ライフサイエンスコーパス: CH

1 CH was associated with older donor and recipient age.

2 CH-3-8 binding to the colchicine-binding site in tubulin

3 CH-3-8 is hydrophobic with an aqueous solubility of 0.97

4 CH-3-8 significantly inhibited the proliferation of thes

5 d NLs with a concentration ratio of 0.3:0.1 (CH:GE).

6 ystem in individuals with CH as follows: (1) CH was consistently present in myeloid cells but varied

7 e (i.e., CD(3)NO(2), CH(3)(15)NO(2), and (13)CH(3)NO(2)), revealing this easy-to-handle compound as a

8 N-CH(3,) -CDH(2,) -CD(2)H, -CD(3), and -(13)CH(3) groups into pharmaceutical amines thus has been de

9 1 and CHCl(3), CCl(4), HCFC-141b, HCFC-142b, CH(2)Cl(2), and HCFC-22, indicating co-location of the e

10 L={(2,6-(i) Pr(2) C(6) H(3) )NC((t) Bu)}(2) CH).

11 he known cyclometallated complex [Th{N(CH(2) CH(2) NSiPr(i) (3) )(2) (CH(2) CH(2) SiPr(i) (2) CHMeCH(

12 (Tren(TIPS) )(OCP)] (2, Tren(TIPS) =[N(CH(2) CH(2) NSiPr(i) (3) )](3-) ), with RbC(8) via [2+2+1] cyc

13 n of (R,R)-((iPr) DuPhos)Co(CO)(2) C(O)CH(2) CH(2) Ph, which upon hydrogenolysis under 4 atm H(2) pro

14 x [Th{N(CH(2) CH(2) NSiPr(i) (3) )(2) (CH(2) CH(2) SiPr(i) (2) CHMeCH(2) )}] (4) by thermolysis; ther

15 with the N-heterocyclic silylenes c-[(CR(2) CH(2) )(NtBu)(2) ]Si: (R=H or methyl) with saturated bac

16 (Me) L={(2,6-(i) Pr(2) C(6) H(3) )NC(Me)}(2) CH), was isolated via reaction of [(Me) LZnSCPh(3) ] (1)

17 complex [Th{N(CH(2) CH(2) NSiPr(i) (3) )(2) (CH(2) CH(2) SiPr(i) (2) CHMeCH(2) )}] (4) by thermolysis

18 lts show that (CH(3) (CH(2) )(3) NH(3) )(2) (CH(3) NH(3) )Pb(2) Br(7) (n = 2) layers undergo two dist

19 uranium-alkyl dimer, [Li(THF)(4) ](2) [U(2) (CH(3) )(10) ], as well as a seven-coordinate uranium-met

20 he magnitude and patterns of C loss (CO(2) , CH(4) and dissolved organic carbon) and soil-water quali

21 nm) exhibits ultra-high CO(2) /N(2) , CO(2) /CH(4) , and C(2) H(2) /C(2) H(4) binary selectivity, bnn

22 rganocatalysts with benzhydrylium ions (Ar(2)CH(+)) and structurally related quinone methides, common

23 t to Ar(2)I(+)) and LB (with respect to Ar(2)CH(+)) indicates that different factors control the ther

24 (O(2)C(t)Bu)(16)]}(2) (4), where B = py-CH(2)CH(2)NHCH(2)C(6)H(4)SCH(3).

25 Ac (3a), NMe(2) (3e), morpholine (3f), OCH(2)CH=CH(2) (3c), SPh (3g), or SePh (3h).

26 dreds of their structural analogues XM(YCH(2)CH(2))(3)N (M = Si, Ge, Sn, Pb, Ti, Al, Cr, Fe, Ni...; Y

27 zolidin-2-iminato groups (L is (NHC(R)=N)(2)(CH(3))P, where NHC(R) is an N-heterocyclic carbene).

