ライフサイエンスコーパス: river

1 rth Indian River Plain containing the Ganges River).

2 from distinct habitats (two lakes versus two rivers).

3 y distance and isolation by resistance (main rivers).

4 en hatchery and natural-origin fish for each river.

5 sediment and porewater of the lower Passaic River.

6 d sediments from Lake Megantic and Chaudiere River.

7 he confluence with the South Fork Shenandoah River.

8 the same surface water from the Mississippi River.

9 from the Fresh Kills Landfill and the Hudson River.

10 a long-term source of nutrients to the Mara River.

11 ed by natural processes in this reach of the river.

12 an, to the Baltic Sea, and upstream the Elbe River.

13 discharge extremes of the lower Mississippi River.

14 ghly contaminated regions across the Passaic River.

15 sured in either the IHSC or the Saint Joseph River.

16 e signature of an independent Saraswati-like river.

17 nce of populations isolated by the Richelieu River.

18 med the atmospheric depositional flux to the river.

19 t loss and influences water quality in large rivers.

20 streams to the benthic-water column zone in rivers.

21 , approximately 50% of the input from Arctic rivers.

22 al problems like eutrophication of lakes and rivers.

23 (87)Sr/(86)Sr of the Ganga compared to other rivers.

24 similar to the estimated export from palaeo rivers.

25 d counterparts in two geographically distant rivers.

26 lake near the confluence of Amazon and Negro rivers.

27 llected from two acid mine drainage impacted rivers.

28 about 130,000 y with respect to inputs from rivers.

29 rs that involved movements between lakes and rivers.

30 ppear to be ubiquitous contaminants in Dutch rivers.

31 R-MLWs in the riparian zone of a third-order river and analyzed for hydrochemical parameters and stab

32 g downstream along the AFFF-impacted Welland River and between water and sediment suggested differenc

33 flood at 5 locations along the South Platte River and from 7 tributaries along the Colorado Front Ra

34 with florescence indexes in the San Leonardo River and in the alluvial plain stretch of the Simeto Ri

35 f PCBs were generally found in the Lower Fox River and in the Indiana Harbor and Ship Canal.

36 treatment plants (WWTPs) situated along the river and Lake Erie.

37 ysis, based on the phenology and duration of river and lake use.

38 The anticipated feed streams are natural river and seawater, both of which contain not only monov

39 y applied to the determination of Cu in tap, river and seawater, rice flour and black tea samples as

40 t these glaciers provide summer meltwater to rivers and aquifers that is sufficient for the basic nee

41 Organic carbon (OC) from rivers and coasts of China were retrieved and statistica

42 deposited in the bay catchment likely enter rivers and provide an unexpected source to northern estu

43 rget species can readily move in streams and rivers and the goal is to measure it, and with that infe

44 ive Tw-Ta across small ponds, lakes, streams/rivers and the sea shore (i.e. downward QH), with Tw-Ta

45 ng that flow and erosional processes in both rivers and volcanoes can produce irreversible structural

46 concentrations might also explain why Arctic rivers annually transport large amounts of Hg to the Arc

47 ess-affected water (OSPW) into the Athabasca River (AR).

48 Eels collected this far into rivers are benthic and fully adapted to freshwater; that

49 Indirect nitrous oxide (N2O) emissions from rivers are currently derived using poorly constrained de

50 Because rivers are dendritic networks, there is only one dispers

51 Streams and rivers are important conduits of terrestrially derived c

52 ed after identification of the Alaskan White River Ash in northern Europe, recognition of ash from th

53 The Tarim River is the longest inland river at an arid area in China.

54 s (inland hyporheic, nearshore hyporheic and river); (b) assembly processes that generated these patt

55 lanis) wild specimens captured in the Lambro river basin (Como, Northern Italy) were investigated in

56 actors to streamflow alteration in the Tarim River Basin (TRB) using the double mass curve method (DM

57 Aquifers in the Upper Colorado River Basin (UCRB) exhibit persistent uranium (U) ground

58 ugh terrestrial transport crossing the major river basin borders is also confirmed by historical sour

59 hes in both regions to streamflow anomalies, river basin characteristics, species traits, and non-nat

60 sh species over 18 years in a large, dryland river basin in southwestern United States.

