SCIENCE TRIBUNE | Thursday, May 23, 2002, Chandigarh, India |
How the ground shakes
Electricity from mud NEW PRODUCTS & DISCOVERIES
|
How the ground shakes
Large strain energy released during an earthquake travels as seismic
waves in all directions through the Earth’s layers, reflecting and
refracting at each interface. These waves are of two types — body
waves and surface waves; the latter are restricted to near the Earth’s
surface (Figure 1). Body waves consist of Primary Waves (P-waves) and
Secondary Waves (S-waves), and surface waves consist of Love waves and
Rayleigh waves. Under P-waves, material particles undergo extensional
and compressional strains along the directions of energy transmission,
but under S-waves, oscillate at right angles to it (Figure 2). Love
waves cause surface motions similar to that by S-waves, but with no
vertical component. Rayleigh wave wakes a material particle oscillate
in an elliptic path in the vertical plane (with horizontal motion
along direction of energy transmission). P-waves are fastest,
followed in sequence by S- Love and Rayleigh waves. For example, in
granities, P- and S-waves have speeds ~4.8 km/sec and ~3.0 km/sec,
respectively. S-waves do not travel through liquids. S-waves do not
travel through liquids. S-waves in association with effects of Love
waves cause maximum damage to structures by their racking motion on
the surface in both verticle and horizontal directions. When P- and
S-waves reach the Earth’s surface, most of their energy is reflected
back. Some of this energy is returned back to the surface by
reflections at different layers of soil and rock. Shaking is more
severe (about twice as much) at the Earthsurface than at substantial
depths. This is often the basis for designing structures buried
underground for smaller levels of acceleration than those above the
ground.
Measuring Instruments The instrument that measures
earthquake shaking, a seismograph, has three components — the
sensor, the recorder and the timer. The principle on which it works is
simple and is explicitly reflected in the early seismograph (Figure 3)
— a pen attached at the tip of an oscillating simple pendulum (a
mass hung by a string from a support) marks on a chart paper that is
held on a drum rotating at a constant speed. A magnet around the
string provides required damping to control the amplitude of
oscillations. The pendulum mass, string, magnet and support together
constitute the sensor; the drum, pen and chart paper constitute the
recorder; and the motor that rotates the drum at constant speed forms
the timer. One such instruments is required in each of two orthogonal
horizontal directions. Of course, for measuring vertical oscillations,
the string pendulum (Figure 3) is replaced with a spring pendulum
oscillating about a fulcrum. Some instruments do not have a timer
device (i.e., the drum holding the chart paper does not rotate). Such
instruments provide only the maximum extent (or scope) of motion
during the earthquake; for this reason they are called seismoscopes. The
analog instruments have evolved over time, but today, digital
instruments using modern computer technology are more commonly used.
The digital instrument records the ground motion on the memory of the
microprocessor that is in-built in the instrument. Shaking of ground
on the Earth’s surface is a net consequence of motions caused by
seismic waves generated by energy release at each material point
within the three-dimensional volume that ruptures at the fault. These
waves arrive at various instants of time, have different amplitudes
and carry different levels of energy. Thus, the motion at any site on
ground is random in nature with its amplitude and direction varying
randomly with time. Large earthquakes at great distances can produce
weak motions that may not damage structures or even be felt by humans.
But, sensitive instruments can record these. This makes it possible to
locate distant earthquakes. However, from engineering viewpoint,
strong motions that can possibly damage structures are of interest.
This can happen with earthquakes in the vicinity or even with large
earthquakes at reasonable medium to large distances.
Characteristics The
motion of the ground can be described in terms of displacement,
velocity or acceleration. The variation of ground acceleration with
time recorded at a point on ground during an earthquake is called an
accelerogram. The nature of accelerograms may vary (Figure 4)
depending on energy released at source, type of slip at fault rupture,
geology along the travel path from fault rupture to the Earth’s
surface, and local soil (Figure 1).They carry distinct information
regarding ground shaking; peak amplitude, duration of strong shaking,
frequency content (e.g., amplitude of shaking associated with each
frequency) and energy content (i.e., energy carried by ground shaking
at each frequency) are often used to distinguish them. Peak amplitude
(peak ground acceleration, PGA) is physically intuitive. For instance,
a horizontal PGA value of 0.6 g (= 0.6 times the acceleration due to
gravity) suggests that the movement of the ground can cause a maximum
horizontal force on a rigid structure equal to 60% of its weight. In a
rigid structure, all points in it move with the ground by the same
amount, and hence experience the same maximum acceleration of PGA.
