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Delineating Soil Horizons. Soil as a Natural Body Parent Material Bedrock Additions Losses Translocations Transformations Differentiation Bedrock.

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Presentation on theme: "Delineating Soil Horizons. Soil as a Natural Body Parent Material Bedrock Additions Losses Translocations Transformations Differentiation Bedrock."— Presentation transcript:

1 Delineating Soil Horizons

2 Soil as a Natural Body Parent Material Bedrock Additions Losses Translocations Transformations Differentiation Bedrock

3 Soil Horizons Roughly parallel layers in the soil with varying composition and properties

4 Master Horizons

5 Criteria for Characterizing Soil Horizons ColorTextureDensityStructure Organic matter MineralogyChemistry

6 Soil Color

7 Mineralogy of the soil/parent material Relative amount of organic matter Hydrology of the soil Soil chemistry Soil Microbes Soil Color Determinants

8 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

9 Soil Color Determination

10 Value Chroma Hue Munsell Soil Color 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. related to total amount of light reflected. measure of the strength of spectral color

11 0 2.5YR 5YR 7.5YR 10YR 0 2.5 Y 5Y 10R

12 Hue 10 R 2.5 YR 5 YR 7.5 YR 10 YR 2.5 Y 5 Y RedYellow Increasingly dominated by yellow spectral color Pages Florida soils dominated by 7.5 YR and 10 YR pages

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15 Soil Color

16 Hue = 10 YR Value = 6 Chroma = 3 Munsell Color 10 YR 6/3

17 10 YR 2/1 10 YR 5/6

18 Pale Red Red Weak Red light Red Pink Dark Red

19 Summary A horizon – mid/low value - low chroma E horizon – high value - low chroma B horizon – ? value - ? chroma

20 Water table depth Oxygen status Development decisions

21 Hue 10YR or Yellower Value≤ 3 Chroma ≤ 1 Hydric Soil Classification “Black Histic”

22 MineralFormulaSizeMunsellColor goethiteFeOOH(1-2 m m)10YR 8/6yellow goethiteFeOOH(~0.2 m m)7.5YR 5/6strong brown hematiteFe 2 O 3 (~0.4 m m)5R 3/6red hematiteFe 2 O 3 (~0.1 m m)10R 4/8red lepidocrociteFeOOH(~0.5 m m)5YR 6/8reddish-yellow lepidocrociteFeOOH(~0.1 m m)2.5YR 4/6red ferrihydriteFe (OH) 3 2.5YR 3/6dark red glauconiteK(Si x Al 4- x )(Al,Fe,Mg)O 10 (OH) 2 5Y 5/1dark gray iron sulfideFeS 10YR 2/1black pyriteFeS 2 10YR 2/1black (metallic) jarositeK Fe 3 (OH) 6 (SO 4 ) 2 5Y 6/4pale yellow todorokiteMnO 4 10YR 2/1black humus 10YR 2/1black calciteCaCO 3 10YR 8/1white dolomiteCaMg (CO 3 ) 2 10YR 8/2white gypsumCaSO 4× 2H 2 O 10YR 8/3very pale brown quartzSiO 2 10YR 6/1light gray

23 Low Value Low Chroma Low Value high Chroma High Value

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25 Criteria for Characterizing Horizons ColorTextureDensityStructure Organic matter MineralogyChemistry

26 Jon Demps Melissa Odal Grant Baysinger Daniel Kristiansen Markihe Anderson Percy Harvin See the Teaching Assistants Before Leaving: Also anyone who has not received a student number

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