ライフサイエンスコーパス: aquifer

1 wn is the source of stray gas in the Trinity Aquifer.

2 eam starts to separate hydraulically from an aquifer.

3 bsurface conduit networks in a coastal karst aquifer.

4 served spring, which drains the investigated aquifer.

5 nthetic biofilm and a subsurface groundwater aquifer.

6 e of organic compounds was identified in the aquifer.

7 rt in a thin aquitard bounded by an adjacent aquifer.

8 e overall groundwater residence times in the aquifer.

9 ge signals have been detected in the shallow aquifer.

10 n to the phyllosilicate clay minerals of the aquifer.

11 As, creating a risk of high As in the beach aquifer.

12 s secondary sources, releasing U back to the aquifer.

13 e, lower saturated zone) within the alluvial aquifer.

14 d the water level in the perched groundwater aquifer.

15 umulation and distribution of FIB in a beach aquifer.

16 r pumping from the United States High Plains Aquifer.

17 trate from the vadose zone into the alluvial aquifer.

18 progress of such redox conversion within the aquifer.

19 ng oil fields compared with those for saline aquifers.

20 transport during remediation of contaminated aquifers.

21 sters dissolved arsenic (As) in contaminated aquifers.

22 import food irrigated from rapidly depleting aquifers.

23 waters and saltwater intrusion into coastal aquifers.

24 d a key process in the removal of nitrate in aquifers.

25 e models for particle transport in fractured aquifers.

26 ving elevated arsenic (As) concentrations in aquifers.

27 ta to trace international exports from these aquifers.

28 rawals could help with regime change in some aquifers.

29 l pathways of hydraulic connectivity between aquifers.

30 anaerobic conditions characteristic of many aquifers.

31 es have had deleterious effects on overlying aquifers.

32 port and permanent loss of fixed nitrogen in aquifers.

33 ntly the largest consumers of these critical aquifers.

34 e fate and longevity of BPA in sediments and aquifers.

35 uality and quantity in adjacent or overlying aquifers.

36 representative of underground reservoirs and aquifers.

37 n important biogeochemical process in anoxic aquifers.

38 o migrate upward into shallow drinking water aquifers.

39 ulations and in engineered storage in saline aquifers.

40 c matter during subsurface mixing in crustal aquifers.

41 implemented in sulfate-bearing, contaminated aquifers.

42 ions in the deeper group of Pliocene-Miocene aquifers.

43 re deposits, marine basins, and contaminated aquifers.

44 s specific to carbon sequestration in saline aquifers.

45 ast transit of water from the surface to the aquifers.

46 ty, and hence its delivery into contaminated aquifers.

47 ward and potentially contaminate groundwater aquifers.

48 le climate patterns are depleting rivers and aquifers.

49 ement of groundwater extraction from coastal aquifers.

50 ward of As-polluted groundwater in overlying aquifers.

51 As concentration (<37 mug/L) in the deepest aquifer (160-260 m) is less related to the As concentrat

52 ue but also relies significantly less on the aquifer (30%) for water needs.

53 y which makes bioremediation of contaminated aquifers a potential solution.

54 ion to groundwater in the Kansas High Plains Aquifer, a rapidly depleting asset supporting significan

55 For instance, in two of the selected USA aquifers, a decrease in anthropogenic influences by 20%

56 rrent NO3(-) production by anammox in anoxic aquifers, a process that has been largely overlooked.

57 ater consumption and it relies heavily on an aquifer (about 50% of agricultural consumption) that is

58 ex sediment and planktonic consortia from an aquifer adjacent to the Colorado River (USA) and reconst

59 xpected to be applicable in studies of other aquifers affected by explosives used in construction.

60 The Rifle alluvial aquifer along the Colorado River in west central Colorad

61 on and nitrogen dynamics indicated the urban aquifer also serves as a biogeochemical reactor.

62 ned by the hydrogeological formations of the aquifer and discharge type.

63 ater (500-5200 and 1200-6600 mug L(-1)) from aquifer and fractured sediments, respectively.

64 to the moisture regimes present in aquitard, aquifer and fractured zones.

