ライフサイエンスコーパス: sandy

1 areas of New York City affected by Hurricane Sandy.

2 areas of New York City affected by Hurricane Sandy.

3 ion in direct flood damages during Hurricane Sandy.

4 Sandy-2 and a previously described rat IgG1 antibody, 5A

5 y-5 displayed activities opposite to that of Sandy-2 by stimulating recombinant BAFF in vitro and end

6 B cells in vitro A single administration of Sandy-2 in mice induced B cell depletion within 2 weeks,

7 One of them, a mouse IgG1 named Sandy-2, prevented the binding of BAFF to all of its rec

8 Interestingly, 5A8 and Sandy-5 displayed activities opposite to that of Sandy-2

9 cluding history of flooding during Hurricane Sandy 7 months prior to the study.

10 rge and wave in the tri-state by considering Sandy, a hypothetical Black Swan (BS) storm, and the 1%

11 of New York City during and after Hurricane Sandy, a tropical cyclone that affected the northeastern

12 e clayey aggregates was 0.32, whereas in the sandy aggregates it was approximately 10 times lower.

13 A on (i) regional flood damages by Hurricane Sandy and (ii) local annual flood losses in Barnegat Bay

14 A sandy and a silt loam sediment were used to establish mi

15 on, MP flow-through experiments conducted on sandy and bentonite clay soil samples confirmed FWP suit

16 ity changes in sandbox experiments where two sandy and clayey soils were initially contaminated with

17 Our results suggest that sandy and green stomatopods are camouflaged from a typic

18 The GF bread was perceived crumbly, dry and sandy and had a longer eating duration than the GC bread

19 ion of blueberries, but the soils tend to be sandy and low in organic matter.

20 might be preferable for DNA extraction from sandy and rocky soils.

21 ong incubation to trace microbial residue in sandy and silty soils.

22 Piermont, New York, U.S.A. during Superstorm Sandy and the 1% annual chance flood and wave event by 8

23 tility enhancer for agricultural purposes in sandy and/or weathered soils.

24 unbleached, punkt, blurred, fade out, weiss, sandy, and albino genes.

25 The results showed that TOC, nature (clay, sandy, and loamy) of the soil, and the concentration of

26 m the upper aquitard (clayey silt) and lower sandy aquifer sediments in Van Phuc (Hanoi area, Vietnam

27 from four ponds were installed in a shallow sandy aquifer underlying a densely populated village and

28 clay fraction dominated Zn retention in the sandy aquifer, the lenses supported additional reaction

29 ane oxidation rates in shallow carbonate and sandy aquifers from central and northern Germany with me

30 ing OMP TolC could spread more widely within sandy aquifers.

31 rain of the Hermansky-Pudlak syndrome strain sandy, are abnormal, indicating that aberrant biogenesis

32 s comprised of deeper, steeper sloped, muddy-sandy areas with less gravel and highly disturbed region

33 Here, we explore the stratigraphy of a sandy barrier to identify the best sea-level indicators

34 n the study area was a lagoon protected by a sandy barrier.

35 Sandy beach and foredune environments are common through

36 o high precision sUAS-SfM and RTK-GPS to map sandy beach and foredune geomorphic change.

37 gs indicate that the Apple lidar can capture sandy beach and foredune geomorphic changes rapidly and

38 se for coastal communities to maintain their sandy beach areas.

39 able beach sand, emphasizing the role of the sandy beach as an aerobic biocatalytical reactor at the

40 Our results suggest that modality in sandy beach benthic communities is unlikely to be explai

41 CoSMoS-COAST predicts that 81% of O'ahu's sandy beach coastline could experience beach loss by 210

42 nt kelp forests on rocky nearshore reefs and sandy beach ecosystems that receive resource subsidies i

43 We conducted this work in sandy beach ecosystems, which rely on the import of mari

44 ial addition for accurate modeling of island sandy beach environments.

45 t of the lagoon shoreline transformed from a sandy beach to a mangrove habitat, accreting by 214 m ov

46 ed to retreat past the present-day extent of sandy beach under 1.0 to 2.0 m of sea-level rise, respec

47 (SOAs) of DWH oil buried in a North Florida sandy beach, (ii) elucidated the long-term succession of

48 buried in the upper 50 cm of a North Florida sandy beach.

49 ntral mechanism facilitating the recovery of sandy beaches after oil contamination.

50 Sea turtles nest on sandy beaches and tend to show high fidelity to specific

51 evolution, and two soft sediment ecosystems, sandy beaches and tidal wetlands.

