ライフサイエンスコーパス: SOC

1 SOC microbiota and MELD score remained similar throughou

2 SOC plays a dominant role in 5d(5) iridates (Ir(4+)), un

3 SOCs consist of porous electrodes-the fuel and air elect

4 Neurocognitive event rates were 0% (SOC alone) and 0.4% (evolocumab plus SOC).

5 13 to 21 November 2014 (1,096 CIS arm; 1,101 SOC arm) and followed for 12 months.

6 seen in 36% SOC-only, 33% SOC + Cel, and 32% SOC + ZA + Cel patients.

7 dverse events were seen in 36% SOC-only, 33% SOC + Cel, and 32% SOC + ZA + Cel patients.

8 Grade 3 to 5 adverse events were seen in 36% SOC-only, 33% SOC + Cel, and 32% SOC + ZA + Cel patients

9 There were 625 SOC, 148; ST, 278; and APP, 199.

10 Eight (80%) SOC participants had a total of 11 SAEs compared to 2 (2

11 When approaching a SOC turning point, conversion from low carbon input crop

12 lectrode through electrochemical poling of a SOC at 2 volts for a few seconds.

13 t plantations have significantly accelerated SOC turnover compared with native forest, an effect that

14 Failure of grassland soils to accumulate SOC was attributed to reduced available soil nitrogen, r

15 rol), standard of care plus zoledronic acid (SOC + ZA), standard of care plus docetaxel (SOC + Doc),

16 In contrast, adaptive SOC is a self-organizing process where local adaptations

17 ZTE images were acquired after SOC MR imaging.

18 All SOC patients received FFP and/or PLT per hospital guidel

19 revealed the presence and interaction of all SOC components in the injured VSMCs, where Homer1 intera

20 ental system of Au/GaAs(111) surface with an SOC gap of approximately 73 meV, facilitating the possib

21 exhibit unrealistic oscillatory behavior and SOC insensitivity to long-term changes in C inputs.

22 owever, the relationship between climate and SOC stability remains unclear.

23 in the parameter space of orbital energy and SOC.

24 s oxide (N2 O) and methane (CH4 ) fluxes and SOC changes (DeltaSOC) at a long-term, irrigated continu

25 e impacts of CO2 fertilization on litter and SOC dynamics can be easily decomposed into the relative

26 e molecular mechanisms that regulate POC and SOC formation are different.

27 ry opportunities to enhance productivity and SOC storage in degraded lands through improved managemen

28 work to frame and guide the study of SOM and SOC and their management for sustained production and cl

29 seous findings was performed between ZTE and SOC MR imaging.

30 We assayed SOC decomposition from these incubations by combining in

31 The scaffolding protein Homer assembles SOC complexes, but its role in VSMCs is not well underst

32 they are also frequently used to help assess SOC dynamics.

33 al factor for SOC change, and the background SOC was the second influence factor.

34 ty in SOC predictions from the process-based SOC models.

35 d C-terminal STIM1 antibodies on TRPC1-based SOCs and STIM1 staining suggest that channel activation

36 fy a new activation mechanism of TRPC1-based SOCs in VSMCs, and a novel role for STIM1, in which stor

37 fy a new activation mechanism of TRPC1-based SOCs in VSMCs, and a novel role for STIM1, where store-o

38 s have shown that stimulation of TRPC1-based SOCs requires G protein alpha q subunit (Galphaq)/phosph

39 Bamboo reduced soil organic C (SOC) content, compared to the cedar plantation.

40 Here, we present the soil organic C (SOC) dynamics along 20 years of forest-to-pasture conver

41 mall change in the amount of soil organic C (SOC) may affect carbon dioxide (CO2) concentrations in t

42 bamboo encroachment affects soil organic C (SOC), soil total N, microbial biomass C (MBC), microbial

43 t of STIM2-dependent store-operated calcium (SOC) entry.

