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Human Digestion Process

November 27, 2011 Leave a comment

image

 

The whole digestive system is around 9 meters long. In a healthy human adult this process can take between 24 and 72 hours. Food digestion physiology varies between individuals and upon other factors such as the characteristics of the food and size of the meal.[16]

[edit] Phases of gastric secretion
  • Cephalic phase – This phase occurs before food enters the stomach and involves preparation of the body for eating and digestion. Sight and thought stimulate the cerebral cortex. Taste and smell stimulus is sent to the hypothalamus and medulla oblongata. After this it is routed through the vagus nerve and release of acetylcholine. Gastric secretion at this phase rises to 40% of maximum rate. Acidity in the stomach is not buffered by food at this point and thus acts to inhibit parietal (secretes acid) and G cell (secretes gastrin) activity via D cell secretion of somatostatin.
  • Gastric phase – This phase takes 3 to 4 hours. It is stimulated by distension of the stomach, presence of food in stomach and decrease in pH. Distention activates long and myenteric reflexes. This activates the release of acetylcholine, which stimulates the release of more gastric juices. As protein enters the stomach, it binds to hydrogen ions, which raises the pH of the stomach. Inhibition of gastrin and gastric acid secretion is lifted. This triggers G cells to release gastrin, which in turn stimulates parietal cells to secrete gastric acid. Gastric acid is about 0.5% hydrochloric acid (HCl), which lowers the pH to the desired pH of 1-3. Acid release is also triggered by acetylcholine and histamine.
  • Intestinal phase – This phase has 2 parts, the excitatory and the inhibitory. Partially digested food fills the duodenum. This triggers intestinal gastrin to be released. Enterogastric reflex inhibits vagal nuclei, activating sympathetic fibers causing the pyloric sphincter to tighten to prevent more food from entering, and inhibits local reflexes.
[edit] Oral cavity

Main article: Mouth (human)

In humans, digestion begins in the oral cavity, otherwise known as the "Buccal Cavity", where food is chewed. Saliva is secreted in large amounts (1-1.5 litres/day) by three pairs of exocrine salivary glands (parotid, submandibular, and sublingual) in the oral cavity, and is mixed with the chewed food by the tongue. Saliva cleans the oral cavity, moistens the food, and contains digestive enzymes such as salivary amylase, which aids in the chemical breakdown of polysaccharides such as starch into disaccharides such as maltose. It also contains mucus, a glycoprotein that helps soften the food and form it into a bolus. An additional enzyme, lingual lipase, hydrolyzes long-chain triglycerides into partial glycerides and free fatty acids.

Swallowing transports the chewed food into the esophagus, passing through the oropharynx and hypopharynx. The mechanism for swallowing is coordinated by the swallowing center in the medulla oblongata and pons. The reflex is initiated by touch receptors in the pharynx as the bolus of food is pushed to the back of the mouth.

[edit] Pharynx

Main article: Human pharynx

The pharynx is the part of the neck and throat situated immediately behind the mouth and nasal cavity, and cranial, or superior, to the esophagus. It is part of the digestive system and respiratory system. Because both food and air pass through the pharynx, a flap of connective tissue, the epiglottis closes over the trachea when food is swallowed to prevent choking or asphyxiation.

The oropharynx is that part of the pharynx behind the oral cavity. It is lined with stratified squamous epithelium. The nasopharynx lies behind the nasal cavity and like the nasal passages is lined with ciliated columnar pseudostratified epithelium.

Like the oropharynx above it the hypopharynx (laryngopharynx) serves as a passageway for food and air and is lined with a stratified squamous epithelium. It lies inferior to the upright epiglottis and extends to the larynx, where the respiratory and digestive pathways diverge. At that point, the laryngopharynx is continuous with the esophagus. During swallowing, food has the "right of way", and air passage temporarily stops.

[edit] Esophagus

Main article: esophagus

The esophagus is a narrow muscular tube about 20-30 centimeters long, which starts at the pharynx at the back of the mouth, passes through the thoracic diaphragm, and ends at the cardiac orifice of the stomach. The wall of the esophagus is made up of two layers of smooth muscles, which form a continuous layer from the esophagus to the colon and contract slowly, over long periods of time. The inner layer of muscles is arranged circularly in a series of descending rings, while the outer layer is arranged longitudinally. At the top of the esophagus, is a flap of tissue called the epiglottis that closes during swallowing to prevent food from entering the trachea (windpipe). The chewed food is pushed down the esophagus to the stomach through peristaltic contraction of these muscles. It takes only about seven seconds for food to pass through the esophagus and now digestion takes place.

[edit] Stomach

Main article: Stomach

The stomach is a small, ‘J’-shaped pouch with walls made of thick, elastic muscles, which stores and helps break down food. Food reduced to very small particles is more likely to be fully digested in the small intestine, and stomach churning has the effect of assisting the physical disassembly begun in the mouth. Ruminants, who are able to digest fibrous material (primarily cellulose), use fore-stomachs and repeated chewing to further the disassembly. Rabbits and some other animals pass some material through their entire digestive systems twice. Most birds ingest small stones to assist in mechanical processing in gizzards.

Food enters the stomach through the cardiac orifice where it is further broken apart and thoroughly mixed with gastric acid, pepsin and other digestive enzymes to break down proteins. The enzymes in the stomach also have an optimum, meaning that they work at a specific pH and temperature better than any others. The acid itself does not break down food molecules, rather it provides an optimum pH for the reaction of the enzyme pepsin and kills many microorganisms that are ingested with the food. It can also denature proteins. This is the process of reducing polypeptide bonds and disrupting salt bridges, which in turn causes a loss of secondary, tertiary, or quaternary protein structure. The parietal cells of the stomach also secrete a glycoprotein called intrinsic factor, which enables the absorption of vitamin B-12. Mucus neck cells are present in the gastric glands of the stomach. They secrete mucus, which along with gastric juice plays and important role in lubrication and protection of the mucosal epithelium from excoriation by the highly concentrated hydrochloric acid. Other small molecules such as alcohol are absorbed in the stomach, passing through the membrane of the stomach and entering the circulatory system directly. Food in the stomach is in semi-liquid form, which upon completion is known as chyme.

