increases the compound muscle action potential amplitude of the flexor and extensor muscles of the treated rats. This T3 stimulation in biodegradable guides was equally well to that obtained by using silicone guides. In conclusion, the administration of T3 in biodegradable guides significantly improves sciatic nerve regeneration, confirming the feasibility of our technique to provide a serious step towards future clinical application of T3 in human peripheral nerve injuries.

Fracture network characterization using hydrological and geophysical data

Les décisions de gestion des eaux souterraines doivent souvent être justiffées par des modèles quantitatifs d'aquifères qui tiennent compte de l'hétérogénéité des propriétés hydrauliques. Les aquifères fracturés sont parmi les plus hétérogènes et très difficiles à étudier. Dans ceux-ci, les fractures connectées, d'ouverture millimètrique, peuvent agir comme conducteurs hydrauliques et donc créer des écoulements très localisés. Le manque général d'informations sur la distribution spatiale des fractures limite la possibilité de construire des modèles quantitatifs de flux et de transport. Les données qui conditionnent les modèles sont généralement spatialement limitées, bruitées et elles ne représentent que des mesures indirectes de propriétés physiques. Ces limitations aux données peuvent être en partie surmontées en combinant différents types de données, telles que les données hydrologiques et de radar à pénétration de sol plus commun ément appelé géoradar. L'utilisation du géoradar en forage est un outil prometteur pour identiffer les fractures individuelles jusqu'à quelques dizaines de mètres dans la formation. Dans cette thèse, je développe des approches pour combiner le géoradar avec les données hydrologiques affn d'améliorer la caractérisation des aquifères fracturés. Des investigations hydrologiques intensives ont déjà été réalisées à partir de trois forage adjacents dans un aquifère cristallin en Bretagne (France). Néanmoins, la dimension des fractures et la géométrie 3-D des fractures conductives restaient mal connue. Affn d'améliorer la caractérisation du réseau de fractures je propose dans un premier temps un traitement géoradar avancé qui permet l'imagerie des fractures individuellement. Les résultats montrent que les fractures perméables précédemment identiffées dans les forages peuvent être caractérisées géométriquement loin du forage et que les fractures qui ne croisent pas les forages peuvent aussi être identiffées. Les résultats d'une deuxième étude montrent que les données géoradar peuvent suivre le transport d'un traceur salin. Ainsi, les fractures qui font partie du réseau conductif et connecté qui dominent l'écoulement et le transport local sont identiffées. C'est la première fois que le transport d'un traceur salin a pu être imagé sur une dizaines de mètres dans des fractures individuelles. Une troisième étude conffrme ces résultats par des expériences répétées et des essais de traçage supplémentaires dans différentes parties du réseau local. En outre, la combinaison des données de surveillance hydrologique et géoradar fournit la preuve que les variations temporelles d'amplitude des signaux géoradar peuvent nous informer sur les changements relatifs de concentrations de traceurs dans la formation. Par conséquent, les données géoradar et hydrologiques sont complémentaires. Je propose ensuite une approche d'inversion stochastique pour générer des modèles 3-D de fractures discrètes qui sont conditionnés à toutes les données disponibles en respectant leurs incertitudes. La génération stochastique des modèles conditionnés par géoradar est capable de reproduire les connexions hydrauliques observées et leur contribution aux écoulements. L'ensemble des modèles conditionnés fournit des estimations quantitatives des dimensions et de l'organisation spatiale des fractures hydrauliquement importantes. Cette thèse montre clairement que l'imagerie géoradar est un outil utile pour caractériser les fractures. La combinaison de mesures géoradar avec des données hydrologiques permet de conditionner avec succès le réseau de fractures et de fournir des modèles quantitatifs. Les approches présentées peuvent être appliquées dans d'autres types de formations rocheuses fracturées où la roche est électriquement résistive.

Análise do número de cerdas internas do órgão de Haller de larvas de Amblyomma nodosum Neumann (Acari, Ixodidae)

A partir de teleógina de Amblyomma nodosum Neumann, 1899, removida de Tamandua tetradactyla (Linnaeus, 1758) foram obtidas posturas que originaram larvas, em condições de laboratório. Um total de 219 larvas foi examinado em microscopia de luz, com objetiva de imersão e microscopia de confocal com varredura a laser. Buscou-se analisar a variação do número das cerdas internas dos lados direito e esquerdo, no fundo da cápsula do Órgão de Haller, com intuito de utilizá-las como um parâmetro quetotáxico na diagnose específica. A média do número de cerdas foi 5,06±0, 71, com valores limites da amplitude de 4-11.

