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1 hat explosive eruptions can also cause magma intrusion.
2 led adverse effects of CO2 leakage and brine intrusion.
3 retard uraninite (UO2) oxidation upon oxygen intrusion.
4 31 Ga, overlapping with the estimated age of intrusion.
5 n rates even with modest levels of saltwater intrusion.
6 cesses involved in the response to territory intrusion.
7 gers and inhibit UO2 reoxidation upon oxygen intrusion.
8 -like feature is consistent with sedimentary intrusion.
9 mands will exacerbate the threat of seawater intrusion.
10  move on substrates that flow in response to intrusion.
11 oethite, but is partially remobilized by CO2 intrusion.
12 coincident with the large-scale Saharan dust intrusion.
13 tributed to metamorphism of coal by basaltic intrusion.
14 n indoor air contaminated through soil vapor intrusion.
15 ved understanding of the potential for vapor intrusion.
16  VOCs and (ii) temporal variability in vapor intrusion.
17 hat some seismic events are related to magma intrusion.
18 es of VOCs and temporal variability in vapor intrusion.
19  as a threat or agonistic call within 2 s of intrusion.
20 ighly aggressive manner when facing homecage intrusion.
21 use of potable water and mitigation of water intrusion.
22 tions and providing defense against pathogen intrusion.
23 rovince, from dominantly flood lavas to sill intrusions.
24 erian volcanism, and by coeval Ni-rich magma intrusions.
25 s stratiform layers in many mafic-ultramafic intrusions.
26 c metamorphic lithologies and large plutonic intrusions.
27 troposphere and lower stratosphere during PV intrusions.
28 ver O2 is supplied, for example, by episodic intrusions.
29 ds, especially those associated with layered intrusions.
30  from the stratosphere, associated with deep intrusions.
31 ntrusion was followed by a series of smaller intrusions.
32  F, and Cs) in water samples within granitic intrusions.
33 y ruminators were more susceptible to memory intrusions.
34  trauma memories, precipitating sensory-rich intrusions.
35 uctural inhomogeneities in the form of solid intrusions.
36 er Asia and North America, resulting in cold intrusions.
37 arkable kilometre-wide subvolcanic peperitic intrusions.
38 ing and frequency of Kilauea's eruptions and intrusions.
39 ospheric ozone concentration and subtropical intrusions account 65% of the co- variability (below 5 k
40 y dyking, provide strong evidence that magma intrusion achieves the majority of plate opening in this
41 ld underlie behavioral response to territory intrusion across species spanning a broad phylogenetic r
42  with new global reference data from layered intrusions, active volcanic provinces, and established l
43                            Thus, suppressing intrusions affected emotional content.
44 croscopic theories-classical capillarity for intrusion and classical nucleation theory (CNT) for extr
45                            The May 2018 rift intrusion and eruption of Kilauea Volcano, Hawai'i, repr
46 rtifacts, the microscopic mechanism of water intrusion and extrusion in the pores, which are thermall
47 lecular simulation and theory of adsorption, intrusion and freezing in porous silica.
48 n equation to describe the thermodynamics of intrusion and in-pore freezing.
49 astal nuclear sites resulting from predicted intrusion and inundation with oxic seawater.
50                                    Saltwater intrusion and organic matter enrichment may increase sul
51  the rift zone, prompting opportunistic dyke intrusion and ultimately facilitating the eruption.
52 during continental breakup leads to magmatic intrusion and volcanism, yet our understanding of the lo
53 h as coastal flooding and erosion, saltwater intrusion and wetland degradation.
54 e restite compositions only, producing mafic intrusions and a pronounced compositional gap.
55 val classes, with no differentiation between intrusions and deliberations.
56  storage requires considering multiple small intrusions and multiple spatial scales, and our approach
57 , with moderately strong connections between intrusions and nightmares, being upset by reminders, and
58 l to other symptoms in the acute phase, with intrusions and physiological reactivity among the most c
59                                              Intrusions and physiological reactivity were central in
60 isms allowing people to control these memory intrusions and reduce their emotional impact.
