The essential oil and its main constituents of Origanum syriacum ssp. sinaicum grown wild in Saint Katherine Protectorate, South Sinai, Egypt

Document Type : Original Article

Authors

1 Department of Environment and Bio-Agriculture, Faculty of Agriculture, Al-Azhar University, Cairo, Egypt

2 Egyptian Environmental Affairs Agency (EEAA), Ministry of Environment, Cairo, Egypt

3 Department of Medicinal and Aromatic Plants Research, National research Centre, Dokki, Cairo, Egypt

Abstract

This work aims to study the essential oil and its main constituents of O. syriacum grown wild in 22 locations in Saint Katherine Protectorate. Origanum syriacum ssp. sinaicum plants collected during the summer season of 2014 from 22 locations in Saint Katherine Protectorate (SPK), South Sinai Egypt. Depending on location length, each location was divided into 2 stands to reach a total of 44 stands. Twenty compounds were identified as the main constituents of the essential oil which accounted for ca 97% from the total compounds of the essential oil. Carvacrol was the major constituent in all collected plants and ranged from 74.2% to 92.68% from the total compounds of the essential oil. Where, P-cymene was identified in the essential oil of all studied stands and ranged for 0.98% to 6.23%. The same was observed for γ-terpinene that was identified in the essential oil of all plants in the 44 stands and accounted for 1.37% as minimum percent up to 7.4% as maximum percent from the total compounds. The oxygenated compounds in the essential oilof O. syriacum were identified as carvacrol, terpienol-4, linalool, borneol, thymol, eugenol, and long pineneepoxid with relative percentage from 76.6%to 94.2%. The non-oxygenated compounds hydrocarbons ranged from 3.7% to18.4% in which P–cymene and ɣ-terpinene were the main non-oxygenated compounds. The relations between the essential oil%, as well as between carvacrol% in the essential oil in the different stands and calcium content, Cl and Na in the soil of the different stands were studied. In conclusion, the essential oil % of O. syriacum ssp. sinaicum and its main constituents changed according to the altitude and soil contents.

Keywords


INTRODUCTION

Medicinal plants and culinary herbs have long been known as one of the basis of traditional medicine in many countries such as Egypt. Some important medicinal wild plants suffered from unwise human manipulation which resulted in the extinction of some species. Projects to recover the genetic diversity of wild plants were carried out in Egypt accompanied with scientific research to evaluate their use based on traditional medicine in Bedouin communities. Indeed, there are a great number of rural jobs dependent on this sector (Viuda-Martos et al., 2010, 2011). Origanum syriacum. ssp. sinaicum (Boiss.) family Labiatae is a rare perennial wild herb endemic to Sinai. O. syriacum is represented by the following three varieties: ssp. syriacum, distribution Palestinian, Jordon, Syria; ssp. bevanii, Turkey, Syria, Lebanon, Cyprus; ssp. sinaicum is cultivated in Northern Sinai in Egypt and Palestinian. The plant was described by Ietswaat in his treatise on the taxonomy of the genus Origanum (Başer et al., 2003). The herbal parts of Origanum species were used by local people for herbal tea and as a spice in soups, salads, olives and meats. The remaining water after the plant water distillation is used orally to reduce cholesterol and glucose levels as well as to treat cancer (Kizil et al., 2008). It is also used as stimulant, analgesic, antitussive, expectorant, sedative, anti-parasitic and anti-helminthic (Dundar et al., 2008). Tepe et al., (2004) found that the plant's essential oil of O. syriacum could be used as a natural preservative in the food industry. Kamel et al., (2001), reported that Origanum plants have many different uses such as powerful disinfectants, flavoring agents, in perfumes and in scenting soaps. Some studies suggested that Origanum may have antioxidant effects which may be due to the oil components of some of the active substances, such as phenols carvacrol and thymol (Baricevic and Bartol, 2002). On the other hand, Sokovic et al., (2007), found that Origanum plant is a good source of antimicrobial compounds. Kalemba and Kunicka, (2003), indicated that this plant was used in ancient times as a natural food preservative and as a flavoring agent. Owlia et al., (2009), found that this plant was successful treatment of infectious diseases.Tackholm (1974)recorded that the Origanum syriacum plant was growing wild in the Sinai Desert of Egypt. Carvacrol and/or thymol represent the major constituents of Origanum essential oil (Sarer et al. 1982, Skoula and Harborne, 2002, Loizzo et al., 2009; Zein et al., 2011). The oil quality is determined by its composition, which varies with genotype, plant development, climate, and soil type (Russo et al., 1998; Baydar et al., 2004). Elgindy et al. (2015) identified 46 compounds in the essential oil of Origanum syriacum plants which collected from Sinai, Egypt. They reported that Carvacrol was dominated in cultivated plants, while thymol, γ-terpinene, linalool and 4-terpineol were dominated in the wild plants. Shalaby et al., (2011), reported the high potentials of O. syriacum var. sinaicum plant as new crop in Egypt. Therefore, this work aims to study the essential oil and its main constituents of O. syriacum grown wild in 22 locations in Saint Katherine Protectorate, South Sinai, Egypt.

