ライフサイエンスコーパス: river

1 ter of restored floodplains along a mid-size river.

2 duction in BC concentrations to the Colorado River.

3 via greater carbon evasion from streams and rivers.

4 ates sulfate that is carried to the ocean by rivers.

5 fate of 216 P. unifilis nests along 88 km of rivers.

6 odplain systems and light-limited whitewater rivers.

7 may impact the chemical pollution burden in rivers.

8 ogical Survey streamgage sites in freshwater rivers.

9 from inland waters to coastal systems making rivers a critical link between terrestrial and ocean car

10 sonal patterns of Al and their drivers in 16 rivers across Nova Scotia, Canada.

11 The Lower Mississippi River Alluvial Valley (LMRAV) is an important economic r

12 s that were analyzed in 3741 samples from 18 river and creek catchments between 2011 and 2016.

13 typical seasonal lake linked to the Yangtze River and is significantly affected by water level fluct

14 We found high, but relatively stable Maumee River and lake concentrations of total P (TP) and solubl

15 % were obtained when the platforms in spiked river and tap water, respectively, were evaluated.

16 of the eastern part, delimited by the Tiber River and the Apennine Mountains, manifest a peculiar mi

17 llei across countries bordered by the Mekong River and the Malay Peninsula.

18 7.1% to 106.5% in the analysis of two spiked river and two lake waters.

19 Ancestral Astyanax are found in surface rivers and derived blind forms are found in cave systems

20 (temporary, shallow wetlands) and perennial rivers and in recently vaccinated animals.

21 valent freshwater volume stored in lakes and rivers and is universally accessible without pipelines o

22 ll agricultural streams that drain to larger rivers and lakes, despite best management practices inte

23 stently to natural features such as streams, rivers and lakeshores.

24 In addition, lakes connected to rivers and streams will also experience flushing due to

25 results indicate that the removal of dams on rivers and their connected reservoirs applies predominan

26 sses the complex problem of removing dams on rivers and their connected reservoirs.

27 One that lives in Mexican rivers and various convergent forms that live in nearby

28 and in three different water matrixes (tap, river, and groundwater), and thereby validated for repea

29 U.S. Department of Energy Hanford, Savannah River, and other sites.

30 se nitrate delivery to the main stem Yenisei River, and ultimately the Arctic Ocean, in the coming de

31 d the spawning migration as adults return to rivers, and the overall abundance and distribution of se

32 osaic ecosystem populated by groundwater-fed rivers, aquatic plants, angiosperm shrublands, and edibl

33 Knickpoints in rivers are created by external factors, such as tectonic

34 in North America, and the La Plata and Nile Rivers are found to contribute extensively to virtual wa

35 Relatively unfragmented rivers are still found in the Balkans, the Baltic states

36 roplatidae: Keroplatinae), which occur along river banks in the Appalachian Mountains in Eastern Unit

37 intrusion of dikes and sills of the Columbia River Basalt Province.

38 O(2) was injected into several deep Columbia River Basalt zones near Wallula, Washington.

39 ted agriculture in the snow-dependent Yakima River Basin (YRB) in the Pacific Northwest United States

40 arcelona catchment area, including the Besos River basin and the Barcelona coast, and in the Ebro Riv

41 In the lower Mississippi river basin and the Cascades, the fraction can be as lar

42 r resources for the Alabama-Coosa-Tallapoosa River Basin in the southeastern United States.

43 am bromide concentrations in the Monongahela River Basin in the water year (WY) 1998 (during a nation

44 The Amazon river basin receives ~2000 mm of precipitation annually

45 ises the North China Type, the Lower Yangtze River Basin Type, the Southwest Type, the Plateau Type,

46 sses in riparian zones of the Lower Savannah River Basin, followed by cultivated crops and pasture/ha

47 Across the Upper Missouri River Basin, the recent drought of 2000 to 2010, known a

48 Per river basin, we quantified a connectivity index (CI) for

49 sions from O&G facilities in the Upper Green River Basin, Wyoming.

