Kramers mechanism of indirect spin-spin couplings of nuclei in crystals

Nuclear spin exchange in the ionic clusters [Tl₄Cl]³⁺, situated in the cavities of cation-substituted chlorosodalite, was investigated by the²⁰³Tl and²⁰⁵Tl NMR method. It was shown that nuclear spin exchange in the ionic crystals is realized by analogy with the Kramers mechanism of indirect exchange of electron spins using the electron shells of the bridging atoms.Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences. Translated from Zhurnal Strukturnoi Khimii, Vol. 34, No. 2, pp. 74–78, March–April, 1993.     

Precise isotope-ratio measurements of lead species by capillary gas chromatography hyphenated to hexapole Multicollector ICP–MS

The precision and accuracy of lead isotope-ratio determination on a short transient signal has been assessed by coupling capillary gas chromatography to the Isoprobe (Micromass, UK), a single-focusing inductively coupled plasma mass spectrometer with multicollector detection. A T-piece connecting the GC transfer line to the torch enabled continuous aspiration of thallium solution for mass-bias correction. The volatile lead species PbEt₄ was derivatized from NIST isotopic certified lead standard SRM 981 and different amounts of PbEt₄ dissolved in iso-octane were injected into the GC. Chromatograms were recorded in multicollection mode by use of Faraday cups; seven isotopes (²⁰⁴Pb, ²⁰⁶Pb, ²⁰⁷Pb, ²⁰⁸Pb, ²⁰³Tl, ²⁰⁵Tl, and ²⁰²Hg) were monitored simultaneously at a transient resolution of 160 ms. PbEt₄ peaks were obtained with a half-width of 1.2 s and a base width of 3.5 s. Lead isotope ratios were calculated from the peak areas integrated for each lead isotope, giving precision in the range of 0.02 to 0.07% for ratios of high-abundant isotopes and injections of 5 and 50 pg absolute amount as lead (five replicates). Mass bias was found to be about 0.5% per mass unit and was corrected by using the continuously measured thallium signals at ²⁰³Tl and ²⁰⁵Tl. After mass-bias correction, deviation of the certified lead ratio values was found to be in the range of 0.02 to 0.15% accuracy.     

Chemical recovery of thallium-203 following production and separation of lead-201

Because of the cost and limited availability of isotopically enriched thallium (>92%²⁰³Tl), its use in the²⁰³Tl(p, 3n)²⁰¹Pb nuclear reaction necessitates chemical recovery. An adaptive method has been developed and evaluated. After the separation of²⁰¹Pb, the²⁰³Tl(I) is oxidized to²⁰³Tl(III) by Cl₂, Br₂ or [Fe(CN)₆]⁻², precipitated as Tl(OH)₃ with NaOH and subsequently converted to Tl₂O₃ by heating. Due to potential loss during recovery, the solubilities of Tl(OH)₃ and Tl₂O₃ in aqueous solution as a function of pH have been studied using the internal tracer²⁰²Tl (T=12.2d), produced during cyclotron irradiation. Effective solubility product constants have been determined to be 5.4·10⁻⁴⁸ and 2.5·10⁻⁴⁷ for Tl(OH)₃ and Tl₂O₃, respectively.     

Isotopic precision for a lead species (PbEt4) using capillary gas chromatography coupled to inductively coupled plasma-multicollector mass spectrometry

Precision and accuracy of lead isotope ratios of a volatile lead species (PbEt₄) were determined by coupling a capillary GC to a magnetic sector multicollector ICP-MS. PbEt₄ was prepared by ethylation of a certified lead isotope solution (NIST SRM 981). Coupling was achieved by a transfer line, which allowed simultaneous introduction of a thallium standard solution to correct for mass discrimination. Seven isotopes (²⁰²Hg, ²⁰³Tl, ²⁰⁴Pb, ²⁰⁵Tl, ²⁰⁶Pb, ²⁰⁷Pb, ²⁰⁸Pb) were monitored simultaneously with a transient resolution of 50 ms. Pb isotope ratios for the PbEt₄ peaks were calculated using transient peak integrals of each isotope signal. Absolute detection limits were 20 (²⁰⁴Pb), 0.7 (²⁰⁶Pb), 1 (²⁰⁷Pb) and 0.3 pg (²⁰⁸Pb). Precision was assessed for five replicate injections of PbEt₄ in iso-octane, corresponding to a total amount of 300 pg of Pb. Precision of isotope ratios for ²⁰⁶Pb, ²⁰⁷Pb and ²⁰⁸Pb were better than 0.07% (RSD), with ratios including ²⁰⁴Pb being one order of magnitude worse. Accuracy using mass bias correction via ²⁰³Tl/²⁰⁵Tl ranged from 0.18% for ²⁰⁸Pb/²⁰⁶Pb to 0.9% for ²⁰⁸Pb/²⁰⁴Pb.     