61 Note that the Tarim River Basin is more vulnerable to the impact of emission

62 long with newly sampled wells in the Yangtze River Basin of China.

63 er resource management and governance at the river basin scale is critical for the sustainable develo

64 from different datasets are inconsistent at river basin scales, and the magnitude of index differenc

65 (CMIP5) models to the arid basin (the Tarim River Basin, TRB) and humid basin (the Yangtze River Bas

66 ver Basin, TRB) and humid basin (the Yangtze River Basin, YRB) were evaluated, determining the respon

67 xtant populations throughout the Mississippi River Basin.

68 ard infrastructures extend across four major river basins, 12,500 stream km, and contribute to 100 lo

69 form species found in the Amazon and Orinoco river basins, yet few resources for genetic studies and

70 tes water inputs to the upper Indus and Aral river basins.

71 nt rainfall datasets with streamflow from 89 river basins.

72 River bed-load transport is a kind of dense granular flo

73 inity, pH, Al, and Fe during an uncontrolled river breach in 2011, however, incorporating sediment bi

74 irical analysis to quantify plastic loads in rivers can be extended easily by additional potential pr

75 Focusing on three UK river catchments with contrasting bedrock and superficia

76 anaged plastic waste (MMPW) generated in the river catchments.

77 e stages: (i) peat initiated in an abandoned river channel with open water and aquatic plants; (ii) i

78 ember 2013 extreme flood in the South Platte River, Colorado, USA.

79 cted Wetland; XR: Xinxue River; XRCW: Xinxue River Constructed Wetland).

80 r wetlands (ZR: Zhaoniu River; ZRCW: Zhaoniu River Constructed Wetland; XR: Xinxue River; XRCW: Xinxu

81 water fishes in the Upper and Lower Colorado River (CR), Alabama-Coosa-Tallapoosa (ACT), and Apalachi

82 s likely to increase with eutrophication and river damming.

83 ring spring season and along the Mississippi River Delta during the fall season.

84 The investigated river delta experiences significant pesticide inputs, le

85 pect compounds in the Sacramento-San Joaquin River Delta in Northern California.

86 ponding wheat grain samples from the Yangtze River Delta region were analyzed by DRIFTS and chemical

87 mites australis mosaic habitat in the Yellow River Delta, China.

88 plant community in the subsiding Mississippi River Delta.

89 We found sites in river deltas had larger OC stocks (175-504 Mg/ha) than t

90 The form and function of river deltas is intricately linked to the evolving struc

91 or plague outbreak hotspots, while navigable rivers determined the geographic pattern of sporadic pla

92 Contingents associated with one river (Detroit or St. Clair) were rarely detected in the

93 reatment facility effluent, and concentrated river DOM (used as a reference).

94 nt, turkey litter leachate, and concentrated river DOM did not stimulate phytoplankton growth greater

95 Characterization of river drainage networks has been a subject of research f

96 We find that the gravel fluxes from rivers draining the central Himalayan mountains, with up

97 The persistence of such a river during the Harappan Bronze Age and the Iron Age Ve

98 an average of 2.6% annually across all eight rivers during the study period, decreasing by 39% from 0

99 s of their migration is crossing of the Mara River, during which thousands drown annually.

100 arcasses and 1,100 tons of biomass enter the river each year.

101 entified three populations along the Yangtze River, each one connected to a group of admixed ancestry

102 animal migration can have large impacts on a river ecosystem, which may influence nutrient cycling an

103 Predicting how river ecosystems respond to warming has been hindered by

104 g is affecting the structure and function of river ecosystems, including their role in transforming a

105 de metropolitan boundaries and impact distal river ecosystems.

106 The Elizabeth River (ER) Superfund site represents a "natural-experime

107 erranean, with one ecotype confined near the river estuaries.

108 ticles and in free-living forms in the Pearl River Estuary (PRE) over a 10-month period.

109 study done in the Lake Superior-Saint Louis River estuary using SourceTracker, a program that calcul

110 pycnocline along a salt wedge estuary (Yarra River estuary, Australia).

