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sputter depth profiling

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Journal Article
Published: 01 December 1988
American Mineralogist (1988) 73 (11-12): 1449–1456.
... and limitations of sputter depth profiles of minerals. Under the experimental conditions used (45° incident 1-kV Ar ions for a total of 20 min per sample; total ion dose = 10 17 ions/cm 2 ), between 10 and 20 nm have been sputtered from each sample, xps measurements have shown that compositional and structural...
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Depth profile into San Carlos olivine comparing the intensity of iron ions using O− and O2+ primary beams. Only the first 200 nm of the profiles are shown. The initial 20–40 nm represent sputtering through the overlying gold coat. The secondary signal for iron appears earlier in profile when O− is used because this primary species penetrates deeper into the sample and, through ion beam mixing, churns iron (and other elements in the olivine) to the surface where they can be sputtered and detected. In comparison, the smaller projected range of O2+ mixes atoms at a shallower level, improving the depth resolution of the profile as revealed by the 54Fe signal appearing at a greater depth. The spacing between data points is ~3× greater when O2+ is used because the sputter yield of the molecular primary beam is ~3× larger than for O− on this phase. Note the larger transient peak for iron between 30–40 nm when O− is used. Varying initial signals for matrix (and diffusing) elements is a common observation in depth profiles of silicates using an O− primary species (Ganguly et al. 1998; Van Orman et al. 2001; Ito and Ganguly 2006). Using the O2+ beam requires an auxiliary electron gun for charge neutralization (Genareau et al. 2007) and adds significant complexity to the depth profiling analysis. It also delivers the best depth resolution. However, most diffusion experiments can be designed so that the most important part of the profile is observed below the transient sputtering region, allowing straightforward use of the O− species.
Published: 01 January 2010
Figure 19. Depth profile into San Carlos olivine comparing the intensity of iron ions using O − and O 2 + primary beams. Only the first 200 nm of the profiles are shown. The initial 20–40 nm represent sputtering through the overlying gold coat. The secondary signal for iron appears earlier
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XPS-determined elemental concentrations for treated tennantite with depth profiling sputtering times (at.% concentrations normalized to 100). The most significant change with depth is the increase in S, Cu and Zn and the decrease in Ag. It must be noted that each point on the horizontal axis denotes a change in concentration with sputtering time on a non-linear scale
Published: 01 August 2006
F ig . 3. XPS-determined elemental concentrations for treated tennantite with depth profiling sputtering times (at.% concentrations normalized to 100). The most significant change with depth is the increase in S, Cu and Zn and the decrease in Ag. It must be noted that each point
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Measured depths of calibration SIMS pits in fluorapatite parallel to the c-axis, in fluorapatite perpendicular to the c-axis, and in chlorapatite parallel to the c-axis sputtered for different numbers of cycles. Best-fit lines are used to calibrate sputter rate in irradiated and baseline depth profiles, allowing conversion of cycle number to depth. Vertical bars show the error imposed by the z-axis step distance. Otherwise this is smaller than the size of the marker.
Published: 01 January 2015
Figure 1 Measured depths of calibration SIMS pits in fluorapatite parallel to the c -axis, in fluorapatite perpendicular to the c -axis, and in chlorapatite parallel to the c -axis sputtered for different numbers of cycles. Best-fit lines are used to calibrate sputter rate in irradiated
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Depth profile into silicon wafer implanted with 1014 atoms B/cm2 (O2+ primary beam, positive secondary ions detected). The background signal at ~6000 Å depth corresponds to ~0.1 ppm B. This low signal indicates that the depth profile was conducted in a manner limiting or excluding the contribution of boron from memory effects or the walls of the sputtered crater (Hervig 1996).
Published: 01 January 2010
Figure 18. Depth profile into silicon wafer implanted with 10 14 atoms B/cm 2 (O 2 + primary beam, positive secondary ions detected). The background signal at ~6000 Å depth corresponds to ~0.1 ppm B. This low signal indicates that the depth profile was conducted in a manner limiting
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Plots of secondary ion intensity as a function of sputter time. (a) Analysis of quartz from the Aue Granite where an increase in 7Li and a decrease in 23Na, 39K, and 54Fe intensity with time were observed. This intensity change is a general phenomena of these measurements, (b) Analysis of neocrystallised quartz within a fluid inclusion trail in the Hakos megaquartz. The sputter time of about 3000 s corresponds to a depth profiling of ≤ 10 μm.
Published: 01 July 2003
) Analysis of neocrystallised quartz within a fluid inclusion trail in the Hakos megaquartz. The sputter time of about 3000 s corresponds to a depth profiling of ≤ 10 μm.
