Effect of Ammonium Compounds as Additives on the Dissolution Rate of Limestone Samples Sourced From Tirunelveli District, Tamil Nadu, India

 

S. Vijaya Chitra

Department of Geology and Mining, Guindy, Chennai - 600 032 India

*Corresponding Author E-mail: vijchitra@yahoo.co.in

 

ABSTRACT:

Sulphur dioxide (SO2) represents one of the most important air pollution generators. The rate of CaCO3 dissolution in slurry scrubbers for flue gas desulphurization affects SO2 absorption, CaSO3 / CaSO4 scaling and ultimate CaCO3 utilization. Limestone is the low cost naturally occurring chemical which is the preferred reagent in many conventional WFGD systems. However, under normal system operating conditions, the limestone dissolves slowly. Therefore, in order to increase the alkalinity of the limestone slurry used in conventional WFGD systems and hence increase the system's SO2 removal efficiency, the use of ammonium compounds as the possible additives has been examined in this study. Under normal operating conditions, once the slurry containing the dissolved limestone is sprayed into the SO2 absorber, the dissolved limestone is quickly depleted making the slurry ineffective in removing more SO2 and requiring a high rate of slurry recycle. As a result, high capital and operating costs are required when low cost limestone is employed as the reagent in WFGD systems. Increasing the limestone dissolution rate in WFGD systems allows courser limestone particles; lower limestone stoichiometry and lower slurry recycle rates to be employed, thereby saving capital and operating costs. Marginal grade limestone samples collected from Tirunelveli district, Tamil Nadu have been taken up for this particular study under conditions similar to those encountered in wet FGD processes.

 

KEYWORDS: Limestone, local source, dissolution, Desulphurization, IndustryAuthor for Correspondence

 


 

INTRODUCTION:

The rocks occurring in southern district of Tamil Nadu comprises of Charnockite, Garnetiferous Biotite Gneiss of Archaean and coastal sedimentary rocks. Due to intense metamorphism coupled with intrusive activities, the formation seen as heterogeneous assemblages of metamorphic facies has developed. The arenaceous facies are represented by quartzite and garnetiferous gneiss1. Argillaceous facies are represented by calcgneisses and calcareous facies are represented by crystalline limestone respectively. These rocks are generally termed as granulite group of rocks. There are some small pockets of shell limestone, Kankar and calcareous sandstone of tertiary age occurring in the coastal regions of Tuticorin, Kanyakumari and Tirunelveli districts

 

Although most of the limestones are similar in chemical and mineralogical composition, the complex organic and chemical origins of carbonate sediments lead to a wide range of textures and fabrics finding wide application in Industrial fields in the resulting limestones

 

Limestone is a low cost naturally occurring chemical which is the preferred reagent in many conventional WFGD systems. However, under normal system operating conditions, the limestone dissolves slowly. Therefore, in order to increase the alkalinities of the limestone slurry used in conventional WFGD systems, system's SO2 removal efficiency is to be enhanced. Once the slurry containing the dissolved limestone is sprayed into the SO2 absorber, the dissolved limestone is quickly depleted making the slurry ineffective in removing more SO2 and requiring a high rate of slurry recycle. As a result, high capital and operating costs are required when low cost limestone is employed as the reagent in WFGD systems.Timckeener2 et al have studied the limestone dissolution rate by changing the variables such as PH, Temperature, Particle size etc..

 

The rate of CaCO3 dissolution in slurry scrubbers for flue gas desulphurization affects SO2 absorption, CaSO3/CaSO4 scaling, and ultimate CaCO3 utilization. The dissolution rates of limestone could become a critical limiting step for desulphurization. Increasing the limestone dissolution rate for limestone-containing slurries used in WFGD systems allows courser limestone particles; lower limestone stiochiometry and lower slurry recycle rates to be employed, thereby saving capital and operating costs. Robert S.Boynton3, has reported that most inorganic salts increase the Ca (OH)2 solubility by 10-15 % in 0.1-0.2%  salt solutions.