44 e we report findings on soil organic carbon (SOC) change in three different cropping systems (soybean

45 We analyzed the soil organic carbon (SOC) concentrations of 87 surface soil samples (0-15 cm)

46 any microbial models of soil organic carbon (SOC) decomposition have been proposed recently to advanc

47 bal warming's effect on soil organic carbon (SOC) decomposition in Asian monsoon forests, we conducte

48 Quantifying soil organic carbon (SOC) decomposition under warming is critical to predict

49 At both sites, sedimentary organic carbon (SOC) Delta(14)C signatures of -631 +/- 54 per thousand (

50 high-resolution maps of soil organic carbon (SOC) distribution by linking National Wetlands Inventory

51 Soil organic carbon (SOC) dynamics are regulated by the complex interplay of

52 y reproduces litter and soil organic carbon (SOC) dynamics of the standard CLM4.5 across different sp

53 Restoration of soil organic carbon (SOC) in agricultural soils can not only improve soil qua

54 Over 75% of the soil organic carbon (SOC) in the top meter of soil is directly affected by hu

55 spatial distribution of soil organic carbon (SOC) loss due to land use and land cover change has been

56 of this replacement on soil organic carbon (SOC) remains paramount for effectively managing ecosyste

57 Changes in soil organic carbon (SOC) stability may alter carbon release from the soil an

58 To better understand soil organic carbon (SOC) stock dynamics and its driving and controlling fact

59 assess the responses of soil organic carbon (SOC) stocks in British semi-natural landscapes to anthro

60 c management impacts on soil organic carbon (SOC) stocks, soil greenhouse gas (GHG) emissions, and gl

61 and composition of the soil organic carbon (SOC) through soil microbial community.

62 ts of forest logging on soil organic carbon (SOC).

63 t (+/-) ritonavir (RTV) or standard of care (SOC) (tenofovir disoproxil fumarate 300 mg, emtricitabin

64 use of readmission despite standard of care (SOC) associated with microbial dysbiosis.

65 strategy (CIS) versus the standard of care (SOC) on the primary outcome of linkage to care within 1

66 o evolocumab, 420 mg, plus standard of care (SOC) or SOC alone.

67 Patients and Methods Standard of care (SOC) was hormone therapy continuously (metastatic) or fo

68 allergy in 3 periods: (1) standard of care (SOC), (2) penicillin skin testing (ST), and (3) computer

69 to provide the CIS or the standard of care (SOC).

70 ed transfusion strategy or standard of care (SOC; 1:1 TEG:SOC).

71 The standard of care (SOC; biannual CD4) was the comparator.

72 e evaluated oral FA/RIF vs standard-of-care (SOC) intravenous antibiotics for treatment of hip or kne

73 logies against the current standard-of-care (SOC) laboratory-based assay in South Africa, when operat

74 y-four patients undergoing standard-of-care (SOC) MR imaging with concomitant CT were enrolled in thi

75 Each patient underwent standard-of-care (SOC) triple-site testing, and swabs were taken to form a

76 erior to contemporary standard optimal care (SOC) encompassing high-sensitivity troponin assays (hs-t

77 Solid oxide cells (SOCs) can operate with high efficiency in two ways-as fu

78 s (POCs) and secondary ossification centers (SOCs) of mammalian long bones.

79 ts of store-operated Ca(2+) influx channels (SOCs) in proliferative and migratory vascular smooth mus

80 +) stores activates store-operated channels (SOCs) composed of canonical transient receptor potential

81 RPC1) protein-based store-operated channels (SOCs) mediates Ca(2+) entry pathways that regulate contr

82 +) stores activates store-operated channels (SOCs), which mediate Ca(2+) entry pathways that regulate

83 +) stores activates store-operated channels (SOCs), which mediate Ca(2+) entry pathways that regulate

84 e of producing 20% gain in state of charge (SOC) under AM1.5 illumination for ca. 1.7 hours without

85 deling, and the spatial overlap coefficient (SOC).

86 tions of the semivolatile organic compounds (SOCs) in the soil were not correlated with the organic c

87 t allocated patients 2:1:1 to SOC (control), SOC + Cel, or SOC + ZA + Cel.

88 20 years after forest-to-pasture conversion SOC in HG decreased by 20%, whereas in LG SOC increased

89 ated curvature-enhanced spin-orbit coupling (SOC) and spinterface effect in carbon-based organic spin

90 en given to the role of spin-orbit coupling (SOC) in 5d oxides, particularly on the formation of nove

91 Engineered spin-orbit coupling (SOC) in cold-atom systems can enable the study of new sy

92 tings are attributed to spin-orbit coupling (SOC) in the ECX(*) radicals.

93 superfluid with Rashba spin-orbit coupling (SOC) interactions.

94 l-established that high spin-orbit coupling (SOC) materials convert a charge current density into a s

95 to the inherently weak spin-orbit coupling (SOC) of OSECs, their inverse spin Hall effect (ISHE) res

96 The influence of spin-orbit coupling (SOC) on the physical properties of the 5d(2) system Sr2M

97 ronic correlations with spin-orbit coupling (SOC) represents a central issue in quantum materials res

98 e, orbital overlap, and spin-orbit coupling (SOC) strength in the FePt film, leading to nonvolatile m

99 rmiology evolution with spin-orbit coupling (SOC) strength.

