ライフサイエンスコーパス: subsurface

1 latile occurrence in the surface and shallow subsurface.

2 ue of disclosing additives injected into the subsurface.

3 udies of its toxicity and persistence in the subsurface.

4 ss that was previously unnoticed in the deep subsurface.

5 tion and persistence in the deep terrestrial subsurface.

6 by the environmental conditions in the deep subsurface.

7 -associated Catellicoccus, through the beach subsurface.

8 oligotrophic conditions that dominate in the subsurface.

9 idered to assess colloid mobilization in the subsurface.

10 were deliberately introduced to react in the subsurface.

11 ansformation of, contaminant mass within the subsurface.

12 es segregate heterogeneously to the hydrogel subsurface.

13 s, Np is often assumed to be immobile in the subsurface.

14 mporally monitor biofilm accumulation in the subsurface.

15 ort processes in the naturally heterogeneous subsurface.

16 ecological risks if actively applied to the subsurface.

17 hemical and microbial processes occurring in subsurface.

18 large volumes of water are injected into the subsurface.

19 sphere by burying this greenhouse gas in the subsurface.

20 at the surface but become predominant in the subsurface.

21 n water quality to include exchange with the subsurface.

22 mopolitan in both the terrestrial and marine subsurface(2-4), the physiological and ecological roles

23 e of the heat buildup occurring in the ocean subsurface 21 months in advance.

24 is contribution, indirect N2O emissions from subsurface agricultural field drains and headwater strea

25 Extended areas of low resistivity in the subsurface alongshore combined with high radon in surfac

26 thod to monitor the transport of mZVI during subsurface amendment in quasi real-time.

27 ay of Raman spectroscopy techniques for deep subsurface analysis of biological tissues unlocks new pr

28 hods sample a relatively small volume in the subsurface and are difficult to collect within and near

29 oflexi) are widely distributed in the marine subsurface and are especially prevalent in deep marine s

30 but genuine risk when drilling into the deep subsurface and can have an immediate and significant imp

31 trations within 1 year, but stabilization of subsurface and deep ocean Hg levels requires aggressive

32 ritical in predicting fluid migration in the subsurface and is relevant to multiple environmental cha

33 ded to fully assess the effects of potential subsurface and surface releases of hydrocarbons on the w

34 ing and biogeochemical reactions in the deep subsurface and thus may be expected to influence the fat

35 ution ground penetrating radar images of the subsurface and transformed into sea-level indicators thr

36 ses reveal that this ubiquitous and abundant subsurface archaeal group has adopted a versatile life s

37 sulfur and carbon fluxes in the terrestrial subsurface are determined by the intersecting activities

38 e biogeochemical changes induced in the deep subsurface are poorly understood.

39 mplete consumption of CH4 is favoured in the subsurface atmosphere under near vapour-saturation condi

40 t climate change, the processes and rates of subsurface/atmospheric natural gas exchange remain uncer

41 and shallow diving states, and labelling all subsurface behaviour as deep dives or shallow dives disc

42 Our results indicate that subsurface behaviour in short-finned pilot whales is mor

43 Current methods to monitor subsurface biofilm growth in situ are indirect.

44 Subsurface biofilms are central to bioremediation of che

45 main by coupling the spatial distribution of subsurface biogeochemical facies with biomass-facies rel

46 Overall, we predict microbial impacts on subsurface biogeochemistry via iron, sulfur, and complex

47 The subsurface biosphere is largely unexplored and contains

48 sses and are specialized for survival in the subsurface biosphere.

49 of 87 surface soil samples (0-15 cm) and 23 subsurface boreholes (0-3 m).

50 In subsurface brines, Na(+) and Ca(2+) are naturally abunda

51 erm release of dissolved contaminants in the subsurface, but whether and how this exchange can affect

52 f the burial process in the sequestration of subsurface C and found our subsurface soils (0-3 m) cont

53 hemical solute concentrations in the shallow subsurface can be spatially highly variable within small

54 Microbial processes in the subsurface can be visualized directly using micromodels

55 uggests a strong biological role in high-CO2 subsurface carbon cycling.