65 Vertical water fluxes in the aquifer and percent coarse material above the well scree

66 stream receiving water from the High Plains Aquifer and the occurrence of fishes characteristic of s

67 scales for transport through the floodplain aquifer and vadose zone.

68 ep shale horizons, reach shallow groundwater aquifers and affect local water quality, either from tho

69 Polar TAs accumulate in underground aquifers and appear to be the most abundant class of org

70 bout the attenuation of solutes within karst aquifers and even less about the attenuation of particul

71 the sandy Holocene and gravelly Pleistocene aquifers and is also abstracted by the pumping station.

72 monitor the reactivity of micropollutants in aquifers and may guide future efforts to accomplish CSIA

73 The interfaces between aquifers and rivers or lakes have been identified as bio

74 widespread host phase for Pb in groundwater aquifers and soil pore fluids.

75 ion) and blue (extracted from rivers, lakes, aquifers, and dams) water demand and crop yields for sev

76 omineralization, CO2 sequestration in porous aquifers, and pressure solution and crystallization in c

77 tory, persistent, highly mobile in soils and aquifers, and yet under-researched.

78 d favoring stronger degradation close to the aquifer-aquitard interface than with increasing depth.

79 Borden research site was selected, where an aquifer-aquitard system was artificially contaminated by

80 Fractured aquifers are a relatively under-studied area of groundwa

81 Depleted gas or oil reservoirs and saline aquifers are considered as suitable reservoirs providing

82 the cereals produced by these overexploited aquifers are critical to US food security (contributing

83 Although karst aquifers are far more susceptible to contamination than

84 Deep groundwater aquifers are poorly characterized but could yield import

85 rsone-amended litter does not influence deep aquifer arsenic concentrations but is transported as ino

86 In the shallowest Holocene-Pleistocene aquifers, arsenic occurrence is best described by distan

87 ial use of saline groundwater of the coastal aquifer as feedwater for desalination in comparison to s

88 nd upwelling regional recharge from the deep aquifer as sources of the rising conductivity.

89 dwater monitoring network (GMN) in a potable aquifer at a CO2 enhanced oil recovery (CO2 EOR) site.

90 en flow may mix dissolved CO2 throughout the aquifer at fast advective time-scales through convective

91 enated groundwater into a saturated alluvial aquifer at the Rifle, CO field site.

92 l West Bengal, India, those from Pleistocene aquifers at depths >70 m beneath paleo-interfluves conta

93 ted to the As concentration of the overlying aquifers because the groundwater here has a component of

94 Because most contaminated aquifers become reduced via biological activity, the rea

95 is a key factor for sustaining the observed aquifer behaviors despite continuous oxygen influx and t

96 of Red River water into arsenic-contaminated aquifers below Hanoi was investigated.

97 Pleistocene aquifers beneath deep paleo-channels typically host grou

98 near-surface horizon and oxic-suboxic gravel aquifers beneath the soil horizons, Fe(III)-oxides were

99 emoving organic pollutants from contaminated aquifers but the major steering factors are still surpri

100 monstrate CO2 leakage detection in a shallow aquifer by monitoring groundwater pH, alkalinity, and di

101 l model whereby FIB are delivered to a beach aquifer by wave-induced infiltration across the beach fa

102 However, contamination of shallow potable aquifers by HVHF at depth has never been fully documente

103 ration in rock, and intrusion of groundwater aquifers by saline water.

104 ydraulic relationship between the stream and aquifer can be altered from hydraulic connection to disc

105 Seepage of SCN(-)-contaminated waters into aquifers can occur from unlined or structurally compromi

106 ured at large point sources into deep saline aquifers can significantly reduce anthropogenic CO2 emis

107 odel solutions, with those representative of aquifer conditions requiring lower NO2(-) reoxidation fl

108 nd into density-stratified coastal carbonate aquifers containing a surprising diversity of endemic an

109 ic contamination in drinking waters by using aquifers containing Pleistocene sediments.