The heat shock response in moss plants is regulated by specific calcium-permeable channels in the plasma membrane.

Land plants are prone to strong thermal variations and must therefore sense early moderate temperature increments to induce appropriate cellular defenses, such as molecular chaperones, in anticipation of upcoming noxious temperatures. To investigate how plants perceive mild changes in ambient temperature, we monitored in recombinant lines of the moss Physcomitrella patens the activation of a heat-inducible promoter, the integrity of a thermolabile enzyme, and the fluctuations of cytoplasmic calcium. Mild temperature increments, or isothermal treatments with membrane fluidizers or Hsp90 inhibitors, induced a heat shock response (HSR) that critically depended on a preceding Ca(2+) transient through the plasma membrane. Electrophysiological experiments revealed the presence of a Ca(2+)-permeable channel in the plasma membrane that is transiently activated by mild temperature increments or chemical perturbations of membrane fluidity. The amplitude of the Ca(2+) influx during the first minutes of a temperature stress modulated the intensity of the HSR, and Ca(2+) channel blockers prevented HSR and the onset of thermotolerance. Our data suggest that early sensing of mild temperature increments occurs at the plasma membrane of plant cells independently from cytosolic protein unfolding. The heat signal is translated into an effective HSR by way of a specific membrane-regulated Ca(2+) influx, leading to thermotolerance.

Twitch and M-wave potentiation induced by intermittent maximal voluntary quadriceps contractions: Differences between direct quadriceps and femoral nerve stimulation.

Introduction: To investigate differences in twitch and M-wave potentiation in the quadriceps femoris when electrical stimulation is applied over the quadriceps muscle belly versus the femoral nerve trunk. Methods: M-waves and mechanical twitches were evoked using direct quadriceps muscle and femoral nerve stimulation between 48 successive isometric maximal voluntary contractions (MVC) from 10 young, healthy subjects. Potentiation was investigated by analyzing the changes in M-wave amplitude recorded from the vastus medialis (VM) and vastus lateralis (VL) muscles and in quadriceps peak twitch force. Results: Potentiation of twitch, VM M-wave, and VL M-wave were greater for femoral nerve than for direct quadriceps stimulation (P<0.05). Despite a 50% decrease in MVC force, the amplitude of the M-waves increased significantly during exercise. Conclusions: In addition to enhanced electrogenic Na(+) -K(+) pumping, other factors (such as synchronization in activation of muscle fibers and muscle architectural properties) might significantly influence the magnitude of M-wave enlargement. © 2013 Wiley Periodicals, Inc.

Pólen coletado por Scaptotrigona depilis (Moure) (Hymenoptera, Meliponini), na região de Dourados, Mato Grosso do Sul, Brasil

Foram identificados os pólens coletados por operárias de Scaptotrigona depilis (Moure, 1942), na Região de Dourados-Ms, durante o período de setembro de 2006 a agosto de 2007. Ao todo foram coletados 42 tipos polínicos, sendo mais representativa em número de espécies, as famílias Myrtaceae (Eucalyptus spp.) e Mimosaceae. Os picos de valores de amplitude de nicho trófico (H') em Setembro (2,32), Novembro (2,29) e Outubro (2,02) mostraram que essa abelha pode ser generalista, dependendo da disponibilidade e características das fontes florais. Os valores de equitatividade (J'), também indicam maior uniformidade de uso das fontes florais durante esses meses de máxima amplitude de nicho. Os fatores ambientais (temperatura, umidade relativa e pluviosidade) não mostraram relação direta com a equitatividade e amplitude do nicho trófico. Estas variáveis parecem estar mais relacionadas com os ciclos diários ou sazonais de produção de pólen e néctar.

Colonic movements in healthy subjects as monitored by a Magnet Tracking System.