Authors index to volume 87

Nuclear relaxation times T₁ and T_1p and T₂ of two Tl isotopes, ²⁰³Tl and ²⁰⁵Tl, in solid TINO₂ were measured betwe en 120 and 430 K. The shorter component of the highly non-exponential T₁ decay shows two minima above and below room temperature, which were assigned to Tl⁺ ionic diffusion to NO^-₂ reorientation.     

Silicon Isotope Fractionation in Maize and its Biogeochemical Significance

Plants that absorb silicon may induce isotope fractionation that causes relative abundance changes in biogeochemical processes in organisms and environment. Silicon isotopes (²⁸Si, ²⁹Si, and ³⁰Si) were determined with high precision using multicollector inductively coupled plasma mass spectrometer. In the present study, the silicon isotope composition was determined in maize and corresponding soil was collected from Zhejiang Province, China. The δ³⁰Si values were from ?2.7 to 3.3‰ in the plant tissues. The isotope fractionation between precipitated and dissolved silicon was 0.9976 and the silicon isotope fractionation in the plants was appeared to be Rayleigh-like process. The fractionation factors between the whole plants and the soil–water-soluble fractions were estimated to be 0.9989, indicating the presence of biochemical silicon isotope fractionation. The active uptake of silicon appeared to play an important role through which the heavy silicon isotopes were preferentially absorbed and transferred to the aboveground plant tissues. However, the roles of a passive mechanism for silicon uptake could not be ruled out through which the light silicon isotopes preferentially precipitated in various plant tissues.     

205Tl NMR studies: Ion pairing of Tl+ and (CH3)2Tl+ with NO 3 − and ClO 4 − in various solvents

The concentration dependence of the²⁰⁵Tl chemical shifts of Tl⁺ and of (CH₃)₂Tl⁺ ions was determined in several solvents with NO ₃ ^– and ClO ₄ ^– counterions. In general, increased ion pairing caused a low-frequency shift of the²⁰⁵Tl resonance, with the exceptions of (CH₃)₂TlNO₃ inn-butylamine and TlNO₃ in N,N-dimethylformamide (DMF) and in hexamethylphosphorotriamide (HMPA). In HMPA,²⁰⁵Tl linewidths of both Tl⁺ and (CH₃)₂Tl⁺ increased dramatically with dilution below 0.1M. Analysis of the data allowed ion-pair formation constants and²⁰⁵Tl chemical shifts for the ion-paired cation and for the free (solvated) cation to be estimated for some of the solvents.     

Thallium(II) in the chemically induced thallium(I)-Thallium(III) exchange

The rate of the electron exchange between thallium(I) and thallium(III) induced by iron(II) has been measured at various concentrations of Tl(I), Tl(III), and Fe(II).²⁰⁴Tl tracer, initially in the Tl(I) state, was used. Exchange induced by the separation method was less than 0.01%. The mechanism earlier discussed is $$\begin{gathered} Tl^{III} + Fe^{II} \rightleftharpoons Tl^{II} + Fe^{III} \left( {k_1 ,k_{ - 1} } \right) \hfill \\ Tl^{II} + Fe^{II} \rightharpoonup Tl^I + Fe^{III} \left( {k_2 } \right) \hfill \\ *Tl^I + Tl^{II} \rightleftharpoons *Tl^{II} + Tl^I \left( {k_I } \right) \hfill \\ *Tl^{II} + Tl^{III} \rightleftharpoons *Tl^{III} + Tl^{II} \left( {k_{III} } \right), \hfill \\ \end{gathered} $$ which provides an exchange path in addition to the two-electron reaction^*Tl^I+Tl^III?^*Tl^III+Tl^I (k_ex). The rate law deduced from this mechanism agrees with experiment over a limited range of conditions but fails to account for the observed effect at low concentrations of Tl(I). The additional rate can be represented by inclusion of a term in which the rate of the induced exchange is independent of the concentration of Tl(I). When treated according to the resulting complete rate law the data are consistent with earlier photochemical studies. The present results in combination with other data give k₂=3·10⁶ M^?1·sec^?1 in 1M perchloric acid at 25°C. This is in satisfactory agreement with a recent pulse radiolysis measurement as well as with independent flash photolysis studies.     

