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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Computing 42 (1989), S. 141-158 
    ISSN: 1436-5057
    Keywords: Primary 68M15 ; secondary 65C20 ; SW engineering ; SW test phases ; residual errors of SW ; SW management ; SW for ISDN-PABX ; reliability modeling ; SW metrics
    Source: Springer Online Journal Archives 1860-2000
    Topics: Computer Science
    Description / Table of Contents: Zusammenfassung Diese Arbeit ist ein Beitrag zur besseren Beherrschung der teuren und langen Testphasen bei der Software-Entwicklung. Ein numerisches Verfahren für prognosen während des Tests großer Software-Systeme wird vorgestellt, das wesentliche Änderungen des Testobjekts bzw. des Testverfahrens berücksichtigt. Das modell ist adaptiv, d. h. die Komplexität des Modells wird durch den betrachteten realen Test gesteuert. Deshalb kann sehr früh die Zahl der zukünftigen Fehlermeldungen in Abhängigkeit der Testaktivität, die Zahl der Restfehler und das Testende prognostiziert werden. Dadurch sind korrigierende Eingriffe in den Test noch rechtzeitig möglich. Die Prognosen wurden während der Entwicklung des weltweit ersten ISDN-Kommunkationscomputers HICOM und anderer Projekte erfolgreich angewendet.
    Notes: Abstract This paper proposes an improved way of controlling the costly and tedious test phases involved in software development. It presents a numerical method of making forecasts while testing large software systems. This method takes into account major changes to the test object and the test method. The model is adaptive; that is, the complexity of the model is controlled by the real test considered here. The number of future errors according to test activities, the number of residual errors and the end of testing can therefore be predicted at a very early stage. Corrective action to adapt the test can thus be taken in good time. The forecasts have been successfully applied to the development of the world's first ISDN communication computer HICOM and other projects.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2015-04-04
    Description: Microseismic monitoring from large arrays using migration-based detection and location techniques is limited by detections of false positive events, which are the interpretation of spurious/noisy signals as real events. Therefore, semblance has been considered to differentiate between false positive and true events. However, semblance by itself is not suitable for variable signals such as those caused by shear source radiation. We present a new methodology for event detection and location using semblance of amplitudes corrected by a source mechanism. Our method is suitable for multichannel processing of microseismic data sets acquired with large arrays. The amplitudes are corrected by the radiation pattern of the inverted source mechanism before the semblance computation. We show that the source mechanism correction is the key factor in maximizing the value of semblance and makes the detection based on semblance superior to simple stacking. We apply this method to a data set recorded by a large surface star-like array on synthetic as well as on field data.
    Keywords: Seismology
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 3
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    Society of Exploration Geophysicists (SEG)
    Publication Date: 2014-12-09
    Description: Determination of moment and moment magnitude for seismic events located by stacking has been an unsolved problem because current methodologies cannot be applied. To solve this problem, we have developed a methodology for moment magnitude $${M}_{w}$$ estimation of (micro) seismic events. Our method was designed for stacking waveforms. We found that magnitude can be determined from the stack of amplitudes corrected for radiation pattern and propagation effects such as geometric spreading, attenuation, and free-surface boundary. From the stack of corrected waveforms, we found the low-frequency limit corresponding to the stack of particle displacement and calculated seismic moment. We found that an unstacked method of estimating moment magnitude on each trace and averaging these estimates was consistent with the method we developed although it was limited to higher magnitude events and more sensitive to noise. We benchmarked our methodology with a case study and found improvement in $${M}_{w}$$ estimation resulting in determination of magnitude for weaker events when unstacked methodology cannot be used.
    Print ISSN: 0016-8033
    Electronic ISSN: 1942-2156
    Topics: Geosciences , Physics
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  • 4
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    Society of Exploration Geophysicists (SEG)
    Publication Date: 2015-01-21
    Description: Microseismic monitoring has become a tool of choice for the development and optimization of oil and gas production from unconventional reservoirs. The primary objective of (micro) seismic monitoring includes localization of (micro) seismic events and characterization of their source mechanisms. Most seismic events are of a nonexplosive nature, and thus, there are waveform (polarity) differences among receivers. Specifically, double-couple sources represented a challenge for migration-based localization techniques. We developed and applied a new migration-type location technique combined with source mechanism inversion that allowed for constructive interference of signal in seismic waveforms. The procedure included constructing image functions by stacking the amplitudes with compensated polarity changes. The compensation weights were calculated by using moment tensor inversion. This method did not require any picking of arrivals at individual receivers, but it required receivers to be distributed in multiple azimuths and offsets. This made the technique suitable for surface or near-surface monitoring, in which a low signal-to-noise ratio (S/N) can be overcome by stacking. Furthermore, the advantage of this technique was that in addition to the position in time and space, we also determined the source mechanism. We determined with numerical tests that the proposed technique can be used for detection and location of events with S/Ns as low as 0.05 at individual (prestacked) receivers. Furthermore, we found that other source mechanism parameters such as magnitude, volumetric, or shear components of the source mechanism were not suitable for the location. Finally, we applied the proposed technique to a microseismic event of moment magnitude $$-0.3$$ induced during the hydraulic fracturing treatment of a gas shale reservoir in North America.
