Soil Science & Fertilizer Chemistry Flashcards
7 cards from real CFA 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 & Fertilizer Chemistry flashcards as text
Which form of phosphorus is most available for plant uptake in the soil solution?
Answer: H2PO4-
H2PO4- (dihydrogen phosphate) is the dominant plant-available form in the slightly acid to neutral pH range (6.0–7.0) where P availability peaks.
Sulfur deficiency symptoms in plants most closely resemble deficiency of which other nutrient?
Answer: Nitrogen
Both sulfur and nitrogen deficiencies cause yellowing (chlorosis) of leaves, but sulfur deficiency appears first on younger leaves while nitrogen deficiency starts on older leaves.
The bulk density of a compacted soil is 1.6 g/cm³. Assuming particle density of 2.65 g/cm³, what is the total porosity?
Answer: About 40%
Porosity = (1 - Db/Dp) × 100 = (1 - 1.6/2.65) × 100 ≈ 39.6%, approximately 40%.
Which soil order is characterized by a spodic horizon containing illuviated organic matter, aluminum, and iron?
Answer: Spodosols
Spodosols are defined by their spodic horizon (Bs or Bhs), where leached humus, Al, and Fe accumulate in a distinct subsurface layer.
When diammonium phosphate (DAP, 18-46-0) dissolves near a seed, the pH of the fertilizer band temporarily:
Answer: Rises to approximately 8
DAP dissolution releases NH3 gas initially, raising the localized pH to about 7.5–8.5 before nitrification proceeds.
Which soil property is MOST directly measured by a standard lime requirement test?
Answer: Buffering capacity against pH change
Lime requirement tests (such as the Shoemaker-McLean-Pratt buffer test) measure the soil's buffering capacity to determine how much lime is needed to raise pH to a target level.
In waterlogged (anaerobic) soils, nitrate nitrogen is most likely to be lost through:
Answer: Denitrification to N2 gas
Denitrification by anaerobic bacteria converts NO3- to N2O and N2 gases, which escape to the atmosphere in waterlogged, oxygen-depleted soils.