View Factor Orientation (or View factor or shape factor) plays an important role in radiation heat transfer. View factor is defined as, "fraction of radiation leaving surface 'i' and strike 'j' ". Summation Rule (View Factor) If there is are similar surfaces 'i' and 'j' , then: Blackbody Radiation Exchange Radiation Exchange between Opaque, Diffuse, Gray surfaces in an Enclosure 1. Opaque 2. Surfaces 3. Two surface enclosure Radiation Shield It is used to protect surfaces from radiation act like a reflective surface. References: Material from Class Lectures + Book named Fundamentals of Heat and Mass Transfer by Theodore L. Bergman + My knowledge. Photoshoped pics are developed. Some pics and GIF from Google. Videos from YouTube ( Engineering Sights ).
Get link
Facebook
X
Pinterest
Email
Other Apps
Introduction and Basic Concepts about Thermodynamics
Get link
Facebook
X
Pinterest
Email
Other Apps
-
THERMODYNAMICS
Thermodynamics actually includes all aspects of energy, energy transformation and relationship among the properties of matter.
Applications of Thermodynamics:
There are many applications of thermodynamics bit some of them are :
1. Human body
2. Refrigeration system
3. Air-conditioning system
4. Aeroplanes
5. Power Plants
6. Automobiles, etc.
SYSTEM AND CONTROL VOLUME:
System is any thing which is under consideration.
Volume of system or under boundary is called control volume.
TYPES OF SYSTEM:
1. OPEN SYSTEM:
System through which mass and energy can cross the boundary is called open system.
2. CLOSE SYSTEM:
System through which energy can transfer but mass cannot cross the boundary.
3. ISOLATED SYSTEM:
System through which mass and energy cannot transfer.
PROPERTIES OF A SYSTEM :
Any characteristic of a system defines property of a system. They are divided into several types:
1. INTENSIVE PROPERTIES:
Properties which does not depend upon the size and quantity of system. For exaqmple: temperature, pressure, density, etc.
2. EXTENSIVE PROPERTIES:
Properties which does depend upon the size and quantity of system. For example: mass, volume, mole, etc.
3. SPECIFIC PROPERTIES:
It is defined as;
Extensive properties per unit mass.
For example:
1. specific volume = volume / mass
2. Specific energy = energy / mass
3. Specfic weight = weight / volume, etc.
CONTINUUM APPROACH:
Consideration of continuity of matter that there are no holes between molecules is called Continuum Approach.
Note: At high altitudes, mean free path becomes much greater so continuum approach is not applicable. For this Rare-fied Gas Flow Theory is used.
RELATIVE DENSITY or SPECIFIC GRAVITY:
Density of solids relative to standard liquid's density that is water.
Specific Gravity = S.G. = Density of substance/Density of water
STATE OF A SYSTEM:
If a system is in equilibrium, then properties give the state of a system.
EQUILIBRIUM:
It imlpies the state of balance. A system ion equilibrium rxperiences no change.
For example:
* Thermal equilibrium: No change in temperature.
*Mechanical equilibrium: No change in pressure.
*Chemical equilibrium: No change in composition.
THE STATE POSTULATE:
It states that;
The state of a simple compressible system is completely specified by two independent intensive properties.
SIMPLE COMPRESSIBLE SYSTEM:
A system in the absence of electrical, mechanical, gravitational motion and surface tension effects is called Simple Compressible System.
PROCESS AND CYCLES:
Process is defined as;
Any change that a system undergoes from one equilibrium state to another.
Cycle is defined as;
If a system returns to its initial state at the end of the process.
QAUSI-EQUILIBRIUM PROCESS OR QUASI-STATIC:
When a process proceeds in such a manner that the system remains infinitesimally close to an equilibrium state at all times is called Quasi-equilibrium process.
ZEROTH LAW OF THERMODYNAMICS:
It states that;
If two bodies are in thermal equilibrium with the third body then they are also in thermal equilibrium with each other.
Projection: The term Projection is defined as: Presentation of an image or an object on a surface. The principles used to graphically represent 3-D objects and structures on 2-D media and it based on two variables: Line of Sight. Plane of Projection. Line of Sight & Plane of Projection: Line of sight is divided into 2 types: Parallel Projection Converging Projection & A plane of projection is an imaginary flat plane upon which the image created by the lines of sight is projected. Orthographic Projection: When the projectors are parallel to each other and perpendicular to the plane of projection. The lines pf sight of the observer create a view on the screen. The screen is referred to as the Plane of Projection (POP). The lines of sight are called Projection lines or projectors. Rules of Orthographic Projection: Edges that are parallel to a plane of projection appear as lines. Edges that are inclined to a plan
TAPING CORRECTIONS There are two types of corrections depending upon the type of errors in tape due to the different conditions. 1. Systematic Errors : Slope Erroneous tape length Temperature Tension Sag 2. Random Errors : Slope Alignment Marking & Plumbing Temperature Tension & Sag 1. Temperature Correction It is necessary to apply this correction, since the length of a tape is increased as its temperature is raised, and consequently, the measured distance is too small. It is given by the formula, C t = 𝛼 (T m – T o )L Where, C t = the correction for temperature, in m. 𝛼 = the coefficient of thermal expansion. T m = the mean temperature during measurement. T o = the temperature at which the tape is standardized. L = the measure length in m. For Foot Unit : C t = 6.45×10^-6 (T m – 68 )L For Metric Unit : C t = 1.16
ENGINEERING SURVEY Surveying is the science, art and technology of determine the relative positions of points above, on or beneath the Earth's surface so as to construct a map, plan or description. TYPES OF SURVEY : There are many types of survey but we discuss some of them. 1. Plane & Geodatic Survey : Ordinary field and topographical surveying in which the Curvature of Earth's surface is disregarded is called Plane Survey. It is performed when the area is smaller than 250sq.km. A survey of a large land area in which corrections are made for the Curvature of Earth's surface is called Geodatic survey. Why Geodatic Survey is important? Earth's surface is not flat, it is sphere. So all the calculations which were made by considering the Earth's surface flat are incorrect. So a new type of survey came into play which made calculations on the basis of geodatic condition of Earth's surface. 2. Topographic Survey : Topographic surv
Comments
Post a Comment
HI, we wI'll contact you later