28 hways for F(-) + CH(3)CH(2)Cl and PH(2)(-) + CH(3)CH(2)Cl using the activation strain model and Kohn-

29 rbon age measurements of inland water CO(2), CH(4) and dissolved and particulate organic carbon in no

30 Here we use measurements of CO(2), CH(4), and CO from aircraft over 5 days within an invers

31 opologues of nitromethane (i.e., CD(3)NO(2), CH(3)(15)NO(2), and (13)CH(3)NO(2)), revealing this easy

32 ies with similar sizes (CO(2)/N(2) and CO(2)/CH(4)), via precise mechanical control of the pore size

33 The results show that (CH(3) (CH(2) )(3) NH(3) )(2) (CH(3) NH(3) )Pb(2) Br(7) (n = 2)

34 ed elimination (E2) pathways for F(-) + CH(3)CH(2)Cl and PH(2)(-) + CH(3)CH(2)Cl using the activation

35 for F(-) + CH(3)CH(2)Cl and PH(2)(-) + CH(3)CH(2)Cl using the activation strain model and Kohn-Sham

36 2)I(7) (with MA = CH(3)NH(3), and BA = CH(3)(CH(2))(3)NH(3)), and 3D MAPbI(3) using the magnetic fiel

37 oromethyl)-pent-2-en-4-ynes [Ar-C=C-C(CF(3))=CH-CHAr'(Ar")] in good yields.

38 (2) B(9) H(9) }Dy{eta(2) :eta(5) -C(6) H(4) (CH(2) )(2) C(2) B(9) H(9) }(2) Li] 3Dy and show that dic

39 HF)(3) (mu-H)(3) Li](2) [{eta(5) -C(6) H(4) (CH(2) )(2) C(2) B(9) H(9) }Dy{eta(2) :eta(5) -C(6) H(4)

40 CMOM-11R; 3-Cl, CMOM-21R; 4-Cl, CMOM-31R; 4-CH(3) , CMOM-41R) and the existing CF(3) SO(3) (-) varia

41 two-electron reduction in 0.1 M NBu(4)PF(6)/CH(2)Cl(2), cyclic voltammetry studies indicate a 1.8 x

42 dium(II)-oxo cluster [Pd(24) O(44) (OH)(8) ((CH(3) )(2) As)(16) ] (Pd(24) ) can be considered as a bi

43 dium(II)-oxo cluster [Pd(16) O(24) (OH)(8) ((CH(3) )(2) As)(8) ] (Pd(16) ) comprises a cyclic palladi

44 ach can convert any aromatic ring bearing a -CH(2) Br or a -CHO group into a pyrene moiety.

45 However, deeper sources of H(2) and abiotic CH(4) are missing from current models, which mainly invo

46 Geological sources of H(2) and abiotic CH(4) have had a critical role in the evolution of our p

47 ates significant amounts of H(2) and abiotic CH(4), as well as H(2)S and NH(3).

48 niated ions of a species with one additional CH(2) and four double bonds (Deltam/z = 0.0057).

49 of the same lipid class with two additional CH(2) and three double bonds (Deltam/z = 0.0025) and the

50 and P depositions might substantially affect CH(4) uptake and alter the global CH(4) cycle.

51 Although CH(4) accumulation in oxic surface waters became apparen

52 ities of GHGs into the atmosphere (CO(2) and CH(4) ) when subjected to anthropogenic interferences (e

53 F with a modern signature for both CO(2) and CH(4) fluxes implying a microbial preference for the mor

54 CO(2) and CH(4) were younger than dissolved and particulate organi

55 ined as the competition between ammonium and CH(4) for the methane mono-oxygenase enzyme.

56 ADC values of thalami, CN, and CH were significantly lower in IUGR than control foetuse

57 uting to ecosystem respiration (R(eco) ) and CH(4) , while we continuously monitored soil temperature

58 mined via simultaneously quenching (*)OH and CH(3)C(O)O(*) with 2,4-hexadiene.

59 stabilized by noncanonical lone pair-pai and CH-pai interactions, as well as hydrogen bonds.

60 a 3-N(CH(3) )(2) -substituted 2-pyrone and (CH(3) )(3) Si-C=P.

61 Annual CH(4) exchanges over the natural forest (9.1 +/- 0.9 g C

62 In this mangrove, the mean annual CH(4) emission was 11.7 +/- 0.4 g CH(4) -C m(-2) year(-1

63 s, indicate an unusual carbohydrate-aromatic CH-pai bonding that promotes glycopeptide self-assembly.