50 m 33 mesocosm experiments with those from 14 river basins and 22 cross-basin studies in Europe, produ

51 characteristics controls the transition from rivers being 'sinks' to 'sources' of microplastics under

52 atives of which are used in the treatment of river blindness and other parasitic diseases.

53 ciasis, a macroparasitic disease that causes river blindness in Western Uganda and other regions of A

54 ood fluoroethers released into the Cape Fear River by a fluorochemical manufacturing facility were de

55 epeated landslides dammed the Yigong Tsangpo River ca. 3500 BC, 1300 BC, 1000 BC, 600 BC, and twice m

56 lmon (Oncorhynchus tshawytscha) from the Eel River, California, USA.

57 nal abandonment and an investigation of Arys river channel dynamics.

58 a and Syr Darya, were the center of advanced river civilizations, and a principal hub of the Silk Roa

59 In Europe, attempts to quantify river connectivity have been hampered by the absence of

60 Overall abundances confirm how rivers contain a significant number of plastic particles

61 , samples from along straight courses of the river contained fewer microplastics than samples from in

62 The river continuum concept (RCC) has been historically used

63 e fate and quality of organic matter along a river continuum.

64 es in flood properties is the variability of river conveyance capacity.

65 nt connectivity, and explicit estimations of river conveyance properties.

66 flood changes to longitudinal variability in river conveyance, precipitation climatology, flows and s

67 dritic spatial configuration correlated with river corridor networks and mean July temperature.

68 ater is routed through drainage networks and river corridors serve as year-round transmission foci.

69 atic(5) and socio-economic(6-8) functions of river corridors.

70 hat a large fraction of the carbon export to rivers could have been mineralized in inland waters.

71 Abrupt changes in river course, called avulsions, naturally nourish sinkin

72 (RCP4.5) will result in ~80% of the dryland rivers crossing a threshold from one type to another, ma

73 deltas to mega-deltas, has been affected by river damming and deforestation.

74 Not all deltas lose land in response to river damming: deltas transitioning towards tide dominan

75 ities following the development of the Pearl River Delta (PRD) megacity, China.

76 saline-alkali reclamation area of the Yellow River Delta (YRD), China.

77 Since the 1990s the Mekong River delta has suffered a large decline in sediment sup

78 bs, including the Yangtze River Delta, Pearl River Delta, and North China Plain.

79 ey manufacturing hubs, including the Yangtze River Delta, Pearl River Delta, and North China Plain.

80 sin and the Barcelona coast, and in the Ebro River Delta, using single particle inductively coupled p

81 River deltas are frequently facing salinity intrusion, t

82 et, we show that 339 million people lived on river deltas in 2017 and 89% of those people live in the

83 River deltas rank among the most economically and ecolog

84 hat will disproportionately impact people on river deltas, particularly in developing and least-devel

85 orm packages which together demonstrate that river deposition was already well established >3.7 Ga.

86 RIC simulation results, in order to estimate river depth in wet nodes.

87 , was used to train two ML models to predict river depth over the domain for an arbitrary discharge.

88 hemicals which were relatively stable in the rivers, DGT and grab sampling were in good agreement.

89 tors (BCFs) are used together with the daily river dilution patterns to predict internal concentratio

90 ads to enhanced seasonalities in both Amazon river discharge and APR ocean salinity.

91 The short-term impacts of extreme river discharge from Hurricane Florence were particularl

92 anges such as climate warming and increasing river discharge might increase CH(4) emissions and hence

93 en concentration, an indication of increased river discharge, explained the second-most variation in

94 relationship between seasonality, ENSO, and river discharge, with significantly higher values occurr

95 ume and receives more than 10% of the global river discharge.

96 flows of a freshwater apex predator, Ganges River dolphin (GRD, Platanista gangetica gangetica), whi

97 the ecology of a small cetacean, the Ganges River dolphin (Platanista gangetica gangetica, GRD), in

98 nce of natural organic matter (NOM; Suwannee River DOM) and 15 LMM thiols, an internally consistent t

99 chlidae: Cichlinae) restricted to only a few river drainages in the Caribbean-slope of Honduras.