61 p was dominated by slow-wave sleep with fast intrusions and reduced hierarchical coupling with spindl
62           The feedback between dyke and sill intrusions and the evolution of stresses within volcanic
63                                     Magmatic intrusions and volcanic eruptions are intimately related
64 upply of gas leads to the formation of a new intrusion, and the cycle repeats.
65 t provided a list of factors affecting vapor intrusion, and the influence of some of these are explor
66 nd 1.5 [0.3] respectively) among flashbacks, intrusions, and avoidance of thoughts, with moderately s
67 vers, revealing numerous objects, few memory intrusions, and precise spatial information.
68 his downregulation of activity during memory intrusions appears to disrupt momentary awareness of unw
69 t in some volcanoes (e.g., Kilauea), but how intrusions are accommodated in other volcanic systems re
70        Wells located within 5 km of granitic intrusions are at risk of containing high levels of [U]
71 ers of monomineralic anorthosites in layered intrusions are products of the chamber replenishment by
72 to true intakes for matches, exclusions, and intrusions, ASA24 performed well.
73 nal tree coring might be applicable in vapor intrusion assessment.
74 eptual and mathematical models of soil vapor intrusion assume that the transport of volatile organic
75 ss became channeled into a stable deep-water intrusion at 900- to 1,300-m depth, as aqueously dissolv
76 rth's surface, few constraints exist on CAMP intrusions at depth.
77          Additionally, female, but not male, intrusion attenuated resident mouse feeding.
78 es in the levels of PTSD symptom clusters of intrusion, avoidance and hyperarousal are associated wit
79 iodic contamination suggested that transient intrusion, backflow, release of particulates, or sloughi
80             Remote sensing indicates that an intrusion began after eruption onset and caused severe (
81 st: 1) repeated emplacement of magma through intrusions below the caldera centre; 2) occasional later
82 s associated with a deep, sub-vertical magma intrusion between Agung and its neighbour Batur.
83                                          The intrusions brought dry and ozone rich air of stratospher
84                                Shallow magma intrusion builds subsurface reservoirs that are drained
85  located within 5-10 km distance of granitic intrusions but do not show correlations with metamorphis
86     Nonvolatile compounds do not cause vapor intrusion, but they still move with the groundwater and
87 ates cooperate to defend their range against intrusion by neighboring groups.
88 s during social interactions, and into which intrusion by others can cause discomfort.
89                      People often respond to intrusions by suppressing their retrieval, excluding the
90  playback experiments simulating territorial intrusions by wild capuchin monkey (Cebus capucinus) gro
91  source, above which the potential for vapor intrusion can be considered negligible, were defined.
92                                        Vapor intrusion can be prevented by natural attenuation in the
93                                        These intrusions can be classified as 'exceptional events', wh
94 between La Nina and western US stratospheric intrusions can be exploited to provide a few months of l
95         Evidence suggests deep stratospheric intrusions can elevate western US surface ozone to unhea
96                                 These iconic intrusions can thus be interpreted as eruptive features
97 rom groundwater to indoor air-known as vapor intrusion-can be an important exposure pathway at hazard
98 e common interpretation procedure of mercury intrusion capillary pressure (MICP) measurement for nano
99 s obtained from X-ray tomography and mercury intrusion capillary pressure porosimetry, we define a di
100 eefs, which frequently experience cold-water intrusions caused by internal wave-induced upwelling, th
101 rations more than doubled during the Saharan intrusion compared with non-Saharan.
102  grooming strength decreased after simulated intrusions compared to female-to-female grooming strengt
103 rface and lead to water permeation and Na(+) intrusion, consistent with ion-toxicity in islet beta-ce
104 ne crystal rims shows that episodes of magma intrusion correlate temporally with recorded seismicity,
105 hermore, a decrease in pH resulting from CO2 intrusion could reactivate the adsorption of Se(IV) and
106                             Furthermore, the intrusions cut basal basalts of the Taimyr lava stratigr
107 l is based on an analysis of the EPA's vapor intrusion database, which contains almost 2,400 indoor a
108  the far-field transport of the oil from the intrusion depth.
