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Facts

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2-D view of soil excavation. Profile is partitioned into soil horizons ... Ditching. Mechanical destruction of hardpans. Irrigation. Vegetation: ... – PowerPoint PPT presentation

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Title: Facts


1
THE DIRT ON FOREST SOILS (CHAPTER 5)
  • Facts
  • Trees require soil!
  • Soils affect forest composition productivity
  • Forests affect soil properties productivity

2
THE DIRT ON FOREST SOILS (CHAPTER 5)
  • Our Topics
  • 1. Soil forming factors
  • 2. Soil properties
  • 3. Forest soil influence on trees ( vice versa)
  • 4. Soil taxonomy (classification)

3
SOIL FORMING FACTORS
  • 1. Initial material (parent material)
  • 2. Climate
  • 3. Organisms
  • 4. Topography

4
SOIL MORPHOLOGY (PROFILE)
  • Soil Profile (see Figs. 5.1 - 5.3 in text)
  • 2-D view of soil excavation
  • Profile is partitioned into soil horizons
  • O fresh decomposing organic matter
  • A organic matter inorganic minerals (mixed by
    disturbance)
  • E mineral horizon that has lost clay, iron
    aluminum
  • B contains weathering products leached from O,
    A, and/or E horizons
  • C little affected by soil-forming processes
  • R hard bedrock

5
SOIL PHYSICAL PROPERTIES
  • Soil Color
  • Depends on
  • 1. Mineral composition (e.g., iron oxides ? red)
  • 2. Organic matter content (e.g., high ? black)
  • 3. Water drainage (e.g., poor drainage ? blue
    green)

6
SOIL PHYSICAL PROPERTIES (continued)
  • Soil Texture (see Fig. 5.4 in text)
  • Determined by proportions of
  • 1. Sand (2 mm - 0.05 mm diameter)
  • 2. Silt (0.05 mm - 0.002 mm)
  • 3. Clay (lt0.002 mm)

7
SOIL PHYSICAL PROPERTIES (continued)
  • Soil Texture (see Fig. 5.4 in text) influences
    (e.g.)
  • Soil structure
  • Aeration
  • Water retention drainage
  • Nutrient supply
  • Root penetrability seedling emergence

8
SOIL PHYSICAL PROPERTIES (continued)
  • Soil texture influences forest species
    composition
  • E.g., sandy soils tend to have trees with low
    moisture nutrient requirements (e.g., pines,
    hemlocks, some oaks)
  • E.g., silt/clay enriched soils tend to have trees
    requiring abundant moisture nutrients (e.g.,
    Douglas-fir, black walnut, some oaks)

9
SOIL PHYSICAL PROPERTIES (continued)
  • Soil Structure (see Fig. 5.5 in text)
  • Determined by arrangement of particles into
    peds
  • Peds classified by
  • 1. Size
  • 2. Shape
  • 3. Degree of distinction

10
SOIL ORGANIC MATTER
  • Originates from
  • Litter (via decomposition)
  • Fine roots (via death decomposition)
  • Improves structure
  • Increases porosity and aeration
  • Dampens temperature fluctuations
  • Energy source for microbes
  • Increases moisture-holding capacity
  • Source of plant nutrients

11
SOIL ORGANIC MATTER (continued)
  • Forest operations affect soil organic matter!
  • Examples
  • Shelterwood harvest vs. clearcut harvest
  • Remove entire stem vs. remove only merchantable
    portion of stem
  • Leave organic debris vs. remove organic debris
    following pruning or thinning
  • Prescribed burn vs. no burn

12
SOIL WATER
  • Serves as nutrient solvent (for transport)
  • Important for
  • Consistency
  • Aeration
  • Temperature
  • Microbial activity
  • Concentrations of nutrients toxic substances
  • Soil erosion
  • Influences distribution composition of
    vegetation
  • Rarely optimum

13
SOIL WATER (continued)
  • Available Water
  • Water that can be absorbed by plant roots
  • Influenced by
  • Precipitation
  • Vegetative demand
  • Soil properties, which affect, e.g.
  • Runoff
  • Soil storage and drainage

