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411.
Restitution coefficients are used to quantify the energy dissipation upon impact when predicting rock fall events. These coefficients
can be determined in situ or in the laboratory. In any case, the usual values for the normal restitution coefficient k
n are below unity. Values greater than one are quite rare, seen as unusual and barely explained. Previous experimental research
conducted in Australia has shown consistent and systematic values of the normal restitution coefficient greater than one.
This was tentatively explained by a combination of parameters such as low impacting angle, rotational energy and block angularity.
The study presented in this paper aims at (1) identifying the critical parameters conducting to high k
n values and (2) at explaining the associated motion mechanisms. The objective was reached with values of k
n up to almost 2. In addition, the study has confirmed the significance of low impacting angle, rotational energy and block
shape in this context. 相似文献
412.
Salt marsh fucoid algae are a conspicuous component of north temperate marshes, yet comparatively little research has been
conducted to examine their ecological effects. We examined the influence of salt marsh fucoids on physical conditions and
the biotic community in a manipulative experiment conducted in a southern Maine back-barrier salt marsh. The biomass of salt
marsh fucoids was higher than that of aboveground Spartina alterniflora in the zone where we conducted the experiment. Average daytime temperatures at the sediment surface were significantly reduced
by the presence of salt marsh fucoids. Density and biomass of standing-dead S. alterniflora was significantly higher when salt marsh fucoids were removed. In contrast, the abundance of various species of epifauna
and infauna were significantly enhanced by the presence of salt marsh fucoids. A regional survey indicated that results from
the study site may be conservative because the biomass of salt marsh fucoids was lowest among other back-barrier marshes.
Salt marsh fucoids are little studied ecosystem engineers whose presence affects the microclimate and biotic community, especially
the animals that constitute the basal components of the salt marsh trophic relay. 相似文献
413.
Etienne Balan Marc Blanchard Michele Lazzeri Jannick Ingrin 《Physics and Chemistry of Minerals》2014,41(2):105-114
Water incorporation in forsterite samples synthesized under low to medium silica-activity conditions mostly occurs via a substitutional mechanism in which a Si vacancy is compensated by four protons. Corresponding IR absorption spectra display a cluster of narrow and weakly anharmonic OH-stretching bands at wavenumbers above 3,500 cm?1. However, this diagnostic spectrum is often superimposed to one broader absorption band, rarely two, displaying pronounced temperature-dependent properties and tentatively assigned to H atoms in interstitial position (Ingrin et al. in Phys Chem Miner 40:499–510, 2013). Here, we investigate the structural and vibrational properties of selected interstitial H-bearing defects in forsterite using a first-principles modeling approach. We show that the broad bands discussed by Ingrin et al. (Phys Chem Miner 40:499–510, 2013) are most likely related to interstitial OH groups in the vacant octahedral sites alternating with the M2 sites along the c axis of the forsterite structure. The corresponding OH defects lead to the formation of fivefold coordinated Si species. Their peculiar thermal properties stem from the vibrational phase relaxation due to the anharmonic coupling of the high-energy local OH-stretching mode with a low-energy vibrational mode. This “exchange mode” corresponds to the hindered longitudinal translation of the OH group. These results suggest that at high pressure, hydrogen incorporation in forsterite is dominated by coexisting interstitial OH groups and (4H)Si defects. 相似文献
414.
Michele Salis Alan A. Ager Mark A. Finney Bachisio Arca Donatella Spano 《Natural Hazards》2014,71(3):1389-1418
We evaluated the spatiotemporal changes in wildfire regime and exposure in a fire-prone Mediterranean area (Sardinia, Italy) in relation to changes in ignition patterns, weather, suppression activities, and land uses. We also used wildfire simulations to identify fine-scale changes in wildfire exposure of important features on the island. Sardinia experienced a sharp reduction in fire number and area burned between the periods 1980–1994 and 1995–2009. Despite this decrease, losses and fatalities from wildfires continue. This suggests that localized areas and seasons of high wildfire risk persist on the island. Our analysis showed (1) a reduction in area burned (60,000–20,000 ha/year) and ignitions (3,700–2,600 fires/year), (2) an advance of 15 days for the fire season peak, (3) an increase in spring temperatures, and (4) an increase in fire exposure for WUI areas. Little change was noted for land use types and associated fuels. Most likely the reduction in fire activity may be due to a combination of social factors and suppression capabilities. On the other hand, simulation modeling suggested pockets of high wildfire exposure in specific places. The combined empirical analyses and simulation modeling provided a robust approach to understanding the spatiotemporal dynamics of wildfire risk on the island. 相似文献
415.