56 These 3D maps probe subsurface carrier dynamics that are inaccessible with t

57 nificant improvement to our knowledge of the subsurface characteristics at these sites, clearly showi

58 This subsurface chemical imaging is based on tumor-targeted,

59 wide range of topical applications including subsurface, chemically specific, noninvasive temperature

60 and pro-NRG2 accumulates on cell bodies atop subsurface cisternae.

61 ill also be helpful in improving designs for subsurface CO2 injection.

62 olution under conditions closely relevant to subsurface CO2 injection.

63 he risk of migration of these chemicals from subsurface CO2 storage sites.

64 Particularly, subsurface cold water plays a key role to reduce these A

65 sensitively detectable microbial tracers for subsurface colloid transport and water flow.

66 on bacteria only rarely replicate quickly in subsurface communities undergoing substantial changes in

67 ning and metaproteomic analysis of this deep subsurface community reveals a carbon cycle driven by au

68 cohydrological separation, whereby different subsurface compartmentalized pools of water supply eithe

69 behavior of fractured cement under realistic subsurface conditions including elevated temperature, hi

70 es from a producing hydrocarbon reservoir at subsurface conditions.

71 ossibility of seawater contamination through subsurface conduit networks in a coastal karst aquifer.

72 Vapor intrusion from volatile subsurface contaminants can be mitigated by aerobic biod

73 Here we specify Southern Ocean surface-subsurface contrasts using a new tool, the combined oxyg

74 ea within about 20 km of the wellhead in the subsurface deepwaters at 1000-1200 m depth to the southw

75 (2.7 at%), pyrrolic-N, owing to surface and subsurface diffusion of C, N and NH is deduced from vari

76 mperatures with single-site resolution using subsurface dopants in silicon.

77 nitia show distinct chemistry in the shallow subsurface (down to several decimeters) relative to the

78 researched recently due to its relevance for subsurface engineering applications including sealing le

79 or transport promoters of some PPCPs in the subsurface environment and could affect their off-site e

80 lumn study was more directly relevant to the subsurface environment because of the high solid:water r

81 biogenic noncrystalline U(IV) species in the subsurface environment when subjected to redox cycling e

82 thus affect their fate and transport in the subsurface environment.

83 e fate of chromate, selenate, and sulfate in subsurface environments and offer new insight into the s

84 an pass through wastewater treatment plants, subsurface environments and potentially also drinking wa

85 Phosphate addition to subsurface environments contaminated with uranium can be

86 Supercritical CO2 is injected into subsurface environments during geologic CO2 sequestratio

87 ent bioattenuation rates could be impeded in subsurface environments near PFAA source zones.

88 Phosphate can be added to subsurface environments to immobilize U(VI) contaminatio

89 es a model of microbial carbon cycle in deep subsurface environments where hydrogen and sulfate are p

90 ntage over other Thermococcus species in hot subsurface environments where organic substrates are pre

91 ltivated microorganisms has been detected in subsurface environments, and we show that H2, CH4, and C

92 e remediation agent for uranium-contaminated subsurface environments, however, the nature of the reac

93 For example, in subsurface environments, mixing of groundwater and injec

94 In complex and heterogeneous subsurface environments, the concentrations of these sol

95 ay improve predictions of Cr(VI) behavior in subsurface environments.

96 , and precipitation on carbonate minerals in subsurface environments.

97 antages will expedite their dissemination in subsurface environments.

98 ant parameters for predicting Pu mobility in subsurface environments.

99 for the oxidation of organic carbon in many subsurface environments.

100 essed nuclear waste streams and contaminated subsurface environments.

101 f such As-bearing pyrites in low-temperature subsurface environments.

102 chanisms influencing macroscale phenomena in subsurface environments.