100 ants mainly showed encamped movements at the river during the dry season, when temporary water source

101 uits and normal faults, and to recharge from rivers during sea level lowstands.

102 matic cases will see currently through-going rivers (e.g. Murrumbidgee, Macintyre) experience step ch

103 le combination of selected habitat features (river, elephant corridor, agricultural field, trees), an

104 Solving river engineering problems typically requires river flow

105 One of the most dramatic events in river environments is the natural diversion, or avulsion

106 When comparing data across river-estuarine or similar transects salinity should be

107 tts Bay, Narragansett Bay, and the Cape Fear River Estuary (CFRE), United States.

108 nkton community composition within the Neuse River Estuary (NRE), North Carolina.

109 ent caused the dramatic decline of the Pearl River estuary coral communities reported from 1980 to 20

110 Yangshan Deep-Water Harbour near the Yangtze River estuary in China and identified more than 4,500 di

111 ncentration, consistent with the rapid Pearl River estuary urbanization as the main cause for this eu

112 sources during the early phase of the Pearl River estuary urbanization.

113 esources through a case study in the Yangtze River estuary.

114 urce of sedimentary organic matter along the river-estuary-ocean continuum.

115 in association with landfalling atmospheric river events.

116 e high emissions scenario, fish in the Yukon River exceed EPA guidelines by 2050.

117 We estimate that rivers export 18 +/- 4 Tg DBC year(-1) globally and that

118 While rivers export ~1% of the OC sequestered by terrestrial v

119 We determine that the six major Arctic rivers exported an average of 20 000 kg y(-1) of total H

120 sity and augmenting fisheries as the world's rivers face unprecedented pressures(10,11).

121 fossils found in marginal-marine, storm- and river-flood deposits from the Middle Devonian Naranco Fo

122 an in oligotrophic blackwater and clearwater river-floodplain systems and light-limited whitewater ri

123 e is altering the frequency and magnitude of river floods in an unprecedented way(1).

124 linked increasing forest cover with reduced river flow and potentially detrimental effects downstrea

125 uld take into account that changes to annual river flow are likely to persist for up to five decades.

126 iver engineering problems typically requires river flow characterization, including the prediction of

127 jority of catchments demonstrated persistent river flow declines after forest establishment.

128 The impact of forests on river flow is sensitive to annual precipitation and pote

129 Forests affect river flow less when annual precipitation is low, and se

130 egies and environmental scenarios (rainfall, river flow rate, and water quality).

131 Partial river flow recovery (towards non-forested conditions) ha

132 Previous reviews have investigated trends in river flow response over time, but the influence of fore

133 Here, we evaluate river flow trends in 43 studies following forest establi

134 ton (PEUK) during spring and after spikes in river flow were also detected, making PEUK periodically

135 Altered river flows and fragmented habitats often simplify river

136 Exceptionally low river flows are predicted to become more frequent and mo

137 itated by wet climatic conditions and higher river flows that favored floodwater farming.

138 Moreover, modeling two- or three-dimensional river flows with high-resolution topographic data for la

139 ean flow conditions in the lower Monongahela River for the WYs of interest, the median-estimated wet

140 Anthropogenic modifications to river form and function are likely responsible for the v

141 ges, (b) investigated the combined impact of river fragmentation and climate change and (c) tested th

142 River fragmentation by dams, presenting physical barrier

143 River fragmentation is predicted to act jointly with cli

144 in a freshwater food web from the urban Orge River, France.

145 tion annually and contributes ~17% of global river freshwater input to the oceans; its hydroclimatic

146 investigate the impact of Cl(-) and Suwannee River fulvic acid (SRFA) on Cu(II) reduction and Cu(I) o

147 he Carpathian Mountains and along the Danube River, further confirming these regions as hot spots for

148 ial) would allow similar analyses of dryland rivers globally where hydroclimate is an important drive

149 imate change could affect larval survival in rivers, growth and maturation in lakes, phenology and th

150 Our results indicate that management of river habitats for dragonfly conservation should incorpo

151 ut can rival monsoon-fed discharges in major rivers hundreds to thousands of kilometers downstream.

