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1 er losses (evapotranspiration, drainage, and runoff).
2 condary wastewater effluent and agricultural runoff).
3 e, predominantly through increased meltwater runoff.
4 le for the release of metals during rainfall runoff.
5  in lake water and contaminated agricultural runoff.
6 ng bare-ice exposure and enhancing meltwater runoff.
7  increases in concentrations during rainfall runoff.
8 rom urban input, sewage waste and irrigation runoff.
9 atment plant effluent and agricultural field runoff.
10 ansformations of N in residential stormwater runoff.
11 asingly being applied to remove nitrate from runoff.
12 obiological contamination load in stormwater runoff.
13 d for microbial load reduction in stormwater runoff.
14 types of bacteria in agricultural subsurface runoff.
15 orage in glacier ice and removal by particle runoff.
16 educing N loading associated with stormwater runoff.
17 arbon and iron in Greenland Ice Sheet (GrIS) runoff.
18 l profile could remobilize this stored Hg in runoff.
19 ich represented 84.4% of the total Cu in the runoff.
20 recipients by up to 40% at otherwise similar runoff.
21 low that are diluted by rainfall and surface runoff.
22 ncipal receiving water body for Austin urban runoff.
23 rganisms in a wetland receiving contaminated runoff.
24 ean due to the effect of sea ice melt and/or runoff.
25 ater bodies receiving agricultural and urban runoff.
26 nductivity generally diluted with increasing runoff.
27 rass cover--dictated the sourcing of NO3- in runoff.
28 ace changes in sediment provenance and river runoff.
29  aqueous concentrations of antimicrobials in runoff.
30 application of animal waste and agricultural runoff.
31 ation) with swine manure diluted to simulate runoff.
32 ndocrine-disrupting activity of agricultural runoff.
33 ources such as atmospheric fallout and urban runoff.
34 e delivery is dominantly controlled by river runoff.
35  primary TBA metabolites, occur in soils and runoff.
36 onmental problems associated with stormwater runoff.
37 dation of coral reefs exposed to terrestrial runoff.
38 (SM) in soil in relation to its transport in runoff.
39 major ion and Hg concentrations in 2008 melt runoff.
40 through wastewater effluent and agricultural runoff.
41 lids, are carried to the ocean by freshwater runoff.
42 , inland seas and shelf waters influenced by runoff.
43 he pond outflow water than in the stormwater runoff.
44        The (206)Pb/(207)Pb isotope ratios of runoff (1.16) were identical to those of topsoil and pre
45 ear(-1) influent load between three sources: runoff (12%), groundwater infiltration (39%), and sewage
46 71%), volatilization (5%), leaching (8%) and runoff (3%), while 13% of SM persisted in topsoil.
47 , and 79.2% on July 29) and summer ice sheet runoff ~3.9 sigma above the 1958-2011 mean resulted in e
48                                 Agricultural runoff accounted for 23% of total metal stream loads fro
49 soil and poultry litter leachates and street runoff, accounted for the remaining 30%.
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  was similar in both years (36% in 2008 melt runoff and 34% in 2009), it is possible that record low
53 antify the link between terrestrial sediment runoff and a downstream coastal marine ecosystem and con
54 heet through its impact on radiative budget, runoff and accumulation.
55 biomass-water feedback associated with water runoff and biomass-dependent infiltration rates.
56 ther, but the water loss from the system via runoff and drainage increased substantially, leading to
57  towards very different partitioning between runoff and evapotranspiration.
58 ange of endogenous hormones were detected in runoff and feedlot surface soils and manure from cattle
59 terization of the relation between meltwater runoff and ice flow.
60 ia were released, they were partitioned into runoff and leachate at similar concentrations, but in di
61 CT systems via two major transport pathways: runoff and leaching.
62  ice mass loss and the associated freshwater runoff and lengthening of open-water periods.
63 etan Plateau for glacier mass balance, river runoff and local ecology, changes in these quantities re
64 can be mobilized from CAFO surfaces in storm runoff and may lead to receiving water concentrations at
65 late and dissolved organic carbon in glacial runoff and near surface coastal waters was aged (12100-1
66 r composition of DON in the urban stormwater runoff and outflow water from an urban stormwater retent
67 flow water, which were only 13% different in runoff and outflow water.
68 c factors, such as nonpoint sources of paved runoff and point sources of sanitary sewage within the d
69  identified with FT-ICR-MS in the stormwater runoff and pond outflow water, which were only 13% diffe
70 ino sugars, lignins, and tannins in DON from runoff and pond outflow water.
