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Impact of Imported Fire Ants on Mississippi Soils

Table 1. Locations, soils, dimensions, and spatial densities of mounds of various ant species.

Species

Location

Soil

Height

Diameter

Mounds

Surface

Reference

in

cm

in

cm

no./a

no./ha

%

Camponotus
intrepidus

Austrailia

Yellow
podzolic

8

20

10-49

26-124

2.2

5.4

0.01

Cowan et al.
1985

Formica cinerea
montana

Wisconsin,
U. S.

Typic
Argiudolls

6

15

15

37

620

1531

1.7

Baxter and
Hole 1967

Formica
exsectoides

Wisconsin,
U. S.

Typic
Hapludalf

15

37

43

110

10

25

-

Salem and
Hole 1968

Formica fusca

B.C.,
Canada

Typic
Dystrochrepts

-

-

-

-

466

1150

6-7

Wiken et al.
1976

Formica
fusca

New York,
U. S.

Aeric
Ochraqualfs

-

-

10-33

25-84

44

109

-

Levan and
Stone 1983

Formica spp.
Pogonomyrmex spp.

Western U. S.

-

14

36

36

91

7

18

2

Scott 1951

Iridomyrmex
purpureus

Austrailia

Sandstone
ridgetops

9

23

63x49

160x125

-

-

-

Cowan et al.
1985

Lasius spp.
Myrmica spp.

Poland

Sandy and silty
alluvial and dune soils

1-4

3-11

3-12

8-30

400-800

1000-2000

0.15-0.75

Czerwinski
et al. 1971

Pogonomyrmex
occidentalis

Colorado,
U.S.

Ustillic
Haplargids

7

17

33

84

16

40

2

Mandel and
Sorenson 1982

Pogonomyrmex
occidentalis

New Mexico,
U.S.

Sandy soil

-

-

-

-

6,7

14,17

1

Carlson and
Whitford 1991




Table 2. Soil series, classifications, site locations, and ant species involved in the study.

Series

Classification

County, location

Species

Figure 6
Symbol

Grenada

Fine-silty, mixed, active, thermic Glossic Fragiudalfs

Hinds, Sec. 9, T. 4 N., R. 3 W.

S. invicta

A

Malbis

Fine-loamy, siliceous, thermic Plinthic Paleudults

Pearl River, Sec. 29, T. 4 S., R. 16 W.

S. invicta

B

Sharkey

Very-fine, smectitic, nonacid, thermic Vertic Haplaquepts

Washington, Sec. 35, T. 19 N., R. 7 W.

S. invicta

C

Malbis

Fine-loamy, siliceous, thermic Plinthic Paleudults

Pearl River, Sec. 31, T. 4 S. R. 16 W.

S. invicta

D

Vaiden

Very-fine, montmorillonitic, thermic Aquic Dystruderts

Monroe, Sec. Sec. 1, T. 15 S., R. 6 E.

S. richteri?

E

Alligator

Very-fine, montmorillonitic, thermic Alic Dystraquerts

Quitman, Sec. 26, T. 7 S., R. 10 W.

S. invicta?

F

Atwood

Fine-silty, mixed, thermic Typic Paleudalfs

Ponotoc, Sec. 9, T. 11 S., R. 3 E.

S. richteri?

G

Falkner

Fine-silty, siliceous, active, thermic Aquic Paleudalfs

Ponotoc, Sec. 7, T. 11 S., R. 3 E.

S. richteri?

H

Loring

Fine-silty, mixed, active, thermic Oxyaquic Fragiudalfs

Marshall, Sec. 17, T. 3 S., R. 2 W.

S. richteri?

I

Oktibehha

Very-fine, smectitic, thermic Chromic Dystruderts

Oktibbeha, Sec. 16, T. 19 N., R. 15 E.

S. richteri?

J

Sumter

Fine-silty, carbonatic, thermic Rendollic Eutrochrepts

Oktibbeha, Sec. 16, T. 19 N., R. 15 E.

S. richteri?

K

Loring

Fine-silty, mixed, active, thermic Oxyaquic Fragiudalfs

Hinds, Sec. 8, T. 4 N., R. 3 W.

S. invicta

L

Kipling

Fine, smectitic, thermic Vertic Paleudalfs

Oktibbeha, Sec. 26, T. 19 N., R. 15 E.

