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1 ng an electric double layer that facilitates wetting.
2  a previously unrecognized transformation in wet acetonitrile in the presence of air to yield a new B
3 s dominated by Warnstorfia fontinaliopsis, a wet-adapted moss commonly found in the Antarctic Peninsu
4 o replicate the strong, instant, and durable wet adhesion of the marine sessile organism.
5 demonstrate that water leads to an increased wet adhesion through increased ionic bond formation.
6 ies at multiple length scales to achieve its wet adhesion.
7 (T&E) treatment regimen with ranibizumab for wet age-related macular degeneration (ARMD) in real life
8 EGF is associated with neovascularization in wet age-related macular degeneration (ARMD), choriocapil
9 ial growth factor inhibitors (anti-VEGF) for wet age-related macular degeneration (wAMD), and to acqu
10 uding proliferative diabetic retinopathy and wet age-related macular degeneration.
11  that function as weatherizers, emulsifiers, wetting agents, and corrosion inhibitors in injected flu
12       Although superbly adapted to resisting wetting, alkali flies are vulnerable to getting stuck in
13 epel even fluorinated solvents, which highly wet all materials.
14  adverse effects of therapy in patients with wet AMD and PDR.
15 loratory data analysis suggests stability of wet AMD over the 36-month period.
16 ased long-term mortality in individuals with wet AMD treated with bevacizumab compared to a same age
17 ubjects with advanced, treatment-experienced wet AMD were randomly assigned (3:1) to treatment and no
18 eovascular age-related macular degeneration (wet AMD) over 36 months.
19      Eligible subjects were >/=65 years, had wet AMD, and had best-corrected visual acuity (BCVA) 10/
20 pared to a same age and gender group without wet AMD.
21 ts based on prespecified criteria for active wet AMD.
22 ed for future evaluation in the treatment of wet AMD.
23 ity in patients treated with bevacizumab for wet AMD.
24 jections are widely used in the treatment of wet-AMD and PDR.
25                            Only 6% (6/97) of wet and 38% (30/80) of dry food were fully compliant.
26 er time was needed for both water and oil to wet and diffuse.
27  catch basins and wetland were similar under wet and drought conditions, E. hirae predominated during
28 ns predict large future fluctuations in both wet and dry conditions, we expect forests to become incr
29 ents during rock mechanics experiments under wet and dry conditions.
30 in the UK with EU guidelines (94% and 61% of wet and dry foods, respectively).
31 f wet days in a year and average duration of wet and dry periods, are undergoing significant changes
32  However, seedlings responded differently to wet and dry phases depending on drought frequency.
33 (C) and nitrogen (N) at similar rates during wet and dry phases.
34  compared relationships among traits between wet and dry seasons to test the effect of seasonality on
35 e exposed oak (Quercus robur) saplings under wet and dry soil moisture conditions to (18) O-depleted
36 raphy and hydrology and creating a mosaic of wet and dry soil surfaces in the Arctic.
37                                  Adhesion to wet and dynamic surfaces, including biological tissues,
38 nging weather conditions can cause cycles of wetting and drying in the unsaturated zone.
39 ncluded major flood and drought years, where wetting and drying treatments further modified the sever
40  alkanes can be controlled to modify surface wetting and environmental interactions.
41 lled surface wettability in terms of ethanol wetting and ethanol removal by harsh drying condition.
42 ions, we also studied solvent evaporation of wetting and non-wetting liquids dispersed in the sponge.
43                 The polymer switches between wetting and nonwetting states when it is reduced and oxi
44 t of microstructure during melting, reactive wetting and solidification of solder pastes on Cu-plated
45 ombinations of the driest ("dry"), wettest ("wet"), and average ("normal") weather years.
46 ial Cu6Sn5 layer is present within 0.05 s of wetting, and explore the kinetics of flux void formation
47 fer surface and actively control the surface wetted area fraction, known to decline monotonically wit
48 oil layers (0-15 cm) compared to the control wet areas.