100 rstanding the molecular spin-orbit coupling (SOC), and a means to tune its strength.

101 QSH phase arises from a spin-orbit coupling (SOC)-induced s-p band inversion or p-p bandgap opening a

102 5d TMOs with pronounced spin-orbit coupling (SOC).

103 to the presence of a spin-orbital coupling (SOC) induced gap at Dirac nodes.

104 stem can trigger self-organized criticality (SOC).

105 same intrinsic SOC, but different curvature SOC due to their distinct curvatures.

106 ns that conventional harvests do not deplete SOC in the mineral soil have been a function of their sh

107 are with both zoledronic acid and docetaxel (SOC + ZA + Doc).

108 (SOC + ZA), standard of care plus docetaxel (SOC + Doc), or standard of care with both zoledronic aci

109 In previous exogenously driven SOC models, adaptation plays no role, and no optimizatio

110 ve an orbital singlet with reduced effective SOC.

111 The effective SOC ratio of the C70 film to the C60 film was estimated

112 of the molecular g-shifts with the effective SOC, depending on subtle aspects of molecular compositio

113 for ventilation defects with PRM emphysema (SOC = 64% +/- 30) was significantly greater than that fo

114 s trapping, SOC = 36% +/- 28; for emphysema, SOC = 1% +/- 2; P = .001) and moderate (for gas trapping

115 s trapping, SOC = 34% +/- 28; for emphysema, SOC = 7% +/- 15; P = .006) COPD.

116 , although some hot-spot areas showed eroded SOC >0.45 Mg C ha(-1) yr(-1).

117 es, ZTE imaging of osseous features exceeded SOC MR imaging.

118 Chinese cropland has experienced SOC change over the past century.

119 Faster SOC decomposition was associated with lower soil microbi

120 Five SOC and no FMT participants developed further HE (P = 0.

121 of 0.78 (95% CI, 0.62 to 0.98; P = .033) for SOC + ZA + Cel.

122 or break system was the critical factor for SOC change, and the background SOC was the second influe

123 0; P = .847; median survival, 70 months) for SOC + Cel and 0.86 (95% CI, 0.70 to 1.05; P =.130; media

124 05; P =.130; median survival, 76 months) for SOC + ZA + Cel.

125 p=0.450), 81 months (41 to not reached) for SOC + Doc (0.78, 0.66-0.93; p=0.006), and 76 months (39

126 OC-only, not reached (32 to not reached) for SOC + ZA (HR 0.94, 95% CI 0.79-1.11; p=0.450), 81 months

127 .006), and 76 months (39 to not reached) for SOC + ZA + Doc (0.82, 0.69-0.97; p=0.022).

128 al was 71 months (IQR 32 to not reached) for SOC-only, not reached (32 to not reached) for SOC + ZA (

129 entifiable regions which can be targeted for SOC restoration efforts.

130 e on failed first-line ART was 3.7 years for SOC and <0.9 years for all routine/adaptive VL strategie

131 scounted life expectancy was 16.69 years for SOC, 16.97 years with VL confirmation of immunologic fai

132 a greenhouse accounting perspective, forest SOC is not the entire story.

133 We show agreement between secondary forest SOC stocks derived purely from biomass information and s

134 st, could possibly help attenuate the forest SOC emission by adding to a carbon pool in landfill.

135 will have a much bigger influence on future SOC losses in mid-latitude mineral soils than land use c

136 ong-term C-input changes and implies greater SOC storage associated with CO2-fertilization-driven inc

137 However, SOC showed different distribution patterns, being concen

138 Ideally, SOCs should perform well, be durable and be inexpensive,

139 the SOC decline (break crop) or even improve SOC (corn monocropping) in mollisols regions.

140 alkyl, O-alkyl, aromatic, and carbonyl C) in SOC.

141 cales, measurements for detecting changes in SOC are needed.

142 repancy could result from varying changes in SOC components and soil microbial communities under warm

143 Here we argue that simulating changes in SOC stocks based on C input that are proportional to cro

144 o bamboo encroachment leads to a decrease in SOC and total soil N, an increase in MBC and WSOC, and a

145 a long-term (i.e. >/=300 years) decrease in SOC when a primary forest is logged and then subjected t

146 There were no differences in SOC stocks in the top 30 cm between grassland up to 17 y

147 The long-term drop in SOC in the mineral soil is driven by the biomass drop fr

148 es showed small losses and even net gains in SOC.

