Interview with Charles F. Richter / by Ann Scheid
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Energy and Magnitude: a Historical Perspective
Pure Appl. Geophys. 176 (2019), 3815–3849 Ó 2018 Springer Nature Switzerland AG https://doi.org/10.1007/s00024-018-1994-7 Pure and Applied Geophysics Energy and Magnitude: A Historical Perspective 1 EMILE A. OKAL Abstract—We present a detailed historical review of early referred to as ‘‘Gutenberg [and Richter]’s energy– attempts to quantify seismic sources through a measure of the magnitude relation’’ features a slope of 1.5 which is energy radiated into seismic waves, in connection with the parallel development of the concept of magnitude. In particular, we explore not predicted a priori by simple physical arguments. the derivation of the widely quoted ‘‘Gutenberg–Richter energy– We will use Gutenberg and Richter’s (1956a) nota- magnitude relationship’’ tion, Q [their Eq. (16) p. 133], for the slope of log10 E versus magnitude [1.5 in (1)]. log10 E ¼ 1:5Ms þ 11:8 ð1Þ We are motivated by the fact that Eq. (1)istobe (E in ergs), and especially the origin of the value 1.5 for the slope. found nowhere in this exact form in any of the tra- By examining all of the relevant papers by Gutenberg and Richter, we note that estimates of this slope kept decreasing for more than ditional references in its support, which incidentally 20 years before Gutenberg’s sudden death, and that the value 1.5 were most probably copied from one referring pub- was obtained through the complex computation of an estimate of lication to the next. They consist of Gutenberg and the energy flux above the hypocenter, based on a number of assumptions and models lacking robustness in the context of Richter (1954)(Seismicity of the Earth), Gutenberg modern seismological theory. -
Beno Gutenberg
NATIONAL ACADEMY OF SCIENCES B E N O G U T E N B ER G 1889—1960 A Biographical Memoir by L E O N KNOP OFF Any opinions expressed in this memoir are those of the author(s) and do not necessarily reflect the views of the National Academy of Sciences. Biographical Memoir COPYRIGHT 1999 NATIONAL ACADEMIES PRESS WASHINGTON D.C. Courtesy of the California Institute of Technology Archives, Pasadena BENO GUTENBERG June 4, 1889–January 25, 1960 BY LEON KNOPOFF ENO GUTENBERG WAS THE foremost observational seismolo- Bgist of the twentieth century. He combined exquisite analysis of seismic records with powerful analytical, inter- pretive, and modeling skills to contribute many important discoveries of the structure of the solid Earth and its atmo- sphere. Perhaps his best known contribution was the pre- cise location of the core of the Earth and the identification of its elastic properties. Other major contributions include the travel-time curves; the discovery of very long-period seis- mic waves with large amplitudes that circle the Earth; the identification of differences in crustal structure between continents and oceans, including the discovery of a signifi- cantly thin crust in the Pacific; the discovery of a low-veloc- ity layer in the mantle (which he interpreted as the zone of decoupling of horizontal motions of the surficial parts from the deeper parts of the Earth); the creation of the magni- tude scale for earthquakes; the relation between magnitudes and energies for earthquakes; the famous universal magni- tude-frequency relation for earthquake distributions; the first density distribution for the mantle; the study of the tem- perature distribution in the Earth; the understanding of microseisms; and the structure of the atmosphere. -
Potential Injection-Induced Seismicity Associated with Oil & Gas
Potential Injection-Induced Seismicity Associated with Oil & Gas Development: A Primer on Technical and Regulatory Considerations Informing Risk Management and Mitigation Potential Injection-Induced Seismicity Associated with Oil & Gas Development: A Primer on Technical and Regulatory Considerations Informing Risk Management and Mitigation Second Edition, 2017 Potential Injection-Induced Seismicity Associated with Oil & Gas Development: A Primer on Technical and Regulatory Considerations Informing Risk Management and Mitigation This report is developed by the StatesFirst Induced Seismicity by Injection Work Group (ISWG) members (the State agencies) with input and support from the ISWG technical advisors (subject matter experts from academia, industry, federal agencies, and environmental organizations) to help better inform all stakeholders and the public on technical and regulatory considerations associated with evaluation and response, seismic monitoring systems, information sharing, and the use of ground motion metrics. It also is intended to summarize the range of approaches that have been used or are currently being used by states to manage and mitigate the risks associated with seismicity that may be induced by injection. StatesFirst is an initiative of the Interstate Oil and Gas Compact Commission and the Ground Water Protection Council. Disclaimer This is an informational document, and is not intended to offer recommended rules or regulations. The ISWG recognizes that management and mitigation of the risks associated with induced -
1. Introduction
EARTHQUAKE MAGNITUDE, INTENSITY, ENERGY, POWER LAW RELATIONS AND SOURCE MECHANISM J.R. Kayal Geological Survey of India, 27, J.L. Nehru Road Road, Kolkata – 700 016 email : [email protected] EARTHQUAKE MAGNITUDE Magnitude is one of the basic and important parameters of an earthquake. It defines the size of an earthquake. The beginners of seismology are, in general, confused about different scales of magnitude, and sometimes they mix-up earthquake intensity with its magnitude. Journalists often report the magnitude value of an earthquake as its intensity; this is wrong. There are now different magnitude scales to define the size of an earthquake. After Richter (1935), various magnitude scales are proposed; all these scales are discussed below. Richter Magnitude (or Local Magnitude) ML Richter (1935) defined the local magnitude ML of an earthquake observed at a station to be ML = log A - log Ao ( ∆) (1) where A is the maximum amplitude in millimetres recorded on the Wood- Anderson seismograph for an earthquake at epicentral distance of ∆ km, and Ao (∆ ) is the maximum amplitude at ∆ km for a standard earthquake. The local magnitude is thus a number characteristic of the earthquake, and independent of the location of the recording station. Three arbitrary choices are made in the above definition: (i) the use of standard Wood-Anderson seismograph, (ii) the use of common logarithms to the base 10, and (iii) selection of the standard earthquake whose amplitudes as a function of distance are represented by Ao (∆). The zero level of Ao (∆) can be fixed by choosing its value at a particular distance. Richter chose the zero level of Ao (∆) to be 1 µm (or 0.001 mm) at a distance of 100 km from the earthquake epicentre. -