103 e in the plasma membrane and presence in the subsurface ER cisternae that are juxtaposed to the plasm

104 Most subsurface exchange will not result in N2O emissions; on

105 emicals derived from the surface rather than subsurface flow of these fluids from the underlying shal

106 voir roof and the physical properties of the subsurface flow path explain the gradual, near-exponenti

107 owing urban groundwater inputs, showing that subsurface flow paths potentially impact nutrient loadin

108 ground surface using conventional oil field subsurface fluid delivery technologies (packer and baile

109 e influence of depositional heterogeneity on subsurface fluid flow is now widely recognized, but inco

110 d gas development or carbon sequestration is subsurface fluid leakage in the near wellbore environmen

111 and gas (AOG) wells can provide pathways for subsurface fluid migration, which can lead to groundwate

112 e evolution, and they offer some support for subsurface fluidization models and mass loss through the

113 We sampled subsurface fluids from scCO2 -water separators at a natu

114 h volumes of deep ( approximately 200-500 m) subsurface fluids.

115 producers, fuelled by chemicals from Earth's subsurface, form the basis of life.

116 The lumps were due to subsurface formation of calcium phosphate crystalline de

117 distributions, porosity, and permeability of subsurface formations.

118 uggests MICP is a promising tool for sealing subsurface fractures in the near wellbore environment.

119 The subsurface geometry of this interaction has not been ful

120 A goal of subsurface geophysical monitoring is the detection and c

121 h substantial improvements particularly near subsurface grain boundaries and the critical buried p-n

122 enrichments, a photosynthetic biofilm and a subsurface groundwater aquifer.

123 rojects involving the artificial recharge of subsurface groundwater aquifers via the reuse of treated

124 Subsurface groundwater-surface water mixing zones (hypor

125 fe on Mars is/was likely to be resident in a subsurface habitat, where methane could be a source of e

126 wing Mn-rich brown spots at their surface or subsurface have been characterized by optical microscopy

127 near dependency between the intensity of the subsurface heat buildup and the magnitude and timing of

128 land surface temperatures due to additional subsurface heat sources such as buildings and their base

129 Here we show that regions with strong subsurface heterogeneity have enhanced present and futur

130 rological models, one of them accounting for subsurface heterogeneity.

131 hich is known to produce particularly strong subsurface heterogeneity.

132 gical models do not adequately consider this subsurface heterogeneity.

133 ver we currently understand little about how subsurface Hg stores participate in gaseous Hg cycling.

134 d environments, the microbial communities in subsurface high-CO2 ecosystems remain relatively unexplo

135 Subsurface, high-CO2 systems are poorly biologically cha

136 important; thus, thermal reactions involving subsurface hydrogen are the primary reaction mechanisms

137 eter-to-decimeter scales and are compared to subsurface hydrogen concentrations observed by Dawn's Ga

138 ogenation on Ni(110) and confirm the role of subsurface hydrogen in the mechanism of this reaction.

139 In addition, we find that subsurface hydrogen noticeably alters reaction barriers,

140 phase atomic hydrogen, surface hydrogen, and subsurface hydrogen reacting with adsorbed CO.

141 In the reaction involving surface or subsurface hydrogen, we investigate four possible pathwa

142 n and land-energy processes with surface and subsurface hydrology to study transpiration partitioning

143 oxide generation and consumption dictated by subsurface (hyporheic) residence times and biological ni

144 This high decomposition potential of OM in subsurface hypoxic waters presents a positive feedback o

145 We exemplify a plethora of subsurface, i.e., "in-chip" microstructures for microflu

146 Here we report the discovery of a massive subsurface ice layer, at least 16 km across, several kil

147 ites for long-term monitoring of the Earth's subsurface in the form of a deep subsurface microbiome i

148 tofluorescence and photon attenuation enable subsurface in vivo sensing.

149 characteristics make them successful in the subsurface, including genes involved in CO and H2 oxidat

150 dy, key questions remain on life in the deep subsurface, including whether it is endemic and the exte

151 s variables such as topography, landuse, and subsurface infiltration capacity combine to determine th

152 creasingly evident, to better understand the subsurface is critical to further understanding the Eart

153 hus, knowledge of microbial transport in the subsurface is crucial for maintaining groundwater health

154 active fission product whose mobility in the subsurface is largely governed by its oxidation state.