149 tion expected from thaw-induced increases in SOC availability.

150 Long-term reductions in SOC mean residence times were coupled to litter inputs.

151 ly one of the main sources of uncertainty in SOC predictions from the process-based SOC models.

152 Homer1 in cultured VSMCs partially inhibited SOCs, VSMC migration, and VSMC proliferation.

153 creases of 73% and 56% compared with initial SOC stocks in the 1980s.

154 ine interaction (HFI) and the same intrinsic SOC, but different curvature SOC due to their distinct c

155 , SOC decomposition would decrease as labile SOC declines under field warming, but observations of SO

156 But the decomposition of labile SOC was similar in warmed plots compared to the control.

157 on SOC in HG decreased by 20%, whereas in LG SOC increased by 41%.

158 We review forest logging SOC studies and provide an overarching conceptual explan

159 Large land areas have lost SOC as a result of land use practices, yet there are com

160 ted to rapid changes in climate, making many SOC stocks vulnerable to losses by decomposition or dist

161 ata from long-term experiments with measured SOC changes.

162 The concentrations of most SOCs in the near-ground atmosphere were dominated by rev

163 This net SOC decrease in HG was due to a larger reduction in C3-d

164 These results suggest that enhanced neuronal SOC causes synaptic loss in HD-afflicted MSNs.

165 593, a neuroprotective inhibitor of neuronal SOC channels, rescues YAC128 MSN spine loss both in vitr

166 del was fitted using a global compilation of SOC data and the History Database of the Global Environm

167 a and found that the chemical composition of SOC did not differ significantly among treatments until

168 a prairie, we assessed the decomposition of SOC components by incubating soils from control and warm

169 tudy aimed to determine the decomposition of SOC components with different turnover times after subje

170 erm warming accelerates the decomposition of SOC components with slow turnover rates and thus amplify

171 responsible for accelerated decomposition of SOC components with slow turnover rates.

172 The decomposition of SOC components with turnover times of years and decades,

173 This gain of SOC was surprisingly three times more than that with sta

174 patterns of SOC loss were found: Hotspots of SOC loss coincided with some major cropping regions as w

175 However, the interrelation of SOC and these drivers and their potential connection net

176 d" contributed nearly equally to the loss of SOC.

177 Dynamic models of SOC help reveal the interaction among soil carbon system

178 ions of Ndep effects against observations of SOC at a regional field scale.

179 nes under field warming, but observations of SOC decomposition under warming do not always support th

180 Using observations of SOC dynamics with detailed soil properties from 90 field

181 We determined the pattern of SOC change resulting from the conversion from forest (C3

182 Important spatial patterns of SOC loss were found: Hotspots of SOC loss coincided with

183 The greatest pool of SOC was found within the Atchafalaya/Vermilion Bay compl

184 ge theoretical problem since the presence of SOC implies that the spin is not a good quantum number.

185 ily influenced by the intrinsic processes of SOC formation and the nutrient status.

186 e results indicated that the decline rate of SOC in recent ten years (0.27 g kg(-1) yr(-1)) has slowe

187 However, the role of SOC for other 5d configurations is less clear.

188 d result in changes in chemical stability of SOC through the altered microbial community composition.

189 re temperature independent, the stability of SOC was not associated with the MAT, but was heavily inf

190 The immediate stimulation of SOC decomposition was caused by warmer soil before the c

191 The study of SOC dynamics under different bioclimatic conditions and

192 l United States, there are 1,153-1,359 Tg of SOC in the upper 0-100 cm of soils across a total of 24

193 esting (92%) was slightly lower than that of SOC testing (96%) for detecting C. trachomatis (P = 0.16

194 g (90%) was significantly lower than that of SOC testing (99%) (P < 0.001).

195 s need to assume a long-term net transfer of SOC from the mineral soil to the atmosphere when primary

196 ficient avenue for the nonvolatile tuning of SOC based magnetism and spintronic effects, but also hel

197 mportant parameter affecting the sorption of SOCs onto soils.

198 smooth muscle cells (VSMCs), stimulation of SOCs composed of canonical transient receptor potential

199 us, the impacts of bioclimatic conditions on SOC and future trends.

200 ient men with cirrhosis with recurrent HE on SOC was conducted with 1:1 randomization.

201 sition and C input (quantity and quality) on SOC dynamics is likely one of the main sources of uncert

202 nd soil C pools (a total of 17 variables) on SOC change rate (rC , Mg C ha(-1) yr(-1) ).

