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ORA SERIES |
Established Series PCS, JYH, UKT 10 Apr., 1977 |
The Ora series are members of the medial, mixed, thermic family of Andic Humudepts [Cambic Umbrisols (Humic Hyperdystric Siltic) classified by WEB]. These soils have dark brown gravelly silt loam Ap horizons, dark brown gravelly silt loam AB horizons, dark brown gravelly silt loam Bw1 horizons, dark yellowish brown gravelly silt loam Bw2 horizons, and dark yellowish brown gravelly silt loam BC horizons. They occur on lava plains and are derived from pyroclastic materials.
Typifying Pedon: Ora gravelly silt loam-upland crops (Colors are for moist soil).
Slope: 7-15%
Elevation: 219 m above m.s.l.
Soil moisture regime: Udic
Soil temperature regime: Thermic
Parent material: Pyroclastic materials
Diagnostic features: An umbric epipedon from a depth of 0 to 35 cm and a cambic horizon from a depth of 35 to 92 cm (An umbric horizon from a depth of 0 to 35 cm and a cambic horizon from a depth of 35 to 92 cm by WRB).
Described by: Song, K. C., D. C. Noh, and S. J. Jung, 15 June, 2011.
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Morphological properties of typifying pedon. |
Ap - 0 to 20 cm. Dark brown (10YR 3/3) gravelly silt loam; weak fine to medium granular structure; friable, slightly sticky and slightly plastic; common fine to medium roots; common fine to medium pores; 10% gravels; clear smooth boundary.
AB - 20 to 35 cm. Dark brown (10YR 3/3) gravelly silt loam; moderate medium to coarse subangular blocky structure; friable, slightly sticky and slightly plastic; common fine to medium roots; common fine to medium pores; 10% gravels; clear smooth boundary.
Bw1 - 35 to 67 cm. Dark brown (10YR 3/3) gravelly silt loam; weak fine to medium subangular blocky structure; friable, slightly sticky and slightly plastic; common fine to medium roots; common fine to medium pores; few worm holes; 15% gravels; clear wavy boundary.
Bw2 - 67 to 92 cm. Dark yellowish brown (10YR 3/4) gravelly silt loam; weak fine to medium subangular blocky structure; friable, slightly sticky and slightly plastic; few fine roots; few fine pores; 20% gravels; clear smooth boundary.
BC - 92 to 160 cm. Dark yellowish brown (10YR 4/4) gravelly silt loam; weak fine to medium subangular blocky structure; friable, slightly sticky and slightly plastic; few fine roots; common fine to medium pores; 25% gravels.
The typifying pedon has an umbric epipedon from a depth of 0 to 35 cm and a cambic horizon from a depth of 35 to 92 cm. That can be classified as Inceptisol. It has an udic soil moisture regime and keys out as Udept. It has an umbric epipedon and keys out as Humudept. It has, throughout one or more horizons with a total thickness of 18 cm or more within 75 cm of the mineral soil surface, a fine-earth fraction with both a bulk density of 1.0 g/cm3 and Al plus 1/2 Fe percentages (by ammonium oxalate) totaling more than 1.0. It can be classified by Andic Humudept. The typifying pedon has medial particle-size class, mixed mineralogy class, and thermic soil temperature regime. Therefore it can be classified as medial, mixed, thermic family of Andic Humudept.
Type Location: About 400 meters south-west of the Namhag Bridge, Yeon Dong, Jeju city, Jeju Do (126° 31' 30.7'', 33° 27' 39.3'').
Range in Characteristics: These soils have umbric epipedons and an argillic horizons. Solum thickness ranges from 100 to 200 cm and depth to hard rock is more than 3 meters. Reaction is medium to slightly acid. Base saturation is less than 60 percent. A horizons are dark brown or very dark grayish brown gravelly silt loam. Bw horizons are dark brown, dark grayish brown, or dark yellowish brown gravelly silt loam, loam, or silty clay loam. C horizons are dark brown or dark yellowish brown gravelly silt loam or silty clay loam. The content of coarse fragments ranges from 10 to 35 percent.
Competing Series and Their Differentiae: These are the Sara and Jeju soils. The Sara soils have medial over cindery texture class. The Jeju soils are belonged to Andic Palehumults.
Setting: The Ora soils are developed on gently sloping to moderately steep lava plains and are derived from pyroclastic materials. Slope ranges from 2 to 30 percent and 2 to 15 percent slopes are predominant.
Principal Associated Soils: The Jeju, Bongseong, Gueom, and Donggwi soils are associated with the Ora soils. They occur on similar physiographic positions.
Drainage and Permeability: Well drained. Permeability is moderately slow. Runoff is medium.
Use and Vegetation: Most of these soils are used for upland crops such as barley, sweet potato, oil vegetables, potato, and the remaining areas are grass land growing grass and shrub.
Distribution and Extent: The Ora soils are of moderate extent and are distributed on lava plains of the northeastern parts in Jeju Do.
Series Established: Jeju city, Jeju Do, 1975. Revised, Jeju city, Jeju Do, 2011.
Laboratory data sheets of typifying pedon.