49  were increased by VEGF antagonism, a common wet ARMD treatment, suggesting that VEGF inhibition coul
50 ion confirms the good stability and improved wetting at the interface between the lithiated Ge layer
51  oleic acid/1% sucrose ester fatty acid (w/w wet base)) had low contact angle, high spread coefficien
52     Consequently, at the watershed scale the Wet Basin may have better overall DIN treatment.
53                                          The Wet Basin was capable of denitrifying 58% of incoming DI
54 w) were greater in the Dry Basin than in the Wet Basin, 2.16 vs 0.75 g N m(-2) yr(-1), respectively.
55                                              Wet Basins had higher proportions of denitrification gen
56 ormwater basins, two often saturated sites ("Wet Basins") and two quick draining sites ("Dry Basins")
57                                        Among wet basins, TNMA emissions had a strong negative correla
58 ng factors (i.e. water content (11%, 35-50%, wet basis) and temperature (20-90 degrees C and back to
59 ntent of the pulp increased from 93% to 97% (wet basis), showing the removal of caustic salts from th
60 s optimal pH was verified through underwater wetting behavior and adsorption experiments.
61 a range of in silico functional analyses and wet bench experiments, our findings highlight new biolog
62                        Noting the paucity of wet-bench data regarding combinatorial effects of ABA an
63 n dry (DRY) and humid (HUM) heat matched for wet bulb globe temperature (WBGT, 27 degrees C).
64 ever, there is growing recognition that leaf wetting can have positive effects.
65 e pressure of P/P0 = 0.4 and ultrafast water wetting capability in less than 10.0 s.
66  Here we combined nanometre-scale imaging of wet cell walls by atomic force microscopy (AFM) with a s
67 hat are difficult to produce by conventional wet chemical or physical methods, thus opening up opport
68                                              Wet chemical screening reveals the very high reactivity
69 opy, as well as additional spectroscopic and wet chemical techniques.
70                                     Combined wet-chemical and spectroscopic analyses showed that both
71                                      Various wet-chemical methods for conversion of NO to nitrite (NO
72                       In this study, besides wet chemistry and scanning electron microscopy (SEM) ana
73  were in the snail's hepatopancreas based on wet chemistry and synchrotron-based investigations.
74           Herein, a general gelatin-assisted wet chemistry method is employed to fabricate well-defin
75                               Traditionally, wet chemistry methods are used to monitor the evolution
76                       Using a combination of wet chemistry, Fe isotope analysis, X-ray absorption spe
77        These indices were calibrated against wet chemistry.
78                           Significantly, the wet-chemistry method involves the preparation of dispers
79                               New convenient wet-chemistry synthetic routes have made it possible to
80 position of a HfO2/Al2O3 gate stack on a HCl wet-cleaned In0.53Ga0.47As substrate by comparing the fo
81 es and are consistent with an early warm and wet climate with active hydrologic cycling involving an
82  79% of this volume coming from landfills in wet climates (>75 cm/yr precipitation) that contain 47%
83 ansferred to the water when the skin remains wet compared to 30 +/- 17% when the skin is dry.
84  impact of coincident drought and antecedent wet conditions (proxy for the climatic factor influencin
85 f immiscible displacement under intermediate-wet conditions is less understood.
86  lead to greater benefits in dry rather than wet conditions, although some recent experimental eviden
87 nd high CO2/N2 selectivity, especially under wet conditions, is a challenge.
88           In contrast to the strong and weak wet conditions, pore-scale physics of immiscible displac
89                                        Under wet conditions, the presence of water altered the chemic
90 ll oil-filled pores were altered towards oil-wet conditions, which suggests that water in surface rou
91 ase immiscible fluid flow under intermediate-wet conditions.
92 for highly efficient CO2/N2 separation under wet conditions.
93 g fluid from weak imbibition to intermediate-wet conditions.
94          Depending on surface topography and wetting conditions, we find that this can lead to full d
95 ell as with the type of heat treatment, dry, wet, conductive heating and using microwaves.
96 ion in the United States primarily relies on wet-cooled plants, which in turn require water below pre
97 t high frequency events, such as fraction of wet days in a year and average duration of wet and dry p
98                                      Mercury wet deposition also varies by geographic region and seas
99       For arsenic speciation, the inputs for wet deposition are not well understood.
100 that TMAO and inorganic arsenic in monsoonal wet deposition are predominantly of marine origin.
