ライフサイエンスコーパス: sand

1 s (Terra Firme, Seasonally Flooded and White Sand).

2 as "reducing lenses") within natural aquifer sand.

3 oleifera chitin-binding protein (MoCBP) on f-sand.

4 raveling wave to move quickly on homogeneous sand.

5 from a major phase in the precursor arkosic sand.

6 s in silt-loam compared to 18 days in silica-sand.

7 d to the flow of coarse, granular media like sand.

8 nt of gas fluxes escaping the surface of the sand.

9 females in substrates with more (>66%) fine sand.

10 homogeneous or heterogeneous unconsolidated sands.

11 ciated with oil refineries and mining of oil sands.

12 imate primary and secondary HNCO for the oil sands.

13 oritic soda (natron) mixed with Nile-derived sands.

14 significantly higher complexity, while fine sands (130 to 166 um) result in significantly higher rou

15 fuel supporting smoldering in mixtures with sand (~175 mg PFAS/kg GAC-sand), with PFAS-spiked, labor

16 mining and upgrading of Athabasca bituminous sands (ABS).

17 Exponential decay of gull marker in sand amended with live Catellicoccus marimammalium sugge

18 pilot-scale granular activated carbon (GAC)-sand and anthracite-sand pilot-scale biofilters were inv

19 ition, we simplified the process of making f-sand and evinced how it could be regenerated using salin

20 und up to 36% lower removal of nests in fine sand and experimental results support the hypothesis tha

21 ialist shovel-nosed snake traversing a model sand and find body inertia is negligible despite rapid t

22 ips between sets of co-varying organisms and sand and mud contents, and positive relationships with t

23 ated fecal indicator bacteria (FIB) in beach sand and pore water represent an important nonpoint sour

24 e on bioremediation of products from the oil sand and shale (e.g., Dilbit and Bakken oil).

25 abitats dominated by hard coral, turf algae, sand and silt, and fleshy algae and reached the highest

26 ver wide ranges of soil texture from clay to sand and soil bulk density from 0.33 g/cm(3) to 1.65 g/c

27 He started Pica eating disorder (sand and sponge) due to anemia from 5 years and 10 month

28 ncing oil spill remediation efforts in beach sands and coastal sediments and underscore the role of u

29 ecovery of agent was optimized from foliage, sand, and glass in a simulated biothreat scenario using

30 ll expression of stray gas in unconsolidated sand aquifers.

31 The results showed that EF1alpha, ACT and SAND are suitable reference genes across all samples tes

32 erated by the extraction of bitumen from oil sands are a major source of NAs and are currently stored

33 dia that mimic field conditions (e.g., soil, sand) are opaque to most forms of radiation, while trans

34 ream oil and gas sector (excluding mined oil sands) are likely at least 25-50% greater than current g

35 esults were obtained using 0.5 g sample, 1 g sand as a solid support, 20 mg activated charcoal and 5

36 glass beads packed at a constant density and sand at a different dry bulk density.

37 of contrasting grain size, (ii) natural fine sand at the column scale; and (ii) streambed-equilibrate

38 Chickpea grains were roasted in sand at three temperatures (180, 200 and 220 degrees C)

39 We conducted experiments in quartz sands at low volumetric water contents (theta) to quanti

40 rn a function of the rate of sea level rise, sand availability, and stress of the plant ecosystem anc

41 We evaluated the effectiveness of a sand barrier around latrine pits in reducing fecal indic

42 A sand barrier can modestly reduce the risk presented by p

43 The sand barrier latrine monitoring well samples had 0.38 me

44 ssigned 34 latrines to include a 50 cm thick sand barrier under and around the pit and 34 received no

45 samples between latrines with and without a sand barrier using multilevel linear models and reported

46 under and around the pit and 34 received no sand barrier.

47 62; p = 0.002), compared to latrines without sand barriers, a reduction of 27% E. coli and 24% thermo

48 tal wetlands, such as marshes and mangroves, sand beaches and dunes, seagrass beds, and coral and oys

49 TOrC biodegradation and (2) biochar-amended sand bearing DOC-cultivated biofilms would achieve enhan

50 rged colloids, and grain transport in eroded sand beds.

