E. Szłyk, M. Barwiołek / Thermochimica Acta 495 (2009) 85–89
89
ture low intensive peaks containing only organic fragments (VTMS
4. Conclusions
R.I. 16% and [CSi(CH3)]+ R.I 100%) were observed. The presence
of organic and chlorine species indicate detachment of VTMS and
chlorine molecules and complex decomposition in the temperature
range 358–474 K. MS spectra of (2) in the range 321–521 K exhibit
the following peaks from olefinic and organometallic species:
Thermal analysis of the complexes (1–4) indicated the metallic
palladium as the final product of the thermal decomposi-
tion, what was evident from TG calculations on thermograms
measured to 1273 K and XRD studies of the residues in the
crucible (Powder Diffraction File) [27]. First stage onset temper-
atures suggest lower stability of complex (1) and (4), whereas
all of them decompose to palladium at temperatures over
478–720 K, what can be promising parameter for CVD of palla-
dium. Analysis of TG/IR spectra of all palladium(II) complexes
indicate the ligand molecules detachment. The VT-MS spectra
revealed fragments containing palladium species in the range
321–548 K. Noted temperatures of palladium formation reveals
the following order PdCl2(DAMDS)2 (4) < PdCl2(VTMS)2 (1) < (3)
PdCl2(DMB)2 < PdCl2(PTMSA)2 (2).
[Si(CH)3]+ (R.I. 44% at 321 K and 50% at 490 K), [PdSi(CH3)3]2 (R.I.
+
7% at 321 K and 4% at 490 K), [PdSiC]+ (R.I. 98% at 321 K and 8% at
490 K). However the spectrum at 321 K present [C6H5CCH2]+ R.I.
100% as the most intensive signal. Such fragments indicate simul-
taneous detachment and fragmentation of PTMSA over 321–490 K.
It can be noted, that the intensity of metal bonded peaks exhibit
reduced relative intensity along the temperature increase. The lat-
ter suggests decomposition of the organometallic fragments and
metallic palladium formation, similarly to processes observed on
TG and DTG curves. In the case of (3) at 548 K peaks which include
metallated species revealed the following data: [PdC4H6Cl]+ R.I.
34%, [PdCl[(CH3)2C C(CH3)H]]+ R.I. 79%, [Pd3[(CH3)2C C(CH3)2]2]
R.I. 10%. Besides that the intensive peaks from organic species were
noted as well: [C4H9]+ R.I. 100% and Cl2 R.I. 62%. Below 548 K frag-
ments with palladium species were not registered, only line from
[CH3CH2CCl]+ (R.I. 28%) ion was detected.
Acknowledgement
Authors wish to thank Polish State Committee for Scientific
Research for a Grant: PBZ-KBN-118/T09/11/2004.
MS spectra of (4) reveal peaks from organic fragments
[CH2 CH CH2]+ (R.I. 38% at 447 K and R.I. 40% at 389 K), [Si(CH)3]+
(R.I. 35% at 447 K and R.I. 52% at 389 K), [CH2CHCHCH2Si(CH3)3]+
(R.I. 40% at 447 K and R.I. 56% at 389 K), while organometallic
fragments: [PdCH2CHCH2]+ (R.I. 72% at 389 K and 98% at 447 K,
[Pd(CH2CHCH2)SiH(CH3)2]+ (R.I. 63% at 389 K and 84% at 447 K)
were noted over 389–447 K. Moreover at 389 K dipalladium ion
([Pd2CH2CHCH2Si]+) has been observed. Similar dipalladium
species were noted in MS of di--chlorodiallylodipalladium(II)
[C6H5PdCl]2. [15] Above results demonstrate, that compounds
(1–4) can be used for the deposition of palladium layers by
Appendix A. Supplementary data
Supplementary data associated with this article can be found, in
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