111 assays were conducted in the N-limited Neuse River Estuary, North Carolina from 2014 to 2015.

112 a commercial mussel raft in the urban Bronx River Estuary, NY, in waters closed to shellfish harvest

113 flowing waterways, such as sewers, springs, rivers, etc., ensuring wide applicability of the develop

114 water samples across four of Brazil's major river floodplain systems (Amazon, Araguaia, Parana, and

115 We analyzed the timing of river floods in Europe over the past five decades, using

116 Mississippi River floods rank among the costliest climate-related di

117 ave an impact on the magnitude and timing of river floods; however, no consistent large-scale climate

118 remes of ENSO climate variability, influence river flow and flooding at the global scale.

119 Glaciers impart unique footprints on river flow at times when other water sources are low.

120 analysis is undertaken using the ERA-20CM-R river flow reconstruction for the twentieth century.

121 ple disturbance events and for management of river flows and fire regimes.

122 gradation (that is, sediment deposition by a river) following the 1999 Chi-Chi and 2008 Wenchuan eart

123 em, which may influence nutrient cycling and river food webs at decadal time scales.

124 However, surface rivers forming on ice shelves could potentially export s

125 Humic Substances Society standards, Suwannee River fulvic acid (SRFA) and Suwannee River natural orga

126 We use Suwanee River Fulvic Acid (SRFA) as a surrogate for HULIS and in

127 acidic nonirradiated and irradiated Suwannee River Fulvic Acid (SRFA) solutions are investigated in t

128 nd gamma-Al2O3) and organic matter [Suwannee River fulvic acid (SRFA)] on Fe(II) oxidation rates and

129 Analyzing Suwannee river fulvic acid as a common HULIS surrogate shows a si

130 HW) and MHW containing 2.5 mg L(-1) Suwannee River fulvic acid.

131 lysis further suggests that the flux of V in rivers has been incremented by about 15% from human acti

132 Riverine environments, such as streams and rivers, have been reported as sources of the potent gree

133 The river hippopotamus (Hippopotamus amphibius), one of the

134 ed (DI) water at pH 5.6 +/- 0.2 and Suwannee River humic acid (SRHA) at pH 5.1 +/- 0.2 using low dose

135 try, and biological activity in the Columbia River HZ, the grain size distributions for sediment samp

136 0 Lower CR) were highest in lowland mainstem rivers impacted by large dams and in desert springs.

137 nditions of Songhua River, the fifth longest river in China, using physical structural integrality (P

138 tion in the Yellow River, the second-longest river in China.

139 90 km stretch of the Simeto River, the main river in Sicily, and the smaller San Leonardo River, whi

140 P) in seven subwatersheds of the Mississippi River in St. Lawn fertilizer and pet waste dominated N a

141 iverine properties (i.e., area and number of rivers in a paleodrainage).

142 accretion along the large deltas of the main rivers in the Arctic.

143 Although ARD impacts >12,000 miles of rivers in the U.S. and has an estimated cleanup cost of

144 lateau were found comparable with most other rivers in the world; and it was revealed that the evasio

145 Results were examined by subpopulations of rivers, including urban or nonurban and three defined ec

146 ted to have flown independently of the Indus River into the Arabian Sea, perhaps along courses of now

147 resent a global model of plastic inputs from rivers into oceans based on waste management, population

148 culate the global plastic debris inputs form rivers into the sea to range between 0.41 and 4 x 10(6)

149 iments in a major urban waterbody fed by the River Irwell, Manchester, UK.

150 er show that the input of (236)U by the Elbe River is negligible, while there might be a maximum inpu

151 PCO2) indicate that water recharged from the river is present in both the sandy Holocene and gravelly

152 The Tarim River is the longest inland river at an arid area in Chi

153 absence of barriers, barriers along mainstem rivers isolate depauperate western fish assemblages from

154 in wastewater-dominated reaches of the Grand River (Kitchener, ON) to verify their feasibility for de

155 ation at 540 river sites (representing 82954 river km) in 2008-2009, and analyzed samples for 50 pers

156 in 48% of the national sampled population of river km, and in 70% of the urban sampled population.

