ライフサイエンスコーパス: erosion

1 is one of the key factors controlling water erosion.

2 ent of depleted soils with fresh bedrock via erosion.

3 ting sediment surface elevation and reducing erosion.

4 from fertilization to stabilization against erosion.

5 in) and significantly reduced initial enamel erosion.

6 n the tremor source related to volcanic vent erosion.

7 oral products to protect against caries and erosion.

8 injury, a process implicated in superficial erosion.

9 eight:device size ratio were associated with erosion.

10 als diagnostic of weathering, deposition and erosion.

11 energy gain can be strongly limited by head erosion.

12 n the deep Earth, or lost to space by impact erosion.

13 lated unconsolidated marine deposits to wind erosion.

14 telomere integrity from damage and telomere erosion.

15 here plant death resulted in increased marsh erosion.

16 plications such as hypotony and conjunctival erosion.

17 underwent ASD closure but did not develop an erosion.

18 , surface area, and size) and increased bone erosion.

19 nation and unloading due to deglaciation and erosion.

20 eight:device size ratio were associated with erosion.

21 l disruption and displacement/transport with erosion.

22 ediments in estuaries, and increased coastal erosion.

23 POC export is mostly controlled by physical erosion.

24 , highlighting regions vulnerable to genetic erosion.

25 rait involved at least two major episodes of erosion.

26 organisms and the associated risk of genetic erosion.

27 alence of non-arc magmatism and the enhanced erosion.

28 ducts might confer protection against enamel erosion.

29 tion even in patients presenting with device erosion.

30 fore-reef habitats are now in a phase of net erosion.

31 sion in the same solution followed by 10-min erosion.

32 assessed wound closure of topically treated erosions.

33 illary hyperplasia developed without surface erosions.

34 uctural lesions, in particular sclerosis and erosions.

35 rees ; P=0.03), a higher frequency of plaque erosion (11.4% versus 0.6%; P=0.04), and a lower prevale

36 itis (3 eyes), endophthalmitis (3 eyes), GDD erosion (2 eyes), and retinal detachment (5 eyes).

37 y disease were more likely to exhibit plaque erosion (8.6% versus 0.3%; P=0.03) and a smaller lipid a

38 as mechanisms that contribute to superficial erosion, a cause of acute coronary syndrome of likely gr

39 xture parameters can differentiate simulated erosion, abrasion, and erosion-abrasion lesions on human

40 (both factorial 4 x 2), with 4 lesion types (erosion, abrasion, erosion-abrasion, and sound [no lesio

41 plsar was able to differentiate erosion from erosion-abrasion (allP< 0.05).

42 trates; only Asfc differentiated erosion and erosion-abrasion enamel lesions (allP< 0.05).

43 part 2, only Asfc differentiated erosion and erosion-abrasion lesions from the sound (no lesion) cont

44 d Tfv were able to differentiate erosion and erosion-abrasion lesions from the sound (no lesion) cont

45 fferentiate simulated erosion, abrasion, and erosion-abrasion lesions on human enamel and dentin.

46 d Tfv were able to differentiate erosion and erosion-abrasion lesions, despite their complicated surf

47 2), with 4 lesion types (erosion, abrasion, erosion-abrasion, and sound [no lesion; control]) and 2

48 st, corresponding to anomalously large beach erosion across the region.

49 there were several relative risk factors for erosion after ASD closure with the Amplatzer septal occl

50 The risk factors for cardiac erosion after device closure are not yet clear.

51 3 women who presented with prolonged facial erosions after cosmetic resurfacing procedures, specific

52 There were 2 incidents of conjunctival erosion and 1 inferotemporal macula-on retinal detachmen

53 a, and to the spatially variable patterns of erosion and accretion along the large deltas of the main

54 and provides a reliable tool to predict the erosion and accretion processes controlling the evolutio

55 mption, and of different magnitudes for soil erosion and biodiversity.

56 assessment of their rheological properties, erosion and biomolecule release in vitro.

57 Oxidative DNA damage triggers telomere erosion and cellular senescence.

58 lymer, which slows down drug release through erosion and diffusion mechanisms.