Constantes de couplage 203Tl?13C et 205Tl?13C

The coupling constants ¹J (²⁰³Tl? ¹³C) and ¹J (²⁰⁵Tl? ¹³C) in phenylthallium (III) trifluoroacetate have been measured.     

Hyperfine structures and level isotope shifts of then 2 S 1/2 (n=7 – 12)- andn 2 D 3/2,5/2 (n=6 – 10)-levels of203,205Tl measured by atomic beam spectroscopy

Applying atomic beam laser spectroscopy, hyperfine constants as well as level isotope shifts of the (6s ² ns)² S _1/2 levels (n = 7 – 12) and (6s ² nd)² D _3/2,5/2 levels (n = 6 – 10) have been measured in²⁰³Tl and²⁰⁵Tl. Furthermore, some new hyperfine constants and level isotope shifts of the Tl² P _1/2,3/2-states are presented together with corrected results of earlier experiments. The hyperfine splittings have been compared with the predictions of the semiempirical theory. For theD-states a relatively poor agreement between these theoretical predictions and experimental results has been found. Using the experimental level isotope shifts and the δ〈r ²〉 value from muonic X-ray data, results of single-configuration Dirac-Fock calculations have been tested.     

The development of a method for the determination of trace elements in fuel alcohol by ETV-ICP-MS using isotope dilution calibration

A method for the determination of Ag, Cd, Cu, Pb and Tl in fuel alcohol by isotope dilution electrothermal vaporization inductively coupled plasma mass spectrometry (ID ETV-ICP-MS) is proposed. The analytes were separated in two groups: Ag and Cu were determined without modifier and Cd, Pb and Tl with the use of Pd as chemical modifier. The employed ETV operational conditions were pyrolysis temperature of 800 °C for Cd, Pb and Tl and of 900 °C for Ag and Cu and vaporization temperature of 2400 °C for both groups. Seven common, one with additive and one anhydrous fuel ethanol samples were analyzed. The spiked and reference isotopes were, respectively, ¹⁰⁹Ag and ¹⁰⁷Ag, ¹¹²Cd and ¹¹¹Cd, ⁶³Cu and ⁶⁵Cu, ²⁰⁶Pb and ²⁰⁸Pb and ²⁰³Tl and ²⁰⁵Tl. The added amounts of the enriched isotope material were the same for all samples: 4.6 ng of ¹⁰⁹Ag, 5 ng of ¹¹²Cd, 21.1 ng of ⁶³Cu, 9 ng of ²⁰⁶Pb and 0.21 ng of ²⁰³Tl. The blank was bi-distilled ethanol, acidified with 0.3% (v/v) nitric acid, as the samples. The limits of detection (LODs) were calculated as three times the standard deviation of the concentrations in the blank (n = 10) and were, in μg L⁻¹, for Ag: 0.02, for Cd: 0.08, for Cu: 0.1, for Pb: 0.05 and for Tl: 0.001. The obtained concentrations in the samples were in agreement with those obtained by external calibration (EC), according to the paired t-test. The isotope dilution (ID) showed to be a robust, fast and simple calibration technique for the analysis of fuel ethanol.     

Kernresonanzuntersuchungen an Thalliumverbindungen,besonders Thallium–Phosphat-Gläsern

NMR Studies on Thallium Compounds, especially of Thallium Phosphate Glasses Nuclear magnetic resonance techniques with ²⁰⁵Tl have been used to study the Character of the Tl–O bond in different Tl-salts and phosphate systems containing Tl. Generally the covalent contribution to the Tl–O bond increases in the order of the Tl Content. Tl₃PO₄ has the highest covalent contribution on the systems investigated. If Tl is successively substituted by K no influence on the Tl–O bond-character has been observed, but Mg causes diminishing of the covalent character. It follows from Paper chromatography that high condensated phosphates (P₈) in acid solutions are hydrolysed the easier the higher the covalent contribution of the Tl–O–bond.     