157 ed organic matter (DOM) in five major Arctic rivers (Kolyma, Lena, Yenisei, Ob, Mackenzie) over 3 yea

158 PFAS emissions estimates from wastewater and rivers may provide the best estimate of inputs to the Ar

159 The lost Saraswati River mentioned in the ancient Indian tradition is postu

160 continual water availability in streams and rivers modulating the influence of leaf chemistry on bre

161 s application in the framework of a regional river monitoring network.

162 The top 20 polluting rivers, mostly located in Asia, account for 67% of the g

163 ncreasing iron (Fe) concentrations in boreal river mouths.

164 Suwannee River natural organic matter (SRN) was used as a surroga

165 wannee River fulvic acid (SRFA) and Suwannee River natural organic matter (SRNOM), LDI was found to i

166 surface water and sediment of the Tennessee River near Decatur, Alabama.

167 , and organic matter quality in a freshwater river network.

168 First, we introduce a graph theory model for river networks and explore the properties of the network

169 spatial and environmental characteristics of river networks can be used to study epidemiology and dis

170 reams, where most carbon and nutrients enter river networks, has hindered effective modelling and man

171 gh a graph-theoretic formulation of drainage river networks, we investigate the eigenvalue spectra of

172 ph techniques in characterizing and modeling river networks.

173 to the branching topology of the associated river networks.

174 ment because there has been little change in river nitrogen concentrations.

175 r conditions, a 59% reduction in Mississippi River nitrogen load is required to reduce hypoxic area t

176 hysteresis has been observed between seismic river noise and discharge during storms, suggesting that

177 The Neuse River, North Carolina, U.S., exemplifies a typical de fa

178 eatment plant nutrient fluxes to local urban river nutrient fluxes and trace the impact of the DITP D

179 also suggest a large synergistic effect from river-ocean mixing, global and local atmospheric CO2 upt

180 that was as high as the one explained by the river of origin.

181 e phosphate quality standards in the lowland rivers of Flanders (northern Belgium) are exceeded in ov

182 n rates of CO2 and CH4 in tributaries of the rivers of the plateau were higher than those in the main

183 With one-time sampling from 32 sites in rivers of the plateau, we found that most of the rivers

184 ) and 0.18 mg-N m(2) d(-1), respectively) in rivers of the Tibetan Plateau were found comparable with

185 ents could be used to scale GHGs envision in rivers of the Tibetan Plateau.

186 CH4 and N2O) concentrations and emissions in rivers of the Tibetan Plateau.

187 Peak runoff in streams and rivers of the western United States is strongly influenc

188 e networks-interconnected streams, ponds and rivers-on the Nansen Ice Shelf in Antarctica that export

189 , of a tropical peatland within a network of rivers or canals.

190 Differential use of specific rivers or lakes by acoustic-tagged lake sturgeon further

191 The interfaces between aquifers and rivers or lakes have been identified as biogeochemical h

192 t and coastal plume of a small peat-draining river over a seasonal cycle.

193 ficiency (AE) varied from 28% for the Animas River particles to 45% for the Snake River particles, in

194 Animas River particles to 45% for the Snake River particles, indicating that particle-bound, or sorb

195 uthors performed a secondary analysis of the RIVER-PCI (Ranolazine in Patients with Incomplete Revasc

196 he Ganga Plain (the part of the North Indian River Plain containing the Ganges River).

197 ebris originates from land-based sources and rivers potentially act as a major transport pathway for

198 However, it is unclear whether the same river properties that structure variation on recent time

199 Rivers provide unrivaled opportunity for clean energy vi

200 t of dam-building on the food security these rivers provide.

