ライフサイエンスコーパス: runoff

1 er losses (evapotranspiration, drainage, and runoff).

2 condary wastewater effluent and agricultural runoff).

3 able water reuse projects or in agricultural runoff).

4 low that are diluted by rainfall and surface runoff.

5 (SM) in soil in relation to its transport in runoff.

6 major ion and Hg concentrations in 2008 melt runoff.

7 through wastewater effluent and agricultural runoff.

8 lids, are carried to the ocean by freshwater runoff.

9 , inland seas and shelf waters influenced by runoff.

10 he pond outflow water than in the stormwater runoff.

11 e, predominantly through increased meltwater runoff.

12 le for the release of metals during rainfall runoff.

13 in lake water and contaminated agricultural runoff.

14 ng bare-ice exposure and enhancing meltwater runoff.

15 increases in concentrations during rainfall runoff.

16 atment plant effluent and agricultural field runoff.

17 ansformations of N in residential stormwater runoff.

18 obiological contamination load in stormwater runoff.

19 d for microbial load reduction in stormwater runoff.

20 types of bacteria in agricultural subsurface runoff.

21 orage in glacier ice and removal by particle runoff.

22 discharges and agricultural nonpoint source runoff.

23 educing N loading associated with stormwater runoff.

24 arbon and iron in Greenland Ice Sheet (GrIS) runoff.

25 l profile could remobilize this stored Hg in runoff.

26 orb rainfall and thereby diminish stormwater runoff.

27 ich represented 84.4% of the total Cu in the runoff.

28 recipients by up to 40% at otherwise similar runoff.

29 ncipal receiving water body for Austin urban runoff.

30 rganisms in a wetland receiving contaminated runoff.

31 ean due to the effect of sea ice melt and/or runoff.

32 ater bodies receiving agricultural and urban runoff.

33 nductivity generally diluted with increasing runoff.

34 L required more rainfall to generate surface runoff.

35 control pollution from agriculture and urban runoff.

36 ts between river flow and pH due to peatland runoff.

37 ts from the ice/snow layer melting and river runoff.

38 to a more humid climate and elevated fluvial runoff.

39 e, changes in regional climate, and nutrient runoff.

40 ore water and less rainfall feeds subsurface runoff.

41 rom urban input, sewage waste and irrigation runoff.

42 asingly being applied to remove nitrate from runoff.

43 ear(-1) influent load between three sources: runoff (12%), groundwater infiltration (39%), and sewage

44 71%), volatilization (5%), leaching (8%) and runoff (3%), while 13% of SM persisted in topsoil.

45 r to pond on the surface (-40%) and commence runoff (-33%), and reduced infiltration (-34%) and sedim

46 ese can absorb surface meltwater and inhibit runoff(4), but this buffering effect is limited if enoug

47 Agricultural runoff accounted for 23% of total metal stream loads fro

48 soil and poultry litter leachates and street runoff, accounted for the remaining 30%.

49 nd the ocean-atmospheric forcings of surface runoff across the southern Andes.

50 ean, was responsible for a poleward shift of runoff, albedo and surface temperature records over the

51 watersheds with the highest levels of oocyst runoff align closely with regions of increased sentinel

52 treatment of these pesticides in stormwater runoff, an approach combining field sampling and watersh

53 was similar in both years (36% in 2008 melt runoff and 34% in 2009), it is possible that record low

54 antify the link between terrestrial sediment runoff and a downstream coastal marine ecosystem and con

55 tensity are increasing with greater nutrient runoff and a warming climate.

56 heet through its impact on radiative budget, runoff and accumulation.

57 th infectious stages traveling in freshwater runoff and being concentrated in particular locations by

58 biomass-water feedback associated with water runoff and biomass-dependent infiltration rates.

59 Measurements of DOC concentrations in soil, runoff and drainage are scarce and their spatial distrib

60 ther, but the water loss from the system via runoff and drainage increased substantially, leading to

61 raphy through interactions between rainfall, runoff and erosion in drainage basins(1-4).

62 towards very different partitioning between runoff and evapotranspiration.

