ライフサイエンスコーパス: He

1 He also downloads a mobile nutrition application she rec

2 He also had a small nodule on the volar surface of his r

3 He also received three different combinations of chemoth

4 He argues that the version of (1) that involves (2) is t

5 He attended Stuyvesant High School in New York City, Phi

6 He attributes the failure of Multiple Risk Factor Interv

7 He attributes the failure of the Multiple Risk Factor In

8 He became tachycardic, tachypneic, and hypotensive.

9 He commended and criticised Darwin on specific issues pe

10 He complained of sudden painless profound visual loss in

11 He denied alcohol abuse or recreational drug use.

12 He developed seizures and acute renal failure requiring

13 He did not have any allergies.

14 He did not report fever, night sweats, or hemoptysis.

15 He did not require intensive care unit care or ventilati

16 He draws in his work on two models of joint action, one

17 He enrolls with enthusiasm, and, feeling empowered, crea

18 He eventually required treatment with ecluzimab therapy;

19 He exhibited a moderately severe and circumscribed impai

20 He experienced 6 acute rejections, and none were resista

21 He experienced episodes of marked ocular hypertension (5

22 He experienced mild gut graft-versus-host disease.

23 He experienced swallowing difficulties, tinnitus, and fe

24 He first developed oral mucosa symptoms and vomiting at

25 He had a history of frequent bruises and PC deficiency,

26 He had a normal haemoglobin, mean cell volume, platelet

27 He had an excellent clinical recovery within 4 days and

28 He had corneal abrasions due to minor repeated corneal t

29 He had eaten landlocked ayu fish (Plecoglossus altivelis

30 He had no other comorbidities and no family history of c

31 He had no symptoms of ototoxicity or peripheral neurotox

32 He had previously experienced intermittent episodes of s

33 He had primarily surgery followed by three rounds of rep

34 He has delivered the Paul Dudley White International Lec

35 He has published seminal work demonstrating the importan

36 He has received awards including the Paul Dudley White A

37 He has since been able to re-integrate into his communit

38 He immigrated to the United States as an adult more than

39 He initially posited that nonnative species closely rela

40 He made fundamental contributions to our understanding o

41 He made many relevant discoveries regarding Kawasaki Dis

42 He makes a helpful suggestion to reconnect diagnosis wit

43 He noticed the symptoms 8 months after starting the trea

44 He obtained a BSc in aerospace engineering from the Univ

45 He presented the Edwin Bierman Award Lecture, "We Know M

46 He presented with multiple areas of superficial white ci

47 He proposed that living organisms were specific examples

48 He provides us with a vision of how science and scientis

49 He received his PhD in biochemistry and MD at the Univer

50 He received his undergraduate degree from Cornell Univer

51 He reported a 10-kg weight loss over 4 months but denied

52 He reported a 4-month history of nonproductive cough, 5-

53 He reports no symptoms of hyperglycemia, such as frequen

54 He responded to 4-week period of induction prednisolone

55 He returns to discuss his results and potential manageme

56 He started Pica eating disorder (sand and sponge) due to

57 He subsequently seroconverted for syphilis.

58 He subsequently went on to residency and fellowship at C

59 He successfully combined five artificial somatosensory p

60 He then divides prognostic uncertainty into developmenta

61 He ultimately was extubated and discharged home.

62 He underwent a left radical orchiectomy, and pathology s

63 He underwent abdominal X-ray, ultrasound (US) and comput

64 He underwent left inguinal orchiectomy, which disclosed

65 He underwent re-excision of melanoma but 2 months later

66 He was a pioneer in targeted cancer therapy and was inst

67 He was accompanied by fever which was persist for severa

68 He was admitted 8 days later and tested positive for SAR

69 He was admitted to evaluate progressive shortness of bre

70 He was also interviewed at the meeting by Vincent Racani

