Delineating Soil Horizons Soil as a Natural Body
Delineating Soil Horizons
Soil as a Natural Body Differentiation Additions Losses Parent Material Translocations Transformations Bedrock
Soil Horizons Roughly parallel layers in the soil with varying composition and properties
Master Horizons
Criteria for Characterizing Soil Horizons Color Texture Density Structure Organic matter Mineralogy Chemistry
Soil Color
Soil Color Determinants • • • Mineralogy of the soil/parent material Relative amount of organic matter Hydrology of the soil Soil chemistry Soil Microbes
Coloring Agents in Soils Organic Matter Grey to Black coloration particularly in topsoil or A horizon material. Can be found in the sub-soil as an accumulation Elements and Compounds Iron, manganese Reddish to yellow-brown Purplish black
Soil Color Determination
Munsell Soil Color Hue Value related to total amount of light reflected. dominant spectral color; related to the wavelength of light. Related to the proportions of red to yellow. In soils we only use 1/5 of the color chips available. Chroma measure of the strength of spectral color
10 R 0 2. 5 YR 7. 5 YR 10 YR 0 2. 5 Y 5 Y
Hue Pages 10 R Red 2. 5 YR 7. 5 YR 10 YR 2. 5 Y 5 Y Yellow Increasingly dominated by yellow spectral color Florida soils dominated by 7. 5 YR and 10 YR pages
Soil Color
Hue = 10 YR Value = 6 Chroma = 3 Munsell Color 10 YR 6/3
10 YR 2/1 10 YR 5/6
Pink Pale Red Weak Red light Red Dark Red
Summary A horizon – mid/low value - low chroma E horizon – high value - low chroma B horizon – ? value - ? chroma
Water table depth Oxygen status Development decisions
Hydric Soil Classification Hue 10 YR or Yellower Value ≤ 3 Chroma ≤ 1 “Black Histic”
Mineral Formula Size Munsell Color goethite Fe. OOH (1 -2 m m) 10 YR 8/6 yellow goethite Fe. OOH (~0. 2 m m) 7. 5 YR 5/6 strong brown hematite Fe 2 O 3 (~0. 4 m m) 5 R 3/6 red hematite Fe 2 O 3 (~0. 1 m m) 10 R 4/8 red lepidocrocite Fe. OOH (~0. 5 m m) 5 YR 6/8 reddish-yellow lepidocrocite Fe. OOH (~0. 1 m m) 2. 5 YR 4/6 red ferrihydrite Fe (OH)3 2. 5 YR 3/6 dark red glauconite K(Six. Al 4 x)(Al, Fe, Mg)O 10(OH)2 5 Y 5/1 dark gray iron sulfide Fe. S 10 YR 2/1 black pyrite Fe. S 2 10 YR 2/1 black (metallic) jarosite K Fe 3 (OH)6 (SO 4)2 5 Y 6/4 pale yellow todorokite Mn. O 4 10 YR 2/1 black humus 10 YR 2/1 black calcite Ca. CO 3 10 YR 8/1 white dolomite Ca. Mg (CO 3)2 10 YR 8/2 white gypsum Ca. SO 4× 2 H 2 O 10 YR 8/3 very pale brown quartz Si. O 2 10 YR 6/1 light gray
Low Value High Value high Chroma Low Chroma
Criteria for Characterizing Horizons Color Texture Density Structure Organic matter Mineralogy Chemistry
See the Teaching Assistants Before Leaving: Jon Demps Melissa Odal Grant Baysinger Daniel Kristiansen Markihe Anderson Percy Harvin Also anyone who has not received a student number
- Slides: 27