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1 ulic retention time of the lake, followed by volatilization.
2 plicating combustive formation versus simple volatilization.
3 annot correctly cover the moisture effect on volatilization.
4 ur/Se metabolism yet was found to mediate Se volatilization.
5 quid extraction or chemical/heat-facilitated volatilization.
6  significantly increased Se accumulation and volatilization.
7  almost complete loss in its capacity for Se volatilization.
8 natures of limited partial melting or impact volatilization.
9  the rate of metabolic loss, and the rate of volatilization.
10 aerobic disposal intended to promote arsenic volatilization.
11 d microbial mercury reduction and subsequent volatilization.
12 the lakes were acting as sources of PCMs via volatilization.
13 quids, which have an air-side limitation for volatilization.
14  from 18 to 94 for 2,4,6-TBA, indicating net volatilization.
15 SM at the plot scale were degradation (71%), volatilization (5%), leaching (8%) and runoff (3%), whil
16 . putida showed high arsenic methylation and volatilization activity.
17  number of special experiments precluded IMI volatilization and contact or oral action of IMI upon ex
18 of oxygen concentrations due to simultaneous volatilization and oxidation.
19 ariations, suggesting a seasonal cycle of Se volatilization and recondensation.
20 ns tested, the most effective in terms of Se volatilization and Se removal from the water column was
21 n suggests that aerosols are not a result of volatilization and subsequent nucleation of ABS or direc
22                                    Pesticide volatilization and vapor drift can have adverse effects
23 redictions showed flushing promoted chemical volatilization, and contaminants did not appreciably sor
24 ntributed by advection, molecular diffusion, volatilization, and flow regime within the PAS, finding
25 n the atmosphere as a result of spray drift, volatilization, and suspension of coated soils.
26 microenvironmental transport and deposition, volatilization, and transfer of pesticide when passenger
27 mistry in China we found that deposition and volatilization are key factors controlling distribution
28         Because of issues such as adsorption/volatilization artifacts, it faces obstacles in measurin
29 d by temperature-dependent processes such as volatilization at warm temperatures.
30  emitted during transient cycles showed that volatilization began at around 40 degrees C, with the ma
31                  With use of TGA and XRD the volatilization behavior of Mo was studied.
32  to enhance rates of contaminant removal via volatilization, but the magnitude of different volatiliz
33                                           Se volatilization by Indian mustard accounted for only 0.7%
34                                      Arsenic volatilization can be mediated by the enzyme arsenite S-
35 e can be emitted, clearly demonstrating that volatilization can occur via processes unrelated to sunl
36                                              Volatilization causes changes in the isotopic compositio
37 of raw dairy manure slurry decreased ammonia volatilization compared with surface application.
38 is of arsM expression, revealed that arsenic volatilization correlated with methanogenic activity.
39 em and to predict 24-h cumulative percentage volatilization (CPV(24h)) losses.
40 cools during microwave-assisted evaporation, volatilization due to overheating at dryness is minimize
41  corresponds to the expected increase in PCB volatilization due to the effect of temperature on vapor
42 artz ampules to minimize the loss of Re from volatilization during melting at 1000 degrees C.
43 d p,p'-dichlorodiphenyldichloroethane), with volatilization during the day and deposition in the nigh
44 ace analysis, where losses of analyte due to volatilization during the evaporation process are minimi
45 ir model allowed a better description of the volatilization dynamics on a diurnal cycle (increasing e
46                                   The larger volatilization estimate at Travis was expected because o
47            In the current study, open-system volatilization experiments (focusing thereby on kinetic/
48                     Fractionation of CFCs in volatilization experiments from pure-phase CFC-11 and CF
49                                     Based on volatilization experiments, emission of DMS to the atmos
50 uced an increase of 8% in the averaged total volatilization flux, however this effect can be neutrali
51                                              Volatilization fluxes of HHCB ranged from 11 +/- 6 to 34
52  technique provides an estimate of potential volatilization fluxes without relying on enclosure-based
53  mass spectrometers typically employ analyte volatilization followed by electron ionization or chemic
54  is, the one-dimensional model for pesticide volatilization following application on bare soil (Volt'
55      Water-air fugacity ratios indicated net volatilization (FR > 1.0) or near equilibrium (FR not si
56 us close to air-surface equilibrium to a net volatilization from Antarctic reservoirs.
57                                    Pesticide volatilization from bare soil exhibits usually a diurnal
58 Cs), only hypothetical emissions via passive volatilization from e-waste were considered whereas for
59  from DMSeP because DMSeP was the rate of Se volatilization from faster than from SeMet and SeMet (bu
60                                      Ammonia volatilization from incubated soil ranged from 140 g kg(
61                      Trichloroethylene (TCE) volatilization from leaves, trunk, and soil was measured
62 ovel genes whose products are involved in Se volatilization from plants, a broccoli (Brassica olerace
63 d in the literature for these compounds, for volatilization from pure liquids.
