Editorial

Earthquake: Causes and precautions

Earthquake i.e. the slightest shaking of the earth causes shivering in the human mind.

Sentinel Digital Desk

Er Prabhat Kishore

(prabhatkishore65@gmail.com)

Earthquake i.e. the slightest shaking of the earth causes shivering in the human mind. This doesn't give them a chance to recover and in the blink of an eye, everything is offered to nature. However, it is an indisputable truth that people do not die due to earthquakes except in a few exceptions; but the death occurs due to unsafe constructions.

Earth's geographical structure, variations and internal movements are responsible for earthquakes. The whole earth is located on 12 major tectonic plates, namely Indian plate, Eurasian plate, Indo-Australian plate, Philippine plate, Antarctic plate, African plate, Arabian plate, South American plate, North American plate, Caribbean plate and Pacific plate. These plates are floating on the fluid lava beneath them and move slowly (approximately 4-5 cm) from their place every year. When a plate comes near another plate, then the plate moves away from someone. Sometimes, one plate collides with the boundary of another plate and faults are generated; due to which the energy below the earth comes out and an earthquake occurs.

The Indian plate extends from the Himalayan Mountains to the Antarctic. It just touches the Pakistan border. It is to the south of the Himalayas while the Eurasian plate (in which countries like China etc. falls) are to the north of the Himalayas. The Indian plate is moving up in the Northeast direction with a speed of 4.7 cm every year; whereas the Eurasian plate is moving north at a speed of 2 cm only. In such a situation, there is a possibility of an earthquake due to the collision of both plates.

The epicentre of an earthquake is the place just below which the geological energy is released by the movement of the plates. At this place, the vibration of the earthquake is high and the shock is strong. As the range of the vibration goes away, its effect gradually decreases. The intensity of an earthquake depends on whether the seismic frequency is upward or in the range. In case the frequency of vibration is upwards, fewer areas are affected.

The intensity of an earthquake (measured on the Richter scale) is the intensity of energy released from inside the earth during an earthquake. Earthquakes with a magnitude of less than 5 on the Richter scale are considered mild. However, it also depends on the composition of the area. If the epicentre of the earthquake is on the bank of the river and high buildings are constructed there without anti-seismic technology, then an earthquake of magnitude 5 on the Richter scale can also be dangerous. Earthquakes of magnitude 2 or less are difficult to record and are not felt. An earthquake with a magnitude of 5 -5.9 is considered moderate and earthquakes with a magnitude of more than 6 are considered fatal.

Indian sub-continent has been divided into five zones of an earthquake by the Bureau of Indian Standards (IS Code 1893-2002); out of which four are currently valid on the basis of studies, as Zone-1 has been merged into Zone-2. Seismic Zone-5 has been considered as the most active i.e. dangerous and Zone-2 is considered as the least active i.e. safe. The intensity is less than 4 magnitudes in Zone-2, 5 in Zone-3, 7 in Zone-4 and more than 8 magnitudes in Zone-5.

Zone-5 covers entire north-eastern states, parts of Jammu & Kashmir, Himachal Pradesh, Uttarakhand, Rann of Kutch, parts of Bihar, and Andaman & Nicobar. Zone-4 covers parts of Jammu &

Kashmir, Ladakh, Himachal Pradesh, Delhi, Uttarakhand, Sikkim, parts of Indo-Gangetic plains (Northern Punjab, Chandigarh, Western UP, Northern part of West Bengal, Bihar), parts of Gujarat and Maharashtra, and West Rajasthan. Zone-3 includes Kerala, Lakshadweep, parts of Uttar Pradesh, Gujarat, parts of Bengal, Punjab, Rajasthan, Madhya Pradesh, Bihar, Jharkhand, Chhattisgarh, Maharashtra, Andhra Pradesh, Odisha, Tamil Nadu, Karnataka, and

Zone-2 covers the rest of the country and a major part of South India.

The entire Himalayan range comes under the high-intensity zone of earthquakes. In the year 1897, Shillong (8.7 Richter scale), in 1905 Kangra (8.0 Richter scale), in 1934 Bihar-Nepal (8.3 Richter scale), and in 1950 Assam-Tibet (8.6 Richter scale) were hit by major earthquakes.

To avoid the wrath of the earthquake, the arrangements and preparedness of disaster management should be effective. Actually, most of the damage to life and property occurs due to unsafe and weak structures. So, there is a dire need to enact laws for building construction on earthquake-resistant technology and strictly enforce it all over the country, especially in the plains and hilly areas. It costs approximately 6-7 per cent extra amount to make new houses with earthquake resistant design, while about 12-15 per cent extra cost is incurred in converting old houses as earthquake resistant.

Efforts have also been made to bring awareness in this direction by the Disaster Management Department of the State Governments. The IS code assigns a Zone Factor (the maximum horizontal acceleration that can be experienced by a structure) to each zone, which is used by the Structural engineers for earthquake resistance design of the structures.

Some basic provisions should be taken care of in the construction of masonry buildings for earthquake protection. Building based on one brick thick-walled structure should be up to three-storeyed only.

Horizontal bands are an important earthquake resistant feature. It holds a masonry building as a single unit tying all the walls together and is similar to a belt tied around the box. Lintel Bands, as well as Plinth bands, are required in every building. Gable bands are essential in buildings with pitched or sloped roofs. A roof band is not necessary for a flat RC roof building, because the roof slab itself plays the role of a band. The Indian Standards IS: 4326-1993 and IS: 13828-1993 provides sizes & details of the bands. In Earthquake Zone-5, bands should also be made on the sills of the windows. Indoors and windows larger than 600 mm, steel bars should be provided in concrete on both sides. It prevents the formation of cracks in the wall during an earthquake.

In the buildings constructed in all the regions, except that falling in Earthquake Zone-3, Tor steel bars should be provided inside the concrete at the corners of all the rooms. Empty pockets should be made in the brick joints for pouring concrete. These standing bars, starting from the foundation and joining all RCC bands, should be bent 300 millimetres inside the slab of the final roof. If the bars are to be joined to reach the full height; then the overlapping length of the two bars should be at least 50 times its diameter and properly tied with wires. For doors, larger than one meter, steel bars in concrete are provided on each side.

The sum of the widths of doors and windows should be in definite proportion to the total length of the wall. It should be less than 50 per cent of the length of the wall in a single storey building, less than 42 per cent in a two-storey building and less than 33 per cent in a three-storey building. The walls between the doors and windows should be equal to the length of at least two bricks. The distance of the door or window from the corner of the wall should be at least equal to the length of one brick. The height of the wall between the window and the ventilator should be kept at least 450 mm.

Earthquake is a natural phenomenon; as a result, it cannot be prevented. But the use of anti-seismic techniques in the construction of buildings and other infrastructural structures can restrict the loss of life as well as property to a minimum level.