MATERIALS AND METHODS

Plant Materials:

Origanum syriacum plants were collected from 22 locations in Saint Katherine Protectorate (SKP), South Sinai, Egypt which includes Frosh, Wadis and Gorge systems during summer season (June) of 2014. Depending on location length, each location was divided into stands in total 44 stands. The geographical (latitudes, longitudes and alludes) data of the different studied stands are shown in Table (1). The plant samples were collected from the aerial parts of growing plants in the same time from all the stands of the study. The plant samples were separately air dried in the shades till the weight was constant and then kept in paper bags and kept in desiccators till essential oil extraction.

Extraction of essential oil (EO):

The essential oil (EO) was extracted from the air-dried areal parts of O. syriacum by hydro-distillation using a Clevenger type apparatus for 3h according to Guenther (1961). The oily layer obtained on top of the aqueous distillate was separated and dried with anhydrous sodium sulfate.  The extracted EOs were kept in sealed air-tight glass vials and covered with aluminum foil at 4◦ C until GC-MS analysis.

Gas Chromatography–Mass Spectrometry (GC-MS):

The GC-MS analysis of the essential oil was carried out using Gas Chromatography-Mass Spectrometry instrument stands at the Department of Medicinal and Aromatic Plants Research, National Research Center, Egypt. Most of the compounds were identified using mass spectra of authentic chemicals (Wiley spectral library collection and NSIT library 2000). Further identifications were carried out using the MS literature data (Adams, 2004).

Soil physical analysis:

The physical properties of the soil samples that collected from all stands were analyzed to determine water, sand, silt and clay contents according to Piper (1950). From these results the soil texture of each stand was determined as shown in Table (2).

Soil chemical analysis:

Some chemical parameters i.e. pH, EC, organic matter, CaCO3, some cations (Ca, Mg, Na and K) and some anions (HCO3, Cl and SO4) were determined in the beasts of the soil samples according to Jackson (1967) and Allen et al. (1976). Oxidizable organic carbon (as indication of the total organic matter) was determined using Walkely and Black rapid titration method as described by Black (1965). The results of these parameters are shown in Table (3).

Statistical Analyses:

Data were statistically analyzed using One-way ANOVA and Post hoc-LSD tests (the least significant difference) (SPSS Inc., 2009) at 0.05, 0.01 and 0.001 level of probability (Snedecor andCochran, 1982).

RESULTS AND DISCUSSION

Data in Table (4) represents the essential oil percentage of the aerial parts of Origanum syriacum ssp. sinaicum   plants collected from the different stands which ranged from 2.25% in stand No.31 to 6.75% in stand No.1. It is clear that the minimum essential oil % was observed in the lowest altitude (1429), while the maximum % (6.75% and 6.5%) were determined in plants of the highest altitudes (2002 and 2016, respectively). Figs. (1a), (2a) and (3a) indicate the relation between essential oil % of Origanum syriacum ssp. sinaicum plants in the different stands and calcium, Cl and Na contents in the soil of the different stands. It is clear that the essential oil decreased with increasing calcium, Cl and Na contents.  The opposite trend was observed with CaCO3, in which the essential oil % increased with increasing CaCo3content of the soil (Fig., 4b). The relation between essential oil percent of O. syriacum plant sand electrical conductivity (EC) in the different stands is presented in Fig. (5a). The results indicated that essential oil %decreased with increasing level of EC. The main oil compounds are shown in Table (5). Twenty compounds were identified as the main constituents of the essential oil and accounted for ca 97% from the total compounds of the oil. Carvacrol was found to be the major compound in all collected plants from different stands and ranged from 74.2% (stand 38) to 92.68% (stand10) from the total compounds of the essential oil. P-cymene was identified in the essential oil of all studied stands and followed like carvacrol in the relative percentages, since it ranged for 0.98% (stand 10) to 6.23% (stand 38). The same was observed for γ-terpinene which was identified in the essential oil of all plants in 44 stands and accounted for 1.37% (stand 6) as minimum percent to7.4% (stand 38) as maximum percent from the total compounds. The Oxygenated compounds in the essential oil of O. syriacum ssp. sinaicum were identified as Carvacrol, Terpienol -4, α-Terpineol,Linalool, Borneol, Thymol, Euginol and Long pineneepoxidl. They accounted from 76.6 % (stand 38) to 94.2% (stand 10), while the non-oxygenated compounds ranged from 3.7% (stand 10) to18.4% (stand 38). Thymol percentage failed to reach 1% in the essential oil of all O. syriacum ssp. sinaicum in all stands, which ranged from 0.0 % (stands 2, 18, 19, 33, 37) to 0.19% (stand 11).  The maximum values of carvacrol (92.68., 91.74, and 91.41) were found in plants at the stands of Shak Musa 1, Wadi al-shak1 and Farsh Al-romana, respectively as shown in Table (5). While, the lowest percentage of carvacrol values (74.21, 79.68 and 79.86.) were found in stands at Wadi elarbain1, Taupq, and Seleebat, respectively.