After consumption of food, digestive "tonic" and peristaltic contractions begin, which helps break down the food and move it through.[16] When the chyme reaches the opening to the duodenum known as the pylorus, contractions "squirt" the food back into the stomach through a process called retropulsion, which exerts additional force and further grinds down food into smaller particles.[16] Gastric emptying is the release of food from the stomach into the duodenum; the process is tightly controlled with liquids being emptied much more quickly than solids.[16] Gastric emptying has attracted medical interest as rapid gastric emptying is related to obesity and delayed gastric emptying syndrome is associated with diabetes mellitus, aging, and gastroesophageal reflux.[16]

The transverse section of the alimentary canal reveals four (or five, see description under mucosa) distinct and well developed layers within the stomach:

  • Serous membrane, a thin layer of mesothelial cells that is the outermost wall of the stomach.
  • Muscular coat, a well-developed layer of muscles used to mix ingested food, composed of three sets running in three different alignments. The outermost layer runs parallel to the vertical axis of the stomach (from top to bottom), the middle is concentric to the axis (horizontally circling the stomach cavity) and the innermost oblique layer, which is responsible for mixing and breaking down ingested food, runs diagonal to the longitudinal axis. The inner layer is unique to the stomach, all other parts of the digestive tract have only the first two layers.
  • Submucosa, composed of connective tissue that links the inner muscular layer to the mucosa and contains the nerves, blood and lymph vessels.
  • Mucosa is the extensively folded innermost layer. It can be divided into the epithelium, lamina propria, and the muscularis mucosae, though some consider the outermost muscularis mucosae to be a distinct layer, as it develops from the mesoderm rather than the endoderm (thus making a total of five layers). The epithelium and lamina are filled with connective tissue and covered in gastric glands that may be simple or branched tubular, and secrete mucus, hydrochloric acid, pepsinogen and rennin. The mucus lubricates the food and also prevents hydrochloric acid from acting on the walls of the stomach.
[edit] Small intestine

Main article: Small intestine

It has three parts Duodenum, Jejunum, and Ileum.

After being processed in the stomach, food is passed to the small intestine via the pyloric sphincter. The majority of digestion and absorption occurs here after the milky chyme enters the duodenum. Here it is further mixed with three different liquids:

The pH level increases in the small intestine. A more basic environment causes more helpful enzymes to activate and begin to help in the breakdown of molecules such as fat globules. Small, finger-like structures called villi, each of which is covered with even smaller hair-like structures called microvilli improve the absorption of nutrients by increasing the surface area of the intestine and enhancing speed at which nutrients are absorbed. Blood containing the absorbed nutrients is carried away from the small intestine via the hepatic portal vein and goes to the liver for filtering, removal of toxins, and nutrient processing.

The small intestine and remainder of the digestive tract undergoes peristalsis to transport food from the stomach to the rectum and allow food to be mixed with the digestive juices and absorbed. The circular muscles and longitudinal muscles are antagonistic muscles, with one contracting as the other relaxes. When the circular muscles contract, the lumen becomes narrower and longer and the food is squeezed and pushed forward. When the longitudinal muscles contract, the circular muscles relax and the gut dilates to become wider and shorter to allow food to enter.

[edit] Large intestine

Main article: Large intestine

After the food has been passed through the small intestine, the food enters the large intestine. Within it, digestion is retained long enough to allow fermentation due to the action of gut bacteria, which breaks down some of the substances that remain after processing in the small intestine; some of the breakdown products are absorbed. In humans, these include most complex saccharides (at most three disaccharides are digestible in humans). In addition, in many vertebrates, the large intestine reabsorbs fluid; in a few, with desert lifestyles, this reabsorbtion makes continued existence possible.

In humans, the large intestine is roughly 1.5 meters long, with three parts: the cecum at the junction with the small intestine, the colon, and the rectum. The colon itself has four parts: the ascending colon, the transverse colon, the descending colon, and the sigmoid colon. The large intestine absorbs water from the bolus and stores feces until it can be egested. Food products that cannot go through the villi, such as cellulose (dietary fiber), are mixed with other waste products from the body and become hard and concentrated feces. The feces is stored in the rectum for a certain period and then the stored feces is eliminated from the body due to the contraction and relaxation through the anus. The exit of this waste material is regulated by the anal sphincter.

 

Source: Human Digestion Process

Categories: Science & Engineering

Samsung 32 Inch LED TV 4, 5, 6 Series Comparision

October 22, 2011 Leave a comment

 

4 Products Match

Display: Sort by: Page: previous 1 next

UA32D6000SR

4.4286

7 reviews

MRP Rs. 54,500/-*

Save Compare

UA32D5900VR

4.3333

6 reviews

MRP Rs. 48,900/-*

Save Compare

UA32D5000PRMXL

4.85

20 reviews

MRP Rs. 45,900/-*

Save Compare

UA32D4000N

4.5

2 reviews

MRP Rs. 40,900/-*

Save Compare

 

clip_image001
clip_image002

product

clip_image003

UA32D6000SR

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UA32D5900VR

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UA32D4000N

Series

Series

6

5

4

Video

Screen Size

81.28cm (32)

81.28cm (32)

32

Resolution

1920 x 1080

1920 x 1080

1366 x 768

Picture Engine

3D HyperReal Engine

HyperReal Engine

HyperReal Engine

Clear Motion Rate

200

100

50

Dynamic Contrast Ratio

 

Mega Contrast

Mega Contrast

Wide Color Enhancer Plus

Wide Colour Enhancer Plus

Wide Colour Enhancer Plus

Wide Colour Enhancer Plus

Display

Ultra Clear Panel

Yes

Yes

 

Audio

Dolby

Dolby Digital Plus / Dolby Pulse

Dolby Digital Plus/Dolby Pulse

Dolby Digital Plus/Dolby Pulse

SRS

SRS TheatreSound HD

SRS TheatreSound HD

SRS TheaterSound HD

dts 2.0 + Digital Out

Yes

Yes

Yes

Sound Output (RMS)

10W x 2

10 watts x 2

10 watts x 2

Speaker Type

Down Firing + Full Range

Down Firing + Full Range

Down Firing + Full Range

Smart TV Functionality

Samsung Apps

Yes

Yes

 

Samsung SMART TV

Yes

Yes

 

