Soil Science & Analysis Flashcards
7 cards from real SAF practice questions. Tap to flip, then mark Knew It or Still Learning — missed cards come back until you master them.
Read the first 7 Soil Science & Analysis flashcards as text
Which soil horizon is characterized by the accumulation of leached materials such as clay, iron oxides, and organic matter?
Answer: B horizon
The B horizon (subsoil) is the illuvial zone where materials leached from upper horizons accumulate.
What does a soil pH of 4.5 indicate about a forest soil's nutrient availability?
Answer: Likely deficiency of phosphorus and molybdenum with possible aluminum toxicity
At pH 4.5, phosphorus and molybdenum become unavailable while aluminum and manganese reach toxic levels.
In a forest soil with a bulk density of 1.6 g/cm³, which condition is most likely indicated?
Answer: Compaction or lack of structure
Bulk density above 1.4-1.5 g/cm³ typically indicates compaction, which restricts root growth and water infiltration.
What is the primary function of mycorrhizal fungi in forest soils?
Answer: Extending effective root surface area for water and nutrient uptake
Mycorrhizal fungi form symbiotic associations with tree roots, dramatically increasing the absorptive surface area for phosphorus, water, and other nutrients.
Which soil texture class has the highest water-holding capacity per unit volume?
Answer: Silty clay loam
Fine-textured soils like silty clay loam have abundant small pores that retain water against gravity, giving them the highest water-holding capacity.
What is cation exchange capacity (CEC) and why is it important for forest management?
Answer: The soil's ability to hold positively charged nutrient ions; indicates nutrient retention potential
CEC measures how many cations a soil can hold and exchange with plant roots, directly indicating its fertility and resistance to nutrient leaching.
Which diagnostic horizon defines a Spodosol in USDA soil taxonomy?
Answer: Spodic horizon with accumulated organic matter and aluminum/iron oxides
Spodosols are defined by the presence of a spodic horizon — a subsurface zone of illuvial organic matter and sesquioxides, common under coniferous forests.