The Magnet Tracking System (MTS) is a minimally-invasive technique of continuous evaluation of gastrointestinal motility. In this study, MTS was used to analyse colonic propulsive dynamics and compare the transit of a magnetic pill with that of standard radio-opaque markers. MTS monitors the progress in real time of a magnetic pill through the gut. Ten men and 10 women with regular daily bowel movements swallowed this pill and 10 radio-opaque markers at 8 pm. Five hours of recordings were conducted during 2 following mornings. Origin, direction, amplitude and velocity of movements were analysed relative to space-time plots of the pill trajectory. Abdominal radiographs were taken to compare the progress of both pill and markers. The magnetic pill lay idle for 90% of its sojourn in the colon; its total retrograde displacement accounted for only 20% of its overall movement. Analysis of these movements showed a bimodal distribution of velocities: around 1.5 and 50 cm min(-1), the latter being responsible for 2/3 of distance traversed. There were more movements overall and more mass movements in males. Net hourly forward progress was greater in the left than right colon, and greater in males. The position of the magnetic pill correlated well with the advancement of markers. MTS showed patterns and propulsion dynamics of colonic segments with as yet unmet precision. Detailed analysis of slow and fast patterns of colonic progress makes it possible to specify the motility of colonic segments, and any variability in gender. Such analysis opens up promising avenues in studies of motility disorders.

O impacto da inovação na performance financeira das empresas

A inovação foi identificada como a principal causa do progresso dos países pelo seu impacto sobre o investimento, a produção, o emprego e no nível de bem-estar da população. Além disso, é de opinião geral que a inovação representa um papel essencial no desempenho económico-financeiro. Ficase, no entanto, muitas vezes, com a sensação de que esta afirmação se refere indistintamente ao crescimento económico no geral, à competitividade das economias nacionais, à concorrência, à rendibilidade, à sobrevivência e ao crescimento de empresas individuais. Por isso, é importante desenvolver pesquisas empíricas para ajudar a esclarecer como, quando, em que sentido, em que amplitude, a inovação é importante no desempenho económico-financeiro da empresa. Tendo esses aspectos presentes, nesta investigação, buscou-se contribuir para um melhor conhecimento destas questões, estabelecendo, assim, como objectivo principal analisar o impacto da inovação no desempenho financeiro das empresas industriais de São Vicente ao longo do período 2010-2013. A análise tem como quadro conceptual as abordagens actuais de referência sobre a temática da inovação e seu impacto no desempenho financeiro, desenvolvendo um suporte teórico, que permite identificar os factores determinantes da inovação no desempenho financeiro das empresas industriais de São Vicente. Para testar empiricamente as hipóteses em investigação e tendo em consideração a complexidade do fenómeno em questão, recorreu-se à análise estatística dos dados recolhidos com recurso ao software SPSS, onde fez-se uma análise univariada dos dados e para proceder à análise do impacto da inovação no desempenho financeiro das empresas inquiridas fez-se uma análise do Coeficiente de Correlação de Pearson. Os resultados obtidos mostram que existem uma associação estatisticamente significativa entre os níveis de investimentos e o desempenho financeiro das empresas da ilha de São Vicente, isto é, as inovações ao nível dos produtos tem tido impacto positivo muito irrisório nos indicadores financeiros, com excepção ao nível dos Activos Líquidos, Passivo. Contudo, registou-se um impacto negativo da inovação ao nível dos processos e das tecnologias, nos indicadores financeiros.

Combining heat stress and moderate hypoxia reduces cycling time to exhaustion without modifying neuromuscular fatigue characteristics.

