戻る
「早戻しボタン」を押すと検索画面に戻ります。 [閉じる]

コーパス検索結果 (1語後でソート)

通し番号をクリックするとPubMedの該当ページを表示します
1 te with levels of isoprene, monoterpenes, or dimethyl sulfide.
2 erexpressing methionine-gamma-lyase produced dimethyl sulfide.
3 on of organosulfur compounds (OSCs), such as dimethyl sulfide.
4 g isoprene, monoterpenes, and very recently, dimethyl sulfide.
5 nisole < ether-sulfides < dialkyl sulfides < dimethyl sulfide.
6 of the ionic liquid on the nucleofugality of dimethyl sulfide.
7 avage pathway to the climatically active gas dimethyl sulfide(3,4).
8 es of domoic acid, a marine algal toxin, and dimethyl sulfide, a volatile precursor to cloud condensa
9 ne adducts were similar to that observed for dimethyl sulfide adducts.
10                                              Dimethyl sulfide, an alternate substrate for thioether S
11 le volatile organic sulfur compounds such as dimethyl sulfide and (2-methylthio)ethanol.
12 amined as borane carriers in comparison with dimethyl sulfide and 1,4-oxathiane: tert-butyl methyl su
13 of tissue disintegration, and the release of dimethyl sulfide and dimethyl disulfide was related to t
14                             The oxidation of dimethyl sulfide and dimethyl selenide, two-electron oxi
15            The AuNPs enable the detection of dimethyl sulfide and histamine at limits of 0.5 and 0.03
16 o important volatile biogenic markers, i.e., dimethyl sulfide and histamine, is developed to monitor
17 depletion, as well as the rapid oxidation of dimethyl sulfide and mercury in the Antarctic boundary l
18  substitutions with the neutral nucleophiles dimethyl sulfide and triethylamine and the bromination w
19  by biotin or the nonphysiological products, dimethyl sulfide and trimethylamine.
20 ions are reactive toward dimethyl disulfide, dimethyl sulfide, and allyl iodide and most toward water
21 s affected by time include 2-methylpropanal, dimethyl sulfide, and benzaldehyde.
22 reased hydrogen sulfide (H2S), methanethiol, dimethyl sulfide, and carbon disulfide concentrations.
23 o coordinate various ligands like imidazole, dimethyl sulfide, and carbon monoxide depending on the r
24 oprene (C(5)H(8)), methyl bromide (CH(3)Br), dimethyl sulfide, and oxygen (O(2)), which increased sub
25 itrite to a water-soluble phosphine (tppts), dimethyl sulfide, and the biological thiols cysteine (Cy
26                Both the alternate substrate, dimethyl sulfide, and the competitive product inhibitor,
27                       Significant amounts of dimethyl sulfide are emitted from cruciferous vegetables
28 hat procellariiform seabird species that use dimethyl sulfide as a foraging cue selectively forage on
29  controlled to release increasing amounts of dimethyl sulfide as the supply of DMSP exceeds cellular
30 iisobutylaluminum hydride (DIBAL) and borane dimethyl sulfide (BMS) has shown great potential in redu
31 tron ionization (EI) were: carbonyl sulfide, dimethyl sulfide, carbon disulfide, 2-methylthiophene, 3
32 riethylsilane, cycloheptatriene, or a borane-dimethyl sulfide complex.
33 chemoselective reductive-opening by a borane-dimethyl sulfide complex.
34 obial nitrate reductase, selenate reductase, dimethyl sulfide dehydrogenase, ethylbenzene dehydrogena
35 l)-R-pyridinium) with dimethylplatinum-micro-dimethyl sulfide dimer.
36 sulfur compounds detected were methanethiol, dimethyl sulfide, dimethyl disulfide, and dimethyl trisu
37 parts per trillion for select VOCs including dimethyl sulfide, dimethylamine, and trimethylamine.
38 sulfoniopropionate (DMSP) cleavage, yielding dimethyl sulfide (DMS) and acrylate, provides vital carb
39 ination with the algal-derived infochemicals dimethyl sulfide (DMS) and dimethylsulfoniopropionate (D
40 reactivity with aldehydes and the effects of dimethyl sulfide (DMS) and Saharan dust on aerosol pH; a
41 sulfoniopropionate (DMSP) and its catabolite dimethyl sulfide (DMS) are key marine nutrients(1,2) tha
42 kite heterojunction formation by introducing dimethyl sulfide (DMS) as a soft Lewis base additive in
43 ide to form water oxide and the oxidation of dimethyl sulfide (DMS) by hydrogen peroxide to form dime
44                                              Dimethyl sulfide (DMS) contributes significantly to the
45                         Oceanic emissions of dimethyl sulfide (DMS) have long been known to influence
46 ay involving dimethyl sulfoxide (DMSO), with dimethyl sulfide (DMS) identified as the reduction produ
47                                              Dimethyl sulfide (DMS) is a key compound in global sulfu
48                                Ocean-emitted dimethyl sulfide (DMS) is a major source of climate-cool
49                                           As dimethyl sulfide (DMS) is a reliable marker for meat fre
50                                              Dimethyl sulfide (DMS) is produced in large quantities a
51                                      Oceanic dimethyl sulfide (DMS) is the largest natural source of
52  laboratory measurements of alpha-pinene and dimethyl sulfide (DMS) oxidation systems, we characteriz
53       The production of the marine trace gas dimethyl sulfide (DMS) provides 90% of the marine biogen
54 nic acid (MSA) formation in the oxidation of dimethyl sulfide (DMS) remains unclear.