64 ics simulations to study the behavior of [Au(CH(3))(2))](-) in bulk and interfacial aqueous environme

65 The simulation results suggest that the [Au(CH(3))(2))](-) complex forms one and two gold-ion-induce

66 MA)Pb(2)I(7) (with MA = CH(3)NH(3), and BA = CH(3)(CH(2))(3)NH(3)), and 3D MAPbI(3) using the magneti

67 Baseline CH measurements were obtained using the Ocular Response

68 rboxylic acids and cyclopropylamines bearing CH(2)F, CHF(2), and CF(3) substituents were synthesized

69 studies establishing an association between CH and hematopoietic malignancy, discuss features of CH

70 el reaction, the Menshutkin reaction between CH(3)I and pyridine in three solvents of varying polarit

71 associated with the major abiotic and biotic CH(3)Cl sinks in the environment, namely, CH(3)Cl degrad

72 ical oxidation of CH(4) to methyl bisulfate (CH(3)OSO(3)H) at ambient pressure and room temperature w

73 eat observations were also observed for both CH(4) and NH(3) emissions.

74 ve been recently discovered to exist in both CH(3)NH(3)PbI(3) thin films and single crystals.

75 h the unsaturated N-heterocyclic silylene c-(CH)(2) (NtBu)(2) Si: proceeds directly to the correspond

76 Although the molecular cation CH(3) NH(3) (+) is intrinsically polar, it is heavily di

77 , chloroform (CHCl(3)), and methyl chloride (CH(3)Cl), are gases not regulated by the Montreal Protoc

78 3)][((Me(3)Si)(2)N)(2)U(mu-N)(mu-kappa(2):CN-CH(2)SiMe(2)NSiMe(3))U(N(SiMe(3))(2))(2)] (DME = 1,2-dim

79 ls was only observed on fruit coated by CNCP-CH with 3% OA, but not that with 1% or 2% OA.

80 eptic Fe(HMTO)(RO) [RO=(CH(3) )(2) CF(3) CO, CH(3) (CF(3) )(2) CO, or Ph(CF(3) )(2) CO] prepared in s

81 he PDF of microsites that produce or consume CH(4) and N(2) O, such that a range of microsites occurs

82 may complex with starch through non-covalent CH-pai bonds along alpha-(1 -> 4) glycosidic chains.

83 s, which are among the first eddy covariance CH(4) exchange data reported for any tropical peatland,

84 thaw and autumn freeze using eddy covariance CH(4) measurements from three Arctic sites with multi-ye

85 hich predominates the much higher cumulative CH(4) emission during autumn freeze (1,212.31 +/- 280.39

86 Data showed that cumulative CH(4) and CO(2) fluxes were similar for all the treatmen

87 Currently, CH(4) emissions are a missing component of VCE C budgets

88 orocarbons, here defined as dichloromethane (CH(2)Cl(2)), perchloroethene (C(2)Cl(4)), chloroform (CH

89 Diffuse CH(4) plumes above cities that are not attributable to d

90 In a second step, direct CH-arylation of phosphorylimidazopyridines with aryl hal

91 Dimethyl sulfide (DMS; CH(3)SCH(3)), a biogenically produced trace gas emitted

92 ent from 1.09 A F(-1) to 0.54 A F(-1) during CH.

93 ticulum (SR) Ca(2+) content increased during CH then decreased in HF (from 32 to 15 mum l(-1) ) poten

94 (SiMe(3) )(2) }] affords the ylides [Ph(3) E=CH(2) ] (E=As, 1As; P, 1P).

95 Hence, we encapsulated CH-3-8 lipid conjugate (LDC) into methoxy poly(ethylene

96 We identified 5 cases of donor-engrafted CH, with 1 case progressing into myelodysplastic syndrom

97 eased methane (CH(4)) emissions and enhanced CH(4) production rates throughout the entire soil profil

98 dectomy is associated with decreased exhaled CH(4).