155 The Martian subsurface is more favourable to organic preservation th

156 or of zwitterionic and cationic PFASs in the subsurface is unknown, batch sorption experiments were c

157 guish between the surface bone layer and the subsurface layer, comprised of a brain tissue mimic modi

158 d microstructural defects appear beneath the subsurface layer.

159 10), soil P was characterized in surface and subsurface layers using sequential fractionation, P K-ed

160 e significant segregation of Pt over Ni-rich subsurface layers, allowing better formation of the crit

161 on the solar radiation penetrating into the subsurface layers, which induces differential heating in

162 ly offset Raman spectroscopy (SORS) to probe subsurface layers.

163 ght into the biochemical cycles that support subsurface life under the extreme condition of CO2 satur

164 culation is a prerequisite for a sustainable subsurface life, a Martian site with iron oxide precipit

165 Subsurface lithoautotrophic microbial ecosystems (SLiMEs

166 ies of sediments are commonly used to define subsurface lithofacies and these same physical propertie

167 on around a particular tree could reveal the subsurface location, or direction, of soil and soil-gas

168 Despite its subsurface location, we were interested in testing wheth

169 pression of co-contaminant biodegradation in subsurface locations where poly- and perfluoroalkyl subs

170 hanged nitrate consumption suggests that the subsurface major nutrient concentrations were lower in t

171 At both sites, PCB concentrations showed subsurface maxima (tropical Atlantic Ocean -800 m, North

172 t-, and labor-intensive; whereas traditional subsurface methods sample a relatively small volume in t

173 me-resolved information reshapes our view of subsurface microbial communities and provides critical n

174 It is not understood how subsurface microbial communities are assembled and wheth

175 Our results indicate that subsurface microbial communities predominantly assemble

176 and these same physical properties influence subsurface microbial communities.

177 arbon source for these two components of the subsurface microbial community is consistent and is temp

178 on of relatively young carbon sources by the subsurface microbial community occurs at sites with vary

179 the Earth's subsurface in the form of a deep subsurface microbiome initiative.

180 l activity, but assembly processes governing subsurface microbiomes remain a critical uncertainty in

181 raises questions about potential impacts of subsurface microbiota on carbon cycling and biogeochemis

182 led characterizations of enzymes from native subsurface microorganisms, without requiring that those

183 al weeks, show persistent ocean currents and subsurface mixing after pulse passage, thereby reducing

184 stivity tomography (ERT) was used to examine subsurface mixing dynamics.

185 on at Von Damm occurs rapidly during shallow subsurface mixing of the same fluids, which may support

186 nced imaging applications such as geological subsurface modelling or biomedical tissue analysis.

187 translucent media including the human body, subsurface monitoring of chemical or catalytic processes

188 d urban stream reaches, indicating effective subsurface N retention or denitrification and minimal im

189 imates) on two key environmental parameters: subsurface nitrate concentration and surface wind stress

190 fshore biomass is positively correlated with subsurface nitrate concentration.

191 Pervasive anoxia in the subsurface ocean during the Proterozoic may have allowed

192 expansion due to the freezing of a possible subsurface ocean generates stresses within the planet's

193 to the discharge of a large fraction of the subsurface ocean heat.

194 charge caused by relatively small changes in subsurface ocean temperature can amplify multi-centennia

195 t, as predicted by a statistical forecast of subsurface ocean temperatures and consistent with the ir

196 To prolong the lifetime of such a subsurface ocean to the present day and to maintain ocea

197 In our model, subsurface ocean warming associated with variations in t

198 Without a subsurface ocean, a positive gravity anomaly requires an

199 of Saturn's moon Enceladus draw water from a subsurface ocean, but the sustainability of conduits lin

200 result of an impact and if Pluto possesses a subsurface ocean, the required positive gravity anomaly

201 t atmosphere-ocean coupling characterized by subsurface oceanic structure is responsible for more rea

202 W) Raman spectra (2800-3600 cm(-1)) from the subsurface of colorectal tissue.

203 sublimation of ices at the surface or in the subsurface of cometary nuclei.