203 ocated men 2:1:1:1 to standard of care only (SOC-only; control), standard of care plus zoledronic aci

204 tients 2:1:1 to SOC (control), SOC + Cel, or SOC + ZA + Cel.

205 en subjects were randomized 1:1 to FA/RIF or SOC.

206 umab, 420 mg, plus standard of care (SOC) or SOC alone.

207 In particular, SOC plays a subtle role in creating the electronic groun

208 ocedure bleeding occurred in only 1 patient (SOC group) after large-volume paracentesis.

209 There were higher percent SOC losses on cropland but since more than twice as much

210 ts' urine exosome gene expression assay plus SOC AUC 0.73 (95% CI, 0.68-0.77) was superior to SOC AUC

211 the urine exosome gene expression assay plus SOC was associated with improved discrimination between

212 ocumab exposure, 2.8% in the evolocumab plus SOC group.

213 After 52 weeks, evolocumab plus SOC was associated with a significant reduction in LDL-C

214 ere 0% (SOC alone) and 0.4% (evolocumab plus SOC).

215 the study received evolocumab, 420 mg, plus SOC.

216 In order to quantify potential SOC losses or sequestration at field, regional, and glob

217 g intensity in cattle activities to preserve SOC stocks and to reduce C emissions after land-cover ch

218 In contrast to previous SOC experiments, here the SOC is both generated and prob

219 rding to the substrate regulating principle, SOC decomposition would decrease as labile SOC declines

220 However, quantifying SOC strengths indirectly through spin relaxation effects

221 patients receiving SOC, 197 (32%) receiving SOC + ZA, 288 (52%) receiving SOC + Doc, and 269 (52%) r

222 32%) receiving SOC + ZA, 288 (52%) receiving SOC + Doc, and 269 (52%) receiving SOC + ZA + Doc.

223 receiving SOC + Doc, and 269 (52%) receiving SOC + ZA + Doc.

224 re reported for 399 (32%) patients receiving SOC, 197 (32%) receiving SOC + ZA, 288 (52%) receiving S

225 achieved similar declines to those receiving SOC.

226 at native forest replacement usually reduces SOC stocks and may switch the forest from a net sink to

227 of litter input into the soil that regulate SOC stability.

228 their complex interconnections in regulating SOC dynamics.

229 hly active nanostructures for reinvigorating SOCs during operation.

230 rall, litter type can control an ecosystem's SOC nature, as reflected by the finding that higher labi

231 Sixteen SOC (53.3%) received FFP, 10 (33.3%) PLT, and 4 (13.3%)

232 ge increase of 1.2 kgCm(-2) (c. 10%) in soil SOC over the period 1750-2010.

233 CO2 as organic carbon by agricultural soils (SOC) is promoted as a climate change mitigation option.

234 three-pool (labile, intermediate and stable) SOC decomposition model.

235 ging from pi-conjugated polymers with strong SOC that contain intrachain platinum atoms, to weak SOC

236 Surface SOC decreased with stover removal and with CT after 14 y

237 ns can impact soil GHG emissions and surface SOC stocks.

238 n strategy or standard of care (SOC; 1:1 TEG:SOC).

239 previously unelucidated control on long-term SOC dynamics in native forests and demonstrate a potenti

240 Short-term SOC flux varies around zero.

241 onfirm by first principles calculations that SOC not only provides the magnetocrystalline anisotropy,

242 arison to Sr2ScOsO6, it is demonstrated that SOC-induced anisotropy has the ability to relieve frustr

243 Given that SOC is a substantial store of potential greenhouse gasse

244 Results of our work indicate that SOC stocks in the NCP croplands increased significantly,

245 The SOC assay had 101 positive, 214 negative, 4 indeterminat

246 rimary outcome versus 43% (477/1,101) at the SOC sites (adjusted relative risk [RR] 1.52, 95% CI 1.19

247 arbon input crop system helped slow down the SOC decline (break crop) or even improve SOC (corn monoc

248 he early 1980s were the main drivers for the SOC stock increase.

249 ntrast to previous SOC experiments, here the SOC is both generated and probed using a direct ultra-na

250 ncidence of new-onset diabetes was 4% in the SOC alone group and, adjusting for duration of evolocuma

251 hieved the primary outcome versus 35% in the SOC group (relative risk [RR]CIS vs SOC = 1.58, 95% CI 1

252 30 days in the CCTA group and 17 [7%] in the SOC group [p = 0.40]).

