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Geology: Soil Formation, Composition and Conservation

Prentice Hall

AB
HUMUSDecayed plant &animal remains
SUBSOILSoil layer made of clay & particles
DECOMPOSERSOrganisms that break down organic waste.
BEDROCKLayer of rock beneath the soil
TOPSOILDark brown soil mix of humus,clay&minerals.
LOAMSoil from clay sand and silt.
SOIL HORIZONsoil layer that differs from the layers around it.
SOILthe surface material in which plants can grow; one of Earth's most valuable resources.
LITTERLeaves or other plant material on top of the soil.
A HORIZONThe top layer of soil, where humus and eroded rock are mixed, forming "Top soil"
B HORIZONDevelops as rainwater washes clay and minerals from A horizon to B horizon.
C HORIZONBedrock (parent rock) weathers and breaks into soil particles.
SOIL TEXTURERanges for Gravel to sand to sitl and finally clay.
SOIL COMPOSITIONH2O 25%, Air 25%, Silt 18%, Sand 18%, Clay 9%, and Organic matter 5%.
DESERTIFICATIONthe advance of desert-like conditions onto areas that were once fertile.
SODThick mass of tough roots at the surface of soil that helps to keep soil in place and hold moisture
DUST BOWLSouthern Plains States that lost their topsoil from 1930 -1938 due to drought
SOIL CONSERVATIONThe management of soil to prevent its loss or destruction
CONTOUR PLOWINGSlows runoff and erosion by plowing along the curves of hills
CONSERVATION PLOWINGdisturbs the soil and plant cover as little as possible
CROP ROTATIONImproves the fertility of soil by groving different crops and sometimes leaving the land fallow (unplanted)
LAND RECLAMATIONrestoring lands for agriculture, lands from mining, or habitats for wildlife

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