S. richteri?

M




Table 3. Site symbols and characteristics of mounds
used for the structural study.1

Site

Drainage
class

Surface
texture

Slope

Vegetation

Mound dimensions2

ID

Height

LBD

SBD

in

cm

in

cm

in

cm

A

Moderately
well-drained

Silt
loam

5-8%

Grass
pasture

1
2
3

7.5
6.3
9.8

19
16
25

19.7
15.0
20.5

50
38
52

16.5
13.0
16.5

42
33
42

B

Well-
drained

Sandy
loam

0-5%

1 m pines,
grasses

1
2
3

7.1
5.1
7.1

18
13
18

33.1
16.1
16.9

84
41
43

28.0
16.1
15.0

71
41
38

C

Poorly
drained

Clay

0-1%

Weeds

1
2
3

9.1
7.5
7.5

23
19
19

29.9
22.0
24.8

76
56
63

26.4
18.5
20.5

67
47
52

1Site symbols are referenced to Figure 6 and Table 3.
2ID=Identification number; LBD=Long basal dimension; and SBD=Short basal dimension.




Table 4. Site symbols and characteristics of mounds used for Sites F-L.1

Site

Drainage
class

Surface
texture

Slope

Vegetation

Mound dimensions2

ID

Height

LBD

SBD

in

cm

in

cm

in

cm

F

Poorly
drained

Clay

0-1%

20-30 feet (6-9 m)
pecan trees


15

38

35

89

35

89

G

Well-
drained

Silt
loam

2-5%

Grass pasture


12

30

24

61

23

58

H

Somewhat
poorly drained

Silt
loam

2-5%

Mowed grass


15

38

34

86

24

61

I

Moderately
well-drained

Silt
loam

5-8%
2-5%

Mowed grass
Weeds

A
B

6
15

15
38

17
36

43
91

17
32

43
81

J

Well-
drained

Silt
loam

0-3%

Weeds, trees


9

23

21

53

21

53

K

Moderately
well-drained

Loam

0-3%

Weeds, trees


10

25

42

107

37

94

L

Moderately
well-drained

Silt
loam

0-3%

Grass pasture

A
B

8
5

20
13

32
26

81
66

28
24

71
61

1Site symbols are referenced to Figure 6 and Table 3.
2ID=Identification number; LBD=Long basal dimension; and SBD=Short basal dimension.




Table 5. Characteristics of channel networks found in mounds on three soil types.1


Malbis

Grenada

Sharkey

% Area in channels

39 (±9)

55 (±4)

55 (±7)

Channels/inch

1.4 (±0.3)

2.3 (±0.4)

1.8 (±0.4)

Channel width (in)

0.25 (±0.05)

0.24 (±0.05)

0.4 (±0.1)

Channel: wall width

0.5 (±0.2)

1.3 (±0.4)

1.9 (±0.4)

1Mean (±standard deviation) of six replicates of percentage of cross-sectional area occupied by channels, number of channels per inch of transect, channel width, and channel width to wall width ratio for channel networks in imported fire ant mounds on
Malbis (Site B), Grenada (Site A), and Sharkey (Site C).




Table 6. Mean bulk density of air-dried clods from crust of the mound, mound interior, and adjacent topsoil control on three soil types.1


Crust

Mound

Control


g cm3

g cm3

g cm3

Malbis sandy loam

1.43 (±0.06)

1.44 (±0.07)

1.63 (±0.03)

Grenada silt loam

1.0 (±0.1)

1.1 (±0.2)

1.51 (±0.03)

Sharkey clay

1.1 (±0.2)

1.57 (±0.07)

1.78 (±0.07)

1Malbis soil is found at Site B, Grenada at Site A, and Sharkey at Site C. These means are based on three replicates (±standard deviation).


Table 7. Mean weight of aggregates remaining from ant
mound crusts, mound interiors, and control topsoil from three soil types
after oscillation in water for 2-32 minutes. 1

Minutes

2

4

8

16

32


g

g

g

g

g

Malbis2

    Crust

1.6b

1.2b

1.1b

0.9b

0.6b

    Mound

3.7a

3.3a

3.1a

2.8a

2.3a

    Control

3.4a

2.8a

2.8a

3.0a

1.6a

Grenda2

    Crust

1.4b

0.8b

0.7b

0.4b

0.3c

    Mound

2.9b

2.5ab

2.3ab

1.7a

1.5b

    Control

3.9a

3.5a

3.2a

2.5a

1.9a

Sharkey2

    Crust

3.2a

3.0a

2.6b

2.2b

1.9c

    Mound

4.1a

4.1a

3.9ab

3.8a

3.3b

    Control

4.2a

4.2a

4.2a

3.9a

3.7a

1Malbis sandy loam is found at Site B, Grenada silt loam at Site A, and Sharkey clay at Site C. Measurements were taken after 5-gram samples were oscillated in water for 2, 4, 8, 16, and 32 minutes. Means are based on three replicates.
2Means in same column and soil with same letter are not significantly different (a=0.05).