52 Sandy beaches are biogeochemical hotspots that bridge ma

53 Most sediment samples came from sandy beaches at the high tide line, and most seawater s

54 We collected 36 intertidal samples at 12 sandy beaches from four regions that spanned distances f

55 on invertebrate body sizes from a variety of sandy beaches in the UK to test the hypothesis that thes

56 t and future shoreline hardening patterns on sandy beaches need deeper analysis.

57 nt, large numbers of SOAs were buried in the sandy beaches of the northeastern Gulf of Mexico.

58 as observed 1-2 m below the shoreline at two sandy beaches on Lake Erie, Ontario, Canada.

59 one, as a proxy for risk of hardening at all sandy beaches on the island of O'ahu, Hawai 'i.

60 karyotes are key ecosystem drivers in marine sandy beaches, an important and dynamic environment; how

61 process which can degrade plastic litter on sandy beaches, desert environments and in agricultural s

62 to Florida, burying oil up to 70 cm depth in sandy beaches, posing a potential threat to environmenta

63 abnormal shoreline dynamics for deltaic and sandy beaches, which are severely impacted by abrupt dec

64 that synchrony cascades from rocky reefs to sandy beaches, with spatiotemporal patterns mediated by

65 e hotspots for biogeochemical cycling within sandy beaches.

66 tructure and ecosystem multifunctionality of sandy beaches.

67 not been addressed in the intertidal zone of sandy beaches.

68 inland mice to near white in mice inhabiting sandy beaches; this light pelage has evolved independent

69 s, descriptions or tags related to Hurricane Sandy bears a striking correlation to the atmospheric pr

70 Continental-scale rivers with a sandy bed sequester a significant proportion of their se

71 proteins (pallidin, muted, cappuccino, HPS7/sandy); BLOC-2, consisting of HPS6/ruby-eye, HPS5/ruby-e

72 Desalination brine can infiltrate into the sandy bottom around the discharge area due to gravity cu

73 In contrast, rocky and coarse sandy bottom habitats with a predominance of rhodoliths,

74 nds helped to avoid 8%, 26%, 52% loss during Sandy, BS storm, and 1% event, respectively.

75 he least irrigation class (< 35%FI), wherein sandy clay and loam recorded the highest (82.1%) and the

76 Sandy clay loam soil in combination with 50 IJs cm(-2) o

77 t using two contrasted soils (sandy soil and sandy clay loam) that were amended with sewage sludge or

78 Data shows the sandy coast bounding river mouths accreted consistently

79 cast meso timescale shoreline evolution in a sandy coastal system and compared against the traditiona

80 Sandy coastlines adjacent to tidal inlets are highly dyn

81 The Hurricane Sandy cohort included data from 960 394 veterans between

82 Of the 960 394 veterans in the Hurricane Sandy cohort, the mean (SD) age was 63 (16) years, and 8

83 For the Hurricane Sandy cohort, those who were flooded and received indivi

84 as more pronounced among healthier veterans (Sandy cohort: 1-year hazard ratio [HR], 1.62 [95% CI, 1.

85 mpared with veterans who had severe illness (Sandy cohort: HR, 1.22 [95% CI, 1.17-1.26]; Harvey cohor

86 istical analysis of network dynamics, called SANDY, combining well-known global topological measures,

87 gnancy compared to those pregnant during non-Sandy conditions.

88 evee, while depositional features, such as a sandy crevasse-splay deposit are found further away from

89 Cutting across these clay patterns are sandy deserts that developed <10 Ma and are well mapped

90 Although they are widespread in modern sandy deserts, star dunes are rarely recognised in the r

91 w sidewinding specialist vipers that inhabit sandy deserts-an isotropic texture that is distinct from

92 investigate user attention to the Hurricane Sandy disaster in 2012, we analyze data from Flickr, a p

93 imens from women who lived through Hurricane Sandy during pregnancy compared to those pregnant during

94 tuarine mud-infilling and restore antecedent sandy ecosystems.

95 divided between two regions characterized by sandy (Eglin Air Force Base) or clayey (Red Hills) soils

96 ith bombing-related acute stress; Superstorm Sandy exposure wasn't.

97 ulane virus, and Escherichia coli TVS 353 in sandy Florida agricultural soil.

98 The lithification of the sandy fossil channel-levee systems is estimated to have

99 mpact crater in Elysium Planitia on a smooth sandy, granule- and pebble-rich surface with few rocks.