Carvacrol % in the essential oil increased with increasing soil calcium content, Cl and Na in the different stands to reach its maximum values with 8-12meq, 60meq/and 175 pp, respectively as shown in Figs. (1b, 2b, 3b). On the other hand, carvacrol percent decreased with increasing CaCO3 in the soil (Fig., 4b). Carvacrol increased with increasing EC values up to 3 then tended to decrease (Fig 5b). The essential oils composition depends on many factors such as climate, geographical location and vegetative stage (Abu Lafi et al., 2007, 2008; Baser et al., 2003and Lukas et al., 2009). Baydar et al., (2004), concluded that oil quality is determined by its composition, which varies with genotype, plant development, climate, and soil type. Sangwan et al., (2001), reported that, there are many factors influence the essential oil composition such as plant ontogeny, site of oil production, photosynthesis, light quality, seasonal and climatic variations, nutritional relationships, plant growth regulators, plant density, moisture, salinity, temperature and harvesting methods, seasonal and climate conditions such as temperature and rainfall, and thus the seasonal variation of the main essential oil components have great impact. Skoula and Harborne (2002), indicated that the essential oil of Origanum is contains of carvacrol and/or thymol as major components, followed by γ-terpinene, p-cymene, linalool, terpinen-4-ol and sabinene hydrate. Russo et al., (1998), found another chemo type between thymol and carvacrol which contains a high content of γ-terpinene or p-cymene. Shalaby et al., (2011), reported that the major constituents in the essential oil of O. syriacum var. sinaicum were dominated by thymol, γ-terpinene and p-cymene. Some studies indicate that the main component of O. syriacum oil differs according to the growing season (Soliman et al., 2007), which found carvacrol was the major component in summer season while thymol was the major component in autumn. On the other hand, Toncer et al. (2010) found that, the carvacrol levels varied from 0.73-8.9%, peaked in August (8.9%) and July (8.8%) and was low in January (0.73%). Also, some components such as α-pinene and β-caryophyllene decreased in winter months however terpinen-4-ol showed the opposite trend and increased in winter. Zein et al. (2011), also noticed a difference in the components of essential oil according to the different growing season, he reported that the thymol and carvacrol increased progressively from February to April, then, decreased in May. Our previous study shows comparative results, where the poor content of thymol and carvacrol in February and March was accompanied by an increased rate of γ-terpinene and p-cymene, which they are the precursors of thymol and carvacrol. This finding may help researchers and farmers about the optimal harvesting time, allowing yielding oil with high content of thymol and carvacrol. The optimal harvesting time was in April just before flowering. In this study, thymo quinone was detected as a trace amount only in samples harvested in February. This promising anticancer molecule was found in essential oil of O. syriacum in previous studies. Thymol, p-cymene, α-terpinene, γ-terpinene, carvacrol were found to be the major components in the oil, since monoterpenes, thymol, p-cymene and γ-terpinene, are biosynthetically related (Muller-Riebau et al., 1997). But the quantitative composition of the essential oil was changed during the 11-month sampling period. Thymol (25.3%) was the major component in summer and autumn plants, while p-cymene was a major component in the winter oils (Toncer et al., 2010).


 

CONCLUSION

Origanum syriacum ssp. sinaicum grown wild in Saint Kathrin Protectorate, South Sinai, Egypt is a Carvacrol chemo type since the major component in its essential oil was carvacrol. The essential oil % of O. syriacum ssp. sinaicum and its main constituents changed according to the altitude and soil contents. No considerable differences were observed for the effect of soil texture neither on essential oil % nor on carvacrol %.

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Table 1. The geographical data (latitudes, longitudes and alludes) of different studied stands in SPK, south Sinai Egypt during June of 2014.

No. of location

Location name

Stands No.

Stands name

E

N

Alt

1

Frosh jabal mousa

1

Farsh al-lozaa-1

33.97037

28.54838

2002

2

Farsh al-lozaa-2

33:96912

28.54906

2016

3

Farsh al-lozaa-3

33.97092

28.54835

1995

4

Farsh al-lozaa-4

33.97164

28.54843

1992

5

Farsh al-sofsafa

33.96465

28.55447

1993

2

Wadi egebal

6

Farsh al-romana-1

33.8826

28.35989

1801

7

Farsh al- romana-2

33.88369

28.53947

1801

3

Shak graginiah

8

Graginiah-1

33.9695

28.52221

1980

9

Graginiah-2

33.97019

28.5235

1890

10

Graginiah-3

33.96853

28.51985

1857

4

Shak mousa

11

Shak mousa-1

33.96383

28.53001

1961

12

Shak mousa-2

33.96734

28.53342

1976

5

Wadi al-arbain

13

Wadi al-arbain -1

33.96139

28. 53936

1726

14

Wadi al-arbain-2

33.96139

28.554026

1720

15

Wadi al-arbain-3

33.85895

28. 54073

1731

6

Wadi al-shak

16

Wadi al-shak-1

33. 93365

28.53454

1855

17

Wadi al-shak-2

33.93315-

28.5365

1844

18

Wadi al-shak-1

33. 93257

28. 53860

1828

7

Wadi itlah

19

Wadi itlah-1

33.9226

28.58395

1429

20

Wadi itlah-2

33:92565

28.57904

1429

21

Wadi itlah-3

33.93108

28.57148

1468

8

 

 

 

 

 

 

