CARA'S TIPS
Agricultural Science · Lesson 16

Practical 3: rocks, soil texture, capillarity, water-holding capacity, porosity and pH

WAECNECO

What the syllabus asks

WAEC: rocks (igneous, sedimentary, metamorphic), soil samples (sand, loam, clay), soil properties and experiments: texture (sedimentation), capillarity, water-holding capacity and drainage, porosity, air, water and organic matter, pH, soil profile.

NECO: rocks (igneous, sedimentary, metamorphic), soil samples (sand, loam, clay), soil properties and experiments: texture (sedimentation), capillarity, water-holding capacity and drainage, porosity, air, water and organic matter, pH, soil profile.

What you will learn

Key points

Start here: Rocks as practical specimens

The ecology part of the WAEC practical syllabus begins with rocks. A typical question places three or four rock specimens on the bench (labelled A, B, C, D) and asks you to (a) name each rock, (b) state the class (igneous, sedimentary or metamorphic) to which it belongs, (c) state two observable features you used, and (d) name the soil each tends to form. Nigeria is a good place to learn rocks: about half the country sits on the ancient Basement Complex of granites, gneisses and schists, while the rest is covered by younger sedimentary basins (the Niger Delta, Benue Trough, Sokoto and Chad basins) and a little volcanic basalt.

Rock specimens and how to tell them apartGranite (igneous)coarse crystals: pink/white feldspar, glassy quartzBasalt (igneous)dark, fine-grained, heavy; Jos PlateauSandstone (sed.)sand grains cemented; gritty, layeredShale (sed.)fine, soft, splits into thin layersLimestone (sed.)grey/white; fizzes with dilute acidMarble (meta.)from limestone; crystalline, fizzesQuartzite (meta.)from sandstone; very hard, no fizzGneiss (meta.)banded light and dark mineralsSlate (meta.)from shale; hard, splits into flat sheets

The three classes of rock

Classes of rock
ClassHow formedTypical featuresNigerian examples
Igneouscooling and hardening of molten magma or lavacrystalline; no layers; no fossils; usually hardgranite (Olumo Rock, Abeokuta), granodiorite and gabbro (Zuma Rock, Niger State), basalt (Jos Plateau)
Sedimentarydeposition and cementing of particles, shells or plant remains in layerslayered (strata); may contain fossils; often softer; grains visiblesandstone, shale (Enugu escarpment), limestone (Ewekoro, Ogun State; Obajana, Kogi State)
Metamorphicexisting rock changed by great heat and/or pressurecrystals often aligned or banded; very hardmarble (Igbeti, Oyo State; Jakura, Kogi State), gneiss and schist (Basement Complex)

Remember the parent–product pairs, which examiners love: limestone → marble, sandstone → quartzite, shale → slate, granite → gneiss.

Model answer: rock specimens

Question: Specimens A, B and C are granite, limestone and marble. (a) Classify each. (b) State one observable feature of each. (c) Name a test to distinguish B from A. Model answer: (a) A igneous; B sedimentary; C metamorphic. (b) A: coarse interlocking crystals of pink/white feldspar, glassy quartz and dark mica; B: grey, fine-grained, may contain fossil shells; C: white or banded, sugary crystalline texture. (c) Add a drop of dilute hydrochloric acid: B fizzes (carbon dioxide), A does not.

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Practice questions

1. Granite is a
  1. igneous rock
  2. sedimentary rock
  3. metamorphic rock
  4. soil
Show answer

A: igneous rock
Formed from magma.

2. Sandstone is a
  1. igneous rock
  2. metamorphic rock
  3. mineral
  4. sedimentary rock
Show answer

D: sedimentary rock
Cemented sand.

3. Marble is formed by metamorphism of
  1. sandstone
  2. clay
  3. limestone
  4. granite
Show answer

C: limestone
Heat and pressure.

4. Sandy soil has
  1. small particles
  2. large particles and good drainage
  3. high water-holding capacity
  4. sticky texture
Show answer

B: large particles and good drainage
Gritty feel.

5. Clay soil has
  1. high water-holding capacity
  2. very large particles
  3. poor nutrient retention
  4. gritty feel
Show answer

A: high water-holding capacity
Sticky and plastic when wet.

Key words

Igneous rock
Rock formed by cooling of molten magma or lava.
Sedimentary rock
Rock formed from layers of deposited and cemented particles.
Metamorphic rock
Rock changed by heat and pressure.
Texture
Relative proportions of sand, silt and clay in a soil.
Structure
Arrangement of soil particles into aggregates.
Capillarity
Upward movement of water through fine soil pores.
Water-holding capacity
Amount of water a soil retains after free drainage.
Porosity
Percentage of soil volume occupied by pores.
Bulk density
Oven-dry mass of soil per unit total volume.
Particle density
Density of the solid particles alone (about 2.65 g/cm³).
Soil profile
Vertical section of soil showing its horizons.
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