110 observations were used to estimate that the aquifer contains approximately 18% water sourced from th

111 ical role in the microbial detoxification of aquifers contaminated with chloroethenes and chlorethane

112 ate the characterization of air pollution or aquifer contamination with organic pollutants.

113 rough stratigraphy typical of fluvio-deltaic aquifers could contaminate deep (>150 m) groundwater wit

114 eakages of CO2 from storage sites to shallow aquifers could have adverse impacts on the quality of po

115 h as those comprising the deeper Pleistocene aquifer) could stimulate microbial communities and resul

116 ) and the overlying Condamine River Alluvial Aquifer (CRAA), using groundwater methane (CH4) concentr

117 ormations worldwide where local and regional aquifer depletions occur.

118 together with their distribution across the aquifer depth and performed semigeneric 2D reactive mass

119 When CO2 is injected in saline aquifers, dissolution causes a local increase in brine d

120 river water becomes anoxic in the uppermost aquifer due to the oxidation of dissolved organic carbon

121 leads to the immobilization of CO2 in saline aquifers, enhancing the security and capacity of storage

122 he prevalence of alkaline conditions in many aquifers, Fe(III) reduction may thus proceed via S(0)-me

123 region, it relies predominantly (81%) on the aquifer for its water supply.

124 upon cereals produced by these overexploited aquifers for 9.2% of its domestic cereal supply.

125 akage into shallow, overlying formations and aquifers from Marcellus Shale gas drilling operations is

126 Aquifers from these regions contribute up to half of the

127 plications for storage of CO2 in deep saline aquifers, fuel cells, oil recovery, and for the remediat

128 the most important variable but near-surface-aquifer geochemical data also were significant.

129 ter, redox differences, and the influence of aquifer geochemistry.

130 In coastal aquifers, groundwater transits the subterranean estuary,

131 Groundwater in the aquifer has a component of downward flow via leakage thr

132 We show that oxidative U(VI) release to the aquifer has the potential to sustain a groundwater conta

133 Deep aquifers have been developed for oil and gas extraction,

134 desh, we illustrate how interactions between aquifer heterogeneity and groundwater exploitation jeopa

135 ge rate, the number of monitoring wells, the aquifer heterogeneity, and the time for a CO2 plume trav

136 at incorporate geostatistical simulations of aquifer heterogeneity.

137 y than those with unconsolidated or fissured aquifers, highlighting the vulnerability of these hydrog

138 oncerns about the potential contamination of aquifers; however, the groundwater fate and transport of

139 ter-methane attenuation in the Poison Canyon aquifer: (i) consumption of methane and sulfate and prod

140 background levels and levels expected in an aquifer impacted by a small leakage, respectively.

141 te the role of contaminated baseflow from an aquifer in driving stream chemistry.

142 were from an unconsolidated sand and gravel aquifer in Kansas, containing 0-4 wt % carbonates.

143 aic Bengal Aquifer System (BAS), the largest aquifer in south Asia.

144 s and Mn contamination including the Glacial Aquifer in the U.S., the Ganges-Brahmaputra-Mehta Basin

145 timulation conditions in an RDX-contaminated aquifer in Umatilla, OR.

146 s of Mo in drinking-water wells from shallow aquifers in a region of widespread CCR disposal in south

147 Elevated arsenic (As) in aquifers in close proximity to in situ oil sands extract

148 ated by human activities, while the selected aquifers in Germany are natural flow-dominated.

149 quifers in the USA, and half of the selected aquifers in Iran are dominated by human activities, whil

150 amples collected from representative potable aquifers in the Gulf Coast area.

151 Aquifers in the Upper Colorado River Basin (UCRB) exhibi

152 that approximately one-third of the selected aquifers in the USA, and half of the selected aquifers i

153 tion appear to have started replenishing the aquifers in western and southern parts of India.

154 ial leakage of reservoir fluids into shallow aquifers, in particular the possible environmental impac

155 d residence time and storage capacity of the aquifer indicate that restoration projects designed to p

156 Simulated transport of E. coli in a beach aquifer is complex and does not correlate with conservat

157 Groundwater chemistry in the shallow aquifer is dominated mainly by silicate mineral weatheri

158 notion that the source of stray gas in this aquifer is the Strawn.