Maen al-raian

22

Maen al-raian-1

33.88637

28.53771

1811

23

Maen al-raian-2

33.84194

28.54008

1834

24

Maen al-raian-3

33.89539

28.5423

1861

9

Abu kasaba

25

Abu kasaba-1

33.89073

28.52291

1854

26

Abu kasaba-2

33.88952

28.52474

1850

`10

Abu towatah

27

Abu towatah-1

33.89023

28.572827

1800

28

Abu towatah-2

33.89052

28.57717

1808

11

Abu walia

29

Abu walia-1

33.40772

28.53904

1921

30

Abu walia-2

33.90899

28.53624

1902

12

Wadi al-Talah

31

Wadi al-talah-1

33.9226

28.58395

1429

32

Wadi al-talah-2

33:92565

28.57904

1451

33

Wadi al-talah-3

33.93108

28.57148

1479

13

Tunea elkalabia

34

Tunea elkalabia

33.90809

28.56388

1850

14

Shak tunea

35

Shak tunea

33.90157

28.57951

1766

15

Tobok

36

Tobok

33.93287

28.54076

1825

16

Shakef tobok

37

Shakef tobok

33.93272

28.54271

1842

17

Taupq

38

Taupq

33.87923

28:55097

1804

18

Meslh

39

Mesalh

33.88888-

28.27527

1804

40

Nakp mesalh

33.87785

28.56882

1853

19

Shake saker

41

Shake saker

33.90013

28.57801

1779

20

Sakarkiah

42

Sakarkiah

33.91119

28.55866

1540

21

Naqb al-zawateen

43

Naqb al-zawateen

33.9338

28.54524

1882

22

Seleebat

44

Seleebat

33.92359

28.54021

1882

 


 

Table 2. Soil Physical properties of different Stands in SPK, south Sinai Egypt during June of 2014.

No.

Stand name

Texture %

Texture

Water content

Fine grave

Coarse sand

fine sand

Silt

clay

1

Farsh al-lozaa-1

1.4

20

59

11

6

4

loamy sand

2

Farsh al-lozaa-2

1.09

37

50

5

4

4

loamy sand

3

Farsh al-lozaa-3

1.95

16

50

12

12

10

sandy loam

4

Farsh al-lozaa-4

1.2

31

46

7

10

6

sandy loam

5

Farsh al-sofsafa

1.07

15

44

15

15

11

sandy loam

6

Farsh al-romana-1

1.7

2

88

8

1

1

Sand

7

Farsh al-romana-2

1.9

21

72

5

1

1

Sand

8

Graginiah-1

0.64

35

45

6

6

8

sandy loam

9

Graginiah-2

0.8

13

45

10

15

17

sandy loam

10

Graginiah-3

0.5

12

56

12

8

12

sandy loam

11

Shak muosa-1

1.7

26

55

8

5

6

loamy sand

12

Shak muosa-2

1.65

10

34

9

7

40

sandy clay

13

Wadi elarbain-1

1.54

23

45

10

12

10

sandy loam

14

Wadi elarbain-2

0.96

22

52

10

8

8

sandy loam

15

Wadi elarbain-3

1.8

15

50

12

12

11

loamy sand

16

Wadi al-shak-1

1.2

30

50

5

9

6

sandy loam

17

Wadi al-shak-2

1.32

30

54

7

6

3

loamy sand

18

Wadi al-shak-3

1.52

12

55

13

11

9

sandy loam

19

Wadi itlah-1

1.46

26

45

9

10

10

sandy loam

20

Wadi itlah-2

1.65

21

65

9

4

1

Sand

21

Wadi itlah-3

1.8

10

42

17

22

9

sandy loam

22

Maen al-raian-1

1.68

25

67

5

2

1

Sand

23

Maen al-raian-2

1.78

7

35

18

25

15

sandy loam

24

Maen al-raian-3

1.46

19

65

9

5

2

Sand

25

Abu kasaba-1

1.2

16

66

7

7

4

loamy sand

26

Abu kasaba-2

1.12

24

62

9

2

3

Sand

27

Abu towatah-1

1.42

25

50

11

9

5

loamy sand

28

Abu towatah-2

1.7

31

60

6

2

1

Sand

29

Abu walia-1

1.67

19

38

11

14

18

sandy clay loama

30

Abu walia-2

1.32

16

67

8

6

3

Sand

31

Wadi al-Talah-1

1.46

13

54

17

11

5

loamy sand

32

Wadi al-talah-2

1.6

22

48

11

12

7

sandy loam

33

Wadi al-talah-3

1.9

13

44

17

18

8

sandy loam

34

Tunea elkalabia

1.14

24

62

6

5

3

Sand

35

Shak tunea

1.3

15

60

13

5

7

loamy sand

36

Tobok

0.5

35

44

8

7

6

loamy sand

37

Shakef tobok

0.6

9

53

15

13

10

sandy loam

38

Taupq

0.76

48

37

4

5

6

sandy loam

39

Shakef meslh

1.82

42

54

2

1

1

Sand

40

Nakp mesalh

0.8

13

48

17

16

6

sandy loam

41

Shakef saker

1.42

16

67

9

5

3

Sand

42

Sakarkiah

1.12

25

51

8

6

10

sandy loam

43

Naqb al-zawateen

1.2

2

91

1

4

2

Sand

44

Seleebat

0.64

16

59

12

7

6

loamy sand

LSD at (0.05)

0.17

6.87

6.87

3.42

2.98

2.90

 

LSD at (0.01)

0.23

8.16

9.11

4.54

3.95

3.85

 

 

 

Table 3. Soil chemical properties of different stands in SPK, south Sinai Egypt during June of 2014.

