ライフサイエンスコーパス: erosion

1 followed by fluvial erosion (and lesser wind erosion).

2 senescence accompanied by increased telomere erosion.

3 craters, indicating geologically recent wind erosion.

4 shear velocity threshold causing soil C(org) erosion.

5 ion that left the protrusion exposed to wave erosion.

6 e called flow relaxation, that explains this erosion.

7 ) m(-2) year(-1) ) or were in a state of net erosion.

8 rapies for acute coronary syndrome caused by erosion.

9 plants as agents that can accelerate coastal erosion.

10 ering-decreased, sustained by an increase in erosion.

11 se section channel with minimum friction and erosion.

12 ct of Campania (Italy) threatened by genetic erosion.

13 rtitioning of denudation into weathering and erosion.

14 romote endothelial damage during superficial erosion.

15 d the Sturtian glaciation, which accelerated erosion.

16 oastal processes that determine flooding and erosion.

17 ses recently implicated in the mechanisms of erosion.

18 ommunities from storm surges and wave-driven erosion.

19 ent budgets can be important drivers of this erosion.

20 on is with haematochezia due to mucosal wall erosion.

21 oned to a source of carbon during periods of erosion.

22 ady-state bone remodeling and arthritic bone erosion.

23 et reshapes the solid Earth via isostasy and erosion.

24 om fluid inclusions in basalt during aeolian erosion.

25 nd potentiates thrombosis due to superficial erosion.

26 anticipated to lead to increases in coastal erosion.

27 , highlighting regions vulnerable to genetic erosion.

28 ons, especially in those with a primary tube erosion.

29 duction in storage capacity and an increased erosion.

30 and therefore cannot be a product of glacial erosion.

31 dilated as the deep rock has been exhumed by erosion.

32 to coral rubble production through physical erosion.

33 l properties and it does not increase dentin erosion.

34 the synovium, cartilage destruction and bone erosion.

35 oup included 5 explanted tubes for recurrent erosions.

36 ing delta morphology and possibly leading to erosion(1-3).

37 rged and carbon stores become compromised by erosion(4,5).

38 was higher than that of T1-weighted MRI for erosion (94% vs 86%, P = .003), sclerosis (97% vs 81%, P

39 The mechanisms that underlie superficial erosion, a cause of coronary thrombosis distinct from pl

40 ure probably does not pertain to superficial erosion, a process heretofore little understood mechanis

41 shoreline changes show that serious coastal erosion actually started much earlier.

42 better viewed as a method for reducing soil erosion, adapting to climate change, and ensuring food s

43 ia for burning, forest disturbance, and soil erosion all decline as early as the first decades of the

44 hydropic change leading to vesiculation and erosion; alternately, or in addition, the formation of i

45 Using extreme sequence erosion (amino acid deletions and substitutions) and sis

46 quent throat clearing, halithosis and dental erosion among others.

47 Marsh edge retreat by wave erosion, an ubiquitous process along estuaries, could af

48 rolysed waxes and lipids, increase post-fire erosion and can lead to long-term productivity losses.

49 e grain surface and regulated by large-scale erosion and clast-scale fracturing.

50 aves, storms, and coastal change (i.e. beach erosion and cliff retreat).

51 e depletion of nutrients and organic matter, erosion and compaction.

52 ses and subsequently the mat deteriorates by erosion and decomposition in winter.

53 ssociated with high infection rates, implant erosion and donor site morbidity.

54 where REEs were likely concentrated by local erosion and drainage into a closed lacustrine basin.

55 But as soil erosion and heterotrophic respiration respond differentl

56 seed was the best choice for preventing wind erosion and improving ecological and economic benefits i

57 ggest that AFL can detect areas of cartilage erosion and may potentially be utilised as a minimally-i

58 One erosion and no serious adverse events were reported.

59 s of agricultural production, including soil erosion and nutrient discharge.

60 nd climate change can cause significant soil erosion and peat deposition in rivers.

61 iver outflow were consequently very low, but erosion and permafrost slumping downstream of the lake i

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

63 VLs over the duration of release, indicating erosion and rearrangement of the lipid layers.

64 d with some flow rate dependencies caused by erosion and restructuring by the fluid shear.

