When a charged object comes into contact with our hand, a process called "charging by conduction" occurs, resulting in the loss of the object's charge. Here's why: 1. Conduction Process: Our bodies conduct electricity. Upon touching a charged object, electrons move between the object and our hand duRead more
When a charged object comes into contact with our hand, a process called “charging by conduction” occurs, resulting in the loss of the object’s charge. Here’s why:
1. Conduction Process: Our bodies conduct electricity. Upon touching a charged object, electrons move between the object and our hand due to our body’s conductive nature.
2. Charge Equalization: Excess charge on the object spreads out or neutralizes as charges shift between the object and our hand. If the object had extra electrons (negative charge), some move to our hand. If it had a shortage (positive charge), some electrons from our hand transfer to the object.
3. Neutralization: Eventually, both the object and our hand reach an equilibrium state, reducing or neutralizing the net charge. This leads to a decrease in the object’s charge as it shares charges with our hand.
4. Grounding Effect: The Earth can absorb excess charges. When we touch the charged object, some charges flow through us to the ground, aiding in the object’s charge loss.
In essence, touching a charged object with our hand causes a redistribution of charges through conduction, resulting in a balanced state between the object and our hand and leading to the loss of the object’s excess charge.
The Richter scale measures the destructive energy of earthquakes. A seismic event registering a magnitude of 3 on this scale is considered minor. Seismographs can detect such tremors, but they generally don't cause substantial damage. A magnitude 3 earthquake is often felt by people nearby but typicRead more
The Richter scale measures the destructive energy of earthquakes. A seismic event registering a magnitude of 3 on this scale is considered minor. Seismographs can detect such tremors, but they generally don’t cause substantial damage.
A magnitude 3 earthquake is often felt by people nearby but typically doesn’t inflict significant harm on structures or infrastructure. While seismographs can record these tremors, they aren’t usually concerning in terms of causing noteworthy damage.
There are three effective measures to protect oneself from lightning during a thunderstorm: 1. Seek Proper Shelter: Immediately seek sturdy, enclosed shelters like buildings or fully enclosed vehicles when thunderstorms approach. Avoid open spaces, tall objects, or isolated trees, and refrain from sRead more
There are three effective measures to protect oneself from lightning during a thunderstorm:
1. Seek Proper Shelter: Immediately seek sturdy, enclosed shelters like buildings or fully enclosed vehicles when thunderstorms approach. Avoid open spaces, tall objects, or isolated trees, and refrain from seeking shelter in sheds or small structures that don’t provide adequate protection from lightning.
2. Avoid Conductive Surfaces: Stay away from conductive surfaces and objects that can conduct electricity, such as metal fences, wires, plumbing, and electronic devices. Additionally, avoid contact with water sources like pools, lakes, or showers, as water conducts electricity.
3. Follow the 30-30 Rule: Use the “30-30 rule” during a thunderstorm. Count the seconds between a lightning flash and the sound of thunder. Seek shelter if this time is 30 seconds or less. Stay indoors for at least 30 minutes after the last observed lightning or thunder to ensure safety.
Implementing these precautions significantly reduces the risk of lightning-related injuries, providing safety during thunderstorms and adverse weather conditions.
When two balloons are charged, their behavior depends on the types of charges they carry: 1. Charged Balloon Repulsion: If both balloons possess the same charge (both positively or both negatively charged), they repel each other. Like charges repel due to the fundamental principle of electrostatic fRead more
When two balloons are charged, their behavior depends on the types of charges they carry:
1. Charged Balloon Repulsion: If both balloons possess the same charge (both positively or both negatively charged), they repel each other. Like charges repel due to the fundamental principle of electrostatic force. This causes the balloons to move away from each other as the similar charges on their surfaces repel.
2. Charged-Uncharged Balloon Attraction: When one balloon is charged and the other is uncharged, an attractive force occurs. The charged balloon induces a temporary opposite charge on the surface of the uncharged balloon through electrostatic induction. This opposite charge leads to an attractive force between the balloons as opposite charges attract each other.
In summary, similarly charged balloons repel each other due to like charges, while a charged balloon can attract an uncharged balloon through electrostatic induction, creating opposite charges and resulting in an attractive force between them.
In India, several states are more susceptible to earthquakes due to their geological positions and proximity to active seismic zones: 1. Himachal Pradesh: Positioned in the northern region, Himachal Pradesh is prone to earthquakes as it lies close to the seismic belts of the Himalayas, where tectoniRead more
In India, several states are more susceptible to earthquakes due to their geological positions and proximity to active seismic zones:
1. Himachal Pradesh: Positioned in the northern region, Himachal Pradesh is prone to earthquakes as it lies close to the seismic belts of the Himalayas, where tectonic activity frequently triggers seismic events.
2. Uttarakhand: Similar to Himachal Pradesh, Uttarakhand faces seismic threats owing to its location near the Himalayan seismic belt. Tectonic interactions along this region contribute to a heightened risk of earthquakes.
3. Assam: Situated in northeastern India, Assam encounters seismic activity owing to its vicinity to the boundary between the Indian and Eurasian plates. The tectonic movements along the eastern Himalayan region and the Indo-Burmese arc render this area susceptible to earthquakes.
These states are more prone to earthquakes due to their geographical settings and proximity to active fault lines and tectonic regions, highlighting the need for preparedness and awareness regarding seismic risks.
Explain why a charged body loses its charge if we touch it with our hand.