No.

Stand name

pH

T.D.S ppm

EC us/cm

Org. matter %

CaCo3 %

Cations

Anions (meq/L)

++Ca

    meq/L

++Mg

 meq/L

Na++

    PPM

+k

PPM

HCO3 -

Cl -

SO4 -

1

Farsh al-lozaa-1

8.10

72.00

111.67

2.99

27.00

1.33

4.17

6.05

9.12

5.00

21.47

20.33

2

Farsh al-lozaa-2

7.87

113.00

176.67

1.84

23.17

2.33

5.50

6.80

5.70

5.00

37.33

41.00

3

Farsh al-lozaa-3

8.47

53.00

83.33

4.00

23.17

1.33

2.50

3.00

5.88

5.00

48.53

50.67

4

Farsh al-lozaa-4

8.70

69.00

106.67

3.27

25.50

1.33

4.83

4.63

6.68

5.00

24.73

77.67

5

Farsh al-sofsafa

7.90

116.33

180.00

2.07

28.83

6.33

5.17

5.88

4.23

5.00

44.80

15.67

6

Farsh al-romana-1

8.73

67.67

103.33

7.91

25.33

2.33

0.17

3.38

8.00

5.00

27.53

47.00

7

Farsh al-romana-2

8.80

62.33

93.33

8.00

23.00

1.33

1.83

4.32

12.28

5.00

31.27

23.33

8

Graginiah-1

7.97

145.00

226.67

0.69

30.50

3.33

5.83

6.38

6.90

5.00

56.47

41.00

9

Graginiah-2

8.13

55.67

86.67

0.69

29.83

2.00

4.50

16.53

3.53

5.00

46.20

35.67

10

Graginiah-3

8.43

53.67

83.33

0.50

29.00

1.67

2.17

11.43

14.50

5.00

36.40

42.67

11

Shak muosa-1

8.07

120.00

186.67

4.30

28.17

2.33

6.17

6.13

4.50

5.00

48.07

60.67

12

Shak muosa-2

7.97

87.67

135.00

2.76

30.00

3.00

2.83

8.87

6.23

5.00

35.93

24.33

13

Wadi elarbain-1

7.73

136.67

210.00

3.45

31.00

3.67

8.17

12.40

12.58

5.00

18.67

31.00

14

Wadi elarbain-2

7.70

76.33

113.33

1.84

27.33

2.33

4.50

10.97

12.85

5.00

15.40

10.33

15

Wadi elarbain-3

7.73

73.33

106.67

4.37

29.33

3.33

6.83

7.38

6.92

5.00

19.13

11.33

16

Wadi al-shak-1

8.53

174.00

266.67

3.68

27.00

4.33

7.50

26.32

16.50

5.00

12.60

15.67

17

Wadi al-shak-2

7.73

516.67

800.00

3.22

31.83

8.67

16.50

25.58

37.40

5.00

13.53

71.00

18

Wadi al-shak-3

7.90

95.33

150.00

3.91

25.33

2.33

4.83

10.10

20.50

5.00

19.13

16.00

19

Wadi itlah-1

8.07

79.67

116.67

6.90

26.67

2.33

2.17

3.12

10.07

5.00

33.60

12.33

20

Wadi itlah-2

8.10

121.33

189.33

7.36

27.33

2.33

3.17

6.82

9.05

5.00

31.03

19.33

21

Wadi itlah-3

8.27

92.00

143.33

6.67

26.67

2.00

4.50

4.60

3.92

5.00

18.20

14.67

22

Maen al-raian-1

9.43

228.00

350.00

8.05

29.50

4.33

7.83

16.82

19.78

5.00

9.80

26.67

23

Maen al-raian-2

8.03

139.33

219.67

5.06

28.00

3.67

5.83

8.00

12.58

5.00

16.57

26.33

24

Maen al-raian-3

8.07

60.33

89.33

4.60

28.00

1.67

4.83

3.60

6.57

5.00

14.47

24.33

25

Abu kasaba-1

7.97

97.67

150.00

3.68

27.83

6.00

4.83

10.18

14.92

5.00

20.53

21.67

26

Abu kasaba-2

8.47

62.00

100.00

4.78

28.00

3.33

6.83

3.17

5.12

5.00

34.07

51.33

27

Abu towatah-1

8.37

45.67

66.67

10.58

30.00

2.00

2.83

3.33

3.32

5.00

17.27

15.00

28

Abu towatah-2

8.63

138.67

213.33

4.60

36.67

2.67

5.17

3.75

11.48

5.00

24.27

62.00

29

Abu walia-1

7.93

139.33

213.33

5.52

31.33

2.67

2.67

13.53

12.37

5.00

23.80

14.17

30

