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1.
Questions concerning the influence of soil type and crop cover on the fate and transport of nitrate (NO3−) were examined. During a growing season, soils derived from glacial material underlying either corn or soybeans were sampled
for levels of NO3− within the pore water. Measured levels of NO3− ranged from below detection limit to 14.9 g NO3− per kilogram of soil (g/kg). In fields with the same crop cover, the silty-clayey soil exhibited a greater decrease in NO3− levels with depth than the sandier soil. Crop uptake of NO3− occurs within the root zone; however, the type of crop cover did not have a direct impact on the fate or transport during
the growing season. The soils underlying soybeans had an increase in NO3− levels following harvest, suggesting that the decomposition of the soybean roots contributed to the net gain of NO3− in the shallow soil. For all of the soil types, conditions below 100 cm are conducive for microbial denitrification, with
both a high water saturation level (>60%) and moderate organic carbon content (1–2%). At depths below 100 cm, temporal differences
in NO3− levels of over a magnitude, up to a 95% reduction, were recorded in the soil units as the growing season progressed. Physical
properties that control the transport of NO3− or denitrification have a larger influence on NO3− levels than crop type.
相似文献
Eric W. PetersonEmail: |
2.
Variously colored gem-quality topazes from Ouro Preto, Minas Gerais, Brazil, were studied by optical absorption spectroscopy and photoluminescence methods. In the near infrared range (750–2500 nm) the absorption spectra display an identical pattern of narrow intense absorption lines caused by overtones and combination vibrations of OH groups, which do not relate to the coloration of the topazes studied. Their colors were found to be caused by combination of three sets of absorption features, (1), (2), and (3) in the visible and near-UV range, which are due to different color center. (1) denotes a pair of broad split bands with maxima 18 000 and 25 000 cm–1 caused by electronic spin-allowed dd transitions of Cr3+ ions. They cause a light rose to deep violet color and characteristic pleochroism of Cr3+-containing topazes. Photoluminescence evidences of at least three different types of Cr3+ complexes which, most probably, differ by ligand surroundings, O4F2, O4F(OH) and O4(OH) (2) Corresponds to the intense weakly polarized UV absorption edge. Two different parts, the thermally stable one, caused by ligand-to-metal charge transfer, and the thermally unstable one, caused by some defect center(s), contribute to the edge. (3) denotes a system of two broad unstructured bands with maxima around 19 000 cm–1 (X>Y Z) and 24 000 cm–1 (Y Z
X). They cause the unique orange color and characteristic pleochroism of Brazilian Imperial topazes. Combinations of (1) and (3) absorption features cause various yellow-rose colors of the samples. Investigations of natural irradiated and thermally treated topazes show that the color centers (1) and (3) transform to each other at annealing and X- or gamma irradiation. The color of natural orange-red Imperial topazes is assumed to be caused by Cr4+, stabilized by other impurity ions and/or defect irradiation EPR centers. At T=300 °C Cr4+ reduces to Cr3+, the color of Imperial topazes changes to pale rose, caused by spin-allowed bands of Cr3+. In artificially irradiated crystals the (3)-center, Cr4+, may be induced according to the reaction 2Cr3+ Cr4+ + Cr2+, which involves chromium pairs in adjacent Al sites of the structure. Such artificially induced color is unstable at room temperature and in daylight. The process of the decay of (3)-centers may be described as a recombination Cr4++Cr2+ 2Cr3+ that results in vanishing of the (3)-bands accompanied by the appearance or increase in Cr3+
dd bands, the original orange color turning to a pale rose. 相似文献
3.