 

The performance-enhancing additive that is incorporated in the limestone slurry in the WFGD system according to this study is a source of water soluble ammonium ions. The dissolution characteristics have been studied by using a pH-Stat method at 25°C, at pH value of 5, stirrer speed of 300 rpm and particle size of 150 microns 61 limestone Samples prepared in the sample size of 150 microns selected from Tirunelveli district of Tamil Nadu were taken up for the dissolution study

 

MATERIALS AND METHODS:

Apparatus:

A top loading stirrer motor driven with rpm indicator, a reaction vessel,   Solutions prepared using Analar standards, pH meter

 

Procedure:

0.75 gm of the sample was taken and 500ml of water added to it and kept for dissolution at 25*c with a disk rotation speed 300 rpm using a motor driven hanging stirrer. The ammonium ions incorporated into the solution through aqueous ammonia and water-soluble ammonium salts, such as ammonium sulfate, ammonium chloride, or ammonium carbonate. It was found that the dissolution rate was dependant on the disk rotating speed when the rotating speed was below 300 rpm when the rotating speed was greater than 300 rpm the lime dissolution become constant. After the suspension pH attained its equilibrium value close to 9 in around 5 min, a solution of pH54which is a typical pH value in industrial slurry scrubbers, was added 25ml of   the aqueous ammonia 25%, and allowed for dissolution for 25 minutes and after checking the pH of the solution another increment of aqueous ammonia 25% has been added and the dissolution rate monitored. This time period choice is made with the consideration that initially the stirrer surface may have not been smooth and free of dust which can make the initial dissolution rate slightly greater and that with time elapse the solution may have a high ion concentration which may result in some deposition on the surface to make the dissolution rate decrease. The solution was allowed to settle and filtered through Whatmann40 filter paper with hot water washings, dried and ignited at 900*c. Percentage dissolution of the sample has been calculated.

 

Similar experiments carried out with water-soluble ammonium salts, such as Ammonium sulfate2%, Ammonium chloride 3%, Ammonium chloride 1.5% or Ammonium Nitrate 1.5% in increments of 50 ml at constant intervals twice with uniform stirring and with periodical checking of the pH values. The variations were observed with all the 61 samples taken up for the study. The pH was automatically controlled to ±0.1 units. The experiment   conducted for twenty five minutes, the period choice was made with the consideration that with time lapse the solution may have a high ion concentration which may result in some deposition on the surface to make the dissolution rate decrease. The consumption rate considered between 15 to 20 minutes. The solution was allowed to settle and filtered through whatmann40 filter paper with hot water washings, dried and ignited at 900*c. Percentage dissolution of the sample has been calculated. A set of 61 samples of present zone of interest have been taken up for the study.

 

RESULTS AND DISCUSSION

Ammonium chloride solution of 1.5% increased the dissolution rate by 20% at 25*c but addition of a solution of aqueous Ammonia 25 % decreased the dissolution rate considerably under similar conditions. Experiments done with Ammonium chloride solution of 3% increased the dissolution slightly. Addition of Ammonium sulphate solution of 2% has been found to enhance the dissolution by 2.5%. Addition of Ammonium nitrate solution of 1.5%% has been found to enhance the dissolution by about 25%. As could be seen from the results the dissolution rate is enhanced by the addition of ammonium ions (Table-1).

 

A series of experiments have been conducted with variations  in addition of water soluble ammonium compounds as additives to test the lime dissolution rate under similar conditions keeping the variables such as  pH, Temperature, and Particle size etc., constant (Table-1).

 

It could be seen from the results that Ammonium chloride has the ability to increase the dissolution rate This phenomenon was first considered a chemical reaction but the activation energy calculated from further tests on dissolution have that ammonium chloride in some way accelerates the mass transfer process indicated dissolution rate to a greater extent. The other Ammonium com pound, Ammonium sulphate 2% improved the limestone dissolution   slightly. Ammonium nitrate 1.5% has been found to enhance the dissolution by about 25%. A change in the concentration of Ammonium chloride improved the dissolution (Table-1).