201 a case study show integrated RTC can improve river quality by over 20% to meet the "good status" requ

202 In tropical rivers, rainfall drives a periodic flood pulse fueling f

203 text] is significantly higher in West Coast river reaches (2.35, n = 96) than in river reaches elsew

204 t Coast river reaches (2.35, n = 96) than in river reaches elsewhere on the continent (1.03, n = 245)

205 The Niagara River receives PPCPs from different wastewater treatment

206 tion of bioavailable DOM was different among rivers reflecting unique characteristics of Arctic river

207 Participants of all ages from Lower River Region (LRR) (N = 1028) and Upper River Region (UR

208 ower River Region (LRR) (N = 1028) and Upper River Region (URR) (N = 840) underwent examination for t

209 The damming of rivers represents one of the most far-reaching human mod

210 Specific behaviours included year-round river residency and multiple lake-migrant behaviours tha

211 River Rhine is a well-known example of this phenomenon b

212 chemical GenX was detected at all downstream river sampling sites with the highest concentration (812

213 Furthermore, river/sea-spiked environmental samples and samples from

214 Autoclaved Elk River sediment slurries sorbed 17.5% of cis-4-MCHM and 3

215 ee climate zones but significantly higher in river sediments than in coasts.

216 in the Hida Mountain Range, and from modern river sediments whose fluvial catchments include these p

217 MPs have been detected in oceans, rivers, sediments, sewages, soil and even table salts.

218 l survey of fish tissue contamination at 540 river sites (representing 82954 river km) in 2008-2009,

219 : see text] emissions varies with stream and river size and shifts from the hyporheic-benthic zone in

220 dges of peat domes where they are bounded by rivers, so that the rate of carbon uptake accompanying t

221 Rivers sourced in the Himalayan mountain range carry som

222 s, and reactive species production, Suwannee River (SRFA) and Pony Lake fulvic acid (PLFA) isolates a

223 d along a longitudinal transect of the South River, starting upstream of the historic Hg contaminatio

224 been well correlated in all the investigated river stretches.

225 along ten 3-km sites within the Upper Neosho River subdrainage, KS, from June-August 2013 yielded thr

226 an Sea, perhaps along courses of now defunct rivers such as Ghaggar, Hakra and Nara.

227 ent was conducted using water from the Fyris River (Sweden).

228 (MeHg) concentration dynamics in the Amazon river system.

229 ing and transport of Hg in this contaminated river system.

230 as developed to identify AMR bacteria in the River Thames.

231 of the changes in the dynamics of the Tiber River that accompanied the construction of Rome's artifi

232 ported an enormous flood in the upper Yellow River that destroyed the Lajia Ruins.

233 e TPS is also the headwater of 9 major Asian rivers that provide fresh water for 1.65 billion people

234 integrated study of PKD in a prealpine Swiss river (the Wigger).

235 d to evaluate riparian conditions of Songhua River, the fifth longest river in China, using physical

236 e obtained for a 90 km stretch of the Simeto River, the main river in Sicily, and the smaller San Leo

237 ions of nitrate transformation in the Yellow River, the second-longest river in China.

238 ough steroid concentrations are low in Swiss rivers, the possibility of additive effects may be of co

239 In large rivers, the ratios of silicon (Si)/nitrogen (N)/phosphor

240 ownings may have played an important role in rivers throughout the world when large migratory herds w

241 of ENSO preconditions the lower Mississippi River to be vulnerable to flooding.

242 is important for forecasting the response of rivers to large influxes of sediment triggered by earthq

243 d biogeochemical and contaminant fluxes from rivers to oceans.

244 5 records of litter breakdown in streams and rivers to quantify its temperature sensitivity, as measu

245 13% of total organic carbon (OC) carried by rivers to the oceans.

246 The 10 top-ranked rivers transport 88-95% of the global load into the sea.

247 ial environment is the primary source of the river-transported microbiota, and that cell export from

248 as derived from eels collected in the Severn River (UK), approximately 50 km upstream of the estuary

249 mplex and the Early Bronze Age from the Lech River valley in southern Bavaria, Germany.

250 ds on the planet, yet coarse gravel in these rivers vanishes within approximately 10-40 kilometres on

251 esicular stomatitis, Rabies, Mokola and Ross River viral envelopes) and self-complementary adeno-asso

252 aviruses, chikungunya virus (CHIKV) and Ross River virus (RRV), and assessed the early antiviral func

253 ith a related arthritogenic alphavirus, Ross River virus, but not in mice infected with West Nile vir

254 at 40 m depth in the aquifer underlying the river was 1.3 +/- 0.8 years, determined by tritium-heliu

255 A 2 m thick layer influenced by river water (upper saturated zone) was not captured by e

256 ses was tested using mixing experiments with river water and artificial seawater.