Table 8. Capillary contact angle of mound crust, mound interior,
and control topsoil materials on three soil types. 1


Malbis2

Grenada2

Sharkey2


degrees

degrees

degrees

Crust

68 ab

69 b

81ab

Mound

82 a

82 a

81 b

Control

60 b

74 ab

85 a

1Malbis sandy loam is found at Site B, Grenada silt loam at Site A, and Sharkey clay at Site C. Means are based on three replicates.
2Means in same column and soil with same letter are not significantly different (a=0.05).




Table 9. Percent clay and organic matter (OM), pH, extractable P, exchangeable K and Ca, and percent moisture in three formicarious (FP) and undisturbed (UP) pedons on Malbis sandy loam (Site D). 1,2

Depth (in)

% Clay

% OM

pH

P (mg kg)

K (cmol kg)

Ca (cmol kg)

% Moisture

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

9-8

14.8

--

1.99*

--

5.32

--

26*

--

0.41

--

1.57*

--

23.53

--

8-6

18.6*

--

1.70*

--

5.07

--

25

--

0.32

--

1.46*

--

22.34

--

6-3

17.3*

--

1.85*

--

5.02

--

30

--

0.32

--

1.63*

--

19.89

--

3-0

16.0*

--

2.50*

--

4.77

--

73

--

0.31

--

1.58*

--

21.08

--

0-2

11.3*

5.0

3.39*

6.56

4.68

4.76

76

45

0.32*

0.17

1.87*

3.27

17.12

27.23

2-5

8.1

5.4

3.02

2.47

4.84*

5.50

47

17

0.33*

0.07

2.06

2.27

14.44

12.91

5-10

10.7

12.3

1.81

1.71

5.17

5.74

27

8

0.25

0.08

2.03

2.16

12.25

12.94

10-17

22.1

19.9

0.75

1.02

5.50

5.83

11

6

0.19

0.10

2.07

2.38

13.45

13.14

17-28

22.3

22.0

0.56

0.55

5.32

5.47

6

4

0.13

0.06

1.79

1.73

14.19

13.98

28-40

26.3

27.8

0.26

0.25

5.17

5.29

3

3

0.06*

0.03

1.25

1.23

14.29

13.87

1Measurements were made on June 27 and 28, 1996, 5 days after 1.9 inches (4.7 cm) of rain over 4 days.
2Means within a mound (above 0-2 inch depth) marked with asterisks are significantly different (a=0.05) from 0-2 inch depth of UP. Means below the mound marked with asterisks are significantly different (a =0.05) from equivalent depth in UP.




Table 10. Percent clay and organic matter (OM), pH, extractable P, exchangeable K and Ca, and percent moisture in
three formicarious (FP) and undisturbed (UP) pedons on Vaiden silt loam (Site E). 1,2

Depth (in)

% Clay

% OM

pH

P (mg kg)

K (cmol kg)

Ca (cmol kg)