152 roups were considered simultaneously, run-of-river hydro had moderate overlap (0.56), while shale gas

153 eneration from renewable (wind farms, run-of-river hydro) and non-renewable (shale gas) sources in Br

154 tributary flows as well as changes to pH and river hydrology and hydrogeomorphology.

155 0-2100: compared with 2009-2029, the average river ice duration declines by 16.7 days under Represent

156 rical change and predicted future changes in river ice extent and duration have not yet been quantifi

157 Although river ice extent has been shown to be declining in many

158 To project future changes in river ice extent, we developed an observationally calibr

159 ervations, we show that the global extent of river ice is declining, and we project a mean decrease i

160 Our results show that, globally, river ice is measurably declining and will continue to d

161 Previous studies of river ice, which suggested that declines in extent and d

162 e Hells Canyon Complex (HCC) along the Snake River (Idaho-Oregon border, U.S.A.) encompasses three su

163 music festival held adjacent to the Traisen River in Austria increased the river's dissolved organic

164 The lower Brahmaputra River in Bangladesh and Northeast India often floods dur

165 Sediments of the Passaic River in New Jersey are contaminated by these compounds.

166 c sediment from 34 stations along the Thames River in Ontario, Canada, to determine the influence of

167 om the Oyogos Yar coast near the Kondratievo River in the Laptev Sea region, Sakha (Yakutia) Republic

168 ver sites from headwater streams to the main river in the River Thames, UK.

169 ium concentrations in lakes, reservoirs, and rivers in Ohio, USA during the summer of 2017.

170 vated nitrogen concentrations in streams and rivers in the Chesapeake Bay watershed have adversely af

171 Using data obtained from 78 sites across six rivers in the mainland Japan and the Amami-Oshima Island

172 his region inhibited headward propagation of river incision into the Tibetan Plateau.

173 ded Sediment Concentration (SSC) in channels/rivers include costs and technological gaps but this pap

174 00, simulated Hg concentrations in the Yukon River increase by 14% for the low emissions scenario, bu

175 ng 2,715 kilometres of stream length for 147 rivers indicate that existing records underestimate barr

176 e.g., decreased fluvially transported upland river inputs, and increased tidally induced marine algae

177 The Detroit River is a significant source of total phosphorus to Lak

178 RIVER is the first randomised trial to determine the eff

179 he estimated total mass of Hg transported by rivers is substantially less than the estimated tons of

180 river modeling, where a system of connected rivers is to be simulated simultaneously.

181 predict mean monthly temperature for 465,775 river km in the western U.S., and then applied simple ye

182 Laboratory, Taconic Biosciences, and Charles River Laboratories; and (3) mice subjected to intestinal

183 utrient loads which drive HABs in the Indian River Lagoon and Lake Okeechobee.

184 ntense ecosystem disruptive HABs, the Indian River Lagoon and the St.

185 requently found in the environment including rivers, lakes and soils.

186 Titan has a methane cycle with clouds, rain, rivers, lakes, and seas; it is the only world known to p

187 linked hb locus of a jawless vertebrate, the river lamprey (Lampetra fluviatilis), shares a range of

188 Selection at ar in the effluent-dominated River Lee may have resulted from historical contaminatio

189 Diminished river loads measured upstream from the coast, however, s

190 Our assessment can guide river management at multiple scales and in various domai

191 on nutrient stress, while highlighting that river management requires more bespoke management soluti

192 In this study, we coupled a simple river model with a first-order toxicokinetic (TK) model

193 h simulations are required for comprehensive river modeling, where a system of connected rivers is to

194 rmine the influence of land use, grain size, river morphology, and relative amount of organic debris

195 In terms of river morphology, samples from along straight courses of

196 negatively correlated with distance from the river mouth and cumulative height of trans-river structu

197 ve height of trans-river structures from the river mouth to each site.

198 storm, with greatest impacts closest to the river mouth.

199 Data shows the sandy coast bounding river mouths accreted consistently at a rate of +2 to +4

200 ms, associated with a range of habitats from river mouths to coral reefs.

201 of past reported values (e.g., for Suwannee River Natural Organic Matter IHSS isolate: 1.8% vs 0.23-

202 dles were found on the shore of the Columbia River near Portland, Oregon.

