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ESEEM spectra

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Comparison of experimental and simulated ESEEM spectra at 25 K at a rotation angle of 76° (𝛉 = 76.1° and φ = 45.4°). The top simulation assumes a single set of two inequivalent H2O protons while the lower simulation includes two sets for each of the two inequivalent H2O protons.
Published: 01 January 2010
Fig. 6. Comparison of experimental and simulated ESEEM spectra at 25 K at a rotation angle of 76° (𝛉 = 76.1° and φ = 45.4°). The top simulation assumes a single set of two inequivalent H 2 O protons while the lower simulation includes two sets for each of the two inequivalent H 2 O protons.
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Stacked plots of the 29Si portion of the experimental and simulated three-pulse ESEEM spectra as a function of rotation angles. Intensity in the vertical axis unlabelled (arbitrary unit).
Published: 01 January 2010
Fig. 5. Stacked plots of the 29 Si portion of the experimental and simulated three-pulse ESEEM spectra as a function of rotation angles. Intensity in the vertical axis unlabelled (arbitrary unit).
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Stacked plots of the 1H portion of the experimental and simulated three-pulse ESEEM spectra as a function of rotation angles. Intensity in the vertical axis unlabelled (arbitrary unit).
Published: 01 January 2010
Fig. 7. Stacked plots of the 1 H portion of the experimental and simulated three-pulse ESEEM spectra as a function of rotation angles. Intensity in the vertical axis unlabelled (arbitrary unit).
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Stacked plots of the 39K portion of the experimental and simulated three-pulse ESEEM spectra as a function of rotation angles. Note that intensity in the vertical axis (unlabelled, arbitrary units) has been reduced five times (relative to those in Fig. 5 and 7) to show the strong 39K spectra.
Published: 01 January 2010
Fig. 8. Stacked plots of the 39 K portion of the experimental and simulated three-pulse ESEEM spectra as a function of rotation angles. Note that intensity in the vertical axis (unlabelled, arbitrary units) has been reduced five times (relative to those in Fig. 5 and 7 ) to show the strong 39
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Stacked plots of the 11B and 10B portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra of Centers I and II in danburite as a function of rotation angles. Intensity in the vertical axis unlabelled (arbitrary unit).
Published: 01 March 2014
Fig. 7 Stacked plots of the 11 B and 10 B portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra of Centers I and II in danburite as a function of rotation angles. Intensity in the vertical axis unlabelled (arbitrary unit).
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Stacked plots of the 1H portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra as a function of rotation angles. Spectral simulations included eight H nuclei. Intensity in the vertical axis unlabeled (arbitrary unit; modified from Mao et al. 2010b).
Published: 01 January 2014
Figure 12 Stacked plots of the 1 H portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra as a function of rotation angles. Spectral simulations included eight H nuclei. Intensity in the vertical axis unlabeled (arbitrary unit; modified from Mao et al. 2010b ).
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Stacked plots of the 29Si portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra of the O− center in hydroxylapophyllite as a function of rotation angles. Spectral simulations included 2 Si nuclei. Intensity in the vertical axis unlabeled (arbitrary unit; modified from Mao et al. 2010b).
Published: 01 January 2014
Figure 11 Stacked plots of the 29 Si portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra of the O − center in hydroxylapophyllite as a function of rotation angles. Spectral simulations included 2 Si nuclei. Intensity in the vertical axis unlabeled (arbitrary
Image
Stacked plots of the 39K portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra as a function of rotation angles. Note that intensity in the vertical axis (unlabeled, arbitrary units) has been reduced five times (relative to those in Figs. 11 and 12) to show the strong 39K spectra. Spectral simulations included four 39K nuclei (modified from Mao et al. 2010b).
Published: 01 January 2014
Figure 13 Stacked plots of the 39 K portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra as a function of rotation angles. Note that intensity in the vertical axis (unlabeled, arbitrary units) has been reduced five times (relative to those in Figs. 11 and 12
Journal Article
Published: 01 January 2010
European Journal of Mineralogy (2010) 22 (1): 89–102.