109  a finite state machine for network security intrusion detection and definable inexact pattern matchi
110  questionnaires after analogue trauma and an intrusion diary completed over 4 days following the expe
111 f magma supply, the timing of secondary dike intrusions differs from that of the aftershocks.
112  that the first of two shocks in a creep- or intrusion-driven swarm triggers the second, when this ne
113 r volcanoes with known typical extrusion and intrusion (dyke) volumes, the new methodology presented
114 Despite progress, important limitations with intrusion effects in low resolution 2D pillar-based meth
115                                              Intrusion elicited robust c-fos mRNA expression in both
116 cell groups contributes to the regulation of intrusion-elicited behavioral responses.
117                             Fewer and weaker intrusion events follow in the two springs after the 199
118 d shift in the number of Potential Vorticity intrusion events over the Pacific are evident.
119 ssessment of the scope of potential seawater intrusion exists.
120 th respect to hydrolysis after several water intrusion-extrusion cycles.
121            We review theoretical results for intrusion/extrusion and freezing in silica pores and dis
122  the underlying mechanisms governing mercury intrusion/extrusion experiments.
123 reased due to nanoscale confinement, and the intrusion/extrusion hysteresis is practically suppressed
124 gest that the most important features of the intrusion/extrusion process can be understood in terms o
125                       As the pressure in the intrusion falls, the gas pocket collapses.
126 biogeochemical cycle study and stratospheric intrusion flux at the surface are discussed.
127            While prevailing models of trauma intrusions focus on dysregulated emotional processes, we
128                                          The intrusion frequency has strong interannual variability d
129  two-fold increase and westward shift in the intrusion frequency over the Pacific Ocean, due to the c
130      Abnormally high slow waves, alpha/delta intrusions, frequent transitions, and muscle twitches ar
131 and immediate rhizosphere to prevent sulfide intrusion from the surrounding sediment is critical for
132                                        Vapor intrusion from volatile subsurface contaminants can be m
133                   Because marine groundwater intrusion has been shown to increase during the summer,
134 ft axis outwards, indicating that axial dyke intrusion has been the primary mechanism of segment grow
135    The limited distribution of lower crustal intrusions implies modest total CAMP volumes of 85,000 t
136 orthern end of the Red Sea, and low nutrient intrusion in comparison with the southern end.
137 s shear zone network dissects an anorthosite intrusion in Lofoten, northern Norway, and separates rel
138     Here we show how a recent segmented dyke intrusion in the Baretharbunga volcanic system grew late
139 ments the first and longest case of seawater intrusion in the WKP, and also indicates significant pos
140           To predict the impact of saltwater intrusion in these environments, we must first gain a be
141 n of carbon release associated with volcanic intrusions in the North Atlantic Igneous Province.
142 verall, and time-series analyses showed that intrusion incidence declined more quickly.
143 tual retrieval, we compared correct recalls, intrusions (incorrect recall of either items from prior
144 ribution, orientation, and dimensions of the intrusions indicate a globally isotropic extensional str
145 nd testosterone secretion; and 3) diminished intrusion-induced c-fos expression in select 5-HTergic b
146                                          The intrusion induces "preferential tropism" of roots by fir
147 n groundwater, and they pose a risk of vapor intrusion into buildings.
148                                     Seawater intrusion into coastal aquifers can increase groundwater
149 ant discharge to marine waters and saltwater intrusion into coastal aquifers.
150 than in intermediate waters and a negligible intrusion into deep waters (>1000 m).
151 ersity is best conserved by minimizing human intrusion into intact and relatively unfragmented landsc
152 ea level rise is expected to cause saltwater intrusion into many historically freshwater ecosystems.
153 ms controlling both brackish water and CO(2) intrusion into shallow aquifers along fault zones.
154 f the synoptically driven warm and moist air intrusion into the Arctic as a primary contributing fact
155 ing it closer to the shelf and enhancing its intrusion into the East China Sea.
