This paper reports investigation data on the temporal variability of total ozone content (TOC) in the Central Asian and Tibet Plateau mountain regions obtained by conventional methods, as well as by spectral, cross-wavelet, and composite analyses. The data of ground-based observation stations located at Huang He, Kunming, and Lake Issyk-Kul, along with the satellite data obtained at SBUV/SBUV2 (SBUV merged total and profile ozone data, Version 8.6) for 1980–2013 and OMI (Ozone Monitoring Instrument) and TOU (Total Ozone Unit) for 2009–2013 have been used. The average relative deviation from the SBUV/SBUV2 data is less than 1% in Kunming and Issyk-Kul for the period of 1980–2013, while the Huang He Station is characterized by an excess of the satellite data over the ground-based information at an average deviation of 2%. According to the Fourier analysis results, the distribution of amplitudes and the periods of TOC oscillations within a range of over 14 months is similar for all series analyzed. Meanwhile, according to the cross-wavelet and composite analyses results, the phase relationships between the series may considerably differ, especially in the periods of 5–7 years. The phase of quasi-decennial oscillations in the Kunming Station is close to the 11-year oscillations of the solar cycle, while in the Huang He and Issyk-Kul stations the TOC variations go ahead of the solar cycle. 相似文献
The effect law of deformation and failure of a jointed rock mass is essential for underground engineering safety and stability evaluation. In order to study the evolution mechanism and precursory characteristics of instability and failure of jointed rock masses, uniaxial compression and acoustic emission (AE) tests are conducted on sandstones with different joint dip angles. To simulate the mechanical behavior of the rock, a jointed rock mass damage constitutive model with AE characteristic parameters is created based on damage mechanics theory and taking into account the effect of rock mass structure and load coupling. To quantify the mechanism of rock instability, a cusp catastrophe model with AE characteristic parameters is created based on catastrophe theory. The results indicate that when the joint dip angle increases from 0° to 90°, the failure mechanism of sandstone shifts from tensile to shear, with 45° being the critical failure mode. Sandstone's compressive strength reduces initially and subsequently increases, resulting in a U-shaped distribution. The developed damage constitutive model's theoretical curve closely matches the test curve, indicating that the model can reasonably describe the damage evolution of sandstone. The cusp catastrophe model has a high forecast accuracy, and when combined with the damage constitutive model, the prediction accuracy can be increased further. The research results can provide theoretical guidance for the safety and stability evaluation of underground engineering.
A geotechnical information system (GTIS) was constructed within a spatial geographic information system (GIS) framework to
reliably predict geotechnical information and accurately estimate site effects at Gyeongju, an urban area in South Korea.
The system was built based on both collected and performed site investigation data in addition to acquired geo-knowledge data.
Seismic zoning maps were constructed using the site period (TG) and mean shear wave velocity to a depth of 30 m (VS30), and these maps were presented as a regional strategy to mitigate earthquake-induced risks in the study area. In particular,
the TG distribution map indicated the susceptibility to ground motion resonance in periods ranging from 0.2 to 0.5 s and the corresponding
seismic vulnerability of buildings with two to five stories. Seismic zonation of site classification according to VS30 values was also performed to determine the site amplification coefficients for seismic design and seismic performance evaluation
at any site and administrative subunit in the study area. In addition, we investigated the site effects according to subsurface
and surface ground irregularities at Gyeongju by seismic response analyses in time domains based on both two- and three-dimensional
spatial finite element models, which were generated using spatial interface coordinates between geotechnical subsurface layers
predicted by the GTIS. This practical study verified that spatial GIS-based geotechnical information can be a very useful
resource in determining how to best mitigate seismic hazards, particularly in urban areas. 相似文献