101 (supercells, disorganized, and QLCS) enhance wet deposition by a factor of at least 1.6 relative to n
102 are widely present and elevated in monsoonal wet deposition identifies major knowledge gaps that need
103 rsenic are the dominant species in monsoonal wet deposition in the summer Indian subcontinent, Bangla
104 ions of both species were found in monsoonal wet deposition in the winter Indian subcontinent, Sri La
105 ling for other factors, we find that mercury wet deposition is greater over high-elevation sites, sea
106 is and on the strong correlations with known wet deposition marine derived elements: boron, iodine, a
107  the effect of precipitation type on mercury wet deposition using a new database of individual rain e
108 r was predicted from measured weekly mercury wet deposition using a scavenging ratio approach, and co
109 ric mercury depletion events', or AMDEs) and wet deposition via precipitation are sources of Hg to th
110 e input flows of summation operatorPCBs from wet deposition, dry deposition, tributary loading, and a
111 ents to terrestrial environments, mainly via wet deposition.
112 ydration that removes all remaining soot via wet deposition.
113                                 Furthermore, wet-deposition measurements in the Arctic showed some of
114 ight into the genesis of thrombosis in blood-wetted devices, and provide a tool for the design of les
115 nd reversible red-blue color change upon the wetting-dewetting transition, suggesting that hydration-
116  with switchable chromogenic properties upon wetting-dewetting transitions is reported.
117                           Drought legacy and wetting direction are perhaps more important determinant
118 for high-performance macrofibers involving a wet-drawing and wet-twisting process of ultralong bacter
119 t with different drought frequency caused by wet-dry cycles of varying periodicity.
120 s of nucleotides) to warm little ponds whose wet-dry cycles promoted rapid polymerization.
121 ation into RNA occurred in just one to a few wet-dry cycles.
122 olation, 2-year cumulative N losses from the wet-dry scenario were greater than the dry-wet scenario.
123 d 2-year cumulative N2 O emissions while the wet-dry sequence increased 2-year cumulative N2 O emissi
124 the sequence of extreme weather years (e.g., wet-dry vs. dry-wet) may affect cumulative N losses.
125  between functioning as C sinks/C sources in wet/dry years.
126 Multifunctionality had a lower resistance to wetting-drying cycles than to warming or N deposition.
127 rption templates for amino acids, and during wetting-drying cycles, promote peptide bond formation.
128 on basin was substantially drier or remained wet during glacial times has been controversial, largely
129 drometeorological conditions were relatively wet during the growing season (e.g. in early spring in s
130           Investigating the impact of drying-wetting (DW) on dynamics of newly-produced AS is critica
131 bial trees were more abundant in dry than in wet ecosystems.
132 e transition in climate from an early, warm, wet environment to today's cold, dry atmosphere.
133                                  Using a dry-wet environmental cycling protocol, hundreds of proto-pe
134 egative effects on plant function, such that wet environments may select for leaves with certain leaf
135 overn soot particle-particle interactions in wet environments such as rain droplets or surface aquati
136 rough either increased WUE or ci in arid and wet environments, respectively.
137 here weakly to tissues, or cannot be used in wet environments.
138 e using polymethyl methacrylate (PMMA) and a wet etch to allow the user to transfer the flakes to a f
139 on processes containing laser patterning and wet etching have demonstrated the advantages of easily t
140 ere lithography technique and subsequent dry/wet etching processes.
141  in substrates typically involve one or more wet-etching steps.
142 duct crystals at quantitative conversion are wet-exfoliated under mild conditions and afford countles
143                                              Wet experiments have identified a great number of human
144                            In order to guide wet experiments, we develop computational methods to pre
145 changes in response to decadal-scale dry and wet extremes during a 13-year period, producing striking
146 dicted bromide concentrations contributed by wet FGD at Pennsylvania intake locations ranged from 5.2
147 entified as being downstream of at least one wet FGD discharge.
148        Coal-fired power plants equipped with wet flue gas desulfurization (FGD) systems have been imp
149 we assess the benefits and costs of treating wet flue gas desulfurization (FGD) wastewater at US CFPP
150 the displacement of a non-wetting fluid by a wetting fluid are pore-filling or piston-like displaceme
151 hat compete during the displacement of a non-wetting fluid by a wetting fluid are pore-filling or pis
152  ordered structures for bilayer monodisperse wet foams with arbitrary liquid fraction.