51 ments, this behavior occurred in the aquifer sand between reducing lenses and was attributed to the s

52 ocally available absorbent materials such as sand, biochar, and teff straw in a media.

53 th nutrients and electron acceptors, but oil sands bitumen was the only organic substrate.

54 her contributions from heavy crude oils, tar sands bitumen, and petroleum coke.

55 is limited by the recalcitrant nature of oil sands bitumen, not the microbial communities resident in

56 udies of alluvium largely limited to smaller sand-bodies amenable to study in-situ by rovers.

57 hwest Portuguese margins, on muddy and muddy-sand bottoms between 200 and 700 m water depths, while i

58 an 100 kilometres upstream is converted into sand by the time it reaches the Ganga Plain.

59 Although quartz sand can adsorb some radium from the solution due to ele

60 esults reveal that SOAs buried deep in beach sands can be decomposed through relatively rapid aerobic

61 ks and spend several weeks per year building sand-castle "bowers" several times their size.

62 y significant cold heavy oil production with sand (CHOPS), airborne measured methane fluxes were five

63 le sand (Fluv), clinopyroxene-dominated lava sand (Cl-LS) and zeolite-dominated lava sand (Ze-LS), ai

64 ious conditions, including the height of the sand column (H) and porous bed (h) and the diameter of t

65 particles (AuNPs) were performed in a quartz sand column with an eluent composed of 10(-2) M NaCl at

66 ncomitantly an enhanced retention within the sand column, compared to the nonchemotactic control.

67 Sand columns containing just 0.5 wt % biochar maintained

68 n that of E. coli K12 in all biochar-amended sand columns.

69 se regions suggest that sediments finer than sand compose most of these highland materials.

70 packed in both homogeneous and heterogeneous sand configurations allowing for visualization and measu

71 ining mostly (immature) plant derived OC and sand containing mostly thermally mature derived OC.

72 an as permanent, natural repositories of oil sands contaminants.

73 Mud and sand content and the presence of microbial heterotrophic

74 ed that the grassland had the lowest overall sand content of 39.98-59.34% in the top 50 cm soil profi

75 l variables-agricultural and urban land use, sand content of soils, basin area, percent riparian area

76 atural geologic setting, as indicated by the sand content of soils.

77 The sand cover did not prevent photodegradation.

78 u, preserved below a 30,000 km(2) contourite sand deposit.

79 the relationship between historic periods of sand deposition in semi-arid grasslands and external cli

80 Large-scale oil production from oil sands deposits in Alberta, Canada has raised concerns ab

81 across six watersheds (five impacted by oil sands development and one unimpacted).

82 y to environmental impact assessments of oil sands developments.

83 l abundances in SOAs compared to surrounding sands distinguished SOAs as hotspots of microbial growth

84 The results show that the height of the sand does not affect the speed of the sand flow.

85 fossil calibrated phylogeny of the new world sand dollar genus Encope, based on one nuclear and four

86 basis of development in cidaroid echinoids, sand dollars, heart urchins, and other nonmodel echinode

87 lis and Neoregelia cruenta, from a Brazilian sand dune forest.

88 on in the tidally ventilated permeable beach sand, emphasizing the role of the sandy beach as an aero

89 ance through hydropower dam construction and sand extraction.

90 We propose functionalized sand (f-sand) filters as a highly effective, energy-effi

91 Moringa oleifera (MO) seeds, functionalized sand (f-sand) filters, achieved a ~7 log(10) virus remov

92 d from off-road diesel activities within oil sands facilities, and an additional 116-186 kg hr(-1) fo

93 NMR well-logging probe to monitor MICP in a sand-filled bioreactor, measuring NMR signal amplitude a

94 cedented high virus removal from a practical sand filter.

95 Sand filters functionalized using a water extract of Mor

96 We propose functionalized sand (f-sand) filters as a highly effective, energy-efficient, a

97 oleifera (MO) seeds, functionalized sand (f-sand) filters, achieved a ~7 log(10) virus removal.

98 onventional water treatment (coagulation and sand filtration combined with granular activated carbon

99 since it can have important implications for sand filtration, the most common water treatment technol

100 to 13 cm into sediment consisting of coarse sand, fine gravel, and medium gravel.