64   To determine the rate-limiting steps in Se volatilization from selenate and selenite, time- and con
65                     Our data suggest that Se volatilization from selenate is limited by the rate of s
66                                           Se volatilization from selenite may be limited by selenite
67 Bs in Zurich are probably released mainly by volatilization from sources that are directly exposed to
68  the basis of the scaled field measurements, volatilization from the leaves and soil may play a signi
69 eric deposition has become negligible, while volatilization from the water surface is still a major r
70 inhibitor product Limus((R)) to decrease NH3 volatilization from urea applied to maize.
71 cids, however, have relatively high KAWs and volatilization from water has been demonstrated.
72 and the output flows due to sediment burial, volatilization from water to air, and transport to Lake
73  of vapor-phase samples, two modes of sample volatilization (heated capillary and thermal desorption
74 enol C6H4N2O5) measured with a micro-orifice volatilization impactor (MOVI) high-resolution chemical
75             BoCOQ5-2 was found to promote Se volatilization in both bacteria and transgenic Arabidops
76  The model captures the general trend of the volatilization in different humidity scenarios.
77 xhibits strong isotopic fractionation during volatilization in planetary rocks, but is hardly fractio
78 pplied was lost (presumably because of NH(3) volatilization) in contrast to far greater losses report
79 elenite-supplied plants, Se accumulation and volatilization increased linearly with external Se conce
80 proposed to account for mass removal and for volatilization into the headspace.
81         In Central China the rate of soil Se volatilization is similar to that of Se deposition, sugg
82 ilizer granules are lost continuously due to volatilization, leaching, denitrification, and surface r
83 Sorption to sludge and biodegradation and/or volatilization losses are important factors that affect
84  and the conditions under which the greatest volatilization losses exist were easily identified using
85                                    Pesticide volatilization losses from soil, calculated with the new
86 curately model literature-reported pesticide volatilization losses from soils.
87                    Plant Se accumulation and volatilization may be applied in crop biofortification a
88 f the lakes' coastal boundary zone suggested volatilization may be responsible for the loss of 64-213
89 latilization, but the magnitude of different volatilization mechanisms, and the relationship between
90 itudes of gas-phase and transpiration-driven volatilization mechanisms.
91 involved in sulfur/selenium assimilation and volatilization, methylation of selenocysteine, and conve
92 quation and a previously described pesticide volatilization model, were compared to previous results
93 ndence on the hydration status into a simple volatilization model.
94 fitting the experimental measurements with a volatilization model.
95                         However, established volatilization models do not explicitly consider the hyd
96 y conditions can be integrated into existing volatilization models that already work well for humid c
97  experimental conditions, and this is due to volatilization, not oxidation.
98                              The largest PAH volatilizations occurred at the sites in Alabama and Mis
99                              The largest PAH volatilizations occurred at the sites in Alabama and Mis
100 dspace analysis is used widely and relies on volatilization of analytes into the headspace above the
101 rs) to near-shore Lake Ontario compared with volatilization of approximately 6 kg y(-1) of mainly lig
102 essed, which was ascribed to photo bleaching/volatilization of BrC and/or due to rising boundary laye
103 % of bromine fluxes from previously reported volatilization of bromomethanes and bromochloromethanes.
104 urements, and used to predict plant-mediated volatilization of common VOCs as well as quantify the co
105  per thousand and -1.9 per thousand) and for volatilization of compounds dissolved in water (-4.4 per
106 ndosulfan (-0.02 to -33 ng/m(2)/day) and net volatilization of heptachlor, aldrin, trans-chlordane, a
107 promising technique for gentle and efficient volatilization of intact organic molecules from surfaces
108                                              Volatilization of Me2AsH and TMAs(III) from contaminated
109 e of unrecorded (contra-band) production and volatilization of mercury during processing and recovery
110     The huge isotopic spread is explained by volatilization of metal halides during basalt eruption--
111  Craig-Gordon isotope model is valid for the volatilization of nonpolar organic liquids with air-side
112 narios, such as isotope fractionation during volatilization of organics from open water surfaces, hav
113 e and Eagle Harbor sites generally displayed volatilization of PBDEs into the atmosphere, mainly BDE-
114 ction of the tropical Atlantic suggested net volatilization of PCBs to the atmosphere.
115                            Results show that volatilization of pesticides from soil largely exceeded
116                                              Volatilization of pesticides from the bare soil surface
117                                The extent of volatilization of PFCAs in the environment will depend o
118          We suggest that both deposition and volatilization of Se could play a key role in Se balance
119 oxic forms of Se by promoting the biological volatilization of Se.
