scholarly journals Northward dispersal of sea kraits (Laticauda semifasciata) beyond their typical range

PLoS ONE ◽  
2017 ◽  
Vol 12 (6) ◽  
pp. e0179871 ◽  
Author(s):  
Jaejin Park ◽  
Il-Hun Kim ◽  
Jonathan J. Fong ◽  
Kyo-Soung Koo ◽  
Woo-Jin Choi ◽  
...  
Keyword(s):  
Laticauda Semifasciata ◽  
Typical Range

Inverse design of layered periodic wave barriers based on deep learning

2021 ◽  
pp. 146442072110168
Author(s):  
Chen-Xu Liu ◽  
Gui-Lan Yu
Keyword(s):  
Deep Learning ◽  
Activation Function ◽  
Periodic Wave ◽  
P Wave ◽  
Soil Parameters ◽  
S Wave ◽  
Output Frequency ◽  
Great Generality ◽  
Typical Range ◽  
Deep Learning Model

This study presents an approach based on deep learning to design layered periodic wave barriers with consideration of typical range of soil parameters. Three cases are considered where P wave and S wave exist separately or simultaneously. The deep learning model is composed of an autoencoder with a pretrained decoder which has three branches to output frequency attenuation domains for three different cases. A periodic activation function is used to improve the design accuracy, and condition variables are applied in the code layer of the autoencoder to meet the requirements of practical multi working conditions. Forty thousand sets of data are generated to train, validate, and test the model, and the designed results are highly consistent with the targets. The presented approach has great generality, feasibility, rapidity, and accuracy on designing layered periodic wave barriers which exhibit good performance in wave suppression in targeted frequency range.

Complete nucleotide sequences of cDNAs encoding long chain α-neurotoxins from sea krait, Laticauda semifasciata

Toxicon ◽  
1999 ◽  
Vol 37 (1) ◽  
pp. 181-185 ◽  
Author(s):  
Toru Tamiya ◽  
Satoshi Ohno ◽  
Eisaku Nishimura ◽  
Takahiko J. Fujimi ◽  
Takahide Tsuchiya
Keyword(s):  
Nucleotide Sequences ◽  
Laticauda Semifasciata ◽  
Long Chain

scholarly journals Compactness by Coarse-Graining in Long-Range Lattice Systems

2020 ◽  
Vol 20 (4) ◽  
pp. 783-794
Author(s):  
Andrea Braides ◽  
Margherita Solci
Keyword(s):  
Long Range ◽  
Coarse Graining ◽  
Interaction Energies ◽  
Lattice Systems ◽  
Range Interaction ◽  
Surface Energies ◽  
Continuum Analysis ◽  
Long Range Interaction ◽  
Typical Range ◽  
Limit Energy

AbstractWe consider energies on a periodic set {\mathcal{L}} of the form {\sum_{i,j\in\mathcal{L}}a^{\varepsilon}_{ij}\lvert u_{i}-u_{j}\rvert}, defined on spin functions {u_{i}\in\{0,1\}}, and we suppose that the typical range of the interactions is {R_{\varepsilon}} with {R_{\varepsilon}\to+\infty}, i.e., if {\lvert i-j\rvert\leq R_{\varepsilon}}, then {a^{\varepsilon}_{ij}\geq c>0}. In a discrete-to-continuum analysis, we prove that the overall behavior as {\varepsilon\to 0} of such functionals is that of an interfacial energy. The proof is performed using a coarse-graining procedure which associates to scaled functions defined on {\varepsilon\mathcal{L}} with equibounded energy a family of sets with equibounded perimeter. This agrees with the case of equibounded {R_{\varepsilon}} and can be seen as an extension of coerciveness result for short-range interactions, but is different from that of other long-range interaction energies, whose limit exits the class of surface energies. A computation of the limit energy is performed in the case {\mathcal{L}=\mathbb{Z}^{d}}.