...Fig. 6. Comparison of experimental and simulated ESEEM spectra at 25 K at a rotation angle of 76° (𝛉 = 76.1° and φ = 45.4°). The top simulation assumes a single set of two inequivalent H 2 O protons while the lower simulation includes two sets for each of the two inequivalent H 2 O protons. ...
FIGURES
First thumbnail for: Radiation-induced defects in apophyllites. II. An ...
Second thumbnail for: Radiation-induced defects in apophyllites. II. An ...
Third thumbnail for: Radiation-induced defects in apophyllites. II. An ...
Journal Article
Published: 01 March 2014
European Journal of Mineralogy (2014) 26 (1): 113–125.
...Fig. 7 Stacked plots of the 11 B and 10 B portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra of Centers I and II in danburite as a function of rotation angles. Intensity in the vertical axis unlabelled (arbitrary unit). ...
FIGURES
First thumbnail for: Arsenic speciation in danburite (CaB 2 Si 2 O 8 ):...
Second thumbnail for: Arsenic speciation in danburite (CaB 2 Si 2 O 8 ):...
Third thumbnail for: Arsenic speciation in danburite (CaB 2 Si 2 O 8 ):...
Journal Article
Published: 01 January 2014
Reviews in Mineralogy and Geochemistry (2014) 78 (1): 655–690.
...Figure 12 Stacked plots of the 1 H portion of the experimental and simulated three-pulse, Fourier-transform ESEEM spectra as a function of rotation angles. Spectral simulations included eight H nuclei. Intensity in the vertical axis unlabeled (arbitrary unit; modified from Mao et al. 2010b ). ...
FIGURES
First thumbnail for: Electron Paramagnetic Resonance Spectroscopy: Basi...
Second thumbnail for: Electron Paramagnetic Resonance Spectroscopy: Basi...
Third thumbnail for: Electron Paramagnetic Resonance Spectroscopy: Basi...
Journal Article
Published: 01 November 2002
European Journal of Mineralogy (2002) 14 (6): 1053–1060.
... of the synthetic analogue of tetrahedrite (Cu 12 Sb 4 S 13 ), Di Benedetto et al. (unpublished data) performed both EEPR and ESEEM experiments to facilitate the interpretation of cw-EPR spectra. The decay of the echo signal ( Fig. 5a ) is due to two different spin-spin and spin-lattice mechanisms. The difference...
FIGURES
First thumbnail for: EPR and magnetic investigations on sulphides and s...
Second thumbnail for: EPR and magnetic investigations on sulphides and s...
Third thumbnail for: EPR and magnetic investigations on sulphides and s...
Journal Article
Published: 01 June 2010
European Journal of Mineralogy (2010) 22 (3): 381–392.
... amplifier was used. Because Mims ENDOR gives rise to blind-spots that originate from an oscillating τ dependence, ENDOR spectra were also recorded as a function of τ and subsequently summed together. Sets of CW-EPR and pulsed ENDOR (and ESEEM) spectra were obtained for one plane whose normal is ~30...
FIGURES
First thumbnail for: Single-crystal EPR and ENDOR study of an Al—O − ce...
Second thumbnail for: Single-crystal EPR and ENDOR study of an Al—O − ce...
Third thumbnail for: Single-crystal EPR and ENDOR study of an Al—O − ce...
Journal Article
Published: 01 August 2009
The Canadian Mineralogist (2009) 47 (4): 933–945.
... analyses yield an average iron content of 0.053(34) wt% Fe 2 O 3 ; single-crystal XRD intensity datasets confirm the space group P 2 cm . Single-crystal EPR spectra measured from 290 to 13 K reveal at least six paramagnetic defects: three Fe 3+ centers, a VO 2+ radical, a Mn 2+ center, and an Al-associated...
FIGURES
First thumbnail for: SINGLE-CRYSTAL EPR STUDY OF Fe 3+ AND VO 2+ IN PRE...
Second thumbnail for: SINGLE-CRYSTAL EPR STUDY OF Fe 3+ AND VO 2+ IN PRE...
Third thumbnail for: SINGLE-CRYSTAL EPR STUDY OF Fe 3+ AND VO 2+ IN PRE...
Journal Article
Published: 01 August 2009
Mineralogical Magazine (2009) 73 (4): 519–535.
