Functional magnetic resonance imaging (fMRI) was used to demonstrate the brain activation during volitional control of breathing in nine healthy human subjects. This type of breathing was induced by acoustic stimuli dictating the respiratory frequency. During the period of dictated breathing not only the frontal and temporal lobes of the brain, but also the parietal lobes were bilaterally activated. The frontal lobe was activated bilaterally in all subjects, with frequent activation of Brodmann areas 4 and 6. In the parietal lobe, activation could mostly be demonstrated in gyrus postcentralis and the same was true for area 22 in the temporal lobe., V. Šmejkal, R. Druga, J. Tintěra., and Obsahuje bibliografii
Functional magnetic resonance imaging (fMRI) was used to demonstrate the brain activation during transition from unconscious to conscious breathing in seven healthy human subjects. In right-handed volunteers, the activated areas were found in both hemispheres. The medial part of the precentral gyrus (area 4) was constantly activated in the left hemisphere. Additional activated areas were demonstrated in the premotor cortex and in the posterior parietal cortex. The activated cortical sites exhibited analogous distribution in the right hemisphere. In two out of the seven subjects, activated sites were also observed in the cerebellar hemispheres, and in the lentiform and caudate nuclei., V. Šmejkal, R. Druga, J. Tintěra., and Obsahuje bibliografii
The diffusion of neuroactive substances in the extracellular space (ECS) plays an important role in short- and long-distance communication between nerve cells and is the underlying mechanism of extrasynaptic (volume) transmission. The diffusion properties of the ECS are described by three parameters: 1. ECS volume fraction α (α = ECS volume/ total tissue volume), 2. tortuosity λ (λ2 = free /apparent diffusion coefficient), reflecting the presence of diffusion barriers represented by, e.g., fine neuronal and glial processes or extracellular matrix molecules and 3. nonspecific uptake k’. These diffusion parameters differ in various brain regions, and diffusion in the CNS is therefore inhomogeneous. Moreover, diffusion barriers may channel the migration of molecules in the ECS, so that diffusion is facilitated in a certain direction, i.e. diffusion in certain brain regions is anisotropic. Changes in the diffusion parameters have been found in many physiological and pathological states in which cell swelling, glial remodeling and extracellular matrix changes are key factors influencing diffusion. Changes in ECS volume, tortuosity and anisotropy significantly affect the accumulation and diffusion of neuroactive substances in the CNS and thus extrasynaptic transmission, neuron-glia communication, transmitter „spillover“ and synaptic cross-talk as well as cell migration, drug delivery and treatment., L. Vargová, E. Syková., and Obsahuje bibliografii a bibliiografické odkazy
Infiltration-outflow experiments were performed on undisturbed soil samples of coarse sandy loam simultaneously with the imaging of flow process by means of magnetic resonance (MR) imaging. The flow in soil under study is highly preferential and exhibits time instability of soil hydraulic properties. For the transient part of infiltration runs, fast 2D imaging was used. For the steady state flow and for the equilibrium state after drainage, horizontal 2D imaging and mapping of longitudinal relaxation (T1) was performed. To obtain the information about internal soil structure all samples were imaged by the computer tomography (CT). The results of all the measurements represent a unique data set. For each sample it contains a record of cumulative infiltration and outflow, hydraulic pressure heads and the simultaneous MR visualization of each particular experiment. Suction pressure heads show a good agreement with the propagation of the wetting front in the sample as displayed by the MR at the very beginning of the each infiltration run. Presented data are the result of first experiment, where MR imaging of infiltration into undisturbed soil samples was combined with concurrent monitoring of suction pressure heads. The next step is to use the gained data for modeling of the infiltration in heterogeneous soil. and Uskutečnili jsme infiltračně výtokový experiment na neporušených vzorcích hlinitopísčité půdy za souběžného snímkování metodou magnetické rezonance (MR). Zkoumaná půda vykazuje výrazné preferenční proudění a časovou závislost hydraulických charakteristik. Pro transientní fáze experimentů jsme použili rychlého vertikálního 2D snímkování. Při ustáleném proudění a při rovnovážném stavu byly pořízeny horizontální 2D snímky a bylo provedeno mapování podélné relaxivity (T1). Pro zjištění vnitřní struktury pevné fáze byly všechny vzorky v suchém stavu snímkovány počítačovou tomografií (CT). Výsledkem experimentu je komplexní soubor dat, který kromě snímků MR obsahuje záznam kumulativní infiltrace výtoku a tlakových výšek. Možnosti metody MR jsou demonstrovány na příkladu porovnání sledu 2D snímků MR s měřenými sacími tlakovými výškami během transientní části infiltrace, kde obě měření shodně zaznamenaly postup čela zvlhčení. Prezentovaná data jsou výsledkem prvního snímkování infiltrace do neporušených vzorků půdy pomocí MR v kombinaci se souběžným měřením sacích tlaků. Dalším krokem bude použití takového souboru dat jako podkladu pro modelování procesu infiltrace do půdy.