Mathematical Modelling of Deciduous Tree Ignition by Ground Lightning Discharge Taking into Account Localization of Reactive Wood

2011 ◽  
Vol 6 (4) ◽  
pp. 95-106
Author(s):  
Nikolay Baranovskiy ◽  
Geniy Kuznetsov
Keyword(s):  
Heat Transfer ◽  
Numerical Simulation ◽  
Mathematical Modelling ◽  
Lightning Discharge ◽  
Deciduous Tree ◽  
Tree Trunk ◽  
Mathematical Statement ◽  
Cylindrical System ◽  
Typical Range

Physical and mathematical statement and results of the numerical simulation of a problem about deciduous tree (birch) ignition by ground lightning discharge are presented. The problem is considered in flat statement in cylindrical system of coordinates. Heat transfer features taking into account localization of reactive wood are considered. The parametrical analysis is carried out and conditions of tree trunk ignition in a typical range of parameters of influence of positive discharges are obtained

scholarly journals The positive relationship between face identification and facial emotion perception ability extends to super-recognisers

2020 ◽  
Author(s):  
Linda Ali ◽  
Josh P Davis
Keyword(s):  
Theoretical Perspective ◽  
Emotion Perception ◽  
Common Mechanism ◽  
Face Identification ◽  
Large Individual ◽  
Face Memory ◽  
Face Identity ◽  
Face Matching ◽  
Identity Processing ◽  
Typical Range

Large individual differences in face identification ability and face emotion perception ability correlate in the neurotypical population. The current study recruited a large sample of participants aged 18-70-years (n = 687). The sample included super-recognisers with exceptional face identity processing skills (n = 74) to determine whether the relationship extends to the top of the ability spectrum. Participants completed one short-term face memory test, a simultaneous face matching test, and two face emotion perception tests. Face memory and face matching scores were moderately positively correlated with each other, and with total scores on the two face emotion perception tests. Super-recognisers outperformed typical-range ability controls at the perception of anger, fear, happy, and neutral, but not disgust or sadness. Identity processing and emotion perception accuracy across the whole sample was influenced by gender and age. From a theoretical perspective, these results demonstrate that correlations found between typical-range ability participants also extend to the top end of the face identification spectrum, implying that a common mechanism may drive performance. Practically, super-recognisers possessing superior face identity processing and emotion perception might enhance the performance of organisations such as police forces or security that rely on these attributes in their staff.

scholarly journals On the role of higher alcohols in the characterization of cachaça

2020 ◽  
Vol 9 (10) ◽  
pp. e8299109135
Author(s):  
Amazile Biagioni Maia ◽  
Lorena Simão Marinho ◽  
David Lee Nelson
Keyword(s):  
Isoamyl Alcohol ◽  
Raw Material ◽  
Alcoholic Beverages ◽  
Higher Alcohols ◽  
Isobutyl Alcohol ◽  
Higher Alcohol ◽  
Three Samples ◽  
Typical Range

There is a growing interest in chemical markers for the identification and certification of cachaça as a cane spirit produced in Brazil. It is known that the higher alcohols that are usually analyzed (propyl alcohol, Isobutyl alcohol and isoamyl alcohol) occur in all alcoholic beverages (fermented and distilled), but the relative proportions can vary markedly according to the peculiarities of the raw material and the production process. In this work, the contents of higher alcohols in 300 samples of alembic cachaça were compared, 220 from the state of Minas Gerais and 80 from other states, as well as three samples of industrial cachaça and 14 samples of whiskeys of various brands. The typical range of total higher alcohols in cachaça was 180-360 mg/100 mL ethanol. Cachaça containing higher alcohol concentrations greater than 360 mg/100 mL ethanol do not comply with Brazilian legislation. However, cachaças with higher alcohols concentrations below 180 mg/100 mL ethanol, as was found in one of the industrial cachaças, signify adulteration, for example, by mixing with fuel alcohol. The C4/C5 ratio varied less than the C3/C5 ratio, being consistently within the range of 0.20-0.50. In the whiskeys analyzed, the concentrations of higher alcohols were in the range of 160 and 270 mg/100 mL. Therefore, this parameter would not assist in differentiating between cachaça and whiskey. But the C4/C5 ratio was consistently different, being always greater than 0.50 for the whiskeys. Thus, the routine analysis of higher alcohols provides useful information both for tracking possible fraud and for assessments related to the identity or origin of cachaça.