257 to detect PA in real samples like tap water, river water and matchstick.

258 ed through the determination of DNZ in soil, river water and wastewater samples and satisfactory reco

259 Infiltrating river water becomes anoxic in the uppermost aquifer due

260 ne, while mixtures that mimic wastewater and river water composition affected embryo development and

261 arsenic release from seawater scenarios than river water due to inhibition of oxide dissolution.

262 ctly linked to the switch to corrosive Flint River water from noncorrosive Detroit water from April 2

263 ndicate that it will take several decades of river water infiltration to leach arsenic from the Holoc

264 senic-bearing mineral oxides in both sea and river water inundations, with less arsenic release from

265 ile degradation of chiral fluoxetine (FL) in river water occurs via non-enantioselective photochemica

266 -A concentrations from an external subset of river water samples (r(2) = 0.41; p < 0.0001; n = 75).

267 (NO3(-)) concentrations were analyzed in 651 river water samples collected from 2011 to 2013.

268 (C2nH2F4nSO3) were detected in all collected river water samples, and therefore appear to be ubiquito

269 gh the study of spiked tap, underground, and river water samples.

270 g molecules, and robust operation in natural river water samples.

271 effluents and at part-per-trillion levels in river water samples.

272 s high as 4.0 times that of the seawater and river water system, (2) the power density measured from

273 The treated Flint River water was 8.6 times more corrosive than Detroit wa

274 l as two water matrices (ultrapure water and river water), including a successive water renewal.

275 nd glucocorticoids, in hospital wastewaters, river water, and municipal wastewater treatment plant (W

276 oresis and colorimetric detection of iron in river water, respectively, demonstrating the simplicity

277 ine, which are typical wastewater markers in river water.

278 ct E. coli with a recovery of 81-97% in e.g. river water.

279 le analysis of Hg(2+) in fish, tap water and river water.

280 upper saturated zone due to the influence of river water.

281 Fe speciation of river waters and salinity-induced aggregates was determi

282 arsenic-contaminated soil exposed to sea and river waters in biogeochemical microcosm reactors across

283 reflecting unique characteristics of Arctic river watersheds.

284 ources, mobility, and transport in the South River, we analyzed total Hg (THg) concentrations and Hg

285 arge data for continuously gaged streams and rivers, we quantified streamflow anomalies (i.e., depart

286 rmore, concentrations of GHGs in the studied rivers were related to dissolved carbon and nitrogen, in

287 rs of the plateau, we found that most of the rivers were supersaturated with CO2, CH4 and N2O during

288 in the alluvial plain stretch of the Simeto River, whereas sucralose, sulfamethoxazole and ibuprofen

289 St. Clair) were rarely detected in the other river, which confirmed that lake sturgeon in the Detroit

290 of antidepressants in fish from the Niagara River, which connects two of the North American Great la

291 iver in Sicily, and the smaller San Leonardo River, which was investigated for a 17 km stretch.

292 the southern belt and along the Mississippi River, while liver cancer was high along the Texas-Mexic

293 we examine these connections in a laboratory river with bimodal sediment size, by tracking the motion

294 This relationship is nonlinear where large rivers with population-rich catchments delivering a disp

295 l lineages are separated by the St. Lawrence River, with a more recent divergence of populations isol

296 6, ACF n = 22) were most prevalent in upland rivers, with flow dependency, greater age and length at

297 n the area encompassed by, and the number of rivers, within a paleodrainage.

298 ormula: see text] emissions from streams and rivers worldwide of different sizes, morphology, land co

299 haoniu River Constructed Wetland; XR: Xinxue River; XRCW: Xinxue River Constructed Wetland).

300 samples from the four wetlands (ZR: Zhaoniu River; ZRCW: Zhaoniu River Constructed Wetland; XR: Xinx