S3W2 Definitions Flashcards

(28 cards)

1
Q

10 Key points for soil protection

A
  1. Knowledge, soil is a 3D body, sphere interactions
  2. Precations for protections
  3. Soil monitoring, health of soils, responses to laws
  4. Remediate polluted soils
  5. Soil as common ground, shared responsibility
  6. Integrity ensured by legals standards
  7. Corporate mandates to improve institutions
  8. All actors involved
  9. Spatial planning, agriculture, forestry especially
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2
Q

Legislations of the EU

A
  • New European Soil Strategy for 2030 + New Soil Monitoring law
  • not as strong as once intended
  • 60% of EU soil unhealthy
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3
Q

Legislations in CH

A
  • USG 1983
  • VSBo 1986
  • VBBo 1998
  • new versions, new defintions for pollutants
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4
Q

Strategy Soil 2020 CH

A
  • recognizes diff. Soil Functions, not just as a place to grow food
  • preserve soil Functions
  • FOEN, ARE, FOAG, federal & cantonal
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5
Q

6 objectives of Strategy Soil 2020

A
  1. Reduction of soil consumption, thr. land planning
  2. Consideration of SF in spatial planning, not sealing fertile soil
  3. Protection against damage, pollutants, erosion
  4. Restoration of degraded Soils, actively put OM on soil
  5. Awareness of value & vulnerability of soil
  6. Strengthening international engagement, Import/Export affected, Telecoppling Effects
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6
Q

Reserach, Institutes, Implementaton of Soil Science in CH

A
  • Universtiteis
  • Agroscope: agricultural research & solutions
  • WSL: forest soils
  • BLW: agriculture
  • BAFU: Soil, Biotechnology
  • Cantons: soil protection agencies
  • Private/engineering offices: construction supervisors, BBB
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7
Q

what is Centre KoBo?

A
  • National Centre of Competence for Soil
  • improve basis for Implementation measures, promoting sustainable use & effective Protection
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8
Q

Tasks of KoBo

A
  • make a Map of CH Soils
  • standardize/improve Methods of surveying Soil
  • define technical standards for Soil Mapping
  • Providing methods for evaluation SF & threats
  • national info for all actors
  • promoting interdisciplinary between actors
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9
Q

SF/T in Meadows

A
  • Restoration of Pastures (Weidefläche)
  • Erosion on steep areas
  • Preventing overgrown areas
  • high Biodiversity of herbs & bushes
  • Long roots of vegetation keep dying, continous OM in Soil
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10
Q

Unofficial Soil Definitions

A
  • living, breathing skin of Planet
  • any loose material on surface of Earth that is capable of supporting life
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11
Q

Definition of Soil

A

Surface component of Earth that developed from..
- geolog. materials of the lithosphere
- dead biomass from biosphere
- and by phys, chem, bio processes

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12
Q

Terms of Non-Soil Material

A

Sediment: displaced soil without in situ Formation
Regolith: weathered rock without bio. influence, no OM
Coal/Peat: biogenic sediments, grows ontop of Soil the dies, environment too wet & no mineral input

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12
Q

Top & Bottom development of Soil

A

Weathering of parent rock, crushing, chem conversion
Settlement of plants, build up of OM, bio & chem reactions

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13
Q

Components of Pedosphere

A

=> Abb. Folie 26
- includes Litter, Topsoil, Subsoil
- does not include Hydrosphere, Lithosphere
- does not include Biosphere (moss layer, trees), but Biosphere does include all of Pedosphere

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14
Q

Environmental Conditions of Pedosphere

A
  • sharp temp. fluctuations
  • low to very high relat. humidity
  • complete darkness to full light
    => subdivided into Humidity, Light, Temperature, Plant Biomass, Microorganism Biomass
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15
Q

Subdivided EC of Pedosphere

A

Humidity: reaches max. on Topsoil
Temp: increases at Surface, ideal conditions for Plants
Light: slow to steep increase on surface
Plant biomass: peak in Topsoil thru. roots
Microorganism biomass: Peak like Plant biomass, degrade dead biomass

16
Q

Terms of Soil Structure

A
  • Horizons: diff. parts of Soil, no OM layer/bedrock, all horizons = Solumn
  • Soil group/type/unit: same horizon sequence, characteristics, not neces. same bedrock
17
Q

Soil (horizon) formation Processes

A
  • Weathering
  • Mineral formation: Iron 2 to oxygen & Iron 3
  • Decomposition of litter, Humus formation
  • Microstructure formation
  • Material transfer
18
Q

Bsp of Solumns

A
  • Bleached horizon thru. leeching
  • microorganisms good at degrading OM when O2 available, otherwise accumulation
    => Soil is continous, new formation/change thru. washing out minerals, erosion, etc
    => Classification can be difficult
19
Q

Terms of other Soil Units

A

Elementary Soil unit: Pedon, 1-10^2m, 0.5-2m depth
Verical pit: Soil Profile
Polypedon: multiple Pedons

20
Q

Soil Composition

A
  • solid, liquid, gaseous Phase
  • 46% Minerals, 4% OM, 25% Water, 25% Air
  • large & varied reactive surface areas, small particles, exchange & reactions
  • Clay, Silt, Sand, Stone, Earthworm & wall (excreting substances), Roots, water filled pores, air filled pores
21
Q

Inhabited Soil Pores

A
  • habitat for soil organisms (Edaphon)
  • Fine pores <2nm: unhabited, too small
  • Medium pores 0.2-10nm: bacteria, fungi, algae, root hairs, etc
  • Coarse & secondary pores > 10nm: roots, nematodes, mites, etc
21
Q

Soil Factors that lead to forming processes

A

S = f(G, C, T, O, A) * Z
G: Geology
C: Climate
T: Topography
O: Organism
A: Anthropogenic
Z: Time

22
Q

Timestamps of soil formation processes

A

Geology - Climate - Organisms - Topography - Soil
=> Abb:
1. Parent material with moss
2. C horizon, OM, broken rock, mineral fragments
3. C horizon, A horizon, OM
3. C horizon, B horizon, A horizon, stored carbon, OM

23
Anthropogenic soil Factor
- direct impact on all other factors - ploughing soil, modification of nutrients, roads, etc
23
Zonal soils
- climate & vegetation determine development - cold climate = bad OM decomposition, little microorganisms
24
Intrazonal & Azonal soils
Intra: differentiation within climate zones due to specific influences of relief, water balance, bedrock, age Azonal: young soils without characteristic profile
25
Formation of Catenas
- horizontal profile of Soils - hills with indentation in middle - erosion on side causes accumulation at bottom - better soil formation on other hill