題目 1 · Resource-based 結構題
7 分Resource 1A shows data from a storm hydrograph recorded for the River Faughan following a heavy rainstorm. The rainstorm began at 08:00 and peak rainfall intensity occurred at 11:00. River discharge began to rise at 09:30, reached a peak discharge of 42 cumecs at 15:00, and returned to its pre-storm base flow of 6 cumecs by 06:00 the following day.
(a) Using Resource 1A, calculate the lag time for this storm event, showing your working. [2]
(b) Describe and explain TWO drainage basin characteristics (other than precipitation) that would produce a short lag time and a high peak discharge (a 'flashy' hydrograph). [5]
(a) Using Resource 1A, calculate the lag time for this storm event, showing your working. [2]
(b) Describe and explain TWO drainage basin characteristics (other than precipitation) that would produce a short lag time and a high peak discharge (a 'flashy' hydrograph). [5]
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解題
(a) Lag time is the time interval between peak rainfall intensity and peak discharge. Peak rainfall occurred at 11:00; peak discharge occurred at 15:00. Lag time \( = 15{:}00 - 11{:}00 = 4 \) hours.
(b) Impermeable geology (e.g. clay or granite): where the underlying rock does not allow water to infiltrate, precipitation is forced to travel as rapid surface (overland) flow rather than infiltrating and moving slowly as throughflow or groundwater flow. This gets water to the channel very quickly, shortening lag time and increasing peak discharge.
Steep relief/slope angle: on steep slopes, gravity accelerates the rate of overland flow and throughflow towards the channel, again reducing the time taken for water to reach the river and producing a higher, sharper peak discharge.
(Other valid factors: small, circular basin shape which concentrates flow at a single point simultaneously; high drainage density providing many channels to quickly collect water; sparse vegetation/urbanisation with impermeable surfaces reducing interception and infiltration.) Final answer: lag time \(=4\) hours; any two well-explained basin characteristics (e.g. impermeable geology, steep relief) that speed the delivery of water to the channel.
(b) Impermeable geology (e.g. clay or granite): where the underlying rock does not allow water to infiltrate, precipitation is forced to travel as rapid surface (overland) flow rather than infiltrating and moving slowly as throughflow or groundwater flow. This gets water to the channel very quickly, shortening lag time and increasing peak discharge.
Steep relief/slope angle: on steep slopes, gravity accelerates the rate of overland flow and throughflow towards the channel, again reducing the time taken for water to reach the river and producing a higher, sharper peak discharge.
(Other valid factors: small, circular basin shape which concentrates flow at a single point simultaneously; high drainage density providing many channels to quickly collect water; sparse vegetation/urbanisation with impermeable surfaces reducing interception and infiltration.) Final answer: lag time \(=4\) hours; any two well-explained basin characteristics (e.g. impermeable geology, steep relief) that speed the delivery of water to the channel.
評分準則
(a) [M1] correctly identify times of peak rainfall and peak discharge; [A1] correct lag time of 4 hours with units. (b) For each of two factors: [1] correct factor named; [1] clear explanation of the mechanism linking the factor to rapid water delivery/short lag time; up to [2] marks per factor's development where greater detail/geographical reasoning is shown, to a maximum of [5] across the two factors. Accept any two valid, distinct drainage basin characteristics (e.g. geology, relief, basin shape, drainage density, land use/vegetation, degree of urbanisation).