59 in both substrates; only Asfc differentiated erosion and erosion-abrasion enamel lesions (allP< 0.05)

60 In part 2, only Asfc differentiated erosion and erosion-abrasion lesions from the sound (no

61 Asfc, Sa, and Tfv were able to differentiate erosion and erosion-abrasion lesions from the sound (no

62 Asfc, Sa, and Tfv were able to differentiate erosion and erosion-abrasion lesions, despite their comp

63 r(-1) (+/-7.08 SE), which accounted for both erosion and fragmentation of dead colonies.

64 Our findings of greater complexity in erosion and greater anisotropy in attrition confirm our

65 es and debris flows can lead to serious bank erosion and inundation of populated areas near rivers.

66 otential land losses associated with coastal erosion and lengthening of the coastal ice-free season f

67 ay result from seasonality, climate history, erosion and mineralogy.

68 e enhanced floods or droughts, stronger soil erosion and nutriment loss, questioning the sustainabili

69 mple, attempting a mass balance between soil erosion and production, which indicates that barren land

70 I mesh sling was associated with the highest erosion and repeated intervention risk, while mesh sling

71 risk, while mesh sling alone had the lowest erosion and repeated intervention risk.

72 zed to influence landscape evolution through erosion and sediment transport by rivers.

73 ressive hybridisation may range from genomic erosion and species collapse to rapid adaptation and spe

74 Erosion and splashing of PFCs can contaminate the plasma

75 Feedbacks between climate, erosion and tectonics influence the rates of chemical we

76 hat microwear complexity would be greater in erosion and that anisotropy would be greater in attritio

77 ischarging ears, especially to look for bone erosion and the integrity of the ossicles.

78 heres appeared to be controlled initially by erosion and then by a second mechanism after day 21, whi

79 significant marine and terrestrial carbonate erosion and to deleterious effects on coral reef and biv

80 ing, the latter likely caused by sublimation erosion and/or collapse.

81 sclerosis, change in the joint space width, erosions and ankylosis.

82 bodies was associated with the occurrence of erosions and blisters (r = 0.985; P = .006) but not urti

83 bcutaneous injections of anti-mLAMalpha3 IgG erosions and crusts occurred predominantly around the sn

84 All 3 patients noted significant healing of erosions and plaques starting from the peripheral aspect

85 performed to examine the occurrence of mesh erosions and subsequent reintervention.

86 and 19 M+ male mice developed more cartilage erosions and thicker subchondral bone plates after DMM t

87 s, along with luminal aggressors, results in erosions and ulcers, with potential complications of ble

88 esions and the number of subjects with large erosions and/or ulcers after 14 days of exposure.

89 roups, including 2 wear types (attrition and erosion) and 2 locations (anterior and posterior teeth;

90 EN1) complex involved in preventing telomere erosion, and genes such as REST and FOXO4 that have been

91 risk, increasing biodiversity, reducing soil erosion, and improving nutrient- and water-use efficienc

92 eir nonculprit plaques exhibited more plaque erosion, and less cholesterol and calcium content.

93 tions are involved in cartilage damage, bone erosion, and resorption processes during osteoarthritis.

94 d worldwide because of land use change, wave erosion, and sea-level rise.

95 that interactions between ice flow, glacial erosion, and sediment transport drive these cycles, whic

96 Earth, has been obscured by the weathering, erosion, and tectonism that followed its formation.

97 e attribute to cometary-specific weathering, erosion, and transient events driven by exposure to sunl

98 anifesting with sub-lamina densa blistering, erosions, and chronic ulcers.

99 Characterized by sterile pustules, erosions, and crusts, EPD is difficult to treat and heal

100 haracterized by chronic, recurrent vesicles, erosions, and maceration in flexural areas.

101 ount of water needed to create the cavity by erosion are of significant importance for understanding

102 pecific mechanisms by which climate controls erosion are poorly understood.

103 y oiled marshes have experienced accelerated erosion as a result of the spill, these habitat impacts

104 Instead of leading to plasmaspheric erosion as geomagnetic storms do, substorms initiated on

105 The data show that foreshore sand erosion as wave height increases results in elevated Esc

106 s deformed by applied stress and by chemical erosion as well.