 

Hillary Ruttol et al5 have reported that upon addition of 0.5 g of ammonium nitrate, the dissolution rate constants increased by 170%. A series of experiments have been conducted to test the lime dissolution rate. Except for the initial stages during which the suspension pH came down to the constant pH of dissolution (pH 5) from its natural pH 9, the conversion varied linearly with time This is probably due to the fact that the lime rotating stirrer is a surface source for dissolution while the limestone particles are well mixed in the solution and it is easier for the system to maintain a uniform pH value (Table-1).

 

 

Table-1


EFFECT OF ADDITIVES

Particle size

150 MICRONS

 

 

 

 

Duration of mixing

2 HOURS

pH

5.00

 

 

 

 

Temperature

25*C

Effect of ammonium compounds

Sl no

%Ca

TCO3

PH5

Ammonia aq 25%

Ammo. chloride 1.5%

Ammo.chloride3%

Ammo. sulphate 2%

Ammonium nitrate

1.5%

Residue wt

% dissolution

Residue wt

% dissolution

Residue wt

% dissolution

Residue wt

% dissolution

Residue wt

% dissolution

Residue wt

% dissolution

1

47.81

81.59

0.3324

55.68

0.5393

28.09

0.2020

73.07

0.2011

73.19

0.3144

58.08

0.1810

75.87

2

46.86

82.76

0.3331

55.59

0.5400

28.00

0.2027

72.97

0.2018

73.09

0.3151

57.99

0.1817

75.77

3

50.39

92.63

0.3071

59.05

0.5140

31.47

0.1767

76.44

0.1758

76.56

0.2891

61.45

0.1557

79.24

4

46.01

84.08

0.3789

49.48

0.5858

21.89

0.2485

66.87

0.2476

66.99

0.3609

51.88

0.2275

69.67

5

46.54

81.03

0.3792

49.44

0.5861

21.85

0.2488

66.83

0.2479

66.95

0.3612

51.84

0.2278

69.63

6

49.82

74.03

0.3302

55.97

0.5371

28.39

0.1998

73.36

0.1989

73.48

0.3122

58.37

0.1788

76.16

7

53.81

88.72

0.2924

61.01

0.4993

33.43

0.1620

78.40

0.1611

78.52

0.2744

63.41

0.1410

81.20

8

51.91

93.92

0.2444

67.41

0.4513

39.83

0.1140

84.80

0.1131

84.92

0.2264

69.81

0.0930

87.60

9

52.11

87.42

0.2912

61.17

0.4981

33.59

0.1608

78.56

0.1599

78.68

0.2732

63.57

0.1398

81.36

10

52.22

86.33

0.2907

61.24

0.4976

33.65

0.1603

78.63

0.1594

78.75

0.2727

63.64

0.1393

81.43

11

52.72

88.43

0.2899

61.35

0.4968

33.76

0.1595

78.73

0.1586

78.85

0.2719

63.75

0.1385

81.53

12

52.05

85.83

0.2843

62.09

0.4912

34.51

0.1539

79.48

0.153

79.60

0.2663

64.49

0.1329

82.28

13

48.82

93.96

0.3501

53.32

0.5570

25.73

0.2197

70.71

0.2188

70.83

0.3321

55.72

0.1987

73.51

14

45.59

87.37

0.3723

50.36

0.5792

22.77

0.2419

67.75

0.241

67.87

0.3543

52.76

0.2209

70.55

15

48.56

84.05

0.3304

55.95

0.5373

28.36

0.2000

73.33

0.1991

73.45

0.3124

58.35

0.1790

76.13

16

46.49

80.98

0.3707

50.57

0.5776

22.99

0.2403

67.96

0.2394

68.08

0.3527

52.97

0.2193

70.76

17

48.84

85.21

0.3498

53.36

0.5567

25.77

0.2194

70.75

0.2185

70.87

0.3318

55.76

0.1984

73.55

18

47.06

71.74

0.3572

52.37

0.5641

24.79

0.2268

69.76

0.2259

69.88

0.3392

54.77

0.2058

72.56

19

47.45

90.81

0.3314

55.81

0.5383

28.23

0.2010

73.20

