LOCATION MANTADOR                ND

Established Series
CJH-KAA-JJB
08/2016

MANTADOR SERIES


The Mantador series consists of very deep, somewhat poorly drained, moderately rapidly permeable soils formed in calcareous moderately coarse glaciolacustrine deposits. These soils are on delta and lake plains. Slope ranges from 0 to 2 percent. Mean annual air temperature is about 5 degrees C, and the mean annual precipitation is about 580 mm.

TAXONOMIC CLASS: Coarse-loamy, mixed, superactive, frigid Aquic Pachic Hapludolls

TYPICAL PEDON: Mantador fine sandy loam - on a plane, nearly level slope of less than 1 percent in a cultivated field. (Colors are for moist soil unless otherwise stated. Where described, the soil was moist throughout.)

Ap1--0 to 8 centimeters; black (10YR 2/1) fine sandy loam, very dark gray (10YR 3/1) dry; moderate medium granular structure; very friable; common very fine roots; neutral; gradual smooth boundary.

Ap2--8 to 30 centimeters; black (10YR 2/1) very fine sandy loam, very dark gray (10YR 3/1) dry; moderate medium subangular blocky structure; very friable; many very fine roots; slight effervescence in lower part in places; neutral; clear smooth boundary.

Bw1--30 to 51 centimeters; very dark grayish brown (10YR 3/2) fine sandy loam, dark grayish brown (10YR 4/2) dry; common medium distinct dark brown (7.5YR 3/2) and common medium faint dark grayish brown (10YR 4/2) redoximorphic concentrations; weak coarse prismatic and weak medium subangular blocky structure; very friable; common very fine roots; krotovina up to 7 cm in diameter in places; slight effervescence; moderately alkaline; clear wavy boundary.

Bw2--51 to 69 centimeters; dark brown (10YR 3/3) fine sandy loam, brown (10YR 5/3) dry; common medium distinct dark brown (7.5YR 3/2) and few fine distinct brown (7.5YR 5/2) redoximorphic concentrations; weak coarse angular blocky and weak medium subangular blocky structure; very friable; common very fine roots; very dark gray (7.5YR 3/1) masses of iron-manganese; strong effervescence; moderately alkaline; clear smooth boundary.

Bk1--69 to 86 centimeters; very dark grayish brown (10YR 3/2) fine sandy loam, grayish brown (10YR 5/2) dry; common coarse distinct dark brown (7.5YR 3/2) redoximorphic concentrations; weak coarse prismatic and weak medium subangular blocky structure; very friable; very friable; common medium rounded black (10YR 2/1) masses of iron-manganese; common grayish brown (10YR 5/2) masses of lime; violent effervescence; moderately alkaline; gradual smooth boundary.

Bk2--86 to 100 centimeters; light yellowish brown (2.5Y 6/4) very fine sandy loam, pale yellow (2.5Y 8/4) dry; many prominent dark brown (7.5YR 3/4) redoximorphic concentrations; weak coarse prismatic and weak medium subangular blocky structure; very friable; very friable; common extremely coarse light yellowish brown (2.5Y 6/3) masses of lime on vertical faces of peds; violent effervescence; moderately alkaline; gradual wavy boundary.

C1--100 to 150 centimeters; light olive brown (2.5Y 5/4) very fine sandy loam, pale yellow (2.5Y 7/4) dry; many fine and medium prominent dark brown (7.5YR 3/4) redoximorphic concentrations; massive; very friable; common fine and medium black (N 2/0) masses of iron-manganese; strong effervescence; moderately alkaline; gradual wavy boundary.

C2--150 to 200 centimeters; gray (2.5Y 5/1) very fine sandy loam, light gray (2.5Y 7/1) dry; common coarse prominent strong brown (7.5YR 5/6) redoximorphic concentrations; massive; very friable; strong effervescence; moderately alkaline.

TYPE LOCATION: Major Land Resource Area 56 - Red River Valley of the North (56); Richland County, North Dakota subset; about 3 miles west and 6 miles south of Colfax; 300 feet north and 300 feet west of the southeast corner of sec. 27, T. 134 N., R. 50 W. Latitude 46 degrees, 23 minutes, 4.8 seconds N, Longitude 96 degrees, 56 minutes, 48 seconds W., NAD 83.