156                        Linear infrastructure intrusions into natural ecosystems, such as motorways an
157                                        Virus intrusions into nondisinfected drinking water distributi
158   Here, we estimate AGI incidence from virus intrusions into the distribution systems of 14 nondisinf
159                                        While intrusions into the South China Sea echoed the Pacific D
160 in persistent, quasi-stationary low-pressure intrusions into the subtropics of the CNP, accompanied b
161  building pressure conditions during a vapor intrusion investigation program to provide an improved u
162 ncentrations in indoor air to evaluate vapor intrusion is complicated by (i) indoor sources of the sa
163 that remobilization of trace elements by CO2 intrusion is not a universal physicochemical effect.
164                                     Seawater intrusion is particularly likely where water tables lie
165 riving the year-to-year variability of these intrusions is thus relevant for effective implementation
166 om groundwater to indoor air--known as vapor intrusion--is an important exposure pathway at sites wit
167 ted and that were excluded, 2) the number of intrusions (items reported but not consumed), and 3) dif
168 attern of contamination points to deep-ocean intrusion layers as the source and is most consistent wi
169 l thought to have been trapped in deep-ocean intrusion layers at depths of approximately 1,000-1,300
170 was further demonstrated that the cold-water intrusions may have originated from depths of ~100 m and
171 mputed by simulations to correlate the water intrusion mechanism with the atomistic details of the ze
172 s including necessary magnitudes of basaltic intrusion, mixing and mobilization of coal and basalt, a
173        Simulations with the analytical vapor intrusion model "Biovapor" corroborated the low explosio
174  The proposed solution relies on a 1-D vapor intrusion model that incorporates a piecewise first-orde
175 ocesses, a three-dimensional numerical vapor intrusion model was used to simulate the degradation, mi
176  the physical understanding in current vapor intrusion models.
177                                    Territory intrusion modulated similar brain functional processes i
178 n conductivity are directly tied to seawater intrusion moving inland and traveling 11 miles against t
179             Thus, the long-held view is that intrusions must precede and feed eruptions.
180  echoed the Pacific Decadal Oscillation, the intrusion northeast of Taiwan decreased markedly before
181          We find that the dimensions of dike intrusions obey a power law analogous to the Gutenberg-R
182 e rifting episodes, we demonstrate that dike intrusions obey scaling relationships similar to earthqu
183 , and again in August of that year, prior to intrusion of an inferred dike between Mount Agung and Ba
184 ed by groundwater pumping caused the lateral intrusion of arsenic contamination more than 120 metres
185  brain targeting of therapeutics without the intrusion of BBB and GI exposure.
186    Evaluation of the duodenoscope identified intrusion of biomaterial under the sealed distal cap; de
187 omalous literal translations, indicating the intrusion of Chinese lexical structures into English pro
188                                 The possible intrusion of CO2 into a given freshwater aquifer due to
189 rotect groundwater aquifers against downward intrusion of contaminants.
190 upflow of deep-lying saline water, extensive intrusion of current Baltic Sea water, and substantial t
191 lteration of the shallow crust caused by the intrusion of dikes and sills of the Columbia River Basal
192 paper we focus on a second mechanism: upward intrusion of displaced brine or brackish-water into a sh
193       This has resulted in the unprecedented intrusion of government and the legal systems into the p
194 interactions, CO2 sequestration in rock, and intrusion of groundwater aquifers by saline water.
195                             We attribute the intrusion of gypsum into membrane pores to the crystalli
196 subtropical wave breaking events lead to the intrusion of high PV (potential vorticity) air along the
197 d/floxed); Rho-Cre(+) mice lack the aberrant intrusion of horizontal cell processes.
198 uorescent dye displacement assay confirm the intrusion of IL molecules into the DNA minor groove.
199 etric bilayer protects the bacterium against intrusion of many toxic substances, including antibiotic
200        Experiments and modeling identify the intrusion of neuronal offline periods as a mechanism tha
201 unlike others-was not caused by the forceful intrusion of new magma into the rift zone.
202 ing in the north and wind-induced horizontal intrusion of nutrient-rich water in the south), and mini
203 re of all three domains has shifted with the intrusion of oil.