Smart Hub

Yes

Yes

 

Search All

Yes

   

Your Video

Yes

   

Social TV

Yes

   

Feature

Samsung 3D

Yes

   

3D Sound (TV)

Yes

   

Allshare (Powerd by DLNA)

Yes

Yes

 

Smart Phone Remote support

Yes

Yes

 

Wireless LAN Adapter Support

Yes (Customer need to buy Adapter)

Yes (Customer need to buy Adapter)

 

ConnectShare™ (USB2.0)

Movie

Movie

Movie

BD Wise

Yes

   

Anynet+ (HDMI-CEC)

Yes

Yes

Yes

HDMI 1.4 3D Auto Setting

Yes

   

HDMI 1.4 A / Return Ch. Support

Yes

   

InstaPort S (HDMI quick switch)

Yes

   

Auto Channel Search

Yes

Yes

Yes

EPG

 

Yes

 

Teletext (TTXT)

Yes

 

Yes

OSD language

Local Languages

Local Languages

Local Languages

Auto Volume Leveler

Yes

Yes

Yes

Auto Power Off

Yes

Yes

Yes

Clock & On/Off timer

Yes

Yes

Yes

Sleep Timer

Yes

Yes

Yes

Game mode

Yes

Yes

Yes

Picture-in-Picture

1 Tuner PIP

1 Tuner PIP

1 Tuner PIP

Input & Output

HDMI

4

4

4

USB

3

2

1

Component In (Y/Pb/Pr)

1

1

1

Composite In (AV)

2 (1 : Common Use for Component Y)

1 (Common Use for Component Y)

1 (Common Use for Component Y)

Digital Audio Out (Optical)

1

1

1

PC In (D-sub)

1

1

1

RF In (Terrestrial/Cable Input)

1

2

1

Headphone

1

 

1

PC Audio In (Mini Jack)

1

1

1

DVI Audio In (Mini Jack)

1 (Common Use for PC Audio In)

1 (Common Use for PC Audio in)

1 (Common Use for PC Audio in)

Audio Out L-R (Mini Jack)

 

1

 

Ethernet (LAN)

1

1

 

Design

Design

ToC

ToC

ToC

Front Color

Rose Black

Rose Black

Dark Grey

Bezel Type

Normal

Normal

Normal

Slim Type

Ultra Slim

Ultra Slim

Ultra Slim

Stand Type

Square

Square

Square

Swivel (left/right)

Yes

Yes

 

Eco

Eco Label

Planet First

   

Eco Mark

Planet First

Planet First

Planet First

Eco Sensor

Yes

Yes

 

Power

Power Supply

AC 100 ~ 240V 50/60Hz

AC100 – 240V 50/60Hz

AC100 – 240V 50/60Hz

Power Consumption (Stand-by)

Under 0.3W

Under 0.3 watt

Under 0.3 watts

Power Consumption (Energy Saving Mode)

38

22 watts

22 watts

Power Consumption (Max.)

100

80 watts

70 watts

Dimension

Package Size (WxHxD)

984 x 560 x 120mm

984 x 560 x 120mm

984 x 560 x 120 mm

Set Size (WxHxD) with Stand

768.0 x 533.4 x 240.0mm

768.0 x 532.1 x 240.0mm

763.6 x 527.1 x 222.7 mm

Set Size (WxHxD) without Stand

768.0 x 475.3 x 29.9mm

768.0 x 468.2 x 29.9mm

763.6 x 463.1 x 29.9 mm

Weight

Package weight

11.4Kg

11.80Kg

10.8Kg

Set weight with stand

9.7Kg

9.96Kg

9.0Kg

Set weight without stand

7.0Kg

7.22Kg

7.0Kg

Accessory

Remote Controller Model

Normal Button Remote

Normal Button Remote

Normal Button Remote

Ultra Slim Wall Mount Support

Yes

Yes

Yes

Vesa Wall Mount Support

No

 

No

Batteries (for Remote Control)

Yes

Yes

Yes

Slim Gender Cable

1 Component (AV share), 1 AV

1 Component (AV share)

1 Component (AV share)

ANT- Cable

   

No

Power Cable

Yes

Yes

Yes

E-Manual

Yes

Yes

Yes

User Manual

Yes

Yes

Yes

clip_image006Copyright© 1995-2009 SAMSUNG. All rights reserved.

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Genuine Windows® software is published by Microsoft and licensed and supported by Microsoft or an authorized licensor. Genuine software helps protect you from the risks of counterfeit software, provides you with special benefits and the experience and support you expect. Learn more by visiting www.microsoft.com/genuine.

 

Source: http://www.samsung.com/in/consumer/type/productcompare.do?&group=tv-audio-video&type=television&pageType=S&acc_ia_fl=N&prda=UA32D6000SRMXL&prdb=UA32D5900VRMXL&prdc=UA32D4000NMXL&view_gb=PRINT

Categories: Science & Engineering

Chemistry: Periodic Table of Elements

August 25, 2011 Leave a comment

image

 

image

 

 

image

Z
clip_image001

Sym
clip_image001[1]

Name
clip_image001[2]

Grp
clip_image001[3]

Prd
clip_image001[4]

Weight
clip_image001[5]

Density
clip_image001[6]

Melt
clip_image001[7]

Boil
clip_image001[8]

Heat
clip_image001[9]

Neg
clip_image001[10]

Abund
clip_image001[11]

1

H

Hydrogen

1

1

1.00794(7)2 3 4

0.00008988

14.175

20.28

14.304

2.20

1400

2

He

Helium

18

1

4.002602(2)2 4

0.0001785

n/a6

4.22

5.193

-

0.008

3

Li

Lithium

1

2

6.941(2)2 3 4 5

0.534

453.85

1615

3.582

0.98

20

4

Be

Beryllium

2

2

9.012182(3)

1.85

1560.15

2742

1.825

1.57

2.8

5

B

Boron

13

2

10.811(7)2 3 4

2.34

2573.15

4200

1.026

2.04

10

6

C

Carbon

14

2

12.0107(8)2 4

2.267

3948.157

4300

0.709

2.55

200

7

N

Nitrogen

15

2

14.0067(2)2 4

0.0012506

63.29

77.36

1.04

3.04

19

8

O

Oxygen

16

2

15.9994(3)2 4

0.001429

50.5

90.20

0.918

3.44

461000

9

F

Fluorine

17

2

18.9984032(5)