Infrared (IR) and nearinfrared (NIR) absorption spectra of hydrous and F-rich topazes were measured to assign an OH bending
mode of topaz. Three absorption peaks at 1165, 3650, and 4803 cm−1 are assigned to OH related absorption peaks. Since a peak at 4803 cm−1 can be assigned to a combination mode of 1165 and 3650 cm−1, the 1165 cm−1 peak is harmonic with the 3650 cm−1 peak. Polarized IR absorption spectra of (100), (010), and (001) planes of the hydrous topaz were measured to examine IR
active orientation of the 1165 cm−1 OH related mode. Three pleochroic distributions of the absorption peak at 1165 cm−1 on (100), (010), and (001) planes indicate an active orientation of the 1165 cm−1 OH related mode. The IR active orientation of the 1165 cm−1 OH related mode in topaz is normal to the OH dipole. The orthogonality and harmonic combination mode indicate that the 1165 cm−1 peak is OH bending mode. The active orientation of OH bending mode is polarized in the plane normal to the OH dipole. The
polarization suggests that anisotropic thermal vibration of protons on the hydroxyl is maximum along the IR active orientation.
Received: August 16, 1996 / Revised, accepted: April 20, 1997 相似文献
4.
Monika Koch-Müller Stanislav S. Matsyuk Dieter Rhede Richard Wirth Natasha Khisina 《Physics and Chemistry of Minerals》2006,33(4):276-287
The incorporation of hydrogen in mantle olivine xenocrysts from the Udachnaya kimberlite pipe was investigated by Fourier-transform infrared spectroscopy and secondary ion mass spectrometry (SIMS). IR spectra were collected in the OH stretching region on oriented single crystals using a conventional IR source at ambient conditions and in situ at temperatures down to −180°C as well as with IR synchrotron radiation. The IR spectra of the samples are complex containing more than 20 strongly polarized OH bands in the range 3,730–3,330 cm−1. Bands at high energies (3,730–3,670 cm−1) were assigned to inclusions of serpentine, talc and the 10 Å phase. All other bands are believed to be intrinsic to olivine. The corresponding point defects are (a) associated with vacant Si sites (3,607 cm−1 E || a, 3,597 E || a, 3,571 cm−1 E || c, 3,567 E || c, and 3,556 E || b), and (b) with vacant M1 sites (most of the bands polarized parallel to a). From the pleochroic behavior and position of the OH bands associated with the vacant M1 sites, we propose two types of hydrogen—one bonded to O1 and another to O2, so that both OH vectors are strongly aligned parallel to a. The O2–H groups may be responsible for the OH bands at higher wavenumbers than those for the O1–H groups. The multiplicity of the corresponding OH bands in the spectra can be explained by different chemical environments and by slightly different distortions of the M1 sites in these high-pressure olivines. Four samples were investigated by SIMS. The calculated integral molar absorption coefficient using the IR and SIMS results of 37,500±5,000 L mol H2O cm−2 is within the uncertainties slightly higher than the value determined by Bell et al. (J Geophys Res 108(B2):2105–2113, 2003) (28,450±1,830 L mol H2O cm−2). The reason for the difference is the different distributions of the absorption intensity of the spectra of both studies (mean wavenumber 3,548 vs. 3,570 cm−1). Olivine samples with a mean wavenumber of about 3,548 cm−1 should be quantified with the absorption coefficient as determined in this study; those containing more bands at higher wavenumber (mean wavenumber 3,570 cm−1) should be quantified using the value determined by Bell et al. (J Geophys Res 108(B2):2105–2113, 2003).
相似文献
Monika Koch-MüllerEmail: Phone: +49-331-2881492 |
5.
Boris Kolesov 《Physics and Chemistry of Minerals》2008,35(5):271-278
Single-crystal polarized Raman spectra (3,000–4,000 cm−1 at 3 ≤ T ≤ 300 K) were measured for synthetic alkali-free and natural beryl, Be2Al3Si6O18·xH2O, to determine the behavior of H2O molecules of both Type I and Type II in the cavities. At low temperature, the H2O molecules of Type I displace from the center of cavity and give rise to very weak hydrogen bonding with the host lattice.
The H2O Type I translational motion is characterized by substantial anharmonicity and looks like a motion of “a particle in the
box” with a frequency of 6.3 cm−1. Water Type II is characterized by a free rotation with respect to the C
2 molecule axis, and it makes possible the water nuclear isomers (i.e. ortho- and para-) to be observed at low temperature.