101 distribution reduces the expected number of sand flies acquiring parasites, it increases the infecti

102 Sand flies and mosquitoes belong to separate lineages of

103 ndemic area for visceral leishmaniasis (VL), sand flies are abundant for a short period of <=3 months

104 Phlebotomine sand flies are hematophagous insects that harbor bacteri

105 Lutzomyia longipalpis sand flies are the major natural vector of Leishmania in

106 attractive to a greater proportion of female sand flies as the infection progresses.

107 icantly more attractive to 50% of the female sand flies at the end of infection compared to before in

108 icantly more attractive to 75% of the female sand flies at the end of infection.

109 The bites of uninfected sand flies favor the transmissibility of L. donovani by

110 rasites, it increases the infection load for sand flies feeding on a patch, increasing their potentia

111 Sand flies inject saliva while feeding in the vertebrate

112 During Leishmania transmission sand flies inoculate parasites and saliva into the skin

113 e that prior exposure to bites of uninfected sand flies potentiates their ability to transmit infecti

114 he blood or skin as a source of infection to sand flies remains unclear, and the possible effect of m

115 Sand flies were collected from different towns (Karaburu

116 After sterile washing steps, sand flies were dissected and guts were separated.

117 Microbiome profiling of wild-caught sand flies will be of great help in the investigating of

118 Salivary proteins of sand flies, specifically maxadilan and LJM11, have been

119 From sand flies, we isolated most of the known Phlebovirus st

120 The parasite is transmitted by the bite of sand flies, which inoculate the promastigote forms into

121 s following challenge with L. major-infected sand flies, while non-immunized animals develop large an

122 nfection transmitted by the bite of infected sand flies.

123 Diptera, such as Drosophila, mosquitoes and sand flies.

124 d macular PKDL, and VL, can be infectious to sand flies.

125 All patients infected sand flies.

126 rasite patches that govern infectiousness to sand flies.

127 y blood-feeding female Lutzomyia longipalpis sand flies.

128 vaccinated dogs that are also infectious to sand flies.

129 t of L. major transmission by L. longipalpis sand flies.

130 Leishmania protozoa transmitted by infected sand flies.

131 of the sand does not affect the speed of the sand flow.

132 geochemistry were therefore performed on oil sands fluid petroleum coke deposits in Alberta, Canada.

133 cted wetlands (CWs) consisting of fluviatile sand (Fluv), clinopyroxene-dominated lava sand (Cl-LS) a

134 sediment influx should result in an elevated sand flux, leading to distinct patterns of aggradation a

135 e, we demonstrate that gut microbes from the sand fly are egested into host skin alongside Leishmania

136 are introduced into mammalian skin through a sand fly bite, but different species cause distinct clin

137 Individuals exposed to sand fly bites develop humoral and cellular immune respo

138 Pre-exposure to uninfected sand fly bites or immunization with defined sand fly sal

139 ns have proven to be effective in preventing sand fly bites, and subsequently infection.

140 probably caused by insufficient exposure to sand fly bites.

141 nduces robust host protection against vector sand fly challenge and because it is marker free, can be

142 ural similarities indicate that mosquito and sand fly D7 proteins have evolved from similar progenito

143 cales provide the best fit with experimental sand fly feeding data, pointing to the importance of the

144 ment site inside the alimentary tract of the sand fly insect vector.

145 ect the biosynthetic pathways leading to the sand fly pheromone sobralene and taxadiene have been mad

146 shown for the first time in the wild-caught sand fly populations of Turkey.

147 experiments demonstrate that pre-exposure to sand fly saliva confers protection against leishmaniasis

148 SDS-PAGE coupled to LC-MS analysis of sand fly saliva, before and after enzymatic deglycosylat

149 mine the diversity of N-glycan structures in sand fly saliva, enzymatically released sugars were fluo

150 species, meaning that the applicability of a sand fly saliva-based vaccine will be limited to a defin

151 functional genomics approach to identify the sand fly salivary components that are responsible for th

152 ts the first detailed structural analysis of sand fly salivary glycans.

153 f immunogenic portions of PdSP15 and LJL143, sand fly salivary proteins demonstrated as potential vac

154 Because of this, sand fly salivary proteins differ structurally from thos

155 Sand fly salivary proteins have been extensively studied

156 sand fly bites or immunization with defined sand fly salivary proteins was shown to negatively impac

157 lop humoral and cellular immune responses to sand fly salivary proteins.

