formation, human interactions, biology, and natural disasters by kate edwards, tyler huntley, kerry...
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![Page 1: Formation, human interactions, biology, and natural disasters By Kate Edwards, Tyler Huntley, Kerry Malm and Brian Murtaugh](https://reader036.vdocuments.net/reader036/viewer/2022062314/56649d375503460f94a0ff8b/html5/thumbnails/1.jpg)
formation, human interactions, biology, and natural disasters
By Kate Edwards, Tyler Huntley, Kerry Malm and Brian Murtaugh
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Introduction
• What is Australasia• Wide range of soil formation and
orders• Specific soil formations in New
Zealand
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Introduction
• Acidic soils in Australia• Dipterocarp forests throughout the region• Natural Disasters in Indonesia
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The Formation of Raw Volcanic Soil in New
Zealand
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Tongariro Volcanic Center
• Located on New Zealand’s North Island.
• Raw volcanic soil dominates the landscape which is formed in tephra also know as volcanic ash.
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Time and Parent Material
•Time: Raw volcanic soils are a very heterogeneous group of soils and are extremely young.
•Parent Material: Tephras of rhyolite, dacite and andesite
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Climate and Topography
• Climate: Cold and high rainfalls.
• Topography: Raw volcanic soil forms in the vicinity of the source volcano
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Biota• Organisms: Most soil animals and
micro-organisms are concentrated in the topsoil.
• Plant Life: Vegetation rapidly recovers on volcanic soils.
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Profile Characteristics• A horizon: is dark
in color• B horizon:10-
15cm thick• C horizon: is pale
yellow-brown
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Distinguishing features of Raw Volcanic Soils
• Naturally low levels of organic matter • Generally coarse in texture• Weakly weathered• Highly susceptible to erosion• Low bulk density • Well drained, very high macroporosity
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Acidic Soils of Australia
Tyler Huntley
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Acidic Sulfate
• Where: SE SW Australia• Acid Subsoils 23 million
hectares in Aus.• 1/3 of Aussi covered• Acid sulfate soils once
made up the sea floor, • Geologically • pH levels
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Agricultural
• Increase in acidification
• Soil nutrient uptake
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Construction
• corrode metal pipes and dissolve concrete.
• foundations of buildings
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Surface Water
• Run-off• Consequences
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Prevention
• Identifying them
• Liming
• Loss of crop production
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Lowland Dipterocarp forests
Soil associations
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General Background
•Where: South East Asia
•Climate: very warm temperatures
•Growth: year round
•Use: timber industry, land degradation issues
•Stand characteristics: uneven aged, multi-layered
•Soils: strongly acidic, infertile, vulnerable to surface erosion
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Types of Soils
• Ultisols – most common in SE Asia• Inceptisols
– Very steep slopes
• Oxisols• Characterized by
– Morphology– Physiochemical properties– Clay mineralogy
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Soil Textures
• Primary factor for vertical distribution and storage of C, N, and P
• Coarse - clay content <35%– Thicker A and E horizons
• More roots and animals• Larger volume of coarse pores
• Fine – clay content >50%– Mostly kaolinite
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Soil Horizons
• Typically A, Ag, Eg, E, Bt or Btg, Bg & C
• No O layer– termites
• A Horizon– 5 cm thick
– Grayish with mottles edged with thin layers of iron oxide
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Soil Horizons
• E Horizon– 3-60 cm thick– Grayish and rust colored mottles– Clay coated in finer soils– Lower limit of major root penetration and
animals
• B Horizon– Argillic (shallower in fine soils)
• C Horizon
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Upper Horizons:Mechanical composition, bulk
density and porosity
• Clay eluviation and illuviation in every soil– Usually in fines
• Bulk density increases with depth
• Higher % coarse pores at surface
• Higher % total pore space at surface
• Water holding capacity correlated with total porosity
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Upper Horizons:Nutrient Cycling
• Highest storage of total C, N and P in the 0-150 cm of soil
– Increase with amount of clay
• Same with available N• Sandy soils
– Large amt of C, not N
• Exchangeable Mg and K correlated with clay• AMOUNTS STILL VARY GREATLY, EVEN
WITH SIMILAR CLIMATE AND VEG
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Charismatic Mega Fauna
• Philippine Eagle• Flying lemur• Tarsier• Philippine Cockatoo• Flying foxes• Bats• Reptiles and
amphibians
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Landslides in Indonesia
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Indonesia
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Climate
• Tropical climate
• Dry season June-September
• Wet season December-March
• Moderate temperatures
• Large range of annual rainfall
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Topography
• Indonesia has a wide range of topographic features
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Vegetation
• Tropical plants
• Flowering plants
• Many trees
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Soils
• Andosol (Andisols)– Very fertile– Used for horticulture and plantations
• Regosols (Inceptisols)– Quartz sand not suitable for dry-land farming
• Grumosols– High Ca & clay content– Used for crops in lowlands
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• Latosol– Tropical rainforests
• Lateritic– Tropical– High Al & Fe oxides
• Hydromorph (Oxisols)
• Alluvial
• Podsol– Highly leached– Coniferous forests
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What is a landslide?
• Material moving down a slope due to gravity
• Many possible triggers
• Look like an avalanche
• 3 types– Slump– Flow– Lahar
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IndonesiaMt. Semeru
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Conclusion
• The soils of New Zealand’s Central North
Island is mostly volcanic in origin
• Farmer’s crop yields are limited by the
acidity of the sub soils in SE/SW Australia
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Conclusion
• Subsoils are as important as topsoil in
tropical Ultisols
• Tropical and volcanic soils in combination
with precipitation leads to more frequently
occurring landslides