Abu walia-2

7.97

111.33

173.33

5.75

30.67

3.33

6.17

2.03

4.50

5.00

12.60

51.67

31

Wadi al-Talah-1

7.90

85.00

132.67

4.37

32.33

2.67

6.83

9.95

11.33

5.00

19.60

19.33

32

Wadi al-talah-2

8.07

74.00

106.67

5.06

28.00

2.00

2.50

5.00

7.25

5.00

21.47

19.33

33

Wadi al-talah-3

8.20

72.00

110.00

8.51

29.67

3.00

3.83

6.22

5.47

5.00

24.27

18.00

34

Tunea elkalabia

8.60

99.67

156.67

2.30

26.00

2.67

7.17

5.95

12.63

5.00

23.80

65.67

35

Shak tunea

8.77

55.67

86.67

3.31

24.83

0.33

5.83

6.97

14.20

5.00

32.20

73.33

36

Tobok

8.77

60.33

96.67

0.50

27.00

1.67

3.50

13.67

12.23

5.00

57.87

41.33

37

Shakef tobok

8.30

77.67

120.00

1.38

29.17

1.33

3.17

9.22

3.85

5.00

41.53

50.00

38

Taupq

7.97

74.67

110.00

0.92

31.25

2.83

3.33

6.17

5.62

5.00

53.67

13.33

39

Shakef meslh

8.17

53.00

80.00

4.14

29.33

1.67

6.83

7.23

2.80

5.00

18.67

11.67

40

Nakp mesalh

8.73

151.00

233.33

1.84

29.83

4.67

7.83

6.43

5.55

5.00

22.87

59.67

41

Shakef saker

7.93

73.00

113.33

4.32

23.17

0.33

4.17

4.98

9.10

5.00

35.93

29.67

42

Sakarkiah

8.30

73.67

116.67

3.63

24.33

3.00

3.17

10.63

4.90

5.00

44.33

56.00

43

Naqb al-zawateen

8.23

78.00

120.00

4.14

25.67

2.33

8.50

11.98

8.05

5.00

41.53

70.00

44

Seleebat

8.13

58.33

90.00

2.07

30.00

1.33

3.83

7.08

10.67

5.00

14.47

28.00

 

LSD at (0.05)

0.26

26.18

41.11

1.81

3.90

1.36

1.98

1.98

2,38

Ns

6.78

5.14

 

LSD at (0.01)

0.34

34.70

54.50

2.40

5.17

1.80

2.62

2.62

3.16

Ns

8.99

6.81

 


 

Table 4. Essential oil percentage of O. syriacum plants in different stands in SPK, south Sinai Egypt during June of 2014.

NO.

Stands

V. O  ml\100g

NO.

Stands

V. O  ml\100g

1

Farsh al-lozaa1

6.75

23

Maen al-raian2

5.50

2

Farsh al-lozaa2

6.50

24

Maen al-raian3

2.75

3

Farsh al-lozaa3

5.00

25

Abu kasaba1

5.00

4

Farsh al-lozaa4

3.50

26

Abu kasaba2

5.00

5

Farsh al-Sofsafa

3.50

27

Abu towatah1

4.50

6

Farsh al-romana1

4.00

28

Abu towatah2

5.25

7

Farsh al-romana2

2.50

29

Abu walia1

5.25

8

Graginiah 1

5.75

30

Abu walia2

4.50

9

Graginiah 2

3.00

31

Wadi al-Talah1

2.25

10

Graginiah 3

4.50

32

Wadi al-Talah2

5.57

11

Shak mousa1

3.25

33

Wadi al-Talah3

4.75

12

Shak mousa2

3.75

34

Tunea elkalabia

3.50

13

Wadi elarbain1

5.50

35

Shak tunea

5.00

14

Wadi elarbain2

5.25

36

Tobok

3.75

15

Wadi elarbain3

3.50

37

Shakef tobok

6.25

16

Wadi al-shak1

4.00

38

Taupq

4.50

17

Wadi al-shak2

3.25

39

Shakef meslh

4.00

18

Wadi al-shak3

3.50

40

Nakp mesalh

4.50

19

Wadi itlah1

5.75

41

Shakef saker

3.50

20

Wadi itlah 2

5.00

42

Sakarkiah

5.25

21

Wadi هtlah3

5.00

43

Naqb al-zawateen

5.00

22

Maen al-raian1

3.50

44

Seleebat

6.00

 

 


 

Table 5. The main constituents of  essential oil of O. syriacum plants grown in stands in SPK, south Sinai Egypt during june of 2014

Composite Name

Stand No.