14
SOIL WATER (continued)
  • Forest operations affect soil water!
  • Ditching
  • Mechanical destruction of hardpans
  • Irrigation
  • Vegetation
  • Establish vegetation (plants remove soil water)
  • Species choice (may either increase or decrease
    soil water)
  • Thinning (increases soil water)
  • Herbicides for weed control (increases soil water)

15
SOIL ORGANISMS
  • Decompose organic matter (which makes nutrients
    available for plants)
  • Incorporate organic matter into soil (which
    improves soil properties)

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16
SOIL ORGANISMS (continued)
  • 1. Roots
  • 2. Mycorrhizae
  • 3. Fungi
  • 4. Bacteria
  • 5. Protozoa
  • 6. Algae
  • 7. Animals (e.g., earthworms, insects)

17
SOIL CHEMICAL PROPERTIES
  • Soil pH
  • Definition
  • pH ? negative logarithm of hydrogen ion
    concentration
  • Numerical scale 1-14
  • Acidic if lt7 (common in forest soils)
  • Basic (alkaline) if gt7
  • Exactly 7 neutral
  • Soil pH important for
  • Health of microbial populations
  • Nutrient availability for plants

18
SOIL CHEMICAL PROPERTIES (continued)
  • Cation Exchange Capacity (CEC)
  • Cations ? positively charged ions (e.g., Ca2)
    many are forms of plant nutrients
  • CEC ? soil ability to adsorb and release cations
  • CEC depends on
  • Soil organic matter (mostly negatively charged
    increases CEC)
  • Amount and type of clay (e.g., CEC low in sandy
    soils)
  • Soil pH

19
SOIL NUTRIENT DEFICIENCIES
  • Nutrient deficiencies detected by
  • 1. Visual plant (tree) symptoms
  • 2. Soil analysis
  • 3. Plant tissue analysis
  • Beware of visual symptoms!
  • Nutrient deficiency symptoms may mimic those of
    disease, insect, or moisture deficiency
  • Soil or plant tissue analyses necessary for
    definitive diagnosis

20
FOREST FERTILIZATION
  • Reduces nutrient deficiencies
  • Increases
  • Insect disease resistance
  • Aesthetic appearance
  • Costs
  • Fiber yield (and so net profit)
  • Environmental pollution
  • Usually uses non-renewable resources
  • Changes soil properties
  • Municipal industrial wastes can be used
    (reduces environmental pollution)

21
SOIL SURVEYShttp//soils.usda.gov/survey/how_to/
  • Soil survey reports contain
  • 1. Soil maps
  • 2. Soil descriptions
  • 3. Soil use and management
  • 4. Soil formation and classification
  • 5. Laboratory data
  • 6. Other general information

22
SOIL SURVEYS (continued)
  • Soil survey reports used for, e.g.
  • 1. Matching planted tree species to soil type
  • 2. Evaluating impacts of proposed uses
  • 3. Predicting water yield and quality
  • 4. Planning recreational facilities
  • 5. Road location design
  • 6. Matching harvest methods to soil conditions

23
SOIL TAXONOMY (CLASSIFICATION)
  • Seven Hierarchical Levels of Soil Classification
    (in U.S.)
  • 1. Order (e.g., Ultisols, Alfisols, Spodosols)
  • 2. Suborder
  • 3. Great group
  • 4. Subgroup
  • 5. Family
  • 6. Series
  • 7. Type (most specific category)

24
INFLUENCE OF FOREST OPERATIONS ON SOIL QUALITY
  • Example 1 Nitrogen Balance(will be
    shown/discussed in class)

25
INFLUENCE OF FOREST OPERATIONS ON SOIL QUALITY
  • Example 2 Soil Erosion
  • Erosion can be caused by, e.g.
  • Recreation
  • Road building
  • Timber harvesting
  • Site preparation (creation of favorable
    conditions for tree planting initial growth)
  • Prescribed burns
  • Chemical treatments
  • Mechanical treatments
  • Combinations of the above
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