相似文献
Boris KolesovEmail: |
6.
Sylvie Demouchy Stephen J. Mackwell David L. Kohlstedt 《Contributions to Mineralogy and Petrology》2007,154(3):279-289
Interdiffusion of Fe and Mg in (Mg,Fe)O has been investigated experimentally under hydrous conditions. Single crystals of
MgO in contact with (Mg0.73Fe0.27)O were annealed hydrothermally at 300 MPa between 1,000 and 1,250°C and using a Ni–NiO buffer. After electron microprobe
analyses, the dependence of the interdiffusivity on Fe concentration was determined using a Boltzmann–Matano analysis. For
a water fugacity of ∼300 MPa, the Fe–Mg interdiffusion coefficient in Fe
x
Mg1−x
O with 0.01 ≤ x ≤ 0.25 can be described by with and C = −80 ± 10 kJ mol−1. For x = 0.1 and at 1,000°C, Fe–Mg interdiffusion is a factor of ∼4 faster under hydrous than under anhydrous conditions. This enhanced
rate of interdiffusion is attributed to an increased concentration of metal vacancies resulting from the incorporation of
hydrogen. Such water-induced enhancement of kinetics may have important implications for the rheological properties of the
lower mantle.
相似文献
Sylvie DemouchyEmail: |
7.
P. Mogilevsky 《Physics and Chemistry of Minerals》2007,34(3):201-214
The regular solid solution model has been applied to solid solubility in the monazite–xenotime systems and is verified against
the available experimental data for LaPO4–YPO4 and CePO4–YPO4 systems. The model is then used to predict the miscibility gaps in a number of other monazite–xenotime systems. The implications
for prospective two-phase monazite–xenotime fiber coatings for applications in ceramic matrix composites (CMCs) are discussed.
相似文献
P. MogilevskyEmail: |
8.
Summary The question of alternative technologies for high-speed Internet access lies at the heart of rural development problems. In
this paper, we focus on one of those technologies, the system combining satellite technologies and Wi-Fi. Based on an empirical
study carried out in three rural areas, we analyze the dynamics of the use and appropriation of that technology by the companies
and organizations participating in the experiment. Considered both from a technical and social standpoint, the technology
‘in use’ appears here in its structuring dimensions.
相似文献
Valérie FautreroEmail: |
9.
D. Vielzeuf A. Baronnet A. L. Perchuk D. Laporte M. B. Baker 《Contributions to Mineralogy and Petrology》2007,154(2):153-170
Concentration gradients in calcium are common in metamorphic or magmatic garnets and can be used to determine the timescales
of geological processes. However, the kinetics of Ca diffusion in garnet is poorly constrained and experimental studies have
to date yielded widely varying diffusion coefficients. In this paper, we describe a new method for generating diffusion profiles
in garnet. We incorporated polished and compositionally homogeneous garnet seeds in a finely ground powder of clinopyroxene
and garnet. During the experiments (1.3 GPa, 1,050–1,250°C, and ƒO2 ≤ the graphite-O2 buffer), the mineral powder partially melted, recrystallized, and formed a 10–50 μm wide overgrowth zone of compositionally
distinct garnet around the seeds. Long duration experiments generated measurable relaxation profiles at these seed/overgrowth
interfaces. We performed analytical transmission electron microscope traverses across the interfaces in each experiment. Thirteen
usable compositional profiles were obtained with characteristic distances of diffusion ranging from 300 to 1,000 nm. From
these profiles, Ca–(Fe, Mg) interdiffusion coefficients were retrieved using an analytical solution for the diffusion equation
and the data were cast in an Arrhenius relation. Linear regression of the data yields an activation energy Q
Ca–(Fe, Mg) equal to 188 ± 48 kJ mol−1 and a frequency factor D
0 equal to 6.6 × 10−14 m2 s−1. Within the compositional range studied, the composition of garnet has no major effect on the Ca–(Fe, Mg) interdiffusion
coefficient. The very slow diffusion rate of Ca is in agreement with natural observations indicating that Ca diffuses more
slowly than Fe and Mg. The Ca diffusion coefficients derived from this study are not model-dependent and can be used to determine
the durations of geological events from Ca relaxation profiles in natural garnets.
