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Shabbir A. Shahid, Samira A. S. Omar - Kuwait Soil Taxonomy.pdf
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List of Figures

Fig. 3.1

Calcic diagnostic horizon in a Typic Haplocalcids prole.

 

 

Calcium carbonates precipitation in soil matrix is evident . . . .

31

Fig. 3.2

Gypsic diagnostic horizon in a Leptic Haplogypsids prole.

 

 

Gypsum accumulation starting at 15 cm is evident . . . . . . . . .

34

Fig. 3.3

Petrogypsic diagnostic horizon in a Typic Petrogypsids

 

 

prole starting at 60 cm depth . . . . . . . . . . . . . . . . . . . . . . . .

36

Fig. 3.4

A salic diagnostic horizon in a Typic Aquisalids prole

 

 

in the coastal area . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

37

Fig. 4.1

Sandy-skeletal soil particle-size class . . . . . . . . . . . . . . . . . . .

49

Fig. 4.2

Sandy soil texture in a Typic torripsamments . . . . . . . . . . . . .

50

Fig. 4.3

A prole of Leptic Haplogypsids showing Gypsic soil

 

 

mineralogy class . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

53

Fig. 5.1

Relative distribution of soil map units in Aridisols

 

 

and Entisols . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

61

Fig. 5.2

A view of sandy desert landscape presenting Entisols soil

 

 

order covering 30% of surveyed area in Kuwait . . . . . . . . . . .

62

Fig. 5.3

A soil prole of Typic Haplocalcids . . . . . . . . . . . . . . . . . . . .

66

Fig. 5.4

A prole of Typic Calcigypsids. Gypsum accumulation

 

 

begins at 90 cm depth. A calcic horizon occurs

 

 

at 3090 cm depth. A decalcied layer at 030 cm . . . . . . . . .

69

Fig. 5.5

A prole of Leptic Haplogypsids. Gypsum accumulation

 

 

begins at 1215 cm from soil surface . . . . . . . . . . . . . . . . . . .

70

Fig. 5.6

A prole of Petrocalcic Petrogypsids. The horizon

 

 

below 25 cm meets the criteria for both a petrocalcic

 

 

and a petrogypsic horizon . . . . . . . . . . . . . . . . . . . . . . . . . . .

71

Fig. 5.7

A prole of Calcic Petrogypsids. A calcic horizon

 

 

occurs at 20 cm and petrogypsic at 40 cm depth . . . . . . . . . . .

72

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xl

List of Figures

 

 

Fig. 5.8 A soil prole showing Typic Petrogypsids (Total depth

75 cm). Petrogypsic horizon started at 60 cm depth. . . . . . . . . 73 Fig. 5.9 A soilscape showing Typic Aquisalids in the coastal area. . . . . 74 Fig. 5.10 A soil prole showing Typic Torripsamments . . . . . . . . . . . . . 77 Fig. 7.1 USDA soil textural triangle (Schoeneberger et al. 2012) . . . . . 103 Fig. 7.2 Vacuum extraction of soil extract from saturated

soil paste . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 108 Fig. 7.3 Pressure membrane apparatus. Porous ceramic plate

is also evident . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 110 Fig. 7.4 Liquid limit measurement device and grooved soil sample. . . . 113 Fig. 7.5 Plastic limit measurement process. . . . . . . . . . . . . . . . . . . . . . 113

List of Tables

Table 6.1

Great groups identied in reconnaissance (KISR 1999a)

 

 

and semi-detailed survey (KISR 1999b) of Kuwait . . . . . . . . .

83

Table 6.2

Soil subgroups identied in reconnaissance (KISR 1999a)

 

 

and semi-detailed survey (KISR 1999b) of Kuwait . . . . . . . . .

83

Table 6.3

Soil families identied during the Reconnaissance Soil

 

 

Survey for the State of Kuwait and correlated to Kuwait

 

 

Soil Taxonomy (KISR 1999a) . . . . . . . . . . . . . . . . . . . . . . . .

84

Table 6.4

Soil series identied during the Semi-Detailed Soil Survey

 

 

for the State of Kuwait and correlated to Kuwait Soil

 

 

Taxonomy (KISR 1999b) . . . . . . . . . . . . . . . . . . . . . . . . . . .

86

xli

Water erosion near Jal Az zor escarpment