71 He was also noted to have some mild developmental delay

72 He was also the first to pith a frog, concluding that pi

73 He was appointed Associate Professor in 1980, and he ass

74 He was born in Hong Kong and received his medical degree

75 He was delivered at full term via spontaneous vaginal de

76 He was diagnosed as having immediate-type food allergies

77 He was diagnosed with anaphylaxis upon visiting our emer

78 He was elected to the Institute of Medicine in 2005.

79 He was immediately resuscitated using crystalloids, supp

80 He was in a septic shock with multiple organ failure up

81 He was initially suspected to have concurrent gallstone

82 He was initially treated as acute appendicitis, undergoi

83 He was Knighted for Services to Science in 2011 and beca

84 He was not doing well during fare-up.

85 He was on treatment for androgenic alopecia with topical

86 He was originally from north Sudan and eventually moved

87 He was placed on a 6 weeks course of topical treatment w

88 He was quite active but reported discomfort from the bul

89 He was referred to the medical oncology team to discuss

90 He was seen in consultation for management of recurrent

91 He was subjected to emergency endovascular treatment.

92 He was successfully treated using laser photocoagulation

93 He was successfully treated with antibiotic therapy and

94 He was treated with high doses of corticosteroids and ac

95 He was visibly nervous in the unfamiliar institutional e

96 He would soon be one of the 4 founders of the Johns Hopk

97 alyzing a larger set of (noble) gases (N(2), He, Ar, and Kr) combined with a physically meaningful ex

98 lective molecular separation of He and O(2), He and CO(2), and He and N(2).

99 either have a rocky core enveloped in a H(2)-He gaseous envelope (gas dwarfs) or contain a significan

100 mponents(12-15), its N(2)/(36)Ar and N(2)/(3)He ratios are indistinguishable from those of the convec

101 ndmember delta(15)N, N(2)/(36)Ar and N(2)/(3)He values.

102 5)N/(14)N from air), N(2)/(36)Ar and N(2)/(3)He.

103 MRI with inhaled hyperpolarized helium 3 ((3)He) allows for functional and structural imaging of the

104 ng proton MRI to hyperpolarized helium 3 ((3)He) MRI ventilation and validated using a sixfold valida

105 dinal changes in hyperpolarized helium 3 ((3)He) MRI ventilation defects in study participants with m

106 Hyperpolarized (HP) helium 3 ((3)He) MRI ventilation maps were co-registered with thoraci

107 MRI with that of hyperpolarized helium 3 ((3)He) MRI with respect to quantitative ventilation measure

108 e-matched CT and hyperpolarized helium 3 ((3)He) MRI.

109 months, suggests that we either sampled a (3)He/(4)He rich magma already in place in the lower ERZ or

110 he ratio R and normalized to the accepted (3)He/(4)He ratio of 1.40 E-06 (R(a)), ranges from peak val

111 Hyperpolarized (129)Xe and (3)He are gases used as contrast media for magnetic resonan

112 tilation MRI (r(S) = -0.51, P < .001) and (3)He MRI (r(S) = -0.61, P < .001) ventilation defect perce

113 The mean DSC for DL ventilation MRI and (3)He MRI ventilation was 0.91 +/- 0.07.

114 exhibit increasing mantle CO(2) flux and (3)He/(4)He ratios as the rift transitions from Archaean (c

115 We interpret the relationships between (3)He/(4)He values, hotspot buoyancy flux, and upper-mantle

116 Even at the maximum classical (3)He/(4)He diffusivity ratio of 1.15, the expected R would

117 Herein we report on elevated (3)He/(4)He ratios in steaming vents in the lower ERZ from

118 e (13)C NMR spectrum of the endofullerene (3)He@C(60) displays a doublet structure due to a J-couplin

119 ection of the deuterium burning D(p,gamma)(3)He reaction.

120 othesis is that, while some hotspots have (3)He/(4)He values ranging from low to high, other hotspots

121 ical modelling and the occurrence of high (3)He/(4)He (that is, primordial) signatures in some volcan

122 Thus, high (3)He/(4)He and anomalous (182)W are preserved exclusively

123 he long-term preservation of ancient high (3)He/(4)He and anomalous (182)W in the geodynamic context

124 subducted, recycled crust-relate to high (3)He/(4)He and anomalous (182)W.

