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GACHEON SERIES |
Established Series SJD, JYH, UKT 4 April, 1974 |
The Gacheon series are members of the coarse loamy over sandy skeletal, mixed, mesic family of Fluvaquentic Endoaquepts [Fluvic Gleyic Hydragric Anthrosols (Dystric) classified by WRB]. These soils have thick grayish brown sandy loam Ap horizons and moderately deep dark gary sandy loam with yellowish brown mottled cambic B horizons. The C horizons are light brownish gray very gravelly loamy coarse sand with few or no mottles. These soils are formed on very gently sloping gravelly alluvial plains.
Typifying Pedon : Gacheon sandy loam-rice (Field description Wanju Gun profile No. 49; colors are for moist soil).
Slope: 0-2%
Elevation: m above m.s.l.
Soil moisture regime: Aquic
Temperature regime: Mesic
Parent material: Alluvium
Diagnostic features: An ochric epipedon from a depth of 0 to 22 cm and a cambic horizon from a depth of 35 to 58 cm (An anthaquic horizon from a depth of 0 to 22 cm and a hydragric horizon from a depth of 22 to 58 cm by WRB).
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Morphological properties of typifying pedon. |
Ap1 - 0 to 10 cm. Grayish brown (2.5Y 5/2) sandy loam; structureless, massive; friable, slightly sticky and slightly plastic; few fine micas; many fine to medium roots; clear smooth boundary; pH 5.5.
Ap2 - 10 to 22 cm. Dark gray (5Y 4/1) sandy loam; common fine to medium prominent dark reddish brown (5YR 3/4) mottles; structureless, massive; friable, slightly sticky and slightly plastic; few fine micas; common fine to medium roots; clear smooth boundary; pH 5.7.
BAg - 22 to 35 cm. Dark gray (5Y 4/1) sandy loam; common fine prominent yellowish brown (10YR 5/8) mottles; weak coarse prismatic structure; friable, slightly sticky and slightly plastic; few fine micas; few fine pores; few fine roots; clear smooth boundary; pH 6.0.
Bg - 35 to 58 cm. Very dark gray (5Y 3/1) gravelly sandy loam; few fine prominent dark yellowish brown (10YR 4/4) mottles; weak coarse prismatic structure; friable, slightly sticky and slightly plastic; few fine micas; about 15 percent gravels; abrupt smooth boundary; pH 6.0.
Cg - 58 to 100 cm. Light brownish gray (2.5Y 6/2) very gravelly to cobbly sand; structureless, single grained; loose, non sticky and non plastic; few fine micas; about 50 percent coarse fragments; pH 6.0.
Type Location: About 300 meters north of Deogcheon Ri, Gwi Myeon, Wanju Gun, Jeollabug Do.
Range in Characteristics: These soils have ochric epipedons and cambic horizons. Solum thickness ranges from 50 to 100 cm. Gravel and cobble contents range from 5 to 35 percent in the solum and from 35 to 90 percent in the C horizons. Depth to bed rock is more than 5 meters or more. Soil reaction is strongly to medium acid and base-saturation is less than 60 percent. Ap horizons are grayish brown, dark grayish brown, very dark grayish brown, or olive gray sandy loam or loam with common fine yellowish brown or dark reddish brown mottles. Bg horizons are dark gray, very dark gray, or olive gray sandy loam or loam with yellowish brown, strong brown, or yellowish red mottles and some gravels. C horizons are gray, dark gray, grayish brown, brownish gray, or light brownish gray very gravelly to cobbly loamy sand or coarse sand.
Competing Series and Their Differentiae: These are the Tongcheon, Seoggye, Deogcheon, Manseong, Gocheon and Seogcheon soils. The Tongcheon soils have fine loamy over sandy skeletal textures and are moderately well drained. The Seoggye soils are coarse loamy over sandy texture family. The Deogcheon soils are well drained class. The Manseong soils are fine loamy over sandy skeletal texture. The Gocheon soils are moderately well drained class. The Seogcheon soils are coarse loamy throughout the horizons and gravel free.