153 provide nutritional minimum (e.g. Cu, 20% of wet food) or exceeded nutritional maximum (e.g. Se, 76%
154 xceeded nutritional maximum (e.g. Se, 76% of wet food).
155 =8 of 11 guidelines (99% and 83% for dry and wet food, respectively), but many failed to provide nutr
156              Using coordination dynamics and wetting forces, we engineer hybrid liquid-solid clusters
157 n gradient shared more species with dry than wet forest communities.
158 al acclimation response of photosynthesis in wet-forest tree species.
159 ent changes in photosynthetic capacity in 10 wet-forest tree species: six from temperate forests and
160 larger than emissions reported for temperate wet forests and tropical peat swamp forests, representin
161 the U.S. since at least 1850 C.E. with cool, wet forests demonstrating the greatest declines.
162                          The neovascular or "wet" form of AMD can be treated to varying degrees with
163 ion (CNV), is a hallmark of the neovascular (wet) form of advanced AMD and leads to significant visio
164                                         Soil wetting from above (precipitation) results in a characte
165 cally different pattern of pore-filling than wetting from below (groundwater), with larger, well-conn
166 terial is fully saturated behind the visible wetted front.
167 nt primary production categories (e.g., oil, wet gas, dry gas) and developmental stages of wells.
168                                     Overall, wet-gas basins (UGR, DJ, Uintah) had higher TNMA emissio
169 jor lineages rapidly diversified in warm and wet habits during the Late Cretaceous, and the rapid div
170 es of varying roughness and compliance under wetted high-shear conditions using an adhesive disc that
171          Large-leaved species predominate in wet, hot, sunny environments; small-leaved species typif
172                 In addition, combined with a wet impregnation method, different substrate-materials-s
173  specific PdBiTe catalyst formulations via a wet-impregnation method, followed by application of resp
174 lies, alkali flies are better able to resist wetting in a 0.5 M Na2CO3 solution.
175 ures; (2) capillary condensation followed by wetting in macro-scale surface scratches beginning appro
176  physical protection, but also by drought or wetting-induced shifts in hydrologic connectivity.
177 while a fingered morphology is found for non-wetting invading fluids, causing the residual amount of
178                                         Leaf wetting is often considered to have negative effects on
179                   In this study, we utilized wet lab migration experiments and quantitative histologi
180 ranscription factor candidates together with wet-lab experiments validating computational models.
181 affolds, utilizing various computational and wet-lab techniques, they often can produce only partial
182          Using the first 47 primer pools for wet-lab validation, we sequenced 25Kb at 99.7% complete
183                                         More wet laboratory research experience is needed, and transl
184 udied solvent evaporation of wetting and non-wetting liquids dispersed in the sponge.
185  arsenic (typically 2000-20000 mug As kg(-1) wet mass), most of which is present as arsenobetaine, an
186 extreme weather years (e.g., wet-dry vs. dry-wet) may affect cumulative N losses.
187             We conducted investigations in a wet meadow (WM), a grassland meadow (GM), a moderately d
188                                              Wet midcontinental climate reflecting negative PNA-like
189 OH steeping can improve the effectiveness of wet milling in disintegrating cell walls through solubil
190 proso millet protein was extracted by either wet milling or 60% (v/v) aqueous ethanol and then used a
191 anol showing better performance than that by wet milling process.
192 oot pieces in 0.75% NaOH in combination with wet milling was investigated to determine whether and ho
193 les and approx. 4% greater starch yield with wet milling.
194 l grits and gluten slurry in dry-milling and wet-milling coproducts, respectively.
195 in the pericarp (45.9% of total ANCs) and in wet-milling they were concentrated in steeping water (79
196  green-up, by as much as 53 +/- 18 d (in the wet miombo).
197 re and increasing the frequency of household wet mopping significantly reduced p,p'-DDT and p,p'-DDE
198        Here, mineral composition of complete wet (n = 97) and dry (n = 80) canine and feline pet food
199 esults reveal that the oxide coating enables wetting of metallic lithium in contact with the garnet e
200  atmosphere to hydration of biomolecules and wetting of solid surfaces.
