997 resultados para MC-ICPMS
Resumo:
Although previous studies have suggested an increased activation of humoral immunity in neurodegenerative diseases, it remains unclear whether this phenomenon is secondary to lesion formation or contributes directly to their development. Using stereotaxic injections in macaque monkey cerebral cortex, we studied the effects of human immunoglobulins on the neuronal cytoskeleton. Under these conditions, several MC-1-immunoreactive axons were observed in the vicinity of injection site. No MC-1 or TG-3 staining was detected in neuronal soma. Ultrastructurally, several axons in the same area displayed curly formations and accumulation of twisted tubules but not paired helical filaments. These data suggest that Fc fragment induce conformational changes of tau and subtle structural alterations in axons in this model. Immunocytochemical analyses in human autopsy materials revealed the presence of human Fc fragments as well as Fc receptors only in large pyramidal neurons known to be vulnerable in brain aging and Alzheimer's disease, further supporting a possible role of immunoglobulins in neurodegeneration.
Resumo:
This paper studies the rate of convergence of an appropriatediscretization scheme of the solution of the Mc Kean-Vlasovequation introduced by Bossy and Talay. More specifically,we consider approximations of the distribution and of thedensity of the solution of the stochastic differentialequation associated to the Mc Kean - Vlasov equation. Thescheme adopted here is a mixed one: Euler/weakly interactingparticle system. If $n$ is the number of weakly interactingparticles and $h$ is the uniform step in the timediscretization, we prove that the rate of convergence of thedistribution functions of the approximating sequence in the $L^1(\Omega\times \Bbb R)$ norm and in the sup norm is of theorder of $\frac 1{\sqrt n} + h $, while for the densities is ofthe order $ h +\frac 1 {\sqrt {nh}}$. This result is obtainedby carefully employing techniques of Malliavin Calculus.
Resumo:
We used exome sequencing of blood DNA in four unrelated patients to identify the genetic basis of metaphyseal chondromatosis with urinary excretion of D-2-hydroxy-glutaric acid (MC-HGA), a rare entity comprising severe chondrodysplasia, organic aciduria, and variable cerebral involvement. No evidence for recessive mutations was found; instead, two patients showed mutations in IDH1 predicting p.R132H and p.R132S as apparent somatic mosaicism. Sanger sequencing confirmed the presence of the mutation in blood DNA in one patient, and in blood and saliva (but not in fibroblast) DNA in the other patient. Mutations at codon 132 of IDH1 change the enzymatic specificity of the cytoplasmic isocitrate dehydrogenase enzyme. They result in increased D-2-hydroxy-glutarate production, α-ketoglutarate depletion, activation of HIF-1α (a key regulator of chondrocyte proliferation at the growth plate), and reduction of N-acetyl-aspartyl-glutamate level in glial cells. Thus, somatic mutations in IDH1 may explain all features of MC-HGA, including sporadic occurrence, metaphyseal disorganization, and chondromatosis, urinary excretion of D-2-hydroxy-glutaric acid, and reduced cerebral myelinization.
Resumo:
Devolatilization reactions and subsequent transfer of fluid from subducted oceanic crust into the overlying mantle wedge are important processes, which are responsible for the specific geochemical characteristics of subduction-related metamorphic rocks, as well as those of arc magmatism. To better understand the geochemical fingerprint induced by fluid mobilization during dehydration and rehydration processes related to subduction zone metamorphism, the trace element and rare earth element (REE) distribution patterns in HP-LT metamorphic assemblages in eclogite-, blueschist- and greenschist-facies rocks of the Ile de Groix were obtained by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS) analysis. This study focuses on 10 massive basic rocks representing former hydrothermally altered mid-ocean ridge basalts (MORB), four banded basic rocks of volcano-sedimentary origin and one micaschist. The main hosts for incompatible trace elements are epidote (REE, Th, U, Pb, Sr), garnet [Y, heavy REE (HREE)], phengite (Cs, Rb, Ba, B), titanite [Ti, Nb, Ta, REE; HREE > LREE (light REE)], rutile (Ti, Nb, Ta) and apatite (REE, Sr). The trace element contents of omphacite, amphibole, albite and chlorite are low. The incompatible trace element contents of minerals are controlled by the stable metamorphic mineral assemblage and directly related to the appearance, disappearance and reappearance of minerals, especially epidote, garnet, titanite, rutile and phengite, during subduction zone metamorphism. Epidote is a key mineral in the trace element exchange process because of its large stability field, ranging from lower greenschist- to blueschist- and eclogite-facies conditions. Different generations of epidote are generally observed and related to the coexisting phases at different stages of the metamorphic cycle (e.g. lawsonite, garnet, titanite). Epidote thus controls most of the REE budget during the changing P-T conditions along the prograde and retrograde path. Phengite also plays an important role in determining the large ion lithophile element (LILE) budget, as it is stable to high P-T conditions. The breakdown of phengite causes the release of LILE during retrogression. A comparison of trace element abundances in whole-rocks and minerals shows that the HP-LT metamorphic rocks largely retain the geochemical characteristics of their basic, volcano-sedimentary and pelitic protoliths, including a hydrothermal alteration overprint before the subduction process. A large part of the incompatible trace elements remained trapped in the rocks and was recycled within the various metamorphic assemblages stable under changing metamorphic conditions during the subduction process, indicating that devolatilization reactions in massive basic rocks do not necessarily imply significant simultaneous trace element and REE release.