0.001696

53.63

85.03

0.824

3.98

585

10

Ne

Neon

18

2

20.1797(6)2 3

0.0008999

24.703

27.07

1.03

-

0.005

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

11

Na

Sodium

1

3

22.98976928(2)

0.971

371.15

1156

1.228

0.93

23600

12

Mg

Magnesium

2

3

24.3050(6)

1.738

923.15

1363

1.023

1.31

23300

13

Al

Aluminium

13

3

26.9815386(8)

2.698

933.4

2792

0.897

1.61

82300

14

Si

Silicon

14

3

28.0855(3)4

2.3296

1683.15

3538

0.705

1.9

282000

15

P

Phosphorus

15

3

30.973762(2)

1.82

317.25

553

0.769

2.19

1050

16

S

Sulfur

16

3

32.065(5)2 4

2.067

388.51

717.8

0.71

2.58

350

17

Cl

Chlorine

17

3

35.453(2)2 3 4

0.003214

172.31

239.11

0.479

3.16

145

18

Ar

Argon

18

3

39.948(1)2 4

0.0017837

83.96

87.30

0.52

-

3.5

19

K

Potassium

1

4

39.0983(1)

0.862

336.5

1032

0.757

0.82

20900

20

Ca

Calcium

2

4

40.078(4)2

1.54

1112.15

1757

0.647

1

41500

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

21

Sc

Scandium

3

4

44.955912(6)

2.989

1812.15

3109

0.568

1.36

22

22

Ti

Titanium

4

4

47.867(1)

4.54

1933.15

3560

0.523

1.54

5650

23

V

Vanadium

5

4

50.9415(1)

6.11

2175.15

3680

0.489

1.63

120

24

Cr

Chromium

6

4

51.9961(6)

7.15

2130.15

2944

0.449

1.66

102

25

Mn

Manganese

7

4

54.938045(5)

7.44

1519.15

2334

0.479

1.55

950

26

Fe

Iron

8

4

55.845(2)

7.874

1808.15

3134

0.449

1.83

56300

27

Co

Cobalt

9

4

58.933195(5)

8.86

1768.15

3200

0.421

1.88

25

28

Ni

Nickel

10

4

58.6934(4)

8.912

1726.15

3186

0.444

1.91

84

29

Cu

Copper

11

4

63.546(3)4

8.96

1357.75

2835

0.385

1.9

60

30

Zn

Zinc

12

4

65.38(2)

7.134

692.88

1180

0.388

1.65

70

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

31

Ga

Gallium

13

4

69.723(1)

5.907

302.91

2477

0.371

1.81

19

32

Ge

Germanium

14

4

72.64(1)

5.323

1211.45

3106

0.32

2.01

1.5

33

As

Arsenic

15

4

74.92160(2)

5.776

1090.157

887

0.329

2.18

1.8

34

Se

Selenium

16

4

78.96(3)4

4.809

494.15

958

0.321

2.55

0.05

35

Br

Bromine

17

4

79.904(1)

3.122

266.05

332.0

0.474

2.96

2.4

36

Kr

Krypton

18

4

83.798(2)2 3

0.003733

115.93

119.93

0.248

3

<0.001

37

Rb

Rubidium

1

5

85.4678(3)2

1.532

312.79

961

0.363

0.82

90

38

Sr

Strontium

2

5

87.62(1)2 4

2.64

1042.15

1655

0.301

0.95

370

39

Y

Yttrium

3

5

88.90585(2)

4.469

1799.15

3609

0.298

1.22

33

40

Zr

Zirconium

4

5

91.224(2)2

6.506

2125.15

4682

0.278

1.33

165

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

41

Nb

Niobium

5

5

92.90638(2)

8.57

2741.15

5017

0.265

1.6

20

42

Mo

Molybdenum

6

5

95.96(2)2

10.22

2890.15

4912

0.251

2.16

1.2

43

Tc

Technetium

7

5

[98]1

11.5

2473.15

5150

-

1.9

<0.001

44

Ru

Ruthenium

8

5

101.07(2)2

12.37

2523.15

4423

0.238

2.2

0.001

45

Rh

Rhodium

9

5

102.90550(2)

12.41

2239.15

3968

0.243

2.28

0.001

46

Pd

Palladium

10

5

106.42(1)2

12.02

1825.15

3236

0.244

2.2

0.015

47

Ag

Silver

11

5

107.8682(2)2

10.501

1234.15

2435

0.235

1.93

0.075

48

Cd

Cadmium

12

5

112.411(8)2

8.69

594.33

1040

0.232

1.69

0.159

49

In

Indium

13

5

114.818(3)

7.31

429.91

2345

0.233

1.78

0.25

50

Sn

Tin

14

5

118.710(7)2

7.287

505.21

2875

0.228

1.96

2.3

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

51

Sb

Antimony

15

5

121.760(1)2

6.685

904.05

1860

0.207

2.05

0.2

52

Te

Tellurium

16

5

127.60(3)2

6.232

722.8

1261

0.202

2.1

0.001

53

I

Iodine

17

5

126.90447(3)

4.93

386.65

457.4

0.214

2.66

0.45

54

Xe

Xenon

18

5

131.293(6)2 3

0.005887

161.45

165.03

0.158

2.6

<0.001

55

Cs

Caesium

1

6

132.9054519(2)

1.873

301.7

944

0.242

0.79

3

56

Ba

Barium

2

6

137.327(7)

3.594

1002.15

2170

0.204

0.89

425

57

La

Lanthanum

 

6

138.90547(7)2

6.145

1193.15

3737

0.195

1.1

39

58

Ce

Cerium

 

6

140.116(1)2

6.77

1071.15

3716

0.192

1.12

66.5

59

Pr

Praseodymium

 

6

140.90765(2)

6.773

1204.15

3793

0.193

1.13

9.2

60

Nd

Neodymium

 

6

144.242(3)2

7.007

1289.15

3347

0.19

1.14

41.5

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

61

Pm

Promethium

 

6

[145]1

7.26

1204.15

3273

-

-

<0.001

62

Sm

Samarium

 

