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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.

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  1. 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.

  2. 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.

  3. 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%.

  4. 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.

  5. 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.

  6. 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.

  7. 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.