Resumo:
The present study arose from the need to determine inorganic arsenic (iAs) at low levels in cereal-based food. Validated methods with a low limit of detection (LOD) are required to analyse these kinds of food. An analytical method for the determination of iAs, methylarsonic acid (MA) and dimethylarsinic acid (DMA) in cereal-based food and infant cereals is reported. The method was optimised and validated to achieve low LODs. Ion chromatography-inductively coupled plasma mass spectrometry (LC-ICPMS) was used for arsenic speciation. The main quality parameters were established. To expand the applicability of the method, different cereal products were analysed: bread, biscuits, breakfast cereals, wheat flour, corn snacks, pasta and infant cereals. The total and inorganic arsenic content of 29 cereal-based food samples ranged between 3.7-35.6 and 3.1-26.0 microg As kg-1, respectively. The present method could be considered a valuable tool for assessing inorganic arsenic contents in cereal-based foods.
Resumo:
The present study arose from the need to determine inorganic arsenic (iAs) at low levels in cereal-based food. Validated methods with a low limit of detection (LOD) are required to analyse these kinds of food. An analytical method for the determination of iAs, methylarsonic acid (MA) and dimethylarsinic acid (DMA) in cereal-based food and infant cereals is reported. The method was optimised and validated to achieve low LODs. Ion chromatography-inductively coupled plasma mass spectrometry (LC-ICPMS) was used for arsenic speciation. The main quality parameters were established. To expand the applicability of the method, different cereal products were analysed: bread, biscuits, breakfast cereals, wheat flour, corn snacks, pasta and infant cereals. The total and inorganic arsenic content of 29 cereal-based food samples ranged between 3.7-35.6 and 3.1-26.0 microg As kg-1, respectively. The present method could be considered a valuable tool for assessing inorganic arsenic contents in cereal-based foods.
Resumo:
Työn tavoitteena oli optimoida LWC-paperitehtaan kahden hiomolinjan rejektinkäsittelyt. Uusituilla rejektilinjoilla on käytössä keskisakeusrejektinjauhatus. Työn keskeinen osa oli teräkoeajot, teräsarjoja tutkittiin kuusi, kolme molemmilla linjoilla. Kahdessa ensimmäisessä teräkoeajossa oli molemmilla linjoilla samanlaiset jauhinterät. Teräkoeajojen tuloksista havaittiin yleisellä tasolla, että suurin osa mitatuista ominaisuuksista parani jauhatusastetta nostettaessa. Ainoastaan repäisylujuus heikkeni. Terävaihtoehdoista pystyttiin poimimaan molemmille linjoille sopiva terävaihtoehto. Rejektinlajittelun havaittiin parantavan edelleen massan laatuominaisuuksia, paitsi repäisylujuutta. Toisena osuutena vertailtiin keskisakeusjauhimen terävaihtoehtoa, jolla saavutettiin hyviä tuloksia, toisen paperitehtaan korkeassa sakeudessa jauhettuun rejektiin. Korkeasakeusjauhimen terää ei erityisesti valikoitu koeajoa varten. Tuloksista havaittiin, että keskisakeusjauhimella saadaan aikaan varsin hyvää LWC-paperiin käytettävää massaa. Keskisakeudessa jauhettu massa oli monilta ominaisuuksiltaan jopa parempaa kuin korkeasakeusjauhimen massa. Työn kolmannessa osuudessa ajettiin rejektilinjalla sakeuskoeajo. Sakeuskoeajosta havaittiin, että optiset ominaisuudet olivat parhaimmillaan jauhimen MC-sakeusalueen keskivaiheilla. Jauhatussakeuden noustessa kuidut jäivät jäykemmiksi ja karkeammiksi. Tikkupitoisuus oli sitä pienempi, mitä alhaisempaa jauhatussakeutta käytettiin. Sakeudella ei ollut selvää vaikutusta lujuusominaisuuksiin. Tulosten perusteella paras jauhatussakeus keskisakeusjauhimella oli sakeusalueen puoliväli. Työn viimeisenä osana selvitettiin miten kytkentämuutos, jossa rejektilinjan viimeisen lajittimen rejekti käännettiin palaamaan jälkilajittelun sijaan rejektilinjan kaariseulalle, vaikutti koko hiomon kapasiteettiin ja rejektilinjan massan laatuun. Koeajojen tuloksena havaittiin, että kytkentämuutolla pystyttiin nostamaan koko hiomon kapasiteettia ja rejektilinjan akseptin laatu parani.
Resumo:
A technique for both extraction and activity measurement of peroxidase extracted from arazá (Eugenia stipitata Mc Vaugh) is described. Peroxidase from arazá pulp fruit was extracted using a combination of protein precipitation with acetone and extraction with 50 mM sodium buffer phosphate (pH 6.0). Optimum activity using guaiacol as H-donor was obtained at pH from 5.0 to 6.5, temperature from 60 to 75 °C, H2O2 between 10 to 15 mM and guaiacol from 80 to 160 mM. Thermal inactivation showed a first-order inactivation kinetic. Reactivation was observed when extracts were heated at 80 °C and afterwards incubated at 25 °C.