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IITK-BMTPC Earthquake Tip 3

             What are Magnitude and Intensity?                                                              page 2
            Table 2: Description of shaking intensity VIII as per   enclosed by  the isoseismal VIII (Figure 2) may have
               MSK scale                                        experienced a PGA of about 0.25-0.30g. However, now
              Intensity VIII - Destruction of Buildings         strong  ground    motion  records   from  seismic
              (a) Fright and  panic. Also,  persons  driving motorcars are   instruments  are relied upon to quantify destructive
                disturbed. Here and there branches of trees break off. Even   ground shaking. These  are critical for cost-effective
                heavy furniture moves and partly overturns. Hanging   earthquake-resistant design.
                lamps are damaged in part.

              (b) Most buildings of Type C suffer damage of Grade 2, and   Table 3: PGAs during shaking of different intensities
                few of Grade 3. Most buildings of Type B suffer damage of   MMI
                Grade 3, and  most buildings of  Type A  suffer damage of   V   VI      VII    VIII    IX    X
                Grade 4.  Occasional breaking of pipe seams occurs.   PGA   0.03-0.04  0.06-0.07 0.10-0.15  0.25-0.30  0.50-0.55  >0.60
                                                                  (g)
                Memorials and monuments move and twist. Tombstones
                overturn. Stonewalls collapse.                  Source: B.A.Bolt, Earthquakes, W.H.Freeman and Co., New York, 1993

              (c) Small landslips occur in hollows and on banked roads on   Based on data from past earthquakes, scientists
                steep  slopes; cracks develop in ground up to  widths of   Gutenberg and Richter in 1956 provided an
                several centimeters. Water in lakes becomes turbid. New
                reservoirs come into existence. Dry wells refill and existing   approximate correlation between the Local Magnitude
                wells become dry. In many cases, changes in flow and level   M L of an earthquake with the intensity I 0  sustained in
                of water are observed.                          the epicentral area as: M L ≈ 3  I 0   + 1. (For using this
                                                                                          2
              Note:
              • Type A structures - rural constructions; Type B - ordinary   equation, the Roman numbers of intensity are replaced
                masonry constructions; Type C - Well-built structures   with the corresponding Arabic numerals, e.g., intensity
              • Single, Few – about 5%; Many – about 50%; Most – about 75%   IX with  9.0). There  are several different relations
              • Grade 1 Damage – Slight damage; Grade 2 – Moderate   proposed by other scientists.
                damage; Grade 3 – Heavy damage; Grade 4 – Destruction;
                Grade 5 – Total damage

            Basic Difference: Magnitude versus Intensity                100 Watt Bulb
               Magnitude of an earthquake is a measure of its size.
            For instance, one can  measure the size of  an
            earthquake by the amount of strain energy released by
            the fault rupture. This means that the magnitude of the
            earthquake is a single value for a given earthquake. On                   Near
            the other hand, intensity is an indicator of the severity
            of shaking generated at a given location. Clearly, the     Bright
            severity of shaking is much higher near the epicenter   (100 lumens)

            than farther away. Thus, during the same earthquake
            of a certain magnitude, different locations experience
            different levels of intensity.                                     Normal
               To elaborate this distinction, consider the analogy         (50 lumens)
            of an electric bulb (Figure 3). The illumination at a                                          Far
            location near a  100-Watt bulb is higher than that
            farther away from it. While the bulb releases 100 Watts                                Dull
            of energy, the intensity of  light (or illumination,                      (20 lumens)
            measured in  lumens)  at  a location depends on the   Figure 3: Reducing illumination with distance

            wattage of the bulb and its distance from the bulb.                   from an electric bulb

            Here, the size of the bulb (100-Watt)  is like the
            magnitude of an earthquake, and the illumination at a   Reading Material
            location like the intensity of shaking at that location.   Richter,C.F., (1958),  Elementary   Seismology, W. H. Freeman and
            Magnitude and Intensity in Seismic Design             Company Inc, USA (Indian Reprint in 1969 by Eurasia Publishing
                                                                  House Private Limited, New Delhi)
               One often asks:  Can  my building withstand  a   http://neic.usgs.gov/neis/general/handouts/magnitude_intensity.
            magnitude 7.0 earthquake? But, the M7.0 earthquake    html
            causes different shaking intensities at different
            locations,  and the damage induced in buildings  at   Authored by:
            these locations is different. Thus, indeed it is particular   C.V.R.Murty
            levels of intensity of  shaking that  buildings  and   Indian Institute of Technology Kanpur
            structures are designed to resist, and not so much the   Kanpur, India
            magnitude. The  peak ground acceleration (PGA),  i.e.,   Sponsored by:
            maximum acceleration  experienced by the ground        Building Materials and Technology Promotion
            during shaking, is one way of quantifying the severity   Council, New Delhi, India
            of the ground shaking. Approximate empirical             This release  is  a property of  IIT Kanpur  and BMTPC  New
            correlations are available between the MM intensities      Delhi. It may be reproduced without changing its contents
            and the PGA that may be experienced (e.g., Table 3).      and with  due  acknowledgement.  Suggestions/comments
                                                                   may be  sent  to:  nicee@iitk.ac.in.  Visit  www.nicee.org  or
            For instance, during the 2001 Bhuj earthquake, the area      www.bmtpc.org, to see previous IITK-BMTPC Earthquake Tips.


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