65 of riverine deltas(8,10), increased coastal erosion and sea-level rise(11) signal a continuing negat

66 n that suggest a late Neoproterozoic crustal erosion and sediment subduction event of unprecedented s

67 We conclude that the two largest surface erosion and subduction lubrication events occurred after

68 V: 1) progression to type A, followed by RPE erosion and subretinal hyperreflective material, then ty

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

70 wetland plants elevates the rate of lateral erosion and that extensive root systems, rather than abo

71 ns, inelastic processes including magma mush erosion and thermal effects, can form a sustained channe

72 The erosion and wear behavior of the gas-solid mixture in th

73 ration and particle size will exacerbate the erosion and wear rate of the pipeline in polysilicon red

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

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

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

77 y, tectonic deformation, followed by fluvial erosion (and lesser wind erosion).

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

79 CD4 T cells accelerates DNA damage, telomere erosion, and cell apoptosis in HIV-infected individuals

80 positively and significantly correlated with erosion, and derive a relationship for use in erosion mo

81 probe further the mechanisms of superficial erosion, and develop point-of-care tests to distinguish

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

83 gration-related changes include deep (>25 m) erosion, and lateral migration of the channel.

84 carbon, retaining nutrients, decreasing soil erosion, and maintaining belowground biodiversity.

85 r mitigating global warming, preventing soil erosion, and reducing biodiversity loss.

86 ea, percent riparian area as forest, channel erosion, and relative bed stability-were found to be imp

87 accounting for diffusive soil creep, runoff erosion, and tectonic uplift, is reminiscent of the subs

88 ent anti-VEGF injections at the time of tube erosion, and the average duration of prior anti-VEGF the

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

90 is, which often originates with painful oral erosions, and pemphigus foliaceus, which is characterise

91 on severity and vulnerability for rupture or erosion; and 2) to use complementary human and mouse stu

92 scale picture emphasizes that fracturing and erosion are as important as atmospheric oxygen in limiti

93 However, structural lesions, such as erosions, are difficult to assess on routine T1-weighted

94 evidence for a significant reduction in bone erosion area and osteoclast numbers in Siglec-15(-/-) mi

95 the associated economic benefits in the wind erosion area.

96 By establishing the contribution of erosion as a key driving force behind the release of bio

97 o remove the smear layer and to cause dentin erosion as EDTA.

98 hierarchy of predictors to quantify surface erosion as well as combinations of features, like glass

99 nts with AMD who underwent tube revision for erosion at the Duke Eye Center from January 1, 1999, to

100 ually release bioactive molecules through an erosion-based process.

101 In order to study the flow and erosion behavior of gas-solid exhaust in the polysilicon

102 ure of the linker, and as per characteristic erosion behavior of polymers with anhydride-ester bonds.

103 Our results provide evidence that most erosion below the Great Unconformity in Colorado occurre

104 s in Pikes regolith, consistent with limited erosion between 717 and 510 Ma.

105 ssumed to control sliding velocity and hence erosion, but this too lacks empirical scrutiny.

106 ukaryotes, telomerase counteracts chromosome erosion by adding repetitive sequence to terminal ends.

107 less-massive atmospheres are susceptible to erosion by stellar wind.

108 (-1) yr(-1), with average losses of P due to erosion by water contributing over 50% of total P losses

109 n estimates (only considering sheet and rill erosion by water) with spatially distributed global P co

110 threatened, though natural processes such as erosion can also play a significant role in forest vulne

111 ductivity losses due to compaction and water erosion can amount to up to double-digit percentages for

112 Shoreline erosion can transition freshwater coastal wetlands from

113 root, although such small-volume subduction erosion cannot fully account for the degree of uplift ob

114 iopectobacterium, shows signatures of genome erosion characteristic of early stages of symbiosis, wit

115 th cordgrass significantly increased coastal erosion, clearly demonstrating that marshes protect shor

116 fluid was found for SDE microcapsules, while erosion-controlled release in simulated gastric and inte

117 nd agricultural landscapes, which favour the erosion, could thus bias the reconstructed landscape tra

118 This remobilization, also known as erosion, depends on the critical shear stress of a parti

119 ns, which span the different permutations of erosion, deposition and transport process representation

120 erosion, deposition, and transport.

121 ned by numerical simulations, match observed erosion/deposition and rock berm damage patterns recorde

122 With sCT, specificity for erosion detection (96% [95% CI: 90, 98] vs 89% [95% CI:

123 presented, we estimated that on average soil erosion displaces 5% of newly fixed land organic carbon

124 Excessive osteoclastic bone erosion disrupts normal bone remodeling and leads to bon

125 osteoclasts has a crucial function for bone erosion during arthritis.

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

127 Estimated soil erosion dynamics were then complemented with land cover

128 systems that are characterised by different erosion dynamics.