99 induced elimination (E2) pathways for F(-) + CH(3)CH(2)Cl and PH(2)(-) + CH(3)CH(2)Cl using the activ

100 For CH(2)Cl(2) and C(2)Cl(4), we extrapolated using populati

101 (~ 950, ~ 1200, ~ 1400, ~ 1500 ng cm(-2) for CH(3), OH, COOH and NH(2) SAMs) were consistent with: sp

102 We did not observe higher concordance for CH within MZ twin pairs as compared with that within DZ

103 totroph community is an important driver for CH(4) production and its highly dynamic accumulation in

104 ematopoietic compartment (a common model for CH) displayed an exaggerated response to TLR9 agonism, i

105 e leads to an initial loss of formamidinium [CH(NH(2))(2) (+)] ions, leaving behind a partially unocc

106 Moreover, the partitioning of total fossil CH(4) emissions (presently 172 to 195 teragrams CH(4) pe

107 r times higher contribution of autumn freeze CH(4) emission to total annual emission than that of spr

108 Changing from CH(2) Cl(2) to the greener alternative toluene alters wh

109 alytic syntheses of oxygenated products from CH(4) in gas-phase heterogeneous catalysis.

110 may increase the risk of transformation from CH to a myeloid malignancy.

111 mangrove F(CH4) reached a peak of over 0.1 g CH(4) -C m(-2) day(-1) during the summertime owing to a

112 heaters emitted 2390 [95% CI: 2250, 2540] g CH(4) yr(-1) on average, 0.93% [0.87%, 0.99%] of their n

113 om 34 of 97 AP wells (mean emission: 0.286 g CH(4) h(-1)).

114 ean annual CH(4) emission was 11.7 +/- 0.4 g CH(4) -C m(-2) year(-1) while the annual net ecosystem C

115 hose of the Acacia plantation (4.7 +/- 1.5 g CH(4) m(-2) year(-1) ).

116 anges over the natural forest (9.1 +/- 0.9 g CH(4) m(-2) year(-1) ) were around twice as high as thos

117 nd sills releases 18 Gt of greenhouse gases (CH(4) and CO(2)).

118 ory yields well average emissions of 55.6 Gg CH(4).

119 e terms is dominating the increase in global CH(4) emissions.

120 lly affect CH(4) uptake and alter the global CH(4) cycle.

121 t for their important contribution to global CH(4) emissions.

122 ect measurement of the association of having CH when controlling for familial factors.

123 enon in the context of clonal hematopoiesis (CH) and the development of therapy-related myeloid neopl

124 The discovery of clonal hematopoiesis (CH) in older individuals has changed the way hematologis

125 Clonal hematopoiesis (CH) is common in older persons and is associated with an

126 tients have persistent clonal hematopoiesis (CH) that may not reflect residual AML.

127 from clinically silent clonal hematopoiesis (CH) to leukemic progression.

128 gnificantly lower in cerebellar hemispheres (CH) (1.239 vs. 1.280.5 x 10(-3) mm(2)/s, p = 0.045), tha

129 lso on various objects of cultural heritage (CH).

130 mbling a lattice array of concave hexagonal (CH)-shaped rods.

131 Autumn freeze exhibits significantly higher CH(4) flux (0.88 +/- 0.03 mg m(-2) hr(-1) ) than spring

132 om the formation of compensated hypertrophy (CH) until signs of heart failure (HF) are apparent using

133 Chronic hypoxia (CH) produces a time-dependent increase of resting ventil

134 ed in PASMCs from mice with chronic hypoxia (CH)-induced PH.

135 days to weeks of chronic sustained hypoxia (CH).

136 istance factor (CRF) and corneal hysteresis (CH).

137 anol under mild acid-catalyzed conditions in CH(2)Cl(2) followed by oxidation with DDQ (2,3-dichloro-

138 SERCA function remains constant in CH but decreases (tau for SERCA-mediated Ca(2+) removal

139 d with their donors, with telomere length in CH vs non-CH CFUs showing varying patterns.

140 20 genes are recurrently found as mutated in CH, indicating they confer some advantage.