6

150.36(2)2

7.52

1345.15

2067

0.197

1.17

7.05

63

Eu

Europium

 

6

151.964(1)2

5.243

1095.15

1802

0.182

1.2

2

64

Gd

Gadolinium

 

6

157.25(3)2

7.895

1585.15

3546

0.236

1.2

6.2

65

Tb

Terbium

 

6

158.92535(2)

8.229

1630.15

3503

0.182

1.2

1.2

66

Dy

Dysprosium

 

6

162.500(1)2

8.55

1680.15

2840

0.17

1.22

5.2

67

Ho

Holmium

 

6

164.93032(2)

8.795

1743.15

2993

0.165

1.23

1.3

68

Er

Erbium

 

6

167.259(3)2

9.066

1795.15

3503

0.168

1.24

3.5

69

Tm

Thulium

 

6

168.93421(2)

9.321

1818.15

2223

0.16

1.25

0.52

70

Yb

Ytterbium

 

6

173.054(5)2

6.965

1097.15

1469

0.155

1.1

3.2

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

71

Lu

Lutetium

3

6

174.9668(1)2

9.84

1936.15

3675

0.154

1.27

0.8

72

Hf

Hafnium

4

6

178.49(2)

13.31

2500.15

4876

0.144

1.3

3

73

Ta

Tantalum

5

6

180.94788(2)

16.654

3269.15

5731

0.14

1.5

2

74

W

Tungsten

6

6

183.84(1)

19.25

3680.15

5828

0.132

2.36

1.3

75

Re

Rhenium

7

6

186.207(1)

21.02

3453.15

5869

0.137

1.9

<0.001

76

Os

Osmium

8

6

190.23(3)2

22.61

3300.15

5285

0.13

2.2

0.002

77

Ir

Iridium

9

6

192.217(3)

22.56

2716.15

4701

0.131

2.2

0.001

78

Pt

Platinum

10

6

195.084(9)

21.46

2045.15

4098

0.133

2.28

0.005

79

Au

Gold

11

6

196.966569(4)

19.282

1337.73

3129

0.129

2.54

0.004

80

Hg

Mercury

12

6

200.59(2)

13.5336

234.43

630

0.14

2

0.085

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

81

Tl

Thallium

13

6

204.3833(2)

11.85

577.15

1746

0.129

1.62

0.85

82

Pb

Lead

14

6

207.2(1)2 4

11.342

600.75

2022

0.129

2.33

14

83

Bi

Bismuth

15

6

208.98040(1)

9.807

544.67

1837

0.122

2.02

0.009

84

Po

Polonium

16

6

[210]1

9.32

527.15

1235

-

2

<0.001

85

At

Astatine

17

6

[210]1

7

575.15

610

-

2.2

<0.001

86

Rn

Radon

18

6

[222]1

0.00973

202.15

211.3

0.094

-

<0.001

87

Fr

Francium

1

7

[223]1

1.87

300.15

950

-

0.7

<0.001

88

Ra

Radium

2

7

[226]1

5.5

973.15

2010

-

0.9

<0.001

89

Ac

Actinium

 

7

[227]1

10.07

1323.15

3471

0.12

1.1

<0.001

90

Th

Thorium

 

7

232.03806(2)1 2

11.72

2028.15

5061

0.113

1.3

9.6

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

91

Pa

Protactinium

 

7

231.03588(2)1

15.37

1873.15

4300

-

1.5

<0.001

92

U

Uranium

 

7

238.02891(3)1

18.95

1405.15

4404

0.116

1.38

2.7

93

Np

Neptunium

 

7

[237]1

20.45

913.15

4273

-

1.36

<0.001

94

Pu

Plutonium

 

7

[244]1

19.84

913.15

3501

-

1.28

<0.001

95

Am

Americium

 

7

[243]1

13.69

1267.15

2880

-

1.3

08

96

Cm

Curium

 

7

[247]1

13.51

1340.15

3383

-

1.3

0

97

Bk

Berkelium

 

7

[247]1

14.79

1259.15

983

-

1.3

0

98

Cf

Californium

 

7

[251]1

15.1

1925.15

1173

-

1.3

0

99

Es

Einsteinium

 

7

[252]1

13.5

1133.15

-

-

1.3

0

100

Fm

Fermium

 

7

[257]1

-

-

-

-

1.3

0

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

101

Md

Mendelevium

 

7

[258]1

-

-

-

-

1.3

0

102

No

Nobelium

 

7

[259]1

-

-

-

-

1.3

0

103

Lr

Lawrencium

3

7

[262]1

-

-

-

-

1.3

0

104

Rf

Rutherfordium

4

7

[261]1

18.1

-

-

-

-

0

105

Db

Dubnium

5

7

[262]1

39

-

-

-

-

0

106

Sg

Seaborgium

6

7

[266]1

35

-

-

-

-

0

107

Bh

Bohrium

7

7

[264]1

37

-

-

-

-

0

108

Hs

Hassium

8

7

[267]1

41

-

-

-

-

0

109

Mt

Meitnerium

9

7

[268]1

35

-

-

-

-

0

110

Ds

Darmstadtium

10

7

[271]1

-

-

-

-

-

0

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

111

Rg

Roentgenium

11

7

[272]1

-

-

-

-

-

0

112

Cn

Copernicium

12

7

[285]1

-

-

-

-

-

0

113

Uut

Ununtrium

13

7

[284]1

-

-

-

-

-

0

114

Uuq

Ununquadium

14

7

[289]1

-

-

-

-

-

0

115

Uup

Ununpentium

15

7

[288]1

-

-

-

-

-

0

116

Uuh

Ununhexium

16

7

[292]1

-

-

-

-

-

0

117

Uus

Ununseptium

17

7

[295]1

-

-

-

-

-

0

118

Uuo

Ununoctium

18

7

[294]1

-

-

-

-

-

0

Z

Sym

Name

Grp

Prd

Weight

Density

Melt

Boil

Heat

Neg

Abund

Categories: Science & Engineering

Material Science: Factors causing Brittleness in Materials

June 2, 2011 Leave a comment

Below are the various factors/conditions under which material behave in brittle fashion:

