Principles of Soil Science - Modules 1, 2, and 3

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Comprehensive practice flashcards covering fundamental soil concepts, soil formation and development, and physical properties of soils.

Last updated 10:56 AM on 9/3/26
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35 Terms

1
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What are the two primary approaches used in the study of soil, and how do they differ?

The pedological approach considers soil as a natural body with emphasis on its origin, characterization, and classification. The edaphological approach considers soil in relation to practical uses, particularly how soil properties affect plant growth.

2
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What are the volumetric proportions of the four major components in an ideal soil for plant growth?

An ideal soil consists of 45%45\% mineral matter, 5%5\% organic matter, 25%25\% water, and 25%25\% air by volume.

3
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<p>Which volumetric breakdown of major soil components is depicted in this diagram?</p>

Which volumetric breakdown of major soil components is depicted in this diagram?

It shows an ideal soil composed of 50%50\% solid materials (45%45\% mineral material and 5%5\% organic material) and 50%50\% pore space (25%25\% air and 25%25\% water).

4
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What are the typical concentrations of the main gases found in soil air?

Soil air is composed largely of elemental nitrogen (78%78\%), oxygen (20%20\%), carbon dioxide (0.5%0.5\%), and traces of other gases.

5
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What are the 16 essential nutrient elements required for normal plant growth?

The 16 essential elements are carbon (CC), hydrogen (HH), oxygen (OO), nitrogen (NN), phosphorus (PP), potassium (KK), calcium (CaCa), magnesium (MgMg), sulfur (SS), iron (FeFe), copper (CuCu), zinc (ZnZn), manganese (MnMn), boron (BB), molybdenum (MoMo), and chlorine (ClCl).

6
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Which 9 essential elements are categorized as macronutrients?

The macronutrients are carbon (CC), hydrogen (HH), oxygen (OO), nitrogen (NN), phosphorus (PP), potassium (KK), calcium (CaCa), magnesium (MgMg), and sulfur (SS).

7
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What is Hans Jenny's (1941) mathematical equation representing the factors of soil formation?

The equation is S=f(CL,LO,R,P,T)S = f(CL, LO, R, P, T), where SS represents soil properties, CLCL represents climate, LOLO represents living organisms, RR represents relief, PP represents parent material, and TT represents time.

8
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What are the eight most abundant chemical elements in the Earth's crust by percentage weight?

They are oxygen (46.6%46.6\%), silicon (27.7%27.7\%), aluminum (8.14%8.14\%), iron (5.0%5.0\%), calcium (3.63%3.63\%), sodium (2.83%2.83\%), magnesium (2.09%2.09\%), and potassium (8.14%8.14\%).

9
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What are the chemical formulas of the primary minerals Quartz, Orthoclase, Na-plagioclase, and Ca-plagioclase?

Quartz is SiO2SiO_2, Orthoclase is KAlSi3O8KAlSi_3O_8, Na-plagioclase is NaAlSi3O8NaAlSi_3O_8, and Ca-plagioclase is CaAl2Si3O8CaAl_2Si_3O_8.

10
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What are the chemical formulas of the primary minerals Muscovite, Biotite, Hornblende, Augite, and Apatite?

Muscovite is KAl3Si3O10(OH)2KAl_3Si_3O_{10}(OH)_2, Biotite is K(Mg,Fe)AlSi3O10(OH)2K(Mg, Fe)AlSi_3O_{10}(OH)_2, Hornblende is Ca2Al2Mg2Fe3Si6O22(OH)2Ca_2Al_2Mg_2Fe_3Si_6O_{22}(OH)_2, Augite is Ca2(Al,Fe)4(Mg,Fe)4Si6O24Ca_2(Al, Fe)_4(Mg, Fe)_4Si_6O_{24}, and Apatite is Ca5(PO4)3(OH)(Cl,F)Ca_5(PO_4)_3(OH)\cdot(Cl, F).