0.2001

73.32

0.3134

58.21

0.1800

76.00

20

46.83

88.21

0.3361

55.19

0.5430

27.60

0.2057

72.57

0.2048

72.69

0.3181

57.59

0.1847

75.37

21

41.29

84.10

0.2912

61.17

0.4981

33.59

0.1608

78.56

0.1599

78.68

0.2732

63.57

0.1398

81.36

22

39.15

83.90

0.2903

61.29

0.4972

33.71

0.1599

78.68

0.159

78.80

0.2723

63.69

0.1389

81.48

23

48.83

83.70

0.2102

71.97

0.5958

20.56

0.0798

89.36

0.0789

89.48

0.1922

74.37

0.0588

92.16

24

44.20

81.28

0.3615

51.80

0.5684

24.21

0.2311

69.19

0.2302

69.31

0.3435

54.20

0.2101

71.99

25

48.84

78.82

0.3098

58.69

0.5167

31.11

0.1794

76.08

0.1785

76.20

0.2918

61.09

0.1584

78.88

26

50.91

93.03

0.3002

59.97

0.5071

32.39

0.1698

77.36

0.1689

77.48

0.2822

62.37

0.1488

80.16

27

50.17

90.98

0.3015

59.80

0.5084

32.21

0.1711

77.19

0.1702

77.31

0.2835

62.20

0.1501

79.99

28

49.00

87.85

0.3114

58.48

0.5183

30.89

0.1810

75.87

0.1801

75.99

0.2934

60.88

0.1600

78.67

29

43.84

74.10

0.3712

50.51

0.5781

22.92

0.2408

67.89

0.2399

68.01

0.3532

52.91

0.2198

70.69

30

52.39

85.26

0.2912

61.17

0.4981

33.59

0.1608

78.56

0.1599

78.68

0.2732

63.57

0.1398

81.36

31

50.73

82.05

0.3016

59.79

0.5085

32.20

0.1712

77.17

0.1703

77.29

0.2836

62.19

0.1502

79.97

32

49.36

85.61

0.3022

59.71

0.5091

32.12

0.1718

77.09

0.1709

77.21

0.2842

62.11

0.1508

79.89

33

50.84

87.33

0.3021

59.72

0.5090

32.13

0.1717

77.11

0.1708

77.23

0.2841

62.12

0.1507

79.91

34

49.07

86.04

0.3102

58.64

0.5171

31.05

0.1798

76.03

0.1789

76.15

0.2922

61.04

0.1588

78.83

35

52.33

93.33

0.3006

59.92

0.5075

32.33

0.1702

77.31

0.1693

77.43

0.2826

62.32

0.1492

80.11

36

49.59

89.23

0.3112

58.51

0.5181

30.92

0.1808

75.89

0.1799

76.01

0.2932

60.91

0.1598

78.69

37

48.22

90.18

0.3204

57.28

0.5273

29.69

0.1900

74.67

0.1891

74.79

0.3024

59.68

0.1690

77.47

38

51.78

88.50

0.3010

59.87

0.5079

32.28

0.1706

77.25

0.1697

77.37

0.2830

62.27

0.1496

80.05

39

45.72

85.32

0.3612

51.84

0.5681

24.25

0.2308

69.23

0.2299

69.35

0.3432

54.24

0.2098

72.03

40

50.52

87.45

0.2021

73.05

0.4090

45.47

0.0717

90.44

0.0708

90.56

0.1841

75.45

0.0507

93.24

41

54.58

91.10

0.2101

71.99

0.4170

44.40

0.0797

89.37

0.0788

89.49

0.1921

74.39

0.0587

92.17

42

49.43

90.66

0.3021

59.72

0.5090

32.13

0.1717

77.11

0.1708

77.23

0.2841

62.12

0.1507

79.91

43

47.56

88.02

0.3372

55.04

0.5441

27.45

0.2068

72.43

0.2059

72.55

0.3192

57.44

0.1858

75.23

44

48.49

89.13

0.3659

51.21

0.5728

23.63

0.2355

68.60

0.2346

68.72

0.3479

53.61

0.2145

71.40

45

53.16

91.15

0.2144

71.41

0.4213

43.83

0.0840

88.80

0.0831

88.92

0.1964

73.81

0.0630

91.60

46

42.91

81.25

0.3748

50.03

0.5817

22.44

0.2444

67.41

0.2435

67.53

0.3568

52.43

0.2234

70.21

47

38.86

81.35

0.5517

26.44

0.6175

17.67

0.4213

43.83

0.4204

43.95

0.5337

28.84

0.4003

46.63

48

45.48