Giuseppina Balassone Volker Kahlenberg Angela Altomare Angela Mormone Rosanna Rizzi Michele Saviano Nicola Mondillo 《Mineralogy and Petrology》2014,108(1):71-90
Sixteen nephelines from different geological occurrences were sampled at the type-locality, the Somma-Vesuvius volcanic complex (southern Italy), and investigated for their chemistry and crystal structure obtained by both single-crystal and powder X-ray diffraction. Nepheline-bearing samples are metamorphic or from magmatic ejecta and pumice deposits. The lower K contents characterize the pumice- and some metamorphic-derived nephelines, whereas the higher ones are found in some samples from magmatic nodules. The amount of the anorthite molecule, quite low on average, can be more variable in the metamorphic nephelines. The crystal-structure investigations on Somma-Vesuvius samples compare well with previous studies of natural nephelines. All 16 nepheline samples adopt space group P63. The observed lattice parameters vary between 9.9768–9.9946 Å (for a) and 8.3614–8.3777 Å (for c), respectively. Furthermore, chemical analysis revealed that all specimens exhibit an excess of Si relative the ideal Si:Al ratio of 1:1. The analysis of the T-O distances in our samples clearly indicates a distinct ordering process of aluminium and silicon on the tetrahedral sites which is an agreement with Loewenstein’s rule. A linear correlation between the distance of symmetry equivalent split atoms O(1)-O(1)’ and the T(1)-O(1)-T(2) tilt angle was observed. The average <B-O> (B = Na) distances of all crystals are very similar which is consistent with the outcome of the site population refinement indicating full occupancy with sodium. Oriented precession-type sections of reciprocal space indicated the presence of at least the most intense family of satellite peaks, demonstrating that this group of satellite reflections can occur not only in nephelines from pegmatites and ijolites but also in rocks from completely different petrological settings. 相似文献
416.
Serena C. Tarantino Michele Zema Tiziana Boffa Ballaran 《Physics and Chemistry of Minerals》2010,37(10):769-778
The structural evolution of two columbites under pressure, one ferrocolumbite from Raode (Africa) and one manganocolumbite
from Kragero (Norway), has been determined by single-crystal X-ray diffraction. Structural investigations at high pressure
have been carried out on samples which were preliminarily annealed to attain the complete cation-ordered state. For each crystal,
five complete datasets have been collected from room pressure up to ca. 7 GPa. Structure refinements converged to final discrepancy
factors R ranging between 5.2 and 5.8% for both the crystals. Structure refinements of X-ray diffraction data at different pressures
allowed characterisation of the mechanisms by which the columbite structure accommodates variations in pressure. A and B octahedral
volumes in both samples decrease linearly as pressure increases, with a larger compression of the larger A site. The difference
in polyhedral bulk moduli of the A sites for the two samples does not appear to relate directly to the octahedral sizes, the
A site being more compressible in the Fe-rich sample than in the Mn-rich one. By far the most compressible direction in both
the analysed samples is along b. The cations are in fact free to move along this direction, thus allowing the octahedral chains to slide over each other;
this effect is particularly evident in the manganocolumbite sample which shows a steep shortening of interchain A–B distances
along b. 相似文献
417.