63 ia were released, they were partitioned into runoff and leachate at similar concentrations, but in di

64 CT systems via two major transport pathways: runoff and leaching.

65 ice mass loss and the associated freshwater runoff and lengthening of open-water periods.

66 etan Plateau for glacier mass balance, river runoff and local ecology, changes in these quantities re

67 late and dissolved organic carbon in glacial runoff and near surface coastal waters was aged (12100-1

68 r composition of DON in the urban stormwater runoff and outflow water from an urban stormwater retent

69 flow water, which were only 13% different in runoff and outflow water.

70 c factors, such as nonpoint sources of paved runoff and point sources of sanitary sewage within the d

71 identified with FT-ICR-MS in the stormwater runoff and pond outflow water, which were only 13% diffe

72 ino sugars, lignins, and tannins in DON from runoff and pond outflow water.

73 on the anthropogenic influences of the paved runoff and sanitary sewage on the DOM quality of WWF usi

74 tures above 0 degrees C per year, freshwater runoff and sea ice in the 1980s) rather than by local ch

75 by human activity, but increased freshwater runoff and sediment fluxes may increase the size of the

76 on the transport of antibiotics and ARGs in runoff and soil following land application of swine manu

77 ospective analysis of representative roadway runoff and stormwater-affected creeks of the U.S. West C

78 the dominant NO3-N sources in the stormwater runoff and that there was a continuum of source changes

79 examine the spatial distribution of parasite runoff and the impacts of precipitation and development

80 gh-resolution geochemical records of surface runoff and vegetation from sediment cores from Lake Towu

81 Nanoplastic debris, resulted from runoff and weathering breakdown of macro- and microplast

82 at reducing nutrient pollution, agricultural runoffs and maintaining riparian vegetation can mitigate

83 precipitation minus total sublimation minus runoff) and a dynamic term.

84 er flow into soil, and the rate or volume of runoff) and two hydrological outcomes (moisture storage,

85 uts throughout the year except during spring runoff, and also during autumn storms in the catchment w

86 an increase in mean seasonal precipitation, runoff, and streamflow.

87 hat DOM pools in supraglacial and subglacial runoff are compositionally diverse and that N-rich mater

88 ned sewer systems when sewage and stormwater runoff are released into water bodies, potentially conta

89 y contaminated baseflow and rainfall/surface runoff, are observed in the Little Rouge Creek throughou

90 ave expanded the Greenland ice sheet's total runoff area by 26 +/- 3 per cent since 2001.

91 ve previously focused on effluent or surface runoff as the primary route of transport from animal fee

92 old-like relationship between FL and surface runoff as well as the influence of plant cover on hydrol

93 ectiveness of soil bioretention for treating runoff, as measured by prevention of both visible cardia

94 r bacteria (FIB, a pollutant responsible for runoff-associated inland and coastal beach closures) in

95 ) s(-1)), limiting dilution of FIB and other runoff-associated pollutants once they enter the bay; (4

96 rations of either total or methyl-mercury in runoff, but export increased by 50-70% in one of the har

97 originates from landscapes draining glacier runoff, but the influence of the influx of riverine orga

98 d increased sediment, nutrient, and chemical runoff, but these forces may also enhance pathogen runof

99 Here we show that clouds enhance meltwater runoff by about one-third relative to clear skies, using

100 he capture, treatment, and recharge of urban runoff can augment water supplies for water-scarce citie

101 We first document how road salt runoff can elevate sodium concentrations in the tissue o

102 nce they enter the bay; (4) once in the bay, runoff can form buoyant plumes that further limit vertic

103 lected milkweed, we then show that road salt runoff can result in increased muscle mass (in males) an

104 reasing urbanization and associated chloride runoff can salinize freshwaters and threaten lake water

105 ffectively managing water quantity; however, runoff carries pollutants, posing risks to the local env

106 The results showed that the surface runoff coefficient was strongly and positively linearly

107 e; with UVR exposure, mortality was 100% for runoff collected across the entire sampling period.

