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1 mensional explicit mixing parcel model (EMPM-Chem).
2 n atmospheric chemical transport model (GEOS-Chem).
3 n atmospheric chemical transport model (GEOS-Chem).
4 arch and Foresting model with Chemistry (WRF-Chem).
5                     Carter-Fenk and Herbert (Chem.
6 tric electrocatalysis' by Jonas Rein et al., Chem.
7 origami nano-mechanics' by Jiahao Ji et al., Chem.
8 l review' by Ramkrishna Das Adhikari et al., Chem.
9 iation applications' by Saba Daliran et al., Chem.
10 hemical reactions' by Yorrick Boeije et al., Chem.
11 to-thermal catalysis' by Diego Mateo et al., Chem.
12 isation catalysts' by Eszter Fazekas et al., Chem.
13 or polymer materials' by Yinjun Chen et al., Chem.
14 alization reactions' by Saba Daliran et al., Chem.
15 ysical understanding' by Guancen Liu et al., Chem.
16  olefins production' by Matteo Monai et al., Chem.
17 ir utility' by Kaustav Bhattacharjee et al., Chem.
18 and future directions' by Bee Ha Gan et al., Chem.
19 ling challenges' by Antonio Vilanova et al., Chem.
20 tial applications' by Romy Ettlinger et al., Chem.
21 ion for MOFtronics' by Mingchao Wang et al., Chem.
22 echanistic aspects' by Jagrit Grover et al., Chem.
23 he atmospheric chemical transport model GEOS-Chem.
24  within chemistry' by Manuel Hertzog et al., Chem.
25 )(dark)/IC(50)(light)) [Rubbiani, R. et al., Chem.
26 e and modulated emotional behavior [Mock Nat Chem.
27 an update to our first review of this topic (Chem.
28 e excellent treatment by Dugave and Demange (Chem.
29 vey of this broad field in Chemical Reviews (Chem.
30 ew approach reported by Struntz et al. (Cell Chem.
31 fur-based batteries' by Ralf Steudel et al., Chem.
32 nanomaterials' by Sayak Subhra Panda et al., Chem.
33                              Antonio et al., Chem.
34 cial receptors' by Stefano Tommasone et al., Chem.
35  catalysis' by Daniel Janssen-Muller et al., Chem.
36  reactors' by Juan Carlos Colmenares et al., Chem.
37 etection using SERS' by Stacey Laing et al., Chem.
38 and chemical sensors' by Ivo Stassen et al., Chem.
39 f drug-like molecules' by Tim Cernak et al., Chem.
40 atile photochrome' by Luuk Kortekaas et al., Chem.
41 e global-scale chemical transport model GEOS-Chem.
42 ions using the chemical transport model GEOS-Chem.
43  based on the SMR, and 60 ppbv, based on WRF-Chem.
44  constant catalyzed by wild type GGTase I (k(chem) = 0.18 +/- 0.02 s(-1)) is not dependent on Mg(II),
45 cs software (NAMD (Phillips et al., J Comput Chem 26(16):1781-802, 2005), VMD (Humphrey et al., J Mol
46 ng (AutoDock Vina (Trott and Olson, J Comput Chem 31(2):455-61, 2010)).
47                                              Chem-8dK showed in vivo efficacy against Pseudomonas aer
48                                              Chem-8dK with a d-lysine replacement in its middle (eigh
49    Finally, we incorporate results into GEOS-Chem, a global chemical transport model, to compute the
50                               We used CAMELS-chem, a new data set with DO concentrations from 236 min
51                                         GEOS-Chem, a widely used atmospheric chemical transport model
52                             We used the GEOS-Chem adjoint model and investigated the changing sensiti
53                                         GEOS-Chem also captures variability in observed concentration
54  Using two atmospheric chemistry models, CAM-chem and GEOS-Chem, our findings reveal that anthropogen
55                                         GEOS-Chem and GRAHM, two complex numerical mercury models, pr
56 g two chemical transport models (CTMs): GEOS-Chem and the Community Multiscale Air Quality (CMAQ) and
57 orecasting model coupled with Chemistry (WRF-Chem) and FINNv1.5 fire emission inventory.
58 the adjacent G36 has very small effects on k(chem) and K(d) for glutamine.
59 mated using a chemical transport model (GEOS-Chem) and satellite aerosol observations.