% Moisture

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

12-11.5

30.3*

--

4.40*

--

4.66

--

68*

--

0.51*

--

10.33

--

2.92*

--

11.5-8

33.2*

--

3.33*

--

4.48

--

58*

--

0.46*

--

10.80

--

5.59*

--

8-4

32.6*

--

3.17*

--

4.50

--

54

--

0.45*

--

10.42

--

11.54*

--

4-0

32.4*

--

2.88*

--

4.67

--

60

--

0.51*

--

9.78

--

14.26

--

0-2

30.0*

16.1

3.42*

8.40

4.86

5.07

45*

13

0.41

0.27

9.89

9.72

16.43

16.93

2-4

26.6*

18.2

2.97

3.16

5.12

4.91

45*

5

0.36*

0.11

8.87

6.93

14.16

15.12

4-11

32.3

29.6

1.32

0.86

4.79

4.71

22*

5

0.16*

0.08

8.78

7.30

17.50

12.78

11-18

34.7

36.2

1.06

0.47

4.69

4.82

18*

6

0.14

0.09

8.75

7.75

16.84

19.46

18-26

36.7

38.3

0.58

0.37

4.72

4.74

9

4

0.11

0.10

9.60

8.91

21.09

20.78

26-34

39.6

41.0

0.46*

0.32

4.72

4.76

5

4

0.10

0.11

10.22

11.01

20.83

23.88

34-40

43.5

43.7

0.33*

0.27

4.83

5.00

3

3

0.11*

0.12

12.93

13.80

23.98

25.51

1Measurements were taken on July 3, 1996, 14 days after 0.8 inch (2 cm) of rain.
2Means within a mound (above 0-2 inch depth) marked with asterisks are significantly different (a=0.05) from 0-2 inch depth of UP. Means below the mound marked with asterisks are significantly different (a=0.05) from the equivalent depth in UP.




Table 11. Percent clay and organic matter (OM), pH, extractable P, exchangeable K and Ca, and percent moisture in formicarious (FP) and undisturbed (UP) pedons on Falkner silt loam (Site H). 1

Depth (in)

% Clay

% OM

pH

P (mg/kg)

K (cmol/kg)

Ca (cmol/kg)

% Moisture

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

15-10

12.1

--

3.73

--

4.42

--

78

--

0.38

--

6.80

--

9.88

--

10-5

12.1

--

3.82

--

4.47

--

92

--

0.38

--

4.18

--

9.95

--

5-0

12.3

--

3.49

--

4.62

--

108

--

0.38

--

4.10

--

9.49

--

0-4

12.3

9.2

2.74

4.60

4.52

5.25

90

6

0.25

0.14

3.69

4.15

11.55

19.61

4-8

12.5

14.6

2.31

0.67

4.60

4.86

65

5

0.20

0.06

3.38

2.65

20.16

20.39

8-19

16.5

17.3

0.48

0.35

4.70

4.72

16

7

0.10

0.08

2.54

1.50

18.03

23.85

19-28

17.5

30.0

0.50

0.25

4.67

4.93

20

4

0.11

0.11

2.17

1.32

25.43

25.32

28-34

20.5

18.6

0.29

0.15

4.67

4.69

8

6

0.11

0.11

1.66

1.47

25.17

26.48

34-46

18.4

20.0

0.15

0.12

4.88

5.00

4

3

0.10

0.10

2.32

1.83

25.00

27.27

46-54

27.4

23.2

0.10

0.09

4.77

4.93

3

3

0.12

0.11

5.99

4.83

27.10

26.15

54-60

26.9

27.9

0.09

0.04

5.14

4.57

3

3

0.14

0.15

7.66

7.79

24.21

23.65

1Measurements were taken on May 31, 1996, 2 days after 0.3 inch (0.7 cm) of rain and 3 days after 0.45 inch (1.1 cm) of rain.




Table 12. Percent clay and organic matter (OM), pH, extractable P, and exchangeable K and Ca in formicarious (FP) and undisturbed (UP) pedons on a Loring silt loam (Mound A, Site I).

Depth (in)

% Clay

% OM

pH

P (mg/kg)

K (cmol/kg)

Ca (cmol/kg)

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

6-5.5

16.9

--

2.80

--

4.85

--

21

--

0.56

--

3.61

--

5.5-4

15.4

--

2.98

--

4.99

--

17

--

0.45

--

3.07

--

4-2

16.7

--

2.71

--

4.86

--

17

--

0.48

--

3.06

--

2-0

16.0

--

2.99

--

4.83

--

21

--

0.52

--

3.29

--

0-2

17.8

15.5

3.29

2.91

4.80

5.46

28

17

0.59

0.47

3.89

5.10

2-4

15.2

15.7

1.19

1.13

4.96

5.16

7

6

0.24

0.17

1.59

1.85

4-16

17.7

17.1

0.95

0.78

5.30

5.33

5

4

0.25

0.12

1.08

1.05

16-24

23.1

22.4

0.49

0.57

5.28

5.30

7

5

0.22

0.17

1.10

1.04

24-32

20.5

21.9

0.16

0.17

5.30

5.37

10

8

0.19

0.18

0.98

0.91

32-40

18.6

20.5

0.09

0.10

5.49

5.68

10

9

0.18

0.17

0.58

0.66

40-50

20.4

22.8

0.07

0.07

5.47

5.79

9

9

0.17

0.19

0.56

0.77

50-60

17.7

20.3

0.05

0.05

6.05

5.82

5

7

0.15

0.18

0.57

0.92




Table 13. Percent clay and organic matter (OM), pH, extractable P, exchangeable K and Ca, and percent moisture in formicarious (FP) and undisturbed (UP) pedons on Loring silt loam (Mound B, Site I). 1