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(a) Representative example of a diffusion profile of oxygen isotopes measured in calcite reacted at 700°C and total pressure of 800 bars with a fluid containing ICO2 = 0.5 for 22 hours (Labotka et al., 1999). Individual isotope ratio measurements were taken as the Cs+ ion beam sputtered from the surface into the interior of the crystal. The aberrant data at the beginning of the profile represents isotope ratios collected while the ion beam was sputtering through the gold coating and established a steady state of implantation into the crystal. (b) Corresponding to this profile is a plot in which the isotopic data are reduced using the solution to the diffusion equation for transport normal to the surface of a semi-infinite volume with a planar surface (e.g. Crank 1975). The slope of the inverse error function of the concentration ratio versus depth plot is proportional to (4Dt)−0.5 and can be used to extract a diffusion coefficient from the profile. Ci, Cs and Ct are the 18O concentrations at the crystal surface, crystal interior (initial value) and at depth x, respectively.
Published: 01 January 2001
sputtered from the surface into the interior of the crystal. The aberrant data at the beginning of the profile represents isotope ratios collected while the ion beam was sputtering through the gold coating and established a steady state of implantation into the crystal. (b) Corresponding to this profile
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Reflected light image of a sputtered crater in Lake County plagioclase (~100×100 μm2) and profilometry scan showing the ~2 μm depth of the crater after the depth profile (redrawn from Genareau et al., 2007).
Published: 01 January 2010
Figure 17. Reflected light image of a sputtered crater in Lake County plagioclase (~100×100 μm 2 ) and profilometry scan showing the ~2 μm depth of the crater after the depth profile (redrawn from Genareau et al., 2007 ).
Series: Short Courses
Published: 01 January 2009
DOI: 10.3749/9780921294818.ch06
EISBN: 978-0-921294-81-8
... by application of an electronic or optical gate that excludes ion signal from the edge of the SIMS crater ( Fig. 6-3 ). Figure 6-4 shows a series of depth profiles measured with an increasingly large percentage of the sputtered area collected, where 100% means signal is acquired from the entire sputtered...
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CO2 depth profiles of exposed and unexposed MI from White Island and Solchiaro. (a) CO2 depth profiles for MI hosted in plagioclase from White Island. Note the erratic CO2 behavior in the shallowest part of the MI. All the profiles refer to exposed MI with the exception of the blue profile that refers to an unexposed MI (Dec 7_5 MI). The unexposed MI is the same one shown in Figure 13. The boundary between the melt and the host is intersected at ~5000 s (see Fig. 13) and, thus, is not shown in this figure; (b) CO2 depth profiles for MI hosted in mafic phenocrysts. The magenta, green, and orange profiles refer to MI from Solchiaro and are hosted in olivine, while the blue and the black profiles refer to MI from White Island and hosted in orthopyroxene and clinopyroxene, respectively. The shallowest parts of the profiles do not show the same erratic behavior for CO2 exhibited by MI hosted in plagioclase (panel a). The green and the blue profiles are from unexposed MI hosted in olivine and in clinopyroxene, respectively. The orange, blue, and black lines go to essentially zero and are not resolvable on this figure. The MI/host interface is at around 7000 s for the MI hosted in olivine and around 4000 s for the MI hosted in clinopyroxene. The other three profiles refer to MI exposed at the surface; (c) CO2 depth profiles for glass standards and blanks used to determine the calibration curves. Note that CO2 concentrations do not show anomalous behavior in the glass standards. The solid vertical lines indicate the duration of the pre-sputtering and the analysis that was used most commonly for our MI analyses. Thus, the somewhat erratic behavior observed in the first few hundred seconds here would normally have been part of the pre-sputtering to remove surface effects and would not have been included in the quantification of CO2 in the MI.
Published: 01 May 2014
Figure 12 CO 2 depth profiles of exposed and unexposed MI from White Island and Solchiaro. ( a ) CO 2 depth profiles for MI hosted in plagioclase from White Island. Note the erratic CO 2 behavior in the shallowest part of the MI. All the profiles refer to exposed MI with the exception
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Cathodoluminescence image of a selected EL-20 zircon. The image shows individual δ18O spot measurements made across the crystal. Inset shows sputter crater cross section drawn to scale to illustrate spatial resolution in depth profiling mode parallel to zircon growth zones.
Published: 01 August 2009
Figure 2 Cathodoluminescence image of a selected EL-20 zircon. The image shows individual δ 18 O spot measurements made across the crystal. Inset shows sputter crater cross section drawn to scale to illustrate spatial resolution in depth profiling mode parallel to zircon growth zones.
Series: Reviews in Economic Geology
Published: 01 January 1997
DOI: 10.5382/Rev.07.08
EISBN: 9781629490144
... through a mass spectrometer. Acquired data may be presented as mass spectra, depth profiles showing element concentrations or isotope ratios, and ion images. SIMS has a number of advantages over electron-beam and X-ray analytical techniques. Secondary-ion intensities can be measured over a dynamic range...
Journal Article
Published: 01 August 2007
American Mineralogist (2007) 92 (8-9): 1374–1382.
... on the basis of euhedral morphology and a relatively homogeneous distribution of surface contamination, such as volcanic glass. Crystals were cleaned, embedded in In, and analyzed by SIMS in depth-profiling mode. We used an O + 2 primary ion beam, which provides a faster sputtering rate than the typically...
