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CS435 Assignment 1 Solution and Discussion

zareen Cyberian's Gold last edited by
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 Assignment No. 01 Semester: Fall 2019
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CS435: Cloud Computing
Total Marks: 20
Due Date: 13th November 2019
Objective:
The objective of this assignment is to enhance the learning capabilities of the students about:
• Transmission Modes (Data Flow)
• TCP/IP Protocol suite
• IP Addressing
• Privileged and Non-Privileged Instructions
Instructions:
Please read the following instructions carefully before submitting assignment:
You need to use MS word document to prepare and submit the assignment on VU-LMS. It should be clear that your assignment will not get any credit if:
The assignment is submitted after due date.
The assignment is not in the required format (.doc or docx)
The submitted assignment does not open or file is corrupt.
Assignment is copied (partial or full) from any source (websites, forums, students, etc)

Assignment
- Question No. 1
  Identify the type of transmission mode (data flow) for each of the following device:
- Question No. 2
  Identify the TCP/IP Protocol layer for each of the following functionalities:
- Question No. 3
  For each of the following IP addresses, identify the class of IP address and
- Question No. 4
  Identify Privileged and Non-Privileged Instructions from the list given below:
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@zareen said in EDU515 Assignment 2 Solution and Discussion:

Write a detailed note on plate tectonics of the Earth. Use diagrams related to the question.

Plate tectonics, theory dealing with the dynamics of Earth’s outer shell—the lithosphere—that revolutionized Earth sciences by providing a uniform context for understanding mountain-building processes, volcanoes, and earthquakes as well as the evolution of Earth’s surface and reconstructing its past continents and oceans.

© MinuteEarth (A Britannica Publishing Partner)

The concept of plate tectonics was formulated in the 1960s. According to the theory, Earth has a rigid outer layer, known as the lithosphere, which is typically about 100 km (60 miles) thick and overlies a plastic (moldable, partially molten) layer called the asthenosphere. The lithosphere is broken up into seven very large continental- and ocean-sized plates, six or seven medium-sized regional plates, and several small ones. These plates move relative to each other, typically at rates of 5 to 10 cm (2 to 4 inches) per year, and interact along their boundaries, where they converge, diverge, or slip past one another. Such interactions are thought to be responsible for most of Earth’s seismic and volcanic activity, although earthquakes and volcanoes can occur in plate interiors. Plate motions cause mountains to rise where plates push together, or converge, and continents to fracture and oceans to form where plates pull apart, or diverge. The continents are embedded in the plates and drift passively with them, which over millions of years results in significant changes in Earth’s geography.

The theory of plate tectonics is based on a broad synthesis of geologic and geophysical data. It is now almost universally accepted, and its adoption represents a true scientific revolution, analogous in its consequences to quantum mechanics in physics or the discovery of the genetic code in biology. Incorporating the much older idea of continental drift, as well as the concept of seafloor spreading, the theory of plate tectonics has provided an overarching framework in which to describe the past geography of continents and oceans, the processes controlling creation and destruction of landforms, and the evolution of Earth’s crust, atmosphere, biosphere, hydrosphere, and climates. During the late 20th and early 21st centuries, it became apparent that plate-tectonic processes profoundly influence the composition of Earth’s atmosphere and oceans, serve as a prime cause of long-term climate change, and make significant contributions to the chemical and physical environment in which life evolves.

For details on the specific effects of plate tectonics, see the articles earthquake and volcano. A detailed treatment of the various land and submarine relief features associated with plate motion is provided in the articles tectonic landform and ocean.

In essence, plate-tectonic theory is elegantly simple. Earth’s surface layer, 50 to 100 km (30 to 60 miles) thick, is rigid and is composed of a set of large and small plates. Together, these plates constitute the lithosphere, from the Greek lithos, meaning “rock.” The lithosphere rests on and slides over an underlying partially molten (and thus weaker but generally denser) layer of plastic partially molten rock known as the asthenosphere, from the Greek asthenos, meaning “weak.” Plate movement is possible because the lithosphere-asthenosphere boundary is a zone of detachment. As the lithospheric plates move across Earth’s surface, driven by forces as yet not fully understood, they interact along their boundaries, diverging, converging, or slipping past each other. While the interiors of the plates are presumed to remain essentially undeformed, plate boundaries are the sites of many of the principal processes that shape the terrestrial surface, including earthquakes, volcanism, and orogeny (that is, formation of mountain ranges).
A cross section of Earth’s outer layers, from the crust through the lower mantle.
A cross section of Earth’s outer layers, from the crust through the lower mantle.
Encyclopædia Britannica, Inc.

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Solution:
// Header Files #include<stdio.h> #include<conio.h> #include<BIOS.H> #inlcude<DOS.H> void interrupt (*oldTimer)(*void); // To store current Timer vector void interrupt newTimer(); //New Timer Function char far *scr= (char far *)0xB8000000; //Screen segment int in, t=0; void main() { clrscr(); oldTimer=getvect(8); setvect(8,newTimer); getch(); } void interrupt newTimer(); { *(scr+t)=0x2A; t++; if(t>=126) { for(i=0;i<4000;i+=2) { *(scr+i)=0x20; // Blank screen *(scr+i+1)=0x07; } t=0; } (*oldTimer)(); } }
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@zareen said in GSC101 Assignment 1 Solution and Discussion:

Question No. 1
a) If the average velocity of the object in the given interval of time is zero then what will be value of its displacement? Explain the reason.
b) Is it possible that an object have weight but no mass? Explain the reason.
Marks = 5+5=10

Q.1 Solution:
a) If the average velocity is continuously zero then this is easy to deal with. The object has not moved at all and so its displacement is zero. If it has moved and the average velocity is zero, then this means that at the end of the time interval, the object was back where it started this means the displacement is zero and so the average velocity is zero over the time period.
b) It is not possible. Mass is quantity of matter in the body which remains always same everywhere. Weight is force of gravity which always changes with gravity. At enter of earth gravity is zero so weight is zero but mass of an object will not zero.

Question No. 2 The required speed of a commercial aeroplane is 120 knots before it can take off. If this plane take 30 s to cover the runway then calculate
a) Acceleration
b) Runway length
[Hint: knot is nautical mile per hour or equal to half a meter per seconds]
Marks =5+5= 10

Q.2 Solution:
1 Knot=1/1.944 meter per seconds

1 Knot=0.514 meter per seconds

120 Knot=0.514 ×120 meter per seconds

120 Knot≈61 meter per seconds
Acceleration
Given:
Vi =0 ms-1
Vf =61 ms-1
t=30s
a=?
Solution:
a=∆v/∆t
a=(vf-vi)/∆t
a=(61-0)/30
a=2 ms^(-2)
Runway length
Given:
Vi=0 ms-1
Vf =61 ms-1
t=30s
a=2ms-2
S=?
Solution:
s=V_i t+1/2 at^2
s=0×30+1/2(2)〖(30)〗^2
s=0+900
s=900 m
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CS435 Assignment 1 Solution and Discussion

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