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541.
Sławomir Jerzy Gibowicz 《Acta Geophysica》2006,54(2):142-157
The following criteria for selection of doublets at Polish coal mines were accepted: the difference in magnitude (based on
seismic moment) of two events not larger than 0.15, the distance between their hypocenters not greater than 150 m, and the
time interval between their occurrence not longer than 10 days. Similarly, the criteria for seismic events at copper mines
are: the difference in magnitude not exceeding 0.15, the distance not greater than 200 m, and the time interval not longer
than 20 days. Seismic events from the Wujek and Ziemowit coal mines that occurred between 1993 and 1995, and seismic events
from the Polkowice copper mine that occurred between 1994 and 1996 and from the Rudna copper mine that occurred between 1994
and 2004 were considered. Their source parameters and focal mechanisms were known in most cases from previous studies. Altogether
108 seismic pairs from coal mines and 118 pairs from copper mines were found, forming doublets, triplets and quadruplets,
within the magnitude range from 0.7 to 3.5. The distance and time intervals between two events forming pairs are not dependent
on magnitude of these events.
The focal mechanism of seismic events forming pairs is similar in over 60 percent of pairs at coal mines and in about one
third of pairs at copper mines. Spatial distributions of doublets in particular sections of coal and copper mines display
dominant linear trends, characteristic for a given area, which are often in conformity with the direction of nodal planes
determined by fault plane solution of one or both the events forming a doublet. In such cases, the rupture plane can be discriminated
among the nodal planes. 相似文献
542.
This paper concerns an analysis of the accuracy of the estimated parameters Ω (Φ, Λ, ω) which define the tectonic plate motions. The study is based on the velocities of station positions in the IERS (International Earth Rotation and Reference Systems Service) which has published new realization of the International Terrestrial Reference System—ITRF2008 for Doppler Orbitography by Radiopositioning Integrated on Satellite DORIS technique. Eurasian, African, Australian, North American, Australian, Pacific, Antarctic and South American plates were used in the analysis. The influence of the number and localization of stations on the plate surface on the estimation accuracy of the tectonic plate motion parameters were discussed. The results were compared with the APKIM 2005 IGN model and our earlier estimation for the SLR technique. In general, a remarkable concurrent agreement between the present and the APKIM 2005 solutions was found. 相似文献
543.
Radosław Rek 《Solar physics》2010,267(2):361-375
Solar flares take place in regions of strong magnetic fields and are generally accepted to be the result of a resistive instability
leading to magnetic reconnection. When new flux emerges into a pre-existing active region it can act as a flare and coronal
mass ejection trigger. In this study we observed active region 10955 after the emergence of small-scale additional flux at
the magnetic inversion line. We found that flaring began when additional positive flux levels exceeded 1.38×1020 Mx (maxwell), approximately 7 h after the initial flux emergence. We focussed on the pre-flare activity of one B-class flare
that occurred on the following day. The earliest indication of activity was a rise in the non-thermal velocity one hour before
the flare. 40 min before flaring began, brightenings and pre-flare flows were observed along two loop systems in the corona,
involving the new flux and the pre-existing active region loops. We discuss the possibility that reconnection between the
new flux and pre-existing loops before the flare drives the flows by either generating slow mode magnetoacoustic waves or
a pressure gradient between the newly reconnected loops. The subsequent B-class flare originated from fast reconnection of
the same loop systems as the pre-flare flows. 相似文献
544.
The influence of meander bend evolution on the formation of multiple cutoffs: findings inferred from floodplain architecture and bend geometry 下载免费PDF全文
Marcin Słowik 《地球表面变化过程与地形》2016,41(5):626-641
The evolution of meander bends and formation of cutoffs, including a series of cutoffs developed simultaneously in a number of bends, have been investigated by many researchers. However, relatively little is known about factors that lead to the development of multiple cutoffs that are formed subsequently at one location. The present study aims to determine the influence of meander bend development on multiple chute cutoff formation in a single bend. The research is based on the sedimentary record of meander migration and cutoffs preserved in a lowland river floodplain (the lower Obra River, Poland). Analysis of changes in meander geometry was conducted to describe the influence of their migration on cutoff formation and in other rivers where multiple cutoffs occurred. The results showed that multiple cutoffs in the lower Obra River have occurred during the last 3000 years, owing to the interaction of upstream and downstream controls: migration of meander bends in opposing directions accompanied by an increase of flood frequency and sediment supply. The flow and sediment supply has been further altered since the nineteenth century due to anthropogenic impacts: an artificial cutoff of the downstream bend and elevation of channel levées. Similar mechanisms driving the formation of multiple cutoff have been found in other river courses, despite significantly higher energy of the compared rivers. Moreover, development of a confined‐shape bend (caused by artificial barrier or autogenic bend behaviour) may also favour the formation of multiple cutoffs. However, counter migration of meanders enhanced by increased flood frequency and sediment supply are primary triggers for such events. Copyright © 2015 John Wiley & Sons, Ltd. 相似文献
545.
Szutowicz Sławomira Królikowska Małgorzata Sitarski Grzegorz 《Earth, Moon, and Planets》2002,90(1-4):119-130
The role of non-gravitational forces in the evolution of orbitalmotion of C/1995 O1 (Hale–Bopp) has been investigated. Inorbital
calculations the observational material covering theperiod from April 1993 up to August 2001 was used. To model thenon-gravitational
acceleration, observed and theoretical profilesof the H2O production rates were employed. A set of forcedprecession models of a rotating cometary nucleus consistent withthe observed
spin axis orientation was fitted to positionalobservations. The non-gravitational models allowed us to constrainthe mass and
radius of the comet. The orbitalevolution of Comet Hale–Bopp was investigated over ±400 k yusing two sets of randomly varied
orbital elements wellrepresenting all positional observations in the pure gravitationalcase, as well as in the non-gravitational
case. The calculationsshowed that the comet's motion is predictable only over an interval ofa few orbital periods. The statistical
conclusions changesignificantly when non-gravitational effects are included in the analysis. 相似文献
546.
547.
Winkelmann Karol Żyliński Kamil Korzec Aleksandra Górski Jarosław 《Geotechnical and Geological Engineering》2022,40(9):4705-4720
Geotechnical and Geological Engineering - This work conducts a probabilistic inquiry on how the variability of the parameter defining soil deformability affects the settlement of the foundation... 相似文献
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