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First thumbnail for: Geochemical variations in late-stage growth of vol...
Second thumbnail for: Geochemical variations in late-stage growth of vol...
Third thumbnail for: Geochemical variations in late-stage growth of vol...
Journal Article
Published: 01 November 2006
European Journal of Mineralogy (2006) 18 (6): 705–718.
...) of ferro-johannsenite deposited by RF plasma sputtering provided iron and manganese for exchange with magnesium from the diopside substrates. Interdiffusion profiles of Fe-Mg and Mn-Mg were analysed by secondary ion mass spectrometry in depth profiling mode. We found that the (Fe,Mn)-Mg interdiffusion...
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First thumbnail for: (Fe,Mn)-Mg interdiffusion in natural diopside: eff...
Second thumbnail for: (Fe,Mn)-Mg interdiffusion in natural diopside: eff...
Third thumbnail for: (Fe,Mn)-Mg interdiffusion in natural diopside: eff...
Image
Sputtered crater in surface of volcanic plagioclase 40 μm deep by 70 μm in diameter obtained on the 3f SIMS in ~6 hours using “aperture illumination,” the O2+ primary beam, and the normal-incidence electron gun for charge neutralization (analysis and image by Dr. Kimberly Genareau, ASU). Note volcanic glass adhering to crystal surface, and the steps in the bottom of the crater. The overlap between these steps and the region of the crater floor allowed into the mass spectrometer will define the depth resolution of this profile.
Published: 01 January 2010
, ASU). Note volcanic glass adhering to crystal surface, and the steps in the bottom of the crater. The overlap between these steps and the region of the crater floor allowed into the mass spectrometer will define the depth resolution of this profile.
Journal Article
Published: 01 September 1999
American Mineralogist (1999) 84 (9): 1392–1399.
... in a CO 2 gas at 1 atm total pressure and temperatures from 550 to 800 degrees C. Diffusion coefficient values were derived from the depth profiles obtained by ion microprobe analysis. The resultant activation energies for Mg tracer diffusion and Ca self-diffusion are, respectively: E a (Mg) = 284+ or -74...
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Depth profiles of (a) 90Zr, (b) 30Si, and (c) 56Fe on a logarithmic scale measured by SIMS for three different samples. Sample Ol40/7-4 is a reference sample, and samples Ol40/7-1 and Ol40/7-2 were annealed at 900 °C for 15 and 60 min, respectively. Note that the Zr profiles (a) are unaffected by the anneal; small differences are due to fine variations in sputter conditions for different samples leading to slightly different sensitivity and spatial resolution. The concentration of Si (b) and Fe (c) decreases drastically in the ZrO2 thin film, but from the comparison with the reference sampl, it can be seen that during the anneal Fe and Si has been transferred in minor proportions from the olivine into the ZrO2 film. This enrichment is attributed solely to grain boundary segregation of Fe, Mg, and Si, because partitioning and diffusion into the volume of ZrO2 should be negligible. Solid lines in b and c are fits obtained by the convolution of ideal step profiles following the procedure of Hofmann (1994).
Published: 01 May 2008
F igure 5. Depth profiles of ( a ) 90 Zr, ( b ) 30 Si, and ( c ) 56 Fe on a logarithmic scale measured by SIMS for three different samples. Sample Ol40/7-4 is a reference sample, and samples Ol40/7-1 and Ol40/7-2 were annealed at 900 °C for 15 and 60 min, respectively. Note that the Zr
Series: European Mineralogical Union Notes in Mineralogy
Published: 01 January 2010
DOI: 10.1180/EMU-notes.8.4
EISBN: 9780903056489
... length in sections 3.3 and 4.3 below. Depth profiling The destructive aspect of sputtering may be used to good effect in removing successive surface layers thereby revealing deeper structures and compositions. If the primary ion beam is rastered in a controlled and uniform way across the surface...
Journal Article
Published: 01 January 2010
Reviews in Mineralogy and Geochemistry (2010) 72 (1): 107–170.
...Figure 19. Depth profile into San Carlos olivine comparing the intensity of iron ions using O − and O 2 + primary beams. Only the first 200 nm of the profiles are shown. The initial 20–40 nm represent sputtering through the overlying gold coat. The secondary signal for iron appears earlier...
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First thumbnail for: Analytical Methods in Diffusion Studies
Second thumbnail for: Analytical Methods in Diffusion Studies
Third thumbnail for: Analytical Methods in Diffusion Studies
Journal Article
Published: 01 April 2004
American Mineralogist (2004) 89 (4): 498–504.
.... It is effective because the atomic collisions in the sample nearsurface that impart excess energy to ejected ions also tend to break up complex molecular species. As an example of energy filtering, a depth profile of Au-implanted pyrite (see Cabri and McMahon 1995 for sample detail), sputtered by a Cs...
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First thumbnail for: SIMS microanalyses for Au in silicates
Second thumbnail for: SIMS microanalyses for Au in silicates
Third thumbnail for: SIMS microanalyses for Au in silicates