71 ing to rapid death of corals when exposed to runoff and resuspended sediments, postulating that the k
72 on the anthropogenic influences of the paved runoff and sanitary sewage on the DOM quality of WWF usi
73 tures above 0 degrees C per year, freshwater runoff and sea ice in the 1980s) rather than by local ch
74  by human activity, but increased freshwater runoff and sediment fluxes may increase the size of the
75 the dominant NO3-N sources in the stormwater runoff and that there was a continuum of source changes
76 examine the spatial distribution of parasite runoff and the impacts of precipitation and development
77 ctions between the routing of North American runoff and the recent freshening of the Canada Basin, an
78   Durban Bay is strongly influenced by urban runoff and tidal hydrology, and sediments therein exhibi
79 gh-resolution geochemical records of surface runoff and vegetation from sediment cores from Lake Towu
80            Nanoplastic debris, resulted from runoff and weathering breakdown of macro- and microplast
81  precipitation minus total sublimation minus runoff) and a dynamic term.
82 uts throughout the year except during spring runoff, and also during autumn storms in the catchment w
83 d wear particles (TRWP) are a constituent of runoff, and determining accurate TRWP concentrations in
84 at least 1 below-the-knee vessel with distal runoff, and life expectancy >1 year.
85 r pathways: atmospheric processes, tributary runoff, and wastewater treatment plant (WWTP) effluents.
86 hat DOM pools in supraglacial and subglacial runoff are compositionally diverse and that N-rich mater
87 ned sewer systems when sewage and stormwater runoff are released into water bodies, potentially conta
88 y contaminated baseflow and rainfall/surface runoff, are observed in the Little Rouge Creek throughou
89 ve previously focused on effluent or surface runoff as the primary route of transport from animal fee
90 s groundwater (as Fe(2+)) and as superficial runoff (as Fe(3+)) into the sea, the latter with the for
91 ectiveness of soil bioretention for treating runoff, as measured by prevention of both visible cardia
92 r bacteria (FIB, a pollutant responsible for runoff-associated inland and coastal beach closures) in
93 ) s(-1)), limiting dilution of FIB and other runoff-associated pollutants once they enter the bay; (4
94 ough passive sampler, deployed in stormwater runoff at the outlet of a residential-industrial catchme
95 environmental benefits, including stormwater runoff attenuation and urban heat island mitigation.
96 n being a measured manipulation of watershed runoff attributable to fertilization, a response of simi
97 us (DP) was prevented not only from incoming runoff, but also from the media and captured PP.
98 rations of either total or methyl-mercury in runoff, but export increased by 50-70% in one of the har
99  originates from landscapes draining glacier runoff, but the influence of the influx of riverine orga
100 d increased sediment, nutrient, and chemical runoff, but these forces may also enhance pathogen runof
101   Here we show that clouds enhance meltwater runoff by about one-third relative to clear skies, using
102              We first document how road salt runoff can elevate sodium concentrations in the tissue o
103 nce they enter the bay; (4) once in the bay, runoff can form buoyant plumes that further limit vertic
104 lected milkweed, we then show that road salt runoff can result in increased muscle mass (in males) an
105 reasing urbanization and associated chloride runoff can salinize freshwaters and threaten lake water
106 ffectively managing water quantity; however, runoff carries pollutants, posing risks to the local env
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  California creek receiving urban stormwater runoff contains fipronil and degradate concentrations tw
112 n developing practices to mitigate pesticide runoff contamination from urban residential areas.
113 ays: P was exported primarily via stormwater runoff, contributing to surface water degradation, where
114 everal options, such as nutrient management, runoff control, and infrastructure upgrades.
115   Metabolite concentrations observed in CAFO runoff correspond to 5-15% of potential maximum steroid
116 o a lesser degree agricultural or stormwater runoff, could be important where they affect a major fra
117 le for temporal bone CT (-56.1%), peripheral runoff CT angiography (-48.6%), CT of the paranasal sinu
118        We used an approach in which specific runoff data determined at hydrological stations situated
119             Interpretation and use of copper runoff data for environmental risk assessment and manage
120 er basin CTA and CFWD were computed based on runoff data, water consumption data and a water balance
121 ntrations of chlortetracyline and tylosin in runoff decreased in consecutive rainfall events, althoug
122 ts such as storm events and surface snowmelt runoff destabilize smaller hot spring environments with
123 -forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes.