11
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What are the chemical formulas of the secondary minerals Calcite, Dolomite, Gypsum, Limonite, and Hematite?

Calcite is CaCO3CaCO_3, Dolomite is CaMg(CO3)2CaMg(CO_3)_2, Gypsum is CaSO42H2OCaSO_4 \cdot 2H_2O, Limonite is Fe2SO33H2OFe_2SO_3 \cdot 3H_2O, and Hematite is Fe2O3Fe_2O_3.

12
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How do extrusive and intrusive igneous rock formations differ?

Extrusive (volcanic) formation occurs when magma is ejected onto the Earth's surface and cools rapidly, forming fine-grained rocks like basalt and andesite. Intrusive (plutonic) formation occurs when magma solidifies slowly inside the crust, forming coarse-grained rocks like granite, diorite, and gabbro.

13
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What are the main chemical weathering processes affecting rocks and minerals?

  1. Hydrolysis: Reaction with water forming acid and base. 2. Hydration: Rigid attachment of water molecules without structural destruction. 3. Oxidation: Transformation of iron from ferrous to ferric form. 4. Carbonation: Reaction with carbonic acid (H2CO3H_2CO_3). 5. Solution: Dissolution of minerals into component ions.
14
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What is the difference between residual and transported parent materials, and how are transported materials classified?

Residual (sedentary) materials develop in place from underlying rock. Transported materials are moved by agents: running water (alluvium), lakes (lacustrine), oceans (marine), glaciers (glacial till/moraine), wind (aeolian), or gravity (colluvium).

15
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What do the soil development processes Melanization, Illuviation, Lessivage, Podzolization, and Laterization refer to?

Melanization is organic matter admixing that darkens mineral soil; Illuviation is material deposition into a lower layer; Lessivage is fine mineral particle washing from A to B horizon; Podzolization (silication) translocates Fe/Al/organic matter concentrating silica; Laterization (desilication) removes silica concentrating Fe/Al oxides (sesquioxides).

16
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<p>Which master soil horizons are shown in this soil profile diagram?</p>

Which master soil horizons are shown in this soil profile diagram?

The diagram depicts horizon O (humus or organic), A (topsoil), E (eluviated horizon), B (subsoil), C (parent material), and R (bedrock).

17
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What is the difference between Solum and Regolith?

Solum refers to the upper layers (AA and BB horizons) where soil formation is active. Regolith refers to the entire loose mantle of weathered rock and soil above bedrock (AA, BB, and CC horizons).

18
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What are the particle size ranges for sand, silt, and clay separates defined by the International Soil Science Society (ISSS)?

Sand ranges from 2.0mm2.0\,mm to 0.02mm0.02\,mm, silt ranges from 0.02mm0.02\,mm to 0.002mm0.002\,mm, and clay is less than 0.002mm0.002\,mm.

19
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What are the five USDA subgroups for sand particles based on size?

  1. Very coarse sand (2.01.0mm2.0 - 1.0\,mm) 2. Coarse sand (1.00.5mm1.0 - 0.5\,mm) 3. Medium sand (0.50.25mm0.5 - 0.25\,mm) 4. Fine sand (0.250.10mm0.25 - 0.10\,mm) 5. Very fine sand (0.100.05mm0.10 - 0.05\,mm)
20
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What is Stoke's Law equation as applied to mechanical soil textural analysis?

The equation is V=KD2V = K D^2, where VV is settling velocity (cm/mincm/min), KK is a constant (60006000 at 25C25^\circ\text{C}), and DD is particle diameter (mmmm).

21
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<p>Which diagram is used to determine soil textural classification based on percentages of sand, silt, and clay?</p>

Which diagram is used to determine soil textural classification based on percentages of sand, silt, and clay?

The Soil Textural Diagram, which plots Percent Clay, Percent Silt, and Percent Sand to define 12 textural soil classes.

22
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<p>How are loam, clay loam, and clay differentiated in the roll method based on ribbon length?</p>

How are loam, clay loam, and clay differentiated in the roll method based on ribbon length?