204            I. emarginata are able to prevent intrusion of particles even smaller than 1 mum into the
205 es for horizontal gene transfer, and enables intrusion of pathogenic organisms through depletion of o
206 jury, repair barrier function, and limit the intrusion of pathogenic organisms.
207  by overt retrieval or refractory access; 2) intrusion of perceptual information on semantic processi
208 st that PCL recognition of H3K36me3 promotes intrusion of PRC2 complexes into active chromatin region
209 sleep-wake cycle with fluctuating vigilance, intrusion of rapid eye movement dream imagery into wakef
210 ness during waking that are thought to be an intrusion of rapid eye movement sleep muscle atonia into
211                     SP arises from anomalous intrusion of REM processes into waking consciousness, in
212  deeper sediments in situ by replicating the intrusion of shallow groundwater through injection of 1,
213 is EEG slowing is linked to the pathological intrusion of sleep-like cortical dynamics within an awak
214         Several ecological changes allow the intrusion of sylvatic reservoirs and triatomines to the
215 of prior work yet simultaneously features an intrusion of unusual combinations.
216 iatric conditions that involve the automatic intrusion of unwanted memories.
217                  During this event, a strong intrusion of warm and moist air and an increase in downw
218                                          The intrusion of water into the pores of hydrophobic materia
219                                          The intrusion of water into this region is slowed down by th
220                 This shift is accompanied by intrusion of water into Trp-cage's interior and the hydr
221  were subsequently pressured to minimize the intrusion of wildlife onto their farm fields by removing
222 thened Siberian High, which favors southward intrusions of cold air to East Asia and thus causes seve
223 duced false recall, with significantly fewer intrusions of critical items.
224                 Helens that record pulsatory intrusions of new magma and volatiles into an existing l
225 also reveal previously unrecognized episodic intrusions of oxygen into the AMZ core, which could peri
226 g reveals that during the spring transition, intrusions of POC-rich surface water descend as coherent
227 echanism responsible for the recent poleward intrusions of southern species like Ehux.
228     Increased nuclear size and less frequent intrusions of the nuclear envelope into the nuclear lume
229 vations have suggested large, rapid seasonal intrusions of water into the upper atmosphere, boosting
230 ity are reflected in patterns of territorial intrusion, offspring paternity, avpr1a expression, and t
231 hwest Scotland we assess the impacts of salt intrusion on carbon accumulation rates.
232 rimental investigation of the effects of CO2 intrusion on the mobility of toxic ions in simplified eq
233                   There are two hot spots of intrusion, one in the Luzon Strait and the other off nor
234 rom northeast Taiwan, weakening the Kuroshio intrusion onto the East China Sea shelf.
235 ersistent contamination had occurred through intrusion or backflow.
236 mide (Br(-)) and iodide (I(-)) from seawater intrusion or high mineral content in the source waters.
237 e interpreted to be ancient vertical tabular intrusions or dikes formed by magmatism in combination w
238                     Once the pressure in the intrusion overcomes the effective tensile strength of th
239 ions including, but not limited to, pathogen intrusion, oxygen or nutrient starvation, proteotoxic an
240  to simulate the degradation, migration, and intrusion pathway of methane and benzene under different
241                          Surprisingly, this 'intrusion' pathway shares common features with axon guid
242 hydrothermal system below the craters, magma intrusion pathways and inherited faults.
243 ng the capillary pressure curve in a mercury intrusion porosimetry (MIP) measurement.
244      Comparisons have been made with mercury intrusion porosimetry and scanning electron microscopy i
245 niques over bulk measurements (e.g., mercury intrusion porosimetry).
246 rocarbon degradation, and increase the vapor intrusion potential for benzene.
247 -derived methane may also increase the vapor intrusion potential of toxic fuel hydrocarbons by stimul
248 iodegradation, thus increasing benzene vapor intrusion potential.