141 The chemical shifts of the (1)H nuclei in CH(3) and NH(3) remained constant with increasing temper

142 Implicit solvation in CH(2)Cl(2) has been included using the PCM and/or SMD co

143 rvations showed a clear diurnal variation in CH(4) exchange over the natural forest where the GWL was

144 acceptable association with the variation in CH(4) production from beef cattle.

145 e.g., nitrogen loading) will likely increase CH(4) emissions from these ecosystems.

146 Rising temperature increases CH(4) uptake of upland soils by 13.8%.

147 O flux to 0.06 g m(-2) yr(-1) and increasing CH(4) 8-fold to 0.8 g m(-2) yr(-1), the meadow now offse

148 delta(18)O-delta(34)S correlation indicates CH(4) advection at the studied site during the Early Hol

149 eaction of the simplest Criegee intermediate CH(2)OO with methane has been performed using the densit

150 In this study we investigated CH(4) emissions from five tree species in two forest typ

151 This study investigates CH(4) emissions during spring thaw and autumn freeze usi

152 We employ the isotopologue CH(2)CDCN to disentangle the unimolecular 3-center DCN e

153 n largely unquantified at levels below ~2 kg CH(4) h(-1).

154 ests resulted in that they emitted at 340 kg CH(4) d(-1) during flooded periods despite their substan

155 emonstrated a clear and consistent diel lake CH(4) flux pattern during stratification and mixing peri

156 ng emissions of other (isotopically-lighter) CH(4) source terms is dominating the increase in global

157 report the synthesis of a vinylene-linked (-CH=CH-) covalent organic framework, COF-701, directly fr

158 nductors, 2D (BA)(2)(MA)Pb(2)I(7) (with MA = CH(3)NH(3), and BA = CH(3)(CH(2))(3)NH(3)), and 3D MAPbI

159 Br) based upon the use of methylammonium (MA=CH(3) NH(3) (+) ) on the perovskite A site.

160 ion that increases the current global marine CH(4) budget by more than 60%.

161 d halogenating agent BnNMe(3).ICl(2) in MeOH-CH(2)Cl(2).

162 the relationship between rumen metabolites, CH(4) production and diets, as well as showing that meta

163 Methane (CH(4) ), a potent greenhouse gas, can form in the sedime

164 Methane (CH(4)) emissions from oil and gas activities are large a

165 Methane (CH(4)), a potent gas with a global warming potential 86-

166 mitters of both ammonia (NH(3)) and methane (CH(4)).

167 to account for over half of annual methane (CH(4) ) emissions and can offset summer photosynthetic c

168 The AD-composting process avoids methane (CH(4)) emissions from landfilling, but emissions of othe

169 ctive C sinks of the biosphere, but methane (CH(4)) emissions can offset their climate cooling effect

170 ing a relatively high amount of dry methane (CH(4)) in the adsorbed phase are largely explored; howev

171 ies had decreased levels of exhaled methane (CH(4)).

172 ssions of the potent greenhouse gas methane (CH(4)).

173 The accelerated increase in global methane (CH(4)) in the atmosphere, accompanied by a decrease in i

174 Our compound exhibits a higher methane (CH(4)) sorptivity as compared to CO(2) at 25 degrees C a

175 Warming exponentially increased methane (CH(4)) emissions and enhanced CH(4) production rates thr

176 sumption of nitrous oxide (N(2) O), methane (CH(4) ), and carbon dioxide (CO(2) ) are affected by com

177 The discovery of methane (CH(4)) accumulation in oxic marine and limnic waters has

178 ling simulations allow the study of methane (CH(4)) sources and sinks at any geographic location.

179 ls, and ~63,000 active wells, whose methane (CH(4)) emissions remain largely unquantified at levels b

180 ur novel 4AP derivatives containing methyl (-CH(3)), methoxy (-OCH(3)) as well as trifluoromethyl (-C

181 norganic mercury (Hg(IN)) and methylmercury (CH(3)Hg) was developed.

