Quiz 5 - Answers 1.)a.)List the five master horizons for describing soil profiles. O, A, E, B, C(2)...
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Transcript of Quiz 5 - Answers 1.)a.)List the five master horizons for describing soil profiles. O, A, E, B, C(2)...
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Quiz 5 - Answers1.) a.) List the five master horizons for describing soil profiles.
O, A, E, B, C (2)b.) What is an elluvial horizon?
Horizon in which there has been movement OUT (exiting) of clays, Fe, Al, O.M.; often designated master horizon=E
2.) For the profiles at the bottom of the page:a.) which soil formed in more than one parent material?
B: (2C) (2)b.) which soil has a transitional horizon?
A: (BC)3.) Name one diagnostic horizon and give a brief description of it.
(Table 3.1) examples: (2)Argillic: subsurface accumulation of high activity claysNatric: subsurface accumulation of high activity clays with >15% NaMollic: thick, dark colored, high B.S., strong structureUmbric: same as mollic, but low B.S.
4.) Which soil is the least weathered and which soil is the most weathered?Oxisols, Alfisols, Mollisols, Entisols, and Inceptisols.
Least: Entisols (2)Most: Oxisols
5.) What end products does Madison Metropolitan sewerage district produce?
+cleaned effluent (liquid) (2)+nutrient rich biosolids (solid)
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Soil Colloids : Chapter 8
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Primary Minerals
• Table 2.2 and Figure 2.4
• Remember definition of mineral– general adjective to describe inorganic materials derived
from rocks• ex: silicate clays
– specific noun to refer to distinct minerals found in nature• ex: quartz, feldspar
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Definitions
• colloids: organic and inorganic matter with very small particle size and a correspondingly large surface area per unit of mass
• silicate clay: colloid with Si in framework
• nonsilicate clay: colloid withOUT Si in framework
• humus: more or less stable fraction of the soil O.M. remaining after the major portions of added plant and animal residues have decomposed
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Definitions
• exchangeable ions:– cations: Al3+, Ca2+, Mg2+, K+, H+, Na+
– anions: Cl-, NO3-, SO42-
• crystal structure: the orderly arrangement of atoms in a crystalline material
• amorphous: noncrystalline
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Important Properties of Soil Colloids
• Size
• Surface Area
• Surface Charge
• Cation/Anion Exchange
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Four Major Types of Soil Colloids
• Inorganic– 1) crystalline silicate clays
– 2) non-crystalline silicate clays
– 3) Fe/Al oxides (non silicate clays)
• Organic– 4) humus
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Structure of Soil Colloids
• Silicate clays Fig 8.4
Building Blocks– tetrahedral
• 4-sided• 1 Si, 4 O
– octahedral• 8-sided• trioctahedral: 6O with 3 Mg2+
• dioctahedral: 6O with 2 Al3+
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Fig. 8.4
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Isomorphic Substitution
• Definition: the replacement of one atom by another of similar size in a crystal lattice without disrupting or changing the crystal structure of the mineral
• Table 8.2
• in tetrahedral sheets:– expected ions: Si4+
– potential replacement ions: Al3+, Fe3+
• in octahedral sheets:– expected ions: Al3+, Mg2+
– potential replacement ions: Al3+, Fe3+, Mg2+, Zn2+, Fe2+
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Structure of Soil Colloids
• Nonsilicate clays = Fe/Al Oxides– no Si– octahedral only (no tetrahedral)– little isomorphic substitution– small negative, sometimes positive charge
• Humus– noncrystalline– large organic molecule (C, O, H, N)– net negative charge– Fig. 8.13
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Genesis of Soil Colloids
• alteration
• decomposition and recrystallization
**parent material and weathering conditions**
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Soils: An Introduction (Singer and Munns)