相似文献
D. VielzeufEmail: |
10.
Isotope and trace element evidence for depleted lithosphere in the source of enriched Ko’olau basalts 总被引:1,自引:0,他引:1
Vincent J. M. Salters Janne Blichert-Toft Zuzana Fekiacova Afi Sachi-Kocher Michael Bizimis 《Contributions to Mineralogy and Petrology》2006,151(3):297-312
We have measured the Hf and Nd isotopic compositions of 38 basalts from the Ko’olau drill hole, Hawai’i. The basalts show
limited variations in both 176Hf/177Hf and 143Nd/144Nd (ε
Nd varies from +4.2 to +7.3 and ε
Hf from +8.0 to +12.3). Their correlated variation has an R
2 of 0.86. The data form an array with a slope of 1.2 on an ε
Hf–ε
Nd isotope correlation diagram, while the slope of all Hawai’ian basalt data is 0.98. Both slopes are significantly shallower
than that of the mantle array of 1.4 defined by ocean island basalts. Previous studies have shown that a shallow slope in
Hf–Nd isotope space can be related to ancient pelagic sediments in the mantle source (Blichert-Toft et al. 1999; Salters and White 1998). However, the combined variations in Ko’olau basalts of Hf–Nd–Pb–Os isotopic compositions and trace element ratios, such
as La/Nb, Th/La and Sr/Nd, are not consistent with the simple addition of a sediment component to the mantle. We instead propose
that the shallow slope on the Hf–Nd isotope correlation diagram for Ko’olau shield stage basalts can be better explained if
the enriched endmember contains either an ancient oceanic lithosphere component or the high-176Hf/177Hf component observed in the Salt Lake Crater (SLC) peridotite xenoliths (which also have a depleted lithosphere origin).
Since Ko’olau basalts have high 187Os/188Os (0.135–0.160) and the SLC xenoliths have 187Os/188Os up to 0.13 (Lassiter et al. 2000) Os-isotopes are consistent with the latter being a component in the enriched Ko’olau source.
相似文献
Vincent J. M. SaltersEmail: |
11.
Sensitivity of high-resolution tropical cyclone intensity forecasts to surface flux parameterization
Chi-Sann Liou 《Natural Hazards》2007,41(3):387-399
Surface flux parameterization schemes used in current dynamic models are primarily based upon measurements at low and moderate
wind speeds. Recent studies show that these parameterization schemes may be incorrect at high wind speeds (e.g., tropical
cyclone forecasts). Five high-resolution numerical model experiments are designed to assess the sensitivity of tropical cyclone
intensity forecasts to changes in the surface flux parameterization. The sensitivity experiments are conducted by running
48 h forecasts of the Coupled Ocean/Atmosphere Mesoscale Prediction System (COAMPS) for six selected tropical cyclones with
individual modifications to surface flux calculation that include: (1) limiting the surface stress for wind speeds greater
than 33 m s−1, or 64 knots (kt); (2) computing the stress at the top of the model bottom grid layer (MBGL) by averaging results from surface
layer similarity and turbulence mixing parameterization for wind speeds greater than 33 m s−1; (3) increasing the roughness lengths for heat and moisture transfer by a factor of ten; (4) setting the roughness lengths
for heat and moisture transfer to 1/10 of the momentum roughness length; and (5) cooling the sea surface temperature (SST)
by a prescribed rate at high winds. Averaged responses for the six storms to these sensitivity tests show that: (i) the limit
on surface stress at high winds significantly increases the cyclone intensity in 48 h forecasts; (ii) the averaged surface
layer stress at high winds increases the cyclone intensity but to a much lesser degree than limiting the surface stress; (iii)
large increases in the roughness lengths for heat and moisture transfer are needed to significantly impact the intensity forecast;
(iv) the different roughness length formula for surface transfer coefficients notably increases C
h/C
d ratio from 0.59 to 0.79 for 25 m s−1 and 0.41 to 0.75 for 50 m s−1 that significantly increases the predicted cyclone intensity; and (v) cooling of the SST by −5.8°C in 48 h reduces the maximum
surface wind speed by −32 kt, or 16.5 m s−1, at 48 h forecast. These results suggest that a surface flux parameterization scheme suitable for tropical cyclone intensity
forecast must correctly model the leveling-off character of surface stress and C
h/C
d ratio at high winds. All modifications to surface flux calculation have little influence on 48 h track forecasts, even though
they may significantly impact the intensity forecasts.