159 he latter 'poroelastic' response of confined aquifers is a well-established phenomenon which has been

160 storage reservoirs to overlying groundwater aquifers is considered one of the major potential risks

161 Joaquin Valley exceeds replenishment of the aquifer, leading to substantial diminution of this resou

162 presented here can be extended to multilayer aquifer/low-permeability systems to assess the significa

163 itu bacterial communities inhabiting shallow aquifers (<30 m) at two sites in Araihazar, Bangladesh,

164 the world's freshwater reserves are found in aquifers, making groundwater one of the most important r

165 hrough groundwater withdrawal and changes in aquifer management during the decade spanning 1996-2005.

166 ion using anoxic microcosms established with aquifer material from a CF-contaminated site.

167 Microcosms established with soil and aquifer materials from five distinct locations dechlorin

168 to characterize the redox properties of the aquifer materials that are responsible for abiotic NA.

169 ring their interaction with Fe oxides in the aquifer matrix.

170 storage formation into an overlying potable aquifer may adversely impact water quality and human hea

171 fronts at the interface between streams and aquifers may therefore provide globally widespread condi

172 known to exist in other uranium-contaminated aquifers, may be regionally important to uranium persist

173 tion by three Fe(III)- and Mn(IV)-containing aquifer minerals: ferrihydrite, goethite, and pyrolusite

174 nium in biofilms sampled from a contaminated aquifer near Rifle, CO.

175 evels of hydrocarbon gases in drinking-water aquifers near gas wells natural or anthropogenic?

176 The Northwest India Aquifer (NWIA) has been shown to have the highest ground

177 corresponds to a vertical flow rate into the aquifer of 19 m/year.

178 Alluvial aquifers of gravel-bedded river floodplains present a co

179 on of these top consumers in four floodplain aquifers of Montana and Washington is methane-derived.

180 llions of people worldwide, with the deltaic aquifers of SE Asia being particularly polluted.

181 enriched in SiO2 and Zn, the large detrital aquifers of the island typically present enhanced concen

182 aseline concentrations of methane in shallow aquifers of the St. Lawrence Lowlands and its sources us

183 Sediments were moistened with synthetic aquifer or deionized water according to the moisture reg

184 This could mean that natural aquifer or stream sediment materials were a primary cont

185 sites, the risk of CO2 migrating to potable aquifers or reaching the atmosphere was negligible due t

186 case of any unplanned migration into shallow aquifers or to the surface.

187 e and public supply water wells drawing from aquifers overlying the Barnett shale formation of Texas.

188 Aquifer physical model experiments were performed to inv

189 ater level fluctuations are dominated by the aquifer poroelastic response to changes in terrestrial w

190 ponds or tube wells to alternatives [managed aquifer recharge (MAR) and rainwater harvesting] that ai

191 Managed aquifer recharge (MAR) is a water reuse technique with t

192 ther trace metal contaminants during managed aquifer recharge (MAR) poses a challenge to maintaining

193 ses to changes in groundwater storage due to aquifer recharge and drainage as well as to changes in s

194 ions remain about how these types of managed aquifer recharge systems should be designed; furthermore

195 e performed metagenomic sequencing of a deep aquifer, recovering two near-complete genomes belonging

196 f aromatic compounds, which hence impact the aquifer redox state and the carbon fate.

197 n water abstraction scenarios on the overall aquifer regime (e.g., depleted, natural flow-dominated,

198 SA, Germany and Iran to evaluate the current aquifer regime.

199 ompiled groundwater chemical data from three aquifer regions across the world that have been reported

200 Contemporary microbial monitoring of aquifers relies on groundwater samples to enumerate nona

201 tions of rhamnolipid for surfactant-enhanced aquifer remediation (SEAR), which may overcome the drawb

202 oil, gas, or produced water to a groundwater aquifer resulting in contamination of drinking water.

203 ate-poor aquifers than in the carbonate-rich aquifers, resulting in potential groundwater acidificati

204 ter recharge, groundwater residence time and aquifer-river exchanges from few hours to several weeks

205 d selective enough to be used in a synthetic aquifer sample.

