Determination of iphosphamide and seven metabolites in blood plasma,as stable trifluoroacetyl derivatives,by electron capture chemical ionization GC-MS

A method is described for the determination of the antitumor agent iphosphamide and seven of its metabolites in the plasma of cancer patients by multiple ion monitoring (MIM) GC-MS, mainly using the electron capture chemical ionization mode, of stable methyl and/or trifluoroacetyl derivatives. The metabolites determined were 2- and 3-dechloroethyliphosphamide, 4-ketoiphosphamide, carboxyiphosphamide, iphosphamide mustard, and two previously undetected metabolites, chloroethylamine and 1,3-oxazolidine-2-one. The isolation of the acidic and neutral metabolites was performed by solid phase extraction on to C₁₈ adsorbent at pH 4. The weakly acidic iphosphamide mustard, isolated under these conditions with a yield of ca 50%, was measured as a stable methyltrifluoroacetyl derivative, in contrast to the corresponding phosphoramide mustard of the isomer cyclophosphamide which decomposes during derivatization. Chloroethylamine and 1,3-oxazolidine-2-one were isolated with high yield by liquid extraction with ethyl acetate at pH 10. Selective measurement of several metabolite derivatives with similar retention times was performed by multiple ion monitoring MS of specific ion masses, using a methyl phenyl siloxane capillary column previously employed in the study of cyclophosphamide metabolites. Quantitation of metabolites in patient plasma samples could be performed in the concentration range 3 ng to 20 μg per ml of original plasma.     

Untersuchungen über Radium- und Bariumfällungen unter Anwendung von Thorium X als Indikator

Zusammenfassung Zunächst wird im Zusammenhang mit Messungen der Fällungsgeschwindigkeit von Thorium X in sulfathaltigen Lösungen eine Methode beschrieben, die es gestattet, während der Fällung, und zwar ohne Störung des Fällungsvorganges, diejenigen Mengen von Thorium X zu bestimmen, die sich jeweils zu bestimmten Zeitpunkten noch in Lösung befinden; dabei konnte der Gehalt an Th X mit Hilfe einer Emanationsmethode genau ermittelt werden.Die Versuchsergebnisse, die in Kurven wiedergegeben sind, lassen deutlich erkennen, daß die Fällung von Th X nicht momentan erfolgt, sondern eine gewisse Zeit beansprucht, die von der Konzentration der zugesetzten Sulfat- und Bariumchloridlösung sowie vom Zusatz anderer Fremdionen abhängig ist; es wird jedoch schließlich immer der gleiche Endzustand vollständiger Ausfällung erreicht, wenn mit äquivalenten Mengen gearbeitet wird.Die Annahme, daß die Fällung momentan erfolgt, daß aber das Fällungsprodukt sich im Laufe der Zeit von einem feinkristallinischen Zustand mit großer Emanierfähigkeit in einen grobkristallinen mit geringer Emanationsabgabe umwandelt, konnte durch besondere Experimente widerlegt werden.Schließlich wird noch eine Apparatur zur Messung des Thorongehalts angegeben, die auch für Untersuchungen des Thoriumgehalts von Quellwässern Anwendung finden kann.

---

Summary A method has been worked out which makes it possible to determine the rate of precipitation of thorium X in solutions containing sulphate ion. The amount of thorium X is determined rapidly and accurately by the thorium emanation—thoron—evolved under fixed conditions. Determinations have been made every 5 minute during the time following precipitation, and the results are given graphically.They bring forward, very clearly, that the precipitation of thorium X requires a certain length of time, depending on the concentration of the sulphate and barium-chloride solutions used and on the presence of other ions. However, if equivalent quantities of barium- and sulphate ions are used, the same final result is always reached.It might have been supposed that the precipitation takes place instantaneously but that in course of time, the precipitate undergoes changes through recrystallisations and that the emanating power changes accordingly. That hypothesis, however, could be disproved by special experiments.At last an apparatus for measuring the thoron content is given which can also be applied for investigations of the thorium content of source waters.