124 d water quality: (1) in the upper watershed, runoff diluted most dissolved constituents, (2) in the u
125                        This review on copper runoff dispersed from unsheltered naturally patinated co
126  experiments were conducted utilizing actual runoff, DOC from straw and compost, and a suite of TOrCs
127 n "ionic pulse" of mercury and major ions in runoff during both snowmelt seasons, but major ion and H
128 teria; (2) small drains can trap dry weather runoff during high tide, and then release it in a bolus
129 ables the integrative sampling of stormwater runoff during periods of weeks to months while weighting
130 . perenne x F. pratensis cultivar can reduce runoff during the events by 51% compared to a leading UK
131 est was demonstrated analyzing the clomazone runoff during the rice growing season in northern Urugua
132  that contaminants in the dissolved phase of runoff (e.g., PAHs) are cardiotoxic and that soil bioret
133 n factors for groundwater (EF5g) and surface runoff (EF5r) were calculated for both field drain and s
134 t minimize the volume of dry and wet weather runoff entering the local storm drain system may be the
135  were found at greater concentrations during runoff-event conditions.
136      Momentum from the water velocity during runoff events created flow through the sampler resulting
137 ds of weeks to months while weighting actual runoff events higher than no flow periods.
138  inorganic N at the time scale of individual runoff events is controlled by hydrologic, rather than b
139 rted 2/3 of their annual water yield during runoff events.
140 nical computed tomographic (CT) angiographic runoff examination.
141 is is further complicated by the dynamics in runoff flows and the large number of discharge points.
142 il-atmosphere water fluxes, and thus surface runoff flux, during repeated, climate-driven, vegetation
143 sport of antimicrobials and ARGs in soil and runoff following land application of swine manure slurry
144 urs both through WWTP effluent discharge and runoff following land applications of biosolids.
145 the laboratory to undiluted and 1:10 diluted runoff for 48 h, then transferred to control water and e
146 rements of iron concentrations in subglacial runoff from a large Greenland Ice Sheet catchment reveal
147 lecules in supraglacial water and subglacial runoff from a large GrIS outlet glacier.
148 vior of Cu in a stormwater wetland receiving runoff from a vineyard catchment (Alsace, France).
149 ssions associated with nitrogen leaching and runoff from agriculture for both the UK and globally.
150  the potential to transform urban stormwater runoff from an environmental threat to a valuable water
151 e of prairie strips also reduced total water runoff from catchments by 37%, resulting in retention of
152                         Roof-top acidic rain runoff from CIGS was found to be the predominant emissio
153                                              Runoff from coal-tar-based (CT) sealcoated pavement is a
154 etic steroids were not detected in manure or runoff from control cattle.
155                    By preventing the rooftop runoff from entering the wastewater treatment plant, bet
156                                              Runoff from farms and output from wastewater treatment p
157                                              Runoff from glaciers and ice sheets has been acknowledge
158             Ubiquitous examples of toxics in runoff from highways and other impervious surfaces inclu
159                                    Pesticide runoff from impervious surfaces is a significant cause o
160 nt hydrology to prevent increased stormwater runoff from land development.
161 erally decrease the overall estrogenicity of runoff from manure-fertilized fields.
162                                       Copper runoff from outdoor surfaces is predominantly governed b
163 t determine the environmental fate of copper runoff from outdoor surfaces.
164        We assessed the impacts of stormwater runoff from sealcoated asphalt on juvenile coho salmon (
165 alcoat to conventional asphalt and collected runoff from simulated rainfall events up to 7 months pos
166 ely) are therefore likely to be delivered by runoff from the Antarctic continent.
167 a progradation was driven by high freshwater runoff from the Greenland Ice Sheet coinciding with peri
168 rther, the NO3-N transport in the stormwater runoff from the residential catchment was driven by mixi
169 hest total mass loading of antimicrobials in runoff from the three rainfall simulation tests.
170         We present evidence that the reduced runoff from this Festulolium cultivar was due to intense
171                    Here we show that surface runoff from three island groups of the maritime Antarcti
172    Mortality following exposure to undiluted runoff from unsealed asphalt pavement and UVR was </=10%
173 s and increase precipitation and terrestrial runoff, further increasing organic matter and nutrient i
174 ment load reaching the delta is delivered by runoff generated by rainfall associated with tropical cy
175  be used to improve numerical simulations of runoff generation, stream water transit time and evapora
176 se estimated from observed precipitation and runoff generation.
177 0 m that is disproportionately important for runoff generation.
178 versely affect water quality through surface runoff, groundwater discharge, and damage to municipal w
179                                Because river runoff has significantly increased across the Eurasian A
180          Atmospheric deposition and riverine runoff have been traditionally considered the main exter
181                             These changes in runoff have impaired streams and riparian areas that pre
182 nges in sodium availability due to road salt runoff have significant effects on the development of so
183  of how climate-driven changes in freshwater runoff have the potential to alter food web dynamics wit
184 mately, an increase in snowpack and snowmelt runoff Hg concentrations.