Depth (in)

% Clay

% OM

pH

P (mg/kg)

K (cmol/kg)

Ca (cmol/kg)

% Moisture

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

14-10

15.9

--

4.21

--

6.36

--

43

--

0.77

--

3.13

--

31.53

--

10-6

17.8

--

3.30

--

5.10

--

24

--

0.68

--

2.49

--

26.93

--

6-0

19.4

--

2.55

--

4.88

--

21

--

0.71

--

2.35

--

28.42

--

0-2

18.0

16.5

1.91

2.60

4.99

5.07

9

8

0.37

0.25

1.71

2.41

26.35

26.89

2-7

18.7

18.3

1.49

1.59

5.15

5.08

7

4

0.23

0.16

1.67

1.83

26.03

28.35

7-11

21.5

26.0

1.08

0.64

5.10

5.21

5

4

0.17

0.16

1.65

2.12

27.41

26.75

11-24

25.4

23.9

0.28

0.31

5.18

5.26

8

8

0.19

0.16

1.59

1.74

27.98

29.52

24-35

19.9

17.3

0.15

0.09

5.40

5.44

9

9

0.17

0.15

1.13

1.46

29.01

25.91

35-48

19.8

19.3

0.05

0.05

5.61

5.24

9

11

0.18

0.17

1.35

1.53

26.83

23.90

48-60

16.7

18.3

0.05

0.05

5.47

5.44

7

9

0.16

0.15

1.31

1.29

26.98

22.90

1Measurements were taken on May 31, 1996, 2 days after 1.2 inches (3 cm) of rain and 3 days after 2.6 inches (6.7 cm) of rain.




Table 14. Percent clay and organic matter (OM), pH, extractable P, exchangeable K and Ca, and percent moisture in formicarious (FP) and undisturbed (UP) pedons on an Oktibbeha silt loam (Site J).

Depth (in)

% Clay

% OM

pH

P (mg/kg)

K (cmol/kg)

Ca (cmol/kg)

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

FP

UP

8.5-8

20.1

--

4.07

--

7.72

--

14

--

0.33

--

20.73

--

8-7

24.3

--

3.96

--

7.86

--

10

--

0.33

--

22.75

--

7-5

22.5

--

3.29

--

8.05

--

8

--

0.33

--

21.40

--

5-3

25.9

--

3.55

--

7.79

--

9

--

0.34

--

21.88

--

3-0

23.7

--

4.10

--

7.68

--

9

--

0.30

--

21.92

--

0-2

21.5

15.5

5.62

5.53

7.68

6.78

11

8

0.36

0.15

22.11

16.57

2-4

17.0

--

4.81

--

7.66

--

10

--

0.28

--

22.86

--

4-6

27.8

17.0

1.82

3.43

7.75

7.33

5

6

0.18

0.11

21.90

15.75

6-10

--

32.3

--

1.31

--

7.53

--

3

--

0.12

--

19.02

10-15

37.2

39.2

0.56

0.80

7.45

7.48

3

3

0.16

0.14

19.85

19.83

15-28

37.7

42.9

0.39

0.41

6.68

6.28

3

3

0.17

0.15

18.74

19.35

28-32

46.5

46.6

0.31

0.30

5.11

5.12

3

3

0.19

0.17

20.81

17.10

32-39

50.3

48.2

0.34

0.25

5.20

4.89

3

3

0.19

0.18

23.09

19.17

39-41

48.3

47.3

0.41

0.29

6.25

5.14

3

3

0.15

0.19

24.74

22.61

41-48

48.3

47.1

0.41

0.40

6.25

7.61

3

3

0.15

0.10

24.74

27.62

48-50

48.4

--

0.36

--

7.58

--

3

--

0.12

--

26.92

--




For more information about Technical Bulletin 223 -- Impact of Imported Fire Ants on Mississippi Soils contact:
Dr. David E. Pettry
Phone: (662) 325-2770
Email:
David E. Pettry


To contact the Experiment Station:
MAFES Director's Office
Box 9740
Mississippi State, MS 39762
Phone: 662/325-3005
Fax: 662/325-3001
E-mail:
MAFES

Visit:
Mississippi Agriculture and Forestry Experiment Station
The Division of Agriculture, Forestry and Veterinary Medicine
Mississippi State University Extension Service
Mississippi State University

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