158 analysis to compare with Old- and New-World sand fly salivary proteins.

159 body response to saliva after the end of the sand fly season.

160 n Tbilisi and other endemic areas with brief sand fly seasons.

161 The patterns of courtship songs in New World sand fly species evolve quickly under sexual selection;

162 at included proteins commonly found in other sand fly species such as the yellow, SP15 and apyrase pr

163 pendent on the phylogenetic proximity of the sand fly species, meaning that the applicability of a sa

164 m D7 proteins AGE83092 and ABI15936 from the sand fly species, Phlebotomus papatasi and P. duboscqi,

165 ibute to reproductive isolation in New World sand fly species, suggesting that auditory communication

166 urring bites from Lutzomyia longipalpis, the sand fly vector of leishmaniasis, immunize individuals w

167 that the infectiousness of patients for the sand fly vector of visceral leishmaniasis is linked to p

168 site is transmitted to a mammalian host by a sand fly vector where it develops as an intracellular pa

169 To survive in its sand fly vector, the trypanosomatid protozoan parasite L

170 sis is a spectrum of diseases transmitted by sand fly vectors that deposit Leishmania spp. parasites

171 vertebrate hosts and the alimentary tract of sand fly vectors.

172 ocytic choriomeningitis virus (LCMV), or the sand fly-transmitted arbovirus Toscana virus (TOSV).

173 s 50 cm long were filled with sterile silica sand following five different setups combining fine and

174 gh Magadi Beds are filled with mud, silt and sand from overlying sediments.

175 ntify the Fe phases into two fractions (fine sand, FSa, and fine silt and clay, FSi + Cl), isolated f

176 ng such behaviour among leopards in the Sabi Sand Game Reserve, South Africa, associated with four no

177 e by 49 leopards Panthera pardus in the Sabi Sand Game Reserve, South Africa, to quantify the magnitu

178 gth of maternal care in leopards in the Sabi Sand Game Reserve, South Africa.

179 and the diameter of the glass beads (D) and sand grains (d).

180 on of CCSHs tends to occur on the surface of sand grains and into pore throats, indicating that small

181 able conditions for clay detachment from the sand grains were encountered.

182 d mica surfaces (representing nanosilver and sand grains) in solutions relevant to agricultural soils

183 This species feasts in the biofilm among sand grains, but also on macroalgae and ice within which

184 eposits as they are trapped between settling sand-grains.

185 nalysis proved useful for PFAS-loaded GAC in sand; however, analyzing soils suffered from interferenc

186 anaceous plant, Capsicum annum against moist sand in dual choice assays.

187 d that distance from haul out, proportion of sand in seabed sediment, and annual mean power were impo

188 tion from mining and upgrading of bituminous sands in northern Alberta, Canada, Sphagnum moss was obt

189 With growth of the Canadian oil sands industry, concerns have been raised about possible

190 exhumed and resided at the surface prior to sand injection, likely before the 717-Ma Sturtian glacia

191 In columns packed with 40-50 mesh Ottawa sand, injection of a PAC (1000 mg/L) + polyDADMAC (5000

192 s, in which males use their mouths to sculpt sand into large species-specific structures for courtshi

193 reveal that the virus removal activity of f-sand is due to the presence of a chitin-binding protein,

194 s created during bitumen extraction from oil sands is a major technical and environmental challenge.

195 matrices (foliage, exposed smooth surfaces, sand) is recommended for retrospective verification of a

196 ving higher stocks than those located on the sand islands in the northwest of the bay.

197 riverine influence located on tide-dominated sand islands), across elevation gradients, with distance

198 erature would be akin to building a house on sand - likely to fall at any moment.

199 acteria, lichen, moss, mixed), soil texture (sand, loam, clay), and climatic zone (arid, semiarid, dr

200 er structure and the thousands of individual sand manipulation behaviors performed throughout constru

201 rees C, were examined as flocculants for oil sands mature fine tailings (MFT).

202 Crude oil buried in intertidal sands may be exposed to alternating oxic and anoxic cond

203 otic, pipemidic acid (PIP), in MnO(2)-coated sand (MCS) columns is altered by the presence of dissolv

204 e mobility of PAA-nano-ZVI within a standard sand medium.