PURPOSE: This study investigated the isolated and combined effects of heat [temperate (22 °C/30 % rH) vs. hot (35 °C/40 % rH)] and hypoxia [sea level (FiO2 0.21) vs. moderate altitude (FiO2 0.15)] on exercise capacity and neuromuscular fatigue characteristics. METHODS: Eleven physically active subjects cycled to exhaustion at constant workload (66 % of the power output associated with their maximal oxygen uptake in temperate conditions) in four different environmental conditions [temperate/sea level (control), hot/sea level (hot), temperate/moderate altitude (hypoxia) and hot/moderate altitude (hot + hypoxia)]. Torque and electromyography (EMG) responses following electrical stimulation of the tibial nerve (plantar-flexion; soleus) were recorded before and 5 min after exercise. RESULTS: Time to exhaustion was reduced (P < 0.05) in hot (-35 ± 15 %) or hypoxia (-36 ± 14 %) compared to control (61 ± 28 min), while hot + hypoxia (-51 ± 20 %) further compromised exercise capacity (P < 0.05). However, the effect of temperature or altitude on end-exercise core temperature (P = 0.089 and P = 0.070, respectively) and rating of perceived exertion (P > 0.05) did not reach significance. Maximal voluntary contraction torque, voluntary activation (twitch interpolation) and peak twitch torque decreased from pre- to post-exercise (-9 ± 1, -4 ± 1 and -6 ± 1 % all trials compounded, respectively; P < 0.05), with no effect of the temperature or altitude. M-wave amplitude and root mean square activity were reduced (P < 0.05) in hot compared to temperate conditions, while normalized maximal EMG activity did not change. Altitude had no effect on any measured parameters. CONCLUSION: Moderate hypoxia in combination with heat stress reduces cycling time to exhaustion without modifying neuromuscular fatigue characteristics. Impaired oxygen delivery or increased cardiovascular strain, increasing relative exercise intensity, may have also contributed to earlier exercise cessation.

Tertiary Himalayan structures and metamorphism in the Kulu Valley (Mandi-Khoksar transect of the Western Himalaya) - Shikar-Beh-nappe and crystalline nappe

The Crystalline Nappe of the High Himalayan Crystalline has been examined along the Kulu Valley and its vicinity (Mandi-Khoksar transect). This nappe was believed to have undergone deformation related only to its transport towards the SW essentially during the `'Main Central Thrust event''. New data has led to the conclusion that during the Himalayan orogeny, two distinctive phases, related to two opposite transport directions, characterize the evolution of this part of the chain, before the creation of the late NE-vergent backfolding. The first phase corresponds to an early NE-vergent folding and thrusting, creating the Tandi Syncline and the NE-oriented Shikar Beh Nappe stack, with a displacement amplitude of about 50 km. Two schistosities, together with a strong stretching lineation are developed at a deep tectonic level under amphibolite facies conditions (kyanite-staurolite-garnet-two mica schists). At a higher tectonic level and in the southern part of the section (Tandy Syncline and southern Kulu Valley between Kulu and Mandi) one or two schistosities are developed in the greenschist facies grade rocks (garnet-biotite and biotite schists). These structures and the associated Barrovian type metamorphism are all related to the NE-verging Shikar Beh Nappe. The creation of the NE-verging Shikar Beh Nappe may be explained by the reactivation of a SW dipping listric normal fault of the N Indian flexural passive margin, during the early stages of the Himalayan orogeny. In the second phase, the still hot metamorphic rocks of the Shikar Beh Nappe were folded and thrust towards the SW (mainly along the MBT and the MCT with a displacement in excess of 100 km) onto the cold, low-grade metamorphic rocks of the Larji-Kulu-Rampur Window or, near Mandi, on the non-metamorphic sandstones of the Ganges Molasse (Siwaliks). Sense of shear criteria and a strong NE-SW stretching-lineation indicate that the Crystalline Nappe has been overthrusted towards the SW. Thermometry on synkinematically crystallised garnet-biotite and garnet-hornblende pairs reveals the lower amphibolite facies temperature conditions related to the Crystalline Nappe formation. From the muscovite and biotite Rb-Sr cooling ages, the Shikar Beh Nappe emplacement occurred before 32 Ma and the southwestward thrusting of the Crystalline Nappe began before 21 Ma. Our model involving two opposite directions of thrusting goes against the conventional idea of only one main SW-oriented transport direction in the High Himalayan Crystalline Nappes.