Horizontal PGA values greater than 1.0 g were recorded during the 1994
Northridge Earthquake in USA. Usually, strong grounds motions carry
significant energy associated with shaking of frequencies in the range
0.03-30Hz (i.e., cycles per sec). Generally, the maximum amplitudes of
horizontal motions in the two orthogonal directions are about the
same. However, the maximum amplitude in the vertical directions is
usually less than that in the horizontal direction. In design codes,
the vertical design acceleration is taken as 1/2 to 2/3 of the
horizontal design acceleration. In contrast, the maximum horizontal
and vertical ground accelerations in the vicinity of the fault rupture
do not seem to have such a correlation. Authored by C. V. R. Murty
for the Indian Institute of Technology Kanpur, Kanpur, India. |
Electricity from mud Self-recharging bacterial batteries that clean up organic
pollution as they generate electricity? Sounds more like science
fiction than science. Microbiologists are coming closer to making
microbial fuel cells a reality. They harnessed bacteria to generate
electricity from underwater sediments. The microbes make excess
elections that they stick directly to graphite wires, which in turn
send current to a second wire much like a car battery. For fuel, the
bacteria use organic material in the sea floor. These bacterial
batteries will probably never power a car, but they should be adequate
to run underwater sensors. Derek Lovely, a microbiologist at the
University of Massachusetts, Amherst, with Daniel Bond led the work on
these non-conventional energy sources. Because organic sediments are
so abundant, there could be an inexhaustible source of fuel. And
because many pollutants are organic, these portable generators might
also help get rid of hazardous materials. The whole field is very
exciting, because the work has broad potential for both helping
pollution cleanup and providing a cheap power supply. This research
has come closer to developing accessible marine batteries as a way to
meet our electricity needs. This was not the first time to notice
that microbes could steal electrons from oxygen-deficient mud and
somehow transfer them to electron-accepting rods placed into the
oxygen-containing sediments over-head. But Lovely and his colleagues,
take a concept that has been known for a while and make good on
it. They used lab fish tanks to recreate the ocean’s saltwater
environment. Collaborator Leonard Tender, positioned graphite wires
which act as electron-accepting anodes into oxygen containing water to
deceive electrons. In three different experiments, they measured the
number of electrons transferred to the anode and then to the cathode.
Even in these crude experiments, the current was enough to power a
small calculator. After several weeks, the researchers identified the
microbes that were growing on the mud-implanted electrodes. To their
surprise, Lovely and his colleagues found that one type of microbe —
Desulfuromanas acetoxidans, from a family called geo-bacteraceae —had
all but taken over the battery electrode, ousting the others. These
geo-microbes are famous for their ability to detoxify toluene and
other organic solvents, notes microbiologist Caroline Harwood of the
University of Iowa. Earlier, microbiologists had shown that different
microbes could move electrons from oxygen-deficient to oxygen-rich
substances through intermediate substances that they produced. The
microbes were involved, but not directly with the electrode, Lovely
explains. But geobacters, as the family is commonly called, need no
such gobetweens. They can convert the mud’s organic matter directly,
and that might prove quite useful in pollution control. Before using
organic pollutants to fuel electricity production leaves the realm of
science fiction, Lovely and his colleagues warn, the work needs to be
replicated in field conditions. Harwood points out that the bacteria
might quickly exhaust local organic fuels and have to be moved to a
different spot. The efficiency of the transfer also needs improving,
something that Lovely and others are fervently working on, otherwise,
it would take fields of electrodes to get enough energy to power many
undersea devices. |
NEW PRODUCTS & DISCOVERIES
How? Korea-based Samsung’s Scurry and Switzerland-based Senseboard
Technologies’ Senseboard (see picture) are virtual keyboards that use sensors
on the back of your hands to track the movement of your fingers. An onboard
processor maps the location of each virtual key tap to a keyboard layout, then
transmits the corresponding character wirelessly to a PDA, cellphone, or other
mobile device. Both virtual keyboards will be available later this year.