125 t Hawaii and Iceland, can host rare, high (3)He/(4)He isotopic ratios (up to 50 times the present atm

126 He-C-Pb-Sr isotope variability, with high (3)He/(4)He ratios related to higher helium concentrations.

127 arth-supporting an ancient origin of high (3)He/(4)He.

128 es-are more buoyant and entrain both high-(3)He/(4)He and low-(3)He/(4)He material.

129 This indicates that a less degassed, high-(3)He/(4)He deep mantle source infiltrates the transition z

130 This can be explained if the high-(3)He/(4)He domain is denser than low-(3)He/(4)He mantle co

131 We show that high-(3)He/(4)He mantle domains with anomalous (182)W have low W

132 components hosted in plumes, and if high-(3)He/(4)He material is entrained from the deep mantle only

133 Only high-(3)He/(4)He OIB exhibit anomalous (182)W-an isotopic signat

134 Rare high-(3)He/(4)He signatures in ocean island basalts (OIB) erupte

135 data on global OIB, show that the highest-(3)He/(4)He and the largest-magnitude (182)W anomalies are

136 provide geochemical data for the highest-(3)He/(4)He lavas from Iceland (up to 42.9 times atmospheri

137 ntage (VDP) was correlated with VDP at HP (3)He MRI (r = 0.90, P < .001).

138 Both model-predicted and HP (3)He MRI VDP were correlated with forced expiratory volume

139 of 0.82 (95% CI: 0.82, 0.83) when the HP (3)He MRI ventilation maps were used as the reference stand

140 aging metrics from in-vivo hyperpolarized (3)He DW MRI are sensitive to longitudinal changes in a coh

141 (rho = -0.66, P < .001) or hyperpolarized (3)He MRI (rho = -0.75, P < .001) were significantly correl

142 dividually from OE MRI and hyperpolarized (3)He MRI by using the same automated quantification tool.

143 performance compared with hyperpolarized (3)He MRI for quantitative measures of ventilation defects

144 and Methods Spirometry and hyperpolarized (3)He MRI were evaluated in participants with mild-to-moder

145 pulmonary function tests, hyperpolarized (3)He MRI, and OE MRI.

146 Both OE MRI-based VDP and hyperpolarized (3)He MRI-based VDP demonstrated good repeatability (ICC =

147 nchodilator spirometry and hyperpolarized (3)He MRI.

148 P < .001) VDP reported at hyperpolarized (3)He MRI.

149 e asthma were scanned with hyperpolarized (3)He MRI.

150 ction technologies currently used involve (3)He-gas-filled proportional counters(6) and light scintil

151 the discovery of superfluidity in liquid (3)He.

152 sociated with recycled materials have low (3)He/(4)He and lack anomalous (182)W.

153 susceptible to being overprinted with low (3)He/(4)He and normal (not anomalous) (182)W characteristi

154 to high, other hotspots exhibit only low (3)He/(4)He ratios.

155 igh-(3)He/(4)He domain is denser than low-(3)He/(4)He mantle components hosted in plumes, and if high

156 and entrain both high-(3)He/(4)He and low-(3)He/(4)He material.

157 ospheric ratio, Ra) compared to the lower (3)He/(4)He ratios identified in mid-ocean-ridge basalts th

158 le plumes, those with the highest maximum (3)He/(4)He ratios have high hotspot buoyancy fluxes and ov

159 plume-fed hotspots with only low maximum (3)He/(4)He ratios.

160 en plotted versus temperature, the narrow (3)He net partial pressure peak reveals at least three shar

161 this field and enable the replacement of (3)He counters by semiconductor-based neutron detectors.

162 d engineering aspects of a field-portable (3)He/(4)He ratio detector, we found elevated ratios at com

163 s bearing upon designs for field portable (3)He/(4)He ratio detectors aimed at earthquake and volcani

164 il loss of cosmic ray spallation products (3)He and (21)Ne enabled us to estimate that the irradiated

165 Results (3)He ADC and Lm(D) were reproducible (mean Bland-Altman an

166 ow-energy industrial enrichment of scarce (3)He from natural sources on Earth, and for radiogenic and

167 Here we show that in superfluid (3)He the role of bound states is more subtle: when a macro

168 raightforward to apply them in superfluid (3)He which can be routinely cooled to below 100 muK.