Merlin Méheut Michele Lazzeri Etienne Balan Francesco Mauri 《Geochimica et cosmochimica acta》2010,74(14):3874-3882
Hydrogen fractionation laws between selected hydrous minerals (brucite, kaolinite, lizardite, and gibbsite) and perfect water gas have been computed from first-principles quantum-mechanical calculations. The β-factor of each phase was calculated using the harmonic phonon dispersion curves obtained within density functional theory. All the fractionation laws show the same shape, with a minimum between 200 °C (brucite) and 500 °C (gibbsite). At low temperatures, the mineral/liquid water fractionation laws have been obtained using the experimental gas/liquid water fractionation laws. The resulting fractionation laws systematically overestimate measurements by 15‰ at low temperatures to 8‰ at ≈400 °C. Based on this general agreement, all calculated laws were empirically corrected with reference to brucite/water data. These considerations suggest that the experimental or natural calibrations by Xu and Zheng (1999) and Horita et al. (2002) (brucite/water), Gilg and Sheppard (1996) (kaolinite/water), Wenner and Taylor (1973) (lizardite/water), and in some extents Vitali et al. (2001) (gibbsite/water) are representative of equilibrium fractionations. Besides, internal isotopic fractionation of hydrogen between inner-surface and inner hydroxyl groups has been computed for kaolinite and lizardite. The obtained fractionation is large, of opposite sign for the two systems (respectively, −23‰ and +63‰ at 25 °C) and is linear in T-2. Internal fractionation of hydrogen in TO phyllosilicates might thus be used in geothermometry. 相似文献
418.
高精度地下水示踪技术及其应用——以毛村地下河流域为例 总被引:9,自引:0,他引:9
笔者以桂林毛村岩溶地下河流域的示踪试验为例, 探索高精度地下水示踪方法在岩溶水文地质研究中的应用。实践证明, 该方法较传统示踪方法具有较大优势。试验中, 从地下河主出口回收I号示踪剂为34%, 地下水平均流速为35.3 m/h, 全部回收率约为60%~70%。示踪结果证实毛村地下河流域具有典型河间地块特征, 存在多个排泄出口, 水文地质边界较复杂; 主出口处示踪剂浓度变化呈宽域多峰, 说明具有多管道、沿途多个较大溶潭特征; II号示踪剂在所有接收点都没有收到, 其原因较为复杂和不确定。枯季部分地下水有沿西南方向断层排泄迹象, 雨季是否存在较大径流, 还需用示踪试验来证实; 流量不均衡, 排泄区可能存在潜流。 相似文献
419.
Tremolite–calcite veins in the footwall of the Simplon Fault,Antigorio Valley,Lepontine Alps (Italy)
Vito Meggiolaro Michele Sapigni Anna Maria Fioretti 《Swiss Journal of Geoscience》2011,104(3):355-365
The lowermost units of the nappe pile of the Lepontine Alps crop out in the Antigorio valley in the footwall of the Simplon
Fault. The whole orthogneiss section of the Antigorio Unit is exposed on both sides of the valley, sandwiched between the
Mesozoic metasedimentary sequences of the Baceno unit below and the Tèggiolo unit above. The petrography and mineral composition
of tremolite–calcite veins occurring in dolomite marble in both metasedimentary sequences were investigated. Tremolite–calcite
(with lesser talc and minor phlogopite) veins have rhythmic banded texture. Banding is due to cyclic differences in modal
abundances and fabric of tremolite and calcite. These veins are very similar to those occurring in dolomite rafts within the
Bergell granite and it is inferred that they formed by the same “fracture-reaction-seal” mechanism. Veins formed by reaction
of a silica-rich aqueous fluid with the host dolomite marble along fractures. According to thermo-barometric calculations,
based on electron microprobe analyses, reaction occurred at temperatures between 450 and 490°C and minimum pressure of 2–3 kbar.
Such temperature conditions occurred in this footwall region of the Simplon Fault Zone around 15 Ma, during exhumation and
cooling of the nappe pile and a transition to brittle behaviour. Aqueous, silica-rich fluids concentrated along fractures,
forming tremolite–calcite veins in the dolomite marbles and quartz veins in the orthogneiss. 相似文献
420.
Mahmudova Ayisha Borsi Iacopo Porta Giovanni Michele 《Computational Geosciences》2022,26(5):1119-1134
Computational Geosciences - Damage in subsurface formations caused by mineral precipitation decreases the porosity and permeability, eventually reducing the production rate of wells in plants... 相似文献