60 sition from a chemical transport model (GEOS-Chem) and satellite observations of aerosol optical dept
61 odel coupled with Chemistry version 3.5 (WRF-Chem)-and three emission scenarios, we assessed the impa
62                           This "cytokine med-chem" approach, rooted in principles of induced proximit
63 satellite data, and a mechanistic model [WRF-Chem]), approaches to model building (e.g., one model fo
64 ons of both C(3)H(8) and C(2)H(6) using GEOS-Chem are in reasonable agreement with ATom and HIPPO obs
65 -dimensional chemistry-transport model (GEOS-Chem) are used to relate the OMI NO2 columns to ground-l
66 ospheric Emission Spectrometer with the GEOS-Chem atmospheric model to better quantify the HCOOH sour
67 IS MAIAC) was combined with simulation (GEOS-Chem) based upon their relative uncertainties as determi
68 uding camouflage soldier fabrics/apparel for chem-bio warfare, color morphing soft robots, rewritable
69  and biocatalytic-chemical-biocatalytic (bio-chem-bio) cascades starting from commercially available
70 eved the same penetration in waveguide-based chem/bio sensing compared to related sensing schemes ope
71 nics facilitating next-generation label-free chem/bio sensor and assay platforms.
72 ing schemes will readily complement existing chem/bio sensor technologies in applications ranging fro
73 his review, current advances in mid-infrared chem/bio sensor technology will be highlighted and contr
74 s for substantial increase in sensitivity of chem/bio sensors.
75 hich inspires us to develop highly selective chem/(bio)sensors for in vivo analysis by precisely engi
76 ents a great challenge in the development of chem/(bio)sensors that are capable of directly and selec
77 f U35 in the tRNA anticodon loop decreases k(chem) by 30-fold and weakens glutamine binding affinity
78 pth (AOD) and chemical transport model (GEOS-Chem) calculations of the relationship between AOD and P
79                                         GEOS-Chem captures observed seasonal trends with no statistic
80   In contrast, the design of the ELIXYS FLEX/CHEM cassette-based synthesizer supports higher temperat
81                                     The GEOS-Chem chemical transport model (CTM) is used to relate ea
82 based smoke plume estimates and (2) the GEOS-Chem chemical transport model (CTM), we identify recent
83 different sensitivity regimes using the GEOS-Chem chemical transport model and apply the method to sa
84    We implement this mechanism into the GEOS-Chem chemical transport model and investigate its impact
85                    Simulations with the GEOS-Chem chemical transport model show large resulting incre
86 emble of aircraft measurements with the GEOS-Chem chemical transport model to constrain present-day N
87                             We used the geos-chem chemical transport model to evaluate local impacts
88                             We used the GEOS-Chem chemical transport model to evaluate the potential
89 ion system based on modern PPLs and the GEOS-Chem chemical transport model, simulating atmospheric CO
90                Using the adjoint of the GEOS-Chem chemical transport model, we calculated sensitiviti
91 in the Goddard Earth Observing System (GEOS)-Chem chemical transport model, we find that global surfa
92 ion of HMS chemistry in the nested-grid GEOS-Chem chemical transport model, whose simulations provide
93  converted to annual averages using the GEOS-Chem chemical transport model.
94 olecular weight fragments that engage RNA or Chem-CLIP fragment mapping (Chem-CLIP-Frag-Map).
95             Transcriptome-wide mapping using Chem-CLIP revealed a highly selective interaction betwee
96                 Target profiling studies via Chem-CLIP showed that 2 bound selectively to the miR-515
97 al cross-linking and isolation by pull-down (Chem-CLIP) to identify and map the binding sites of low
98 al Cross-Linking and Isolation by Pull Down (Chem-CLIP) to study the cellular selectivity and the on-
99 al Cross-Linking and Isolation by Pull-Down (Chem-CLIP), a small-molecule RNA target validation appro
100                                          The Chem-CLIP-Frag-Map approach should prove general to expe
101 at engage RNA or Chem-CLIP fragment mapping (Chem-CLIP-Frag-Map).
102                                        Using Chem-CLIP-Frag-Map, we identified several fragments that
103 bind to r(CGG)(exp) in cellulo as shown with Chem-CLIP-Map, an approach to map small molecule binding
104 n by Pull-down combined with NGS Sequencing (Chem-CLIP-seq) data identified collagen type XV alpha 1
105 ch and Forecasting model with Chemistry (WRF/Chem) coupled with the Model of Emissions of Gases and A
106 ssability with dose-sparing chemical action, Chem-CRISPR/dCas13(FCPF) establishes a proximity-induced
107 stem for epigenome editing, we now introduce Chem-CRISPR/dCas13(FCPF), a modular platform that covale
108                     Building on our previous Chem-CRISPR/dCas9(FCPF) system for epigenome editing, we
109 d an Eulerian chemical transport model (GEOS-Chem CTM) to develop top-down constraints on U.S. CO sou
110   The configurations tested are (1) the GEOS-Chem default configuration, which uses instantaneous equ
111                             Reconciling GEOS-Chem deposition velocities with observations resulted in
112    We describe here the use of DNA-encoded X-Chem (DEX) screening, combined with selection of appropr
113                                         GEOS-Chem estimates mean atmospheric lifetimes of <1 day for
114  reactions of porphyrin-Compound II species (Chem.-Eur.