169 ly solid-state analogue to the superfluid (3)He-A phase(1,2), with an odd-parity order parameter that

170 The (3)He enrichment relative to (4)He in lab air, expressed as

171 The (3)He neutron spin filters are used in conjunction with spe

172 ude 77.5 +/- 0.2 mHz at 340 K between the (3)He nucleus and a (13)C nucleus of the enclosing carbon s

173 or capable of sub-daily monitoring of the (3)He/(4)He ratio.

174 sly low values of (4)He relative to their (3)He/(4)He ratio, similar to previous findings there and s

175 study, 18 participants with IPF underwent (3)He DW MRI at 1.5 T and 11 participants underwent an iden

176 entilation MRI was highly correlated with (3)He MRI ventilation defect percentage (r(S) = 0.83, P < .

177 As compared with (3)He MRI, DCNN model ventilation maps had a mean r value o

178 ntum liquid droplet is examined through a (4)He cluster by removing the attractive tail in the intera

179 ains with anomalous (182)W have low W and (4)He concentrations compared to recycled materials and are

180 r distribution of the emitted neutron and (4)He.

181 f groundwater tracer tests with dissolved (4)He.

182 odelling and the occurrence of high (3)He/(4)He (that is, primordial) signatures in some volcanic roc

183 Thus, high (3)He/(4)He and anomalous (182)W are preserved exclusively in man

184 g-term preservation of ancient high (3)He/(4)He and anomalous (182)W in the geodynamic context of cru

185 cted, recycled crust-relate to high (3)He/(4)He and anomalous (182)W.

186 ed with recycled materials have low (3)He/(4)He and lack anomalous (182)W.

187 more buoyant and entrain both high-(3)He/(4)He and low-(3)He/(4)He material.

188 tible to being overprinted with low (3)He/(4)He and normal (not anomalous) (182)W characteristic of s

189 n global OIB, show that the highest-(3)He/(4)He and the largest-magnitude (182)W anomalies are found

190 ndicates that a less degassed, high-(3)He/(4)He deep mantle source infiltrates the transition zone, w

191 Even at the maximum classical (3)He/(4)He diffusivity ratio of 1.15, the expected R would be on

192 This can be explained if the high-(3)He/(4)He domain is denser than low-(3)He/(4)He mantle componen

193 ii and Iceland, can host rare, high (3)He/(4)He isotopic ratios (up to 50 times the present atmospher

194 de geochemical data for the highest-(3)He/(4)He lavas from Iceland (up to 42.9 times atmospheric) wit

195 )He/(4)He domain is denser than low-(3)He/(4)He mantle components hosted in plumes, and if high-(3)He

196 We show that high-(3)He/(4)He mantle domains with anomalous (182)W have low W and (

197 nents hosted in plumes, and if high-(3)He/(4)He material is entrained from the deep mantle only by th

198 train both high-(3)He/(4)He and low-(3)He/(4)He material.

199 Only high-(3)He/(4)He OIB exhibit anomalous (182)W-an isotopic signature in

200 neering aspects of a field-portable (3)He/(4)He ratio detector, we found elevated ratios at comparati

201 ing upon designs for field portable (3)He/(4)He ratio detectors aimed at earthquake and volcanic erup

202 io R and normalized to the accepted (3)He/(4)He ratio of 1.40 E-06 (R(a)), ranges from peak values of

203 w values of (4)He relative to their (3)He/(4)He ratio, similar to previous findings there and suggest

204 able of sub-daily monitoring of the (3)He/(4)He ratio.

205 it increasing mantle CO(2) flux and (3)He/(4)He ratios as the rift transitions from Archaean (cratoni

206 mes, those with the highest maximum (3)He/(4)He ratios have high hotspot buoyancy fluxes and overlie

207 ic ratio, Ra) compared to the lower (3)He/(4)He ratios identified in mid-ocean-ridge basalts that for

208 Herein we report on elevated (3)He/(4)He ratios in steaming vents in the lower ERZ from sample

209 b-Sr isotope variability, with high (3)He/(4)He ratios related to higher helium concentrations.