205 the PAD is threatened by encroachment of oil sands mining in the Athabasca watershed and hydroelectri

206 in the subsurface, suggesting that utilizing sand mixed with biochar can act as a promising biofilter

207 pportionment, which revealed that nearby oil sands operations contribute to 86% of the total mass of

208 ized to watershed area were highest near oil sands operations.

209 tion in field studies, covering of soil with sand or irrigation after herbicide application.

210 enera restricted to floodplain, swamp, white-sand or plateau forests of Central Amazonia.

211 e different setups combining fine and coarse sands or a mixture of both mimicking potential water tre

212 ed to the haul road dust and unprocessed oil sands ores and was the most similar source material to n

213 r plot was amended 16 years ago with process sand, organic matter, and seeded (partially treated), an

214 e plot was amended 16 years ago with process sand, organic matter, gypsum, and seeded (fully treated)

215 Oil sands (OS) are an important type of heavy oil deposit, f

216 surface mining and bitumen extraction of oil sands (OS) generates over one million barrels of heavy o

217 major industrial facilities such as the oil sands (OS), which consume large quantities of diesel fue

218 conditions, the amount of FIB accumulated in sand over 5-6 days was found to be sufficient to trigger

219 simulate the transport of bacteria within a sand-packed column containing a distribution of chemoatt

220 ibition by tungstate in advective upflow oil-sand-packed columns.

221 Here, we inoculated replicated, sand-packed, continuous mesocosms with groundwater from

222 profiles for Rb(+) and Br(-) in unsaturated sand packs were measured with a synchrotron X-ray microp

223 ral ease of movement of seawater through the sand patties as shown with a (35)SO4(2-) radiotracer.

224 We collected sand patties deposited in the swash zone on Gulf of Mexi

225 tal fate and effects of "oxyhydrocarbons" in sand patties deposited on beaches are not well-known.

226 solved organic matter (DOM) leached from the sand patties under dark and irradiated conditions were s

227 These results confirm that sand patties undergo a gradual dissolution of DOM in bot

228 When sand patties were exposed to simulated sunlight, a large

229 vated toxicity of leachates derived from oil sands petroleum coke.

230 SPs possess functional domains (SAND, PHD, bromodomain) that dock to DNA or post-transla

231 r activated carbon (GAC)-sand and anthracite-sand pilot-scale biofilters were investigated to determi

232 of electrode composition, surface treatment (sanding, polishing, plasma treatment), and graphite sour

233 The dry and nutrient-poor beach sand presents a taxing environment for microbial growth,

234 d with tap water as opposed to simulated oil sands process water.

235 n naphthenic acids (NAs) associated with oil sands process-affected water (OSPW) and those found natu

236 Oil sands process-affected water (OSPW) generated by the ext

237 n raised about possible seepage of toxic oil sands process-affected water (OSPW) into the Athabasca R

238 If oil sands process-affected water (OSPW) is to be returned to

239 Previously, we showed in vitro that the oil sands process-affected water (OSPW) organic fraction (OF

240 Oil sands process-affected water (OSPW) samples from differe

241 advance analytical methods for detecting oil sands process-affected water (OSPW) seepage from mining

242 od, complex mixtures of IOCs, e.g., from oil sands process-affected water (OSPW), have not yet been s

243 anic compounds are major contaminants in oil sands process-affected water (OSPW), of which naphthenic

244 and need for storage of large volumes of oil sands process-affected water (OSPW).

245 It seems that sand-protecting barriers play an important role in reveg

246 rface, kaolinite, a secondary mineral of the sand, provided favorable conditions for particle attachm

247 ogenic K12 strains in water-saturated Quincy sand (QS) columns amended with oxidized (OX) or unoxidiz

248 h aquifer with FIB primarily associated with sand rather than freely residing in the pore water.

249 lfuron had no effect on goosegrass in silica-sand regardless of evaporative demand.

250 Snowpacks in the Alberta Oil Sands Region (AOSR) of Canada contain elevated loadings

251 n have multiple sources in the Athabasca Oil Sands Region (AOSR).