107 for estimating the degree of uncertainty of erosion assessments.

108 What controls erosion at a microscopic level remains debated, especial

109 sponge interactions can alter reef accretion/erosion balance and are important to predict trends on c

110 of not only wave height (and associated sand erosion) but also the time elapsed since a preceding per

111 bed shear stresses exceed the threshold for erosion by a small amount.

112 r 40 cycles of recycling and after suffering erosion by corrosive media.

113 Understanding soil erosion by water is essential for a range of research ar

114 Dover Strait by lake overspill, plunge pool erosion by waterfalls and subsequent dam breaching.

115 However, lateral erosion can lead to rapid marsh loss as marshes build ve

116 deficiency, which was almost universal among erosion cases, there were several relative risk factors

117 ted to documented EDEL (category 1: erythema/erosion; category 2: ulcer).

118 We also show that infection phenotypes (fin erosion, cell apoptosis and muscle degeneration) are dir

119 Thrombi because of superficial intimal erosion characteristically complicate matrix-rich athero

120 hange, land management and land degradation (erosion, compaction, sealing and salinization).

121 the amount of mesh used and subsequent mesh erosions, complications, and invasive repeated intervent

122 Telomere erosion contributes to human diseases ranging from BM fa

123 improvement and ammonium mitigation for wind erosion control and other applications.

124 Both microsphere formulations exhibited erosion-controlled release in vitro, indicated by simila

125 Even if erosion could potentially induce a sink for atmospheric

126 RATIONALE: Superficial erosion currently causes up to a third of acute coronary

127 All specimens were then exposed to five erosion cycles, each consisted of a further 30 min immer

128 of cystic or adipose contents and of sacral erosion/destruction.

129 he risk of repeated surgery with concomitant erosion diagnosis was also the highest in the vaginal me

130 eshold in wave energy above which salt marsh erosion drastically accelerates.

131 a potential overall increase in global soil erosion driven by cropland expansion.

132 Direct comparisons of erosion during pulsed heat loading between PFC candidate

133 sses of surface clay caused by periodic wind erosion (dust) and rainfall inundation (flood) events.

134 h an autosomal dominant epithelial recurrent erosion dystrophy (ERED).

135 e three solutions against citric acid enamel erosion, enamel specimens were immersed in the correspon

136 We advocate that subduction erosion enhanced by abundant seamount subduction at 9-11

137 Here we show that deep ice-sheet erosion-enough to expose basement rocks-has occurred in

138 causative mutation in our recurrent corneal erosion families, and its presence in 4 independent fami

139 We find that the spatial organization of the erosion flux is heterogeneous in space and occurs along

140 ows [Formula: see text], where J is the mean erosion flux.

141 We concluded that erosion fluxes were in the same order of current carbon

142 eatest geometric means were noted in dentine erosion for complexity and dentine attrition for anisotr

143 es, whereas eplsar was able to differentiate erosion from erosion-abrasion (allP< 0.05).

144 here were two phases of transgressional soil erosion from terrace surfaces during lake-level rise in

145 We found that hot spot erosion governs the preferential usage of some Prdm9 all

146 Skeletal erosion has been found to represent an independent progn

147 This explains why net erosion has occurred in some areas of the subaqueous del

148 s all the more surprising given that genomic erosion has resulted in the loss of transcription fideli

149 ed regions to increased coastal flooding and erosion hazards.

150 Clinical response (healing of erosions, improvement in erythema, and alleviation of pa

151 in 2, device embolization in 1, and cardiac erosion in 3.

152 Our results indicate the severity of wind erosion in a desert-oasis ecotone and thus encourage ado

153 tly diminished RANKL positive cells and bone erosion in CIA mice.

154 a target candidate for the treatment of bone erosion in inflammatory arthritis.

155 to prevent rapid allele fixation and hotspot erosion in populations.

156 reased COMMD1 expression with decreased bone erosion in rheumatoid arthritis.