204 led pulsatile delivery of glutamate into the subsurface of explanted wild-type rat retinas elicits hi

205 The laser damage precursors in subsurface of fused silica (e.g. photosensitive impuriti

206 olation from the surface to the >5,000-y-old subsurface of marine sediment and identify a small core

207 Earth, methane on Mars is most likely in the subsurface of the crust.

208 sible threat initiating from the hydrophilic subsurface of the IOLs.

209 iches, such as the marine versus terrestrial subsurface, often expands the understanding of the genet

210 tand the distribution of remaining lingering subsurface oil residues from the Exxon Valdez oil spill

211 explicit predictions of the distribution of subsurface oil.

212 unter probability of different categories of subsurface oil.

213 can affect the safety and efficiency of the subsurface operation.

214 turning Circulation must be accomplished via subsurface pathways.

215 Here we present a 135-kyr record of shallow subsurface pCO2 and nutrient levels from the Norwegian S

216 res much of the variation that occurs during subsurface periods.

217 We found subsurface placement of phosphorus applications to be th

218 elevated above surface by the formation of a subsurface planar nanowire, a structure initiated mid-wa

219 c flowcell (i.e., micromodel) that simulates subsurface porous media.

220 material, possibly via explosive release of subsurface pressure or via creation of overhangs by subl

221 hydrological sciences, the heterogeneity of subsurface properties, such as hydraulic conductivities

222 ility compared with regions with homogeneous subsurface properties.

223 o hydraulic fracturing additives and related subsurface reactions, such as through the reaction of sh

224 The subsurface recalcitrance of perfluoroalkyl acids (PFAAs)

225 Fe(II)-rich clay minerals found in subsurface redox transition zones (RTZs) can serve as im

226 ain and the formation of dislocations in the subsurface region via a surface diffusion and trapping p

227 ental electronic processes that occur at the subsurface regions of inorganic solid photocatalysts.

228 2 and brine through a permeable sandstone at subsurface reservoir conditions, and low capillary numbe

229 Shallow magma intrusion builds subsurface reservoirs that are drained by volcanic erupt

230 st amounts of old, geologic methane (CH4) in subsurface reservoirs.

231 N2O emission from stream sediments requires subsurface residence times (and microbially mediated red

232 ility if leaked CO2 or brine interferes with subsurface resources, and estimates the MLR reduction ac

233 effects of evaporation and tide and waves on subsurface salinity distribution on a beach face.

234 ments, evaporation is an important driver of subsurface salinity gradients in marsh systems.

235 Trees could provide a similar subsurface sample where roots act as the "sampler' and a

236 pill in May 2010, which included one typical subsurface sample with a PAH concentration of 1.09 mug/L

237 columns packed with a natural heterogeneous subsurface sandy sediment.

238 orce the idea that grain-size disposition in subsurface sandy sediments drives the interstitial fluxe

239 We hypothesized that natural subsurface scCO2 reservoirs, which serve as analogs for

240 rial and archaeal communities inhabiting the subsurface seabed live under strong energy limitation an

241 Subsurface sediment, partitioned into 22 flow-through co

242 ns assembled from the metagenome of deep-sea subsurface sediments shows that the metabolism of some l

243 etogenesis was also confirmed in Peru Margin subsurface sediments where Bathyarchaeota are abundant.

244 omains exist within rocks, lithic fragments, subsurface sediments, and soil aggregates.

245 nd woody debris that accumulate in soils and subsurface sediments.

246 and abundant in the energy-deficient marine subsurface sediments.

247 coastal sediments, and deep-sea surface and subsurface sediments.

248 y formation of authigenic arsenian pyrite in subsurface sediments.

249 ntensify over region undergoing strong ocean subsurface shoaling where upper ocean heat content can d

250 nides and other adsorbed contaminants in the subsurface, significantly increasing their mobility.

251 isk assessment of the hydraulic integrity of subsurface sites.