Atranes

The PMR spectra of acidified solutions of metalloatrane-3,7,10-trione dihydrates containing a group-IIIB metal atom (M=Al, Ga, In, Tl) in D₂O were studied. The equivalence of the three atrane half-rings in all of the investigated molecules and of the methylene protons in each half-ring was proved. Spin-spin coupling of²⁰³Tl and²⁰⁵Tl with protons, which is apparently realized through a TlN transannular coordinate bond, is observed in the PMR spectrum of thallatrane-3,7,10-trione (M=Tl). The factors that determine the magnitudes of the chemical shifts of the methylene protons are discussed.See [1] for communication XXXII.Translated from Khimiya Geterotsiklicheskikh Soedinenii, No. 3, pp. 312–314, March, 1973.     

An inexpensive, fast, and reliable method for vacuum extraction of soil and plant water for stable isotope analyses by mass spectrometry

The stable isotopes of water (hydrogen and oxygen isotopes) are of utmost interest in ecology and the geosciences. In many cases water has to be extracted directly from a matrix such as soil or plant tissue before isotopes can be analyzed by mass spectrometry. Currently, the most widely used technique for water is cryogenic vacuum extraction. We present a simple and inexpensive modification of this method and document tests conducted with soils of various grain size and tree core replicates taken on four occasions during 2010. The accuracies for sandy soils are between 0.4‰ and 3‰ over a range of 21‰ and 165‰ for δ¹⁸O and δ²H, respectively. Spiking tests with water of known isotope composition were conducted with soil and tree core samples; they indicate reliable precision after an extraction time of 15 min for sandy soils. For clayey soils and tree cores, the deviations were up to 0.63‰ and 4.7‰ for δ¹⁸O and δ²H, respectively. This indicates either that the extraction time should be extended or that mechanisms different from Rayleigh fractionation play a role. The modified protocol allows a fast and reliable extraction of large numbers of water samples from soil and plant material in preparation for stable isotope analyses. Copyright © 2011 John Wiley & Sons, Ltd.     

Synthesis and ESR spectra of [4,6-di-tert-butyl-N-(2,6-diisopropylphenyl)-o-iminobenzosemiquinonato]thallium(i)

[4,6-Di-tert-butyl-N-(2,6-diisopropylphenyl)-o-iminobenzosemiquinonato]thallium(i) was synthesized and characterized by IR and ESR spectroscopy. The hyperfine coupling constants with ^203/205Tl nuclei were found to depend strongly on the nature (solvating ability) of solvents. At 298 K, the HFC constant a _Tl changes from 3.09 mT in n-hexane up to 19.70 mT in tetramethylethylenediamine. The coordination number of solvation was found to be 1 for DMF—benzene and pyridine—hexane systems. The thermodynamic characteristics of solvation in the pyridine—hexane system were determined.     

Crystalline and Glassy Phases in the Ternary System Tl/Bi/Cl: Synthesis and Crystal Structures of the Thallium(I) Chloridobismutates(III) Tl3BiCl6 and TlBi2Cl7

Slow cooling of melts composed of TlCl and BiCl₃ allows for the isolation of the compounds Tl₃BiCl₆ ( 1 ) and TlBi₂Cl₇ ( 2 ). Compound 1 is formed by sublimation at 480 °C from the black melt of 3 TlCl + 1 BiCl₃ as colourless crystals. The crystal structure determination (tetragonal, P4₂/m) consists of nearly regular octahedral [BiCl₆]^3– anions and two independent Tl⁺ cations, which have coordination number 8 in form of a slightly distorted cube and 10 in form of an Edshamar polyhedron, respectively. The structure is not isotypic with the recently reported naturally occurring form of Tl₃BiCl₆, the mineral steropesite. Compound 2 is obtained from a dark red melt of composition TlCl + 2 BiCl₃. On rapid cooling, this melt solidifies to a metastable dark red glass which at ambient temperature crystallises to a light amber crystalline powder within some weeks. The structure of 2 was determined by powder diffraction (triclinic, P\bar{1} ). A distinct lone pair effect is present causing an irregular coordination on the two independent bismuth atoms. Taking Bi–Cl bonds up to 3.5 Å into account, both bismuth atoms gain coordination number seven. ²⁰³Tl and ²⁰⁵Tl solid state NMR and XANES spectra on the Bi and Tl‐L_III edges of both glassy and crystalline TlBi₂Cl₇ show that a close structural similarity exists between both forms. In contrast, the Raman spectra show distinct differences in the bands of the Bi–Cl vibrations region.     

