7: Composition of the Solid Phase Flashcards
What can parent material be made out of?
Igneous, metamorphic, and sedimentary rocks
Weathering
A process of transformation that involves the destruction of the parent material and synthesis of new minerals in the soil
Physical and chemical weathering
Physical (mechanical) weathering
Breakdown of rock without changing chemical composition
Main agents are temperature, abrasion, and plants/animals
Chemical weathering
Chemical transformation of the soil minerals through the action of geological agents and organisms.
Main agents are geological (oxygen, water) agents and organisms
Igneous rocks
Granite and basalt
What are the minerals in granite and how do they affect the soil once weathered?
Quartz: resistant to weathering and doesn’t contain minerals
Feldspars and muscovite: more easily-weathered but still contain few nutrients
Soils derived from granitic rock are coarse-textured and have low fertility
What are the minerals in basalt and how do they affect the soil once weathered?
Dominated by small-grained, easily weathered, nutrient-rich minerals including hornblende, augite, biotite.
Parent materials and soils derived from basaltic rock are fine-textured and fertile
Sedimentary rocks
Sandstone, limestone, and shale
Compacted or cemented particles weathered from any type of preexisting rocks. Resistance to weathering depends on dominant minerals and cementing agent.
Silica: high resistance
Calcite-containing rocks: least resistant
Sandstone and how it affects soil
Sand-sized particles translocated and deposited by water. Cemented by pressure and CaCO3 or SiO2.
Coarse-textured soils with low fertility
Shale and how it affects soil
Clay particles translocated and deposited by water and compacted. Shale rock susceptible to weathering.
Fine-textured, relatively fertile soils
Limestone and how it affects soil
Mainly formed in shallow oceans where CaCO3 accumulates and is cemented.
Easily weathered, and soil formed is fine-textured, have a neutral to basic pH, and high fertility
Metamorphic rocks
Formed when rocks are subjected to high heat, pressure, or hot mineral-rich fluids (or any combination of these factors)
Usually more resistant to physical weathering
Soil organic matter (OM)
Mixture of all plant, animal, and microbial organic components of the soil at a given time.
Transitions from biomass to detritus to humus, which has the organic colloids