相似文献
Chi-Sann LiouEmail: |
12.
The radiation sensitivity, time stability and optical sensitivity of [Si45−] paramagnetic centers in natural zircon crystals, particularly those from the Late Neopleistocenic tuff of the Elbrus Volcano,
have been studied. Optical bleaching was shown to result in the recombination of [Si45−] centers, while the concentration of centers increases in the absence of light due to the internal radiation background.
The data obtained show the infeasibility of using [Si45−] centers in zircons as paleodosimeters in conventional dating methods using electron paramagnetic resonance (EPR) spectroscopy.
New specific techniques need to be developed for EPR dating of zircons. 相似文献
13.
Joachim Kuhlemann Klaas van der Borg Paul D. Bons Martin Danišík Wolfgang Frisch 《International Journal of Earth Sciences》2008,97(3):549-564
A study of erosion rates by in-situ 10Be concentrations in granites of Miocene high-elevation paleosurfaces in Corsica indicates maximum erosion rates between 8
and 24 mm/kyear. The regional distribution of measured erosion rates indicates that the local climatic conditions, namely
precipitation, the petrographic composition of granites, and the degree of brittle deformation govern erosion rates. Chemical
erosion dominates even at elevations around 2,000 m in presently subalpine climate conditions. Field evidence indicates that
erosion operates by continuous dissolution and/or disintegration to grains (grusification). The erosion rates are relatively
high with respect to the preservation of inferred Early Miocene landscapes. We infer temporal burial in the Middle Miocene
and significantly lower erosion rates in the Neogene until ∼3 Ma to explain the preservation of paleosurfaces, in line with
fission track data. Valley incision rates that are a magnitude higher than erosion rates on summit surfaces result in relief
enhancement and long-term isostatic surface uplift. On the other hand, widening and deepening of valleys by cyclic glaciation
progressively destroys the summit surface relics.
相似文献
Wolfgang FrischEmail: |
14.
Melt inclusion formation mechanisms and compositional effects in high-An feldspar and high-Fo olivine in anhydrous mafic silicate liquids 总被引:1,自引:1,他引:0
Important aspects of melt inclusion formation and potential compositions effects have been addressed through a series of experiments using anorthite/fosterite saturated anhydrous mafic liquids. Experimental charges were cooled from 1,300 to 1,230 and 1,210°C at rates of 1–10°/min followed by 0–24 h isothermal periods. Hopper and skeletal crystal morphologies with variable degrees of completeness developed during the cooling period. Planar overgrowth of these textures during isothermal periods led to the formation of inclusions, the majority of which formed after 6 h of isothermal run time. We suggest that the change in morphologies is related to a decrease in growth rates and changes in dominant growth mechanisms. In general, inclusion compositions were uniform and similar to the host glass, indicating that with the isothermal times required for most inclusions to form, a boundary layer was not entrapped that could be detected within the limits of our analyses.
相似文献
Edward KohutEmail: Phone: +1-541-7373023Fax: +1-541-7371200 |
Roger L. NielsenEmail: Phone: +1-541-7371235 |
15.