115 the chemical step for tRNA aminoacylation (k(chem)) exceeds the steady-state rate by nearly 10-fold.
116 ce of the polymer bridge like a conventional Chem-FET.
117 orecasting model coupled with Chemistry (WRF-Chem) for the first time, aiming to improve fine particu
118 atmospheric chemical transport modeling (WRF-Chem) for the post-monsoon to winter transition to unrav
119         Chemical transformation constants (k(chem)) for the mutant enzymes were lower by 1.1-6.0-fold
120                                      The CAM-Chem global chemical transport model reproduced annual a
121 le and composition information from the GEOS-Chem global chemical transport model.
122     Impairment of gephyrin assembly prevents chem-iLTP and, in parallel, blocks the accumulation and
123                                              Chem-iLTP expression requires synaptic recruitment of th
124 nd GABA(A)R similar to those observed during chem-iLTP in cultures were found in the rat visual corte
125 nstrate that during chemically induced iLTP (chem-iLTP), GABA(A)Rs are immobilized and confined at sy
126  use a global chemical transport model (GEOS-Chem) in its high-performance configuration (GCHP) for h
127  in steady-state kinetic analysis, and the k(chem) in single turnover kinetic analysis.
128 1A) or aspartate (Kbeta311D) decreases the k(chem) in the absence of magnesium 9-41-fold without sign
129 bal scale, the chemical transport model GEOS-Chem is used to identify regions characterized by lower
130 of overall reaction rates as a function of k(chem), k(inact), K(i), and V(r), which was validated wit
131 g the pre-steady state efficiency constant k(chem)/K(D)(DNA).
132 rence between huPNP and PfPNP supports the k(chem)/kcat binding argument for transition state analogu
133 activity against human red blood cells among Chem-KVL analogues and maintained high antimicrobial pro
134 rd microorganisms, its 14-mer tandem repeat (Chem-KVL) was highly active against different bacteria i
135 ell selectivity and proteolytic stability to Chem-KVL.
136 ived using a hybrid chemical transport (Geos-Chem)/land-use regression model and natural log transfor
137 cific antibodies, we found that induction of chem-LTD produces a persistent dephosphorylation of the
138                      Chemically induced LTD (Chem-LTD) and homosynaptic LTD are mutually occluding, s
139                                        Query Chem makes it possible to search the Web for information
140                              Here we present Chem-map for in situ mapping of small molecules that int
141                               We demonstrate Chem-map for three distinct drug-binding modalities as f
142 xorubicin in human leukemia cells; using the Chem-map of doxorubicin in cells exposed to the histone
143                         In situ mapping with Chem-map of small-molecule interactions with DNA and chr
144                                              Chem(-/-) mice are leaner than wild-type mice but gain m
145                                              Chem(-/-) mice develop insulin resistance when on a high
146             Compared to wild-type mice, male Chem(-/-) mice have decreased oxygen consumption, CO(2)
147            Additionally, body temperature of Chem(-/-) mice is lower than that of wild-type mice.
148                      Brown adipose depots in Chem(-/-) mice weigh more than in wild-type mice, but wi
149                          Chemerin-deficient (Chem(-/-) ) mice were compared to wild-type mice when fe
150 t demonstrates the potential importance of a Chem-MIF effect in a PSN where plasma zones develop.
151 ver, these potential chemical MIF reactions (Chem-MIFs) are not identified in conditions close to the
152                                      The WRF-Chem model also indicates an important role for peroxyac
153 end differences were predicted using the WRF-Chem model and evaluated using satellite and aircraft ob
154                              We use the GEOS-Chem model coupled to meteorology from a general circula
155 aking aspen, using simulations with the GEOS-Chem model for 2010.
156 , we exploit recent developments to the GEOS-Chem model in its high-performance implementation to con
157         We embed these emissions in the GEOS-Chem model nested over the African continent to simulate
158   For this modelling study, we used the GEOS-Chem model nested over the UK to simulate ambient PM(2.5
159  measurements, AEROSNOW retrievals, and GEOS-Chem model simulations.
