qualifiers Flashcards

1
Q

> 2/3 recognizable plant tissue

A

fibric

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2
Q

hemic

A

<2/3 recofnisablie plant tissue & > 1/6 recognizable plant tissue (medium)

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3
Q

<1/6 recognizable plant tissue

A

sapric

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4
Q

base saturation higher then 50%

A

eutric

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5
Q

base saturation lower then 50%

A

dystric

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6
Q

by adding organic material such as excrements and kitchen refuse mixed into the
natural soil; high animal activity; result deep cultivation, intensive fertilization & applicationn organic waste

A

hortic

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7
Q

by adding organic material such as charcoal, ash, plant residues, bones & kitchen refuse; limited animal activity (Terra Preta de Indio = Amazon dark earths)

A

pretic

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8
Q

by adding and mixing mineral material such as carbonate rich sea sand or limnic sediments into the natural soil; cultivation in raised beds

A

terric

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9
Q

by adding sods of grass/herbs/shrubs taken from other places, mixed with manure and ash; mainly in sandy soils

A

plaggic

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10
Q

by accumulation of sediments from irrigation water; pronounced higher silt and clay content in topsoil (irrigated)

A

irragric

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11
Q

soils under paddy cultivation; relative dense pan allowing water to transport reduced Fe and Mn to the subsoil (rainfed)

A

hydragric

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12
Q

soils under paddy cultivation; puddling under waterlogged conditions creates dense plough pan allowing irrigation water to stagnate (rainfed)

A

anthraquic

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13
Q

without contact with other soils/ fine earth fraction

A

isolatic

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14
Q

perenniaally frozen layer (visible ice or, if not enough water, <0°C)

A

cryic

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15
Q

unfrozen (noncryotic) soil and rock

A

talik

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16
Q

massive body of ground ice, leads to deformation of the ocerlying soil an rock

A

pingo

17
Q

subsurface layer with distinctly higher clay content than the overlying layer and/or presence of illuvial clay; high content of exchangeable Na+

A

natric

18
Q

stagnant water for a period long enough to let reducing conditions occur

A

stagnic

19
Q

polished and grooved aggregate surfaces

A

slickensides

20
Q

constant churning; cracks that open and close periodically

A

peloturbation

21
Q

hearing of the underlying material to the surface creating a micro relief

A

gilgai relief

22
Q

if >=5% glasses in sand and coarse silt fractions; lower degree of weathering; glassy aggregates & other glass coated primary minerals

A

vitric

23
Q

active Al and Fe materials, having the lowest bulk density
(≤ 0.9 kg.dm-³) among mineral soils, high anion exchange capacity, high contents of organic matter and ferrihydrite and high plant-available water capacity.

A

andic

24
Q

precursor of iron oxides

A

ferrihydrite

25
Q

allophanes, imogolite minerals; acid to neutral (andosol); lighter colour; on rhyolitic to andesitic tephra

A

silandic

26
Q

al-humus complexes; extremely acid to acid; blackish colour (andosol); on basaltic tephra

A

aluandic

27
Q

subsoil horizon where organomineral complexes have been accumulating. This is as a consequence of strong acidity dus to intruding of organic acids of the surface layer. Organic matter in upper part & Fe oxides spread over a higher depth range.

A

spodic

28
Q

light colored material due to eluviation in the horizon

A

albic

29
Q

soft horizon with concretions of Fe oxides

A

plinthic

30
Q

horizon consisting of hard concretions (nodules) of Fe oxides

A

pisoplinthic

31
Q

horizon that is a continuous hard layer due to Fe oxides

A

petroplinthic

32
Q

an iron-rich, humus-poor mixture of kaolinitic clay with quartz and other constituents that changes irreversibly to a hardpan or to irregular aggregates on exposure to repeated wetting and drying.

A

plinthite

33
Q

removal of Na+ from exchange sites and subsequent dispersal and leaching

A

solodization

34
Q

hydromorphic soil forming process, reduction and oxidation phase; process can lead to clay mineral transformation

A

ferrolysis

35
Q
A