182 ) compared to the intact PSF (4.0 +/- 2.0 mg CH(4) m(-2) hr(-1) ) due to prolonged higher WT and more

183 igher in fire-affected areas (7.8 +/- 2.2 mg CH(4) m(-2) hr(-1) ) compared to the intact PSF (4.0 +/-

184 nese(II) to form lithium manganate [Li(2) Mn(CH(2) SiMe(3) )(4) ] enables the efficient direct Mn-I e

185 Multiple CH genes are key regulators of neural stem cell biology

186 ependent clones in individuals with multiple CH mutations; and (3) telomere shortening determined in

187 st rate of methane production was 0.15 mumol CH(4) g(-1) oil d(-1) , orders of magnitude lower than o

188 We could now synthesize 2-N(CH(3) )(2) -functionalized phosphinines, starting from a

189 tionalized phosphinines, starting from a 3-N(CH(3) )(2) -substituted 2-pyrone and (CH(3) )(3) Si-C=P.

190 such as the degree of pyramidality of the N(CH(2))(3) moiety-the positive end of the molecular dipol

191 and the known cyclometallated complex [Th{N(CH(2) CH(2) NSiPr(i) (3) )(2) (CH(2) CH(2) SiPr(i) (2) C

192 of [Th(Tren(TIPS) )(OCP)] (2, Tren(TIPS) =[N(CH(2) CH(2) NSiPr(i) (3) )](3-) ), with RbC(8) via [2+2+

193 The controlled installation of N-CH(3,) -CDH(2,) -CD(2)H, -CD(3), and -(13)CH(3) groups i

194 ic CH(3)Cl sinks in the environment, namely, CH(3)Cl degradation by hydroxyl ((.)OH) and chlorine ((.

195 n) after being normalized to the neighboring CH stretching band.

196 ith both positive and negative signs for net CH(4) and N(2) O flux.

197 ir donors, with telomere length in CH vs non-CH CFUs showing varying patterns.

198 e, Sn, Pb, Ti, Al, Cr, Fe, Ni...; Y = O, NR, CH(2), S), i.e., substituted 5-azabicyclo[3.3.3]undecans

199 In this work, we show that [Fe(II)(Me(3)NTB)(CH(3)CN)](CF(3)SO(3))(2) (Me(3)NTB = tris((1-methyl-1H-b

200 ception of (R,R)-((iPr) DuPhos)Co(CO)(2) C(O)CH(2) CH(2) Ph, which upon hydrogenolysis under 4 atm H(

201 It reacted as a borylated Horner P(=O)CH(2)B carbon nucleophile with carbon dioxide to give a

202 onoxide to give a cyclic five-membered P(=O)-CH(2)-B compound, the product of reductive cleavage of c

203 reduce the uncertainty in the estimation of CH(4) emissions from a globally important ecosystem, pro

204 hematopoietic stressors in the evolution of CH to acute myeloid leukemia or myelodysplastic syndrome

205 ematopoietic malignancy, discuss features of CH that are predictive of leukemic progression, and expl

206 S as a novel tool to reconstruct the flux of CH(4) emissions in geological records and to indirectly

207 oduce H(2) and favour the abiotic genesis of CH(4) in shallow settings.

208 iations between PTH-CH and family history of CH (OR 3.32, 95% CI 1.31 to 8.63), chronic form (OR 3.29

209 We present aircraft measurements of CH(4) emissions from offshore oil and gas platforms coll

210 we performed high-resolution measurements of CH(4) flux from several lakes, using an automated and se

211 eport selective electrochemical oxidation of CH(4) to methyl bisulfate (CH(3)OSO(3)H) at ambient pres

212 Additionally, the percentage of CH(4) producers increased 4-fold from the first to ninth

213 lition and 2.6-3.3 Tg from spring release of CH(4) stored in bubbles in winter lake ice.

214 r findings demonstrate a high sensitivity of CH(4) emissions to global change with important implicat

215 Composting is the largest source of CH(4), carbon dioxide (CO(2)), nitrous oxide (N(2)O), an

216 e among the largest anthropogenic sources of CH(4) emissions, but the precise magnitude of these cont

217 Herein, we present the synthesis of (CH(3)NH(3))(2)NaTi(3)F(12), which comprises an S = 1/2 k

218 hication, and plant community composition on CH(4) emissions from an estuarine tidal wetland.