203 Monitoring of the Colorado River near the Moab, Utah, wastewater treatment plant (W

204 olved organic carbon (DOC) from soils to the river network is an overlooked component of the terrestr

205 global increase in terrestrial DOC inputs to river network of 35 Tg C year(-1) (14%) from 1860 to 201

206 Streams and river networks are increasingly recognized as significan

207 ingly erratic depinning events along smectic river networks correlated over system spanning scales.

208 oral trends in DOC leaching from soil to the river networks from 1860 to 2010.

209 quantified impedance using data on road and river networks, land cover, and topography.

210 s are believed to have been transferred from river networks.

211 adromous species was indirect and related to river-ocean connectivity.

212 lacier (Hunza region), dammed the proglacial river of Muchuhar Glacier, which formed an ice-dammed la

213 tified flow-ecology responses in the Karnali River of Nepal during the low-flow season when habitat w

214 n) within the food web of the Yadkin-Pee Dee River of North Carolina and South Carolina, US.

215 Therefore, it seems the great rivers of Central Asia were not just static "stage sets"

216 iched bacteria from sediments of the Passaic River on two organohalides, trichloroethene (TCE) and 1,

217 ented the importance of tropical mountainous rivers on global silicate weathering and suspended sedim

218 is influenced by Mississippi and Atchafalaya River outflow, remained fairly stable over this time per

219 allenges of monitoring biological threats to rivers over long time periods and across large geographi

220 cs, we identified 17 novel viruses in Clinch River pheasantshells.

221 ations of OPEs in samples from the Mackenzie River plume suggest riverine discharge as an OPE source

222 The concentrations of Ce-NPs in the river ranged from 18.1 x 10(6) to 278 x 10(6) NPs/L, and

223 3.4 +/- 0.2 x 10(-5) mg.mL(-1).min(-1)) and river red gum honeys (E. camaldulensis; 3.2 +/- 0.2 x 10

224 n lime concretion black soils along the Huai River region of China.

225 nificant environmental changes in the Yellow River region.

226 x and composition of carbon (C) from land to rivers represents a critical component of the global C c

227 ensity are agricultural pressure, density of river-road crossings, extent of surface water and elevat

228 scopy structures of Fab in complex with Ross River (RRV), Mayaro, or chikungunya viruses reveal a con

229 /16, indicating drought conditions with less river runoff, rainfall and higher ocean salinities.

230 o the Traisen River in Austria increased the river's dissolved organic carbon (DOC) concentration fro

231 Sediment from one river sampled downstream from the WWTP showed the fastes

232 , with ARGs unique to WWTP and WWTP-impacted river samples predominantly belonging to the aminoglycos

233 Mitigation strategies, together with river sanctuary and distanced-based approaches, should b

234 lonan coast were significantly attenuated by river-sea environmental dilution.

235 tles inoculated with the original, unamended river sediment.

236 ources downstream of dams compensate for the river-sediment lost to impoundments.

237 River segment and substrate type were the most important

238 NOM-amended soil collected from the Savannah River Site (SRS) or unamended vadose zone soil and expos

239 egacy defense nuclear tank waste at Savannah River Site is highly desirable for the purpose of nuclea

240 This was conducted at 12 river sites from headwater streams to the main river in

241 (GLM) and the associated Saint John/Wolastoq River (SJWR), we studied the spatial (i.e., across the m

242 lakes and estuaries along the Chattahoochee River (Southeastern USA).

243 to 2050, which highlights the importance of river-specific strategies for waterway exploitation worl

244 f HCV among prison inmates in Calabar, Cross River State, Nigeria and the associated factors.

245 the contiguous region of Bayelsa, Delta, and Rivers states, or another more restricted, yet unidentif

246 pulations of roach (Rutilus rutilus) inhabit river stretches polluted with estrogenic WwTW effluents.

247 e river mouth and cumulative height of trans-river structures from the river mouth to each site.

248 Expanding our approach to include other river styles (e.g. mixed bedrock-alluvial) would allow s

249 d North Sea region encompasses catchments of rivers such as Scheldt and Meuse.