---

Résumé Les auteurs décrivent une méthode qui leur a permis de déterminer la vitesse de précipitation du thorium X en solutions contenant de l'ion sulfurique. Le thorium X est dosé par son émanation — le thoron — sous des conditions fixées, et les dosages peuvent se faire à intervalles régulières pendant le temps que demande la précipitation.Les résultats montrent que la précipitation du thorium X ne se fait point à l'instant, mais demande un certain temps, dépendant de la concentration des solutions de sulfate et de chlorure de baryum ajoutées et aussi de la présence d'ions étrangers.Les auteurs réfutent par leurs expériences la théorie que la précipitation se fait momentanément et que le précipité change peu à peu son état cristallin et par cela même, sa faculté de dégager l'émanation.Enfin les auteurs décrivent un appareil pour les dosages de thoron, qui pourra servir de même pour déterminer la teneur en thorium dans les eaux vives.

     

Rotational Motion of a Solute Molecule in a Highly Viscous Liquid Studied byC NMR: 1,3-Dibromoadamantane in Polymeric Chlorotrifluoroethene

The viscosity-dependent retarding effect of a polymeric solvent on the rotation of small solute molecules is investigated by¹³C NMR relaxation measurements. It is found that the relaxation data of 1,3-dibromoadamantane in highly viscous polymeric chlorotrifluoroethene can be explained neither by isotropic nor by realistic anisotropic tumbling in a single environment. The experimental data are rationalized in terms of fast exchange between at least two environments with correlation times differing by up to two orders of magnitude. The study shows that a uniform retardation of molecular tumbling by a polymeric solvent, desirable for shifting the NMR observation window in studies of intramolecular mobility, is not always feasible.     

Monitoring of ionic concentrations in airborne particles and rain water in an urban area of central Germany

The primary objective of this investigation was to document fluctuations of levels of ions in airborne particles and in rain water with the help of ion chromatography. The environmental emission situation in the investigated geographic area is characterized by a widespread use of domestic coal-burning furnaces. The use of a parallel impactor for particulate sampling permits the results to be interpreted additionally in terms of particle size. The anions and cations were extracted from the filters in the sampling devices into ethanol-water mixtures by sonication. Rain water samples were analysed after a simple dilution step. The data obtained on ionic fluctuations are compared with similar data sets published by other laboratories.     

Proof of the Mixing Theorem for Statistical Systems in Classical Physics

In a general measure-theoretic context, it is proved that the action of a stochastic map on a pair of probability distributions can be characterized by the criterion of decreasing mixing distance.     

Reihenentwicklungen im Weylschen Grenzkreisfall über einem halbunendlichen Intervall

Zusammenfassung Im Anschlu an eine frühere Arbeit beweisen wir im Grenzkreisfall für das Intervall s< einen Entwicklungssatz für reelle Funktionen bei vorgeschriebenen reellen Randbedingungen in s=0 und s=. Die Hilfsmittel sind: 1) der reelle Ansatz; 2) der explizite Ausdruck für die Greensche Funktion von Weyl und 3) die allgemeine Parsevalsche Gleichung.     

Accurate determination of wavenumbers for iodine molecular lines in the red spectral region

The hyperfine structure of various absorption lines of molecular iodine with wavenumbers between 12980 and 13890 cm^–1 has been resolved using Doppler-free polarization spectroscopy. The wavenumbers of theo-component of 17 rovibrational lines of I₂ due to the transitionB ³ _ou ⁺ –X¹ _g ⁺ with even rotational quantum numbers have been determined with an accuracy of 0.001 cm^–1. A comparison of the centers of gravity of these 17 lines with the values of the iodine atlas of Gerstenkorn et al. yields a difference of thus corroborating the data of the iodine atlas in the red region within limits of error.