252 lights the considerable amounts of carbon in subsurface soil below 30 cm, which is missed by standard

253 occur during the "zero curtain" period, when subsurface soil temperatures are poised near 0 degrees C

254 sequestration of subsurface C and found our subsurface soils (0-3 m) contained considerably more C t

255 In subsurface soils, few legacy P transformations were dete

256 ion fluxes (about 70%) were primarily due to subsurface sources of raw gas that migrated to the atmos

257 >2500 years, indicating the benzene was from subsurface sources such as natural hydrocarbon migration

258 oordinated surface square site adjacent to a subsurface stacking fault.

259 Research on the subsurface storage of CO2 is aimed at reducing uncertain

260 While moraine subsurface structure and internal processes are likely t

261 f the Orientale multiring basin, producing a subsurface structure consistent with high-resolution gra

262 ighly turbid layers mask chemically distinct subsurface structures.

263 roduction, where morphological, chemical and subsurface studies of nanocomposites, nanoparticle uptak

264 etely retained the pathogenic E. coli in the subsurface, suggesting that utilizing sand mixed with bi

265 ts (i.e., compounds designed to react in the subsurface) suggests that relevant transformation produc

266 ed nuclear waste and present in contaminated subsurface systems represents a major environmental chal

267 genetic intervention, rapid kinetics, remote subsurface targeting, and long persistence of photoconve

268 nic teleconnection between AMOC strength and subsurface temperature in the EEA impacted the intensity

269 Our subsurface temperature record shows abrupt subsurface wa

270 MOC to the WAM, we generated a new record of subsurface temperature variability over the last 21 kyr

271 ve correlation between AMOC strength and EEA subsurface temperatures caused by changes in ocean circu

272 al method for the noninvasive measurement of subsurface temperatures within diffusely scattering (tur

273 ith the creation of acidic conditions in the subsurface, the potential for generation of undesirable

274 ed by examining the evolution of surface and subsurface thermohaline properties, and an analysis of v

275 netration depth to noninvasively interrogate subsurface tissue features.

276 in Kr and Xe which are potentially valuable subsurface tracers.

277 phene layer, and demonstrate the tip-induced subsurface translation of neon atoms.

278 cline potentially play a significant role in subsurface transport of mass, heat, and salt in the glob

279 cal and hydrological processes governing the subsurface transport of PFASs at a former fire training

280 ating the rate coefficients into field-scale subsurface transport simulations showed that, in this sa

281 m under such conditions is needed to predict subsurface uranium behavior and optimize the selection a

282 The oxyl was separately observed by a subsurface vibration near 800 cm(-1) from Ti-O located i

283 t an n-SrTiO3/aqueous interface, we reveal a subsurface vibration of the oxygen directly below, and u

284 ls' decay, specifically probed by the oxyl's subsurface vibration, parallels that of the photocurrent

285 One can envision using the subsurface vibrations and their coupling across the inte

286 These experiments demonstrate subsurface vibrations and their coupling to solvent and

287 es into fragmentation processes operating in subsurface volcanic conduits.

288 of erupted material is much greater than the subsurface volume change inferred from ground displaceme

289 e bed to uplift, isolating the terminus from subsurface warming and allowing the ice sheet to advance

290 In the north Atlantic, subsurface warming causes larger increase in frequency o

291 r subsurface temperature record shows abrupt subsurface warming during both the Younger Dryas (YD) an

292 Such subsurface warming in AOGCM also acts to alter large dec

293 arch underscores the necessity of monitoring subsurface wastewater formation pressures and monitoring

294 d jet leads to increased upwelling of cooler subsurface water and strengthened equatorward transport,

295 contrast, peptide decomposition rate in the subsurface water, enriched with Pi (0.4-1.2 muM), was tw

296 on hypoxia formation in Pi-enriched coastal subsurface waters, as a higher OM decomposition rate lea

297 mulations known to be present in the shallow subsurface were reached.

298 1% in the form of micro-cavities at the weld subsurface where peak volumetric strain and triaxiality

299 impact craters is consistent with ice in the subsurface, which might have favored relaxation, yet lar

300 the solid agar created multiple surface and subsurface wrinkles with varying wavelengths across the