160 le with vertical shape factors from the GEOS-Chem model that capture the contrasting shapes observed
161 sions projections for 2050, and use the GEOS-Chem model to calculate global mercury deposition.
162 hain in Africa that we implement in the GEOS-Chem model to quantify the contribution of charcoal to s
163                       We also apply the EMPM-Chem model to simulate how IEPOX-SOA formation evolves i
164                    To do so, we use the GEOS-Chem model with focus on the eastern United States (US)
165 ned on the parameters simulated from the WRF-Chem model, and it suggests that six predictive paramete
166 sults from other studies in Nevada, and GEOS-Chem modeling results point toward a free troposphere co
167 ospheric chemistry models, CAM-chem and GEOS-Chem, our findings reveal that anthropogenic primary OA
168 stigation of intrinsic warhead reactivity (k(chem)), rate of covalent bond formation and proximity (k
169                        Simulations with GEOS-Chem reproduce OM trends and suggest that decreases acro
170                                        Query Chem's search results can retrieve many interesting stru
171                                       A GEOS-Chem sensitivity simulation indicates that HCHO levels w
172 ovide detailed protocols for carrying out TT(chem)-seq and DRB/TT(chem)-seq, including computational
173                           We describe how TT(chem)-seq can be used in combination with transient inhi
174 ols for carrying out TT(chem)-seq and DRB/TT(chem)-seq, including computational analysis.
175 for RNA fragmentation that we refer to as TT(chem)-seq.
176 on rates in vivo, a technique we call DRB/TT(chem)-seq.
177 unoprecipitation followed by sequencing) and Chem-seq (chemical affinity capture and massively parall
178                                  We show how Chem-seq can be combined with ChIP-seq to gain unique in
179 pture and massively parallel DNA sequencing (Chem-seq) to identify the sites bound by small chemical
180 IP-sequencing-like approach, referred to as "Chem-seq," we were next able to efficiently map the geno
181 rvised learning framework, we treat the GEOS-Chem simulated data set as the target, with predictors d
182                                A nested GEOS-Chem simulation for the ELA region produced a dry/wet de
183                                       A GEOS-Chem simulation reveals that secondary inorganic aerosol
184                                 We used GEOS-Chem simulations (2x2.5 masculine grid resolution) to es
185   In contrast, AERONET observations and GEOS-Chem simulations consistently capture Arctic Haze in spr
186                             Four 1-month WRF-Chem simulations for August 2007, with and without fire
187 tthew are analyzed using high-resolution WRF-Chem simulations.
188 otein kinase inhibitors published in J. Med. Chem. since 1993 can be modeled using a template extract
189 ical review, an update of our 2007 review in Chem. Soc. Rev., we focus on the "click" reactions that
190 istry, and chemistry students (from here bio/chem students) completed a minor in computer science.
191                                  We use GEOS-Chem to estimate that the largest contribution of DICE-A
192     We use the chemical transport model GEOS-Chem to evaluate the hypothesis that atmospheric polycyc
193 use the global chemical transport model GEOS-Chem to explore possible scenarios representative of spe
194 the global 3-D chemical transport model GEOS-Chem to simulate long-range atmospheric transport of pol
195                                We apply EMPM-Chem to simulate turbulence and droplet-resolved IEPOX-S
196  a global 3-D chemical transport model (GEOS-Chem) to identify the sources and processes that control
197 orecasting model coupled with Chemistry (WRF-Chem) to produce a 72-h forecast daily in a dynamical do
198                             We used the GEOS-chem transport model to estimate address-specific, one-y
199                    Model simulations in GEOS-Chem, updated with the chemistry described herein, highl
200 by the global chemical transport model, GEOS-Chem v13.0.0, using a scaled C(2)H(6) spatial proxy.
201 nimal changes are seen in Kd, kcat/KM, and k(chem) values.
202                                          CAM-Chem was adapted to include a two-way sea-air flux param
203 D atmospheric chemical transport model (GEOS-Chem), we quantify global and regional NF(3) emission fr
204 ate molecular organometallic chemistry (SMOM-chem), well-defined isobutane and cyclohexane sigma-comp
205 search Forecasting Model with Chemistry (WRF-Chem) which indicates transport to Reno from large fires
206 shore from the Western US associated in GEOS-Chem with elevated ozone in the lower free troposphere.
207 asting Model with atmospheric chemistry (WRF-Chem) with emissions of volatile organic compounds (VOCs
208  The method, an extension to the ChemDiverse/Chem-X software (Oxford Molecular, Oxford, England), has

 
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