157 ning to yield enantioenriched amines with no erosion in stereochemical integrity.

158 fibroblasts (SF) and the development of bone erosion in the collagen-induced arthritis (CIA) mouse.

159 In particular, the role of erosion in the global C cycle is not totally disentangle

160 We also find multiple signatures of genetic erosion in the two remnant Iberian lynx populations, inc

161 dies of Pt(111) homoepitaxial growth and ion erosion in ultrahigh vacuum.

162 was brought about by subsidence and glacial erosion in West Antarctica during the Late Oligocene and

163 e microwear characteristics of attrition and erosion in worn natural teeth, we scanned 50 extracted h

164 anti-DCC-treated mice, whereas there were no erosions in anti-Netrin-1/anti-Unc5b-treated-animals.

165 ntribute to antagonize inflammation and bone erosions in RA.

166 Micro-computed tomography showed bony erosions in untreated or anti-DCC-treated mice, whereas

167 pain or even physical disability (i.e. joint erosions) in HEDS patients.

168 olicies are needed to prevent or reduce soil erosion, in order to maintain soil health and productivi

169 line without erosion, the model suggested an erosion-induced sink of atmospheric C consistent with pr

170 at chromosome ends to compensate for the DNA erosion inherent in genome replication.

171 Glenoid morphology (version, vault depth, erosion), injury or disease (osteoarthritis, Bankart and

172 asal cell and papillary hyperplasia, surface erosions, intercellular space width, endoscopic grade of

173 To investigate this issue, we coupled soil erosion into a biogeochemistry model, running at 1 km(2)

174 ely to have an oversized device, and to have erosion into the aorta, than survivors.

175 ccluder is generally safe and effective, but erosion into the pericardial space or aorta has been des

176 bservations support that, for laminar flows, erosion is a dynamical phase transition that shares simi

177 While water erosion is identified as the most serious cause of soil

178 mography demonstrate that superficial plaque erosion is more common than previously thought.

179 e rate of hemodynamic compromise and cardiac erosion is rare.

180 btedly shaped by subaerial weathering and/or erosion, it is obvious that northern Shatsky Rise was re

181 Estimated coastal erosion losses were also larger for RCP8.5.

182 Coronary artery thrombosis caused by plaque erosion may be on the rise in an era of intense lipid lo

183 ile calculations suggest that foreshore sand erosion may be the dominant mechanism for releasing E. c

184 The impacts of climate change on soil erosion may bring serious economic, social and environme

185 ation of patients with of ACS resulting from erosion may permit a less invasive approach to managemen

186 re related to the occurrence of blisters and erosions may encourage further studies on the associatio

187 solution (250 x 250 m) global potential soil erosion model, using a combination of remote sensing, GI

188 nd therapeutic options for nonhealing facial erosions occurring after ablative procedures (carbon dio

189 osition of levees in some slope segments and erosion of a conduit in other segments.

190 ort due to resuspension of streambed solids, erosion of alluvial tailings, and overland flow.

191 ly of reworked, secondary contamination from erosion of anthropogenically labeled sediments elsewhere

192 and enantiodetermining with no evidence for erosion of cobalt alkyl stereochemistry by competing bet

193 results indicate that the long-term massive erosion of continental silicates was critical to the sub

194 ecies emitted during the progressive thermal erosion of cratonic lithosphere by plume activity or int

195 gle diastereoisomers and without significant erosion of ee, making this a practical catalytic synthes

196 aryl groups on the sulfenyl moiety prevented erosion of enantiomeric composition at these elevated te

197 and gamma-butyrolactone derivatives, without erosion of enantiomeric purity.

198 hols and tetrahydrofuran derivatives without erosion of enantiomeric purity.

199 -directed cyclopalladation, thereby avoiding erosion of enantioselectivity.

200 In addition, the time-dependent erosion of episodic details of traumatic memories might

201 Our results suggest that erosion of gene regulation by mutation load significantl

202 Many factors contribute to the erosion of muscle mass following burn trauma and we prop

203 Many factors contribute to the erosion of muscle mass following burn trauma, and we hav

204 eighborhood crime, lower housing prices, and erosion of neighborhood social cohesion.