Prices not set. Popular Science
Automatic docking guidance
To allow passengers to move into the terminal building as quickly as
possible and without being exposed to the weather, telescoping bridges or
jetways are becoming more and more common, replacing rolling gangways and
airport buses. But docking at the extendable jetways requires a high level of
precision. The pilot must stop the aircraft at the exact right parking
position. Because the view from the cockpit is very limited, this process is
difficult without outside help by marshals. The new system developed at the
Fraunhofer Institute for Information and Data Processing IITB in Karlsruhe by
Volker Gengenbach does away with the requirement of a marshal, a report in
Fraunhofer Gesellschaft said. In the new system the groundcrew first enter the
craft type and expected arrival time into the computer. A video camera at the
outside wall of the building then acquires the aircraft as it taxis in. Using
the available model data, the docking approach path and optimal stopping
position are calculated. "The approach line is measured 10 to 20 times per
second," explains Gengenbach. PTI
Viruses to build microprocessors
The viruses are just 30 nanometres across, far smaller than
the 130-nanometre wide components in today’s microchips.They provide the
perfect scaffold for tiny electronic systems because they can be made to
arrange themselves into crystal-like arrays. This raises the tantalising
possibility of self-organising circuits, which need little or no intervention
to help them build useful three-dimensional structures that can be populated
with circuit components. Until now, nanotechnologists have only constructed
flat nanocircuits, using components like carbon nanotubes as transistors, but
what they wanted to achieve was to find a way for these molecular circuits to
build themselves, a report in New Scientist said. For their work, chemist MG
Finn and virologist Jack Johnson, both of the Scripps Research Institute in La
Jolla, California, selected cowpea mosaic virus, a common pathogen which stunts
the growth of the black-eyed pea plant. This virus is encased in a protective
protein coat that has 20 faces and 12 corners, or vertices. The researchers
inserted DNA segments into the virus’s genome that cause the pathogen to
produce cysteine amino acids on the vertices of its viral shell. The resulting
cysteine complex at each vertex sports sulphur-containing thiol groups, which
bind readily to gold. So when the team added ultrafine gold particles to the
cysteine-loaded viruses, they ended up with viruses studded with a pattern of
gold electrodes. PTI
Plastic surgical material
The material,
made of thermoplastic polymers that can be absorbed by the body, can be
engineered to retain a memory of a specific shape and to then transform itself
into that shape when warmed to body temperature, said Robert Langer, the
co-author of the study published in the electronic version of the journal
Science. The other author is Andress Lendlein, a former researcher at the
Massachusetts Institute of Technology, now teaches at the University of
Technology in Germany, Y Tevtththehe Techissbhe. Langer, a professor of
chemistry at MIT, said the plastic could be used to make implants or bone
screws that are not much bigger than a piece of string when they are inserted
into the body. Once they warm up, the devices change to form the appropriate
implant. "In a test on mice, we showed we can make these sutures
(surgical stitches) actually tie themselves," said Langer. He said that
since the material has a memory, it could be threaded into an incision as a
loose knot. When it warms to the body’s temperature, the material
"remembers" its designed shape and size and shrinks to tighten the
wound. Later after the wound is healed, the material dissolves and is
harmlessly absorbed by the body. "It is like a smart suture," said
Langer. "That could be very important in closing and incision in a place
that is hard to reach by surgeon. PTI |
SCIENCE & TECHNOLOGY CROSSWORD
Clues : Across 1. An ion that has a positive and a negative
charge on same group of atoms. 7. Connecting an electric conductor to
the ground. 8. A specialised Indian body advising on matters relating
to energy.(abbr.) 9. Longer is this, heavier is the beam. 12.
Bangalore based research institute named after C.V.Raman. 13. A
colourless crystalline solid acid used in beverages. 15. A rain gauge
is called so. 18. Tendency of solvent when partitioned from a more
concentrated solution, to diffuse through into that solution. 20. A
substance having nuclear carbon skeleton of the sterol or a similar
structure. 22. One of the best engineering firms. 23. A mineral
found in crystals separable into thin transparent plates. 24. An
alloy of Iron, Carbon and other metals in small proportions. Down 1.
A current produced in a semiconductor when subjected to strong
electric field. 2. A small piece of insulation. 3. A transition
metal having Ir as its symbol and 77 atomic number. 4. A device used
to maintain the temperature in an appliance within a range. 5. A
disease usually occurring after 6 to 12 minutes strenuous
activity. 6. An inert gas used in lights and signs. 10. …..head is
the area surrounding a coal mine. 11. Acid prepared by oxidation of
ethyl alcohol with acidified potassium permanganate. 14. Equivalent
to degree in engineering. 16. Most important system for PCs. 17. A
system to find the direction and distance of an object by analysing
the reflection of microwaves. 18. An electric circuit through which
no current is passing. 19. One of 4 quantum numbers assigned to an
electron and having only 2 values. 21.A mixture of naturally
occurring hydrocarbons. Solution to last week’s crossword. |