206 sands and overlying reduced, gray, Holocene aquifer sands.

207 hanisms of As transformation and mobility in aquifer sediment (in particular, the PRB downstream link

208 through columns constructed with homogenized aquifer sediment and continuously infused with lactate,

209 the site-specific groundwater chemistry and aquifer sediment properties.

210 role in the mobilization of As from Fe-rich aquifer sediment under anoxic conditions.

211 for the genome was obtained from terrestrial aquifer sediment, in which RIFRC-1 comprised approximate

212 speciation and mobility of As in downstream aquifer sediment, where up to 47% of total As initially

213 t organisms in biogeochemical cycling in the aquifer sediment.

214 ng high arsenic associated with fine-grained aquifer sediment.

215 cale cultivation-independent metagenomics to aquifer sediments and groundwater, and reconstruct 2,540

216 iver Site, South Carolina, and in subsurface aquifer sediments collected downgradient from the basin.

217 The presence of aquifer sediments decreased the efficiency of the remedi

218 ons using contaminated canal and groundwater aquifer sediments from an industrial site.

219 to quartz, goethite, birnessite, illite, and aquifer sediments induced an average isotopic fractionat

220 In this unique long-term study, aquifer sediments subjected to reductive Cr(VI) immobili

221 study examines As retention and transport in aquifer sediments using a multistage column experiment i

222 ease from Holocene and Pleistocene Cambodian aquifer sediments was investigated using microcosm exper

223 In microcosms from heavily contaminated aquifer sediments, a phylotype with 92.7% sequence simil

224 ize the propensity of As desorption from the aquifer sediments.

225 ere present and active in both the canal and aquifer sediments.

226 than those measured in the associated upland aquifer sediments; similarly, the Pu concentration solid

227 be used as indicative parameters in potable aquifers, selection of geochemical parameters for CO2 le

228 ngs suggest that HFO-1234yf recalcitrance in aquifers should be expected; however, HFO-1234yf is not

229 tland than in the low-organic matter content aquifer soils.

230 pure metal oxides, clays, and representative aquifer solids collected from field sites in the presenc

231 nalysis of paired samples of groundwater and aquifer solids, indicated that solid/water partitioning

232 nd manganese-containing minerals, clays, and aquifer solids.

233 fide which favors stabilization of metals in aquifer solids.

234 nt mass diffuses from the aquitard following aquifer source mass depletion.

235 ter quality and to ensuring the viability of aquifer storage and recovery techniques.

236 arity between Bravo Dome and major US saline aquifers suggests that significant amounts of CO2 are li

237 e water mass loading and unloading above the aquifer surface.

238 iod from the tropical, fluvio-deltaic Bengal Aquifer System (BAS), the largest aquifer in south Asia.

239 nation patterns throughout the Delta's multi-aquifer system as observed in a spatially exhaustive dat

240 at the hydraulic connectedness of the stream-aquifer system can reach a critical disconnection state

241 show that the biogeochemical response of the aquifer system has not mobilized naturally occurring tra

242 documented the response of the Poison Canyon aquifer system several years after upward migration of m

243 as a major driving forcing affecting coastal aquifer system, and deterministic modeling has been very

244 water as the most saline source to a coastal aquifer system, thereby concluding that seawater infiltr

245 arsenic throughout the Mekong Delta's multi-aquifer system, with implications for management of simi

246 tion of peat, which is commonly found in the aquifer system.

247 ely analyze the physical processes of stream-aquifer systems from connection to disconnection.

248 le use of groundwater resources in all three aquifer systems intensified from 2000 to 2008, making it

249 oundwater transfers from these overexploited aquifer systems to their final destination.

250 s, Mississippi Embayment, and Central Valley aquifer systems totaled 17.93 km(3), 9.18 km(3), and 6.8

251 s, Mississippi Embayment, and Central Valley aquifer systems within the United States are currently b

252 of hydrochemical parameters present in many aquifer systems.

253 ies, large plumes of HCHs persist within two aquifer systems.