108 We investigated acute toxicity of simulated runoff collected from 5 h to 111 days after application

109 Irrigation runoff concentrations of 17alpha-trenbolone (17alpha-TBO

110 both snowmelt seasons, but major ion and Hg runoff concentrations were roughly 50% higher in 2008 th

111 ays: P was exported primarily via stormwater runoff, contributing to surface water degradation, where

112 o a lesser degree agricultural or stormwater runoff, could be important where they affect a major fra

113 le for temporal bone CT (-56.1%), peripheral runoff CT angiography (-48.6%), CT of the paranasal sinu

114 Interpretation and use of copper runoff data for environmental risk assessment and manage

115 typhoon tracks with landscape topography and runoff data to estimate the water inflow into a reservoi

116 ts such as storm events and surface snowmelt runoff destabilize smaller hot spring environments with

117 -forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes.

118 d water quality: (1) in the upper watershed, runoff diluted most dissolved constituents, (2) in the u

119 experiments were conducted utilizing actual runoff, DOC from straw and compost, and a suite of TOrCs

120 hat future warming may lead to less nutrient runoff due to increased evapotranspiration and decreased

121 n "ionic pulse" of mercury and major ions in runoff during both snowmelt seasons, but major ion and H

122 teria; (2) small drains can trap dry weather runoff during high tide, and then release it in a bolus

123 est was demonstrated analyzing the clomazone runoff during the rice growing season in northern Urugua

124 gical floods need to account for the extreme runoffs during lake outbursts, given the increasing tren

125 that contaminants in the dissolved phase of runoff (e.g., PAHs) are cardiotoxic and that soil bioret

126 hydrological processes (times to ponding and runoff, early [sorptivity] and final [infiltration] stag

127 n factors for groundwater (EF5g) and surface runoff (EF5r) were calculated for both field drain and s

128 the severity of drought events by decreasing runoff efficiency in the basin since the late 20th centu

129 t minimize the volume of dry and wet weather runoff entering the local storm drain system may be the

130 number accounting for diffusive soil creep, runoff erosion, and tectonic uplift, is reminiscent of t

131 were found at greater concentrations during runoff-event conditions.

132 rganic chemicals in urban stormwater from 50 runoff events at 21 sites across the United States demon

133 with storms can affect lakes via short-term runoff events from watersheds and physical mixing of the

134 n for potential environmental effects during runoff events.

135 iment prey and is temporally associated with runoff events.

136 orted 2/3 of their annual water yield during runoff events.

137 il-atmosphere water fluxes, and thus surface runoff flux, during repeated, climate-driven, vegetation

138 urs both through WWTP effluent discharge and runoff following land applications of biosolids.

139 the laboratory to undiluted and 1:10 diluted runoff for 48 h, then transferred to control water and e

140 small earthen dams, meant to capture surface runoff for livestock watering, were a major component of

141 rements of iron concentrations in subglacial runoff from a large Greenland Ice Sheet catchment reveal

142 lecules in supraglacial water and subglacial runoff from a large GrIS outlet glacier.

143 vior of Cu in a stormwater wetland receiving runoff from a vineyard catchment (Alsace, France).

144 ssions associated with nitrogen leaching and runoff from agriculture for both the UK and globally.

145 the potential to transform urban stormwater runoff from an environmental threat to a valuable water

146 e of prairie strips also reduced total water runoff from catchments by 37%, resulting in retention of

147 Runoff from coal-tar-based (CT) sealcoated pavement is a

148 By preventing the rooftop runoff from entering the wastewater treatment plant, bet

149 Runoff from farms and output from wastewater treatment p

150 Runoff from glaciers and ice sheets has been acknowledge

151 However, the influence of refreezing on runoff from Greenland remains largely unquantified.

152 pectively-approximately double the estimated runoff from Greenland's high-elevation interior, as pred

153 Ubiquitous examples of toxics in runoff from highways and other impervious surfaces inclu

154 lement mobilization and export in subglacial runoff from ice sheets is poorly constrained at present.

