492 research outputs found
S-, P- and D-wave resonances in positronium-sodium and positronium-potassium scattering
Scattering of positronium (Ps) by sodium and potassium atoms has been
investigated employing a three-Ps-state coupled-channel model with Ps(1s,2s,2p)
states using a time-reversal-symmetric regularized electron-exchange model
potential fitted to reproduce accurate theoretical results for PsNa and PsK
binding energies. We find a narrow S-wave singlet resonance at 4.58 eV of width
0.002 eV in the Ps-Na system and at 4.77 eV of width 0.003 eV in the Ps-K
system. Singlet P-wave resonances in both systems are found at 5.07 eV of width
0.3 eV. Singlet D-wave structures are found at 5.3 eV in both systems. We also
report results for elastic and Ps-excitation cross sections for Ps scattering
by Na and K.Comment: 9 pages, 5 figures, Accepted in Journal of Physics
Fixed points of Suzuki type generalized multivalued mappings in fuzzy metric spaces with applications
The aim of this paper is to introduce a class of multivalued mappings satisfying a
Suzuki type generalized contractive condition in the framework of fuzzy metric
spaces and to present fixed point results for such mappings. Some examples are
presented to support the results proved herein. As an application, a common fixed
point result for a hybrid pair of single and multivalued mappings is obtained. We
show the existence and uniqueness of a common bounded solution of functional
equations arising in dynamic programming. Our results generalize and extend various
results in the existing literature.http://link.springer.com/journal/11784hb201
Physical and Chemical Properties of Red and Black Soils of Selected Benchmark Spots for Carbon Sequestration Studies in Semi-Arid Tropics of India : Global Theme on Agroecosystems Report no. 35
Physical (nine characteristics) and chemical (14) properties of red and black soils are described: sand, silt, clay, fine clay,
BD, COLE, HC (hydraulic conductivity) and WDC; pH (H2O and KCl), EC, OC, CaCO3, clay CO3, extractable Ca,
Mg, Na, K, CEC, clay CEC, BS and ESP are described in three ecosystems, namely sub-humid (moist and dry) [SH (m)
and SH (d)], semi-arid (moist and dry) [SA (m) and SA (d)] and arid in SAT, India.
Clay contents vary between 30% in arid system to 82% in sub-humid (dry) system and 79% in semi-arid (dry) system.
The red soils contain 8–-55% clay. Fine clay (<0.2 μm) content ranges between 9–54% in red soils; for black soils nearly
50% of total clay (<2 μm) remains in finer (<0.2 μm) fractions. The overall relation between SOC and BD is negative;
however, the correlation between SIC and BD within a depth of 0–30 cm soil depth is positive. Increase in relative
proportion of coarse fragments increases the pore space, effecting decrease in BD values. The inherent relation between
total clay and COLE in different bioclimatic systems indicates a positive correlation with a relatively high value (r = 0.83)
in arid bioclimatic system. Except sub-humid (moist) and arid bioclimates, a positive correlation between COLE and
slickensides is observed in most of the Vertisols in SAT India. A general decreasing trend of SOC with increase in HC
is observed. Conversely, an increasing trend of HC has been found with decrease in SIC. In all the bioclimates, there
is an increasing trend of SOC with decrease in ESP and an increasing trend of SIC with increase in ESP This is due to
preferential release of Ca2+ ions and their precipitation as CaCO3 in soil, thereby increasing the relative concentration
of Na+ ions in the exchange complex effecting high value of ESP In general, a positive correlation between amount of
fine clay and SOC in surface soils has been found.
The SOC values in the surface (0–30 cm) follow the trend of forest system > permanent fallow (grassland), horticultural
system > agricultural system > wasteland. Surface soils of agricultural and horticultural systems store higher SIC as
compared to other systems. The surface soils of semi-arid (moist) show higher SOC under agricultural system due to
inclusion of sun hemp for green manuring in crop rotation. The average SOC values follow the trend of SA (m) (0.825%)
> SH (d) (0.804%) > SH (m) (0.642%) > SA (d) (0.633%) > arid (0.594%) for black soils under agricultural system.
The values of SOC follow the trend of SH (m) (1.35) > SA (d) (0.84) > SA (m) (0.70) for the red soils used for
cultivation.
The level of SIC values in surface soils under agricultural system followed the trend of arid (2.34%) > SH (d) (1.06%)
> SA (m) (0.99%) > SA (d) (0.94%) > SH (m) (0.54%) for black soils. In red soils, CaCO3 in general is not found
except in soils of semi-arid (dry) bioclimatic system.
The SOC in surface horizon under agricultural systems shows higher values for cereal-based system (0.79%), followed
by soybean systems (0.70%) and cotton-based systems (0.68%). Interestingly, the SIC values have been found to be the
highest in cotton-based systems (1.53%), followed by soybean-based systems (0.66%) and cereal-based systems (0.29%).
This trend is opposite to that of the corresponding SOC values.
