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Soils (week 1)

Soils Lecture

QuestionAnswer
Solum Horizon O, A, B - B layer has roots
Regolith Horizon O, A, B, C - what has been broken down into smaller minerals above bedrock - C layer is rarely touched
Soil air Atmospheric gasses 1. carbon dioxide 2. oxygen 3. nitrogen
Organic matter and biomass Biosphere - plants, animals, microbes, their products and remains
Soil particles Lithosphere - minerals in rocks, clay, sediments
Soil water Hydrosphere - water dissolved and substances are left
6 main roles of soils 1. physical support 2. affects flow of water 3. recycles material 4. habitat 5. affects atmosphere 6. engineering medium
what does physical support/growth do to soils - Supports plants and root structure - Supplies water, air, temperature control, nutrients - Protection from toxins - bind unwanted material so other plants can't get
What provides the main components for plants Macro- C02, H2O, O2, Ca, Mg, NH4, K, NO3, HPO4, SO4, SI3O Micro- Cu, Co, Fe, Mn, Ni, Na, Zn, Bo, Cl
How does hydrology affect soils - Bigger pores allow faster transportations and storage - a way to slow down or speed up the water flow through soil - like a sponge that will slowly release as the environment needs
how does the atmosphere affect soils decomposing matter in he soil releases CO2
how does soil recycle - used by decomposition - are needs to lack or low oxygen - cold temps and low oxygen slow decomposition
Pedosphere's 4 main components pore space (air and water) minerals 45% organic 5%
What does organic matter do - stabilizes soil - waters - nutrients - carbon is plant food
What holds the most water clay soil holds the most then sandy then silty
4 common issues within soil 1. erosion 2. salt accumulation 3. organic matter and nutrients depletion 4. oil spills
What happens to the pore pace of soils if heavy machinery is being used on it frequently the pore space will shrink more and more making it harder to absorb and hold water aswell as draining it through
Igneous rock composed of primary minerals formed from cooling magma bigger the dark spots, longer it took to cool
dark coloured rocks often contain iron and magnesium causing them to break down easier
intrusive rocks formed from magma that cools and solidifies within the crust of the planet. - small crystals
extrusive rock formed on the surface of the Earth from lava, which is magma that has emerged from underground. - small crystals
sedimentary rock produced from weathered materials from other rocks - collect and build up under water as it drips and reconsolidates
metamorphic rock other rocks that have changed in some way due to high heat and/or pressure
Physical weathering material breaks down to smaller sizes, but composition remians mostly the same
chemical weathering material releases soluble materials and/or changed composition
Physical weathering (temp) repeated cooling and heating results in expansion and contraction of the rocks and can break the rock if water gets into the cracks
physical weathering (abrasion) water movement over long periods windblown from sand and dust glaciers sliding off rocks
chemical weathering (hydration) water binds to a mineral, thereby changings the composition ex. 5Fe2O3+9H2O -> Fe10O15 x 9H2O
Chemical weathering (hydrolysis) water molecules split into H+ and OH- (H+ often replaces a cation) ex. KAlSi3O8 + H2O <-> HAlSi3O8 + K+ + OH-
Chemical weathering (dssolution) water dissolves the mineral Gypsum dissolving ex. CaSO4 x H2O + H2O <-> Ca+2Soa-2 + 4H2O
Chemical weathering (acid reactiooons) acid that can dissolve the rock ex. Calcite
Oxidation loses an electron
reduction gains an electron
Chemical reduction (complexation) - biological processes produce many acids - H+ solubilizes elements (ex. Al and Si) - organic reactions with elements (removing Al)
chemical weathering (oxidaion/reduction) the loss/gain of an electron may destabilize/change the crystal structure
Created by: Alyssa22122
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