Potential Induced Seismicity Guide a Resource of Technical & Regulatory Considerations Associated with Fluid Injection
2021 UPDATE Potential Induced Seismicity Guide A Resource of Technical & Regulatory Considerations Associated with Fluid Injection Potential Induced Seismicity Guide: A Resource of Technical and Regulatory Considerations Associated with Fluid Injection Disclaimer This is an informational document and is not intended to offer recommended rules or regulations. The Induced Seismicity Workgroup (ISWG), an effort of the State Oil and Gas Regulatory Exchange (Exchange) recognizes that management and mitigation of the risks associated with induced seismicity are best considered at the state level with specific considerations at local, regional, or cross-state levels, due to significant variability in local geology and surface conditions (e.g., population, building conditions, infrastructure, critical facilities, seismic monitoring capabilities, etc.). Neither the State Oil and Gas Regulatory Exchange (Exchange), nor the ISWG, nor any person acting on their behalf makes any warranty, express or implied; or assumes any legal liability or responsibility for the accuracy, completeness, or any third party’s use or reliance on any information, apparatus, product, or process disclosed; or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not constitute or imply its endorsement, recommendation, or favor by the Exchange, the ISWG nor any person acting on their behalf. The views and opinions of authors expressed herein do not necessarily state or reflect those of the Exchange, or the ISWG. Recommended Citation Ground Water Protection Council and Interstate Oil and Gas Compact Commission. Potential Induced Seismicity Guide: A Resource of Technical and Regulatory Considerations Associated with Fluid Injection, March 2021, 250 pages. -
Seismicity in the Pannonian Region – Earthquake Data
EGU Stephan Mueller Special Publication Series, 3, 9–28, 2002 c European Geosciences Union 2002 Seismicity in the Pannonian Region – earthquake data L. Toth,´ P. Monus,´ T. Zs´ıros, and M. Kiszely Seismological Observatory, Hungarian Academy of Sciences Meredek u. 18, H-1112 Budapest, Hungary Received: 2 May 2000 – Accepted: 16 July 2001 Abstract. A comprehensive earthquake catalogue has local scale is a more complicated task and should be per- been compiled, listing historical and instrumentally recorded formed with great care. Not only because almost 10% of all earthquakes throughout the Pannonian Region bounded by earthquakes occur within plate interiors globally, but also as 44.0–50.0 N latitude and 13.0–28.0 E longitude. The cata- plates continue to move, plate boundaries change over geo- logue contains more than 20 000 events ranging in date from logic time and weakened boundary regions become part of 456 AD to 1998 and is considered to be complete for earth- the interiors of the plates. These zones of weakness within quakes larger than M 6.4 since 1500, for earthquakes larger the continents can cause earthquakes, either in response to than M 4.7 since 1800 and for magnitudes greater than 3.5 stresses that originate at the edges of the plate or in response since 1880. In combination with the stress data derived from to local gravitational stresses. 190 focal mechanism solutions for individual earthquakes Nevertheless, the study of the recent tectonics requires in- these data provide a relatively strong basis for evaluating put data from the seismic activity of the area: if existing seismic sources and seismotectonic models both within and tectonic features are active in the present, or were active in surrounding the Pannonian Basin. -
EG0800378 the Role of Tectonic and Seismicity in Siting of Nuclear Power Plant M.A.H
EG0800378 The Role of Tectonic and Seismicity in Siting of Nuclear Power Plant M.A.H. Abdel Aziz Siting and Environmental Department, National Center for Nuclear Safety and Radiation Control ABSTRACT The site selection for the a nuclear power plant (NPP) is controlled by many criteria. One of the most important criterion is the tectonic and seismicity of the site and its surroundings. Since, it is preferable the site in concern is characterized by low tectonic and low seismicity to avoid the damage effects associated with the occurrence of destructive earthquakes. The investigation of the tectonic and seismicity maps of egypt has been carried out to candidate potential areas or sites for nuclear power plant installation from seismicity point of view. Also, the design basis ground motion in terms of peak ground acceleration and response spectra of some of the potential sites are defined through the conduct of probabilistic seismic hazard analysis The study revealed that although there is no criterion to exclude areas of high tectonic and high seismicity as potential sites for nuclear power plant installation but, it is preferable avoiding such areas. This is attributed to the critical seismic curve that characterizes such areas and is required high seismic design levels to resist the destructive vibratory ground motion associated with the expected earthquake. Cosequently, the required high seismic design levels will have a negative impact on the economic cost of the facility compared with that built in low and moderate seismic areas. Hence, areas like the gulf of suez, the norhern part of the Red Sea and the southern part of Sinai Peninsula should be avoided as potential sites for NPP from the tectonic and seismicity point of view.