205 The findings suggest that erosion of nuclear gatekeeping function, which is found

206 DNA-binding specificity of PRDM9 and gradual erosion of PRDM9-binding sites by gene conversion will a

207 2003 and peaked in 2005 caused an unexpected erosion of resilience and a shift to an ASS; both for th

208 igand (RANKL) is critically involved in bone erosion of rheumatoid arthritis (RA).

209 ed weathering caused by accelerated physical erosion of rocks due to elevated climate-related mechani

210 nces of many other minerals suggest enhanced erosion of Rodinian volcanic arcs and orogens.

211 ed storminess are expected to accelerate the erosion of soft-cliff coastlines, threatening coastal in

212 s cannot be accounted for solely by the slow erosion of telomeres due to incomplete replication that

213 eral dissolution alone suggest that there is erosion of the altered layer as it develops.

214 t safety practice was jeopardized because of erosion of the clinical disposition.

215 ycoproteins as a nutrient source, leading to erosion of the colonic mucus barrier.

216 These support a model of initial erosion of the Dover Strait by lake overspill, plunge po

217 actions proceed with high yields and without erosion of the ee value of the parent beta-hydroxy ynami

218 In 2 patients, full-thickness erosion of the esophageal wall with partial endoluminal

219 Slower elongation led to erosion of the GTP cap and an increase in the frequency

220 of Victoria crater and their minimum age by erosion of the meteorites.

221 logeographers will continue to contribute to erosion of the simple vicariance vs. dispersal paradigm,

222 To protect from erosion of the tube in glaucoma drainage device (GDD), t

223 ation and a concomitant increase in top-down erosion of the upper surface of the deep brine layer by

224 recent asthenospheric upwelling and thermal erosion of thickened lithosphere, which is spatially con

225 The results show that erosion of X. laevis genes and functional regulatory ele

226 quartz sand removed by deep, ongoing glacial erosion on land and deposited offshore in the marine sed

227 ce of epithelial desquamation, erythema, and erosions on gingival tissue is usually described in the

228 the system spontaneously evolves toward the erosion onset.

229 No epithelial erythema, erosions, or ulcerations were seen.

230 urial and that alternative tectonic drivers (erosion, outgassing) provide testable and plausible expl

231 We also study the erosion patterns formed underneath a sublimating block o

232 The Reevaluating the Inhibition of Stress Erosions Pilot Trial determined the feasibility of under

233 Erosion potential is an important indicator of delta vul

234 Here, we investigate the erosion potential of the Yangtze Delta.

235 hannel incision of the main gully, and sheet erosion processes.

236 rth's surface requires understanding glacial erosion processes.

237 decreased significantly in patients without erosion progression.

238 itive than previously thought to continental erosion (providing lithogenic particles to the ocean), p

239 d a significant correlation between upstream erosion rate and local [Formula: see text] at sites wher

240 includes this additional mechanism, with the erosion rate based on the thickness of the altered layer

241 2 gas cluster ion beam (O2-GCIB) exhibits an erosion rate comparable to the frequently used O2(+) pro

242 Our results show two slowdowns in erosion rate, one from approximately 6.1-5.2 Ma and anot

243 We estimated that 143 of 187 Mha have C erosion rates <0.05 Mg C ha(-1) yr(-1), although some ho

244 This pattern parallels patterns in erosion rates (and hence sediment supplies).

245 Finally, this study demonstrates that paleo-erosion rates can be a powerful proxy for ancient contin

246 sed on a large dataset of salt marsh lateral erosion rates collected around the world, here, we deter

247 shes to violent storms and their predictable erosion rates during moderate events should be taken int

248 gravel-bedded rivers and >600 (10)Be-derived erosion rates from across North America to explore the h

249 l impacts on marsh edge erosion, with higher erosion rates occurring for ~1-2 years after the spill a

250 We address this question using erosion rates of ancient watersheds to constrain Mio-Pli

251 ose geomorphic environments with the highest erosion rates worldwide.

252 to experience the highest estimates of soil erosion rates.