... in previous X-band (∼9.4 GHz) EPR studies ( Table 1 ). Moreover, our multifrequency EPR spectra, together with results from pulsed electron nuclear double resonance (ENDOR) spectroscopy, electron spin echo envelope modulation (ESEEM) spectroscopy, and density functional theory (DFT) calculations, provided...
FIGURES
First thumbnail for: Radiation-induced defects in quartz: a multifreque...
Second thumbnail for: Radiation-induced defects in quartz: a multifreque...
Third thumbnail for: Radiation-induced defects in quartz: a multifreque...
Journal Article
Published: 01 August 2011
American Mineralogist (2011) 96 (8-9): 1331–1342.
... spectra of as-is stishovite reveal two high-spin (S = 3/2) Cr 3+ centers: one with D 2 h symmetry and another of triclinic symmetry. Quantitatively determined spin Hamiltonian parameters, including matrices g , D , and A ( 53 Cr) and high-spin Zeeman term BS 3 , suggest that the D 2 h center represents...
FIGURES
First thumbnail for: Mechanisms of Cr and H incorporation in stishovite...
Second thumbnail for: Mechanisms of Cr and H incorporation in stishovite...
Third thumbnail for: Mechanisms of Cr and H incorporation in stishovite...
Journal Article
Published: 01 August 2009
Mineralogical Magazine (2009) 73 (4): 537–550.
... are 27.2° and 25.4° for the [AlO 4 /H + (a > )] 0 and [AlO 4 /H + (a < )] 0 defects respectively. These angles are about 10° smaller that those deduced from the polarized IR spectra ( Pankrath, 1991 ), which suggested two OH orientations with angles at ∼36° and 34°. However, the difference of about...
FIGURES
First thumbnail for: Theoretical calculations of [AlO 4 / M + ] 0 defec...
Second thumbnail for: Theoretical calculations of [AlO 4 / M + ] 0 defec...
Third thumbnail for: Theoretical calculations of [AlO 4 / M + ] 0 defec...
Journal Article
Journal: Economic Geology
Published: 01 November 2008
Economic Geology (2008) 103 (7): 1571–1580.
...Baoqun Hu; Yuanming Pan; Sanda Botis; Brett Rogers; Tom Kotzer; Gary Yeo Abstract Room-temperature powder electron paramagnetic resonance (EPR) spectra of drusy quartz (i.e., euhedral quartz crystals as coatings on or infillings in cavities and fractures) from five uranium mineralized areas...
FIGURES
First thumbnail for: RADIATION-INDUCED DEFECTS IN DRUSY QUARTZ, ATHABAS...
Second thumbnail for: RADIATION-INDUCED DEFECTS IN DRUSY QUARTZ, ATHABAS...
Third thumbnail for: RADIATION-INDUCED DEFECTS IN DRUSY QUARTZ, ATHABAS...
Journal Article
Published: 16 July 2024
The Canadian Journal of Mineralogy and Petrology (2024) 62 (4): 625–641.
...Leo K. L. Cheung; Cameron Mackay; James Sykes; Yuanming Pan Abstract Quartz grains from the ACKIO uranium prospect, located near the eastern margin of the Athabasca Basin, Saskatchewan, have been investigated using powder X-band electron paramagnetic resonance (EPR) spectroscopy. The EPR spectra...
FIGURES
First thumbnail for: Distribution of Radiation-Induced Defects in Quart...
Second thumbnail for: Distribution of Radiation-Induced Defects in Quart...
Third thumbnail for: Distribution of Radiation-Induced Defects in Quart...
Journal Article
Published: 01 May 2017
The Canadian Mineralogist (2017) 55 (3): 457–472.
... paramagnetic resonance (EPR) spectroscopy as well as cathodoluminescence (CL) imaging and spectroscopy. Powder EPR spectra confirm that quartz from the Arrow deposit contains a suite of radiation-induced defects, including characteristic silicon vacancy hole centers formed from bombardment of α particles...
FIGURES
First thumbnail for: Radiation-induced Damage in Quartz At the Arrow Ur...
Second thumbnail for: Radiation-induced Damage in Quartz At the Arrow Ur...
Third thumbnail for: Radiation-induced Damage in Quartz At the Arrow Ur...