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

16

17

18

19

20

21

22

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

Thujene

0.66

0.55

0.66

0.56

0.64

0.31

0.69

0.51

0.77

0.18

0.72

0.66

0.82

0.72

0.64

0.63

0.51

0.76

0.29

0.73

1.08

1.00

α-pinen

0.27

0.25

0.33

0.31

0.32

0.17

0.35

0.14

0.34

0.07

0.34

0.34

0.43

0.35

0.34

0.31

0.22

0.36

0.13

0.38

0.52

0.51

Comphere

0.02

0.00

0.04

0.03

0.03

0.02

0.04

0.02

0.04

0.00

0.04

0.04

0.04

0.04

0.04

0.03

0.02

0.03

0.00

0.05

0.05

0.05

α-myrcene

0.02

0.05

0.01

0.01

0.00

0.00

0.02

0.01

0.02

0.00

0.02

0.00

0.02

0.00

0.02

0.00

0.00

0.02

0.03

0.02

0.02

0.00

Octanol

0.02

0.00

0.03

0.03

0.00

0.01

0.04

0.00

0.04

0.00

0.00

0.00

0.00

0.00

0.00

0.00

0.05

0.00

0.03

0.06

0.01

0.00

α-Tirpenene

0.78

0.49

0.60

0.50

0.69

0.33

0.76

0.60

1.16

0.27

0.92

0.94

1.00

0.79

0.65

0.70

0.54

0.57

0.28

0.86

1.12

1.32

P – Cymene

3.06

2.12

2.94

2.20

2.75

2.01

2.75

2.13

2.92

0.98

3.52

3.02

4.10

3.47

3.26

2.80

2.33

2.62

1.71

3.80

4.85

4.10

Di –limonene

0.14

0.10

0.00

0.00

0.13

0.00

0.14

0.00

0.17

0.04

0.00

0.15

0.00

0.16

0.00

0.00

0.10

0.00

0.10

0.17

0.00

0.19

α-phyllanderen

0.11

0.10

0.09

0.10

0.09

0.06

0.10

0.11

0.12

0.03

0.12

0.12

0.11

0.14

0.11

0.08

0.08

0.07

0.05

0.14

0.15

0.15

ɣ-terpinene

4.11

2.85

2.28

2.06

3.24

1.37

3.66

2.56

5.93

1.73

4.13

4.29

4.78

3.36

2.84

3.21

2.59

2.16

1.67

3.89

5.20

6.29

Trams – sabinen hydrate

0.35

0.03

0.49

0.58

0.48

0.46

0.55

0.57

0.59

0.32

0.48

0.62

0.61

0.57

0.66

0.49

0.50

0.24

0.60

0.62

0.95

0.59

Linalool

0.16

0.20

0.15

0.22

0.18

0.20

0.21

0.16

0.15

0.30

0.32

0.28

0.11

0.21

0.16

0.32

0.17

0.10

0.16

0.26

0.20

0.21

Borneol

0.10

0.06

0.11

0.09

0.12

0.08

0.11

0.10

0.19

0.14

0.19

0.21

0.20

0.25

0.23

0.23

0.14

0.12

0.13

0.25

0.27

0.22

Terpieol -4

0.63

0.29

0.55

0.42

0.40

0.42

0.48

0.42

0.11

0.09

0.11

0.09

0.11

0.13

0.13

0.12

0.08

0.08

0.08

0.16

0.16

0.15

α-Terpieol

0.15

0.05

0.13

0.11

0.12

0.14

0.15

0.10

0.11

0.12

0.15

0.11

0.11

0.16

0.14

0.21

0.13

0.08

0.11

0.17

0.16

0.16

Carvone

0.02

0.17

0.02

0.02

0.04

0.05

0.05

0.04

0.04

0.03

0.05

0.04

0.04

0.05

0.06

0.06

0.02

0.03

0.03

0.07

0.06

0.06

Thymol

0.14

0.00

0.15

0.13

0.15

0.14

0.16

0.16

0.15

0.10

0.19

0.02

0.02

0.03

0.03

0.03

0.01

0.00

0.00

0.02

0.03

0.02

Carvacroal

86.35

89.10

88.53

89.58

87.48

91.74

86.27

89.26

82.35

92.68

84.71

84.44

83.54

85.08

86.59

86.53

89.31

90.03

91.41

83.66

79.68

79.86

Euginol

0.10

0.12

0.06

0.11

0.05

0.09

0.11

0.12

0.18

0.08

0.25

0.09

0.07

0.08

0.11

0.21

0.09

0.05

0.11

0.16

0.10

0.11

Long pinene epoxid

0.53

0.69

0.52

0.63

0.70

0.64

0.69

0.82

1.62

0.75

0.89

1.35

0.84

0.88

0.82

0.77

0.57

0.38

1.00

0.86

0.87

0.94

Total of oxyginated compounds

88.18

90.51

90.24

91.32

89.23

93.47

88.22

91.16

84.9

94.26

86.85

86.63

85.04

86.86

88.25

88.45

90.52

90.87

93

85.59

81.52

81.72

Total of non oxyginated compounds

9.54

6.71

7.45

6.37

8.38

4.77

9.11

6.67

12.1

3.65

10.3

10.18

11.91

9.61

8.58

8.28

6.94

6.83

4.92

10.74

13.96

14.21

Total

97.72

97.22

97.69

97.69

97.61

98.24

97.33

97.83

97.00

97.91

97.15

96.81

96.95

96.47

96.83

96.73

97.46

97.70

97.92

96.33

95.48

95.93

 

 

 

 

 

 

 

Table 5. cont.

Composite Name

Stand No.

