Molecular beam relaxation spectrometry (MBRS) measurement of the desorption rate constant for CO on Ni(110)

1975 ◽  
Vol 52 (3) ◽  
pp. 677-680 ◽  
Author(s):  
C.R. Helms ◽  
R.J. Madix
1995 ◽  
Vol 386 ◽  
Author(s):  
G. Maeda ◽  
I. Takahashi ◽  
H. Kondo ◽  
J. Ryuta ◽  
T. Shingyouji

ABSTRACTVariation in the surface concentration of Fe, Ni, Cu and Zn on Si wafers due to treatment in NH4OH/H2aO2/H2O solution called SC1 is investigated. The metal concentration on the wafer surface depends on the initial surface concentration, concentration in the solution, adsorption probability, desorption rate constant and the treatment time. The surface metal concentration behavior is explained by taking into account the effects of these parameters. The variation in the desorption rate constant with the metal species, the concentration in the solution, treatment temperature and mixing ratio of SC1 is discussed.


A method for investigating the lifetimes of adsorbed molecules on solid surfaces is described. A molecular beam of hydrogen was projected on to the surface of a spinning nickel disk, and the hydrogen evaporating from the surface at different times after deposition was collected and measured with a mass spectrometer. On a slightly oxidized nickel surface all the hydrogen was adsorbed. The subsequent evaporation was a first-order process with a rate constant of 4·5 x 10 11 exp ( -11·5 kcal/ RT ) S -1 . With a mixed molecular beam of hydrogen and deuterium no exchange was produced by the adsorption, which is considered to be molecular. Attempts to remove the oxide film from the nickel surface gave an un­stable surface on which no clear results were obtained. The lifetime of hydrogen on a copper surface was too short to measure.


1995 ◽  
Vol 395 ◽  
Author(s):  
O. Brandt ◽  
H. Yang ◽  
A. Trampert ◽  
K. H. Ploog

ABSTRACTWe present a study of the growth of cubic GaN films on (001) GaAs by molecular beam epitaxy. Our investigations focus on the nucleation stage as well as on the subsequent growth of GaN. The phenomenon of epitaxial growth at this extreme mismatch (20%) is demonstrated to arise from a coincidence lattice between GaAs and GaN. The presence of a high-density of stacking faults in the GaN layer is explained within this understanding as being a natural consequence of the coalescence of perfectly relaxed nuclei. We furthermore analyze the growth kinetics of GaN via the surface reconstruction transitions observed upon an impinging Ga flux, from which we obtain both the desorption rate of Ga as well as the diffusion coefficient of Ga adatoms on the Ga-stabilized GaN surface. The diffusivity of Ga is found to be very low at the growth temperatures commonly used during molecular beam epitaxy, which provides an explanation for the microscopic surface roughness observed on our samples.


Konversi ◽  
2018 ◽  
Vol 6 (2) ◽  
pp. 21 ◽  
Author(s):  
Muhammad Prasanto Bimantio

Abstract - Zeolites can be used as adsorbent, ion exchange, catalyst, or catalyst carrier. Application of fertilizer use in the zeolite also be one of the interesting topic. Zeolites in a mixture of fertilizer can use to control the release of nutrients. The purpose of this research is to study the effect of grain size and time of the activation of zeolite to adsorption and desorption of NH4OH and KCl as modeling of ZA and KCl fertilizer, to obtain the value of adsorption rate constant (ka) and desorption rate constant (kd). This research procedure include: the process of adsorption by adding zeolite with various size and time of activation into a sealed beaker glass and let the adsorption process occurs for 24 hours. After 24 hours, the solution was filtered, the zeolite then put in 100 ml of aquadest into a sealed beaker glass and let the desorption process happened for another 24 hours. Three samples with the largest difference solution concentrations looked for the value of the ka and kd. Zeolite configuration with the largest ka is trialed with fertilizer and compared with the value of ka obtained from modeling. The result for NH4OH adsorbate, -50+60 mesh 2 hours configuration zeolite give the largest ka. For KCl adsorbate, -30+40 mesh 4 hours configuration zeolite give the largest ka. The value between modeling and trials with fertilizers are not much different. Keywords: zeolite, ZA fertilizer, KCl fertilizer, mathematical modelling.