201  face of the chromatography paper to prevent wetting of the sample beyond the hydrophilic testing reg
202 ence on the wettability alteration (less oil wet) of calcite surface.
203 y not solely reflect the negative effects of wetting on plant function.
204 can provide insight into the effects of leaf wetting on plant, community, and ecosystem function.
205 d to realize both reversible and pluripotent wetting on topographic surfaces.
206                           We describe stable wetted/open and dewetted/closed states, and uncover conf
207 d stable reference material in the form of a wet paste.
208          Here we demonstrate that pore-scale wetting patterns interact with antecedent soil moisture
209 losses of nucleobases to pond seepage during wet periods, and to UV photodissociation during dry peri
210 tter process can lead to trapping of the non-wetting phase.
211 s during dry phases and at high rates during wet phases.
212       Our results show that for intermediate-wet porous media, pore geometry has a strong influence o
213 lenges in storing natural gas as hydrates in wetted porous carbon materials is also included.
214 f ambient precipitation to form a drought to wet precipitation gradient) was conducted over three gro
215 blocked <2 years, drain blocked <7 years and wet pristine site), and examined whether hydrological le
216 topography in nature, thereby overcoming the wetting problems in previous conventional solid systems.
217                                         The "wet process", including blanching, sweating and drying,
218 ct synthesis of OMCs is still limited to the wet processing of phenol-formaldehyde polycondensation,
219                      Modification of surface wetting properties and conjugation with fluorescent tags
220 ly derived surfaces shows that the different wetting properties are due to the surface morphology and
221                   We demonstrate directional wetting properties as well as structural coloration base
222                                              Wetting properties control flow of immiscible fluids in
223                   The colorimetric and water wetting properties of as-fabricated arrays were found to
224 found to be a significant determinant in the wetting range of the polymer.
225                                           It wets RE and AE, and flows by capillarity through the pap
226 tile methodology, which also uses low-cost, "wet" reagents, is scalable and done at ambient pressure.
227 t oil recovery was observed for the most oil-wet sample, where the oil remained connected in thin she
228 e wet-dry scenario were greater than the dry-wet scenario.
229                       Mothers nursing in the wet season (July to October) produced significantly less
230 .65 billion people and many ecosystems, with wet season (May-September) precipitation being the criti
231   This may be intensified by seasonality, as wet season conditions can alter resource availability, f
232 -Interim and MERRA2 reanalysis, we find that wet season precipitation displays vertical gradients (i.
233          FIBs were more prevalent during the wet season than the dry season, and L. pneumophila was o
234 asons, having a greater influence during the wet season when efflux was high than during the dry seas
235   Data from 24-hour diet recalls (55% in the wet season) of n = 6,226 participants (34% women) in rur
236 was introduced in the dry season than in the wet season, driven by an increase in home range overlap
237 ficant contribution of micronutrients in the wet season.
238 able isotopes across five streams during the wet season.
239  L. pneumophila was only observed during the wet season.
240                          During this period, wet-season Sahelian temperatures have not risen, ruling
241  to its potential efficiency during dry than wet seasons (consistent with water limitation of photosy
242 e for a moderate Hadean climate with dry and wet seasons and a lower atmospheric abundance of CO2 tha
243 lications, including energy storage, surface wetting/self-cleaning, photocatalysis and sensors.
244 red with the normal-normal scenario, the dry-wet sequence decreased 2-year cumulative N2 O emissions
245 t reduction of sludge mass (80% reduction of wet sludge volume) and consequent disposal cost.
246         We measured NO emission pulses after wetting soils from similar lithologies along an altitudi
247 ein alloy fibre with whole fibronectin using wet spinning approaches in order to synergize their resp
248 embrane was developed via a one-step dry-jet wet spinning.
249 in the contact region during dry winters and wet springs.
250                                In normal and wet summers, both species responded to precipitation red
251 stically lead to higher adhesion energies on wet surfaces as compared with those of existing adhesive
252 nds which inhibit migration of Salmonella on wet surfaces.
253 s with hydrophobic methacrylate adhesives on wet surfaces.