Setting: The Gacheon soils are on nearly level and very gently sloping alluvial plains. Slopes are dominantly about 1 percent and ranges from 0 to 2 percent.
Principal Associated Soils: These are the Hwangryong, Namgye, Hagsan, Tongcheon and Subug series. The Hwangryong soils that have sandy skeletal texture family and somewhat excessively drained, are associated with river sides. The sandy skeletal and moderately well drained Namgye soils are also associated with river sides. The Hagsan and Tongcheon soils are similar physiographic positions. The Subug soils are associated with local valley and fan areas.
Drainage and Permeability: The Gacheon soils are imperfectly drained and permeability is moderately rapid. Runoff is slow.
Use and Vegetation: Most of these soils are used for paddy rice and barley.
Distribution and Extent: The Gacheon soils are of small extent and occur on alluvial plains along the streams throughout the country.
Series Established: Wanju Gun, Jeollabug Do, 1973.
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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0-10 |
Ap1 |
8.6 |
29.1 |
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14.7 |
27.1 |
12.5 |
5.6 |
2.4 |
10-22 |
Ap2 |
9.0 |
30.6 |
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15.1 |
27.0 |
12.2 |
4.1 |
2.0 |
22-35 |
BAg |
7.4 |
23.5 |
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7.2 |
17.1 |
23.0 |
14.2 |
7.6 |
35-58 |
Bg |
6.7 |
22.2 |
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8.0 |
16.7 |
22.0 |
15.8 |
8.6 |
58-100 |
Cg |
3.1 |
8.7 |
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4.3 |
9.1 |
29.7 |
31.8 |
13.3 |
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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0-10 |
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1.34 |
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10-22 |
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0.97 |
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22-35 |
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0.51 |
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35-58 |
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0.57 |
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58-100 |
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0.18 |
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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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0-10 |
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38.6 |
23.4 |
7.2 |
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10-22 |
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36.5 |
23.8 |
7.1 |
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22-35 |
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27.8 |
19.5 |
6.1 |
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35-58 |
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- |
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22.9 |
17.2 |
5.9 |
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58-100 |
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- |
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9.7 |
5.8 |
4.0 |
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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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0-10 |
2.05 |
0.38 |
0.15 |
0.11 |
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7.10 |
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10-22 |
1.82 |
0.34 |
0.06 |
0.10 |
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7.25 |
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22-35 |
1.82 |
0.41 |
0.06 |
0.08 |
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5.70 |
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35-58 |
1.70 |
0.38 |
0.06 |
0.08 |
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5.15 |
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58-100 |
0.82 |
0.23 |
0.06 |
0.07 |
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2.45 |
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Depth (cm) |
(Base Sat) |
CO3 as |
Res |
Cond |
(------ 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 |
8I |
8C1d |
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8C1f |
8C1f |
8J |
6G12 |
6C9a |
6V2 |
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---- Pct ---- |
ohms/cm |
dS/m |
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1: 1 |
1: 2 |
1: 1 |
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- Pct of ˂2mm - |
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0-10 |
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37.9 |
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4.2 |
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4.8 |
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10-22 |
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32.0 |
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4.1 |
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4.9 |
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22-35 |
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41.6 |
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4.3 |
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5.5 |
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35-58 |
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43.1 |
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4.3 |
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5.6 |
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58-100 |
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48.2 |
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4.8 |
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6.1 |
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Depth (cm) |
Active |
Easily Red |
Avail. |
Extractable |
S.G. |
Atterberg |
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Fe |
Mn |
SiO2 |
Acti. |
Limits % |
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% |
ppm |
ppm |
H |
Al |
LL |
PI |
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0-10 |
0.54 |
31 |
43 |
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10-22 |
0.58 |
45 |
50 |
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22-35 |
0.67 |
54 |
55 |
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35-58 |
0.55 |
52 |
54 |
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58-100 |
0.34 |
11 |
39 |
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