210 -fed hotspots with only low maximum (3)He/(4)He ratios.

211 gh, other hotspots exhibit only low (3)He/(4)He ratios.

212 , suggests that we either sampled a (3)He/(4)He rich magma already in place in the lower ERZ or a sha

213 Rare high-(3)He/(4)He signatures in ocean island basalts (OIB) erupted at v

214 s is that, while some hotspots have (3)He/(4)He values ranging from low to high, other hotspots exhib

215 interpret the relationships between (3)He/(4)He values, hotspot buoyancy flux, and upper-mantle shear

216 upporting an ancient origin of high (3)He/(4)He.

217 Superfluidity, first discovered in liquid (4)He, is closely related to Bose-Einstein condensation (BE

218 district) with anomalously low values of (4)He relative to their (3)He/(4)He ratio, similar to previ

219 se diagram evolves from the known case of (4)He, as the system is made more (and less) quantum, and c

220 an be successfully operated in superfluid (4)He, it is straightforward to apply them in superfluid (3

221 nection of quantum vortices in superfluid (4)He, using submicrometer frozen air tracers.

222 ity function (DPDF) analysis we show that (4)He atoms in the Bose-Einstein condensate have environmen

223 The (3)He enrichment relative to (4)He in lab air, expressed as the ratio R and normalized t

224 nent isotherms and by mixed gas (CO(2)/CH(4)/He) breakthrough experiments.

225 A He-pressure medium was used to minimize the effect of un

226 L., Kakazu, A., He, J., Bazan, H.

227 clues regarding the survival of the ancient He and W signatures in Earth's mantle.

228 separation of He and O(2), He and CO(2), and He and N(2).

229 ation potentials, the helium ions He(2+) and He(+) were the first to combine with free electrons, for

230 ader system is used with the 100 MeV/n H and He beams to provide a nearly continuous distribution of

231 Different reactant gases (Ar, He, O(2), and N(2)) and reactant gas mixtures are tested

232 The task force endorsed the "Be He@lthy, Be Mobile" WHO initiative and debated the quali

233 The interaction between He atoms and K-PHI is partially originating from charge

234 In this issue of Blood, He et al discuss their discovery that methylation of fms

235 In this issue of Blood, He et al show that a tumor necrosis factor alpha (TNFalp

236 Two recent publications in Immunity by He et al. (2019) report on the diurnal regulation of the

237 t within KwaZulu-Natal, South Africa, have C-He isotope systematics that support an origin from degas

238 a precision better than 1% for N2, O2, CO2, He, Ar, 2% for Kr, 8% for Xe, and 3% for CH4, N2O and Ne

239 aking sample; while for continuous cultures, He (or other inert gases) is used as an internal tracer

240 gases with small effective diameters (i.e., He, H(2) , and O(2) ).

241 The energy of formation of endohedral He@F(8)@Ge(60)F(52) is exothermic by -10.4 kcal mol(-1),

242 The endohedral He/Li@F(8)@Ge(60)F(52) cages are significantly more stab

243 ubble forms around the localized excitation (He[Formula: see text]) within 1 ps.

244 We found extreme He-C-Pb-Sr isotope variability, with high (3)He/(4)He ra

245 radiation stability, we conducted the first He(2+) ion irradiation study of a metal-organic framewor

246 the diffusion of radiogenic elements (e.g., He and Pb) in host mineral.

247 text]), negative pions (- pai), and helium (He) ion beams resulted in 10, 17 and 1.3 times larger Gd

248 We demonstrate that even helium (He) gas molecules, which are known to have the lowest bo

249 xistence of founder effects: heterozygosity (He = 0.667) and allelic richness (Ar = 4.298) were simil

250 Content; 0.87) and expected heterozygosity (He = 0.79-0.82).

251 rozygosity (Ho) and expected heterozygosity (He) in these highly inbred lines were 0.291 and 0.359, r

252 a cochineal allergy.Current disease history: He has been suffering from atopic dermatitis, bronchial

253 nt on the diffusion of vacancy and implanted He atoms.

