MK ACADEMIC READING · TEST 021

Real pressure.
Original practice.

Three original passages, 40 questions and 60 minutes. The question logic uses Cambridge-style paraphrasing, distractors and difficulty progression.

60 MINUTES40 QUESTIONS3 PASSAGESACADEMIC

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ACADEMIC READING · MK021Candidate
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Reading Passage 1

Rebuilding the World’s Peatlands

Why restoring wet ground is more complicated than simply adding water

You should spend about 20 minutes on Questions 1–13.

APeatlands are landscapes in which partially decayed plant material accumulates because waterlogged conditions slow the activity of organisms that would normally break it down. They occupy only a small fraction of the Earth’s land surface, yet they contain an exceptionally large store of carbon. In intact bogs and fens, new plant growth adds material at the surface while older remains are preserved below. The result is a soil that may deepen by only millimetres each year but can represent thousands of years of biological history.

BThe same water that protects the carbon also makes peatlands inconvenient for many conventional forms of agriculture and forestry. For centuries, people have cut channels through bogs to lower the water table, creating firmer ground for grazing, crops or tree plantations. Drainage changes the chemistry of the soil. Air enters pores that were previously saturated, microbes become more active, and stored organic matter begins to decompose. Carbon that accumulated slowly over centuries can then return to the atmosphere within decades.

CThe damage is not limited to greenhouse-gas emissions. Dry peat shrinks and can physically subside, leaving fields lower than neighbouring rivers or sea level. In tropical regions, drained peat is also highly vulnerable to fire. Such fires may smoulder below the surface for weeks, releasing smoke over huge areas and making them difficult to extinguish. Repeated burning can remove metres of peat and expose mineral soil that formed long before the wetland itself.

DRestoration usually begins with a deceptively simple objective: keep water in the landscape. Practitioners block drainage ditches, remove pumps or construct low barriers so that rainfall is retained and the water table rises. Yet rewetting is not the same as returning a peatland to its former state. Plants adapted to dry conditions may already dominate, nutrients may have changed, and land surfaces can be too uneven for water to spread naturally. Recovery therefore tends to be gradual and site-specific.

EThis creates a difficult accounting problem. Rewetting normally reduces carbon dioxide emissions from exposed peat, but waterlogged soils can produce methane, a more powerful greenhouse gas over shorter time periods. Methane emissions may increase during the early stages of restoration before plant communities stabilise. Scientists therefore assess several gases over many years rather than declaring a project successful after the first wet season. A restored site may offer clear climate benefits while still producing an initially confusing emissions profile.

FThe social side of restoration can be just as complicated. A drained peatland may support farms, forestry jobs or infrastructure even if its ecological condition is poor. Simply flooding it can remove income from people who did not cause the original drainage. Some projects now pair restoration with paludiculture: the commercial production of crops that tolerate wet soils, such as reeds, mosses or certain berries. The goal is to keep the peat wet while maintaining some economic use of the land.

GThere is growing interest in paying land managers for the carbon benefits of rewetting. In theory, money from climate programmes could make restoration financially competitive with drainage-based agriculture. In practice, calculating the amount of carbon saved is difficult. Emissions vary with water depth, vegetation, temperature and the condition of the peat before work begins. A project also needs evidence that the carbon benefit would not have happened anyway and that future drainage will not reverse it.

HNew monitoring tools may reduce some of this uncertainty. Satellites can detect changes in surface moisture and vegetation across large areas, while sensors on the ground measure water levels and greenhouse gases in detail. Neither approach is sufficient alone. Remote observations cover large territories but do not directly measure every process below the surface; field instruments are precise but expensive to deploy everywhere. Restoration is therefore becoming an exercise in combining ecological knowledge, local livelihoods and several imperfect forms of evidence. Restoration projects also have to work at landscape scale because water ignores ownership boundaries. Blocking a ditch on one parcel may raise water levels on neighbouring land, while a road embankment can prevent a restored area from reconnecting hydrologically with the rest of the bog. Engineers sometimes install adjustable structures so water can be managed during unusually wet seasons. Ecologists, meanwhile, compare restored plots with intact reference sites rather than expecting every location to return to an identical historical condition. This broader perspective has shifted restoration from a narrow engineering task toward long-term management of an entire water system.

Questions 1–6

MATCHING HEADINGS
Choose the correct heading for Paragraphs B–G from the list below.
List of Headings
i.A climate solution with an early complication
ii.Why drainage changes the behaviour of stored carbon
iii.Making wet land economically useful
iv.Damage that continues after the water disappears
v.A straightforward aim with a complex recovery
vi.A financial market limited by measurement problems
vii.An approach that combines two kinds of observation
viii.Why peatlands are easier to farm than forests
ix.Evidence that all restored sites recover at the same speed
QUESTION 1
Paragraph B
QUESTION 2
Paragraph C
QUESTION 3
Paragraph D
QUESTION 4
Paragraph E
QUESTION 5
Paragraph F
QUESTION 6
Paragraph G

Questions 7–10

TRUE / FALSE / NOT GIVEN
Do the following statements agree with the information in Reading Passage 1?
QUESTION 7
Peatlands contain little carbon because they cover only a small area of land.
QUESTION 8
Removing water from peat can eventually cause the ground surface to become lower.
QUESTION 9
A rewetted peatland always reduces every greenhouse-gas emission immediately.
QUESTION 10
Satellite monitoring is more expensive than taking measurements on the ground.

Questions 11–13

SUMMARY COMPLETION
Complete the summary below. Choose ONE WORD ONLY from the passage for each answer.
QUESTION 11
A common restoration measure is to obstruct existing ______ so that less water escapes from the peatland.
QUESTION 12
Where farming must continue, some projects use ______, which relies on crops suited to saturated soils.
QUESTION 13
Researchers also track ______ because this gas can rise during the first phase after rewetting.