254 cussion about their potential to contaminate aquifers tapped by domestic groundwater wells.

255 gether with stray flowing gas in the Trinity Aquifer, Texas.

256 y, a variable representing three-dimensional aquifer texture from the Central Valley Hydrologic Model

257 were more significant in the carbonate-poor aquifers than in the carbonate-rich aquifers, resulting

258 from a global Hesperian cryosphere-confined aquifer that was infused by south polar meltwater infilt

259 end on groundwater from geologically complex aquifers that are over-exploited and threatened by conta

260 mining and ore processing; often in alluvial aquifers that contain organic-rich, reduced sediments th

261 ciers provide summer meltwater to rivers and aquifers that is sufficient for the basic needs of 136 m

262 In anoxic groundwater aquifers, the long-term survival of Dehalococcoides mcca

263 In many urban areas with contaminated aquifers, there exists a desire for sustainable heating

264 oparticles to increase the mobility of As in aquifers, thereby accounting for discrepancies between p

265 rp rise in numbers in the last decades, with aquifer thermal energy storage (ATES) and borehole therm

266 and attenuation of particles within a karst aquifer through multitracer testing, using four differen

267 on of the widespread As-pollution in shallow aquifers through exploitation of deep Pleistocene aquife

268 iltration to leach arsenic from the Holocene aquifer to below the World Health Organization limit of

269 ed, well-drained soils, and transport in the aquifer to the well screen.

270 aracterization of biogeochemical reactivity, aquifer transport properties, groundwater recharge, grou

271 ource of metals released into a CO2-impacted aquifer, two batch experiments were conducted.

272 te can be stable over decadal time scales in aquifers under low DO conditions.

273 The groundwater age at 40 m depth in the aquifer underlying the river was 1.3 +/- 0.8 years, dete

274 allow to intermediate depth fractures to the aquifer used as a potable water source.

275 aquitard with mass exchange with an adjacent aquifer using the method of images.

276 ere investigated at multiple locations in an aquifer variably affected by a large, wastewater-derived

277 rtificial recharge of subsurface groundwater aquifers via the reuse of treated municipal wastewater.

278 Aquifer vulnerability models were developed to map groun

279 urce mechanism of chloride to the floodplain aquifer was high-concentration, overbank flood events in

280 th these physiological attributes, the local aquifer was microoxic with small concentrations of avail

281 impact on methane chemistry in the overlying aquifers was investigated.

282 r injection pipeline flowing anaerobe saline aquifer water.

283 r growth conditions relevant in contaminated aquifers, we investigated Dehalococcoides-level populati

284 Thermogenic methane was detected in two aquifer wells indicating a potential contamination pathw

285 f alpha-HCH from the Quaternary and Tertiary aquifers were analyzed.

286 Sites representing karst aquifers were of significantly worse microbial quality t

287 (127)I and (129)I are similar within the SRS aquifer/wetland system.

288 an serve as long-term contaminant sources to aquifers when contaminant mass diffuses from the aquitar

289 the convection and mixing of CO2 in a brine aquifer, where the spread of dissolved CO2 is enhanced b

290 ilization of geogenic uranium in the studied aquifers which are unaffected by nuclear activities.

291 seawater, pumped from beach wells in coastal aquifers which penetrate beneath the freshwater-seawater

292 ut has consumed the reducing capacity of the aquifers, which is present as pyrite, degradable organic

293 s indicate FIB rapidly accumulate in a beach aquifer with FIB primarily associated with sand rather t

294 and ibuprofen was released into a mesoscale aquifer with quasi-two-dimensional flow.

295 ed 39-90% of potential N2 production in this aquifer, with rates on the order of 10 nmol N2-N L(-1) d

296 ore susceptible to contamination than porous aquifers, with the transport of particulate matter being

297 purified recycled water recharge of shallow aquifers within Orange County, CA.

298 n from the near-surface to fractured-bedrock aquifers within the Piedmont.

299 factor for megacity groundwater supplies in aquifers worldwide.

300 ers through exploitation of deep Pleistocene aquifers would improve if guided by an understanding of