RANGE IN CHARACTERISTICS:
Thickness of mollic epipedon - 40 to 80 cm
Depth to carbonates - 20 to 40 cm
Texture of particle size control section - fine sandy loam or very fine sandy loam
Clay content of particle size control section - less than 10 percent
Silt content of particle size control section - 10 to 20 percent
Sand content of particle size control section - greater than 70 percent of which more than 20 percent is very fine sand
Rock fragments - 0 percent
Slightly to moderately saline phases are recognized

Ap and A horizon:
Hue-10YR
Value-2 and 3 dry
Chroma-1
Texture-fine sandy loam, very fine sandy loam, loam, or loamy very fine sand
Reaction-pH 6.6 to 7.8
Thickness-25 to 38 centimeters

Bw horizon:
Hue-10YR or 2.5Y
Value-2 or 3 and 4 or 5 dry
Chroma-2 or 3
Texture-very fine sandy loam or fine sandy loam
Reaction-pH 7.4 to 8.4
Thickness-0 to 50 centimeters


Bk horizon:
Hue-10YR or 2.5Y
Value-3 to 6 and 4 to 8 dry
Chroma-2 to 6
Texture-fine sandy loam, very fine sandy loam, or loamy very fine sand
It is silt loam below a depth of 100 cm in some pedons
Reaction-pH 7.4 to 8.4
Concentrations-5 to 25 percent calcium carbonate equivalent diffused or in masses
Some pedons have a BC horizon
Thickness-25 to 80 centimeters

Some pedons have a BC horizon

Cg horizon:
Hue-2.5Y or 5Y
Value-5 or 6 and 6 or 7 dry
Chroma-1 to 6
Texture-fine sandy loam, very fine sandy loam, or loamy very fine sand
It is fine sand, silt loam, silty clay loam, or silty clay below a depth of 100 cm in some pedons
Discontinuities are common below 100 cm
Reaction-pH 7.4 to 8.4

COMPETING SERIES: There are no other series with this classification.

GEOGRAPHIC SETTING:
Landform-- level and nearly level glacial lake plains and delta plains
Slope--0 to 2 percent
Parent material--calcareous, moderately coarse glaciolacustrine or deltaic sediments
Elevation-230 to 450 meters
Mean annual air temperature--3 to 7 degrees C
Mean annual precipitation--500 to 650 millimeters
Frost-free period--110 to 160 days

GEOGRAPHICALLY ASSOCIATED SOILS:
Delamere - are on adjacent dips and flats and are on lower landscape positions with saturation within 40 centimeters from the surface at some time during the period of April through June
Egeland - are on higher lying convex areas and are well drained
Embden - are on slightly higher positions and do not have carbonates within 40 centimeters
Glyndon - are on slightly lower positions, have a calcic horizon within a depth of 40 cm, and are coarse-silty
Tiffany - are in depressions
Wyndmere - are on slightly lower positions, and have a calcic horizon within a depth of 40 cm

DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY:
Drainage class-somewhat poorly drained-an apparent seasonal high water table is at a depth of 40 to 100 centimeters below the surface at some time during the period of April through June
Runoff--negligible
Saturated hydraulic conductivity-10 to <100 micrometers per second (high)

USE AND VEGETATION: Most areas are used to grow spring-seeded small grains, flax, potatoes and corn. Native vegetation is blue grama, little bluestem, needleandthread and prairie sandreed.

DISTRIBUTION AND EXTENT:
Physiographic Division-Interior Plains
Physiographic Province-Central Lowland
Physiographic section-Western Lake section
MLRA--Red River Valley of the North (56) in North Dakota
LRR-Northern Great Plains Spring Wheat Region (F)
Extent--moderate

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: St. Paul, Minnesota.

SERIES ESTABLISHED: Richland County, North Dakota, 2005.

REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - the zone from the surface of the soil to a depth of 51 centimeters (Ap1, Ap2 and Bw1 horizons)- the Bw2 horizon has the color, but not the organic matter to be mollic; calcic horizon - the zone from 69 to 100 centimeters (Bk1 and Bk2 horizons); characteristics associated with wetness - redoximorphic features within a depth of 40 cm, hue of 10YR and chroma of 2 within 75 centimeters (Bw1 horizon).

ADDITIONAL DATA: S93ND077-012, S93ND077-013, S93ND077-014, S94ND077-021 (type location), and S94ND077-024, S97ND077-002, S98ND077-002, S99ND077-005, S99ND077-006, S00ND077-032.


National Cooperative Soil Survey
U.S.A.