129 Telomere erosion, dysfunction, and fusion can lead to a state of

130 we combine spatially distributed global soil erosion estimates (only considering sheet and rill erosi

131 on years may indicate a massive global-scale erosion event near that time.

132 VEGF had on average a greater number of tube erosion events (2.1+/-0.7 events) compared with patients

133 we discovered over 400 unique human ortholog erosion events across 58 mammals.

134 prehensive estimates of seagrass soil C(org) erosion following eutrophication-driven seagrass loss in

135 e decline in sediment supply causing coastal erosion, following catchment disturbance through hydropo

136 t thermal and isostatic consequences of this erosion for global continental freeboard.

137 The results show that the wear and erosion from Nos.

138 uently compared with the basic principles of erosion from sediment transport.

139 Accelerated soil erosion has become a pervasive feature on landscapes aro

140 This study suggests that soil erosion has been altering terrestrial and aquatic ecosys

141 protein-coding genes, and subsequent genomic erosion has generated gene presence-absence polymorphism

142 Rainfall erosivity (or water erosion) has severe implications on agriculture, water,

143 Winter and early spring wind soil erosion have considerable impacts on ecosystems, human w

144 Land susceptibility to wind erosion hazard in Isfahan province, Iran, was mapped by

145 ion accuracy for land susceptibility to wind erosion hazard.

146 ques for mapping land susceptibility to wind erosion hazards.

147 nfirms the relevance of compaction and water erosion impacts for agricultural LCAs.

148 measurements to estimate eutrophication and erosion impacts of three crop rotation systems under two

149 s for the assessment of compaction and water erosion impacts within one framework, which can be expan

150 change was the main driver of inferred soil erosion in 70% of all studied watersheds.

151 nusual microarchitecture that controls tooth erosion in a way that maintains functional cusp shape.

152 ff on salt marsh edges generally hasten edge erosion in coastal marshes and that the erosion protecti

153 gh interactions between rainfall, runoff and erosion in drainage basins(1-4).

154 pproaches to attenuate inflammation and bone erosion in endodontic disease and other inflammation-rel

155 rily responsible for protection against edge erosion in marshes.

156 This proposed fluvial erosion in tesserae provides support for climate models

157 biotinylated cofactors to Sav may lead to an erosion in the catalytic performance, depending on the c

158 c-15 is directly involved in pathologic bone erosion in the K/BxN serum-transfer arthritis model.

159 e the most critical factors controlling wind erosion in the study area.

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

161 blasts suppressed both inflammation and bone erosions in mouse models of resolving and persistent art

162 d to higher rates of recurrent glaucoma tube erosions in patients with AMD.

163 significant difference in the number of tube erosions in patients with anti-VEGF (15 tubes, 4.8%) ver

164 to changing the concept of axSpA from one of erosions in the sacroiliac joints to a spectrum of disea

165 ses likely predispose plaques to superficial erosion, including experiencing disturbed flow, basement

166 bances than to climate change; human-induced erosion increased the dominance of dense-wooded, non-zoo

167 In addition, the water erosion intensity, road construction, channel gradient,

168 set further demonstrates that the most rapid erosion is achieved at temperate glaciers with high mean

169 In many parts of Africa, soil erosion is an important problem, which is evident from h

170 t under present day Martian rates of aeolian erosion is highly unlikely to produce detectable changes

171 ructure, an accurate estimation of shoreline erosion is required.

172 ith macroscopic release studies confirm that erosion is the key release mechanism.

173 avy-element core, but the efficiency of such erosion is uncertain and depends on both the immiscibili

174 Fluvial erosion is usually assumed to be absent on Venus, preclu

175 hardening can be triggered when evidence of erosion is within 6.1 m ("20 ft") of certain structures,

176 ac2-b expression leads to skin fragility and erosions is unknown.

177 w hydraulics, sediment transport and bedrock erosion lead to undulating bedforms, which grow to becom

178 of the ecosystem services investigated, soil erosion levels were actually higher in scenarios with hi

179 uptake, we found that ESMs that ignore soil erosion likely offset the erosional carbon loss by incre

180 Diversification reduced erosion losses up to 60%.

181 ch paper presents an assessment of shoreline erosion magnitudes using field measurements coupled with

182 Erosion management strategies should target agricultural

183 provide an indirect record of North American erosion, mass transfer and sediment storage from the lat

184 uch as LDL (low-density lipoprotein), plaque erosion may assume greater clinical importance.