82.79

0.2235

70.20

0.4304

42.61

0.0931

87.59

0.0922

87.71

0.2055

72.60

0.0721

90.39

49

44.61

82.53

0.3007

59.91

0.5076

32.32

0.1703

77.29

0.1694

77.41

0.2827

62.31

0.1493

80.09

50

47.69

83.03

0.3010

59.87

0.5079

32.28

0.1706

77.25

0.1697

77.37

0.2830

62.27

0.1496

80.05

51

51.76

86.27

0.2491

66.79

0.4560

39.20

0.1187

84.17

0.1178

84.29

0.2311

69.19

0.0977

86.97

52

39.74

81.30

0.5317

29.11

0.6386

14.85

0.4013

46.49

0.4004

46.61

0.5137

31.51

0.3803

49.29

53

49.66

87.36

0.2512

66.51

0.4581

38.92

0.1208

83.89

0.1199

84.01

0.2332

68.91

0.0998

86.69

54

49.20

80.56

0.2499

66.68

0.4568

39.09

0.1195

84.07

0.1186

84.19

0.2319

69.08

0.0985

86.87

55

49.73

80.65

0.2412

67.84

0.4481

40.25

0.1108

85.23

0.1099

85.35

0.2232

70.24

0.0898

88.03

56

51.85

89.96

0.2136

71.52

0.4205

43.93

0.0832

88.91

0.0823

89.03

0.1956

73.92

0.0622

91.71

57

52.77

92.99

0.2009

73.21

0.4200

44.00

0.0705

90.60

0.0696

90.72

0.1829

75.61

0.0495

93.40

58

44.99

81.20

0.3012

59.84

0.5081

32.25

0.1708

77.23

0.1699

77.35

0.2832

62.24

0.1498

80.03

59

48.18

82.10

0.3201

57.32

0.5270

29.73

0.1897

74.71

0.1888

74.83

0.3021

59.72

0.1687

77.51

60

47.23

83.10

0.3211

57.19

0.5280

29.60

0.1907

74.57

0.1898

74.69

0.3031

59.59

0.1697

77.37

61

47.30

80.77

0.3204

57.28

0.5273

29.69

0.1900

74.67

0.1891

74.79

0.3024

59.68

0.1690

77.47

 


 

Fig 1.

 

 


Berner, A.R. and J.W. Morse6 have studied the dissolution Kinetics of Calcium Carbonate in Sea Water. Gao xiang et al7 have studied the dissolution rate of limestone for flue wet gas desulphurization in the presence of sulphite. Ukawa, N., et al8 have reported effects of Salts on limestone dissolution Rate in wet Limestone .Flue Gas Desulfurization". Optimisation of a wet FGD pilot plant using fine limestone and organic acids has been studied by Jan B.W. Frandsen,Søren Kiil and Jan Erik Johnson9. Dissolution of Limestone in Simulated slurries for removal of Sulfur Dioxide from Stack Gases10 has been taken up for studies by Kim, K.Y., M.E. Deming et al Samples collected from certain areas of Pillaiyanatham village in Sankarankoil taluk, Tirunelveli district showed to be of more industrial utility and the dissolution rate in the presence of additives has been found to be 55-67% Samples collected from certain Karanthaneri, Venkatrangapuram, Kilasadaiyamankulam, Gangainadankulam showed calcium content ranging from the dissolution percentage has been found to be 65-75% suitable for FGD purpose. In the Samples of Nanguneri Taluks Tirunelveli district the dissolution rate has been found to be 65-85% suitable for FGD purpose. Samples from Venkatrangapuram, Karisalapatti, Pillaikulam, Ganganarkulam and Pattankadu villages of Ambasamudram taluk, Tirunelveli district the dissolution has been found to be 51-73 % .The samples collected from these areas could be useful for FGD systems with addition of ammonium compounds in suitable concentrations.

