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

17
Q

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

18
Q

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

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

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.

24
Q

precursor of iron oxides

A

ferrihydrite

25
allophanes, imogolite minerals; acid to neutral (andosol); lighter colour; on rhyolitic to andesitic tephra
silandic
26
al-humus complexes; extremely acid to acid; blackish colour (andosol); on basaltic tephra
aluandic
27
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.
spodic
28
light colored material due to eluviation in the horizon
albic
29
soft horizon with concretions of Fe oxides
plinthic
30
horizon consisting of hard concretions (nodules) of Fe oxides
pisoplinthic
31
horizon that is a continuous hard layer due to Fe oxides
petroplinthic
32
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.
plinthite
33
removal of Na+ from exchange sites and subsequent dispersal and leaching
solodization
34
hydromorphic soil forming process, reduction and oxidation phase; process can lead to clay mineral transformation
ferrolysis
35