The study addresses population dynamics in Ghana on the urban and regional levels between 1984 and 2000. At the urban level,
the development trends are analyzed for urban localities (population above 5,000) on the basis of geo-coded census data. Potential
driving forces for rapid population growth related to size, location, accessibility and facility counts are examined using
bivariate and multivariate analysis. An index of weighted accessibility relative to other urban localities provides significant
explanation at the national level, as does initial locality size. At the regional level, population development is analyzed
to provide insight into the rural–urban relations. The level of urbanization is steadily increasing but varies considerably
between regions. Areas of high population growth are found in some rural areas that have a remote location relative to the
large urban centers. This seems to indicate the existence of ‘frontier’ regions, i.e. areas that experience a high degree
of in-migration by people aiming to undertake specific farming activities. A high proportion of the population growth in these
areas appears to take place in relatively small towns. The paper concludes with a more in-depth discussion of the development
characteristics of Ghana’s Western Region. This region has experienced one of the highest regional population growth rates,
mainly due to its status as a ‘frontier’ for cocoa production.
相似文献
Lasse Moller-JensenEmail: |
16.
Alexej N. Platonov Klaus Langer Stanislav S. Matsyuk 《Physics and Chemistry of Minerals》2008,35(6):331-337
In the course of a thorough study of the influences of the second coordination sphere on the crystal field parameters of the
3d
N
-ions and the character of 3d
N
–O bonds in oxygen based minerals, 19 natural Cr3+-bearing (Mg,Ca)-garnets from upper mantle rocks were analysed and studied by electronic absorption spectroscopy, EAS. The
garnets had compositions with populations of the [8]
X-sites by 0.881 ± 0.053 (Ca + Mg) and changing Ca-fractions in the range 0.020 ≤ w
Ca[8] ≤ 0.745, while the [6]
Y-site fraction was constant with x
Cr3+
[6] = 0.335 ± 0.023. The garnets had colours from deeply violet-red for low Ca-contents (up to x
Ca = 0.28), grey with 0.28 ≤ x
Ca ≤ 0.4 and green with 0.4 ≤ x
Ca. The crystal field parameter of octahedral Cr3+ 10Dq decreases strongly on increasing Ca-fraction from 17,850 cm−1 at x
Ca[8] = 0.020 to 16,580 cm−1 at x
Ca[8] = 0.745. The data could be fit with two model which do statistically not differ: (1) two linear functions with a discontinuity
close to x
Ca[8] ≈ 0.3,
(2) one continuous second order function,
The behaviour of the crystal field parameter 10Dq and band widths on changing Ca-contents favour the first model, which is
interpreted tentatively by different influences of Ca in the structure above and below x
Ca[8] ≈ 0.3. The covalency of the Cr–O bond as reflected in the behaviour of the nephelauxetic ratio
decreases on increasing Ca-contents. 相似文献
17.
Land tenure rights reflect the deeper structures of society, particularly gender distinctions in relation to land. Considering
the structural differences between patrilineal and matrilineal customary tenure systems in East Timor are understudied, this
paper explores men and women’s experiences in accessing land under such arrangements. The comparative analysis of two patrilineal
with one matrilineal land tenure systems in Ainaro and Manufahi districts suggests a significant degree of flexibility within
both systems with respect to the norms of gendered inheritance. Therefore, the binary constructs of ‘patrilineal’ and ‘matrilineal’
societies are limiting. Both men and women in these communities may acquire land rights under different circumstances, mainly
through negotiations with their parents or hamlet chief. Daughters in the patrilineal communities could inherit family land
upon their parents’ death and sons in the matrilineal community could gain land by cultivating and maintaining unclaimed customary
land. Empirical evidence show that inheritance principally determines usufruct rights to land, but marriage exchange practices
complicates a deeper understanding of traditional East Timorese land rights.
相似文献
Pyone Myat ThuEmail: |
18.