185 Acute coronary syndromes because of erosion may not require immediate invasive therapy.

186 anges in microhardness, smear layer removal, erosion, mineral content distribution, apatite/collagen

187 The flow model and erosion model of exhaust gas and silicon particles were

188 rosion, and derive a relationship for use in erosion models.

189 ll density to a large density, the mean wind erosion modulus decreased from 68 to 17 kg.hm(-2).h(-1)

190 Among them, the mean wind erosion modulus of spring sowing bare land was as high a

191 ment transported in the stratum and the wind erosion modulus.

192 d with high hydrodynamic energy, significant erosion occurred.

193 The wear and erosion of 2 regions from Nos.

194 Erosion of a supramolecular gel has not yet been reporte

195 Rupture and erosion of advanced atherosclerotic lesions with a resul

196 hromboembolic events secondary to rupture or erosion of advanced atherosclerotic plaques represent th

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

198 We also show that the erosion of crustal rocks from whether plumes (mafic in a

199 ile epigenetic profiling uncovered the focal erosion of DNA methylation at oncogenic regulatory regio

200 low stability and high activity may lead to erosion of efficiency and/or kinetic selectivity, making

201 can be modulated by catalyst design, with no erosion of enantiomeric excess.

202 rity and reduced tree recovery foreshadow an erosion of forest resilience.

203 ogy, we observe a significant age-associated erosion of LINE-1 methylation in cfDNA suggesting that t

204 ntly been attributed to increased uplift and erosion of mountains and consequent increases in silicat

205 f architecture (AQuA) HiChIP, which revealed erosion of native SE contacts, and aberrant spreading of

206 populations unique to the GIT and the rapid erosion of pathogen-specific CD8 tissue-resident memory

207 for periods of up to 1 h without significant erosion of peak shape.

208 We tested for localized erosion of reproductive isolation by comparing site-wise

209 Total wind-erosion of sediment transport of CK was 18.6 g.m(-2) min

210 This is partly because of the severe erosion of statistical power resulting from the massive

211 e is typified by astrocytosis, microgliosis, erosion of the blood-brain barrier (BBB), formation of i

212 pG density is protective against age-related erosion of the epigenetic landscape and may explain inte

213 Erosion of the fracture surface increased access to iron

214 A possible explanation is erosion of the initially compact heavy-element core, but

215 hnological and social factors, including the erosion of the provider-patient relationship, the emerge

216 tions, but it does not robustly predict fast erosion of the Y (or W) in large populations or the step

217 c architecture present a paradox: mutational erosion of these genomes should lead to decline in mitoc

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

219 The erosion of this natural intensification barrier is espec

220 For instance, erosion of upper organic and organo-mineral soil horizon

221 Through comparative analysis, the erosion of upper wall of single furnace main channel is

222 ins a conserved DNA methylation pattern, the erosion of which provides a distinct competitive advanta

223 s a more general pattern seen in the ongoing erosion of working-class life for those born after 1950.

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

225 tion had a "strawberry-like" appearance with erosions of polyps (P = 0.000).

226 milar to the patterns resulting from fluvial erosion on Earth.

227 imate the role of land cover change and soil erosion on river transport of Hg in a heavily ASGM-impac

228 evaluation of smear layer removal and dentin erosion on root segments and energy dispersive X-ray spe

229 s of disturbance size, increases the rate of erosion on wave-stressed shorelines.

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

231 such studies primarily reported reduced soil erosion or increased vegetation cover but lower water av

232 lated to land surface processes such as soil erosion or lake biogeochemistry but are attributed mainl

233 Coastal erosion outpaces land generation along many of the world

234 iming, the amplitude, and the extent of soil erosion over millennial time scales.

235 r disease, as well as vacA s1/m2 and gastric erosion (P < 0.05).

236 Understanding the biological bases of erosion points to novel therapies for acute coronary syn

237 Drug release, polymer erosion, polymer degradation, and implant diffusivity we

238 plays a pivotal role in triggering telomere erosion, premature T-cell aging, and CD4 T-cell apoptosi

239 moderated by catchment responses to changing erosion pressure, with active downcutting associated wit

240 berate removal of C or lateral transport via erosion processes (e.g. support measures, bare fallow re

241 tructions of soil redistribution due to soil erosion processes.

242 s with very high drug loading and controlled erosion profiles are relevant as they may offer new oppo

243 decreased significantly in patients without erosion progression.