254 ith an intermediate recovery in a more water-wet system, where the oil was trapped in ganglia in the
255 and Rs in response to drought indicated that wet systems had an overall risk of increased loss of C b
256 xturally equilibrated metallic melt does not wet the silicate grain boundaries and tends to reside in
257 ont morphology emerges if the invading fluid wets the beads while a fingered morphology is found for
258 CO3 which causes water to penetrate and thus wet their setose cuticle.
259 sity, negligible nontoxicity, and ability to wet to nonmetallic materials.
260 nergetic and kinetic features for the cavity wetting transition suggest that reversible hydration-lev
261 he MorphS surfaces, the distinctly different wetting transitions of liquids with different surface te
262                     Both ex situ and in situ wetting transitions on the MorphS surfaces are solely du
263 (epilayers), as in the case of the so-called wetting transparency documented for graphene.
264 espectively) than stimulated under the three wet treatments (by 8.9, 14.3, and 18.5% under the +20, +
265 es produce nondormant seeds, particularly in wet tropical forests, a biogeographic pattern that is no
266 9th-century plant geographers noted that the wet tropics harbor plants with exceptionally large leave
267 ance macrofibers involving a wet-drawing and wet-twisting process of ultralong bacterial cellulose na
268 igated how controlled fire and an artificial wet-up event, in combination with exposure to the longer
269 frameworks can be conformally and reversibly wet upon complex topography in nature, thereby overcomin
270 ed by the ratio of the standard deviation of wetting velocity to the characteristic wetting velocity
271 on of wetting velocity to the characteristic wetting velocity was put forward to signify the strength
272 Escherichia coli were also comparable during wet versus drought conditions, and the relative abundanc
273 atial (marsh versus estuarine) and temporal (wet versus dry season) characteristics.
274 cers of Hg deposition pathway (Delta(200)Hg, wet vs dry Hg deposition) and atmospheric Hg sources and
275 ientation, and hence switchable, anisotropic wetting was realized.
276 = 3.04, 95% CI: 1.54, 5.98); exposure during wet weather further increased rates (e.g., for earache o
277 ality of dissolved organic matter (DOM) in a wet weather overflow (WWF) can be broadly influenced by
278 associated with incident illness only during wet weather.
279 after seawater exposure during both dry- and wet-weather periods and to determine the relationship be
280 riod, decreasing by 39% from 0.171 mug g(-1) wet weight (w.w.) in 1980 to 0.104 mug g(-1) w.w.
281 4% of calculated basal metabolic rate (BMR), wet weight (WW) absorption <23 g .
282 getative compartments with up to 97 ng g(-1) wet weight (ww) and 94 ng g(-1) ww in birch leaves and s
283 atorVMS concentrations (median: 178 ng g(-1) wet weight (ww)) compared with those from the urban indu
284 th intestinal failure, increasing intestinal wet weight absorption and reducing diarrhea.
285 ounds (TICs), ranged from 0.05 to 35.03 ng/g wet weight and from 0.03 to 3.32 muM in tuna lipid.
286  fish levels ranged from 0.16 to 138.29 ng/g wet weight and lipid-normalized concentrations from 0.1
287 igmaPFASs ranged between 0.66-45 ng per g of wet weight of the whole body.
288 ors ranged from 1.3, 3.7, 4.0, and 4.4 L/kg (wet weight) for fish muscle, zooplankton, predatory inve
289                              PFASs Log BAFs (wet weight) ranged from 2.6 +/- 0.8 for perfluorohexanes
290 variation in energy density (energy per unit wet weight).
291  38 (char), and 9.9 +/- 5.9 (trout) ng g(-1) wet weight.
292 y standards (EQS) for biota are expressed as wet weight.
293  at an average annual rate of -14.9 pg g(-1) wet weight.
294  fish muscle (e.g. , PFOS: 0.28-2.1 ng g(-1) wet-weight), with little or no differences when comparin
295 ust as snow and water accumulates during the wet winter months.
296                                In the record wet year of 2013/2014, however, Rs was independent on N
297 n both years and herbivore protection in the wet year only.
298    A common method for imposing both dry and wet years is to alter each ambient precipitation event.
299  ER switched from autotrophic respiration in wet years to heterotrophic in dry years.
300                                       During wet years, growth conditions for algae could also be enh

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