100 e(II), relative to the oxic near-surface and sandy gravel layers.

101 The sandy gravel material from the field site was also used

102 s a dynamic prealpine river with an alluvial sandy-gravel aquifer, which is characterized by short gr

103 t explain the broad geographic patterns, and sandy habitat best explains local patterns of movement.

104 In 2012, Hurricane Sandy hit the East Coast of the United States, creating

105 harged from the river is present in both the sandy Holocene and gravelly Pleistocene aquifers and is

106 of firearm violence on school campuses since Sandy Hook and the ongoing toll on lives and health, the

107 gia basin, the New York Bight basin, and the Sandy Hook basin offer promising basalt-hosted reservoir

108 antially after the December 2012 shooting at Sandy Hook Elementary School in Newtown, Connecticut, wh

109 posure to the 9/11 terrorist attacks and the Sandy Hook School shootings were both significantly asso

110 onal shootings in the immediate aftermath of Sandy Hook.

111 was comparable to that in aggregates from a sandy, hydrocarbon-contaminated soil (~23%) scanned for

112 these areas, even though prior to Hurricane Sandy in 2012, no inlet was present in the eastern bay i

113 t (CT) sustained huge structural loss during Sandy in 2012.

114 ce of additional flood events like Hurricane Sandy in recent centuries, and highlight the inadequacie

115 The sandy inland mouse (Pseudomys hermannsburgensis) experie

116 de of flooding in New York City by Hurricane Sandy is commonly believed to be extremely rare, with es

117 barchan dune and 26.0 cm x 25.4 cm on moving sandy land at valley slopes.

118 Revegetation on sandy land has attracted worldwide attention, especially

119 idance to the ongoing vegetation recovery on sandy land, an important component of the Project on Con

120 the Yellow River floods could transform into sandy land.

121 ikely the pioneer plants for revegetation on sandy land.

122 The carbonate-cemented sandy layers served as nucleus for subsequent coralligen

123 nd linear increases in J(CO2) on an alluvial sandy loam and a lowland clay soil, and an asymptotic in

124 g Koc values for (14)C60 were equivalent for sandy loam and silt loam (3.55 log[mL/g]) but higher for

125 ontained three 20 mm(2) channels emulating a sandy loam microstructure.

126 tify the prion adsorption capacity of whole, sandy loam soil (SLS) typically found in CWD endemic are

127 e (14)CO2 production in the silt loam or the sandy loam soil after 754 and 328 days, respectively, su

128 were grown for 8 d in microcosms packed with sandy loam soil at 1.2 g cm(-3) dry bulk density.

129 umber plants were cultivated for 150 days in sandy loam soil treated with 0 to 750 mg TiO2 NPs kg(-1)

130 ent were grown in tubes of sieved (<250 mum) sandy loam soil under two different water regimes.

131 ture grass (Paspalum notatum) was grown on a sandy loam soil while provided factorial additions of N

132 on of nAu was (i) greater on biochars than a sandy loam soil, (ii) greater at higher ionic strength a

133 ir effects on water retention curve (WRC) of sandy loam soil, chosen for its agricultural relevance a

134 les in a silty clay loam soil than in a fine sandy loam soil.

135 ng factor, the linear J(CO2) response on the sandy loam was reinforced by positive feedbacks from abo

136 We assessed the effects of three soil types, sandy loam, silty clay and clay, on the ANPP response of

137 (arsenopyrite and lollingite) embedded in a sandy matrix and injecting oxic solutions into the initi

138 )) derived from the natural dysbindin mutant Sandy mice, we have explored the role of dysbindin in do

139 ructural loss by coastal wetlands was low in Sandy, modest in the BS storm, and significant in the 1%

140 The rooting horizon is a dark grey sandy mudstone showing limited root penetration.

141 the lowest quality is assigned to the RRT5 (sandy mudstone/siltstone microfacies) which is represent

142 rkose arenite, glauconitic quartz wacke, and sandy mudstone/siltstone.

143 morphogenesis, the most severely affected is sandy, muted, and buff followed by subtle gray.

144 Although the permeability of the sandy Nankai Trough materials are higher than that of th

145 te explained variation, with deeper roots on sandy, nutrient-poor soils relative to clayey, nutrient-

146 liams, then at Oxford University with A.G. ("Sandy") Ogston, and finally back at Wisconsin with Willi

147 at start 4 weeks after landfall of Hurricane Sandy on October 29, 2012, and ending 2 years later, cre

148 arge-scale atmospheric patterns that steered Sandy onto the coast will become more frequent in the co

149 in regions that were affected by Hurricanes Sandy or Harvey.