244 For sediment-starved and erosion-prone coasts, large-scale enhancement of sedimen

245 edge erosion in coastal marshes and that the erosion protection function of wetlands relates more to

246 e Earth surface shifted to human-driven soil erosion rate already 4,000 y ago.

247 Glacial erosion rate is usually modelled as a function of glacie

248 use canopy trait maps to assess how variable erosion rate within catchments influence hillslope contr

249 Inputs for carbon export include erosion rates and overwash extent.

250 However, geological records of erosion rates are potentially subject to averaging biase

251 In particular, inferred soil erosion rates increased in 35% of the watersheds, and mo

252 ssess the relative changes in lake-watershed erosion rates over the last 12,000 y.

253 Moreover, high erosion rates, along with a well-developed hydrographic

254 t statistically robust relationships between erosion rates, sliding velocities, and climate from a gl

255 to experience the highest estimates of soil erosion rates.

256 ering intensity reconcile marine isotope and erosion records with the need to maintain mass balance i

257 mpaired drinking water resources, while soil erosion reduces water quality and agronomic productivity

258 atient-doctor relationship or facilitate its erosion remains to be seen.

259 Using an Earth system model (ESM) with soil erosion represented, we estimated that on average soil e

260 ity, storms, short-term climate variability, erosion response and consequent flooding responses.

261 centennial to millennial timescales and the erosion response of the coast, highlighting a need to mo

262 face winds by up to 25%; paradoxically, wind erosion results in faster winds regionally.

263 ed soil organic carbon content, reduced soil erosion, salinization, and compaction, fire management,

264 based synthetic CT (sCT) in the depiction of erosions, sclerosis, and ankylosis of the SI joints comp

265 ndependently recorded if structural lesions (erosions, sclerosis, and ankylosis) were present on T1-w

266 Smear layer and dentin erosion scores were analyzed with Kruskal-Wallis and Dun

267 Thrombi that complicate superficial erosion seem more platelet-rich than the fibrinous clots

268 , but there is uncertainty about how glacial erosion should be parameterised in landscape evolution m

269 -use change are expected to enhance peatland erosion, significant alterations to invertebrate biodive

270 nization, accelerated deforestation and soil erosion since the 1980s.

271 ion has received little attention in glacial erosion studies, but our data illustrate its importance.

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

273 Plaques complicated by erosion tend to be matrix-rich, lipid-poor, and usually

274 Glaciers are highly effective agents of erosion that have profoundly shaped Earth's surface, but

275 changes in channel base-level have initiated erosion that migrates upstream (such as tectonic uplift

276 nt, P(v) is controlled by spatially variable erosion that occurs in transient landscapes.

277 Although soil erosion that removes land organic carbon has increased s

278 We propose a new mechanism for Y/W erosion that works over faster timescales, in large popu

279 The effects of wind erosion, the "winter rapeseed + " multiple cropping syst

280 storage, the soil evaporation and total wind erosion, the amount of sediment transported in the strat

281 d based on the gas-solid flow theory and the erosion theory.

282 ecord is commonly assumed to be biased, with erosion thought to eliminate older craters, even on stab

283 Human-caused erosion through bedrock, however, has only been observed

284 make predictions about the responses of soil erosion to long-term climate and land cover changes.

285 The deep erosion, topographic inversions, and an absence of dunes

286 atially heterogeneous Neoproterozoic glacial erosion totaling a global average of 3-5 vertical kilome

287 than 5% of crypts and no crypt destruction, erosions, ulcerations, or granulation tissue) and clinic

288 variability in, and controls on, rocky coast erosion under changing conditions.

289 ure the time and spatially dependent surface erosion (velocity) with high spatial resolution during t

290 inguish acute coronary syndromes provoked by erosion versus rupture that may direct more precision ma

291 (e.g. glacio-eustasy, continental uplift and erosion, volcanism, asteroid impact) play a moderating r

292 Tube erosion was noted 46.5+/-60.7 days from the preceding an

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

294 Thirteen factors controlling wind erosion were mapped, and multicollinearity among these f

295 Radiographically, no late frame fractures or erosions were identified.

296 reduce water nutrient contamination and soil erosion while maintaining farm productivity and profitab

297 Inevitably such a nonhomogeneous erosion will lead to the development of surface topograp

298 showed severe negative volumetric shoreline erosion with an average of 5.2 m/year with some exceptio

299 rkshire, UK, to model the changes in coastal erosion within the last 7 kyr and for the first time qua

300 dies and satellite imagery, that soil C(org) erosion (within the top 50 cm) following seagrass loss l