254 For experiments carried out in He, we observe the total CCS distributions to follow the

255 on is generally maximized by buffers rich in He or H(2) that elevate ion mobility and lead to promine

256 n achieved overall only with buffers rich in He or H(2).

257 to very small charge transfer interactions, He gas adsorption saturates at 8 at%, which however can

258 We found that, while interstitial He can modify the properties, a dose significantly large

259 igher ionization potentials, the helium ions He(2+) and He(+) were the first to combine with free ele

260 e stable than their parent exohedral isomers He/Li@Ge(60)F(52) by -182.46 and -49.22 kcal mol(-1), re

261 In this issue of the JCI, He et al. report on their employment of a battery of lin

262 We also consider the addition of Li, He, Cs, and Bi, to probe the utility of the exo/ endo ca

263 P., Lightle, R., Moore, T., Dimaano, M., He, T.

264 tion at room temperature to obtain a maximum He concentration of 5 at.

265 We measured He-Sr-Pb isotope ratios in superdeep diamond fluid inclu

266 the bubble collapses and releases metastable He[Formula: see text] at the droplet surface.

267 lity was examined using gamma-rays and 5 MeV He(2+) ions to simulate alpha particles.

268 the most electropositive elements, while Ne, He, and F remain the most electronegative ones.

269 No He bubbles were observed in the SiOC layers of the nanol

270 differential cross sections for inelastic NO-He collisions in the 0.2 to 8.5 centimeter(-1) range wit

271 The announcement of He Jiankui's germline editing of human embryos has been

272 eak surface interactions, such as binding of He or N(2) , yield significant state-dependent shifts, i

273 ything other than vociferous condemnation of He's announcement.

274 Implantation resulted in the formation of He bubbles and an increase in the average size of the Fe

275 We study double ionization of He driven by near-single-cycle laser pulses at low inten

276 in single-photon direct double ionization of He.

277 ity upon exposure to approximately 25 MGy of He(2+) ion irradiation.

278 We show that the presence of He atoms causes strong electron localization and makes t

279 promising selective molecular separation of He and O(2), He and CO(2), and He and N(2).

280 an adsorption energy of - 4.6 kJ mol(-1) per He atom.

281 arkable characteristics of negative polarity He-CTD.

282 rements were made with a new, field-portable He isotope detector capable of sub-daily monitoring of t

283 e Bell spin states for the "general reader." He then challenged the "physicist reader" to explain the

284 2018, news broke that the Chinese researcher He Jiankui had created the world's first genome-edited b

285 Zircon (U-Th)/He dates for basement below the Great Unconformity are 9

286 agreement with a previously published (U-Th)/He thermochronology profile, our model shows that rocks

287 Our ToF-SIMS results show that He ion irradiation leads to oxygen penetration into the

288 2008 and 2018 in 18 Centers enrolled in the He.Rc.O.Le.S. Italian register.

289 We show that the He and Ne isotopic and elemental signatures of the Yello

290 found to be true geometric minima, with the He atoms clearly located in the first shell around the a

291 activities were determined in laser-treated (He-Ne laser, 632 nm, 5 mW) common buckwheat (CBW) and ta

292 py of the formation of bubble lattices under He ion bombardment.

293 there and suggestive of a previously unknown He isotopic fractionation.

294 atly ameliorates the pressure increases upon He or H(2) aspiration.

295 Values of lambda obtained using He atoms compare favorably with known values for the bul

296 Mobility measurements were taken using He and N(2) as the drift gases.

297 ed shortly prior to and at the summit, where He Jiankui gave an account of his activities.

298 evidence of colonization was detected, with He increasing along the expansion front, while genetic d

299 solute collision cross sections (Omega) with He, N2, Ar, CO2, and N2O were measured for the 20 common

300 XRD, He-ion imaging, HR-TEM, EELS, PL, fluorescence lifetime