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1 els of arsenate (As(V)) in drinking water as arsine.
2 throline and L-L is either a phosphine or an arsine.
3 he standard reached with tris-trimethylsilyl arsine.
4 pounds do not form any or only less volatile arsines.
5 ne pressurized under nitrogen and doped with arsine and a propylene real sample from a cracker plant
6 ynthesis of InAs NCs with tris(dimethylamino)arsine and alane N,N-dimethylethylamine as the reducing
7 s at 20 degrees C, a loss of only 25-50% for arsine and stibine and the above-mentioned tin compounds
8 reduces the production of the less volatile arsines and iAs is almost exclusively formed, therefore
9 4,6-triiodobenzene with triphenylphosphine, -arsine, and -stibine provides cocrystals based on I...P,
12 ioctylamine coupled with tris(trimethylsilyl)arsine as arsenic precursor and oleic acid as ligand.
15 its at ppbv to ppmv levels were obtained for arsine (AsH(3)), phosphine (PH(3)), and hydrogen selenid
18 ries of structurally differentiated cationic arsines containing imidazolium, cyclopropenium, formamid
19 y and that further understanding of biogenic arsine evolution and degradation are required to adequat
20 t hydrogen ions concentration leading to the arsine formation from iAs compounds detected as As(III)
22 cation exchange column connected in series)-arsine generation-ICP-MS system provided complete separa
24 of germanium with the enhanced properties of arsine/germanium chemistry that promises scale-up to lar
25 of monodentate and bidentate phosphines and arsines have been screened in the coupling of alkyl hali
26 ilable chemicals, such as tris(dimethylamino)arsine, have recently emerged as alternative As precurso
29 tes the premise that incorporation of organo(arsines) into MOF scaffolds is a safer and more convenie
33 alladium-based precatalysts and phosphine or arsine ligands were screened to validate the approach ta
39 -As intramolecular coupling in the phosphine-arsine peri-substituted acenaphthene 3, affording therma
41 d a gas-diffusion cell for the separation of arsine prior to its spectrophotometric determination bas
42 ambient temperature seems to cause enhanced arsine release from soils, and potentially also from the
43 arsenic in each subfraction are converted to arsine sequentially by hydride generation at pH 4.50 and
46 rsine ((TMSi)(3)As) and tris-trimethylgermyl arsine ((TMGe)(3)As), several attempts have been made to
47 senic precursors such as tris-trimethylsilyl arsine ((TMSi)(3)As) and tris-trimethylgermyl arsine ((T
48 emistry of the newly prepared alpha-cationic arsines toward different metal centers and their reactiv