भूकंप से कम होगा नुकसान, ग्राउंड मोशन सिमुलेशन प्रक्रिया होगी कारगर, CSIR के वैज्ञानिक से EXCLUSIVE बातचीत

ETVBHARAT

सीएसआईआर बेंगलुरु के वरिष्ठ वैज्ञानिक डॉ इम्तियाज ए परवेज ने भूकंप और उससे जुड़ी रिसर्च के बारे में बताया

Transcript

00:00foreign

00:18foreign

00:24foreign

00:26foreign

00:27So, what can we do with Vagyanic?

00:29We will talk about this as well.

00:31Dr. Intiaji will talk about it.

00:33The most important thing is that

00:35people live in the world.

00:37There is also a place of fear.

00:39There is also a place of fear.

00:41People go out of the house.

00:43We are also doing research.

00:45However, there is no need to be done.

00:47What can we do with Vagyanic?

00:49What should we do with Vagyanic?

00:51What should we do with Vagyanic?

00:53What should we do with Vagyanic?

00:55Vagyanic is very difficult.

00:57It is very difficult.

00:59It is very difficult.

01:01There are three things for Vagyanic is very important.

01:05When? Where?

01:07And how big is it?

01:09We all know two things.

01:11The third thing is,

01:13how big is it and how big is it?

01:15For example, the Himalayan belt.

01:17The Himalayan belt

01:19is very important.

01:21It is very important.

01:23It is very important.

01:25We know that the Earthquake will come.

01:27Many scientists, many Vagyanic have also known

01:29that in Uttarakhand, Central Himalaya,

01:33or Kashmir Himalaya,

01:35there is so much stress accumulated

01:37that it will be released.

01:39And that can be released in some big Vagyanic.

01:41But to say that when it will be released,

01:44the Earthquake condition is very difficult.

01:47But the Vagyanic can do it,

01:49that when we know that it will come,

01:51that it will come,

01:53that we have so much knowledge

01:55that the Vagyanic is what will happen.

01:57The Vagyanic is what will happen.

01:59The Vagyanic is what will happen.

02:01For example, if we talk about Delhi,

02:03about Dharadun,

02:05about Chandigarh,

02:07about Chandigarh or Kashmir,

02:09about Shilagar,

02:11then the Vagyanic is what will happen.

02:13When the Vagyanic is coming,

02:15the Vagyanic is not coming,

02:17but the Vagyanic is coming.

02:19So we can simulate this.

02:21We can simulate this.

02:23We can simulate all the input parameters

02:25in the high-performance computing system.

02:27We can simulate it.

02:28Just like it is a realistic earthquake.

02:31So I can simulate it.

02:33I know that the ground motion,

02:35the ground motion,

02:36the ground motion,

02:37the acceleration,

02:38the velocity,

02:39the displacement,

02:40the displacement,

02:41how much it will happen.

02:43The decision makers,

02:45or the civil engineers,

02:46it is very necessary

02:48so that at that point,

02:50they can be aware of it

02:52and make their construction

02:53and make their construction

02:54which doesn't have to come.

02:56Do you see any place

02:58in the future

02:59where the amount of energy

03:01has been increased?

03:03The amount of energy

03:04has been released?

03:05The amount of energy

03:06is in the whole world.

03:08The GPS study tells us

03:10that in the segment

03:12where the energy

03:14has been released.

03:15But the energy

03:16has been increased.

03:17So the energy

03:18in the central Himalaya

03:19or even the northwest Himalaya

03:21has been increased.

03:23When will it be released?

03:25This is difficult.

03:27Okay, sir.

03:28This is also the solution

03:29that the slow hukam

03:30of energy has been released.

03:31Is it because

03:32the big hukam

03:33is going to come

03:34to come?

03:35It is not going to come.

03:37It is not going to come.

03:38But yes,

03:39it is also believed

03:40that the energy

03:41is increased.

03:42The power of energy

03:44is held

03:46since there are

03:476 or 7

03:48in the frame

03:49that a large hukam

03:50is based on

03:51about

03:53the power of energy

03:54which is

03:56built up

03:57slowly.

03:58The power of energy

03:59will live

04:00become the full presence.

04:01The power of energy

04:02powers

04:03will much be

04:05very difficult.

04:06So what do we need to do with the preparation and precautions, because in the past 500-700 years there is no big shock.

04:11So how do we need to focus on the measures and focus on the measures?

04:15I have told you that knowing that the shock will come.

04:18The shock of the shock is 7 or 8 months.

04:22We should have to simulate the shock of the shock.

04:28Not only the ground motion, but the sediment will amplify the ground motion.

04:35So if we are doing the sight response, we will find a scenario that we can find that if the shock will come,

04:47then we will find the shock of the ground.

04:53When there is a shock, there is no shock, there is no shock.

04:59But if there is a shock, then what will the impact of the shock?

05:03The impact will be the same.

05:05The rocky terrain, there will be a little impact.

05:09And as you know, the city or populated areas are more than plain.

05:14And the plain area is on the sediment.

05:18The soil is quite deep.

05:23That is a problem.

05:25Because the sediment will amplify that signal.

05:30So if your house is in a rocky area,

05:34and there is a sediment,

05:36then the sediment will be more damp.

05:38Then there will be more amplification.

05:40So in the lower areas of the land,

05:42the land from the forest.

05:43It will be very strong,

05:44and so far from the sea.

05:45I think it really can be a big impact.

05:47We will see the surrounding areas of the land of the land.

05:50So in the forest you can see the...

05:52It is a very strong impact,

05:54it is a different challenge.

05:55The land slide is a different thing, but the land slide is not able to get from it because the climate change is changing, the rain is changing.

06:11The land slide is changing, and then the land slide.

06:16So now we are doing a mission mode project in CSIR

06:22which we are talking about the Himalayan Earthquakes,

06:28which we are talking about the Himalayan Earthquakes,

06:32and we are talking about the climate,

06:36which is a cloudburst.

06:39So all of this is a very big project from CSIR,

06:43which we are trying to address.

06:52Thank you very much.

06:54Dr. Imtiaj,

06:56who told me that this is not a good thing,

06:59but it is not a good thing,

07:01but it is not a good thing.

07:03It is not a good thing,

07:05it is not a good thing,

07:07it is not a good thing,

07:09it is not a good thing,

07:11it is not a good thing,

07:13especially if we talk about the Himalayan Earthquakes,

07:15it is not a good thing,

07:17so it is a good thing,

07:18so we need to give it to you.

07:20I am like,

07:21so that is not a bad thing,

07:22I am not a good thing,

07:23and I have a bad thing,

07:24because there is no good thing,

07:25so we are going to talk about it,

07:27and we can't see.

07:28This is not a good thing,

07:29but I think it is a good thing.

07:30We have to learn from here in the history.

07:31There is a 여러 three years,

07:32the two years ago.

07:33I am a two years after the ministry.

07:34We are working in the history of freedom,

07:36so we are all in the history of the Tokyo Disney community,

07:39I feel the three years after this time,

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