155 Pesticide runoff from impervious surfaces is a significant cause o

156 of hydraulic flood control structures, local runoff from industrialized areas, and active superfund s

157 the Java Sea through local precipitation and runoff from Kalimantan, Indonesia.

158 t determine the environmental fate of copper runoff from outdoor surfaces.

159 nters of 2016-2017 and 2017-2018, stormwater runoff from residential areas was monitored in paired ci

160 We assessed the impacts of stormwater runoff from sealcoated asphalt on juvenile coho salmon (

161 alcoat to conventional asphalt and collected runoff from simulated rainfall events up to 7 months pos

162 ely) are therefore likely to be delivered by runoff from the Antarctic continent.

163 om lacustrine organic production and surface runoff from the catchment accumulated in the lake.

164 a progradation was driven by high freshwater runoff from the Greenland Ice Sheet coinciding with peri

165 n at the ice surface and enhancing meltwater runoff from the largest cryospheric contributor to conte

166 rther, the NO3-N transport in the stormwater runoff from the residential catchment was driven by mixi

167 Although runoff from the top of ice slabs has added less than one

168 Here we show that surface runoff from three island groups of the maritime Antarcti

169 Mortality following exposure to undiluted runoff from unsealed asphalt pavement and UVR was </=10%

170 s and increase precipitation and terrestrial runoff, further increasing organic matter and nutrient i

171 ment load reaching the delta is delivered by runoff generated by rainfall associated with tropical cy

172 connectivity could explain the mechanism of runoff generation in semi-arid areas while further exper

173 be used to improve numerical simulations of runoff generation, stream water transit time and evapora

174 se estimated from observed precipitation and runoff generation.

175 0 m that is disproportionately important for runoff generation.

176 versely affect water quality through surface runoff, groundwater discharge, and damage to municipal w

177 In recent decades, meltwater runoff has accelerated to become the dominant mechanism

178 Atmospheric deposition and riverine runoff have been traditionally considered the main exter

179 nges in sodium availability due to road salt runoff have significant effects on the development of so

180 of how climate-driven changes in freshwater runoff have the potential to alter food web dynamics wit

181 mately, an increase in snowpack and snowmelt runoff Hg concentrations.

182 The main drivers of Greenland ice sheet runoff, however, remain poorly understood.

183 ng pesticide exposure following agricultural runoff (i.e., pulse disturbance).

184 8% of snowpack Hg was exported with snowmelt runoff in 2008 and 41% in 2009.

185 average, which results, in part, from higher runoff in glaciated catchments.

186 Peak runoff in streams and rivers of the western United State

187 From mid-May to August 2011, extreme runoff in the Columbia River ranged from 14,000 to over

188 ned atmospheric conditions promoted enhanced runoff, increased the surface temperatures and decreased

189 Consequently, GICs runoff increases 65% faster than meltwater production, t

190 In the dry season, runoff increases over most monsoon regions, due to stoma

191 Comparably, runoff indexed hazards simulated by the Variable Infiltr

192 re of Hg transported away from the mine with runoff into the creek, eventually affecting ecosystems d

193 Transported via surface and subsurface runoff into wetlands, their ultimate aquatic fate remain

194 e to their propensity to be transported with runoff, IPAs likely end up in surface waters where they

195 of bioavailable iron associated with glacial runoff is 0.40-2.54 Tg per year in Greenland and 0.06-0.

196 Urban stormwater runoff is a globally significant threat to the ecologica

197 Precipitation induced runoff is an important pathway for agrichemicals to ente

198 We found that runoff is highly sensitive to vegetation migration; warm

199 lting, suggests that their export in glacial runoff is likely to be important for biological producti

200 In the Juncal catchment in Chile, runoff is likely to sharply decrease in the future and t

201 Significant runoff is observed during the second half of the Medieva

202 aracteristics of monsoonal precipitation and runoff is poorly understood.