Avaliação da estimativa de substituição de Fe por Al em hematitas de solos

Hematitas de nove solos e uma de itabirito foram tratadas com NaOH 5 mol L-1 e analisadas por difratometria de raios X (DRX), usando varredura escalonada (0,02°2θ/20 s). Determinaram-se o espaçamento d e as dimensões a0 e c0 da cela unitária. As amostras foram dissolvidas com ditionito-citrato-bicarbonato de sódio (DCB), para determinar os teores de Fe (Fe d) e Al (Al d). A substituição em Al foi estimada por DRX a partir de a0, usando-se regressões correntemente em uso, baseadas em hematitas sintetizadas a 25°C (Al25) e a 70°C (Al70). Ao parâmetro a0, variando de 0,50380 a 0,50200 nm, correspondeu uma amplitude de zero a 0,125 mol mol-1 Al d. Os valores estimados pela regressão entre a0 e Al d desviaram-se da regressão Al70 por -0,003 a +0,009 mol mol-1 Al, enquanto a regressão baseada em Al25 superestimou a substituição, em média, por 0,03 mol mol-1 Al. Os resultados indicaram que, para a estimativa da substituição de Fe por Al em hematitas de solos por DRX, a regressão estabelecida com hematitas sintetizadas a 70°C (Al mol mol-1 = 31,09 - 61,714a0) é a mais adequada.

Caracterização do intervalo hídrico ótimo de um latossolo roxo sob plantio direto

O crescimento do sistema radicular e da parte aérea das plantas é influenciado por vários atributos físicos do solo, com complexas interações que envolvem o potencial da água no solo, o teor de oxigênio e a resistência do solo à penetração das raízes. O Intervalo Hídrico Ótimo (IHO) é um parâmetro físico do solo que incorpora os efeitos do conteúdo de água no solo sobre as variações do potencial mátrico, aeração e resistência mecânica do solo. O IHO não tem sido avaliado em solos tropicais, razão por que o objetivo deste trabalho é o de caracterizá-lo num Latossolo Roxo (Typic Hapludox), cultivado com milho no sistema de plantio direto. Para este fim, foram obtidas, nas posições linha e entrelinha da cultura do milho, 72 amostras de solo com estrutura indeformada, nas quais foram determinadas a curva de retenção de água, a curva de resistência à penetração e a densidade do solo, necessárias à obtenção do limite superior e inferior que definem o IHO. Segundo os resultados, o IHO variou positivamente até a densidade de 1,1 Mg m-3 e negativamente para densidades superiores. A amplitude de variação do IHO foi de 0,0073 até 0,125 m³ m-3. No limite inferior do IHO, em relação ao ponto de murcha, a resistência à penetração foi o fator limitante em 85% das amostras, enquanto a capacidade de campo foi o limite superior em 97% das amostras em relação à porosidade de aeração. As modificações na estrutura do solo, refletidas pela variação na densidade, foram mais sensivelmente descritas pelo IHO do que pela água disponível entre a capacidade de o campo e o ponto de murcha permanente. A resistência à penetração e a porosidade de aeração foram fortemente influenciadas pela densidade do solo; neste solo, a redução nos limites do IHO foi determinada pela variação da resistência do solo. Avaliações suplementares do IHO, em solos tropicais, são necessárias sob condições de ampla variação de textura e manejo.

Efeito da adsorção de fosfato em parâmetros físicos e na compressibilidade de solos tropicais

A elevada adsorção de fosfato em solos tropicais oxídicos altera o balanço de cargas nas superfícies das partículas e pode aumentar a dispersão. Conseqüentemente, isto pode influir na distribuição de tamanhos de poros, estabilidade de agregados e suscetibilidade à compactação. Para avaliar o efeito da adsorção de fosfato nas curvas de compressão e limites de consistência de solos, foram amostradas as camadas de 0-3 e 27-30 cm de um Latossolo Vermelho-Escuro (LE) e de um Cambissolo (C), ambos de textura muito argilosa, na microrregião dos Campos da Mantiqueira (MG). Foi adicionada solução de fosfato à metade das amostras para atingir a sua capacidade máxima de adsorção. As pressões de preconsolidação foram obtidas a partir das curvas de compressão, que representam, graficamente, a densidade do solo em função do logarítmo da pressão aplicada. Os limites de liquidez, plasticidade e de contração foram também determinados para cada amostra com e sem fosfato. Os resultados mostraram um deslocamento das curvas de compressibilidade no sentido de menores pressões de preconsolidação, em função do aumento de umidade e adsorção de P. Esse deslocamento foi mais pronunciado nas amostras do Latossolo, principalmente na camada de 0-3 cm, mostrando redução na capacidade de suporte de cargas dos solos. A adsorção de fosfato também alterou os limites de consistência, reduzindo a amplitude da zona de friabilidade e, conseqüentemente, alterando a capacidade de trabalho e tráfego dos solos.