253 er Neogene cooling or increasing Pleistocene erosion rates.

254 tribute less than 1% to long-term salt marsh erosion rates.

255 y records, as well as between global CO2 and erosion records.

256 We challenge the previous annual soil erosion reference values as our estimate, of 35.9 Pg yr(

257 ecord a detailed history of accumulation and erosion related to climate processes.

258 easing threats, such as coastal flooding and erosion, saltwater intrusion and wetland degradation.

259 ne ice cap, while accounting for postglacial erosion, sediment deposition and spatial variations in l

260 ncentrations are geographically unrelated to erosion sensitive areas, to point-source P-emissions or

261 Erosion shapes our landscape and occurs when a sufficien

262 placebo application 3 times daily at 2 open erosion sites for 2 weeks.

263 Limited stereochemical erosion stems from the intervention of a trisolvated-mon

264 Plaque rupture or erosion stimulates platelet activation, aggregation, and

265 ry in the geomorphic response of badlands to erosion such that in the early evolution stages, vegetat

266 ns exceeds the critical bed shear stress for erosion (tau cr ) accounts for 63% of the total observed

267 unexpected given active regional uplift and erosion that are thought to rejuvenate weathering supply

268 ographic history, reveal patterns of genomic erosion that might limit their viability, and offer tool

269 e magnitude of wave forces acting on wetland erosion that must be included in ecosystem restoration d

270 CLL cells caused an appreciable compact bone erosion that was prevented by Denosumab.

271 nitentes are snow and ice features formed by erosion that, on Earth, are characterized by bowl-shaped

272 s to protect finer particles underneath from erosion, the contribution of granular physics to river-b

273 In comparison with a baseline without erosion, the model suggested an erosion-induced sink of

274 Despite transiently increasing skin erosions, the clinical status of both subjects stabilize

275 Here we show that accounting for erosion thresholds during canyon incision results in nea

276 linked to infection-driven inflammatory bone erosion, thrives within a highly inflamed milieu and dis

277 ight evolve to a threshold state for bedrock erosion, thus implying much lower flood discharges than

278 apply our general formulation for salt marsh erosion to historical wave climates at eight salt marsh

279 ration of realistic calculations of sediment erosion, transport and deposition.

280 subaqueous delta will experience continuous erosion under sediment starvation and climate change in

281 -4.1 Ma and 3.3 Ma were in response to rapid erosions/uplift of the basin;

282 ight temporal-scale dependency of soil loss: erosion variability decreases at larger scales but the r

283 ignificantly affected by tectonic uplift and erosion via changes to the inorganic carbon cycle that a

284 The rate of cardiac erosion was 0.3% (average 83, range 12-171 days from imp

285 The incidence of tube erosion was 1% and 3% in the Ahmed Glaucoma Valve and Ba

286 The median duration from implant to erosion was 14 days, but was >1 year in 16 patients.

287 s capacity to protect against initial enamel erosion was also tested in vitro via changes in surface

288 Erosion was likewise monitored in vivo by non-invasive o

289 Bone erosion was particularly evident in long bone shafts, pr

290 llowed an exponential trend, suggesting that erosion was the predominant mechanism of the enzymatic b

291 The highest risk of erosions was found in the vaginal mesh plus sling group

292 Here, we use models for erosion, weathering and biogeochemical cycling to show t

293 ation, cartilage degradation, and local bone erosion were assessed at the wrist, knee, and ankle join

294 A total of 125 erosions were reported between 2002 and 2014, including

295 ge are the primary cause of accelerated soil erosion, which has substantial implications for nutrient

296 ely-segregating genomes mitigates mutational erosion, while paternal leakage exacerbates the ratchet

297 ed a threshold for oil impacts on marsh edge erosion, with higher erosion rates occurring for ~1-2 ye

298 s of ecosystems are experiencing substantial erosion, with potentially pervasive effects on ecosystem

299 lar eruptions with scale, as well as mucosal erosions, with lichenoid features on histologic analysis

300 ed that in addition to steady state telomere erosion, WRN depleted cells are also sensitive to telome