With the help of data generated, 14 systems (five in cotton, three in soybean, four in cereals, one in horticulture and
one under forest) have been identified as ideal for organic carbon sequestration, keeping in view the existing level of
management practices vis-à-vis soil health
Search of the early O3 LIGO data for continuous gravitational waves from the Cassiopeia A and Vela Jr. supernova remnants
partially_open1412sìWe present directed searches for continuous gravitational waves from the neutron stars in the Cassiopeia A (Cas A) and Vela Jr. supernova remnants. We carry out the searches in the LIGO detector data from the first six months of the third Advanced LIGO and Virgo observing run using the weave semicoherent method, which sums matched-filter detection-statistic values over many time segments spanning the observation period. No gravitational wave signal is detected in the search band of 20–976 Hz for assumed source ages greater than 300 years for Cas A and greater than 700 years for Vela Jr. Estimates from simulated continuous wave signals indicate we achieve the most sensitive results to date across the explored parameter space volume, probing to strain magnitudes as low as
∼6.3×10^−26 for Cas A and ∼5.6×10^−26 for Vela Jr. at frequencies near 166 Hz at 95% efficiency.openAbbott, R.; Abbott, T. D.; Acernese, F.; Ackley, K.; Adams, C.; Adhikari, N.; Adhikari, R. X.; Adya, V. B.; Affeldt, C.; Agarwal, D.; Agathos, M.; Agatsuma, K.; Aggarwal, N.; Aguiar, O. D.; Aiello, L.; Ain, A.; Ajith, P.; Albanesi, S.; Allocca, A.; Altin, P. A.; Amato, A.; Anand, C.; Anand, S.; Ananyeva, A.; Anderson, S. B.; Anderson, W. G.; Andrade, T.; Andres, N.; Andrić, T.; Angelova, S. V.; Ansoldi, S.; Antelis, J. M.; Antier, S.; Appert, S.; Arai, K.; Araya, M. C.; Areeda, J. S.; Arène, M.; Arnaud, N.; Aronson, S. M.; Arun, K. G.; Asali, Y.; Ashton, G.; Assiduo, M.; Aston, S. M.; Astone, P.; Aubin, F.; Austin, C.; Babak, S.; Badaracco, F.; Bader, M. K. M.; Badger, C.; Bae, S.; Baer, A. M.; Bagnasco, S.; Bai, Y.; Baird, J.; Ball, M.; Ballardin, G.; Ballmer, S. W.; Balsamo, A.; Baltus, G.; Banagiri, S.; Bankar, D.; Barayoga, J. C.; Barbieri, C.; Barish, B. 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M.; Maggiore, R.; Magnozzi, M.; Mahesh, S.; Majorana, E.; Makarem, C.; Maksimovic, I.; Maliakal, S.; Malik, A.; Man, N.; Mandic, V.; Mangano, V.; Mango, J. L.; Mansell, G. L.; Manske, M.; Mantovani, M.; Mapelli, M.; Marchesoni, F.; Marion, F.; Mark, Z.; Márka, S.; Márka, Z.; Markakis, C.; Markosyan, A. S.; Markowitz, A.; Maros, E.; Marquina, A.; Marsat, S.; Martelli, F.; Martin, I. W.; Martin, R. M.; Martinez, M.; Martinez, V. A.; Martinez, V.; Martinovic, K.; Martynov, D. V.; Marx, E. J.; Masalehdan, H.; Mason, K.; Massera, E.; Masserot, A.; Massinger, T. J.; Masso-Reid, M.; Mastrogiovanni, S.; Matas, A.; Mateu-Lucena, M.; Matichard, F.; Matiushechkina, M.; Mavalvala, N.; McCann, J. J.; McCarthy, R.; McClelland, D. E.; McClincy, P. K.; McCormick, S.; McCuller, L.; McGhee, G. I.; McGuire, S. C.; McIsaac, C.; McIver, J.; McRae, T.; McWilliams, S. T.; Meacher, D.; Mehmet, M.; Mehta, A. K.; Meijer, Q.; Melatos, A.; Melchor, D. A.; Mendell, G.; Menendez-Vazquez, A.; Menoni, C. 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All-sky search for gravitational wave emission from scalar boson clouds around spinning black holes in LIGO O3 data
Search for continuous gravitational wave emission from the Milky Way center in O3 LIGO-Virgo data
Search for gravitational waves from Scorpius X-1 with a hidden Markov model in O3 LIGO data
Results are presented for a semi-coherent search for continuous gravitational waves from the low-mass X-ray binary Scorpius X-1, using a hidden Markov model (HMM) to allow for spin wandering. This search improves on previous HMM-based searches of Laser Interferometer Gravitational-wave Observatory (LIGO) data by including the orbital period in the search template grid, and by analyzing data from the latest (third) observing run (O3). In the frequency range searched, from 60 to 500 Hz, we find no evidence of gravitational radiation. This is the most sensitive search for Scorpius X-1 using a HMM to date. For the most sensitive sub-band, starting at Hz, we report an upper limit on gravitational wave strain (at confidence) of , assuming the orbital inclination angle takes its electromagnetically restricted value . The upper limits on gravitational wave strain reported here are on average a factor of lower than in the O2 HMM search. This is the first Scorpius X-1 HMM search with upper limits that reach below the indirect torque-balance limit for certain sub-bands, assuming
Search for Subsolar-Mass Binaries in the First Half of Advanced LIGO’s and Advanced Virgo’s Third Observing Run
Constraints on dark photon dark matter using data from LIGO's and Virgo's third observing run
We present a search for dark photon dark matter that could couple to
gravitational-wave interferometers using data from Advanced LIGO and Virgo's
third observing run. To perform this analysis, we use two methods, one based on
cross-correlation of the strain channels in the two nearly aligned LIGO
detectors, and one that looks for excess power in the strain channels of the
LIGO and Virgo detectors. The excess power method optimizes the Fourier
Transform coherence time as a function of frequency, to account for the
expected signal width due to Doppler modulations. We do not find any evidence
of dark photon dark matter with a mass between eV/, which corresponds to frequencies between 10-2000
Hz, and therefore provide upper limits on the square of the minimum coupling of
dark photons to baryons, i.e. dark matter. For the
cross-correlation method, the best median constraint on the squared coupling is
at eV/; for the
other analysis, the best constraint is at eV/. These limits improve upon those obtained
in direct dark matter detection experiments by a factor of for
eV/, and are, in absolute terms, the
most stringent constraint so far in a large mass range eV/.Comment: 20 pages, 7 figure
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