The thermal expansion of gehlenite, Ca2Al[AlSiO7], (up to T=830 K), TbCaAl[Al2O7] (up to T=1,100 K) and SmCaAl[Al2O7] (up to T=1,024 K) has been determined. All compounds are of the melilite structure type with space group
Thermal expansion data was obtained from in situ X-ray powder diffraction experiments in-house and at HASYLAB at the Deutsches Elektronen Synchrotron (DESY) in Hamburg (Germany). The thermal expansion coefficients for gehlenite were found to be: α1=7.2(4)×10−6 K−1+3.6(7)×10−9ΔT K−2 and α3=15.0(1)×10−6 K−1. For TbCaAl[Al2O7] the respective values are: α1=7.0(2)×10−6 K−1+2.0(2)×10−9ΔT K−2 and α3=8.5(2)×10−6 K−1+2.0(3)×10−9ΔT K−2, and the thermal expansion coefficients for SmCaAl[Al2O7] are: α1=6.9(2)× 10−6 K−1+1.7(2)×10−9ΔT K−2 and α3=9.344(5)×10−6 K−1. The expansion-mechanisms of the three compounds are explained in terms of structural trends obtained from Rietveld refinements
of the crystal structures of the compounds against the powder diffraction patterns. No structural phase transitions have been
observed. While gehlenite behaves like a ’proper’ layer structure, the aluminates show increased framework structure behaviour.
This is most probably explained by stronger coulombic interactions between the tetrahedral conformation and the layer-bridging
cations due to the coupled substitution (Ca2++Si4+)-(Ln
3++Al3+) in the melilite-type structure.
Electronic Supplementary Material Supplementary material is available for this article at 相似文献
19.
The thermal expansion of gehlenite, Ca2Al[AlSiO7], (up to T=830 K), TbCaAl[Al2O7] (up to T=1100 K) and SmCaAl[Al2O7] (up to T=1024 K) has been determined. All compounds are of the melilite structure type with space group
Thermal expansion data were obtained from in situ X-ray powder diffraction experiments in-house and at HASYLAB at the Deutsches
Elektronen Synchrotron (DESY) in Hamburg (Germany). The thermal expansion coefficients for gehlenite were found to be: α1=7.2(4)×10−6×K−1+3.6(7)×10−9ΔT×K−2 and α3=15.0(1)×10−6×K−1. For TbCaAl[Al2O7] the respective values are: α1=7.0(2)×10−6×K−1+2.0(2)×10−9ΔT×K−2 and α3=8.5(2)×10−6×K−1+2.0(3)×10−9ΔT×K−2, and the thermal expansion coefficients for SmCaAl[Al2O7] are: α1=6.9(2)×10−6×K−1+1.7(2)×10−9ΔT×K−2 and α3=9.344(5)×10−6×K−1. The expansion mechanisms of the three compounds are explained in terms of structural trends obtained from Rietveld refinements
of the crystal structures of the compounds against the powder diffraction patterns. No structural phase transitions have been
observed. While gehlenite behaves like a ‘proper’ layer structure, the aluminates show increased framework structure behavior.
This is most probably explained by stronger coulombic interactions between the tetrahedral conformation and the layer-bridging
cations due to the coupled substitution (Ca2++Si4+)–(Ln
3++Al3+) in the melilite-type structure.
This article has been mistakenly published twice. The first and original version of it is available at . 相似文献
20.
Cathelijne de Busser 《GeoJournal》2006,67(4):283-294
Contrary to the absence of a uniform Spanish identity (a phenomenon that is often referred to as Spain being a ‘nation of
nations’), Spain’s confessional map is remarkably homogeneous. From the beginning of its existence as a political conglomeration,
Spain has been a mono-confessional Catholic territory. Even at present, Catholicism is an intrinsic feature of Spanish society
and – though officially a secular state – of state policy. A closer look at Spain’s religious situation and its corresponding
pattern of church–state relations reveals, however, some recent cracks in the century’s old bond between Spain and Catholicism.
Particularly secularization and religious pluralism challenge Spain’s mono-confessional Catholic nature, a development that
fits well into Spain’s post-Francoist focus on Europe and European (secular) values. This paper discusses Spanish church–state
relations from the beginning of its political existence until present times. Special attention will be paid to more recent
societal developments and their impact on religious Spain and church–state relations.
相似文献
Cathelijne de BusserEmail: |