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04-BS-14 · December 2014

Question 7 of 21: Question 3, Part 1: Groundwater Zone Cross-Section

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

04-BS-14 Geology – National Examinations, December 2014. Closed-book exam (Casio/Sharp-approved calculator permitted). The paper format asks for Questions 1–4 plus 1 of the 3 remaining Questions (5, 6 or 7); every question and every part is answered below.

Reference texts: Goodman, Engineering Geology: Rock in Engineering Construction; Freeze & Cherry, Groundwater; Marshak, Earth: Portrait of a Planet.

Question 3, Part 1: Groundwater Zone Cross-Section (6 marks)

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Given. A vertical column of ground from the surface down to some depth below the water table.

Find. A labelled cross-section locating all six named features in correct relative vertical order.

Approach. Everything above the water table is unsaturated (the zone of aeration, subdivided top-to-bottom into the belt of soil moisture, an intermediate vadose zone, and the capillary fringe immediately above the water table); everything below the water table is saturated (the zone of saturation, whose water is the groundwater proper).

Ground surface (d) Belt of soil moisture Intermediate vadose zone (unsaturated) (a) Capillary fringe (b) Zone of aeration (c) Water table (e) Zone of saturation (f) Groundwater fills all pore space
Vertical section: unsaturated zone of aeration (belt of soil moisture → vadose zone → capillary fringe) overlying the water table, above the saturated zone of saturation (groundwater).

The belt of soil moisture is the thin, biologically active near-surface layer from which plant roots draw water; the underlying intermediate (vadose) zone is unsaturated pore space through which infiltrating water percolates downward under gravity; the capillary fringe is a thin zone directly above the water table where water is pulled upward by surface tension into partially saturated pores, forming the transition into full saturation. Together these three constitute the zone of aeration (vadose zone, broadly). The water table is the surface where pore-water pressure equals atmospheric pressure (the top of the saturated zone as normally measured in an open well). Below it, the zone of saturation has every pore, fracture, and void completely filled with water – this water is the groundwater proper, which can be extracted by wells or discharge naturally at springs.

FeaturePosition in section
(d) Belt of soil moistureUppermost, just below ground surface
(b) Zone of aerationEntire unsaturated interval (d, intermediate zone, and a)
(a) Capillary fringeBase of the zone of aeration, directly above the water table
(c) Water tableBoundary between unsaturated and saturated zones
(e) Zone of saturationEverything below the water table
(f) GroundwaterThe water filling the zone of saturation