When a charged object comes into contact with our hand, a process called "charging by conduction" occurs, resulting in the loss of the object's charge. Here's why: 1. Conduction Process: Our bodies conduct electricity. Upon touching a charged object, electrons move between the object and our hand duRead more
When a charged object comes into contact with our hand, a process called “charging by conduction” occurs, resulting in the loss of the object’s charge. Here’s why:
1. Conduction Process: Our bodies conduct electricity. Upon touching a charged object, electrons move between the object and our hand due to our body’s conductive nature.
2. Charge Equalization: Excess charge on the object spreads out or neutralizes as charges shift between the object and our hand. If the object had extra electrons (negative charge), some move to our hand. If it had a shortage (positive charge), some electrons from our hand transfer to the object.
3. Neutralization: Eventually, both the object and our hand reach an equilibrium state, reducing or neutralizing the net charge. This leads to a decrease in the object’s charge as it shares charges with our hand.
4. Grounding Effect: The Earth can absorb excess charges. When we touch the charged object, some charges flow through us to the ground, aiding in the object’s charge loss.
In essence, touching a charged object with our hand causes a redistribution of charges through conduction, resulting in a balanced state between the object and our hand and leading to the loss of the object’s excess charge.
See lessName the scale on which the destructive energy of an earthquake is measured. An earthquake measures 3 on this scale. Would it be recorded by a seismograph? Is it likely to cause much damage?
The Richter scale measures the destructive energy of earthquakes. A seismic event registering a magnitude of 3 on this scale is considered minor. Seismographs can detect such tremors, but they generally don't cause substantial damage. A magnitude 3 earthquake is often felt by people nearby but typicRead more
The Richter scale measures the destructive energy of earthquakes. A seismic event registering a magnitude of 3 on this scale is considered minor. Seismographs can detect such tremors, but they generally don’t cause substantial damage.
A magnitude 3 earthquake is often felt by people nearby but typically doesn’t inflict significant harm on structures or infrastructure. While seismographs can record these tremors, they aren’t usually concerning in terms of causing noteworthy damage.
See lessSuggest three measures to protect ourselves from lightning.
There are three effective measures to protect oneself from lightning during a thunderstorm: 1. Seek Proper Shelter: Immediately seek sturdy, enclosed shelters like buildings or fully enclosed vehicles when thunderstorms approach. Avoid open spaces, tall objects, or isolated trees, and refrain from sRead more
There are three effective measures to protect oneself from lightning during a thunderstorm:
1. Seek Proper Shelter: Immediately seek sturdy, enclosed shelters like buildings or fully enclosed vehicles when thunderstorms approach. Avoid open spaces, tall objects, or isolated trees, and refrain from seeking shelter in sheds or small structures that don’t provide adequate protection from lightning.
2. Avoid Conductive Surfaces: Stay away from conductive surfaces and objects that can conduct electricity, such as metal fences, wires, plumbing, and electronic devices. Additionally, avoid contact with water sources like pools, lakes, or showers, as water conducts electricity.
3. Follow the 30-30 Rule: Use the “30-30 rule” during a thunderstorm. Count the seconds between a lightning flash and the sound of thunder. Seek shelter if this time is 30 seconds or less. Stay indoors for at least 30 minutes after the last observed lightning or thunder to ensure safety.
Implementing these precautions significantly reduces the risk of lightning-related injuries, providing safety during thunderstorms and adverse weather conditions.
See lessExplain why a charged balloon is repelled by another charged balloon whereas an uncharged balloon is attracted by another charged balloon?
When two balloons are charged, their behavior depends on the types of charges they carry: 1. Charged Balloon Repulsion: If both balloons possess the same charge (both positively or both negatively charged), they repel each other. Like charges repel due to the fundamental principle of electrostatic fRead more
When two balloons are charged, their behavior depends on the types of charges they carry:
1. Charged Balloon Repulsion: If both balloons possess the same charge (both positively or both negatively charged), they repel each other. Like charges repel due to the fundamental principle of electrostatic force. This causes the balloons to move away from each other as the similar charges on their surfaces repel.
2. Charged-Uncharged Balloon Attraction: When one balloon is charged and the other is uncharged, an attractive force occurs. The charged balloon induces a temporary opposite charge on the surface of the uncharged balloon through electrostatic induction. This opposite charge leads to an attractive force between the balloons as opposite charges attract each other.
In summary, similarly charged balloons repel each other due to like charges, while a charged balloon can attract an uncharged balloon through electrostatic induction, creating opposite charges and resulting in an attractive force between them.
See lessList three states in India where earthquakes are more likely to strike.
In India, several states are more susceptible to earthquakes due to their geological positions and proximity to active seismic zones: 1. Himachal Pradesh: Positioned in the northern region, Himachal Pradesh is prone to earthquakes as it lies close to the seismic belts of the Himalayas, where tectoniRead more
In India, several states are more susceptible to earthquakes due to their geological positions and proximity to active seismic zones:
1. Himachal Pradesh: Positioned in the northern region, Himachal Pradesh is prone to earthquakes as it lies close to the seismic belts of the Himalayas, where tectonic activity frequently triggers seismic events.
2. Uttarakhand: Similar to Himachal Pradesh, Uttarakhand faces seismic threats owing to its location near the Himalayan seismic belt. Tectonic interactions along this region contribute to a heightened risk of earthquakes.
3. Assam: Situated in northeastern India, Assam encounters seismic activity owing to its vicinity to the boundary between the Indian and Eurasian plates. The tectonic movements along the eastern Himalayan region and the Indo-Burmese arc render this area susceptible to earthquakes.
These states are more prone to earthquakes due to their geographical settings and proximity to active fault lines and tectonic regions, highlighting the need for preparedness and awareness regarding seismic risks.
See less