3,946 research outputs found
Hydroclimatic variability in loess delta D-wax records from the central Chinese Loess Plateau over the past 250 ka
This study reports hydrogen isotopic records from the central Chinese Loess Plateau (CLP) over the past 250 ka. After eliminating the influence of ice and local temperatures, the delta D-wax records extracted from two loess sites at Xifeng and Luochuan can be taken to represent arid/humid alternations in the hydrological environment in this marginal Asian Summer Monsoon (ASM) region; they also contain integrated information on summer precipitation patterns and the corresponding responses to these changes by predominant vegetation cover types. These arid/humid alternations show 100 ka, 40 ka and 20 ka cycles. An increase in precipitation in association with an enhanced summer monsoon has historically been taken to be the major factor driving a humid environment in the central CLP. However, hydroclimatic changes in delta D-wax records differ for the central CLP, central China and southern China. Over a 20 ka cycle, the influence of solar insolation on hydroclimatic changes can be shown to be consistent throughout the central CLP. However, changes in the relative location of the land and sea may have caused different hydroclimatic responses between southern China and the central CLP on a glacial-interglacial scale. The hydroclimatic variability in the central CLP would suggest that an enhanced summer monsoon due to climatic warming is the key to understanding decreased drought degree in this marginal monsoonal region
Developments of a 2D Position Sensitive Neutron Detector
Chinese Spallation Neutron Source (CSNS), one project of the 12th
five-year-plan scheme of China, is under construction in Guangdong province.
Three neutron spectrometers will be installed at the first phase of the
project, where two-dimensional position sensitive thermal neutron detectors are
required. Before the construction of the neutron detector, a prototype of
two-dimensional 200 mmx200 mm Multi-wire Proportional Chamber (MWPC) with the
flowing gas of Ar/CO2 (90/10) has been constructed and tested with the 55Fe
X-Ray using part of the electronics in 2009, which showed a good performance.
Following the test in 2009, the neutron detector has been constructed with the
complete electronics and filled with the 6atm.3He + 2.5atm.C3H8 gas mixture in
2010. The neutron detector has been primarily tested with an Am/Be source. In
this paper, some new developments of the neutron detector including the design
of the high pressure chamber, the optimization of the gas purifying system and
the gas filling process will be reported. The results and discussion are also
presented in this paper.Comment: 5 page
An operator approach to the rational solutions of the classical Yang-Baxter equation
Motivated by the study of the operator forms of the constant classical
Yang-Baxter equation given by Semonov-Tian-Shansky, Kupershmidt and the others,
we try to construct the rational solutions of the classical Yang-Baxter
equation with parameters by certain linear operators. The fact that the
rational solutions of the CYBE for the simple complex Lie algebras can be
interpreted in term of certain linear operators motivates us to give the notion
of -operators such that these linear operators are the -operators associated to the adjoint representations. Such a study can be
generalized to the Lie algebras with nondegenerate symmetric invariant bilinear
forms. Furthermore we give a construction of a rational solution of the CYBE
from an -operator associated to the coadjoint representation and an
arbitrary representation with a trivial product in the representation space
respectively.Comment: 23page
Geochemistry of magmatic and hydrothermal zircon from the highly evolved Baerzhe alkaline granite: implications for Zr-REE-Nb mineralization
Source-Frequency Phase-Referencing Observation of AGNs with KaVA Using Simultaneous Dual-Frequency Receiving
The KVN(Korean VLBI Network)-style simultaneous multi-frequency receiving
mode is demonstrated to be promising for mm-VLBI observations. Recently, other
Very long baseline interferometry (VLBI) facilities all over the globe start to
implement compatible optics systems. Simultaneous dual/multi-frequency VLBI
observations at mm wavelengths with international baselines are thus possible.
In this paper, we present the results from the first successful simultaneous
22/43 GHz dual-frequency observation with KaVA(KVN and VERA array), including
images and astrometric results. Our analysis shows that the newly implemented
simultaneous receiving system has brought a significant extension of the
coherence time of the 43 GHz visibility phases along the international
baselines. The astrometric results obtained with KaVA are consistent with those
obtained with the independent analysis of the KVN data. Our results thus
confirm the good performance of the simultaneous receiving systems for the
non-KVN stations. Future simultaneous observations with more global stations
bring even higher sensitivity and micro-arcsecond level astrometric
measurements of the targets.Comment: 8 pages, 6 figures, Published in JKA
Pairing symmetry and properties of iron-based high temperature superconductors
Pairing symmetry is important to indentify the pairing mechanism. The
analysis becomes particularly timely and important for the newly discovered
iron-based multi-orbital superconductors. From group theory point of view we
classified all pairing matrices (in the orbital space) that carry irreducible
representations of the system. The quasiparticle gap falls into three
categories: full, nodal and gapless. The nodal-gap states show conventional
Volovik effect even for on-site pairing. The gapless states are odd in orbital
space, have a negative superfluid density and are therefore unstable. In
connection to experiments we proposed possible pairing states and implications
for the pairing mechanism.Comment: 4 pages, 1 table, 2 figures, polished versio
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Where were the monsoon regions and arid zones in Asia prior to the Tibetan Plateau uplift?
The impact of the Tibetan Plateau uplift on the Asian monsoons and inland arid climates is an important but also controversial question in studies of paleoenvironmental change during the Cenozoic. In order to achieve a good understanding of the background for the formation of the Asian monsoons and arid environments, it is necessary to know the characteristics of the distribution of monsoon regions and arid zones in Asia before the plateau uplift. In this study, we discuss in detail the patterns of distribution of the Asian monsoon and arid regions before the plateau uplift on the basis of modeling results without topography from a global coupled atmosphere–ocean general circulation model, compare our results with previous simulation studies and available biogeological data, and review the uncertainties in the current knowledge. Based on what we know at the moment, tropical monsoon climates existed south of 20°N in South and Southeast Asia before the plateau uplift, while the East Asian monsoon was entirely absent in the extratropics. These tropical monsoons mainly resulted from the seasonal shifts of the Inter-Tropical Convergence Zone. There may have been a quasi-monsoon region in central-southern Siberia. Most of the arid regions in the Asian continent were limited to the latitudes of 20–40°N, corresponding to the range of the subtropical high pressure year-around. In the meantime, the present-day arid regions located in the relatively high latitudes in Central Asia were most likely absent before the plateau uplift. The main results from the above modeling analyses are qualitatively consistent with the available biogeological data. These results highlight the importance of the uplift of the Tibetan Plateau in the Cenozoic evolution of the Asian climate pattern of dry–wet conditions. Future studies should be focused on effects of the changes in land–sea distribution and atmospheric CO2 concentrations before and after the plateau uplift, and also on cross-comparisons between numerical simulations and geological evidence, so that a comprehensive understanding of the evolution of the Cenozoic paleoenvironments in Asia can be achieved
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