    Print ISSN: 0016-8033
    Electronic ISSN: 1942-2156
    Topics: Geosciences , Physics
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  • 5
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    Society of Exploration Geophysicists (SEG)
    Publication Date: 2012-12-14
    Description: We report on and discuss the continuous seismic activity in the Dallas-Fort Worth (DFW) area. There was no reported seismic activity by USGS/NEIS until 31 October 2008, approximately seven weeks after the start of salt-water disposal at a nearby injection well in the southern part of the DFW airport. The salt-water disposal injection ceased in August 2009. The event detection based on crosscorrelation between several template events from DFW area and continuous seismic record shows that the seismic activity has been continuous for more than three years. Continuous monitoring at a local station allows us to complete the catalog down to a magnitude of zero, providing more detailed information on seismicity in the DFW area. This seismic activity migrated in space from a cluster southwest of the injection well to a cluster 2 km northeast of the injection well after May 2010. We show that the crosscorrelation detection at the WMOK regional station is not able to detect both south and northeast clusters of events without using multiple template events. Furthermore, we show magnitudes of the largest events increase since May 2010.
    Print ISSN: 1070-485X
    Electronic ISSN: 1938-3789
    Topics: Geosciences
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  • 6
    Publication Date: 2014-02-13
    Description: Differentiation between natural and induced seismicity is crucial for the ability to safely and soundly carry out various underground experiments and operations. This paper defines an objective tool for one of the criteria used to discriminate between natural and induced seismicity. The qualitative correlation between earthquake rates and the injected volume has been an established tool for investigating the possibility of induced, or triggered, seismicity. We derive mathematically, and verify using numerical examples, that the definition of normalized cross-correlation (NCC) between positive random functions exhibits high values with a limit equal to one, if these functions (such as earthquake rates and injection volumes) have a large mean and low standard deviation. In such a case, the high NCC values do not necessarily imply temporal relationship between the phenomena. Instead of positive-value time histories, the functions with their running mean subtracted should be used for cross-correlation. The NCC of such functions (called here NCCEP) may be close to zero, or may oscillate between positive and negative values in cases where seismicity is not related to injection. We apply this method for case studies of seismicity in Colorado, the United Kingdom, Switzerland and south-central Oklahoma, and show that NCCEP reliably determines induced seismicity. Finally, we introduce a geomechanical model explaining the positive cross-correlation observed in the induced seismicity data sets.
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 7
    Publication Date: 2014-06-21
    Description: Seismic monitoring can greatly benefit from imaging events with a low signal-to-noise ratio (SNR) as the number of the events with a low signal grows exponentially. One way to detect weaker events is improvement of a SNR by migration-type stacking of waveforms from multiple stations. We have developed a new method of location of seismic events that involves stacking of seismic phases and amplitudes along diffraction traveltime curves to suppress noise and detect seismic events with a SNR lower than that on individual receivers. The stacking includes polarity correction based on a simultaneous seismic moment tensor inversion and detection algorithm on the stack function. We applied this method to locate microseismicity induced by hydraulic fracturing. First we calibrated the velocity model by locating perforation shots at known locations. Then we processed 3 d of data from microseismic monitoring of shale stimulation and benchmarked migration-type locations of the largest events that were manually located. The detected and located events induced by hydraulic fracturing in this case study are mostly shear events forming narrow bands along the maximum horizontal stress direction approximately 100 m above the injection intervals. The proposed technique is fully automated and feasible for real-time seismic monitoring.
    Keywords: Seismology
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 8
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    Society of Exploration Geophysicists (SEG)
    Publication Date: 2015-08-01
    Description: Microseismic monitoring allows an inversion of advanced parameters that characterize a reservoir such as a stress-field orientation in addition to usual locations and source mechanisms. By inverting source mechanisms of microseismic events induced by hydraulic fracturing in a shale reservoir and using those mechanisms, one can obtain the stress field. Stress-field inversions using source mechanisms inverted from manually and automatically picked P-wave arrival amplitudes were compared. Stress fields determined from manual and automated P-wave arrival amplitudes are consistent. This implies that one can use the automated inversion of source mechanisms to reliably determine the stress field. The resulting stress fields are stable and consistent with the regional stress field measured in the region on the World Stress Map. Obtained maximum regional stress in the vertical direction, which is typical for most sedimentary basins, and a maximum horizontal stress oriented approximately 75° from the direction of the drilled lateral sections of wells. Finally, an inverted-shape ratio is used to plot Mohr diagrams that illustrate the most likely fault planes activated through hydraulic fracturing.
    Print ISSN: 1070-485X
    Electronic ISSN: 1938-3789
    Topics: Geosciences
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  • 9
    Publication Date: 2018-03-06
    Description: Ecosystem structure and function in the eastern Bering Sea are impacted by seasonal, interannual, and spatial variation of the zooplankton community. Zooplankton abundance, community composition and individual responses of key taxa, in spring, summer, and fall were evaluated across ecoregions during three years with high sea-ice, 2008–2010 (cold years). Interannual variations were greatest in spring, but less pronounced compared with intra-annual variations. Intra-annual variations were greatest in the south middle domain in spring and the north middle domain in all seasons. Models using environmental variables were able to explain 69–77% of zooplankton community variation within each season. Among individual taxa, Calanus marshallae/glacialis had delayed stage progression in spring 2009 compared with 2008 and 2010 on the south middle shelf, likely due to late ice retreat and cold temperatures that increased development times. In contrast, stage progression was fastest in summer 2008 likely due to warmer temperatures. Our findings indicate that intra-annual variation of zooplankton community composition, life history stage, and abundance within a cold period may affect the amount of high–lipid zooplankton prey (e.g. Neocalanus and Calanus spp. copepods and euphausiids) available seasonally for forage fish (e.g. age-0 walleye pollock) to grow to a sufficient size (to avoid size-dependent predation) and have sufficient lipid stores (to avoid starvation) to survive the first winter at sea.
    Print ISSN: 1054-3139
    Electronic ISSN: 1095-9289
    Topics: Biology , Geosciences , Physics
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  • 10
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