  1.  Low temperature aiding stress increase to move dislocations. At, higher temperatures then the brittle-ductile temperature, the material yields plastically
  2. Surface Condition/Finishing free of defects results in limited plastic deformation caused by dislocation motion. Presence of surface flaws makes crystals prone to brittle failure
  3. Grain Size and the Stress Required to Move a Dislocation: the stress to nucleate a crack by slip intersection increases with decreasing grain size.  Thus, fine grained materials have a lower transition temperature compared to coarse grained materials
  4. In Polymeric Materials molecular motion is frozen below glass transition temperature causing viscous flow or high elasticity restricted.  Thus polymers behave brittle under these conditions and this behavior can be explained by Griffith theory.  
  5.  
Categories: Science & Engineering

Material Science: Crystal lattice, planes and directions, Miller Indices

March 26, 2011 Leave a comment
Categories: Science & Engineering

Material Science: Phases

March 26, 2011 Leave a comment

Phase: A phase may be defined as a homogeneous portion of a system that has uniform physical and chemical characteristics. Every pure material is considered to be a phase;

If more than one phase is present in a given system, each will have its own distinct properties, and a boundary separating the phases will exist across which there will be a discontinuous and abrupt change in physical and/or chemical characteristics. When two phases are present in a system, it is not necessary that there be a difference in both physical and chemical properties; a disparity in one or the other set of properties is sufficient. Also, when a substance can exist in two or more polymorphic forms (e.g., having both FCC and BCC structures), each of these structures is a separate phase because their respective physical characteristics differ.

Equilibrium: A system is at equilibrium if its free energy is at a minimum under some specified combination of temperature, pressure, and composition. Phase equilibrium is reflected by a constancy with time in the phase characteristics of a system.

There are three externally controllable parameters that will affect phase structure—viz. temperature, pressure, and composition—

and phase diagrams are constructed when various combinations of these parameters are plotted against one another.

Lever rule for phase analysis, which follows the rule of mass conservation, states that the quantities of the individual components present in an alloy must be equal to the sum of their quantities in the liquid and the solid phases. Lever rule also indicates that quantities of phases being in equilibrium are inversely proportional to respective phases, in case of, two components.

Categories: Science & Engineering

Material Science: Griffith’s theory

March 26, 2011 1 comment

Griffith’s theory

Griffith’s theory of failure is based on the assumption that the low order of tensile strength in common materials is due to the presence of small cracks or flaws. Actual stresses may occur around these flaws, which are of the order of magnitude of molecular cohesion values, while the average tensile strength may be quite low. Mohr’s theory predicts that failure of materials is due to failure in shear, whereas Griffith’s theory postulates that it is due to failure at crack tips.

- http://www.maden.hacettepe.edu.tr/dmmrt/dmmrt522.html

Links

Ductile & Brittle Fracture – http://nhml.com/resources_NHML_Ductile-Brittle-Fracture.php

Categories: Science & Engineering

Material Science: Ceramics

March 26, 2011 Leave a comment

Definitions:

Ceramics are known for their high temperature melting points, high mechanical strengths, electrical, magnetic, optical and thermal properties.

- http://www.mse.uiuc.edu/home/introduction.html

The word ceramic is derived from the Greek word κεραμικός (keramikos). The term covers inorganic non-metallic materials which are formed by the action of heat.

- http://en.wikipedia.org/wiki/Ceramic

The percentage ionic character: of a bond between elements A and B (A being the most electronegative) may be approximated by the expression

% ionic character = {1 – exp[-(0.25)(XA - XB)2]} x 100

where XA and XB are the electronegativities for the respective elements.

Two characteristics of the component ions in crystalline ceramic materials influence the crystal structure:

- the magnitude of the electrical charge on each of the component ions, and,

- the relative sizes of the cations and anions.

Question and Answers:

1. Why are ceramics brittle and most metals not?

In ceramic materials, the atoms are not free to move under stress as they are in metals.

- http://matse1.mse.uiuc.edu/ceramics/quiz.html

Ceramics have very high yield strengths, and thus very little plastic deformation takes place at crack tips in these materials. The local stress ahead of the crack tip reaches excess of the ideal strength and is thus large enough to break apart the interatomic bonds there. The crack then spreads between a pair of atomic planes giving rise to an atomically flat surface by cleavage. The energy required simply to break the interatomic bonds is much less than that absorbed by ductile tearing in a tough material, and this is why materials like ceramics and glasses are so brittle. The crack mechanism in Ceramics is called Cleavege.

- Engineering Materials 1

The atoms in ceramic materials are held together by a chemical bond which will be discussed a bit later. Briefly though, the two most common

chemical bonds for ceramic materials are covalent and ionic. Covalent and ionic bonds are much stronger than in metallic bonds and, generally speaking, this is why ceramics are brittle and metals are ductile.

http://www.ndt-ed.org/EducationResources/CommunityCollege/Materials/Introduction/ceramics.htm

Brittle Fracture of Ceramics

Stress–Strain Behavior

At room temperature, virtually all ceramics are brittle. Microcracks, the presence

of which is very difficult to control, result in amplification of applied tensile stresses

and account for relatively low fracture strengths (flexural strengths). This amplification

does not occur with compressive loads, and, consequently, ceramics are

stronger in compression. Fractographic analysis of the fracture surface of a ceramic

material may reveal the location and source of the crack-producing flaw, as well as

the magnitude of the fracture stress. Representative strengths of ceramic materials

are determined by performing transverse bending tests to fracture.

Mechanisms of Plastic Deformation

Any plastic deformation of crystalline ceramics is a result of dislocation motion; the

brittleness of these materials is explained, in part, by the limited number of operable

slip systems. The mode of plastic deformation for noncrystalline materials is by

viscous flow; a material’s resistance to deformation is expressed as viscosity.At room

temperature, the viscosities of many noncrystalline ceramics are extremely high.

Miscellaneous Mechanical Considerations

Many ceramic bodies contain residual porosity, which is deleterious to both their moduli

of elasticity and fracture strengths. In addition to their inherent brittleness, ceramic

materials are distinctively hard. Also, since these materials are frequently utilized at

elevated temperatures and under applied loads, creep characteristics are important.

