Site degradation Flashcards

1
Q

Typical chars of bc soils

A
  • Forest soils have developed since last ice age +/- 10,000 years • In BC mostly from glacial till
  • Physical, chemical, biological processes altered the parent material (+/- 1m) and turned it into soil
  • Typical rooting depth 60 cm or less
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2
Q

Compaction vs puddling

A
  • Compaction is an increase in soil density from applied forces (weight and vibration)
  • Puddling is the destruction of soil structure and loss of macropore space (when soil is wet)
  • Compaction lasts a long time (20+ years) • Can cause regeneration delay (50% > density = 25% less growth)
  • Increased surfaced erosion
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3
Q

What soil chars effect compaction?

A
  • Coarse fragment content
  • Texture
  • Soil Density
  • Soil Moisture
  • Humus thickness
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4
Q

What is displacement (aka scalping)

A
  • Moving or burying of productive soil
  • Caused by blading or stump removal during trail construction
  • Occasionally by cable yarding
  • Why a problem?

– Exposes poorer denser soils – Buries productive topsoils – More susceptible to erosion

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5
Q

What soil type is at highest risk of compaction?

A

Silt loam or silty clay loam

High clay actually resists compaction in some cases

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6
Q

What is surface erosion?

A

Loss of soil through water transport

  • Natural forest soils rarely have overland water flow except in streams and gullies
  • Compaction can cause overland water flow by damaging the infiltration capacity of the soil
  • Compacted areas with exposed mineral soils become a major source of sediment
  • Water is intercepted by road cuts and ditches
  • Fill slopes are often over steepened and supported by wood
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7
Q

What are most forestry wasting events resultant of?

A

Roads

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8
Q

Where is the most productive part of the soil horizon?

A

Top 30 cm

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9
Q

When is wasting considered to cause more risk?

A
  • Proximity to streams
  • Slope steepness
  • Low soil permeability
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10
Q

What are some strategies to avoid degradation?

A
  • Road design
  • Layout and boundaries – Good deflection – Windfirm boundaries – Riparian reserves
  • Yarding – Control debris (streams) – Time of year (dry soils)
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11
Q

What are some strategies to avoid deg on backspar trails?

A
  • Leave forest floor intact
  • Don’t excavate; or plan to rehabilitate
  • Minimise trail width • Cut stumps low to avoid digging
  • Outslope trails, waterbars
  • Avoid wet areas
  • Use lots of slash and remove later
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12
Q

What are some road design tactics to reduce wasting on poor soils or steep slopes

A

Full bench cut and end haul to eliminate placement of fill on slope or running surface.

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13
Q

Some plant indicators of instability?

A

Skunk cabbage, sedge, Indian hellebore, Devils club.

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14
Q

How can skidding damage be mitigated?

A
  • Designate Skid trails!!! – On moderate sites – Where multiple entries
  • Use low ground pressure machines
  • Skid when soil is dry or frozen
  • Run machine on slash • Keep blade up
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15
Q

How can deg be minimized during mechanized harvesting

A
  • Minimize number of passes
  • Avoid wet areas
  • Use slash
  • Dry or frozen soil conditions
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16
Q

What is soil degradation?

What are some results?

A

• Definition - A reduction in the long-term soil productivity by management practices

– Causes lower forest productivity – Reduced water quality – Damage to fish and wildlife habitat – Reduced visual quality

• It is loss within the net area to reforest (i.e. not permanent access structures)