250 Rivers support some of Earth's richest biodiversity(1) a

251 ions into groundwater reaching the Athabasca River system adjacent to the reclaimed pond at Tar Islan

252 uring the rapid expansion of agriculture and river system modification associated with European colon

253 anista gangetica gangetica, GRD), in a large river system of Nepal.

254 ne boundary, probably via a continuous paleo-river system or along the Tethys coastal line, which are

255 s in an anthropogenically altered California river system.

256 control the distribution of microplastics in river systems.

257 importance of connectivity within dendritic river systems.

258 by microplastics retained within the world's river systems.

259 er quality of one of Europe's most important river systems.

260 nd monitor ECs at the catchment scale in the River Thames system (U.K.) and explored their sources an

261 m headwater streams to the main river in the River Thames, UK.

262 ter in major (sub)tropical and high-latitude rivers than in major temperate rivers, with further sign

263 one-third of Earth's landmass is drained by rivers that seasonally freeze over.

264 chment characteristics for up to 1406 larger rivers that were analysed between 1990 and 2016.

265 Aral Sea basin in Central Asia and its major rivers, the Amu Darya and Syr Darya, were the center of

266 For rivers, the effects of nutrient enrichment were dependen

267 program that focused on the six major Arctic rivers to establish a contemporary (2012-2017) benchmark

268 ole of land cover change and soil erosion on river transport of Hg in a heavily ASGM-impacted watersh

269 o Basin, an expansive network of streams and rivers transport and cycle terrigenous C sourced from th

270 aration of five specific dominantly alluvial river types and quantification of their present-day catc

271 -replacement, at 11 sites along the Colorado River upstream and downstream of the WWTP and analyzed f

272 ears, at the site of Dhaba in the Middle Son River Valley of Central India.

273 icrobial prevalence less well in adults from river villages with more regular access to markets.

274 these declines, we studied mussels in Clinch River, Virginia and Tennessee, USA, where the endemic an

275 iruses, including chikungunya virus and Ross River virus.

276 east by 500 thousand years ago (ka) the Solo River was diverted into the Kendeng Hills, and that it f

277 6) to 45.1 x 10(6) Ag-NPs/L) in the analyzed rivers was limited to certain hotspots close to wastewat

278 -2) with 2.0 M NaCl as the draw solution and river water (0.017 M) as the feed water at an applied hy

279 such as groundwater, bottled mineral water, river water and borehole water and food samples.

280 harvesting the "blue" osmotic energy between river water and sea water.

281 f 107 +/- 10% and 96 +/- 8% were obtained in river water for 3 and 5 muM of atrazine, respectively.

282 almost the same sensitivity in the simulated river water samples as in phosphate buffer, reflecting i

283 soil in an infiltration pond recharged with river water using a set of in situ sensors measuring eve

284 ses of collected water samples (groundwater, river water, and seawater) demonstrated the applicabilit

285 Sources included river water, groundwater, and an upland reservoir.

286 outdoor air particulates, sea sediment, and river water.

287 advantage of El Nino floodwaters as well as river water.

288 lastics of up to 1 mum in drinking, tap, and river water.

289 he detection of photosynthetic herbicides in river water.

290 lds in the U.S. and especially in the Maumee River Watershed (MRW).

291 ere, we studied DOM dynamics in the Altamaha River watershed in Georgia, USA, a fluvial system where

292 In the Colorado River watershed in Madre de Dios, Peru, mining and defor

293 ibited exploratory movements to and from the river, while females showed an increase in the frequency

294 g downstream through a mesh enclosure in the river with and without predator cues present to measure

295 f the vertebrate immune system, by comparing river with cave morphotypes.

296 e to changes in the dilution capacity of the river with elevated concentrations under lower flows in

297 e first time the geomorphology of 29 dryland rivers with catchments across a humid to arid gradient c

298 omparing the eroded organic carbon export to rivers with the particulate organic carbon export to oce

299 high-latitude rivers than in major temperate rivers, with further significant differences between bio

300 Johns River within Jacksonville, FL.