55                Oceanic emissions of volatile dimethyl sulfide (DMS) represent the largest natural sou
56                          Marine emissions of dimethyl sulfide (DMS) to the atmosphere play a fundamen
57 tal thiols, S-methyl-l-methionine (SMM), and dimethyl sulfide (DMS) were analysed periodically.
58 methanethiol (MeSH), ethanethiol (EtSH), and dimethyl sulfide (DMS) were assessed in wines post-bottl
59 P lyases cleave DMSP, producing acrylate and dimethyl sulfide (DMS), a climate-active gas with roles
60                              The presence of dimethyl sulfide (DMS), either as a component originatin
61                                              Dimethyl sulfide (DMS), emitted from the oceans, is the
62 e conversion of dimethyl sulfoxide (DMSO) to dimethyl sulfide (DMS), reversibly, in the presence of s
63                 Oceans dominate emissions of dimethyl sulfide (DMS), the major natural sulfur source.
64 ntermediates in the atmospheric oxidation of dimethyl sulfide (DMS), was generated by flash pyrolysis
65 BlMGL) produced the sulfur volatile compound dimethyl sulfide (DMS).
66 sms(2,3) and the major precursor for gaseous dimethyl sulfide (DMS).
67  the marine volatile organic sulfur compound dimethyl sulfide (DMS).
68                                              Dimethyl sulfide (DMS; CH(3)SCH(3)), a biogenically prod
69 nism by which anthropogenic SO(2) and marine dimethyl sulfide emissions generate secondary biogenic a
70 terised by a high level of sulfur compounds (dimethyl sulfide, ethanethiol), and ester and alcohol co
71               While transgenic lines emitted dimethyl sulfide from leaves and roots, no sulfur-contai
72  the olefin followed by brief treatment with dimethyl sulfide gave a mixture of diastereomeric ozonid
73 none 12c in CH2Cl2 and reductive workup with dimethyl sulfide generated unstable beta-formyl ester 21
74 ived metabolites, including volatile esters, dimethyl sulfide, glycerol and mannoproteins with harves
75                                              Dimethyl sulfide has been studied in the context of glob
76 m the solvolysis data, the nucleofugality of dimethyl sulfide in different proportions of this ionic
77 ules of keystone significance: saxitoxin and dimethyl sulfide in marine communities and tetrodotoxin
78           Furthermore, DMSO was converted to dimethyl sulfide in situ, which served as the methylthio
79 lent yield and enantiomeric excess by borane-dimethyl sulfide in the presence of a chiral oxazaboroli
80 e that the ability of DMSOR to be reduced by dimethyl sulfide is lost upon mutation of Tyr-114 and th
81 own to arise on extended aerobic exposure to dimethyl sulfide, is susceptible to a further degradativ
82 y a compensatory (100-fold) up-regulation in dimethyl sulfide metabolic enzymes.
83              We identified carbon disulfide, dimethyl sulfide, methionol and benzothiazole as key sul
84 y, the release of acetone, carbon disulfide, dimethyl sulfide, nitromethane, pentane, 3-methylfuran,
85 um carbonate precipitation and production of dimethyl sulfide, often blooms in mid-latitude at the be
86 usly shunts as much as 59% of DMSP uptake to dimethyl sulfide production.
87 ted with tailpipe emissions of formaldehyde, dimethyl sulfide, propene, and methyl ketene.
88  reaction in which the accumulating product, dimethyl sulfide, reacts with oxidized enzyme to yield t
89 our results, we postulate a heme-based redox/dimethyl sulfide sensory function of MA4561 and propose
90 xothermic reactions (ca. 50 kcal mol(-1) for dimethyl sulfide) that can fragment or be stabilized via
91 , converting phosphines to phosphine oxides, dimethyl sulfide to dimethyl sulfoxide, and dibenzylamin
92               Further, the nucleofugality of dimethyl sulfide was determined in mixtures containing h
93                        The nucleofugality of dimethyl sulfide was measured in solvent mixtures contai
94 uch faster than the corresponding adducts of dimethyl sulfide, which are currently used extensively.
95 hanol with H(3)O(+), acetone with NO(+), and dimethyl sulfide with O(2)(+*) reagent ions in single br