A study of the reactions of Ni and NiO ions relevant to planetary upper atmospheres
The reactions between Ni + ( 2 D) and O 3 , O 2 , N 2 , CO 2 and H 2 O were studied at 294 K using the pulsed laser ablation at 532 nm of a nickel metal target in a fast flow tube, with mass spectrometric detection of Ni + and NiO + . The rate coefficient for the reaction of Ni + with O 3 is k (294...
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Veröffentlicht in: | Physical chemistry chemical physics : PCCP 2020-04, Vol.22 (16), p.894-8951 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The reactions between Ni
+
(
2
D) and O
3
, O
2
, N
2
, CO
2
and H
2
O were studied at 294 K using the pulsed laser ablation at 532 nm of a nickel metal target in a fast flow tube, with mass spectrometric detection of Ni
+
and NiO
+
. The rate coefficient for the reaction of Ni
+
with O
3
is
k
(294 K) = (9.7 ± 2.1) × 10
−10
cm
3
molecule
−1
s
−1
; the reaction proceeds at the ion-permanent dipole enhanced Langevin capture rate with a predicted
T
−0.16
dependence. Electronic structure theory calculations were combined with Rice-Ramsperger-Kassel-Markus theory to extrapolate the measured recombination rate coefficients to the temperature and pressure conditions of planetary upper atmospheres. The following low-pressure limiting rate coefficients were obtained for
T
= 120-400 K and He bath gas (in cm
6
molecule
−2
s
−1
, uncertainty ±
σ
at 180 K): log
10
(
k
, Ni
+
+ N
2
) = −27.5009 + 1.0667log
10
(
T
) − 0.74741(log
10
(
T
))
2
,
σ
= 29%; log
10
(
k
, Ni
+
+ O
2
) = −27.8098 + 1.3065log
10
(
T
) − 0.81136(log
10
(
T
))
2
,
σ
= 32%; log
10
(
k
, Ni
+
+ CO
2
) = −29.805 + 4.2282log
10
(
T
) − 1.4303(log
10
(
T
))
2
,
σ
= 28%; log
10
(
k
, Ni
+
+ H
2
O) = −24.318 + 0.20448log
10
(
T
) − 0.66676(log
10
(
T
))
2
,
σ
= 28%). Other rate coefficients measured (at 294 K, in cm
3
molecule
−1
s
−1
) were:
k
(NiO
+
+ O) = (1.7 ± 1.2) × 10
−10
;
k
(NiO
+
+ CO) = (7.4 ± 1.3) × 10
−11
;
k
(NiO
+
+ O
3
) = (2.7 ± 1.0) × 10
−10
with (29 ± 21)% forming Ni
+
as opposed to NiO
2
+
;
k
(NiO
2
+
+ O
3
) = (2.9 ± 1.4) × 10
−10
, with (16 ± 9)% forming NiO
+
as opposed to ONiO
2
+
; and
k
(Ni
+
·N
2
+ O) = (7 ± 4) × 10
−12
. The chemistry of Ni
+
and NiO
+
in the upper atmospheres of Earth and Mars is then discussed.
The reactions between Ni
+
and O
3
, O
2
, N
2
, CO
2
and H
2
O; NiO
+
and O, O
3
and CO; and NiO
2
+
and O
3
were studied at 294 K using the pulsed laser ablation of a nickel metal target in a fast flow tube, with mass spectrometric detection of Ni
+
and NiO
+
. |
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ISSN: | 1463-9076 1463-9084 |
DOI: | 10.1039/d0cp01124j |