23

24

25

26

27

28

29

30

31

32

33

34

35

36

37

38

39

40

41

42

43

44

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

A%

Thujene

0.74

0.17

0.84

0.91

1.06

0.75

0.43

0.80

0.84

0.87

0.49

0.75

0.79

0.64

0.28

0.85

0.91

0.52

0.20

0.38

1.03

0.48

α-pinen

0.36

0.00

0.39

0.43

0.51

0.40

0.20

0.41

0.39

0.42

0.00

0.45

0.39

0.39

0.17

0.50

0.41

0.28

0.14

0.23

0.52

0.21

Comphore

0.03

0.02

0.05

0.04

0.05

0.04

0.02

0.04

0.04

0.05

0.41

0.00

0.00

0.00

0.00

0.06

0.04

0.03

0.02

0.03

0.06

0.03

α-myrcene

0.00

0.00

0.00

0.02

0.02

0.00

0.00

0.00

0.03

0.02

0.06

0.00

0.00

0.00

0.00

0.00

0.02

0.00

0.00

0.00

0.02

0.00

Octanol

0.00

0.00

0.02

0.00

0.00

0.00

0.02

0.00

0.00

0.02

0.04

0.04

0.03

0.00

0.00

0.02

0.00

0.12

0.03

0.02

0.00

0.00

α-Tirpenene

0.88

0.54

0.87

0.74

1.11

0.64

0.55

1.12

0.94

1.04

0.70

0.89

0.91

0.69

0.48

1.49

1.16

0.63

0.59

0.61

1.08

0.71

P – Cymene

2.85

2.21

3.38

3.30

3.80

3.22

1.90

3.33

3.93

3.13

2.29

3.98

3.84

3.36

2.29

6.23

3.60

2.52

4.40

3.16

4.07

3.31

Di –limonene

0.14

0.00

0.17

0.00

0.18

0.00

0.00

0.16

0.00

0.17

0.16

0.00

0.19

0.00

0.00

0.26

0.18

0.00

0.00

0.00

0.19

0.00

α-phyllanderen

0.10

0.07

0.12

0.12

0.17

0.13

0.06

0.13

0.15

0.12

0.08

0.12

0.15

0.10

0.05

0.23

0.15

0.09

0.07

0.07

0.15

0.09

 γ-Terpinene

4.47

2.73

4.08

2.93

5.05

2.30

2.75

5.30

4.09

5.06

3.09

3.95

4.09

2.75

2.74

7.40

5.41

2.61

2.67

3.08

4.64

3.35

Trams – sabinen hydrate

0.73

0.50

0.69

0.61

0.65

0.53

0.68

0.82

0.44

0.53

0.49

1.20

0.73

0.67

0.74

1.32

0.73

0.78

0.92

0.76

0.58

0.56

Linalool

0.16

0.16

0.28

0.22

1.84

0.25

0.18

0.25

0.29

0.31

0.09

0.16

0.20

0.11

0.00

0.31

0.18

0.29

0.22

0.28

0.25

0.29

Borneol

0.27

0.26

0.25

0.22

0.00

0.32

0.22

0.30

0.22

0.20

0.18

0.41

0.24

0.27

0.22

0.42

0.27

0.29

0.42

0.37

0.26

0.25

Terpienol -4

0.17

0.12

0.22

0.11

0.12

0.12

0.14

0.16

0.14

0.16

0.12

0.16

0.13

0.14

0.16

0.32

0.17

0.16

0.16

0.13

0.17

0.15

 α-Terpineol

0.14

0.11

0.15

0.14

0.11

0.15

0.17

0.15

0.17

0.16

0.12

0.18

0.12

0.11

0.07

0.18

0.18

0.13

0.15

0.21

0.16

0.21

Carvone

0.07

0.05

0.08

0.06

0.05

0.06

0.07

0.06

0.05

0.05

0.05

0.09

0.06

0.05

0.00

0.07

0.06

0.06

0.08

0.06

0.07

0.07

Thymol

0.02

0.01

0.03

0.02

0.01

0.02

0.04

0.02

0.03

0.02

0.00

0.03

0.04

0.01

0.00

0.03

0.02

0.05

0.03

0.03

0.02

0.03

Carvacroal

84.05

89.34

83.68

85.83

80.66

86.86

88.01

82.17

83.38

83.13

85.60

82.78

83.55

86.99

90.22

74.21

81.49

87.39

85.78

86.41

81.60

85.63

Euginol

0.14

0.08

0.09

0.11

0.11

0.10

0.13

0.09

0.14

0.05

0.10

0.16

0.13

0.05

0.08

0.10

0.10

0.08

0.16

0.12

0.12

0.13

Long pinene epoxid

1.28

0.89

0.92

0.82

0.72

0.93

1.34

0.88

1.02

0.88

0.67

0.77

0.97

0.56

0.44

1.02

0.70

0.86

0.98

0.79

0.96

0.89

Total of oxyginated compounds

86.26

90.99

85.67

87.51

83.62

88.79

90.25

84.06

85.43

84.96

87.29

84.65

85.38

88.24

91.19

76.65

83.15

89.28

87.92

88.37

83.6

87.61

Total of non oxyginated compounds

10.34

6.27

10.64

9.12

12.6

8.03

6.66

12.13

10.86

11.43

7.45

11.47

11.18

8.65

6.75

18.37

12.63

7.61

9.1

8.37

12.35

8.78

Total

96.60

97.26

96.31

96.63

96.22

96.82

96.91

96.19

96.29

96.39

94.74

96.12

96.56

96.89

97.94

95.02

95.78

96.89

97.02

96.74

95.95

96.39

 

 

 

 

 

 


 

Fig.1. Texture types of soil and their percentages.