For crystalline ceramics, plastic deformation occurs, as with metals, by the motion

of dislocations (Chapter 7). One reason for the hardness and brittleness of these

materials is the difficulty of slip (or dislocation motion). For crystalline ceramic materials

for which the bonding is predominantly ionic, there are very few slip systems

(crystallographic planes and directions within those planes) along which dislocations

may move.This is a consequence of the electrically charged nature of the ions.

For slip in some directions, ions of like charge are brought into close proximity to

one another; because of electrostatic repulsion, this mode of slip is very restricted,

to the extent that plastic deformation in ceramics is rarely measurable at room temperature.

By way of contrast, in metals, since all atoms are electrically neutral, considerably

more slip systems are operable and, consequently, dislocation motion is

much more facile.

On the other hand, for ceramics in which the bonding is highly covalent, slip is

also difficult and they are brittle for the following reasons: (1) the covalent bonds

are relatively strong, (2) there are also limited numbers of slip systems, and (3) dislocation

structures are complex.

This causes detriment to fracture strength thus stress redistribution do not occur to any appreciable extent around flaws and discontinuities.

The brittle fracture process consists of the formation and propagation of cracks

through the cross section of material in a direction perpendicular to the applied

load. Crack growth in crystalline ceramics may be either transgranular (i.e., through

the grains) or intergranular (i.e., along grain boundaries); for transgranular fracture,

cracks propagate along specific crystallographic (or cleavage) planes, planes of high

atomic density.

Ceramics have very high yield strengths, and thus very little plastic deformation takes place at crack tips in these materials. The local stress ahead of the crack tip reaches excess of the ideal strength and is thus large enough to break apart the interatomic bonds there. The crack then spreads between a pair of atomic planes giving rise to an atomically flat surface by cleavage. The energy required simply to break the interatomic bonds is much less than that absorbed by ductile tearing in a tough material, and this is why materials like ceramics and glasses are so brittle. The crack mechanism in Ceramics is called Cleavege.

very high yield strengths, and thus very little plastic deformation takes place at crack tips in these materials.

Stress redistribution do not occur to any appreciable extent around flaws and discontinuities in brittle materials

The effect of a stress raiser is more significant in brittle than in ductile materials. For a ductile material, plastic deformation ensues when the maximum stress exceeds the yield strength. This leads to a more uniform distribution of stress in the vicinity of the stress raiser and to the development of a maximum stress concentration factor less than the theoretical value. Such yielding and stress redistribution do not occur to any appreciable extent around flaws and discontinuities in brittle materials; therefore, essentially the theoretical stress concentration will result.

This causes detriment to fracture strength and very high yield strengths, and thus very little plastic deformation takes place at crack tips in these materials. For a

The local stress ahead of the crack tip reaches excess of the ideal strength and is thus large enough to break apart the interatomic bonds there.

The crack then spreads between a pair of atomic planes giving rise to an atomically flat surface by cleavage. The energy required simply to break the interatomic bonds is much less than that absorbed by ductile tearing in a tough material, and this is why materials like ceramics and glasses are so brittle. The crack mechanism in Ceramics is called Cleavege.

These stress-raisers account for relatively low fracture strengths (flexural strengths).

Due to presence of stress raisers, Ceramics have significantly lower fracture strength.

When the magnitude of a tensile stress at the tip of one of these flaws exceeds the value of this critical stress, a crack forms and then propagates, which results in fracture.

The atoms in ceramic materials are most commonly held together by the two covalent and ionic primary bonds (or) mix of them. Covalent and ionic bonds are much stronger than metallic bonds. Both these bond types have a very few/limited slip systems (crystallographic planes and directions within those planes) as a consequence dislocations are limited and results in a negligible or no plastic deformation at room temperature. Ceramics, have very small and omnipresent flaws in the material that serve as stress raisers-points at which the magnitude of an applied tensile stress is amplified. These stress raisers may be minute surface or interior cracks (microcracks), internal pores, and grain corners, which are

virtually impossible to eliminate or control.

The measured fracture strengths for most brittle materials are significantly lower

than those predicted by theoretical calculations based on atomic bonding energies.

This discrepancy is explained by the presence of very small, microscopic flaws

or cracks that always exist under normal conditions at the surface and within the

interior of a body of material.These flaws are a detriment to the fracture strength

because an applied stress may be amplified or concentrated at the tip, the magnitude

of this amplification depending on crack orientation and geometry. This

phenomenon is demonstrated in Figure 8.8, a stress profile across a cross section

containing an internal crack. As indicated by this profile, the magnitude of this

localized stress diminishes with distance away from the crack tip. At positions far

Furthermore, the effect of a stress raiser is more significant in brittle than in

ductile materials. For a ductile material, plastic deformation ensues when the maximum

stress exceeds the yield strength. This leads to a more uniform distribution

of stress in the vicinity of the stress raiser and to the development of a maximum

stress concentration factor less than the theoretical value. Such yielding and stress

redistribution do not occur to any appreciable extent around flaws and discontinuities

in brittle materials; therefore, essentially the theoretical stress concentration

will result.

The brittle fracture process consists of the formation and propagation of cracks

through the cross section of material in a direction perpendicular to the applied

load. Crack growth in crystalline ceramics may be either transgranular (i.e., through

the grains) or intergranular (i.e., along grain boundaries); for transgranular fracture,

cracks propagate along specific crystallographic (or cleavage) planes, planes of high

atomic density.

Brittle materials, for which appreciable plastic deformation is not possible in

front of an advancing crack, have low values and are vulnerable to catastrophic

failure. On the other hand, values are relatively large for ductile materials. Fracture

mechanics is especially useful in predicting catastrophic failure in materials

having intermediate ductilities

Using principles of fracture mechanics, it is possible to show that the critical

stress required for crack propagation in a brittle material is described by the

expression

(8.3)

where

All brittle materials contain a population of small cracks and flaws that have a

variety of sizes, geometries, and orientations.When the magnitude of a tensile stress

at the tip of one of these flaws exceeds the value of this critical stress, a crack forms

and then propagates, which results in fracture. Very small and virtually defect-free

metallic and ceramic whiskers have been grown with fracture strengths that approach

their theoretical values.

Thus Ceramics are brittle. Whereas,

bonding is predominantly ionic, there are very few slip systems

(crystallographic planes and directions within those planes) along which dislocations

may move.This is a consequence of the electrically charged nature of the ions.