120 rate-limiting steps for the assimilation and volatilization of selenate to dimethyl selenide (DMSe):
121                                   Biological volatilization of selenium, Se, in a contaminated area i
122 can produce both the hot, CO2-rich fluid (by volatilization of surface carbonates or other CO2 source
123 k for evaluating the potential importance of volatilization of TCE and similar compounds at phytoreme
124 porally and spatially to estimate the annual volatilization of TCE at the Travis (0.82 +/- 0.51 kg/yr
125 phase interface causes local heating and the volatilization of the analyte species.
126 que is directly on-line and does not require volatilization of the eluent.
127                 The results demonstrate that volatilization of the four halogenated compounds from wa
128 EMPI covers a larger m/z range than external volatilization of the sample prior to introduction to th
129 n methods poses recovery problems because of volatilization of the target analyte as the chloride or
130 a 1-3 orders of magnitude enhancement in the volatilization of these analytes and shorter fiber expos
131  assessed by comparing with two data sets on volatilization of trifluralin applied to bare soil.
132  non-irradiated fuel, suggesting non-uniform volatilization of U from melted fuels with different lev
133 rk that transpiration is the main driver for volatilization of VOCs, but also demonstrate that vapor-
134 to that of Se deposition, suggesting that Se volatilization offsets it's deposition, resulting in neg
135 om bronchial epithelial cells was lost after volatilization or lyophilization treatment.
136 studies have focused mostly on pure compound volatilization or on compounds dissolved in organic liqu
137 direct use has several disadvantages such as volatilization or oxidation.
138 in, PBDEs may become bioaccessible following volatilization or polymer deterioration.
139 microbially mediated mercury methylation and volatilization pathways in polar marine environments.
140 ll as quantify the contribution of different volatilization pathways.
141                                              Volatilization PCB fluxes were calculated using the modi
142 the mechanistically based description of the volatilization process under dry conditions.
143 es over the Indian and Southern Ocean, while volatilization processes and additional atmospheric emis
144 ce the availability of Hg for methylation or volatilization processes and has substantial potential t
145 halene was the PAH with the highest observed volatilization rate of 52000 ng/m(2) day(-1) in June 201
146 hthene was the PAH with the highest observed volatilization rate of 6800 ng/m(2)/day in September 201
147                               A study of the volatilization rate of the nerve agent VX (O-ethyl S-2-(
148 anic liquids with air-side limitation of the volatilization rate.
149 ion mechanisms, and the relationship between volatilization rates and contaminant physiochemical prop
150                                           Se-volatilization rates were 2- to 3-fold higher from plant
151 h external Se concentration up to 20 &mgr;M; volatilization rates were also linearly correlated with
152 nium accumulation and up to threefold faster volatilization rates.
153 ates using the two-film model suggested that volatilization removes 980-1360 kg of total BAs from Bot
154 the environment through runoff, leaching and volatilization, resulting in three-dimensional (3D) poll
155                Four approaches for pesticide volatilization screening based on Fick's Law were invest
156 a pyrolysis temperature of 1300 degrees C, a volatilization temperature of 2300 degrees C and Mg as a
157 m N retention and partitioned more losses to volatilization than estimated from observed N budgets of
158 vironmental fate of PFAMs is suggested to be volatilization to the atmosphere followed by oxidation b
159 tigate potential transfer up the food chain, volatilization to the atmosphere, as well as direct phyt
160 within 72 h, with up to 61% being removed by volatilization to the atmosphere.
161 r to simulate on line in situ derivatization-volatilization-transfer steps.
162  plant selenium accumulation, tolerance, and volatilization: upregulation of genes involved in sulfur
163 aluate the role of methanogenesis in arsenic volatilization using methanogen inhibitors.
164    A numerical model for vegetation-mediated volatilization was developed, calibrated with tracer mea
165 throughout leaf development, and monoterpene volatilization was found to occur at a very low rate, wh
166                                      Arsenic volatilization was highest in methanogenic mesocosms, bu
167                                              Volatilization was negligible (<0.04%).
168                                              Volatilization was primarily through the leaf (0.34 +/-
169 on-dependent kinetics of Se accumulation and volatilization were studied in Indian mustard (Brassica
170 o the shoot, away from the root, the site of volatilization, whereas only approximately 10% of the se
171                        Biologically based Se volatilization, which converts Se into volatile compound
172  type and was defective in elemental mercury volatilization, while the merR mutant was mercury resist
173 e to incomplete solubilization and potential volatilization, whilst other methods may require large,
174  which combines direct particle sampling and volatilization with online chemical ionization mass spec

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