253 Per protocol, all subjects in the SOC group received blood product transfusions versus 5 i

254 25%) in the CIS+ group, and 767 (38%) in the SOC group.

255 nced the labile carbon pool size and not the SOC stability.

256 Cognition improved in the FMT, but not the SOC, group.

257 um- and spin-resolved in situ probing of the SOC band structure and eigenstates.

258 re on the day of diagnosis versus 16% of the SOC group (RRCIS vs SOC = 9.13, 95% CI 1.65-50.40).

259 ilization of carbon sources younger than the SOC, likely from the DOC pool.

260 r semiconductors and link it directly to the SOC strength in a series of high-mobility molecular semi

261 Participants in the CIS arm versus the SOC arm had the following secondary outcomes: linkage to

262 o weak SOC polymers, to C60 films, where the SOC is predominantly caused by the curvature of the mole

263 with 315 (97.8%) results consistent with the SOC result.

264 Here, we asked whether these SOC components and Homer1 are present in the same comple

265 andom assignment allocated patients 2:1:1 to SOC (control), SOC + Cel, or SOC + ZA + Cel.

266 contributed the higher ratios of labile C to SOC and lower ratios of recalcitrant C to SOC in bamboo

267 to SOC and lower ratios of recalcitrant C to SOC in bamboo soils compared with cedar soils.

268 ntly lower use of blood products compared to SOC (transfusion guided by INR and platelet count), with

269 ol donor is safe in recurrent HE compared to SOC alone.

270 rimary outcome was safety of FMT compared to SOC using FMT-related serious adverse events (SAEs).

271 or cephalosporin, comparing interventions to SOC using multivariable logistic regression.

272 AUC 0.73 (95% CI, 0.68-0.77) was superior to SOC AUC 0.63 (95% CI, 0.58-0.68) (P < .001).

273 intricate with many channels contributing to SOCs.

274 re than half (57%) of the additional topsoil SOC is predicted to have a short turnover time (c. 20 ye

275 consistent with observed changes in topsoil SOC concentration in the late 20(th) Century, derived fr

276 l evolution (at 250 m resolution) of topsoil SOC driven by climate change and land use change for Fra

277 s) to pasture (C4 plants) by analysing total SOC stocks and the natural abundance of the stable isoto

278 In general, total SOC stocks at 30 cm depth in the forest were similar for

279 ount and annual precipitation, and the total SOC stock at the beginning of the trials.

280 ntly greater than that for PRM gas trapping (SOC = 36% +/- 18; P = .01).

281 2; P = .001) and moderate (for gas trapping, SOC = 34% +/- 28; for emphysema, SOC = 7% +/- 15; P = .0

282 ema in patients with mild (for gas trapping, SOC = 36% +/- 28; for emphysema, SOC = 1% +/- 2; P = .00

283 opose a novel activation mechanism for TRPC1 SOCs in VSMCs, in which store depletion induces formatio

284 at PKC is obligatory for activation of TRPC1 SOCs in VSMCs, and the present study investigates if the

285 GF109203X all inhibited activation of TRPC1 SOCs, and U73122 and GF109203X also reduced store-operat

286 erated PLC activity and stimulation of TRPC1 SOCs.

287 Swaziland were randomized 1:1 to CIS versus SOC.

288 ign disease: AUC 0.77 (95% CI, 0.71-0.83) vs SOC AUC 0.66 (95% CI, 0.58-0.72) (P < .001).

289 % in the SOC group (relative risk [RR]CIS vs SOC = 1.58, 95% CI 1.05-2.39).

290 gnosis versus 16% of the SOC group (RRCIS vs SOC = 9.13, 95% CI 1.65-50.40).

291 in VSMCs and how Homer1 contributes to VSMC SOCs, proliferation, and migration leading to neointima

292 t contain intrachain platinum atoms, to weak SOC polymers, to C60 films, where the SOC is predominant

293 lusion to limit C input, and to test whether SOC decomposition is driven by substrate lability under

294 is a critical step in understanding whether SOC sequestration can be an effective climate mitigation

295 % to -60%) vs 2% (95% CI, -5% to -0.2%) with SOC alone (P < .001).

296 ation of osseous features when compared with SOC MR image sets.

297 Compared with SOC, the adjusted hazard ratio was 0.98 (95% CI, 0.80 to

298 e confirmation was cost-saving compared with SOC.

299 5-year budget by $310/patient compared with SOC.

300 g pasture establishment were correlated with SOC changes.