219 Finally, we examine stressor effects on CH(4) emissions from VCEs and we hypothesize that future

220 tigate the influence of heritable factors on CH, we performed deep targeted sequencing of blood DNA f

221 II(8-14) and full-length fibronectin (FN) on CH(3)-, OH-, COOH-, and NH(2)-terminated alkane-thiol se

222 The N and P impacts on CH(4) uptake indicate that projected increases in N and

223 lling 'side-on' orientation and unfolding on CH(3) SAM; greater numbers of FN molecules arranged 'end

224 reath tests results at baseline (H(2) and/or CH(4) >= 15 ppm).

225 have been discerned for HATs involving OH or CH moieties.

226 regioselectively yielded either 5'-dAdo. or .CH(3), and indeed, each of the three SAM S-C bonds can b

227 rbon dioxide to give a bicyclic product by P-CH(2) attack on CO(2) combined with internal P=O to boro

228 e derivatives PBN-CH(2)NHAc, 4-AcNHCH(2)-PBN-CH(2)NHAc, and 4-MeO-PBN-CH(2)NHAc were the easiest to o

229 The acetamide derivatives PBN-CH(2)NHAc, 4-AcNHCH(2)-PBN-CH(2)NHAc, and 4-MeO-PBN-CH(2

230 Ac, 4-AcNHCH(2)-PBN-CH(2)NHAc, and 4-MeO-PBN-CH(2)NHAc were the easiest to oxidize.

231 ry low concentrations (0.1-10 muM), with PBN-CH(2)NHAc and 4-HOOC-PBN being the two most promising ag

232 Peak CH(4) fluxes were greater during the wet season when the

233 ol cohort included 553 patients with primary CH without any history of trauma who attended the headac

234 kton classes in Lake Stechlin per se produce CH(4) under oxic conditions.

235 evealed significant associations between PTH-CH and family history of CH (OR 3.32, 95% CI 1.31 to 8.6

236 in a headache centre and diagnosed with PTH-CH that developed within 7 days of head trauma.

237 Twenty-six patients with PTH-CH were identified.

238 iF(8)(O(2)C(t)Bu)(16)]}(2) (4), where B = py-CH(2)CH(2)NHCH(2)C(6)H(4)SCH(3).

239 ental evidence of gas-phase methyl radicals (CH(3) (.) ) in the ODHP reaction over boron-based cataly

240 However, reconstructing CH(4) dynamics in geological records is challenging.

241 role of aquatic environments in the regional CH(4) cycle.

242 s due to Ab-induced membrane-associated ring CH (MARCH) E3 ubiquitin ligase-mediated ubiquitination a

243 d or mice that lack membrane-associated RING-CH 8 (MARCH8), the E3 ubiquitin ligase responsible for M

244 The use of heteroleptic Fe(HMTO)(RO) [RO=(CH(3) )(2) CF(3) CO, CH(3) (CF(3) )(2) CO, or Ph(CF(3) )

245 Their reaction with CuBr.S(CH(3) )(2) affords Cu(I) complexes with the first exampl

246 lfurs and carboxamide oxygens within Mn-mu-S-CH(2) -C-O, 5-membered rings.

247 Through several mechanisms, including short CH...F contacts, bifurcation, and long-range dispersion,

248 Substituent factors of F(-Si(CH(3))(2)OR) and F(-SiCH(3)(OR)(2)) are proposed for use

249 Similarly, CH with additional, non-PIGA, somatic alterations occurs

250 eter, water level, soil temperature and soil CH(4) fluxes explained 54% of the variance in stem CH(4)

251 The warming-induced rise in soil CH(4) and N(2) O emissions (1.84 Pg CO(2) -equivalent/ye

252 d phase are largely explored; however, solid CH(4) storage in confined pores of MOFs in the form of h

253 intermediate is favoured due to stabilizing CH-pai-stacking interactions.

254 fluxes explained 54% of the variance in stem CH(4) emissions from individual trees.