185      The main drivers of Greenland ice sheet runoff, however, remain poorly understood.
186 ng pesticide exposure following agricultural runoff (i.e., pulse disturbance).
187 8% of snowpack Hg was exported with snowmelt runoff in 2008 and 41% in 2009.
188 average, which results, in part, from higher runoff in glaciated catchments.
189                                         Peak runoff in streams and rivers of the western United State
190 , synoptic monitoring of tDOM and freshwater runoff in surface polar waters, this novel approach will
191         From mid-May to August 2011, extreme runoff in the Columbia River ranged from 14,000 to over
192 solved organic matter (tDOM) and continental runoff in the surface Arctic Ocean.
193 ned atmospheric conditions promoted enhanced runoff, increased the surface temperatures and decreased
194                           Consequently, GICs runoff increases 65% faster than meltwater production, t
195                                  Comparably, runoff indexed hazards simulated by the Variable Infiltr
196 articulate phosphorus (PP) concentrations in runoff inflow were significantly reduced compared to out
197 re of Hg transported away from the mine with runoff into the creek, eventually affecting ecosystems d
198       Transported via surface and subsurface runoff into wetlands, their ultimate aquatic fate remain
199 e to their propensity to be transported with runoff, IPAs likely end up in surface waters where they
200 of bioavailable iron associated with glacial runoff is 0.40-2.54 Tg per year in Greenland and 0.06-0.
201                             Urban stormwater runoff is a globally significant threat to the ecologica
202                                  Continental runoff is a major source of freshwater, nutrients and te
203 iments to soils, suggesting that erosion and runoff is a potential pathway for AgNPs to enter waterwa
204                        Precipitation induced runoff is an important pathway for agrichemicals to ente
205                                We found that runoff is highly sensitive to vegetation migration; warm
206            In the Juncal catchment in Chile, runoff is likely to sharply decrease in the future and t
207           We suggest that enhanced ice sheet runoff is primarily associated with albedo effects due t
208 ered to local rivers, DSi in groundwater and runoff is redirected to the combined stormwater-sewage o
209 rainfall simulator induced 1 h of release in runoff/leachate partitioning boxes at three rainfall int
210 ally discharges into the environment through runoff, leaching and volatilization, resulting in three-
211  are transported through the environment via runoff, leaching, and land application of manure; howeve
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 ) in the urban corridor and lower watershed, runoff mobilized soluble constituents accumulated on the
215 to CT, NT resulted in an overall increase of runoff NO3(-) concentration, but similar runoff NO3(-) l
216  of runoff NO3(-) concentration, but similar runoff NO3(-) load.
217                 Total dissolved Hg meltwater runoff of 14.3 (+/- 0.7) mg/ha in 2008 and 8.1 (+/- 0.4)
218 ges in landscapes and climate can accelerate runoff of diverse pathogens from terrestrial to aquatic
219 tlers, an activity that would have increased runoff of fine-grained material.
220 he northern Baltic Sea, leading to a greater runoff of fresh water and terrestrial dissolved organic
221  deposition through rainfall, vegetation and runoff of soils.
222 nd have an important role in determining the runoff of the middle Yellow River.
223 urricanes, coastal development, agricultural runoff, oil spills, and fishing.
224  can further reduce the impact of stormwater runoff on aquatic environment at a minimal environmental
225 tal model to assess the effects of untreated runoff on the expression of genes that are classically r
226 rost suggest that the impacts of continental runoff on these processes are changing.
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  an environmental loss; surplus P is lost by runoff or accumulates as residual soil P.
232                      In excess (e.g., due to runoff or wastewater discharges), P is also a primary ca
233 riving from aeolian dust deposition, glacial runoff, or river discharges can form an important source
234                            Snowmelt, surface runoff, or stormwater releases in urban environments can
235 ock beneath landscapes influences subsurface runoff paths, erosional processes, moisture availability
236  the snowpack through the entire spring melt runoff period for two years.
237 ution; and (5) local winds can force buoyant runoff plumes back against the shoreline, where water de
238                      Heavy metals from urban runoff preserved in sedimentary deposits record long-ter
239 tic environment is highly dependent on local runoff quality indicating that a combined system of gree
240  corrosion rate cannot be used to assess the runoff rate.
241 le that explained the crossover year was the runoff ratio, defined as the ratio of annual mean stream
242 ds outweighed the weak influence of trees on runoff reduction.
