340-349 Flashcards

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1
Q

soil texture

A

relitive poroportions of diffferent sized inorganic minerl particles of sand. silt, and clay

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2
Q

sand

A

largest soil particles (0.05 to 2mm in diameter)

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3
Q

silt

A

meddium sized particles (0.002 to 0.05 mm in diamiter)

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4
Q

clay

A

small partilces (less than 0.002 mm in diamiter)

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5
Q

ions

A

charged forms of soil minerals

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6
Q

loam

A

ideal agricultural soil, combo of different soil particle sizes

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7
Q

soil acidity

A

(pH) affects plants from nutrients mineral varies in deffernt Ph’s. optimum: 6.0 to 7.0

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8
Q

soil taxamony

A

classification fo soils into 12 orders, and each order into many different series

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9
Q

spodosols

A

from places with colder climats, amplle ercipitation, and good drainage. not food farmland because too acidic and nutrient poor because of leaching

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10
Q

alfisols

A

from temperate decidiuos forsts.

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11
Q

mollisols

A

from temperate, semiarid, and fertile soils. grows worlds grain crops

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12
Q

aridosols

A

from arid regions of all continents. provides rangeland for grazing animals, crops may be grown if water is supplys for irrigation

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13
Q

oxisols

A

low in nurtient minerals, exist an tropical and sub tropical areas with ample percipotation. thigs decompse very quickly

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14
Q

substainable soil use

A

the wise use of soil resources, without a reduction in the amount of ertility in the soil, so that it is productive for future generaitons.

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15
Q

soil erosion

A

the wearing away or remmoval of soil from the land

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16
Q

soil erosion in the USA

A

water erosion is severe across the midwestern grain belt. soil erodes 25% quicker then natural processes can replace it

17
Q

salinization

A

gradual accumulation of salt in soil, often as a result of improper irragation methods

18
Q

desertification

A

degradation of once fertile rangeland, agriculteral land, or tropical dry forest into nonproductive desert