Depth (cm) |
Horizon |
( --- Total ---) |
(-- Clay --) |
(-- Silt --) |
(------- Sand -------) |
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Clay |
Silt |
Sand |
Fine |
Coarse |
Fine |
Coarse |
VF |
F |
M |
C |
VC |
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LT |
.002 |
.05 |
LT |
LT |
.002 |
.02 |
.05 |
.10 |
.25 |
.5 |
1 |
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.002 |
- .05 |
- 2 |
.0002 |
.002 |
- .02 |
- .05 |
- .10 |
- .25 |
- .50 |
- 1 |
- 2 |
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- - - - - - - - - - - Pct of ˂ 2mm (3A1) - - - - - - - - - - - |
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0-20 |
Ap |
22.9 |
71.6 |
5.5 |
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41.3 |
30.3 |
0.9 |
1.5 |
1.2 |
1.2 |
0.7 |
20-35 |
BA |
21.1 |
72.5 |
6.4 |
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36.7 |
35.8 |
1.3 |
1.9 |
1.4 |
1.4 |
0.4 |
35-67 |
Bw1 |
19.3 |
73.1 |
7.5 |
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35.2 |
37.9 |
1.9 |
2.3 |
1.6 |
1.3 |
0.4 |
67-92 |
Bw2 |
21.1 |
71.8 |
6.0 |
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32.6 |
39.2 |
1.6 |
2.1 |
1.2 |
0.9 |
0.2 |
92-160 |
BC |
25.3 |
64.9 |
9.8 |
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24.6 |
40.3 |
2.5 |
3.7 |
2.0 |
1.3 |
0.3 |
Depth (cm) |
Coarse Fractions(mm) |
˃2mm |
Orgn |
Total |
Extr |
Total |
(-- Dith -Cit --) |
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Weight |
Wt |
C |
N |
P |
S |
Extractable |
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2-5 |
5-20 |
20-75 |
.1-75 |
Pct of |
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Fe |
Al |
Mn |
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Whole |
6A1c |
6B3a |
6S3 |
6R3a |
6C2b |
6G7a |
6D2a |
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Pct of ˂ 75mm (3B1) |
Soil |
Pct ˂ 2mm |
g/kg |
Pct of ˂ 2mm |
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0-20 |
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5.32 |
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20-35 |
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4.61 |
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35-67 |
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3.96 |
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67-92 |
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1.75 |
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92-160 |
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1.17 |
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Depth (cm) |
Ratio/Clay |
Atterberg |
( Bulk Density ) |
COLE |
(- Water Content -) |
WRD |
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CEC |
1500 |
Limits |
Field |
33 |
Oven |
Whole |
Field |
10 |
33 |
1500 |
Whole |
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kPa |
LL |
PI |
Moist |
kPa |
Dry |
Soil |
Moist |
kPa |
kPa |
kPa |
Soil |
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8D1 |
8D1 |
4P1 |
4P |
4A3a |
4A1d |
4A1h |
4D1 |
4B4 |
4B1c |
4B1c |
4B2a |
4C1 |
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Pct ˂0.4mm |
- - g/cc - - |
cm/cm |
-- Pct of ˂2mm -- |
cm/cm |
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0-20 |
1.35 |
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0.66 |
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56.6 |
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20-35 |
1.43 |
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0.59 |
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76.9 |
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35-67 |
1.52 |
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0.68 |
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54.1 |
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67-92 |
1.08 |
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0.67 |
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52.0 |
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92-160 |
0.91 |
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Depth (cm) |
( NH4OAc Extractable Bases ) |
Acid- |
Extr |
(----- CEC -----) |
Al |
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Ca |
Mg |
K |
Na |
Sum |
ity |
Al |
Sum |
NH4- |
Bases |
Sat |
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5B5a |
5B5a |
5B5a |
5B5a |
Bases |
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Cats |
OAc |
+ Al |
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6N2e |
6O2d |
6Q2b |
6P2b |
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6H5a |
6G9a |
5A3a |
5A8b |
5A3b |
5G1 |
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- - - - - - - - - - - - meq / 100g - - - - - - - - - - - - |
Pct |
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0-20 |
4.0 |
1.5 |
0.6 |
0.2 |
6.2 |
35.5 |
0 |
41.7 |
30.8 |
6.2 |
0 |
20-35 |
3.2 |
1.1 |
0.4 |
0.2 |
4.8 |
36.6 |
1.0 |
41.4 |
39.2 |
5.8 |
17.2 |
35-67 |
1.9 |
0.6 |
0.2 |
0.2 |
2.9 |
38.8 |
0.7 |
41.7 |
29.4 |
3.6 |
19.4 |
67-92 |
2.0 |
1.4 |
0.2 |
0.3 |
3.9 |
23.9 |
0.8 |
27.9 |
23.9 |
4.7 |
17.0 |
92-160 |
2.1 |
2.1 |
0.1 |
0.6 |
5.0 |
21.9 |
0 |
26.8 |
23.1 |
5.0 |
0 |
Depth (cm) |
(Base Sat) |
CO3 as |
Res |
P Ret |
(------ pH ------) |
Acid Oxalate Extraction |
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Sum |
NH4- |
CaCO3 |
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NaF |
KCl |
CaCl2 |
H2O |
Opt |
Al |
Fe |
Si |
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OAc |
˂2mm |
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.01M |
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Den |
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5C3 |
5C1 |
6E1g |
8E1 |
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8C1d |
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8C1f |
8C1f |
8J |
6G12 |
6C9a |
6V2 |
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---- Pct ---- |
ohms/cm |
Pct |
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1: 1 |
1: 2 |
1: 1 |
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- Pct of ˂2mm - |
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0-20 |
15.0 |
20.2 |
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55.2 |
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4.6 |
5.0 |
5.6 |
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0.60 |
0.92 |
0.09 |
20-35 |
11.5 |
15.8 |
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82.6 |
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4.5 |
4.9 |
5.5 |
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1.13 |
1.38 |
0.20 |
35-67 |
6.9 |
9.7 |
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91.9 |
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4.5 |
4.8 |
5.7 |
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1.53 |
1.32 |
0.40 |
67-92 |
14.1 |
16.4 |
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86.0 |
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4.5 |
4.9 |
6.0 |
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0.97 |
1.04 |
0.17 |
92-160 |
18.5 |
21.6 |
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83.7 |
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5.0 |
5.0 |
6.1 |
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1.01 |
1.15 |
0.18 |