243 tectable over background freshwater and soil/runoff related signals, even at tens of kilometers downs
244                    The results indicate that runoff remains acutely toxic for weeks to months after C
245 ug/AU 17alpha-TBOH) of the dose leached into runoff, respectively.
246 al precipitation not routed to the oceans as runoff returns to the atmosphere as evapotranspiration.
247 olite 17beta-TBOH intermittently occurred in runoff samples at 5-26 ng/L and may be correlated to ana
248       Test organisms exposed to undiluted CT runoff samples collected during the 3 days (C. dubia) or
249                         Analysis of 33 urban runoff samples collected from locations around the San F
250  Melengesterol acetate was detected in 6% of runoff samples from feedlots holding cattle administered
251                                   Stormwater runoff samples were collected over 25 stormwater events
252 dwaters, 16 eutrophic waters, 4 agricultural runoff samples, 9 stormwater runoff samples, and 12 muni
253  4 agricultural runoff samples, 9 stormwater runoff samples, and 12 municipal wastewater effluents.
254  observed in poultry litter and agricultural runoff samples.
255 more sustainable city by reducing stormwater runoff, saving infrastructural cost, increasing the numb
256 ly to sharply decrease in the future and the runoff seasonality is sensitive to projected climatic ch
257 he world, a much larger volume of stormwater runoff should be harvested than infiltrated to maintain
258         Rapid Pb transport during stormwater runoff significantly impairs surface water quality.
259 owever, Isortoq discharges tended lower than runoff simulations from the Modele Atmospherique Regiona
260  a factor of approximately 2-5 in irrigation runoff, suggesting that both endogenous and exogenous st
261 esulted in significantly higher erm genes in runoff than did incorporation and injection methods.
262  been initiated by North America fresh water runoff that caused a sustained reduction of North Atlant
263 onstruction, we route meltwater and seasonal runoff through the time-evolving Mississippi drainage ba
264  of DON increased from 10% in the stormwater runoff to 40% in the pond outflow water and DON was less
265                           Impacts of surface runoff to aquatic species are an ongoing area of concern
266 WFs), and relate the GWFs per river basin to runoff to calculate the N-related water pollution level
267  implications for the management of nutrient runoff to coastal zones.
268      This led, in conjunction with increased runoff, to enhanced submarine glacier melting.
269 (GS), keeping transpiration (EC) and, hence, runoff unaltered.
270 lations show evidence for enhanced ice sheet runoff under volcanically forced conditions despite atmo
271 r is rainwater insofar as it does not become runoff) used for producing, consuming, exporting, and im
272 nce to enhanced melt could be compromised if runoff variability increases further with future climate
273                      The age of aquatic C in runoff varied little throughout the year and appeared to
274 d to them through wastewater and animal farm runoff, very little is known about their effects in the
275 ted catchments as a consequence of increased runoff volume.
276 d to road density, the dominant control over runoff volume.
277                                              Runoff was collected before entering surface waters and
278          The increase in concentrations with runoff was due to higher levels of particle-associated c
279                             Whereas sealcoat runoff was more acutely lethal to salmon, a spectrum of
280                   Biodegradation of TOrCs in runoff was more enhanced by compost DOC than straw DOC (
281 olved organic phosphorus (DOP) from incoming runoff was not found, leaching of dissolved phosphorus (
282                                  The extreme runoff was the direct result of both melting of anomalou
283 ith driving rain, leading to highly polluted runoff water (up to several mg L(-1) biocides) being inf
284                  In this study, we collected runoff water from 6 large communities, each consisting o
285  pyrethroid residues with loose particles in runoff water from concrete surfaces after treatment with
286                                              Runoff water from three catchments, two harvested and on
287 as pyrethroids have been frequently found in runoff water from urban areas and the offsite movement i
288 t discharge contributions: MOXA prevailed in runoff water, whereas MESA was associated with slower fl
289  The brine is produced by either rainfall or runoff water.
290  contributed to the lakes enrichment through runoff waters that are more concentrated in solutes or l
291 e origination of pesticide residues in urban runoff, we investigated the association of pyrethroid re
292  factors influencing precipitation and river runoff were positively correlated with the growth of juv
293 ever, 17alpha-TBOH concentrations in initial runoff were predicted to exceed threshold levels (i.e.,
294 tively), but dramatically increased parasite runoff when combined (175% average increase).
295 s or sources of N to stormwater depending on runoff, which in turn was inversely related to retention
296 range of potential impacts of trees on urban runoff, which includes deposition of nutrient-rich leaf
297 , but these forces may also enhance pathogen runoff, which threatens human, animal, and ecosystem hea
298  of the initial terbutryn was emitted to the runoff, while 64-80% remained in the coating.
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

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