150 ulation of soil organic matter in the site's sandy, organic matter-poor soils.

151 nd biological soil crusts of Phanerozoic eon sandy palaeosols.

152 Sandy patches and rubbery papules were found in 41 of 11

153 The sandy patches with grains showed moderate cellular immun

154 st unfavorable conditions were projected for Sandy Point where hatching success has already declined

155 conditions (Playa Grande, Pacific Ocean and Sandy Point, Caribbean Sea), but the effect varied in ar

156 this widely occurring waterborne pathogen in sandy porous media.

157 Superstorm Sandy ravaged the eastern seaboard of the United States,

158 nrichment caused soil carbon gains most dry, sandy regions, considerable absolute losses of soil carb

159 ring a 16-week field incubation in a flooded sandy rice paddy soil in Thailand.

160 ook salmon (Oncorhynchus tshawytscha) in the Sandy River (OR, USA), assuming that sediment is flushed

161 eek and Still Creek-in northwestern Oregon's Sandy River Basin were monitored for temperature, dissol

162 e abundance were detected in both gravel and sandy riverbeds and showed a simple, common vertical dis

163 activity peaked deeper down (4-8 cm) in the sandy riverbeds, coincident with a peak in n-damo 16S rR

164 o activity was confined to the more reduced, sandy riverbeds.

165 8.1B ($4.7B-$14.0B, 5th-95th percentiles) of Sandy's damages are attributable to climate-mediated ant

166 a level rise, the return period of Hurricane Sandy's flood height decreased by a factor of approximat

167 over the 21st century is also accounted for, Sandy's return period is estimated to decrease by approx

168 persistence of the westward flow that led to Sandy's unprecedented track, implying that future atmosp

169 t 16 loci are associated with HPS, including sandy (sdy; ref. 7).

170 t sp. nov. were anchored within the shallow, sandy sea bed and lived in dense, typically monospecific

171 ds more efficient in delivering non-cohesive sandy sediment along the coasts?" Here we relate flow st

172 Sandy sediment beaches covering 70% of non-ice-covered c

173 In the sandy sediment containing limited natural organic carbon

174 tic stages favour delivering of non-cohesive sandy sediment more than the persistent stages.

175 Unconsolidated sandy sediment on isolated surfaces in the Canyonlands r

176 y 100% of TB transformed to TD except in the sandy sediment where 51-60% of 17alpha-TB was converted

177 icant for E2 in both sediments and TB in the sandy sediment with beta-isomers decaying more rapidly t

178 a marked impact on the surface charge of the sandy sediment, significantly affecting the mobility of

179 cked with a natural heterogeneous subsurface sandy sediment.

180 ed plant-related material, while OM from the sandy sediments (OMS) is more bioavailable and related t

181 ea that grain-size disposition in subsurface sandy sediments drives the interstitial fluxes, influenc

182 ger R(u) in clayey/organic sediments than in sandy sediments further confirmed the role of soil-speci

183 creasing in concentration from the pristine, sandy sediments of Wells (ME), to industrially contamina

184 0 degrees C) water quality changes in anoxic sandy sediments.

185 Monitoring sandy shoreline evolution from years to decades is criti

186 to unravel the forcing-response spectrum of sandy shorelines globally.

187 Its sharp upper contact with a thick sandy silt implies that the two beds formed in rapid suc

188 id Pleistocene sedimentation loads permeable sandy silt of Miocene age, successfully predicts the obs

189 e to the low-energy context of the enclosing sandy silt stratum.

190 ntration series of copper-paint contaminated sandy, silty-sand, and silty sediment types, DGT-probes

191 s tissues and sediments from an open coastal sandy site (Ryde, UK) and a muddy tidal inlet site (Farl

192 org)/N was higher at the muddy site than the sandy site, suggesting a greater contribution of marine

193 In sandy sites, the difference in vegetation type caused sh

194 el of the snake enables the device to ascend sandy slopes close to the angle of maximum slope stabili

195 ates without slip, including ascending loose sandy slopes, crossing sand ripples, escaping from buryi

196 onial octocorals inhabiting mostly muddy and sandy soft sediments, globally.

197 on the extractability of Cu from a standard sandy soil (Lufa 2.1).