Isotope Effects of Samarium and Ytterbium in the Acetate/Amalgam Separation System

The data on the fractionation of all stable isotopes of ytterbium and samarium in a Me(III) acetate/Me amalgam system were obtained. The light isotopes were preferentially fractionated into the amalgam phase. The single separation gains per mass difference were found to be in the range (4.90÷17.8)·10^–4 for ytterbium and (2.2÷3.8)·10^–4 for samarium. The divergence from the linear dependence between separation gains and isotope mass differences was observed and explained as the effect of nuclear field shift and nuclear spin effects. The maximum value of _u.m. was observed to be 17.8·10^–4 for the lightest, neutron deficit isotope of ytterbium, ¹⁶⁸Yb. The same value for the lightest isotope of samarium, ¹⁴⁴Sm, with a magic number of neutrons (82), was close to the mean for other isotopes.     

Investigation of 205Tl NMR shielding,structural, and electronical properties in thallium halides by applying PBE-GGA,YS-PBE0 and mBJ functionals

We report the structural, electronical, and heavy nuclear ²⁰⁵Tl Nuclear Magnetic Resonance (NMR) shielding properties of thallium halides TlX (X = F, Cl, Br, and I) by the first principles calculation. The Perdew–Burke–Ernzerhof Generalized Gradient Approximation, Yukawa Screened-PBE0 hybrid functional, and modified Becke–Johnson (mBJ) functionals including the relativistic and spin-orbit coupling effects are applied for calculation of the exchange-correlation potentials. Calculated PDOS spectra display that the valence band is composed of the X-s, Tl-5d, X-p, and Tl-6s states, and these states play an important role in ²⁰⁵Tl NMR shielding. Our findings indicate that the nuclear magnetic shielding parameters depend on the electronic properties. Obtained results by mBJ show that there is a close agreement between the experimental and the calculated NMR parameters.     

The trigonal–bipyramidal triiodo­thallium(III) complex [TlI3{(CH3)2SO}2]

The title compound, bis(dimethyl sulfoxide)triiodo­thallium(III), [TlI₃(C₂H₆OS)₂], was crystallized from equimolar amounts of Tl^II and I₂ in a dimethyl sulfoxide (DMSO) solution. After the initial redox reaction, the thallium(III)–iodo complex forms and precipitates as a DMSO solvate. In the crystal structure, Tl is surrounded by three iodide ligands in the equatorial plane and two O‐coordinated DMSO mol­ecules in the axial positions, forming a slightly distorted trigonal bipyramid. The complex lies on a twofold rotation axis, making the DMSO mol­ecules and two of the I atoms crystallographically equivalent.     

Oxygen isotope homogeneity assessment for apatite U-Th-Pb geochronology reference materials

Secondary ion mass spectrometry (SIMS) measurement of oxygen isotopes in apatite has been employed more and more in petrogenetic, metallogenic, and climate change studies. Well-characterised reference materials are needed due to the matrix effect, but they are yet to be well established. In this study, we conducted in-situ oxygen isotopic and chemical analyses on six commonly used apatite reference materials (ie, Emerald, Kovdor, McClure, Mud Tank, Otter Lake, and Slyudyanka) and two in-house apatite references (Qinghu and GEMS 203) to assess their oxygen isotope homogeneity and applicability for microbeam analyses. Our results show that all these apatite references are in general chemically homogeneous. In terms of oxygen isotopes, GEMS 203 (δ¹⁸O = 9.85 ± 0.40‰ [2SD], corrected by Durango 3), Kovdor (δ¹⁸O = 6.55 ± 0.38‰, 2SD), and McClure (δ¹⁸O = 5.94 ± 0.42‰, 2SD) are fairly homogeneous, whereas Emerald (δ¹⁸O = 10.37 ± 0.45‰, 2SD), Mud Tank (δ¹⁸O = 6.35 ± 0.46‰, 2SD), Otter Lake (δ¹⁸O = 9.71 ± 0.47‰, 2SD), Qinghu (δ¹⁸O = 5.44 ± 0.49‰, 2SD), and Slyudyanka (δ¹⁸O = 17.49 ± 0.43‰, 2SD) are less homogenous. This indicates that the former group represents better reference materials for in-situ oxygen isotopic analyses, whilst the latter group can be used as secondary reference material for analytical quality control.