203 Glacial runoff is predicted to increase in many parts of the Arc

204 We suggest that enhanced ice sheet runoff is primarily associated with albedo effects due t

205 ered to local rivers, DSi in groundwater and runoff is redirected to the combined stormwater-sewage o

206 ons related to the impact of these impulsive runoffs is "are flash floods more efficient in deliverin

207 rainfall simulator induced 1 h of release in runoff/leachate partitioning boxes at three rainfall int

208 are transported through the environment via runoff, leaching, and land application of manure; howeve

209 Excessive nitrogen runoff leads to degraded water quality, harming human an

210 Total N and P runoff losses were up to 39% and 30% lower, respectively

211 at levels above toxicity benchmarks and that runoff may be a major pollutant source to urban surface

212 nt source pollution (NPS) such as stormwater runoff may introduce high loads of bacteria, impairing s

213 nted microcosms and least consistent for raw runoff microcosms.

214 ecipitation volume (mm), daily total surface runoff (mm), surface pressure (mbar), wind speed (m/s),

215 ) in the urban corridor and lower watershed, runoff mobilized soluble constituents accumulated on the

216 distributed hydrologic models (Precipitation-Runoff Modeling System, Variable Infiltration Capacity,

217 to CT, NT resulted in an overall increase of runoff NO3(-) concentration, but similar runoff NO3(-) l

218 of runoff NO3(-) concentration, but similar runoff NO3(-) load.

219 Total dissolved Hg meltwater runoff of 14.3 (+/- 0.7) mg/ha in 2008 and 8.1 (+/- 0.4)

220 ges in landscapes and climate can accelerate runoff of diverse pathogens from terrestrial to aquatic

221 he northern Baltic Sea, leading to a greater runoff of fresh water and terrestrial dissolved organic

222 deposition through rainfall, vegetation and runoff of soils.

223 nd have an important role in determining the runoff of the middle Yellow River.

224 urricanes, coastal development, agricultural runoff, oil spills, and fishing.

225 tal model to assess the effects of untreated runoff on the expression of genes that are classically r

226 long-term ecological effects of agricultural runoff on these populations remains largely unknown.

227 We derive the dependency of wintertime runoff on this warming effect in combination with the ef

228 Detrimental effects of road salt runoff on urban streams are compounded by its facilitate

229 cance for efforts to mitigate the impacts of runoff on water quality.

230 vironments either via spray drift or surface runoff or (due to neonicotinoids' systemic nature) via s

231 In excess (e.g., due to runoff or wastewater discharges), P is also a primary ca

232 riving from aeolian dust deposition, glacial runoff, or river discharges can form an important source

233 Snowmelt, surface runoff, or stormwater releases in urban environments can

234 Runoff over ice slabs is set to contribute 7 to 33 milli

235 ion (p < 0.001; OR = 1.14), and high surface runoff (p < 0.001; OR = 1.37), while low groundwater con

236 in models significantly alters infiltration-runoff partitioning and recharge in wet and vegetated re

237 ock beneath landscapes influences subsurface runoff paths, erosional processes, moisture availability

238 the snowpack through the entire spring melt runoff period for two years.

239 the rainy season in 2012 and 2013 using four runoff plots.

240 ution; and (5) local winds can force buoyant runoff plumes back against the shoreline, where water de

241 Nutrient leaching and runoff pollution can lead to eutrophication and impaired

242 Zn/d) due to diffuse groundwater and surface runoff pollution sources at higher flows.

243 Heavy metals from urban runoff preserved in sedimentary deposits record long-ter

244 of multi-GCM ensemble uncertainty on direct runoff projections for headwater watersheds could be an

245 atersheds with high fertilizer and pesticide runoff promote low levels of growth anomalies, a chronic

246 ndicating drought conditions with less river runoff, rainfall and higher ocean salinities.

247 r had no significant effect on sorptivity or runoff rate/amount, but increased moisture storage (+14%

248 pheric evasion is the main methane sink once runoff reaches the ice margin, with estimated diffusive

249 ds outweighed the weak influence of trees on runoff reduction.

250 hydrological controls that reflect rainfall-runoff regimes in different climate zones.

251 tectable over background freshwater and soil/runoff related signals, even at tens of kilometers downs

252 The results indicate that runoff remains acutely toxic for weeks to months after C

253 ug/AU 17alpha-TBOH) of the dose leached into runoff, respectively.