198 irst carried out using two contrasted soils (sandy soil and sandy clay loam) that were amended with s

199 ken from a high-P clay-rich soil and a low-P sandy soil by combining advanced spectrometric and spect

200 re, we performed microcosm incubations using sandy soil from an agricultural site in Midwest USA.

201 scarce at the depths of their tunnels in the sandy soil of our study site (20-64 cm), but here we des

202 m Huelva, which was associated with a higher sandy soil percentage in the Huelva orchard.

203 d to two soils with contrasted properties: a sandy soil poor in organic matter and a clay soil rich i

204 upinus albus) grown in mesocosms filled with sandy soil results in a set of root architectural parame

205 Mercury associated with sandy soil up to 6 cm below the surface can be emitted,

206 rom a breeding line called Seri and grown in sandy soil with low fertilization.

207 Wet sandy soil with porosity of about 0.5 contracted during

208 correlate well with diesel removal from the sandy soil, but this is not the case with the clayey soi

209 nds were consistent with those measured in a sandy soil, except that the mobility of dissolved inorga

210 le influence on the ANPP-CO2 response on the sandy soil, possibly because Sorghastrum increased large

211 In sandy soil, the removal of the diesel and products from

212 40, and 100 g kg(-1) of residual solids to a sandy soil, while experiment 2 investigated a loading ra

213 ncluding upland and lowland clay soils and a sandy soil.

214 the regeneration of fertility on a degraded sandy soil.

215 up can measure the RWU and redistribution of sandy-soil water content with unprecedented precision.

216 s shaped by soil texture, with ecosystems in sandy soils being relatively more sensitive to soil dryi

217 Embolism resistance increased in trees on sandy soils but did not vary with tree height.

218 nation of rainfall (favoring grasses), soil (sandy soils favoring trees), and fire (limiting trees un

219 For the same reason, plants in sandy soils have limited potential to adjust to water li

220 The plant grows in the wild, on sandy soils little used for agriculture in Southern Afri

221 bsurface water with low hardness residing in sandy soils may have a higher potential of being contami

222 nd evaporative demand, and may be reduced in sandy soils that hold less water.

223 ffect size on finer textured soils, while on sandy soils the same increase in precipitation produced

224 nductivity and solute breakthrough curves in sandy soils were investigated in the presence of varying

225 also found kit foxes selected for silty and sandy soils, which are conducive to den construction, as

226 revealed a significant link between prenatal Sandy stress (PNSS) and child HPA dysfunction, evident b

227 rption in the oxic Al- and Fe-hydroxide-rich sandy subsoil.

228 y exceeds 20 cm in depth, especially in soft sandy substrates typical of Florida, making the great ma

229 particles were injected into a contaminated sandy subsurface area in Sarnia, Ontario.

230 period, for example, with VSWC <0.07 in this sandy surface soil.

231 n of immediate pre-glacial fluvially derived sandy systems where rivers from the Norwegian mainland b

232 vent-related potential assessment, Hurricane Sandy, the second costliest hurricane in United States h

233 (ZCTAs) impacted by flooding from Hurricane Sandy throughout the study period.

234 we compare resultant deposition by Hurricane Sandy to earlier storm-induced flood layers in order to

235 rior reports attributing the transition from sandy to muddy conditions to coastal protection structur

236 Rather, the shift from alongshore sandy to riverine muddy sediment supply was the key driv

237 Two sandy tsunami deposits extend over 1.5 km inland of the

238 reveal the coastline remained predominantly sandy until 2002, with shoreline shifts averaging less t

239 In contrast, sandy uplands exhibited slower recovery and persistent g

240 Among residents aged 65 years, Hurricane Sandy was associated with a higher rate of ED visits due

241 Among adults aged 18-64 years, Hurricane Sandy was associated with a higher rate of ED visits for

242 a fundamental role in seed establishment in sandy, wave swept marine environments.

243 hypothesis in multiple sequences (units) of sandy, weakly stratified sediments at Wakulla Springs, F

244 Simulated surge and wave for Sandy were verified with data at numerous stations.

245 riods affect U stability, we dosed saturated sandy wetland mesocosms planted with Scirpus acutus with

246 hat short periods of drought conditions in a sandy wetland, which expose reduced sediments to air, ma

247 We applied these strategies to Hurricane Sandy, which struck the northeastern United States in Oc

248 Whether events like Sandy will become more frequent as anthropogenic greenho

249 e number of ED visits on and after Hurricane Sandy with all other days, 2005-2014, adjusting for temp