Types of loam form ribbons 2.5cm\le 2.5\,cm; types of clay loam form ribbons 2.55cm2.5 - 5\,cm; types of clay form ribbons 5cm\ge 5\,cm.

23
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Why do calcium ions (Ca2+Ca^{2+}) promote soil aggregation while sodium ions (Na+Na^+) cause soil dispersion?

Calcium ions (Ca2+Ca^{2+}) have a smaller hydrated size and double positive charge, allowing them to come close to clay surfaces, neutralize negative charges, and form aggregates (floccules). Sodium ions (Na+Na^+) have a larger hydrated radius and single positive charge, failing to neutralize charges and causing clay particles to repel.

24
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<p>Which type of soil structure is illustrated in this diagram?</p>

Which type of soil structure is illustrated in this diagram?

Granular structure, which consists of rounded, porous aggregates characteristic of surface soils with high organic matter.

25
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<p>Which type of soil structure is illustrated in this diagram?</p>

Which type of soil structure is illustrated in this diagram?

Subangular blocky structure, consisting of cube-like aggregates with somewhat rounded edges.

26
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<p>Which type of soil structure is illustrated in this diagram?</p>

Which type of soil structure is illustrated in this diagram?

Angular blocky structure, characterized by cube-like aggregates with sharp edges and distinct rectangular faces.

27
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<p>Which soil structural types are shown from left to right in this diagram?</p>

Which soil structural types are shown from left to right in this diagram?

Prismatic structure (pillar-like with level tops), Columnar structure (pillar-like with rounded tops), and Platy structure (disc-like horizontal aggregates).

28
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What is the formula for calculating Soil Bulk Density (BDBD)?

The formula is BD=WsVtBD = \frac{W_s}{V_t}, where WsW_s is oven-dry weight of soil (gg) and VtV_t is total soil volume (cm3cm^3), expressed in g/cm3g/cm^3.

29
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What is the formula for calculating Soil Particle Density (PDPD)?

The formula is PD=WsVsPD = \frac{W_s}{V_s}, where WsW_s is oven-dry weight of soil solids (gg) and VsV_s is volume of soil solids (cm3cm^3), expressed in g/cm3g/cm^3.

30
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What is the formula to calculate percent soil porosity (PSPS) from bulk density (BDBD) and particle density (PDPD)?

The formula is PS=(1BDPD)×100PS = \left(1 - \frac{BD}{PD}\right) \times 100.

31
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<p>What molecular properties shown in this diagram explain why water molecules are dipolar?</p>

What molecular properties shown in this diagram explain why water molecules are dipolar?

Hydrogen atoms attach to the oxygen atom at an angle of 105105^\circ, making the hydrogen side electropositive (+pole+\text{pole}) and the oxygen side electronegative (pole-\text{pole}).

32
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What are the definitions of adhesion, cohesion, and osmosis in soil water dynamics?

Cohesion is the attraction between water molecules. Adhesion is the attraction between water molecules and solid surfaces. Osmosis is the attraction between water molecules and solutes.

33
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What are the Soil Moisture Tension (SMT) values at Hygroscopic Coefficient, Permanent Wilting Point, and Field Capacity?

Hygroscopic coefficient is held at 31atm31\,atm (or bars); Permanent Wilting Point (PWPPWP) is held at 15bars15\,bars; Field Capacity (FCFC) is held at 13bar\frac{1}{3}\,bar.

34
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How is plant available water (AWAW) in soil calculated?

Available water is calculated as AW=FCPWPAW = FC - PWP, where FCFC is moisture content at field capacity and PWPPWP is moisture content at permanent wilting point.

35
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What are the three components of the Munsell Soil Color Chart and what does each indicate?

  1. Hue: Dominant spectral color (e.g., 10YR10YR). 2. Value: Lightness or darkness of color ranging from 11 (dark) to 88 (light). 3. Chroma: Purity or strength of color ranging from 11 (pale) to 88 (bright).