252 An environmental sample from the oil sands region of Alberta, Canada, and dissolved organic m

253 els of heavy oil each day in the Alberta Oil Sands Region of Canada.

254 ir pollutant mixtures was applied in the Oil Sands region of northern Alberta, Canada.

255 wetlands situated in Alberta's Athabasca oil sands region revealed increased concentrations of polycy

256 lected during 2011-2014 in the Athabasca oil sands region were analyzed using two-dimensional gas chr

257 vironmental contaminant in the Athabasca oil sands region, but the ecotoxicological hazards posed by

258 This suggests landscapes across the oil sands region, which are dominated by low-relief wetlands

259 ge to environmental research in Canada's oil sands region.

260 at biomagnifies through foodwebs) due to oil sands related activities.

261 Surface mining and extraction of oil sands results in the generation of and need for storage

262 We find that tidal flats, defined as sand, rock or mud flats that undergo regular tidal inund

263 10)Be burial dating results derived from two sand samples from the fossiliferous deposits show that t

264 eady heavily biodegraded oil reservoirs, oil sands samples were amended with nutrients and electron a

265 red through a mixture of zeolite and coarse, sand-sized crystalline quartz.

266 Here, we explore the effect of clay- to sand-sized mineral abrasives (quartz, volcanic ash, loes

267 nts were conducted with an undisturbed loamy sand soil to investigate the influence of flow interrupt

268 with permanently deformable substrates like sand, soil, and mud, principles of motion on such materi

269 tics to the local environment, but other oil sands sources must also be considered.

270 -dependent performance of a diversity of non-sand-specialist snakes but overestimates the capability

271 n everyday activity, such as when walking on sand, suggests the existence of long-term motor memories

272 s, adding a small amount of celestite on the sand surface (20-30 mg/g) increased radium removal from

273 be topographically mapped onto a dynamic 3D sand surface through time.

274 ite, precipitating celestite directly on the sand surface was found to be the best option as it provi

275 y capillary flow due to evaporation onto the sand surface, where it was rapidly photodegraded.

276 e of column flood experiments through silica sand, systematically varying salinity and acidity condit

277 containing NAs in the subsurface near an oil sands tailings pond.

278 of golf-ball-size DWH-SOAs embedded in beach sand takes at least 32 years, while SOA degradation with

279 riments were conducted in a laboratory-scale sand tank packed with silt and aqueous tetrachloroethene

280 n functionalizing the proppant (i.e., quartz sand) that is used in hydraulic fracturing to prevent th

281 es and upgraders of the Athabasca Bituminous Sands, the largest reservoir of bitumen in the world.

282 Moreover, the flow of sand through a fixed porous bed could be regarded as par

283 at investigate the speed of the flow of fine sand through a fixed porous bed of packed glass beads un

284 s are needed for the result that the flow of sand through a porous bed or multiple parallel pipes can

285 From maps sketched in sand to supercomputing software, humans ubiquitously enh

286 Specimens of silica sand treated via enzyme induced carbonate precipitation

287 of surficial dust, over thin unconsolidated sand, underlain by a variable thickness duricrust, with

288 ibution from the source occurred in the fine sand versus pea gravel.

289 The performance of sand was compared with that of different types of classi

290 , teff straw was derived from teff stem, and sand was obtained from indigenous crushed stones.

291 Sand was studied as a solid support in ultrasound-assist

292 etcoke), haul road dust, and unprocessed oil sands were also analyzed.

293 f acid-washed glass beads or standard Ottawa sand, which presented less surface heterogeneity.

294 sediment consisting of coarse silt and fine sand, while the particles might infiltrate up to 13 cm i

295 ua gracilis seeds were planted in sterilized sand with (inoculated) and without (controls) soil micro

296 Our data showed that mixing sand with PW350-UO at a 20 wt % application rate almost

297 uricrust, with poorly sorted, unconsolidated sand with rocks beneath.

298 We studied this force scale by coating sand with ~ 2 mum-thick polydimethysiloxane, creating a

299 g in mixtures with sand (~175 mg PFAS/kg GAC-sand), with PFAS-spiked, laboratory-constructed soil (~4

300 lava sand (Cl-LS) and zeolite-dominated lava sand (Ze-LS), aiming at quantifying metal behaviour in C