255 The P alleviation of N-suppressed CH(4) sink is primarily attributed to substrate competit

256 ated that contemporary N addition suppresses CH(4) sink in global grassland by 11.4% and concurrent N

257 ut the entire soil profile; although surface CH(4) production rates remain much greater than those at

258 4) emissions (presently 172 to 195 teragrams CH(4) per year)(2,3) between anthropogenic and natural g

259 latter account for about 40 to 60 teragrams CH(4) per year(6,7).

260 ventory estimates total emissions of 0.53 Tg CH(4)/yr [0.40-0.71 Tg CH(4)/yr, 95% CI] and corresponds

261 (2) and total CH(4) emission is 13.8-17.7 Tg CH(4) year(-1): 11.2-14.4 Tg via diffusion and ebullitio

262 emissions of 0.53 Tg CH(4)/yr [0.40-0.71 Tg CH(4)/yr, 95% CI] and corresponds to a loss rate of 2.9%

263 ohort of older adults with HLH we found that CH was more prevalent than in control cohorts.

264 Our data suggest that CH is more common in individuals with adult-onset HLH an

265 itionally, we report for the first time that CH-pai interactions at Phe28 directly contribute to AF9'

266 The results show that (CH(3) (CH(2) )(3) NH(3) )(2) (CH(3) NH(3) )Pb(2) Br(7) (

267 ses in which CH was previously detected, the CH mutation was present at tMN diagnosis.

268 s, it is ever more important to evaluate the CH(4) emissions inventory.

269 Potential biomaterials exploiting the CH-pai bond-based stabilization, as exemplified by an en

270 for both hydrogen atom abstraction from the CH reagent and the selective formation of the C-O coupli

271 ffluents and high temperatures, while in the CH test chamber, the samples were exposed mainly to fire

272 Br(6) octahedra and of the C-N groups in the CH(3)NH(3) cations.

273 The peak positions of the CH(2) stretching modes indicate a progressive increase i

274 understanding of the function of some of the CH-associated genes.

275 On the CH stack, the proteinaceous paint layers were exposed to

276 perimental results show that a lens with the CH structure has good focusing intensity and can focus a

277 The CHs were also visited by nonterritorial cheetah males an

278 The CHs/territories were distributed in a regular pattern ac

279 turally occurring local wildlife prey in the CHs.

280 We hypothesized that the CHs pose an increased predation risk to young calves for

281 seagrass ecosystems are about 0.33-0.39 Tmol CH(4) -C/year-an addition that increases the current glo

282 normoxic ventilation with acclimatization to CH, indicating this is a distinct mechanism from the inc

283 to interact strongly with saccharides due to CH-pai and/or OH-pai interactions.

284 of the base and subsequently hydrogenated to CH(3)OH at relatively mild temperatures (100-140 degrees

285 , we review proposed mechanisms that lead to CH, specifically in the context of stem cell biology, ba

286 Together CH(4) emissions from mangrove, salt marsh, and seagrass

287 ea of lakes is 1,095 x 10(3) km(2) and total CH(4) emission is 13.8-17.7 Tg CH(4) year(-1): 11.2-14.4

288 (25.6 +/- 2.3%, mean +/- SD) of annual total CH(4) emissions.

289 f appliances, contributing to 0.14% of total CH(4) emissions from the NG sector in the United States.

290 otometrically in acetonitrile solution using CH acids as indicators.

291 rences in the inductor structure (i.e., O vs CH(2)).

292 me polymer could only load 1.6 +/- 0.4 (w/w) CH-3-8 using the same method.

293 rt a Mars van Krevelen redox mechanism where CH(4) is activated by reaction with a hematite surface o

294 Among cases in which CH was previously detected, the CH mutation was present

295 While CH(3)Cl is the largest contributor of atmospheric chlori

296 ) at equivalent oxidant concentrations, with CH(3)C(O)OO(*) as the most abundant carbon-centered radi

297 Salinity was negatively correlated with CH(4) emissions from salt marshes, but not seagrasses an

298 8 measurements taken from 4 experiments with CH(4) measurements taken in respiration chambers.

299 the hematopoietic system in individuals with CH as follows: (1) CH was consistently present in myeloi

300 For X = CH(3) and OCH(3), these conditions led to undecabrominat