The ellipsoidal form of clasts with practical applications to fabric and size analyses of fluvial gravels

1980 ◽  
Vol 17 (12) ◽  
pp. 1725-1739 ◽  
Author(s):  
Emlyn H. Koster ◽  
Brian R. Rust ◽  
Don J. Gendzwill
Keyword(s):  
Statistical Analysis ◽  
Flow Direction ◽  
Probability Distributions ◽  
Size Analysis ◽  
Shape Variation ◽  
Practical Applications ◽  
Flow Interactions ◽  
Typical Range ◽  
Plane Area ◽  
Key Parameter

The widespread assumption that most water-worn gravel clasts approximate ellipsoids is confirmed by a statistical analysis of available data. The analysis demonstrates a Gaussian distribution of V/Ve ratios, centred on unit ratio, where V is clast volume and Ve the volume of a symmetric ellipsoid with equivalent triaxial dimensions. For internally isotropic and unbroken clasts, ellipsoidal form evolves as the rounding due to abrasion reaches its final stages. There appears to be no other major control on the tendency towards ellipsoidal geometry. The ellipsoidal tendency assists the interpretation of fluvial gravel deposits, which depends greatly on accurate description of clast size and fabric.Firstly, it facilitates calculation of Ap, the plane area projected upstream by clasts, a key parameter in bed–flow interactions such as preferred fabric. Formulae are derived to calculate Ap for ellipsoidal clasts with any configuration relative to flow direction. Viewing fabric in terms of the Ap variable supports and explains earlier conclusions concerning the controls on variability of imbrication angle.Secondly, an investigation of the relative merits of six size measures as descriptors of areal trends and predictors of nominal diameter, dn, concludes that (abc)1/3(the formula for dn of an ellipsoid) is superior. Other measures, namely, a, b, c, (a + c)/2, and (a + b + c)/3, are all subject to error in proportion to the degree of shape variation. Also, since downstream fining is typically accompanied by a changing proportion of oblate, bladed, prolate, and equant forms, dn is subject to inconsistent levels of under- or overestimation. The commonly used b dimension is endorsed as an acceptable predictor of dn, but a severely overestimates dn and should be abandoned. Information on errors in size analysis is presented as nomograms in the form of contoured c/b versus b/a plots and as probability distributions based on the typical range of shape variation in fluvial gravel.

scholarly journals Redox state of southern Tibetan upper mantle and ultrapotassic magmas

Geology ◽  
2020 ◽  
Vol 48 (7) ◽  
pp. 733-736 ◽  
Author(s):  
Weikai Li ◽  
Zhiming Yang ◽  
Massimo Chiaradia ◽  
Yong Lai ◽  
Chao Yu ◽  
...  
Keyword(s):  
Upper Mantle ◽  
Lithospheric Mantle ◽  
Redox State ◽  
Volcanic Rocks ◽  
Mantle Xenoliths ◽  
Continental Plate ◽  
Cratonic Mantle ◽  
Tectonic Settings ◽  
Mantle Condition ◽  
Typical Range

Abstract The redox state of Earth’s upper mantle in several tectonic settings, such as cratonic mantle, oceanic mantle, and mantle wedges beneath magmatic arcs, has been well documented. In contrast, oxygen fugacity () data of upper mantle under orogens worldwide are rare, and the mechanism responsible for the mantle condition under orogens is not well constrained. In this study, we investigated the of mantle xenoliths derived from the southern Tibetan lithospheric mantle beneath the Himalayan orogen, and that of postcollisional ultrapotassic volcanic rocks hosting the xenoliths. The of mantle xenoliths ranges from ΔFMQ = +0.5 to +1.2 (where ΔFMQ is the deviation of log from the fayalite-magnetite-quartz buffer), indicating that the southern Tibetan lithospheric mantle is more oxidized than cratonic and oceanic mantle, and it falls within the typical range of mantle wedge values. Mineralogical evidence suggests that water-rich fluids and sediment melts liberated from both the subducting Neo-Tethyan oceanic slab and perhaps the Indian continental plate could have oxidized the southern Tibetan lithospheric mantle. The conditions of ultrapotassic magmas show a shift toward more oxidized conditions during ascent (from ΔFMQ = +0.8 to +3.0). Crustal evolution processes (e.g., fractionation) could influence magmatic , and thus the redox state of mantle-derived magma may not simply represent its mantle source.

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