249 are reduced eightfold compared with CNT, the intrusion pressure is increased due to nanoscale confine
250                          Relative to the non-intrusion probe ERP, that to the intrusion probe was mor
251  to the non-intrusion probe ERP, that to the intrusion probe was more negative over frontal scalp (ap
252     The reaction time difference between the intrusion probe, a match of a to-be-rejected digit, and
253 match of a to-be-rejected digit, and the non-intrusion probe, which did not match any of the 4 digits
254                                              Intrusion/re-experiencing and avoidance subscale symptom
255 hat the barotropic nature of the subtropical intrusions restricts the tracers within the UT.
256  that current approaches to manage the vapor intrusion risk for conventional fuel released might need
257 mends as a screening tool in assessing vapor intrusion risks.
258 ation; fixational eye movements and saccadic intrusions (SIs) continuously change the position of gaz
259           We review the high pressure forced intrusion studies of water in hydrophobic microporous ma
260                                     Physical intrusions such as a square rod added into the 2D granul
261 c carbon concentrations during surface water intrusion support heterotrophy, which succumbs to autotr
262 indings on a measure of clinical post-trauma intrusion symptoms at 1 week, but not on other symptom c
263  traumatization and an increased severity of intrusion symptoms may be related to hypocortisolism.
264  to be negatively related to the severity of intrusion symptoms, the number of different lifetime tra
265 d that the better people were at suppressing intrusions, the more it reduced their emotional response
266 the existing link between soil-gas and vapor intrusion, this study also indicates that directional tr
267  River deltas are frequently facing salinity intrusion, thus challenging agricultural production in t
268                                        These intrusions transcend multiple scales in time and space,
269 on account of the high pressure shift of the intrusion transition.
270 However, male-female aggression decreased in intrusion trials compared to other interaction types, co
271 ecursory summit inflation, showing that this intrusion-unlike others-was not caused by the forceful i
272                                        Vapor intrusion (VI) by volatile organic compounds (VOCs) in t
273 nmental Protection Agency (U.S. EPA)'s vapor intrusion (VI) database, there appears to be a trend sho
274 ns related to the investigation of TCE vapor intrusion (VI) in two houses.
275                                        Vapor intrusion (VI) investigations often require sampling of
276 lene (TCE) in indoor air in support of vapor intrusion (VI) investigations.
277                             A complete vapor intrusion (VI) model, describing vapor entry of volatile
278                                        Vapor intrusion (VI) pathway assessment and data interpretatio
279                                Current vapor intrusion (VI) pathway assessment heavily weights concen
280  building-specific diagnostic tool for vapor intrusion (VI) pathway assessment which offers advantage
281 bility of estimating the risk posed by vapor intrusion (VI) processes have often looked to informatio
282  the emerging public health problem of vapor intrusion (VI).
283  In both cases, the initial and largest dike intrusion was followed by a series of smaller intrusions
284 ns was sufficient to determine whether vapor intrusion was the primary source of VOCs in indoor air a
285                                The number of intrusions was higher in ASA24 (P < 0.01).
286 portantly, participants who did not suppress intrusions well showed increased negative affect, sugges
287 edented snapshots of the traceless bacterial intrusion were obtained using cryo-electron microscopy.
288         Beyond seasonal time scales, the two intrusions were not synchronous during 1993-2013.
289  impacted sites several months following oil intrusion when the highest concentrations of oil were pr
290  available during retrieval and lead to more intrusions when retrieval fails.
291 show more frequent late spring stratospheric intrusions when the polar jet meanders towards the weste
292 ere more likely to run away from territorial intrusions when their group had a numeric advantage; eac
293 ich liquid layer, generating a localised gas intrusion, which initially grows through plastic deforma
294 lving crustal-scale nappe folds and magmatic intrusions, which are coeval with supradetachment basins
295 erior cortical atrophy showed large saccadic intrusions whose frequency correlated significantly with
296 astal legacy nuclear sites to inundation and intrusion with oxygenated seawater.
297 matites are shallow, coarse-grained magmatic intrusions with crystals occasionally approaching meters
298 ion and aperture measurements from 519 sheet intrusions within Volcan Taburiente (La Palma, Canary Is
299                                        Vapor intrusion would also be exacerbated if methanogenic acti
300 bination of mechanical deformation and magma intrusion, yet the spatial and temporal scales over whic

 
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