For slip in some directions, ions of like charge are brought into close proximity to

one another; because of electrostatic repulsion, this mode of slip is very restricted,

to the extent that plastic deformation in ceramics is rarely measurable at room temperature.

By way of contrast, in metals, since all atoms are electrically neutral, considerably

more slip systems are operable and, consequently, dislocation motion is

much more facile.

On the other hand, for ceramics in which the bonding is highly covalent, slip is

also difficult and they are brittle for the following reasons: (1) the covalent bonds

are relatively strong, (2) there are also limited numbers of slip systems, and (3) dislocation

structures are complex.

2. What are the two general classes of ceramics and how are they different?

+ Ceramics

+ Based on crystal structure

- 1. Crystalline – regular structure

- 2. Noncrystalline (amorphous)-irregular structure

+ Based on material used

- 1. Traditional – clay, cement & glass

- 2. Advanced – newer, high strength, high temperature materials

- http://matse1.mse.uiuc.edu/ceramics/quiz.html

3. List the parts of your body that are ceramic materials. How do you know that they are?

Bones and teeth – hard, brittle and temperature resistant.

- http://matse1.mse.uiuc.edu/ceramics/quiz.html

General properties Of Ceramics

1. High melting points

2. Tend to be brittle

3. Have both ionic and covalent bonds

4.

Advantages Of Ceramics

1. Hard

2. Temperature resistance

3. Corrosion resistance

4. Inexpensive

Dis-advantages Of Ceramics

1. Brittle

2. Hard to machine (mold/shape)

3.

- http://matse1.mse.uiuc.edu/ceramics/quiz.html

Categories: Science & Engineering

Material Science: Why are ceramics brittle and most metals not?

March 26, 2011 2 comments

1. Why are ceramics brittle and most metals not?

Ceramics materials have very small and omnipresent flaws as minute surface or interior cracks (microcracks), internal pores, and grain corners, which are virtually impossible to eliminate or control. These flaws serve as stress raisers such that depending on crack orientation and geometry, applied stress may be amplified or concentrated at the tip of the crack. When the magnitude of a tensile stress at the tip of one of these flaws exceeds the value of this critical stress which is large enough to break apart the interatomic bonds, a crack forms and then propagates, which results in fracture. Crack then propagates through the cross section of material in a direction perpendicular to the applied load. The energy required simply to break the interatomic bonds is much less than that absorbed by ductile tearing in a tough material, and this is why materials like ceramics and glasses are so brittle.

In more detail:

Bond type: The atoms in ceramic materials are most commonly held together by the two covalent and ionic primary bonds (or) mix of them. Covalent and ionic bonds are much stronger than metallic bonds.

Slip systems: Both these bond types have a very few/limited slip systems (crystallographic planes and directions within those planes) as a consequence dislocations are limited and results in a negligible or no plastic deformation at room temperature.

Stress raisers: The effect of a stress raiser is more significant in brittle than in ductile materials. For a ductile material, plastic deformation ensues when the maximum stress exceeds the yield strength. This leads to a more uniform distribution of stress in the vicinity of the stress raiser and to the development of a maximum stress concentration factor less than the theoretical value. Such yielding and stress redistribution do not occur to any appreciable extent around flaws and discontinuities in brittle materials; therefore, essentially the theoretical stress concentration will result.

Fracture strength: The measured fracture strengths for most brittle materials are significantly lower than those predicted by theoretical calculations based on atomic bonding energies.

Categories: Science & Engineering

Material Science: Defects/Imperfections and Impurities

March 26, 2011 Leave a comment

The simplest of the point defects is a vacancy, or vacant lattice site, one normally occupied from which an atom is missing.

Impurity point defects are found in solid solutions, of which there are two types: substitutional and interstitial.

A dislocation is a linear or one-dimensional defect around which some of the atoms are misaligned.

An edge dislocation moves in response to a shear stress applied in a direction perpendicular to its line;

One type of dislocation is an extra portion of a plane of atoms, or half-plane, the edge of which terminates within the crystal. This is termed an edge dislocation; it is a linear defect that centers around the line that is defined along the end of the extra half-plane of atoms. This is sometimes termed the dislocation line, which, for the edge dislocation, is perpendicular to the plane of the page.Within the region around the dislocation

line there is some localized lattice distortion. The atoms above the dislocation line are squeezed together, and those below are pulled apart; this is reflected in the slight curvature for the vertical planes of atoms as they bend around this extra half-plane.The magnitude of this distortion decreases with distance away from the dislocation line; at positions far removed, the crystal lattice is virtually perfect.

Another type of dislocation, called a screw dislocation, exists, which may be thought of as being formed by a shear stress that is applied to produce the distortion: the upper front region of the crystal is shifted one atomic distance to the right relative to the bottom portion.

The magnitude and direction of the lattice distortion associated with a dislocation is expressed in terms of a Burgers vector, denoted by a b. Also, even though a dislocation changes direction and nature within a crystal (e.g., from edge to mixed to screw), the Burgers vector will be the same at all points along its line.

Interfacial defects are boundaries that have two dimensions and normally separate regions of the materials that have different crystal structures and/or crystallographic orientations. These imperfections include external surfaces, grain boundaries, twin boundaries, stacking faults, and phase boundaries.

Other possible interfacial defects include stacking faults, phase boundaries, and ferromagnetic domain walls. Stacking faults are found in FCC metals when there is an interruption in the ABCABCABC . . . stacking sequence of close-packed planes.

Other defects exist in all solid materials that are much larger than those heretofore discussed. These include pores, cracks, foreign inclusions, and other phases. They are normally introduced during processing and fabrication steps. Some of these defects and their effects on the properties of materials.

Every atom in a solid material is vibrating very rapidly about its lattice position within the crystal. In a sense, these atomic vibrations may be thought of as imperfections or defects. At any instant of time not all atoms vibrate at the same frequency and amplitude, nor with the same energy. At a given temperature there will exist a distribution of energies for the constituent atoms about an average energy.

The process by which plastic deformation is produced by dislocation motion is termed slip; the crystallographic plane along which the dislocation line traverses is the slip plane

Categories: Science & Engineering
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