Under normal system operating conditions, the limestone dissolves slowly. Under similar operating conditions SO2 removal efficiency is higher when additives are added to the system along with lime stones. These additives are relatively inexpensive, tend not to oxidize and could be recovered from waste water. Such additives have been reported to improve system performance by buffering the slurry pH and improving its effectiveness. The performance enhancement that is achieved in many cases is of a sufficient magnitude. The limestone dissolution rate for limestone-containing slurries used in wet flue gas desulfurization (WFGD) systems is enhanced by the addition of ammonium ions.

 

Patent of Gal, Eli11 states that the performance-enhancing additive that had been incorporated in the limestone slurry in the WFGD system according to their invention was a source of ammonium ions. The impact of dissolved ammonium ions on the limestone dissolution rate has been indicated by the dissolution rate curves., With no chlorides present, the dissolution rate has been reported to increase from 14.6 mmole/h/g to 127 mmole/h/g when 1000 ppm ammonium ions (as ammonium sulfate) are added to the slurry. The rate increases to 197 and 286 mmole/h/g when 3090 ppm and 6440 ppm ammonium ions are used, respectively. With 50,000 ppm chlorides, the dissolution rate is only 8.8 mmole/h/g, but increases five-fold to 42.4 mmole /h/g with 6440 ppm ammonium ions in the solution.

The limestone dissolution rate for limestone-containing slurries used in wet flue gas desulfurization (WFGD) systems is enhanced by the addition of ammonium ions11

 

Increasing the limestone dissolution rate (Fig.1) for limestone-containing slurries used in WFGD systems allows courser limestone particles; lower limestone stoichiometry and lower slurry recycle rates to be employed, thereby saving capital and operating costs. The ammonium ions may be recovered and reused in the process. It is imperative that much research and development programme should be undertaken for the proper utilization of existing marginal grade   limestone deposits. Since many of the applications have either not developed or only established to a small extent, there is a tremendous scope. To mitigate this adverse effect of reduced availability, focused efforts are required for proper utilization of marginal grade limestone for different industrial purposes.

 

A careful search for the new deposits adopting modern methods of prospecting and exploration is essential. After fixing the new finds, they may be sorted according to their suitability for the different industries; the recent technological innovations the world over have also provided ways and means of utilizing relatively impure varieties of limestone to lead to a better method of predicting and optimizing the performance for FGD. It would especially be desirable if the capital and operating costs of limestone-based WFGD systems could be reduced by the use of a low cost recoverable additive while at the same time, achieving significantly increased limestone dissolution rates and hence increased SO2 removal efficiency. It is towards providing such performance-enhanced limestone-based WFGD systems that the present study is focused.

 

It has been proposed to  do further study on the effect of  other additives on the dissolution rate of the limestone samples from Tjrunelveli district. Tamil Nadu, India with the intention of increasing the utility level of  the marginal grade limestones available in the present zone of study for FGD purposes.

 

ACKNOWLEDGEMENT:

The author expresses her sincere thanks to the Commissioner of Geology and Mining, Guindy, Chennai.600 032 for the encouragement throughout this work.

 

REFERENCES:

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9.       Jan B.W. Frandsen, Søren Kiil and Jan Erik Johnson. Optimisation of a wet  FGD pilot plant using fine limestone and organic acids, Chemical Engineering Science: May 2001: 56(!0): 3275-3287

10.     Kim, K.Y., M.E. Deming, and J.D. Hatfield, Dissolution of Limestone in Simulated Slurries for Removal of Sulfur Dioxide from Stack Gases: Env. Sci. Tech. 1975: 9(10), 949-52.

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Received on 21.05.2010        Modified on 12.06.2010

Accepted on 24.06.2010        © AJRC All right reserved

Asian J. Research Chem. 3(4): Oct. - Dec. 2010; Page 990-994