The chemical structure of a premixed fuel-rich methane flame has been investigated by using a four-stage modulated molecular beam inlet to a quadrupole mass spectrometer. The premixed, laminar, flat flame analysed had the following composition (all molar percentages) and conditions: 26.7% CH 4 - 33.3% O 2 - 40.0% Ar ( ϕ = 1.60), pressure = 4.13 kPa, cold-gas velocity at 293 K is 0.80 m s -1 . Mole fraction profiles throughout the flame were measured for the stable species CH 4 , O 2 , H 2 O, H 2 , CO, CO 2 , C 2 H 2 , C 2 H 4 and for the radical species H, OH, CH, CH 2 , CH 3 . These profiles were used to determine the major reaction routes of the CH i ( i = 3, 2, 1) radicals within the fuel-rich flame. It is concluded that in rich flames the methane is consumed mainly through CH 4 + H → >CH 3 + H 2 . (2) The methyl radical then undergoes either recombination to form C 2 -hydrocarbons or hydrogen abstraction via CH 3 + H → CH 2 + H 2 . (12) This is a significant route for the consumption of the methyl radical throughout the flame and is the major route for CH 2 production. The majority of the CH 2 is then consumed via CH 2 + O 2 → > products. (16) This is an important oxidation route in the rich methane flame. The CH radical is produced and consumed in reactions analogous to (12) and (16), but this is a relatively minor reaction path. A rate constant of 2.2 x 10 13 cm 3 mol -1 s -1 at 1810 K is calculated for reaction (16) by using a rate constant for (12) of 1.0 x 10 13 cm 3 mol -1 s -1 at 1770 K. This value of k 12 is consistent with the results of the present work and falls within the range of values calculated in the paper. Molecular-beam inlet mass spectrometry may be used to obtain accurately spatially resolved concentration profiles through flames of stable and radical species. The main limitation of the technique is the wide error limits on the measured radical concentrations.


2017 ◽  
Vol 14 (5) ◽  
pp. 288 ◽  
Author(s):  
Jeison M. Arroyave ◽  
Carolina C. Waiman ◽  
Graciela P. Zanini ◽  
Wenfeng Tan ◽  
Marcelo J. Avena

Environmental contextGlyphosate is a heavily used herbicide that is mobilised in soil and sediments through adsorption–desorption processes from the surface of mineral particles. We demonstrate that the desorption rate of glyphosate from goethite, a ubiquitous mineral, is nearly independent of the concentration and nature of the substance that is used to desorb it. The results elucidate the desorption mechanism and are relevant to understand and predict the environmental mobility of glyphosate. AbstractThe desorption kinetics of glyphosate (Gly) from goethite was studied in a flow cell using attenuated total reflectance Fourier-transform infrared spectroscopy. Because Gly forms an inner-sphere surface complex by coordinating to Fe atoms at the goethite surface, the desorption process is actually a ligand-exchange reaction, where Gly is the leaving ligand and water molecules or dissolved substances are the entering ligands. A series of possible entering ligands that can be found in nature was tested to evaluate their effect on the desorption kinetics of Gly. Contrarily to expectations, the desorption rate was quite independent of the entering ligand concentration. Moreover, the identity of this ligand (phosphate, citrate, sulfate, oxalate, EDTA, thiocyanate, humic acid, water) had only a small effect on the value of the desorption rate constant. By analogy with the reactivity of transition metal complexes in solution, it is concluded that the rate is mainly controlled by the breaking of the Fe–Gly bond, through a dissociative or a dissociative interchange mechanism. The results are relevant in understanding and predicting the environmental mobility of Gly: irrespective of the identity of the entering ligand, Gly will always desorb from iron (hydr)oxides in nature at nearly the same rate, simplifying calculations and predictions enormously. The importance of studying desorption kinetics using mineral surfaces and environmentally relevant molecules is also highlighted.


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