254 hydrological connectivity structure and the runoff response to rainfall were analyzed.

255 al precipitation not routed to the oceans as runoff returns to the atmosphere as evapotranspiration.

256 eads to an increase in the yield of expected runoff RNA by suppressing the formation of undesired lon

257 complementary to the 3' end of the expected runoff RNA effectively prevents self-primed extension, e

258 cis self-primed extension, in which released runoff RNA folds back on itself to prime its own RNA-tem

259 lengths shorter and longer than the expected runoff RNA.

260 Test organisms exposed to undiluted CT runoff samples collected during the 3 days (C. dubia) or

261 Stormwater runoff samples were collected over 25 stormwater events

262 dwaters, 16 eutrophic waters, 4 agricultural runoff samples, 9 stormwater runoff samples, and 12 muni

263 4 agricultural runoff samples, 9 stormwater runoff samples, and 12 municipal wastewater effluents.

264 ly to sharply decrease in the future and the runoff seasonality is sensitive to projected climatic ch

265 he world, a much larger volume of stormwater runoff should be harvested than infiltrated to maintain

266 owever, Isortoq discharges tended lower than runoff simulations from the Modele Atmospherique Regiona

267 been initiated by North America fresh water runoff that caused a sustained reduction of North Atlant

268 inity due to an arid climate and low fluvial runoff therefore seems to be a prerequisite for the form

269 of DON increased from 10% in the stormwater runoff to 40% in the pond outflow water and DON was less

270 WFs), and relate the GWFs per river basin to runoff to calculate the N-related water pollution level

271 y allow manure-borne antibiotics and ARGs in runoff to reach background levels under the experimental

272 (GS), keeping transpiration (EC) and, hence, runoff unaltered.

273 lations show evidence for enhanced ice sheet runoff under volcanically forced conditions despite atmo

274 r is rainwater insofar as it does not become runoff) used for producing, consuming, exporting, and im

275 variability can predict 20% to 45% of annual runoff variability between 28 degrees and 46 degrees S.

276 The age of aquatic C in runoff varied little throughout the year and appeared to

277 d to them through wastewater and animal farm runoff, very little is known about their effects in the

278 d to road density, the dominant control over runoff volume.

279 ted catchments as a consequence of increased runoff volume.

280 Runoff was collected before entering surface waters and

281 The increase in concentrations with runoff was due to higher levels of particle-associated c

282 Whereas sealcoat runoff was more acutely lethal to salmon, a spectrum of

283 Biodegradation of TOrCs in runoff was more enhanced by compost DOC than straw DOC (

284 The extreme runoff was the direct result of both melting of anomalou

285 make IFGEM suitable for treating stormwater runoff, wastewater effluent, and agricultural discharge

286 ith driving rain, leading to highly polluted runoff water (up to several mg L(-1) biocides) being inf

287 t discharge contributions: MOXA prevailed in runoff water, whereas MESA was associated with slower fl

288 The brine is produced by either rainfall or runoff water.

289 contributed to the lakes enrichment through runoff waters that are more concentrated in solutes or l

290 d chemicals and chemicals typical for street runoff were detected.

291 factors influencing precipitation and river runoff were positively correlated with the growth of juv

292 ever, 17alpha-TBOH concentrations in initial runoff were predicted to exceed threshold levels (i.e.,

293 tively), but dramatically increased parasite runoff when combined (175% average increase).

294 s or sources of N to stormwater depending on runoff, which in turn was inversely related to retention

295 range of potential impacts of trees on urban runoff, which includes deposition of nutrient-rich leaf

296 , but these forces may also enhance pathogen runoff, which threatens human, animal, and ecosystem hea

297 of the initial terbutryn was emitted to the runoff, while 64-80% remained in the coating.

298 he 16S rRNA gene) decreased significantly in runoff with increased setback distance.

299 lpha-TBOH concentrations in rainfall-induced runoff with partial subsequent attenuation.

300 It was hypothesized that (1) DOC-augmented runoff would demonstrate enhanced TOrC biodegradation an